Environmental Degradation and Transformation of Organic Chemicals (2007)(en)(710s) 0849372410, 978-0-8493-7241-4

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Environmental Degradation and Transformation of Organic Chemicals

Environmental Degradation and Transformation of Organic Chemicals Alasdair H. Neilson and Ann-Sofie Allard

Boca Raton London New York

CRC Press is an imprint of the Taylor & Francis Group, an informa business

CRC Press Taylor & Francis Group 6000 Broken Sound Parkway NW, Suite 300 Boca Raton, FL 33487-2742 © 2008 by Taylor & Francis Group, LLC CRC Press is an imprint of Taylor & Francis Group, an Informa business No claim to original U.S. Government works Printed in the United States of America on acid-free paper 10 9 8 7 6 5 4 3 2 1 International Standard Book Number-10: 0-8493-7241-0 (Hardcover) International Standard Book Number-13: 978-0-8493-7241-4 (Hardcover) This book contains information obtained from authentic and highly regarded sources. Reprinted material is quoted with permission, and sources are indicated. A wide variety of references are listed. Reasonable efforts have been made to publish reliable data and information, but the author and the publisher cannot assume responsibility for the validity of all materials or for the consequences of their use. No part of this book may be reprinted, reproduced, transmitted, or utilized in any form by any electronic, mechanical, or other means, now known or hereafter invented, including photocopying, microfilming, and recording, or in any information storage or retrieval system, without written permission from the publishers. For permission to photocopy or use material electronically from this work, please access www.copyright.com (http:// www.copyright.com/) or contact the Copyright Clearance Center, Inc. (CCC) 222 Rosewood Drive, Danvers, MA 01923, 978-750-8400. CCC is a not-for-profit organization that provides licenses and registration for a variety of users. For organizations that have been granted a photocopy license by the CCC, a separate system of payment has been arranged. Trademark Notice: Product or corporate names may be trademarks or registered trademarks, and are used only for identification and explanation without intent to infringe. Library of Congress Cataloging-in-Publication Data Neilson, Alasdair H. Environmental degradation and transformation of organic chemicals / Alasdair H. Neilson and Ann-Sofie Allard. p. cm. Rev. ed. of: Organic chemicals. c2000. Includes bibliographical references and index. ISBN 978-0-8493-7241-4 (alk. paper) 1. Aquatic organisms--Effect of water pollution on. 2. Organic water pollutants--Environmental aspects. I. Allard, Ann-Sofie. II. Neilson, Alasdair H. Organic chemicals. III. Title. QH545.W3N45 2008 577’.14--dc22 Visit the Taylor & Francis Web site at http://www.taylorandfrancis.com and the CRC Press Web site at http://www.crcpress.com

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Contents Preface ............................................................................................................................................xix Acknowledgments ........................................................................................................................ xxiii Authors ...........................................................................................................................................xxv

SECTION I Degradation and Transformation Processes Chapter 1

Abiotic Reactions .........................................................................................................3

Introduction........................................................................................................................................3 Photochemical Reactions in Aqueous and Terrestrial Environments ...............................................3 The Diversity of Photochemical Transformations .............................................................................4 The Role of Hydroxyl Radicals ..............................................................................................4 Illustrative Examples of Photochemical Transformations in Aqueous Solutions ..................5 Hydroxyl Radicals in the Destruction of Contaminants ....................................................................9 Fenton’s Reagent .....................................................................................................................9 Polyoxometalates (Heteropolyacids) ..................................................................................... 10 Photolytic Degradation on TiO2 ........................................................................................... 10 Other Photochemically Induced Reactions...................................................................................... 11 The Role of Humic Matter: Singlet Dioxygen ................................................................................. 12 Interactions between Photochemical and Other Reactions ............................................................. 13 Reactions in the Troposphere........................................................................................................... 14 Survey of Reactions .............................................................................................................. 15 Survey of Reactants .............................................................................................................. 17 Aliphatic Hydrocarbons ............................................................................................. 17 Aromatic Hydrocarbons............................................................................................. 17 Biogenic Terpenes ...................................................................................................... 17 Reentry of Tropospheric Transformation Products ......................................................................... 18 Halogenated Alkanes and Alkenes....................................................................................... 18 Arenes and Nitroarenes ........................................................................................................20 Alkylated Arenes .................................................................................................................. 21 Sulides and Disulides ......................................................................................................... 21 Chemically Mediated Transformations ........................................................................................... 22 Hydrolysis ............................................................................................................................. 22 Reductive Displacement: Dehalogenation and Desulfurization ...........................................25 Reductive Dehalogenation ...............................................................................................................25 Zero-Valent Metals ...............................................................................................................25 Chromous Chloride ..............................................................................................................26 Porphyrins and Corrins ........................................................................................................26 Thiol Reductants .............................................................................................................................. 27 Reductive Desulfurization ...............................................................................................................28 Reductions Other than Dehalogenation ................................................................................28 Nucleophilic Reactions ......................................................................................................... 29

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Contents

Oxidations ............................................................................................................................. 30 Anodic Oxidation....................................................................................................... 30 Ozone ...................................................................................................................... 30 Hydrogen Peroxide..................................................................................................... 32 Manganese Dioxide ................................................................................................... 32 Sulfate Radicals ......................................................................................................... 32 Halogenation ......................................................................................................................... 32 Thermal Reactions ................................................................................................................34 Gas Phase ...................................................................................................................34 In Water...................................................................................................................... 36 Electrocatalytic Reactions .................................................................................................... 37 References ........................................................................................................................................ 38 Chapter 2

Biotic Reactions.......................................................................................................... 51

Part 1 Microbial Reactions .............................................................................................................. 51 Introduction .......................................................................................................................... 51 Deinitions—Degradation and Transformation .................................................................... 51 Biodegradation of Enantiomers ............................................................................................ 54 Sequential Microbial and Chemical Reactions .................................................................... 55 The Spectrum of Organisms................................................................................................. 57 Bacteria in Their Natural Habitats............................................................................. 57 Marine and Oligotrophic Bacteria ............................................................................. 58 Lithotrophic Bacteria .................................................................................................60 Phototrophic Organisms ............................................................................................ 61 Aerobic and Facultatively Anaerobic Bacteria .......................................................... 62 Bacterial Metabolism of C1 Compounds: Methanotrophs, Methylotrophs, and Related Organisms .............................................................................................. 69 Methane Monooxygenase and Related Systems ........................................................ 69 Anaerobic Bacteria ............................................................................................................... 72 Clostridia.................................................................................................................... 73 Anaerobic Sulfate-Reducing Bacteria ....................................................................... 73 Other Anaerobic Bacteria .......................................................................................... 73 Organisms from Extreme Environments .............................................................................. 74 Psychrophiles ............................................................................................................. 74 Thermophiles ............................................................................................................. 75 Alkaliphiles................................................................................................................ 75 Halophiles .................................................................................................................. 75 Eukaryotic Microorganisms: Fungi and Yeasts ................................................................... 75 Metabolism by Fungi ................................................................................................. 75 Metabolism by Yeasts ................................................................................................ 77 References ............................................................................................................................. 78 Part 2 Reactions Mediated by Higher Organisms ........................................................................... 91 Introduction .......................................................................................................................... 91 Metabolism by Fish .............................................................................................................. 93 Metabolism by Other Organisms.......................................................................................... 95 Mussels ...................................................................................................................... 95 Insects ...................................................................................................................................96 Invertebrates .........................................................................................................................96 Isopods ......................................................................................................................97 Oligochaetes ...............................................................................................................97 Polychaetes .................................................................................................................97

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Higher Plants ........................................................................................................................97 Other Organisms...................................................................................................................99 References ........................................................................................................................... 100 Chapter 3

Mechanistic Aspects ................................................................................................ 103

Part 1 Introduction of Oxygen ....................................................................................................... 103 Monooxygenation ............................................................................................................... 103 Hydroxylation of Alkanes ........................................................................................ 103 Epoxidation of Alkenes ........................................................................................... 104 Cycloalkanone Monooxygenases ............................................................................. 105 Monooxygenation of Aromatic Compounds ............................................................ 106 Reactions of Aromatic Hydrocarbons ..................................................................... 107 Reactions of Hydroxybenzoates and Related Compounds ...................................... 108 Monooxygenation of Phenols ................................................................................... 110 Cytochrome P450 Systems ................................................................................................. 113 Prokaryotic Organisms ............................................................................................ 114 Eukaryotic Organisms ............................................................................................. 116 Dioxygenation ..................................................................................................................... 118 Dioxygenases Involved in Dihydroxylation of Arenes ............................................ 118 Ring-Fission Dioxygenases ...................................................................................... 123 Incorporation of Oxygen from Water: Oxidoreductases and Hydratases........................... 129 Oxidoreductases ....................................................................................................... 129 Hydratases ................................................................................................................ 130 Oxidases, Peroxidases, and Haloperoxidases ..................................................................... 131 Oxidases ................................................................................................................... 131 Peroxidases .............................................................................................................. 133 Haloperoxidases ....................................................................................................... 134 References ........................................................................................................................... 135 Part 2 Electron Acceptors Other than Oxygen .............................................................................. 147 Introduction ........................................................................................................................ 147 Oxyanions: Nitrate, Sulfate, Chlorate, Selenate, and Arsenate .......................................... 148 Nitrate and Related Compounds .............................................................................. 148 Sulfate and Related Compounds .............................................................................. 150 Chlorate and Perchlorate.......................................................................................... 150 Selenate and Arsenate .............................................................................................. 151 Metal Cations and Oxyanions ............................................................................................ 152 V(V), Mn(IV), Fe(III), Tc(VII), and U(VI) ............................................................. 152 Humic Acid and Anthraquinone-2,6-Disulfonate in Redox Systems ..................................................................................................... 154 Dehalorespiration................................................................................................................ 156 Alkane Sulfonates as Terminal Electron Acceptors........................................................... 156 Nitroalkanes as Electron Acceptor ..................................................................................... 156 References ........................................................................................................................... 157 Part 3 Reductases and Related Enzymes ....................................................................................... 162 Reduction of Nitroarenes .................................................................................................... 162 Nitrate Ester Reductase ...................................................................................................... 162 Enones (α, β-Unsaturated Ketones) and Related Reductases ............................................. 163 Aerobic Conditions .................................................................................................. 163 Anaerobic Conditions .............................................................................................. 163 Azo Reductase .................................................................................................................... 163

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Aldehyde Oxidoreductases ................................................................................................. 164 F420 -Dependent (Desazatetrahydrofolate) Reductases........................................................ 164 Other Carbocyclic Aromatic Compounds .......................................................................... 164 Reduction of Carbocyclic Rings .............................................................................. 164 Dehydroxylation ....................................................................................................... 165 Reduction of Azaarene Rings .................................................................................. 165 Metal Cations and Oxyanions ............................................................................................ 165 References ........................................................................................................................... 166 Part 4 Microbial Reactions to Chemical Stress ............................................................................. 168 Introduction ........................................................................................................................ 168 Hydrocarbon Tolerance............................................................................................ 168 Antibiotic Resistance ............................................................................................... 170 Resistance to Metals and Metalloids .................................................................................. 172 Reduction ................................................................................................................. 172 Methylation .............................................................................................................. 173 Eflux Systems ......................................................................................................... 175 Chlorophenol Tolerance ........................................................................................... 176 Resistance to High Acidity ...................................................................................... 176 References ........................................................................................................................... 177 Part 5 Enzymes Containing Manganese, Iron, Nickel, Copper, Molybdenum, Tungsten, and Vanadium ..................................................................................................... 181 Manganese .......................................................................................................................... 181 Iron .................................................................................................................................. 181 Nickel .................................................................................................................................. 182 Copper................................................................................................................................. 184 Molybdenum ....................................................................................................................... 185 Molybdopterin Oxidoreductases .............................................................................. 185 Tungsten .............................................................................................................................. 187 Vanadium ............................................................................................................................ 188 References ........................................................................................................................... 188 Chapter 4

Determinants and Interactions ................................................................................. 193

Single Substrates: Several Organisms ........................................................................................... 193 Cometabolism and Related Phenomena......................................................................................... 195 Induction of Catabolic Enzymes .................................................................................................... 195 Pre-Exposure to an Analog Substrate ................................................................................ 195 Enzyme Induction by Growth on Structurally Unrelated Compounds .............................. 197 Role of Readily Degraded Substrates ............................................................................................ 198 Physical Parameters .......................................................................................................................200 Temperature ........................................................................................................................200 Oxygen Concentration ........................................................................................................ 201 Anaerobic Bacteria ..................................................................................................202 Aerobic and Facultatively Anaerobic Organisms ....................................................202 Redox Potential ...................................................................................................................205 Association of Bacteria with Particulate Material: “Free” and “Bound” Substrates .............................................................................................................205 Biological Mechanisms for Association with Organic Components of Soil and Sediment ...........................................................................................................206 Aging ..................................................................................................................................208

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Substrate Concentration, Transport into Cells, and Toxicity ......................................................... 210 Utilization of Low Substrate Concentrations ..................................................................... 211 Existence of Threshold Concentrations .............................................................................. 212 Strategies Used by Cells for Substrates with Low or Negligible Water Solubility ............ 213 Transport Mechanisms ....................................................................................................... 214 Pre-Exposure: Pristine and Contaminated Environments ............................................................. 215 Rates of Metabolic Reaction .......................................................................................................... 218 Kinetic Aspects................................................................................................................... 218 Metabolic Aspects: Nutrients......................................................................................................... 219 Regulation and Toxic Metabolites ................................................................................................. 220 Regulation ........................................................................................................................... 220 Toxic or Inhibitory Metabolites .......................................................................................... 222 Catabolic Plasmids.........................................................................................................................224 References ...................................................................................................................................... 227

SECTION II Experimental Procedures Chapter 5

General Experimental Procedures ........................................................................... 245

Introduction.................................................................................................................................... 245 Abiotic Reactions ................................................................................................................ 245 Microbial Reactions ............................................................................................................246 Storage of Samples ............................................................................................................. 247 Determination of Ready Biodegradability ......................................................................... 247 The Inoculum ...........................................................................................................248 Concentration of the Substrate.................................................................................248 Endpoints .................................................................................................................248 Design of Experiments on Inherent Biodegradability ........................................................248 Metabolic Limitations..............................................................................................248 Application to Marine Systems................................................................................ 249 Isolation and Elective Enrichment ........................................................................... 249 General Procedures .................................................................................................. 250 Basal Media ............................................................................................................. 252 Mineral Media ......................................................................................................... 252 Trace Elements ......................................................................................................... 253 Control of pH ...........................................................................................................254 Vitamins...................................................................................................................254 Sterilization ..............................................................................................................254 Metal Concentration in Metabolism ........................................................................254 Redox Potential of Media ........................................................................................ 256 Organic Substrates .............................................................................................................. 256 Toxic Compounds .................................................................................................... 256 Volatile Compounds................................................................................................. 257 Solid Media ......................................................................................................................... 257 Growth at the Expense of Alternative Substrates ............................................................... 258 Techniques for Anaerobic Bacteria .................................................................................... 258 Design of Experiments on Biodegradation and Biotransformation ................................... 259 Pure Cultures and Stable Consortia.................................................................................... 259 Cell Growth at the Expense of the Xenobiotic ...................................................................260

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Stable Enrichment Cultures ................................................................................................260 Use of Dense Cell Suspensions........................................................................................... 261 Use of Immobilized Cells ................................................................................................... 261 Application of Continuous Culture Procedures.................................................................. 262 Simultaneous Presence of Two Substrates ......................................................................... 263 Use of Unenriched Cultures: Undeined Natural Consortia ...............................................264 Microcosm Experiments.....................................................................................................264 Experiments in Models of Natural Aquatic Systems .........................................................266 Evaluation of Degradation Using Metabolites.................................................................... 267 Experimental Problems: Water Solubility, Volatility, Sampling, and Association of the Substrate with Microbial Cells ........................................... 268 References ...................................................................................................................................... 269

Chapter 6

Elucidation of Metabolic Pathways .......................................................................... 277

Introduction.................................................................................................................................... 277 Part 1 Application of Natural and Synthetic Isotopes ................................................................... 277 Carbon (14C and 13C)........................................................................................................... 277 Sulfur (35S) and Chlorine (36Cl) .......................................................................................... 278 Hydrogen (2H) and Oxygen (18O) ........................................................................................ 278 Other Isotopes .....................................................................................................................280 Isotope Effects and Stable Isotope Fractionation ...............................................................280 Experimental Procedures......................................................................................... 282 References ........................................................................................................................... 282 Part 2 Nondestructive Methods for Structure Determination .......................................................284 Application of NMR ...........................................................................................................284 Hydrogen 1H ............................................................................................................ 285 Carbon 13C ............................................................................................................... 285 Nitrogen 15N ............................................................................................................. 286 Oxygen 17O ............................................................................................................... 287 Fluorine 19F .............................................................................................................. 287 Phosphorus 31P ......................................................................................................... 288 Silicon 29Si ............................................................................................................... 288 Application of EPR ............................................................................................................. 288 Elucidation of the Unexpected Complexity of an Apparently Straightforward Metabolic Pathway ..................................................................................... 289 Hydroxyl Radicals and Their Role in the Toxicity of H2O2 to Bacteria ......................................................................................... 289 Elucidation of the Mechanism of Pyruvate Formate Lyase........................................................................................................... 289 The Function of Humic Acids in Reactions Catalyzed by Geobacter metallireducens .......................................................................................... 289 The Mechanism of Anaerobic Activation of Toluene .............................................. 289 Dioxygenation with Elimination of Halide .............................................................. 289 The Anaerobic Degradation of Benzoate ................................................................290 Manganese-Containing Enzymes ............................................................................ 290 Turnover of Naphthalene Dioxygenase ....................................................................290 Enzyme Structure ...............................................................................................................290 References ........................................................................................................................... 291

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SECTION III Pathways and Mechanisms of Degradation and Transformation Chapter 7

Aliphatic Compounds............................................................................................... 297

Part 1 Alkanes and Related Compounds ....................................................................................... 297 Alkanes ............................................................................................................................... 297 Aerobic Conditions .................................................................................................. 297 Anaerobic Conditions ..............................................................................................304 Alkenes ............................................................................................................................... 305 Aerobic Conditions .................................................................................................. 305 Anaerobic Conditions ..............................................................................................308 Alkynes ...............................................................................................................................308 Alkanols ..............................................................................................................................309 Aerobic Conditions ..................................................................................................309 Anaerobic Conditions .............................................................................................. 310 Alkanones ........................................................................................................................... 310 Alkylamines and Amino Acids .......................................................................................... 311 Aerobic Conditions .................................................................................................. 311 Anaerobic Conditions .............................................................................................. 316 Alkanoic Acids ................................................................................................................... 317 Aerobic Conditions .................................................................................................. 317 Anaerobic Conditions .............................................................................................. 318 Anaerobic Conditions .............................................................................................. 318 Amides and Related Compounds ....................................................................................... 321 Amides .................................................................................................................... 321 Nitriles ................................................................................................................................ 322 Isonitriles ............................................................................................................................ 322 Sulfonylureas and Thiocarbamates .................................................................................... 322 Carbon Monoxide ............................................................................................................... 323 Cyanide ............................................................................................................................... 323 Thiocyanate ........................................................................................................................ 324 References ........................................................................................................................... 324 Part 2 Cycloalkanes ....................................................................................................................... 336 Monoterpenes ..................................................................................................................... 339 Steroids ............................................................................................................................... 341 Hydroxylation........................................................................................................... 341 Other Aerobic Transformations and Degradation ................................................... 341 Anaerobic Transformation ....................................................................................... 343 Diterpenoids........................................................................................................................344 Polycyclic Substrates ..........................................................................................................344 References ...........................................................................................................................346 Part 3 Alkanes, Cycloalkanes and Related Compounds with Chlorine, Bromine, or Iodine Substituents ......................................................................................................................... 349 Chlorinated, Brominated, and Iodinated Alkanes, Alkenes, and Alkanoates ................... 349 Elimination Reactions.............................................................................................. 350 Corrinoid Pathways .................................................................................................. 355 Nucleophilic Substitution: Hydrolytic Reactions of Halogenated Alkanes and Alkanoates ....................................................... 358

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Glutathione-Mediated and Other Reactions Involving Nucleophilic Sulfur .................................................................................... 363 Monooxygenation..................................................................................................... 363 Reductive Reactions: Dehalogenation Including Dehalorespiration ....................... 366 References ........................................................................................................................... 370 Part 4 Fluorinated Aliphatic Compounds ...................................................................................... 378 Alkanes and Alkenes .......................................................................................................... 378 Fluorohydrocarbons ................................................................................................. 378 Chloroluorocarbons and Hydrochloroluorocarbons .............................................. 379 Carboxylic Acids...................................................................................................... 380 Perluoroalkyl Carboxylates and Sulfonates ............................................................ 382 References ........................................................................................................................... 382

Chapter 8

Carbocyclic Aromatic Compounds without Halogen Substituents .......................... 385

Part 1 Monocyclic Aromatic Hydrocarbons .................................................................................. 385 Introduction ........................................................................................................................ 385 Monocyclic Arenes ............................................................................................................. 385 Aerobic Conditions .................................................................................................. 385 Anaerobic Conditions .............................................................................................. 389 Synthetic Applications ............................................................................................. 392 References ........................................................................................................................... 394 Part 2 Polycyclic Aromatic Hydrocarbons (PAHs)........................................................................ 398 Introduction ........................................................................................................................ 398 Aerobic Reactions Carried Out by Bacteria ............................................................ 399 PAHs with Three or More Rings .............................................................................402 Anaerobic Reactions Carried Out by Bacteria ........................................................408 Fungal Transformations ...........................................................................................409 White-Rot Fungi ...................................................................................................... 413 References ........................................................................................................................... 417 Part 3 Aromatic Carboxylates, Carboxaldehydes, and Related Compounds ................................ 424 Introduction ........................................................................................................................ 424 Benzoates ............................................................................................................................ 424 Aerobic Conditions .................................................................................................. 424 Hydroxybenzoates and Related Compounds ...................................................................... 425 Mechanisms for Fission of Oxygenated Rings ........................................................ 428 Alternative Pathways for the Degradation of Benzoates and Related Compounds............................................................................. 432 Aerobic Reduction of Arene Carboxylates ......................................................................... 433 Arenes with an Oxygenated C2 or C3 Side Chain ............................................................... 433 Anaerobic Metabolism ............................................................................................. 435 Aldehydes ........................................................................................................................... 439 References ........................................................................................................................... 439 Part 4 Nonhalogenated Phenols and Anilines ...............................................................................446 Phenols ................................................................................................................................446 Aerobic Degradation ................................................................................................446 Anaerobic Degradation ............................................................................................449 Anilines.................................................................................................................... 452 References ........................................................................................................................... 452

Contents

Chapter 9

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Substituted Carbocyclic Aromatic Compounds ....................................................... 455

Part 1 Halogenated Arenes and Carboxylates with Chlorine, Bromine, or Iodine Substituents.......................................................................................................... 455 Introduction ........................................................................................................................ 455 Halogenated Arene Hydrocarbons ..................................................................................... 455 Aerobic Conditions .................................................................................................. 455 Monocyclic Chlorinated Arenes ......................................................................................... 456 Anaerobic Conditions .............................................................................................. 458 Polychlorinated Biphenyls .................................................................................................. 458 Aerobic Degradation ................................................................................................ 458 Degradation Is Initiated by Dioxygenation .............................................................. 459 Ring Fission by 2,3-Dihydroxybiphenyl Dioxygenase ............................................ 461 Metabolites............................................................................................................... 463 Fungal Dehalogenation .......................................................................................................465 Reductive Dehalogenation ..................................................................................................465 The Role of Temperature .........................................................................................466 Polyhalogenated Dioxins and Diphenyl Ethers........................................................468 Halogenated Benzoates.......................................................................................................468 Dioxygenation ..........................................................................................................469 Hydrolytic Reactions................................................................................................ 472 Mechanisms for the Ring Fission of Substituted Catechols ............................................... 472 Reductive Loss of Halogen ...................................................................................... 474 Halogenated Phenylacetates ............................................................................................... 475 Fungal Reactions...................................................................................................... 476 References ........................................................................................................................... 476 Part 2 Halogenated (Chlorine, Bromine, and Iodine) Phenols and Anilines ........................................................................................................................ 482 Phenols ................................................................................................................................ 482 Aerobic Conditions .................................................................................................. 482 Fungi and Yeasts ...................................................................................................... 486 Anaerobic Conditions .............................................................................................. 487 Anilines .............................................................................................................................. 489 Aerobic Conditions .................................................................................................. 489 Anaerobic Conditions .............................................................................................. 490 References ........................................................................................................................... 491 Part 3 Fluorinated Hydrocarbons, Carboxylates, Phenols, and Anilines ...................................... 494 Fluorinated Aromatic Hydrocarbons.................................................................................. 494 Aerobic Conditions .................................................................................................. 494 Metabolism by Yeasts and Fungi ............................................................................. 495 Anaerobic Denitrifying Conditions ......................................................................... 495 Fluorobenzoates .................................................................................................................. 496 Aerobic Conditions .................................................................................................. 496 Diluorobenzoates .................................................................................................... 498 Degradation under Denitrifying Conditions ............................................................ 499 Fluorinated Phenols ............................................................................................................500 Aerobic Conditions ..................................................................................................500 Anaerobic Conditions .............................................................................................. 501 Aromatic Triluoromethyl Compounds ..............................................................................502 References ........................................................................................................................... 503

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Part 4 Arene Sulfonates .................................................................................................................506 References ...........................................................................................................................508 Part 5 Aromatic Compounds with Nitro Substituents ...................................................................508 Nitroarenes..........................................................................................................................508 Reduction of Nitro Groups.......................................................................................509 Reduction of the Ring .............................................................................................. 512 Dioxygenation .......................................................................................................... 512 Side-Chain Oxidation .............................................................................................. 513 Peroxidase Oxidation ............................................................................................... 513 Nitrobenzoates .................................................................................................................... 514 Nitrophenols........................................................................................................................ 514 References ........................................................................................................................... 517 Part 6 Azoarenes ............................................................................................................................ 520 References ........................................................................................................................... 521 Chapter 10

Heterocyclic Aromatic Compounds ....................................................................... 523

Part 1 Azaarenes ............................................................................................................................ 523 Five-Membered Monocyclic Aza, Oxa, and Thiaarenes .................................................... 523 Aerobic Conditions .................................................................................................. 523 Indole and Carbazole .......................................................................................................... 524 Indole and 3-Alkylindoles ....................................................................................... 524 Carbazole ................................................................................................................. 527 Pyridine .............................................................................................................................. 527 Aerobic Conditions .................................................................................................. 527 Anaerobic Conditions .............................................................................................. 534 Quinoline and Isoquinoline ................................................................................................ 536 Bacterial Metabolism ............................................................................................... 536 Hydroxylation........................................................................................................... 537 Dioxygenation .......................................................................................................... 537 Pyrimidine and Related Compounds Excluding Purines ...................................................540 Aerobic Conditions ..................................................................................................540 Anaerobic Conditions .............................................................................................. 541 Purines ................................................................................................................................ 542 Aerobic Degradation ................................................................................................ 542 Anaerobic Degradation ............................................................................................ 542 Ring-Fission Reactions ............................................................................................544 Triazines ............................................................................................................................. 545 1,3,5-Triazines.......................................................................................................... 545 1,2,4-Triazines..........................................................................................................546 References ...........................................................................................................................546 Part 2 Oxaarenes ............................................................................................................................ 553 Aerobic Conditions ............................................................................................................. 553 Monocyclic Oxaarenes............................................................................................. 553 Polycyclic Oxaarenes ............................................................................................... 553 References ........................................................................................................................... 562 Part 3 Thiaarenes: Benzothiophenes, Dibenzothiophenes, and Benzothiazole ............................ 565 Benzothiazole ..................................................................................................................... 567 References ........................................................................................................................... 568

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Chapter 11 Miscellaneous Compounds ...................................................................................... 569 Part 1 Carboxylate, Sulfate, Phosphate, and Nitrate Esters ........................................................... 569 Carboxylates ....................................................................................................................... 569 Sulfates ............................................................................................................................... 569 Phosphates .......................................................................................................................... 570 Nitrates................................................................................................................................ 571 References ........................................................................................................................... 572 Part 2 Ethers and Sulides .............................................................................................................. 573 Aliphatic and Benzylic Ethers ............................................................................................ 573 Aryl Ethers.......................................................................................................................... 576 Diaryl Ethers ............................................................................................................ 576 Aryl-Alkyl Ethers .................................................................................................... 576 Sulides, Disulides, and Related Compounds .................................................................... 578 References ........................................................................................................................... 581 Part 3 Aliphatic Nitramines and Nitroalkanes .............................................................................. 585 Nitramines .......................................................................................................................... 585 Nitroalkanes........................................................................................................................ 585 References ........................................................................................................................... 586 Part 4 Aliphatic Phosphonates and Sulfonates .............................................................................. 588 Introduction ........................................................................................................................ 588 Phosphonates ...................................................................................................................... 588 Sulfonates ........................................................................................................................... 589 Boronates ............................................................................................................................ 591 References ........................................................................................................................... 591 Part 5 Degradation of Organic Compounds of Metals and Metalloids ......................................... 592 Tin .................................................................................................................................. 593 Lead .................................................................................................................................. 593 Mercury .............................................................................................................................. 594 Arsenic ................................................................................................................................ 594 References ........................................................................................................................... 594

SECTION IV

Bioremediation

Chapter 12 Bioremediation: Overview ....................................................................................... 599 Introduction.................................................................................................................................... 599 Strategies............................................................................................................................. 599 Contaminants ......................................................................................................................600 Sites ..................................................................................................................................602 Chemical Procedures ..........................................................................................................602 Phytoremediation ................................................................................................................602 Primary Role of Plants.............................................................................................603 Secondary Role of Plants .........................................................................................605 Degradative Enzymes ..............................................................................................606 The Role of Plant Exudates in Degradation ............................................................607 Other Functions of Bacteria in the Rhizosphere .....................................................607 The Role of Mycorrhizal Fungi ...............................................................................609

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Microbiological Aspects ................................................................................................................ 610 Regulation of Pathways ...................................................................................................... 610 Alternative Electron Acceptors .......................................................................................... 611 Aging .................................................................................................................................. 611 Bioilms............................................................................................................................... 611 Metabolites and Enzymes ................................................................................................... 611 Utilization of Nitrogen, Sulfur, and Phosphorus ................................................................ 612 Substrate Concentration ...................................................................................................... 612 Temperature ........................................................................................................................ 613 References ...................................................................................................................................... 613

Chapter 13 Evaluation of Bioremediation ................................................................................... 621 Introduction.................................................................................................................................... 621 Analysis of Populations ................................................................................................................. 622 Analysis of Degradative Populations.................................................................................. 622 Application to the Degradation of Speciic Contaminants................................................. 623 Hydrocarbons ........................................................................................................... 623 Trichloroethene ........................................................................................................ 624 Phenol .................................................................................................................... 624 Chlorophenol............................................................................................................ 625 Chlorobenzoate ........................................................................................................ 625 Phenylurea Herbicides ............................................................................................. 625 Dehalogenation of Chloroalkanoates....................................................................... 626 Dechlorination of PCBs ........................................................................................... 626 Application to Speciic Groups of Organisms .................................................................... 626 Nondirected Examination of Natural Populations ............................................................. 627 Application of Stable Isotopes ....................................................................................................... 627 Stable Isotope Probes.......................................................................................................... 627 Application of Stable Isotope Enrichment.......................................................................... 628 Application of δ13C .................................................................................................. 629 References ...................................................................................................................................... 633

Chapter 14 Applications of Bioremediation ............................................................................... 639 Introduction.................................................................................................................................... 639 Part 1 Petroleum Hydrocarbons: Reinery Waste and Stranded Oil.............................................. 639 Terrestrial Habitats .............................................................................................................640 Alkanes ....................................................................................................................640 Naphthenates ............................................................................................................ 641 Marine Habitats .................................................................................................................. 641 The Bafin Island Oil Spill Project .......................................................................... 641 Conclusion .......................................................................................................................... 642 References ........................................................................................................................... 642 Part 2 Coal Distillation Products ................................................................................................... 643 Introduction ........................................................................................................................ 643 On-Site or Off-Site Treatment ............................................................................................644 The Physical State of the Contaminant ..............................................................................646

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Environmental Parameters ................................................................................................. 647 Determinants ...................................................................................................................... 647 The Range of Substrates .......................................................................................... 647 The Range of Degradative Bacteria .........................................................................648 Bioavailability and the Use of Surfactants ..............................................................649 Supplementation with Fungi ............................................................................................... 650 Application of Higher Plants .............................................................................................. 652 Anoxic or Anaerobic Environments ................................................................................... 652 Hydrocarbons ........................................................................................................... 652 Phenols .................................................................................................................... 652 Heteroarenes ............................................................................................................ 653 Abiotic Transformations ..................................................................................................... 653 Conclusions ......................................................................................................................... 654 References ........................................................................................................................... 654 Part 3 Wood Preservation Sites: Chlorophenolic Compounds ...................................................... 658 Aerobic Bacteria ................................................................................................................. 659 Degradation by Fungi ......................................................................................................... 659 Anaerobic Dechlorination ..................................................................................................660 Conclusion ..........................................................................................................................660 References ...........................................................................................................................660 Part 4 Chemical Waste................................................................................................................... 661 Chlorinated Alicyclic Hydrocarbons .................................................................................. 662 Chlorinated and Brominated Aromatic Hydrocarbons ...................................................... 662 Chlorobenzenes .................................................................................................................. 662 DDT .................................................................................................................................. 663 Polychlorinated Biphenyls .................................................................................................. 663 Aerobic Conditions ..................................................................................................664 Anaerobic Conditions ..............................................................................................665 Polybrominated Biphenyls and Diphenyl Ethers ................................................................666 Chlorinated Dibenzodioxins...............................................................................................666 Organoluoro Compounds .................................................................................................. 667 Conclusion ..........................................................................................................................668 References ...........................................................................................................................668 Part 5 Agrochemicals .................................................................................................................... 671 Phenoxyalkanoic Acids....................................................................................................... 672 Chlorinated Anilines .......................................................................................................... 672 Triazines ............................................................................................................................. 673 1,3,5-Triazines.......................................................................................................... 673 1,2,4-Triazines.......................................................................................................... 673 2,4-Dintro-6-sec-Butylphenol (Dinoseb)................................................................. 673 References ........................................................................................................................... 674 Part 6 Military Waste..................................................................................................................... 675 Explosives ........................................................................................................................... 675 Nitroarenes.......................................................................................................................... 675 Nitrodiphenylamines .......................................................................................................... 676 Nitrate Esters ...................................................................................................................... 676 Nitramines .......................................................................................................................... 676 Conclusions ......................................................................................................................... 677 Chemical Warfare Agents .................................................................................................. 677 References ........................................................................................................................... 677

xviii

Contents

Part 7 Groundwater Contamination ............................................................................................... 679 Benzene/Toluene/Ethylbenzene/Xylenes............................................................................ 679 Aerobic Conditions .................................................................................................. 679 Anoxic or Anaerobic Conditions .............................................................................680 Halogenated Alkanes and Alkenes..................................................................................... 682 Tetrachloromethane ................................................................................................. 682 Chloroethenes .......................................................................................................... 682 Aerobic Conditions .................................................................................................. 682 Application of Indigenous Bacteria ......................................................................... 683 Application of Exogenous Bacteria .........................................................................684 Anoxic and Anaerobic Conditions ...........................................................................684 Application of Higher Plants ................................................................................... 685 Conclusion .......................................................................................................................... 686 Methyl tert-Butyl Ether....................................................................................................... 686 References ........................................................................................................................... 687 Finale: A Hierarchical Strategy .....................................................................................................690 I. Laboratory Experiments..................................................................................................690 II. Microcosm Experiments ................................................................................................ 691 III. Large-Scale Operations ................................................................................................ 691 Concluding Comments................................................................................................................... 692 Index .............................................................................................................................................. 693

Preface This volume is an updated and expanded version of a previous edition Organic Chemicals: An Environmental Perspective. This one deals, however, with only degradation and transformation in their widest senses, and the sections in the earlier volumes on analysis, distribution, and ecotoxicology have been omitted since these lie beyond my current competence. In addition, there are specialized volumes that already cover these topics. I have been extremely fortunate in having as coauthor Ann-Soie Allard, who has been a research collaborator for many years. She has been both guide and illustrator, and without her constant help and encouragement, this volume would neither have begun nor would it have come to fruition. Degradation and transformation occupy a central position in assessing the environmental impact of organic contaminants. We have avoided the term “pollutant” on account of its negative connotation. Although phase partition is not discussed, this is an important factor in determining biodegradability since a contaminant will seldom remain in the phase to which it is initially discharged. This must be considered as the following examples illustrate: 1. Compounds deposited as solids (including agrochemicals and contaminants) may reach groundwater and watercourses as a result of partition and leaching. 2. Substances with even marginal volatility will enter the atmosphere, and after transformation may then reenter the aquatic and terrestrial environments through precipitation. 3. Aquatic biota may bring about transformation to metabolites that are then disseminated to a considerable distance from their source. 4. Particularly polar contaminants may associate with polymeric humic components of soil, water, and sediment. Their biodegradation then depends on the degree to which these processes are reversible and the contaminants become accessible to microorganisms (bioavailable). This is especially signiicant after weathering (aging), even for nonpolar compounds. Contaminants seldom consist of single substances. The pathways used for biodegradation of some components may be incompatible with those for others that are present, or the pathway for a single compound. Examples of this are given, though in less detail than they merit. In this volume, emphasis is placed on the pathways by which degradation or transformation has taken place, and the approach is essentially chemical and mechanistic. There are several reasons for this. 1. Biochemical reactions parallel those in organic chemistry and, for both of them, a mechanistic approach has proved valuable. In addition, most of the principles that have emerged apply equally to the aquatic, the atmospheric, and the terrestrial environments. 2. Metabolites may be produced by biochemical transformation of the substrate rather than by degradation, or may result from partial abiotic reactions. These products may be (a) terminal and persistent or (b) toxic to other components of an ecosystem—including the microorganisms that produce them. Both of these represent important considerations that are illustrated by examples in this book. 3. Pathways can provide a guide to the probable reactions that other contaminants may undergo including those that bear only a partial—or even more remote structural resemblance. This is especially important in view of the widening spectrum of contaminants that is the result of the impressive ingenuity of the organic chemist, and particularly for the complexity and novelty of pharmaceutical and agrochemical products. xix

xx

Preface

A word of caution is appropriate. The reactions that are used for illustration are very seldom speciic for a single taxon—or even close relatives, and it is not generally possible to establish the range of organisms that will be able to carry out the reaction. The contents of the chapters are interdependent. In summary they deal with the following: Chapters 1 through 4 provide a broad perspective on abiotic and biotic reactions, including the signiicance of a range of environmental determinants. Chapters 5 and 6 attempt to provide a brief introduction to experimental procedures with emphasis on procedures for establishing the structure of metabolites using isotopes and physical methods. Chapters 7 through 11 outline details of biochemical reactions involved in the biodegradation of the major groups of aliphatic, carbocyclic aromatic, and heterocyclic compounds. Although emphasis is placed on the pathways, rather general accounts of the enzymes involved and the genetics are provided where they are available. Chapters 12 through 14 deal with bioremediation that has attracted increasing concern with the realization of the hazard presented by the disposal of unwanted chemicals, or byproducts from their manufacture. These chapters should be viewed within the wider context of metabolic details that have been presented in Chapters 7 through 11. There are a number of inevitable omissions and limitations in the material that is covered. 1. Emphasis is placed exclusively on xenobiotics, although some of them are also naturally occurring metabolites. There are substantial groups of compounds that are not discussed. These include the following: a. Naturally occurring polymers—cellulose, chitin, lignin, and polyisoprenoids; synthetic polyamides, polyurethanes, and polysiloxanes. b. Natural products including polypyrroles such as hemin and chlorophyll; plant and microbial metabolites. c. Agrochemicals including veterinary chemotherapeutic agents that have come into use in large-scale animal husbandry. d. Pharmaceuticals including hormone disrupters about which there has arisen serious concern. e. Halogenated metabolites produced by marine biota, even though some such as halomethanes, polybrominated phenols, and polybrominated diphenyl ethers are also xenobiotics. It is expected that the pharmaceutical industry that has hitherto been dominated by synthetic products—except for antibiotics—will come to rely increasingly on metabolites produced by marine biota including microorganisms. 2. The number of references that are cited is necessarily restrictive and, although numerous, they represent merely an eclectic selection from a vast literature. Relevant references have no doubt been omitted, but the writers can assure the authors of these that there is no malice in the selection. They invariably refer to the primary literature that has been subjected to the scrutiny of peer review. It is therefore assured that even when the interpretations of the authors should prove faulty—and this is inevitable—a solid and reproducible basis of fact is available to the critical reader. Some older work has been cited when this has led to lasting concepts, though other early work may be dificult to evaluate by the standards of today; and no doubt work at the cutting edge of current research will rightly require modiication and extension in the future. 3. Although some of the examples used for illustration in Chapter 14 impinge on biological wastewater treatment technology, a systematic account of these lies beyond the scope of this volume and the competence of the authors. It is worth noting, however, that anaerobic reactors that are developed to treat wastewater with the object of producing methane may

Preface

xxi

not necessarily degrade recalcitrant xenobiotics for which inoculation with speciic microorganisms may be necessary. 4. No discussion of models will be found in this volume, either for the analysis of degradation kinetics or for the prediction of biodegradability. For these, the interested reader should consult monographs by experts. The nomenclature of bacteria has presented serious problems principally for two reasons: (a) the number of new taxa that are being described appears to be increasing exponentially and (b) it is seldom possible to determine the correct taxonomic assignment for important organisms that have been used in the historical literature. Although no consistent attempt has been made to provide the current assignment for all taxa, we have tried to use those that occur most frequently.

Acknowledgments It is a pleasure to thank Östen Ekengren, director of Environmental Technology and Toxicology for his generosity in extending access to library facilities. We thank Springer Verlag for kind permission to use a number of igures that were used in chapters that we have contributed to Volume 3J (1998), Volume 3N (2002), and Volume 3R (2003) of The Handbook of Environmental Chemistry of which I was volume editor.

xxiii

Authors Alasdair H. Neilson was principal scientist until retirement from IVL Swedish Environmental Research Institute in Stockholm. He studied chemistry at the University of Glasgow and obtained his PhD in organic chemistry from Alexander Todd’s laboratory at Cambridge. He carried out research at Cambridge in organic chemistry, and in theoretical chemistry with Charles Coulson at Oxford. He held academic positions in the universities of Glasgow and Sussex, and obtained industrial experience in the pharmaceutical industry. He consolidated his experience by turning to research in microbiology during a prolonged stay with Roger Stanier and Mike Doudoroff in Berkeley. His interests have ranged widely and included studies on nitrogen ixation, carbon and nitrogen metabolism in algae, and various aspects of environmental science including biodegradation and biotransformation, chemical and microbiological reactions in contaminated sediments, and ecotoxicology. With his group of collaborators, these studies have resulted in publications in Applied and Environmental Microbiology, Journal of Chromatography, Environmental Science & Technology, and Ecotoxicology & Environmental Safety, and in chapters contributed to several volumes of The Handbook of Environmental Chemistry. He is a member of the American Chemical Society, the American Society for Microbiology, the American Society of Crystallography, and the AAAS. Ann-Soie Allard was trained as a chemical microbiologist and is currently a senior microbiologist at IVL Swedish Environmental Research Institute in Stockholm. She has carried out research in a wide range of environmental issues including water quality, processes for the removal of hormone disrupters, biodegradation and biotransformation of organic contaminants in aquatic and terrestrial systems, and ecotoxicology. She has implemented studies on the uptake and metabolism of organic contaminants and metals in higher plants in the context of bioremediation. Her studies have been published in Applied and Environmental Microbiology, International Biodeterioration and Biodegradation, Environmental Chemistry and Ecotoxicology, and Journal of Environmental Science and Health, and in chapters contributed to several volumes of The Handbook of Environmental Chemistry. She is a member of the American Chemical Society.

xxv

Section I Degradation and Transformation Processes

1 Abiotic Reactions INTRODUCTION Virtually any of the plethora of reactions in organic chemistry may be exploited for the abiotic degradation of xenobiotics. These include nucleophilic displacement, oxidation, reduction, thermal reactions, and halogenation. Hydrolytic reactions may convert compounds such as esters, amides or nitriles into the corresponding carboxylic acids, or ureas and carbamides into the amines. These abiotic reactions may therefore be the irst step in the degradation of such compounds. The transformation products may, however, be resistant to further chemical transformation so that their ultimate fate is dependent upon subsequent microbial reactions. For example, for some urea herbicides, the limiting factor is the rate of microbial degradation of the chlorinated anilines that are the initial products of hydrolysis. The role of abiotic reactions should therefore always be taken into consideration, and should be carefully evaluated in laboratory experiments on biodegradation and biotransformation. The results of experiments directed to microbial degradation are probably discarded if they show substantial interference from abiotic reactions. A good illustration of the complementary roles of abiotic and biotic processes is offered by the degradation of tributyltin compounds. Earlier experiments (Seligman et al. 1986) had demonstrated the degradation of tributyltin to dibutyltin primarily by microbial processes. It was subsequently shown, however, that an important abiotic reaction mediated by ine-grained sediments resulted in the formation of monobutyltin and inorganic tin also (Stang et al. 1992). It was therefore concluded that both processes were important in determining the fate of tributyltin in the marine environment. A study of the carbamate biocides, carbaryl, and propham illustrates the care that should be exercised in determining the relative importance of chemical hydrolysis, photolysis, and bacterial degradation (Figure 1.1) (Wolfe et al. 1978). For carbaryl, the half-life for hydrolysis increased from 0.15 d at pH 9 to 1500 d at pH 5, while that for photolysis was 6.6 d: biodegradation was too slow to be signiicant. In contrast, the half-lives of propham for hydrolysis and photolysis were >104 and 121 d—so greatly exceeding the half-life of 2.9 d for biodegradation that abiotic processes would be considered to be of subordinate signiicance. Close attention to structural features of xenobiotics is therefore clearly imperative before making generalizations on the relative signiicance of alternative degradative pathways.

PHOTOCHEMICAL REACTIONS IN AQUEOUS AND TERRESTRIAL ENVIRONMENTS Photochemical reactions are important in atmospheric reactions, in terrestrial areas of high solar irradiation such as the surface of soils, and in aquatic systems containing ultraviolet (UV)absorbing humic and fulvic acids (Zepp et al. 1981a,b). They may be relevant especially for otherwise recalcitrant compounds. It has also been shown (Zepp and Schlotzhauer 1983) that although the presence of algae may enhance photometabolism, this is subservient to direct photolysis at the cell densities likely to be encountered in rivers and lakes. It should be noted that different products may be produced in natural river water and in buffered medium. For example, photolysis of triclopyr (3,5,6-trichloro-2-pyridyloxyacetic acid) in sterile medium at pH 7 resulted in hydrolytic replacement of one chlorine atom, whereas in river water the ring was degraded to form oxamic acid as the principal product (Woodburn et al. 1993). Particular attention has therefore been understandably directed to the photolytic degradation of biocides—including agrochemicals—that are applied to terrestrial systems and enter the aquatic system through leaching. There has been increased interest 3

4

Environmental Degradation and Transformation of Organic Chemicals O−CO−NHCH3

NH−CO−O−CH(CH3)2

(A)

FIGURE 1.1

(B)

Carbaryl (A) and propham (B). OH O

O O

O

O

O

O HO 2 C

O O O

FIGURE 1.2 Photochemical transformation of santonin.

in their phototoxicity toward a range of biota (references in Monson et al. 1999), and this may be attributed to some of the reactions and transformations that are discussed later in this chapter. It should be emphasized that photochemical reactions may produce molecules structurally more complex and less susceptible to degradation than their precursors, even though the deep-seated rearrangements induced in complex compounds such as the terpene santonin during UV irradiation (Figure 1.2) are not likely to be encountered in environmental situations.

THE DIVERSITY OF PHOTOCHEMICAL TRANSFORMATIONS In broad terms, the following types of reactions are mediated by the homolytic ission products of water (formally, hydrogen, and hydroxyl radicals), and by molecular oxygen including its excited states—hydrolysis, elimination, oxidation, reduction, and cyclization.

THE ROLE OF HYDROXYL RADICALS The hydroxyl radical plays two essentially different roles: (a) as a reactant mediating the transformations of xenobiotics and (b) as a toxicant that damages DNA. They are important in a number of environments: (1) in aquatic systems under irradiation, (2) in the troposphere, which is discussed later, and (3) in biological systems in the context of superoxide dismutase and the role of iron. Hydroxyl radicals in aqueous media can be generated by several mechanisms: a. Photolysis of nitrite and nitrate (Brezonik and Fulkerson-Brekken 1998) b. Fenton reaction with H2O2 and Fe2+ in the absence or presence (Fukushima and Tatsumi 2001) of light c. Photolysis of fulvic acids under anaerobic conditions (Vaughan and Blough 1998) d. Reaction of Fe(III) or Cu(II) complexes of humic acids with hydrogen peroxide (Paciolla et al. 1999).

5

Abiotic Reactions

ILLUSTRATIVE EXAMPLES OF PHOTOCHEMICAL TRANSFORMATIONS IN AQUEOUS SOLUTIONS 1. Atrazine is successively transformed to 2,4,6-trihydroxy-1,3,5-triazine (Pelizzetti et al. 1990) by dealkylation of the alkylamine side chains and hydrolytic displacement of the ring chlorine and amino groups (Figure 1.3). A comparison has been made between direct photolysis and nitrate-mediated hydroxyl radical reactions (Torrents et al. 1997): the rates of the latter were much greater under the conditions of this experiment, and the major difference in the products was the absence of ring hydroxylation with loss of chloride. 2. Pentachlorophenol produces a wide variety of transformation products, including chloranilic acid (2,5-dichloro-3,6-dihydroxybenzo-1,4-quinone) by hydrolysis and oxidation, a dichlorocyclopentanedione by ring contraction, and dichloromaleic acid by cleavage of the aromatic ring (Figure 1.4) (Wong and Crosby 1981). 3. The main products of photolysis of 3-triluoromethyl-4-nitrophenol are 2,5 dihydroxybenzoate produced by hydrolytic loss of the nitro group and oxidation of the triluoromethyl group, together with a compound identiied as a condensation product of the original compound and the dihydroxybenzoate (Figure 1.5) (Carey and Cox 1981). Cl N

N

N NHC 3 H 7 i

N

C 2 H 5 NH

Cl

Cl

H2N

N N

N NH 2

N

HO

N

OH

FIGURE 1.3 Photochemical transformation of atrazine. OH Cl

OH

Cl

Cl

O

Cl OH Cl

OH

Cl

O Cl

Cl

Cl

HO

Cl

O Cl

Cl

Cl

Cl

Cl

Cl

CO2H

Cl

CO2H

O OH

FIGURE 1.4

Cl

Cl

Cl

Cl

Photochemical transformation of pentachlorophenol.

CF3

CF3 NO2

O

OH

OH

OH

OH

CO2H

CF3 O

FIGURE 1.5 Photochemical transformation of 3-triluoromethyl-4-nitrophenol.

OH

6

Environmental Degradation and Transformation of Organic Chemicals

4. A potential insecticide that is a derivative of tetrahydro-1,3-thiazine undergoes a number of reactions resulting in some 43 products of which the dimeric azo compound is the principal one in aqueous solutions (Figure 1.6) (Kleier et al. 1985). 5. The herbicide triluralin undergoes a photochemical reaction in which the n-propyl side chain of the amine reacts with the vicinal nitro group to form the benzopyrazine (Figure 1.7) (Soderquist et al. 1975). 6. Heptachlor and cis-chlordane, both of which are chiral, produce caged or half-caged structures (Figure 1.8) on irradiation, and these products have been identiied in biota from the Baltic, the Arctic, and the Antarctic (Buser and Müller 1993). 7. Methylcyclopentadienyl manganese tricarbonyl that has been suggested as a fuel additive is decomposed primarily by photolysis in aqueous medium. This resulted in the formation of methylcyclopentadiene that may plausibly be presumed to polymerize, and a manganese carbonyl that decomposed to Mn3O4 (Garrison et al. 1995). 8. Stilbenes that are used as luorescent whitening agents are photolytically degraded by reactions involving cis–trans isomerization followed by hydration of the double bond, or oxidative ission of the double bond to yield aldehydes (Kramer et al. 1996). 9. The photolysis of chloroalkanes and chloroalkenes has received considerable attention and results in the formation of phosgene as one of the inal products. The photodegradation of 1,1,1-trichloroethane involves hydrogen abstraction and oxidation to trichloroacetaldehyde that is degraded by a complex series of reactions to phosgene (Platz et al. 1995; Nelson et al. 1990). Tetrachloroethene is degraded by reaction with chlorine radicals and oxidation to pentachloropropanol radical that also forms phosgene (Franklin 1994). Attention is drawn to these reactions in the context of the atmospheric dissemination of xenobiotics. 10. Although ethylenediaminetetraacetic acid (EDTA) is biodegradable under speciic laboratory conditions (Belly et al. 1975; Lauff et al. 1990; Nörtemann 1992; Witschel et al. 1997), NO2

N

N

N

S

S

N C

+ S

N

N

S

FIGURE 1.6 Photochemical transformation of tetrahydro-1,3-thiazine. Pr n

Pr n

Pr n

N

Et

H

Et

N

O 2N

NO 2

N N+

O 2N

CF 3

CF 3

N

O 2N

O: −

CF 3

FIGURE 1.7 Photochemical transformation of triluralin. Cl

Cl

Cl Cl

Cl

Cl

Cl Cl

Cl

FIGURE 1.8

Cl

Cl

Cl

Photochemical transformation of chlordane.

Cl

Cl

N

7

Abiotic Reactions O F N Et

O

HO2 C

12.

13.

14.

15.

16.

N

H 2N

N

O

11.

CO 2 H

N

O CO 2H

HO2 C

FIGURE 1.9

F

CO 2 H

N

HO2C HO2C

CO 2 H N H

HO2C

CO2H N

Photochemical degradation of enroloxin.

the primary mode of degradation in the natural aquatic environment involves photolysis of the Fe complex (Lockhart and Blakeley 1975; Kari and Giger 1995). Its persistence is critically determined not only by the degree of insolation but also on the concentration of Fe in the environment, since complexes with other metals including Ca and Zn are relatively resistant to photolysis (Kari et al. 1995). The available evidence suggests that in contrast to nitrotriacetic acid (NTA) that is more readily biodegradable, EDTA is likely to be persistent except in environments in which concentrations of Fe greatly exceed those of other cations. The photolytic degradation of the luoroquinolone enroloxacin involves a number of reactions that produce 6-luoro-7-amino-1-cyclopropylquinolone 2-carboxylic acid that is then degraded to CO2 via reactions involving ission of the benzenoid ring with loss of luoride, dealkylation, and decarboxylation (Burhenne et al. 1997a,b) (Figure 1.9). Photolysis of the oxime group in the pyrazole miticide fenpyroximate resulted in the formation of two principal transformation products: the nitrile via an elimination reaction and the aldehyde by hydrolysis (Swanson et al. 1995). Photochemical transformation of pyrene in aqueous media produced the 1,6- and 1,8quinones as stable end products after initial formation of 1-hydroxypyrene (Sigman et al. 1998). The transformation of isoquinoline has been studied both under photochemical conditions with hydrogen peroxide, and in the dark with hydroxyl radicals (Beitz et al. 1998). The former resulted in ission of the pyridine ring with the formation of phthalic dialdehyde and phthalimide, whereas the major product from the latter reaction involved oxidation of the benzene ring with formation of the isoquinoline-5,8-quinone and a hydroxylated quinone. In the presence of both light and hydrogen peroxide, 2,4-dinitrotoluene is oxidized to the corresponding carboxylic acid; this is then decarboxylated to 1,3-dinitrobenzene, which is degraded further by hydroxylation and ring ission (Figure 1.10) (Ho 1986). Analogous reaction products were formed from 2,4,6-trinitrotoluene and hydroxylated to various nitrophenols and nitrocatechols before ission of the aromatic rings, and included the dimeric 2,2′-carboxy-3,3′,5,5′-tetranitroazoxybenzene (Godejohann et al. 1998). Nitrobenzene, 1-chloro-2,4-dinitrobenzene, 2,4-dinitrophenol, and 4-nitrophenol were degraded with the formation of formate, oxalate, and nitrate (Einschlag et al. 2002). It has been suggested that the photochemical reaction of pentachlorophenol in aqueous solution to produce octachlorodibenzo[1,4] dioxin and some of the heptachloro congener could account for the discrepancy between values for the emission of chlorinated dioxins and their deposition, which is signiicant for the octachloro congener (Baker and Hites 2000).

8

Environmental Degradation and Transformation of Organic Chemicals CO2 H

CH3

NO2

NO2

NO2

NO2

OH

OH

NO2

NO2

OH

NO2

O2 N

CO2 H CO2 H

NO2

FIGURE 1.10

Me

N

FIGURE 1.11

NO 2

Photochemical transformation of 2,4-dinitrotoluene.

N Me

Me

N

N

Me

CO 2

MeNH 2 + CO 2

Photochemical transformation of paraquat.

CO 2 H Cl

Cl

FIGURE 1.12

N

CH 2 CO 2 H

CH 2

N H

N H

Photochemical transformation of diclofenac.

17. The psychopharmaceutical drug luoxetine (Prozac) is degraded both directly and by the faster reaction with OH radicals (Lam et al. 2005). In both reactions, the ring bearing the CF3 group was degraded in high yield to 4-(diluoromethylene)-cyclohexa-2,5-diene-1-one. 18. Whereas photolysis of 2- and 4-chlorophenols in aqueous solution produced catechol and hydroquinone, in ice the more toxic dimeric chlorinated dihydroxybiphenyls were formed (Bláha et al. 2004). 19. The photodegradation of the contact herbicide paraquat yielded many degradation products, but the major pathway produced 1,2,3,4-tetrahydro-1-ketopyrido[1,2-a]-5-pyrazinium that was further degraded to pyridine-2-carboxamide and pyridine-2-carboxylate (Figure 1.11) (Smith and Grove 1969). 20. Photodegradation of the nonsteroidal anti-inlammatory drug diclofenac produced carbazole-1-acetate as the major product (Figure 1.12) (Moore et al. 1990). In a lake under natural conditions, it was rapidly decomposed photochemically though none of the products produced in laboratory experiments could be detected (Buser et al. 1998). 21. Phototransformation of DDT in the presence of surfactants produced DDE by elimination and DDD by reductive dechlorination (Chu 1999).

9

Abiotic Reactions

HYDROXYL RADICALS IN THE DESTRUCTION OF CONTAMINANTS The destruction of contaminants has directed attention to the use of hydroxyl radical–mediated reactions. These reactions should be viewed against those with hydroxyl radicals that occur in the atmosphere.

FENTON’S REAGENT Hydrogen peroxide in the presence of Fe2+ or Fe3+ (Fenton’s reagent) has been used in a range of conigurations including irradiation, electrochemical, and both cathodic and anodic conditions (references in Wang et al. 2004). In all of these, the reaction involves hydroxyl radicals and has been studied particularly intensively for the destruction of agrochemicals including chlorinated phenoxyacetic acid (Sun and Pignatello 1993) and chloroacetanilide herbicides (Friedman et al. 2006). Systematic investigations have been carried out on the effect of pH, the molar ratio of H2O2/ substrate, and the possible complications resulting from the formation of iron complexes. Although this reaction may have limited environmental relevance except under rather special circumstances, it has been applied in combination with biological treatment of polycyclic aromatic hydrocarbons (PAHs) (Pradhan et al. 1997). Attention is drawn to it here since, under conditions where the concentration of oxidant is limiting, intermediates may be formed that are stable and that may possibly exert adverse environmental effects. Some examples that illustrate the formation of intermediates are given, although it should be emphasized that total destruction of the relevant xenobiotics under optimal conditions can be successfully accomplished. The structures of the products that are produced by the action of Fenton’s reagent on chlorobenzene are shown in Figure 1.13a (Sedlak and Andren 1991), on 2,4-dichlorophenoxyacetate in Figure 1.13b (Sun and Pignatello 1993), and on pentachlorophenol in Figure 1.13c (Fukushima and Tatsumi 2001). The UV-enhanced Fenton transformation of atrazine produced 2,4-diamino-6-hydroxy-1,3,5-triazine by a series of interacting reactions (Chan and Chu 2006). Whereas the degradation of azo dyes by Fenton’s reagent produced water- and CH2Cl2-soluble transformation products including nitrobenzene from Disperse Orange 3 O

Cl

(a)

Cl

Cl

OH ;

Cl

;

O

O

CH 2 Cl

Cl O

Cl ;

(b)

Cl

O

O

Cl Cl

Cl O

Cl

Cl

HO

Cl

(c)

FIGURE 1.13

Cl

Cl

O

;

Cl

chlorophenol.

Cl

Cl

Cl

Cl

O

Cl Cl

Cl Cl

Transformation products from (a) chlorobenzene, (b) 2,4-dichlorophenoxyacetate, (c) penta-

10

Environmental Degradation and Transformation of Organic Chemicals

that contains a nitro group, benzene was tentatively identiied among volatile products from Solvent Yellow 14 (Spadaro et al. 1994).

POLYOXOMETALATES (HETEROPOLYACIDS) These are complexes formed between tungstates and molybdates, and silicate or phosphate, and have been used to generate hydroxyl radicals photochemically. The tungstates PW12O403− and SiW12O404− have been used most frequently. a. Degradation of 2,4,6-trichlorophenol by PW12O403− formed a number of products as intermediates, including 2,6-dichlorohydroquinone followed by ission of the ring to maleate, oxalate, acetate, and formate (Androulaki et al. 2000). b. Nonaluoropentanoic acid was decomposed in aqueous solution to luoride and CO2 catalyzed by H3PW12O40 under UV-visible light radiation. The reaction was initiated by decarboxylation followed by a series of reactions involving oxidations (Hori et al. 2004b). c. The polyoxometalate PW12O403− was immobilized on an anion-exchange resin, and used to demonstrate the degradation in the presence of H2O2 of the phthalein dye rhodamine B to phthalate and a number of short-chain aliphatic mono- and dicarboxylates (Lei et al. 2005). They have also been used to bring about photochemical reduction of Hg2+ via Hg22+ to Hg0 (Troupis et al. 2005).

PHOTOLYTIC DEGRADATION ON TiO2 The mechanism involves photochemical production of a free electron in the conduction band (ecb−) and a corresponding hole (hvb+) in the valence band. Both of these produce H2O2 and thence hydroxyl radicals. a. In the presence of slurries of TiO2 that served as a photochemical sensitizer, methyl tert-butyl ether was photochemically decomposed at wavelengths 310 nm is signiicant and that therefore, in contrast to previous assumptions, the latter reaction makes an important contribution (Ravishankara et al. 1998). Nitrate radicals are formed from NO that is produced during combustion processes and these are signiicant only during the night in the absence of photochemically produced OH radicals. They are formed by the reactions NO + O3 → NO2 + O2; NO2 + O3 → NO3 + O2 The concentrations of all these depend on local conditions, the time of day, and both altitude and latitude. Values of ca. 106 molecules/cm3 for OH, 108 –1010 molecules/cm3 for NO3, and ca. 1011 molecules/cm3 for ozone have been reported. Not all of these reactants are equally important, and the rates of reaction with a substrate vary considerably. Reactions with hydroxyl radicals are generally the most important, and some illustrative values are given for the rates of reaction (cm3/s/molecule) with hydroxyl radicals, nitrate radicals, and ozone (Atkinson 1990; summary of PAHs by Arey 1998) Hydroxyl Radicals 2.54 × 10–12 15.8 × 10–12 23.16 × 10–11

n-Butane Acetaldehyde Naphthalene

Nitrate Radicals 6.5 × 10–17 2.7 × 10–15 3.6 × 10–28 [NO2]

Ozone 9.8 × 10–24 < 10–20 < 2 × 10–19

SURVEY OF REACTIONS The major reactions carried out by hydroxyl and nitrate radicals may conveniently be represented for a primary alkane RH or a secondary alkane R2CH. In both, hydrogen abstraction is the initiating reaction. 1. Hydrogen abstraction RH + HO → R + H2O RH + NO3 → R + HNO3 2. Formation of alkylperoxy radicals R + O2 → R–O–O 3. Reactions of alkylperoxy radicals with NOx R–O–O + NO → R–O + NO2 R–O–O + NO → R–O–NO2 4. Reactions of alkyloxy radicals R2CH–O + O2 → R2CO + HO2 R2CH–O + NO → R2CH–O–NO2 → R2CO + HNO

16

Environmental Degradation and Transformation of Organic Chemicals

The concentration of NO determines the relative importance of reaction 3, and the formation of NO2 is particularly signiicant since this is readily photolyzed to produce O(3P) that reacts with oxygen to produce ozone. This alkane–NOx reaction may produce O3 at the troposphere–stratosphere interface: NO2 → NO + O(3P); O(3P) + O2 → O3 This is the main reaction for the formation of ozone although, under equilibrium conditions, the concentrations of NO2, NO, and O3 are interdependent and no net synthesis of O3 occurs. When, however, the equilibrium is disturbed and NO is removed by reactions with alkylperoxy radicals (reactions 1+2+3), synthesis of O3 may take place. RH + OH → R + H2O; R + O2 → RO2; RO2 + NO → RO + NO2 The extent to which this occurs depends on a number of issues (Finlayson-Pitts and Pitts 1997), including the reactivity of the hydrocarbon that is itself a function of many factors. It has been proposed that the possibility of ozone formation is best described by a reactivity index of incremental hydrocarbon reactivity (Carter and Atkinson 1987, 1989) that combines the rate of formation of O3 with that of the reduction in the concentration of NO. The method has been applied, for example, to oxygenate additives to automobile fuel (Japar et al. 1991), while both anthropogenic compounds and naturally occurring hydrocarbons may be reactive. Clearly, whether or not ozone is formed depends also on the rate at which, for example, unsaturated hydrocarbons react with it. Rates of reactions of ozone with alkanes are, as noted above, much slower than for reaction with OH radicals, and reactions with ozone are of the greatest signiicance with unsaturated aliphatic compounds. The pathways plausibly follow those involved in chemical ozonization (Hudlický 1990). The kinetics of the various reactions have been explored in detail using large-volume chambers that can be used to simulate reactions in the troposphere. They have frequently used hydroxyl radicals formed by photolysis of methyl (or ethyl) nitrite, with the addition of NO to inhibit photolysis of NO2. This would result in the formation of O(3P) atoms, and subsequent reaction with O2 would produce ozone, and hence NO3 radicals from NO2. Nitrate radicals are produced by the thermal decomposition of N2O5, and in experiments with O3, a scavenger for hydroxyl radicals is added. Details of the different experimental procedures for the measurement of absolute and relative rates have been summarized, and attention drawn to the often considerable spread of values for experiments carried out at room temperature (~298 K) (Atkinson 1986). It should be emphasized that in the real troposphere, both the rates—and possibly the products—of transformation will be determined by seasonal differences both in temperature and the intensity of solar radiation. These are determined both by latitude and altitude. The kinetics of the reactions of several xenobiotics with hydroxyl or nitrate radicals have been examined under simulated atmospheric conditions and include those given in Table 1.1. For polychlorinated biphenyls (PCBs), rate constants were highly dependent on the number of chlorine atoms, and calculated atmospheric lifetimes varied from 2 d for 3-chlorobiphenyl to 34 d for 236-25 pentachlorobiphenyl (Anderson and Hites 1996). It was estimated that loss by hydroxylation in the atmosphere was a primary process for the removal of PCBs from the environment. It was later shown that the products were chlorinated benzoic acids produced by initial reaction with a hydroxyl radical at the 1-position followed by transannular dioxygenation at the 2- and 5-positions followed by ring ission (Brubaker and Hites 1998). Reactions of hydroxyl radicals with polychlorinated dibenzo[1,4]dioxins and dibenzofurans also play an important role for their removal from the atmosphere (Brubaker and Hites 1997). The gas phase and the particulate phase are in equilibrium, and the results show that gas-phase reactions with hydroxyl radicals are important for the

17

Abiotic Reactions

TABLE 1.1 Degradation of Contaminants under Simulated Atmospheric Conditions Xenobiotic Aliphatic and aromatic hydrocarbons Substituted monocyclic aromatic compounds Terpenes Amines Heteroarenes Chlorinated aromatic hydrocarbons Volatile methyl–silicon compounds Methylcyclopentadienyl manganese (CO)3

Reference Tuazon et al. (1986) Tuazon et al. (1986) Atkinson et al. (1985a) Atkinson et al. (1987) Atkinson et al. (1985b) Kwok et al. (1995) Tuazon et al. (2000) Wallington et al. (1999)

compounds with fewer numbers of chlorine substituents, whereas for those with higher numbers of substituents particle-phase removal is signiicant. Considerable attention has been directed in determining the products from reactions of aliphatic hydrocarbons, aromatic compounds, and unsaturated compounds including biogenic terpenes that exhibit appreciable volatility. These studies have been conducted both in simulation chambers and using natural sunlight in the presence of NO.

SURVEY OF REACTANTS Aliphatic Hydrocarbons A range of transformation products has been identiied from simulated reactions of alkanes. These include alkyl nitrates by reactions that have already been given, but also include a range of hydroxycarbonyls that are summarized in Table 1.2 (Reisen et al. 2005). Aromatic Hydrocarbons Fission of the rings of aromatic hydrocarbons may take place. For example, o-xylene forms diacetyl, methylglyoxal, and glyoxal (Tuazon et al. 1986), which are also produced by ozonolysis (Levine and Cole 1932), while naphthalene forms 2-formylcinnamaldehyde (Arey 1998). The photooxidation of alkyl benzenes that are atmospheric contaminants with high volatility has been studied in detail and the reaction pathways have been delineated (Yu et al. 1997). Products from alkyl benzenes included both those with the ring intact, such as aromatic aldehydes and quinones, together with a wide range of aliphatic compounds containing alcohol, ketone, and epoxy functional groups resulting from ring ission. The signiicance of epoxide intermediates (Yu and Jeffries 1997) is noted in the next section, and attention is drawn later to the important reactions of arenes that result in the production of nitroarenes. Biogenic Terpenes Monoterpenes are appreciably volatile and are produced in substantial quantities by a range of higher plants and trees. Only summary of examples are given here. 1. Photochemical reactions of isoprene (references in Grosjean et al. 1993a). 2. Products from reaction of α-pinene with ozone that produced a range of cyclobutane carboxylic acids (Kamens et al. 1999). 3. Rapid reactions of linalool with OH radicals, NO3 radicals, and ozone in which the major products were acetone and 5-ethenyldihydro-5-methyl-2(3H)-furanone (Shu et al. 1997).

18

Environmental Degradation and Transformation of Organic Chemicals

TABLE 1.2 Products from Simulated Reactions of Alkanes Alkane n-Pentane n-Hexane

n-Heptane

n-Octane

Product

Alkane

Product

5-Hydroxypentan-2-one 5-Hydroxypentanal 5-Hydroxyhexan-2-one 6-Hydroxyhexan-3-one 4-Hydroxyhexanal 5-Hydroxyheptan-2-one 6-Hydroxyheptan-3-one 1-Hydroxyheptan-4-one 4-Hydroxyheptanal 5-Hydroxyoctan-2-one 6-Hydroxyoctan-3-one 7-Hydroxyoctan-4-one 4-Hydroxyoctanal

n-Heptane

5-Hydroxyheptan-2-one 6-Hydroxyheptan-3-one 1-Hydroxyheptan-4-one 4-Hydroxyheptanal 5-Hydroxyoctan-2-one 6-Hydroxyoctan-3-one 7-Hydroxyoctan-4-one 4-Hydroxyoctanal

n-Octane

4. Plant metabolite cis-hex-3-ene-1-ol that is the precursor of peroxypropionyl nitrate (Grosjean et al. 1993b) analogous to peroxyacetyl nitrate. 5. Degradation of many terpenes has been examined including β-pinene, d-limonene, and trans-caryophyllene (Grosjean et al. 1993c). 6. Products formed by reaction of NO3 radicals with α-pinene have been identiied and include pinane epoxide, 2-hydroxypinane-3-nitrate, and 3-ketopinan-2-nitrate formed by reactions at the double bond, and pinonaldehyde that is produced by ring ission between C-2 and C-3 (Wängberg et al. 1997). These reactions should be viewed in the general context of “odd nitrogen” to which alkyl nitrates belong (Schneider et al. 1998). 7. Gas-phase products from the reactions of ozone with the monoterpenes (–)-β-pinene and (+)-sabinene included the ketones formed by oxidative ission of the exocyclic C=C bonds as well as ozonides from the addition of ozone to this bond (Griesbaum et al. 1998).

REENTRY OF TROPOSPHERIC TRANSFORMATION PRODUCTS An important aspect of atmospheric reactions is the possibility that tropospheric transformation products subsequently enter aquatic and terrestrial ecosystems through precipitation or by particle deposition.

HALOGENATED ALKANES AND ALKENES The stability of perchloroluoroalkanes is due to the absence of hydrogen atoms that may be abstracted by reaction with hydroxyl radicals. Attention has therefore been directed to chloroluoroalkanes containing at least one hydrogen atom (Hayman and Derwent 1997). Considerable effort has also been directed to the reactions of chloroalkanes and chloroalkenes, and this deserves a rather more detailed examination in the light of interest in the products that are formed. a. There has been concern over the fate of halogenated aliphatic compounds in the atmosphere, and a single illustration of the diverse consequences is noted here. The initial

19

Abiotic Reactions

reaction of 1,1,1-trichloroethane with hydroxyl radicals produces the Cl3C–CH2 radical by abstraction of H and then undergoes a complex series of reactions including the following: Cl3C–CH2 + O2 → Cl3C–CH2O2 2Cl3C–CH2O2 → 2Cl3C–CH2O Cl3C–CH2O + O2 → Cl3C–CHO In addition, the alkoxy radical Cl3C–CH2O produces highly reactive COCl2 (phosgene) (Platz et al. 1995; Nelson et al. 1990) that has been identiied in atmospheric samples and was attributed to the transformation of gem-dichloro aliphatic compounds (Grosjean 1991). b. The atmospheric degradation of tetrachloroethene is initiated by reaction with Cl radicals and produces trichloroacetyl chloride as the primary intermediate which is formed followed by the following reactions (Franklin 1994): Cl2C=CCl2 + Cl → Cl3C–CCl2 Cl3C–CCl2 + O2 → Cl3C–CCl2O2 Cl3C–CCl2O2 + NO → Cl3C–CCl2O + NO2 Cl3C–CCl2O → Cl3C–COCl + Cl → COCl2 + CCl3 CCl3 + O2 + NO → COCl2 + NO2 + Cl An overview of the reactions involving trihalomethanes (haloforms) CHXYZ, where X, Y, and Z are halogen atoms, has been given in the context of ozone depletion (Hayman and Derwent 1997). Interest in the formation of trichloroacetaldehyde formed from trichloroethane and tetrachloroethene is heightened by the phytotoxicity of trichloroacetic acid (Frank et al. 1994), and by its occurrence in rainwater that seems to be a major source of this contaminant (Müller et al. 1996). The situation in Japan seems, however, to underscore the possible signiicance of other sources including chlorinated wastewater (Hashimoto et al. 1998). Whereas there is no doubt about the occurrence of trichloroacetic acid in rainwater (Stidson et al. 2004), its major source is unresolved since questions remain on the rate of hydrolysis of trichloroacetaldehyde (Jordan et al. 1999). Low concentrations of triluoroacetate have been found in lakes in California and Nevada (Wujcik et al. 1998). It is formed by atmospheric reactions from 1,1,1,2-tetraluoroethane and from the chloroluorocarbon replacement compound CF3–CH2F (HFC-134a) in an estimated yield of 7–20% (Wallington et al. 1996). CF3OH that is formed from CF3 in the stratosphere is apparently a sink for its oxidation products (Wallington and Schneider 1994). CF3–CH2F + OH → CF3–CHF CF3–CHF + O2 → CF3–CHFO2 CF3–CHFO2 + NO → CF3–CHFO + NO2 CF3–CHFO + O2 → CF3–COF CF3–CHFO → CF3 + H–COF

20

Environmental Degradation and Transformation of Organic Chemicals

It has been suggested that an alternative source of triluoroacetic acid in the environment may be provided by the aqueous photolysis of TFM and related triluoromethylphenols (Ellis and Mabury 2000). Although triluoroacetate is accumulated by a range of biota through incorporation into biomolecules (Standley and Bott 1998), unlike trichloroacetate, it is only weakly phytotoxic, and there is no evidence for its inhibitory effect on methanogenesis (Emptage et al. 1997). Attention has been directed to the transformation of perluorotelomer alcohols CF3(CF2)7–CH2CH2OH that could be the source of the ubiquitous perluorinated carboxylic acids (PFCAs), and that have been produced during simulated atmospheric reactions with chlorine radicals as surrogate for hydroxyl radicals (Ellis et al. 2004).

ARENES AND NITROARENES The transformation of arenes in the troposphere has been discussed in detail (Arey 1998). Their destruction can be mediated by reaction with hydroxyl radicals, and from naphthalene a wide range of compounds is produced, including 1- and 2-naphthols, 2-formylcinnamaldehyde, phthalic anhydride, and with less certainty 1,4-naphthoquinone and 2,3-epoxynaphthoquinone. Both 1- and 2-nitronaphthalene were formed through the intervention of NO2 (Bunce et al. 1997). Attention has also been directed to the composition of secondary organic aerosols from the photooxidation of monocyclic aromatic hydrocarbons in the presence of NOx (Forstner et al. 1997); the main products from a range of alkylated aromatics were 2,5-furandione and the 3-methyl and 3-ethyl congeners. Considerable attention has been directed to the formation of nitroarenes that may be formed by several mechanisms: (a) initial reaction with hydroxyl radicals followed by reactions with nitrate radicals or NO2 and (b) direct reaction with nitrate radicals. The irst is important for arenes in the troposphere, whereas the second is a thermal reaction that occurs during combustion of arenes. The kinetics of formation of nitroarenes by gas-phase reaction with N2O5 has been examined for naphthalene (Pitts et al. 1985a) and methylnaphthalenes (Zielinska et al. 1989); biphenyl (Atkinson et al. 1987b,c); acephenanthrylene (Zielinska et al. 1988); and for adsorbed pyrene (Pitts et al. 1985b). Both 1- and 2-nitronaphthalene were formed through OH radical–initiated reactions with naphthalene by the intervention of NO2 (Bunce et al. 1997). The major product from the irst group of reactions is 2-nitronaphthalene, and a number of other nitroarenes have been identiied including nitropyrene and nitroluoranthenes (Arey 1998). The tentative identiication of hydroxylated nitroarenes in air particulate samples (Nishioka et al. 1988) is consistent with the operation of this dual mechanism. Reaction of methyl arenes with nitrate radicals in the gas phase gives rise to a number of products. From toluene, the major product was benzaldehyde with lesser amounts of 2-nitrotoluene > benzyl alcohol nitrate > 4-nitrotoluene > 3-nitrotoluene (Chlodini et al. 1993). An important example is the formation of the mutagenic 2-nitro- and 6-nitro-6H-dibenzo[b,d]pyran-6-ones (Figure 1.18) from the oxidation of phenanthrene in the presence of NOx and methyl nitrite as a source of hydroxyl radicals (Helmig et al. 1992a). These compounds have been identiied in samples of ambient air (Helmig et al. 1992b), and analogous compounds from pyrene have been tentatively identiied (Sasaki et al. 1995). These compounds add further examples to the list of mononitroarenes that already include 2-nitropyrene and 2-nitroluoranthene, and it appears plausible to suggest that NO 2

O O

FIGURE 1.18

Product from the photochemical reaction of phenanthrene and NOx.

Abiotic Reactions

21

comparable reactions are involved in the formation of the 1,6- and 1,8-dinitroarenes that have been identiied in diesel exhaust. 3-Nitrobenzanthrone that is formally analogous to the dibenzopyrones noted earlier has also been identiied in diesel exhaust and is also highly mutagenic to Salmonella typhimurium strain TA 98 (Enya et al. 1997). Many nitroarenes including 2-nitronaphthalene are direct-acting, frameshift mutagens in the Ames test (Rosenkranz and Mermelstein 1983). Although the mechanism has not been inally resolved, it appears to involve metabolic participation of the test organisms, for example, by reduction. In addition, nitroarenes may be reduced microbiologically to the corresponding amino compounds, and in terrestrial and aquatic systems these may have undesirable properties: (a) some including 2-aminonaphthalene are carcinogenic to mammals and (b) they react with components of humic and fulvic acids, which makes them more recalcitrant to degradation and therefore more persistent in ecosystems. Although nitroluoranthenes and nitropyrenes are established atmospheric products from the nitration of the respective PAHs, their direct mutagenic activity is unable to account for the total mutagenic activity of airborne samples. It has been shown that the concentrations of 1- and 2-nitrotriphenylenes were higher than those of 1-nitropyrene, and that 1-nitrotriphenylene was a highly active direct-acting mutagen in S. typhimurium strains TA98 and YG 1024 (Ishii et al. 2000). Nitrated phenols have been found in rainwater, and are secondary products from atmospheric oxidation of benzene and alkylated toluenes followed by nitration (Kohler and Heeb 2003). Plausible mechanisms for the formation of 2,4-dinitrophenol from 2- and 4-nitropohenol in the atmospheric liquid phase have been proposed (Vione et al. 2005), and include nitration by NO2 or NO3 radicals. A wide range of azaarenes is produced during combustion (Herod 1998), and these may enter the troposphere, with formation of the corresponding nitro derivatives.

ALKYLATED ARENES The products from the oxidation of alkylbenzenes under simulated atmospheric conditions have been examined. Both ring epoxides that were highly functionalized, and aliphatic epoxides from ring ission were tentatively identiied (Yu and Jeffries 1997). Formation of the epoxides, many of which are mutagenic, may cause concern over the transformation products of monocyclic aromatic hydrocarbons in the atmosphere. Toluene is an important atmospheric contaminant and its photochemistry has been explored using EUROPHORE, which is described in Chapter 5 (Klotz et al. 1998). This used natural illumination in a large-volume chamber equipped with differential optical spectroscopy (path length 326.8 m) and Fourier transform spectroscopy (path length 128 m) to minimize artifacts from sampling or treatment for analysis. Concentrations of NOx resembled those found in the atmosphere, and concentrations of ozone were low at the beginning of the experiment. The major reaction involved OH radicals that initiated two reactions: (a) removal of a hydrogen atom from the methyl group to form benzaldehyde and (b) formation of a toluene-hydroxyl adduct (methyl-hydroxy-cyclohexadienyl radical) that reacted with oxygen to produce o-, m-, and p-cresol that reacted further with nitrate radicals.

SULFIDES AND DISULFIDES Sulides and disulides can be produced by bacterial reactions in the marine environment. 2-Dimethylthiopropionic acid is produced by algae and by the marsh grass Spartina alternifolia, and may then be metabolized in sediment slurries under anoxic conditions to dimethyl sulide (Kiene and Taylor 1988), and by aerobic bacteria to methyl sulide (Taylor and Gilchrist 1991). Further details are given in Chapter 11, Part 2. Methyl sulide can also be produced by biological methylation of sulide itself (HS−). Carbon radicals are not the initial atmospheric products from organic sulides and disulides, and the reactions also provide an example in which the rates of reaction with nitrate

22

Environmental Degradation and Transformation of Organic Chemicals

radicals exceed those with hydroxyl radicals. Dimethyl sulides—and possibly methyl sulide as well—are oxidized in the troposphere to sulfur dioxide and methanesulfonic acids: CH3–SH → CH3–SO3H CH3–S–S–CH3 → CH3–SO3H + CH3–SO CH3–SO → CH3 + SO2 It has been suggested that these compounds may play a critical role in promoting cloud formation (Charleson et al. 1987), so that the long-term effect of the biosynthesis of methyl sulides on climate alteration may be important. And yet, at irst glance this seems far removed from the production of an osmolyte by marine algae and its metabolism in aquatic systems. The occurrence of methyl sulfates in atmospheric samples (Eatough et al. 1986) should be noted, although the mechanism of its formation appears not to have been established. These reactions provide a good example of the long chain of events that may bring about environmental effects through the subtle interaction of biotic and abiotic reactions in both the aquatic and atmospheric environments. Appreciation of interactive processes that have been outlined has been able to illuminate discussion of mechanisms for reactions as diverse as the acidiication of water masses, climate alteration, ozone formation and destruction, and the possible environmental roles of trichloroacetic acid and nitroarenes.

CHEMICALLY MEDIATED TRANSFORMATIONS Only a limited number of the plethora of known chemical reactions has been observed in transforming xenobiotics in the environment. An attempt is made merely to present a classiication of the reactions that take place with illustrations of their occurrence.

HYDROLYSIS Organic compounds containing carbonyl groups lanked by alkoxy groups (esters) or by amino- or substituted amino groups (amides, carbamates, and ureas) may be hydrolyzed by purely abiotic reactions under appropriate conditions of pH. The generally high pH of seawater (ca. 8.2) suggests that chemical hydrolysis may be important in this environment. In contrast, although very few natural aquatic ecosystems have pH values suficiently low for acidic hydrolysis to be of major importance, this could be important in terrestrial systems when the pH is lowered by fermentation of organic substrates. It is therefore important to distinguish between alkaline or neutral, and acidic hydrolytic mechanisms. It should also be appreciated that both hydrolytic and photolytic mechanisms may operate simultaneously and that the products of these reactions may not necessarily be identical. It has already been noted that substantial numbers of important agrochemicals contain carbonyl groups, so that abiotic hydrolysis may be the primary reaction in their transformation: the example of carbaryl has already been cited (Wolfe et al. 1978). The same general principles may be extended to phosphate and thiophosphate esters, although in these cases it is important to bear in mind the stability to hydrolysis of primary and secondary phosphate esters under the neutral or alkaline conditions that prevail in most natural ecosystems. In contrast, sulfate esters and sulfamides are generally quite resistant to chemical hydrolysis except under rather drastic conditions, and microbial sulfatases and sulfamidases generally mediate their hydrolysis. Some examples illustrate the range of hydrolytic reactions that involve diverse agrochemicals that may enter aquatic systems by leaching from the soil.

23

Abiotic Reactions

1. The cyclic sulite of α- and β-endosulfan (Singh et al. 1991). 2. The carbamate phenmedipham that results in the intermediate formation of m-tolyl isocyanate (Figure 1.19) (Bergon et al. 1985). 3. 2-(Thiocyanomethylthio)benzthiazole initially forms 2-thiobenzthiazole, which is transient and then rapidly degrades photochemically to benzothiazole and 2-hydroxybenzothiazole (Brownlee et al. 1992). 4. Aldicarb undergoes simple hydrolysis at pH values above 7, whereas at pH values bromides > chlorides, while tertiary halides are the most reactive and primary halides the least (Castro and Kray 1963, 1966). 2. The stereospeciicity of dehalogenation of vicinal dibromides to oleins was examined for reducing agents including Cr(II), iodide, and Fe0 (Totten et al. 2001). For dibromostilbene, the (E)-stilbene represented >70% of the total olein that was produced, and for threodibromopentane reduction by Cr(II) produced ca. 70% of (E)-pent-2-ene, whereas values for iodide and Fe0 were α > δ > β. Tetrachlorocyclohexene was formed as a transient intermediate with chlorobenzene as the ultimate product (Rodríguez-Garrido et al. 2004). An additional aspect of these dehalogenations that elucidates the role of vitamin B12 is provided by experiments with Shewanella alga strain BrY (Workman et al. 1997). This organism carries out reduction of Fe(III) and Co(III) during growth with lactate and H2, and was used to reduce vitamin B12a anaerobically in the presence of an electron donor. The biologically reduced vitamin B12 was then able to transform tetrachloromethane to CO. The reactions of alkyl halides with Fe(II) deuteroporphyrin IX have been examined (Wade and Castro 1973). Three classes of reaction were observed (i) hydrogenolysis, (ii) elimination to alkenes, and (iii) coupling of alkyl free radicals. Further discussion has been given in Castro (1998). Experiments have been carried out to mimic the reactions of model systems for coenzyme F430 that is involved in the terminal step in the biosynthesis of methane, and that is able to dechlorinate CCl4 successively to CHCl3 and CH2Cl2 (Krone et al. 1989). Nickel(I) isobacteriochlorin anion was generated electrolytically and used to examine the reactions with alkyl halides in dimethylformamide (Helvenston and Castro 1992). The three classes of reaction were the same as those observed with Fe(II) deuteroporphyrin IX that have already been noted. Experiments that were carried out to compare nanoscale catalysts composed of Fe, Ni, and Co complexes of several porphyrins, or cyanocobalamin have already been noted (Dror et al. 2005).

THIOL REDUCTANTS It has been shown that thiols can carry out dehalogenation both in the presence and absence of quinone mediators: a. The formation of tetrachloroethene from hexachloroethane in the presence of 5-hydroxynaphtho-1,4-quinone (juglone) (Perlinger et al. 1996).

28

Environmental Degradation and Transformation of Organic Chemicals

b. The reduction of hexachloroethane by both HS− and polysulides (S42−) to tetrachloroethene and pentachloroethane (Miller et al. 1998). c. The transformation of tetrachloromethane by HS− and cysteine in the presence of quinones as electron-transfer mediators has been examined (Doong and Chiang 2005). 5-Hydroxy-naphtho-1,4-quinone (juglone) was the most effective and much greater than anthraquinone 2,6-disulfate. The enhancement was the result of the formation of mercaptoquinones or, from anthraquinone 2,6-disulfate semiquinone radicals.

REDUCTIVE DESULFURIZATION In the context of diagenesis in recent anoxic sediments, reduced carotenoids, steroids, and hopanoids have been identiied, and it has been suggested that reduction by sulide, produced for example, by the reduction of sulfate could play an important part (Hebting et al. 2006). The partial reduction of carotenoids by sulide has been observed as a result of the addition of sulide to selected allylic double bonds, followed by reductive desulfurization. This is supported by the inding that the thiol in allylic thiols could be reductively removed by sulide to produce unsaturated products from freeradical reactions (Hebting et al. 2003).

REDUCTIONS OTHER THAN DEHALOGENATION Aromatic nitro compounds include both important explosives and a number of agrochemicals. Concern with their fate has motivated extensive examination of their reduction to amines under a range of conditions. 1. Reduction of monocyclic aromatic nitro compounds has been demonstrated: (a) with reduced sulfur compounds mediated by a naphthoquinone or an iron porphyrin (Schwarzenbach et al. 1990), and (b) by Fe(II) and magnetite produced by the action of the anaerobic bacterium Geobacter metallireducens (Heijman et al. 1993). Quinone-mediated reduction of monocyclic aromatic nitro compounds by the supernatant monocyclic aromatic nitro compounds has been noted (Glaus et al. 1992), and these reactions may be signiicant in determining the fate of aromatic nitro compounds in reducing environments (Dunnivant et al. 1992). 2. The reduction of 2,4,6-trinitrotoluene with Fe0 has been extensively studied (references in Bandstra et al. 2005), and it has inally produced 2,4,6-triaminotoluene that could undergo polymerization. 3. The degradation of triluralin [2,6-dinitro-N,N-dipropyl-4-(triluoromethyl)benzenamine] by Fe(II)/goethite has been examined under anaerobic conditions as a model for reactions in looded soils (Klupinski and Chin 2003). A range of transformation products was found including those produced by reduction of the nitro groups, dealkylation, and formation of benziminazoles presumably via intermediate nitroso compounds (Figure 1.26). A number of other abiotic reductions have been described: 1. The aerobic biodegradation of monocyclic azaarenes frequently involves reduction (Chapter 10, Part 1), but purely chemical reduction may take place under highly anaerobic conditions. This has been encountered with the substituted 1,2,4-triazolo[1,5a]pyrimidine (Flumetsulam) (Wolt et al. 1992) (Figure 1.27). 2. Cell-free supernatants may mediate reductions. The reduction of aromatic nitro compounds by SH− was mediated by the iltrate from a strain of Streptomyces sp. that is known to synthesize 2-amino-3-carboxy-5-hydroxybenzo-1,4-quinone (cinnaquinone)

29

Abiotic Reactions NO2 N

F3 C

NO2

NH2

N NO2 F3 C

NO2

N N

F3 C

FIGURE 1.26

Degradation of 2,6-dinitro-N,N-dipropyl(triluoromethyl)benzenamine. F

F N

N

N

NH−SO 2 F

N

NH−SO 2 N

N

CH 3

F

N

N H

CH 3

FIGURE 1.27 Reductive degradation of 1,2,4-triazolo[1,5a]pyrimidine.

and the 6,6′-diquinone (dicinnaquinone) as secondary metabolites (Glaus et al. 1992). The quinones presumably function as electron-transfer mediators. 3. Dimerization of a number of arylalkenes catalyzed by vitamin B12 and Ti(III) as reductant has been examined (Shey et al. 2002). Mechanisms were examined including the requirement of a reductant, and a reaction was proposed that involved the formation of radicals at the benzylic carbon atoms.

NUCLEOPHILIC REACTIONS Although the foregoing reactions involve dehalogenation by reduction or elimination, nucleophilic displacement of chloride may also be important. This has been examined with dihalomethanes using HS− at concentrations that might be encountered in environments where active anaerobic sulfate reduction is taking place. The rates of reaction with HS− exceeded those for hydrolysis and at pH values above 7 in systems that are in equilibrium with elementary sulfur, the rates with polysulide exceeded those with HS−. The principal product from dihalomethanes was the polythiomethylene HS−(CH2–S)nH (Roberts et al. 1992). Attention is briely drawn to hydrolytic procedures that have been considered for the destruction of xenobiotics. Although these are carried out under conditions that are not relevant to the aquatic environment, they may be useful as a background to alternative remediation programs. Three examples involving CaO and related compounds may be used as examples of important and unprecedented reactions: 1. The destruction of DDT by ball milling with CaO resulted in substantial loss of chloride and produced a graphitic product containing some residual chlorine. In addition, an exceptional rearrangement occurred with the formation of bis(4-chlorophenyl)ethyne that was identiied by 1H NMR (Hall et al. 1996) (Figure 1.28). 2. Treatment of 1,2,3,4-tetrachlorodibenzo[1,4]dioxin on Ca-based sorbents at temperatures of 160–300°C resulted in its conversion into products with molecular masses of

30

Environmental Degradation and Transformation of Organic Chemicals

Cl

Cl

C

Cl

C

C

Cl

CCl2

FIGURE 1.28 Alkaline destruction of DDT. CHO CO 2 H

CHO NH 2

N

CO N CONH 2

N CONH 2

N

N CHO

O CHO

FIGURE 1.29 Ozonization of carbamazepine.

302 and 394 that were tentatively identiied as chlorinated benzofurans and 1-phenylnaphthalene or anthracenes (Gullett et al. 1997). 3. CaO was activated by the addition of Ni (acetylacetonate)2 followed by calcining at 973 K. This resulted in the production of nickel on the carbonate matrix, and was effective in decomposing dichlorodiluoromethane (CFC-12) to CO2 at 723 K—with low amounts of CO—while the halogen was combined as CaFCl (Tamai et al. 2006).

OXIDATIONS These have already been noted in the context of hydroxyl radical-initiated oxidations, and reference should be made to an extensive review by Worobey (1989) that covers a wider range of abiotic oxidations. Some have attracted interest in the context of the destruction of xenobiotics, and reference has already been made to photochemically induced oxidations. Anodic Oxidation An interesting study examined the anodic oxidation of EDTA at alkaline pH on a smooth platinum electrode (Pakalapati et al. 1996). Degradation was initiated by removal of the acetate side chains as formaldehyde, followed by deamination of the ethylenediamine that formed glyoxal and oxalate. Oxalate and formaldehyde are oxidized to CO2, and adsoption was an integral part of the oxidation. Ozone Although reactions carried out by ozone have attracted enormous attention in the atmospheric environment, ozone has also been used extensively in the treatment of drinking water without the production of undesirable trihalomethanes from the use of molecular chlorine (Richardson et al. 1999). It has been examined for the removal of a number of contaminants, and ozone is considered to be a selective oxidant, even though quite complex reactions may occur. 1. Laboratory experiments on the ozonization of the dibenzoazepine drug carbamazepine (McDowell et al. 2005) showed the occurrence of a number of transformation products that were initiated by reaction at the oleinic double bond between the rings (Figure 1.29). 2. The degradation of aminodinitrotoluenes has been examined, and destruction of the rings took place with the release of NO3− and NO2−. Use of 15N amino compounds revealed that pyruvamide was formed from the 2-amino compound and oxamic acid from the 4-amino compound (Spanggord et al. 2000).

31

Abiotic Reactions

3. Ozone attacks the rings of PAHs rather indiscriminately with ission of the rings to produce aldehyde groups. There has been concern, however, since the products may be more harmful than their precursors. In the studies that are used as illustration, in vitro gap junctional intracellular communication (GJIC) was used to assess adverse alteration on the expression of genes at the transcription, translational, or posttranslational level: a. Pyrene was degraded to two groups of compounds: phenanthrene rings with one or more carbonyl groups by oxidation and ission of ∆9–10, and biphenyls with four carbonyl groups ortho to the ring junction by ission of both ∆9–10 and ∆4–5 (Herner et al. 2001). b. The product from chrysene was produced by oxidation and ission of ∆11–12 to the dialdehyde (Luster-Teasley et al. 2002). 4. Effective removal of the estrogens 17β-estradiol, estrone, and 17α-ethynylestradiol has been achieved using ozone under conditions that simulated those used for water treatment (Deborde et al. 2005). Analysis of the products showed the occurrence of two reactions: a. Fission of rings A and B in estrone and 17β-estradiol to yield products with a carboxyl group at C9 and a carboxyethyl group at C8 (Figure 1.30a). b. Oxidation of ring A to a 1,2-dione that underwent a benzylic acid rearrangement with ring contraction to a cyclopentane carboxylate (Figure 1.30b). Analogous reactions were postulated to occur for 17α-ethynylestradiol and, on the basis of experiments with model compounds, oxidation of the ethynyl group to –COCHO (Huber et al. 2004). 5. Combined treatment of atrazine with ozone and H2O2 resulted in retention of the triazine ring, and oxidative dealkylation with or without replacement of the 2-chloro group by hydroxyl (Nélieu et al. 2000). Reaction with ozone and hydroxyl radicals formed the analogous products with the additional formation of the acetamido group from one of the N-alkylated groups (Acero et al. 2000). 6. A range of products was obtained from aniline including those from oxidative coupling (azozybenzene, azobenzene, and benzidine), and phenazine by dimerization (Chan and Larson 1991). Oxidation of m-phenylenediamine was initiated by the oxidation of two molecules to produce an N-phenyl-2-aminoquinone-imine that reacted with m-phenylenediamine to produce 2-amino-5-phenylaminoquinone-imine after further oxidation (Kami et al. 2000).

OH

HO 2 C OH (a)

CO 2 H OH

OH

(b) HO O

HO 2C HO

O

FIGURE 1.30

(a) and (b) Ozonization of estrone/estradiol.

32

Environmental Degradation and Transformation of Organic Chemicals

Hydrogen Peroxide The use of hydrogen peroxide in conjunction with Fe(II) (Fenton’s reagent) or ozone has already been noted. It has been used alone to examine the products from o- and m-phenylenediamines in the context of their mutagenicity (Watanabe et al. 1989). Successive reactions produced 3,4-diaminophenazine from o-phenylenediamine, and 3,7-diaminophenazine from m-phenylenediamine. Manganese Dioxide Manganese dioxide has been used to carry out a range of chemical oxidations, and is the reagent of choice for the oxidation of allylic alcohols (Hudlický 1990). There are several methods for its preparation that may account for differences in its activity. Although it has seldom been exploited for the oxidation of contaminants, two widely different applications have been described: 1. The transformation of several luoroquinolone antibacterials was examined and a number of products from cipraloxacin were tentatively identiied (Zhang and Huang 2005). The quinolone ring was unchanged, and the major product was produced by ission of the piperazine ring to an aniline. 2. The oxidation of triclosan was initiated by oxidation to the PhO • radical. In analogy with reactions established in biomimetic synthesis, this underwent coupling to produce biphenyl ethers and biphenyls that were oxidized further to diphenoquinones (Zhang and Huang 2003). Sulfate Radicals The photochemical generation of sulfate radicals for the degradation of perluorocarboxylic acids has already been noted (Hori et al. 2005a,b). Sulfate radicals are powerful oxidants, and can be produced by the Co-mediated degradation of peroxymonosulfate (HSO5−). They have been shown to be effective for the degradation of 2,4-dichlorophenol and atrazine with the formation of sulfate (Anipsitakis and Dionysiou 2003), and it was shown that they were more effective than conventional Fenton oxidation with hydroxyl radicals, and were effective over a wider range of pH. Sulfate radicals are powerful oxidizing agents and can oxidize chloride to chlorine radicals and molecular chlorine that may be incorporated into the reactant. For example, reaction of peroxymonosulfate with 2,4-dichlorophenol in the presence of chloride produced 2,4,6-trichlorophenol; 2,3,5,6-tetrachlorohydroquinone; and the ring ission products penta- and tetrachloroacetone, and tetrachloromethane (Anipsitakis et al. 2006). Dioxirane that is produced in situ by the reaction of methylpyruvate and peroxymonosulfate has been evaluated as (a) an effective disinfecting agent (Wong et al. 2006) and (b) oxidant of alkenes, alkanes, and phenols (references in Wong et al. 2006).

HALOGENATION Halogenation is important for disinfecting drinking water supplies, generally using molecular chlorine. Most attention has been directed to the adverse production of haloforms and haloacetates from reactions of chlorine with natural substrates, although in water containing bromide/iodide, a number of other reactions may occur. a. While attempts to decrease the formation of haloforms have used chloramination, the undesirable formation of iodoform may take place in the presence of iodide (Leitner 1998). b. The formation of iodoacetate and iodinated propenoates has been demonstrated (Plewa et al. 2004), and the cytotoxic and genotoxic properties of the former (Cemeli et al. 2006) has aroused concern.

33

Abiotic Reactions

c. In water containing particularly high concentrations of bromide, there is a rather special situation; chlorination with a mixture of chlorine and ClO2 produced 2,3,5tribromopyrrole—putatively from humic acids—that is strongly cytotoxic and genotoxic (Richardson et al. 2003). In addition, there is interest in the halogenation of a wide range of anthropogenic contaminants, some of which may occur in raw water before treatment. 1. Pyrene is a common PAH contaminant and may occur in drinking water. Chlorination of water with or without bromide that may be present in coastal environments has been examined. Both chlorinated and brominated pyrenes with halogen substituents at the 1,3-, 1,6-, and 1,8-positions were found, and could putatively be produced by reaction of pyrene with hypochlorous acid and hypochlorite (Hu et al. 2006). 2. Degradation of the insecticide chlorpyrifos has been examined in solutions of aqueous chlorine in which the primary oxidant is hypochlorous acid/hypochlorite. The inal product was 2,3,5-trichloropyrid-2-one produced either directly, or via initial oxidative conversion of the thioate ester by replacement of the sulfur with oxygen (Duirk and Collette 2006). An analogous oxidation was found with diazinon (Zhang and Pehkonen 1999). 3. Transformation of the widely used over-the-counter analgesic acetaminophen (paracetamol) during chlorination produced the toxic 1,4-benzoquinone via the N-acetylquinone-imine and minor amounts of products from chlorination of the phenolic ring (Bedner and Maccrehan 2006). 4. The chlorination of the antibacterial sulfonamide sulfamethoxazole was initiated by Nchlorination of the primary amine. Further reaction of the N,N-dichlorinated compound resulted in the inal production of 3-amino-5-methyloxazole and 1,4-benzoquinone-imine (Dodd and Huang 2004).

Cl (a)

A

A

A

+

HO

HO

HO Cl

Cl

O (b)

C

O

D

C

CO 2 H Cl

D

C

Cl C (c)

Cl

A HO

A O

C

Cl A

B HO

O C

FIGURE 1.31

Chlorination of estrone.

34

Environmental Degradation and Transformation of Organic Chemicals

5. The effect of chlorinating estrone in aqueous solution has been examined. Three reactions involving chlorination of different rings emerged: i. Ring A to produce 2- and 4-chlorinated products (Figure 1.31a) ii. Ring D at C16 followed by hydrolytic ring ission of ring D (Figure 1.31b) iii. Ring A at C10 followed by ission of ring B with the formation of a ketone in ring C at C9 (Figure 1.31c) (Hu et al. 2003). 6. Amino acids have been found in samples of river water (Lee et al. 2006), and chlorination of glycine may produce cyanogen chloride, via N,N-dichloroglycine. At pH values >6, this is converted into cyanogen chloride, whereas at lower pH values N-chloromethylimine is formed (Na and Olson 2006).

THERMAL REACTIONS Gas Phase The products of incomplete combustion may be associated with particulate matter before their discharge into the atmosphere, and these may ultimately enter the aquatic and terrestrial environments in the form of precipitation and dry deposition. It is therefore essential to ensure total destruction of the contaminants, generally by raising the temperature. The spectrum of compounds that have been examined is quite extensive, and several of them are produced by reactions between hydrocarbons and inorganic sulfur or nitrogen constituents of air. Some illustrative examples involving other types of reaction include the following: 1. The pyrolysis of vinylidene chloride produced a range of chlorinated aromatic compounds including polychlorinated benzenes, styrenes, and naphthalenes (Yasahura and Morita 1988), and a series of chlorinated acids including chlorobenzoic acids has been identiied in emissions from a municipal incinerator (Mowrer and Nordin 1987). 2. Nitroaromatic compounds have been identiied in diesel engine emissions (Salmeen et al. 1984), and attention has been directed particularly to 1,8- and 1,6-dinitropyrene that are mutagenic, and possibly carcinogenic (Nakagawa et al. 1983). 3. A wide range of azaarenes including acridines and benzacridines, 4-azaluorene, and 10-azabenzo[a]pyrene (Figure 1.32) has been identiied in particulate samples of urban air, and some of them have been recovered from contaminated sediments (Yamauchi and Handa 1987). 4. Ketonic and quinonoid derivatives of aromatic hydrocarbons have been identiied in automobile (Alsberg et al. 1985) and diesel exhaust particulates (Levsen 1988), and have been recovered from samples of marine sediments (Fernández et al. 1992). 5. Halogenated phenols, particularly 2-bromo-, 2,4-dibromo-, and 2,4,6-tribromophenol, have been identiied in automotive emissions and are the products of thermal reactions involving the dibromoethane fuel additive (Müller and Buser 1986). It could therefore no longer be assumed that such compounds are exclusively the products of biosynthesis by marine algae. 6. Complex reactions occur during high-temperature treatment of aromatic hydrocarbons. An important class of reactions involves the cyclization and condensation of simpler

N

FIGURE 1.32

N

Azaarenes identiied in particulate samples of urban air.

35

Abiotic Reactions

CH 3

CH 3

CH 3

FIGURE 1.33

Products from the pyrolysis of 2-methylnaphthalene.

PAHs to form highly condensed polycyclic compounds. This is discussed more fully by Zander (1995). a. A number of pentacyclic aromatic hydrocarbons have been identiied as products of the gas-phase pyrolysis of methylnaphthalenes. These were formed from 1-methyl- and 2-methylnaphthalene by dimerization (Lang and Bufleb 1958) at various positions, whereas direct coupling with loss of the methyl group was found to be dominant with 2-methylnaphthalene (Lijinsky and Taha 1961) (Figure 1.33). b. A hypothetical scheme involving 2-carbon and 4-carbon additions has been used to illustrate the formation of coronene (circumbenzene) and ovalene (circumnaphthalene) from phenanthrene (Figure 1.34). 7. Concern has been expressed over the formation of chlorinated dibenzo[1,4]dioxins and dibenzofurans during the thermal transformation of organic material in the presence of chloride or organochlorine compounds. a. The high-temperature oxidation of 2-chlorophenol yielded a number of products. At 600°C these included 4,6-dichlorodibenzofuran, 1-chlorodibenzo[1,4]dioxin, and low concentrations of 2,4- and 2,6-dichlorophenol that were produced by reactions with chloride radicals and hydroxyl radicals. They were, however, essentially eliminated at temperatures above 800°C (Evans and Dellinger 2005a). In contrast, under comparable conditions, although a mixture of 2-chloro- and 2-bromophenol also yielded a range of halogenated dibenzofurans, 4,6-dibromodibenzofuran was not produced (Evans and Dellinger 2005b). b. In experiments to clarify the ameliorating effect on the formation of these undesirable products, the effect of adding urea was studied. Reaction of graphite, CuCl2, and urea at 300°C resulted in substantial reduction in the amounts of chlorinated dioxins and furans that were produced, and the formation of 2,6-dichlorobenzonitrile, 4-chloro2-methylaniline, and pentachloropyridine (Kuzuhara et al. 2005).

36

Environmental Degradation and Transformation of Organic Chemicals

C2

C4

C2

C2

C2

C2

FIGURE 1.34

C2

Successive C2 and C4 addition reactions.

In Water There are two distinct conditions that have been used: above the critical temperature and pressure (374°C and 218 atm) water becomes a supercritical luid in which the distinction between the liquid and gaseous states disappears. Since supercritical water can dissolve nonpolar compounds, it has been examined for the degradation of such contaminants. Subcritical water in which the liquid state is maintained by the pressure of the containing vessel has also achieved attention. 1. Destruction of the explosives RDX, HMX, and TNT has been examined using subcritical water in both laboratory- and pilot-scale experiments. In contaminated soils at 150°C, considerable amounts of TNT remained in the soil after reaction for 5 h, and of HMX for 2.5 h. In the pilot-scale experiments, heating at 275°C for 1 h accomplished complete destruction of RDX and TNT, and ca. 98% destruction of HMX (Hawthorne et al. 2000).

Abiotic Reactions

37

2. PCBs a. Destruction of PCBs containing congeners with two to eight chlorine substituents was examined in supercritical water under oxidizing or alkaline reducing conditions. The latter were more effective and, although chlorinated dibenzofurans with one to six chlorine substituents were formed at temperatures of 250°C they were removed at 350°C. Experiments with the 245-245 hexachloro congener were used to illustrate the formation of chlorinated dibenzofurans (Weber et al. 2002). b. Examination of the destruction of Arochlor 1254 in paint scrapings at 350°C revealed the signiicance of the metals. Experiments with zero-valent metal additions in the absence of paint showed their effectiveness in the order Pb≡Cu >Al >Zn >Fe. With Pb and Cu destruction of tetra to heptachloro congeners to predominantly monochlorobiphenyl occurred (Kubátova et al. 2003). c. Zero-valent iron has been used for the reductive dechlorination of PCBs in subcritical water at 250°C (Yak et al. 1999). Extensive loss of the more highly chlorinated congeners in Arochlor 12609 took place with the formation of congeners having one to four chlorine substituents, while with longer exposure times these were virtually eliminated. 3. At 200°C destruction of γ-hexachlorocyclohexane in subcritical water occurred in 1 h, and for dieldrin in 1 h at 300°C. The pathway for γ-HCH involved successive formation of 1,2,4-trichloro-, 1,4-dichloro-, and monochlorobenzene that was hydrolyzed to phenol (Kubátova et al. 2002). 4. The use of subcritical water at 275°C was successful in removing PAHs with two to six rings (including the carcinogenic benzo[a]pyrene) from soil at a contaminated site, and the wastewater that was produced appeared to be suitable for further exploitation (Lagadec et al. 2000).

ELECTROCATALYTIC REACTIONS The energy for the ission of the covalent bond in organic contaminants is normally supplied thermally using thermodynamically accessible chemical or biochemical reactions, or by the introduction of catalysts to lower the activation energy of the reactions. There has been interest, however, in using electrical energy in a number of forms to carry out these reactions. A selection of processes for the destruction of contaminant is noted with some illustrative examples. 1. The simplest applications involve direct anodic oxidation in aqueous media. a. During the anodic oxidation of EDTA at alkaline pH on a smooth platinum electrode (Pakalapati et al. 1996), degradation was initiated by removal of the acetate side chains as formaldehyde, followed by deamination of the ethylenediamine that is formed to glyoxal and oxalate. Oxalate and formaldehyde were oxidized to CO2. b. Using a platinum electrode coated with a metal oxide ilm (Ti, Ru, Sn, and Sb) in conjunction with a solid Naion membrane, complete destruction of 4-chlorophenol could be achieved in reactions involving the formation of benzoquinone followed by ring ission to succinate acetate and CO2 (Johnson et al. 1999). On account of the products this was termed “electrochemical incineration.” 2. Electrohydraulic discharge plasmas have been used in different conigurations. a. The degradation of 2,4,6-trinitrotoluene has been carried out in the presence of ozone. The hydroxyl radicals that were produced brought about oxidation to an intermediate that was identiied as 2,4,6-trinitrobenzaldehyde (Lang et al. 1998). b. The degradation of 4-chlorophenol and 3,4-dichloroaniline was carried out by the shock wave that was developed in the cell (Willberg et al. 1996).

38

Environmental Degradation and Transformation of Organic Chemicals

3. Variants of glow discharge plasmas have been used: a. The dechlorination of pentachlorophenol took place with the formation of C1 and C2 carboxylic acids (Sharma et al. 2000). b. In the presence of Fe(III), degradation of phenol which took place by hydroxylation followed by ring ission (Liu and Jiang 2005) in reactions are analogous to those in the electro-Fenton reaction that has been examined for the degradation of 4-nitrophenol (Oturan et al. 2000). 4. Electrolytic reduction has been carried out under several conditions. a. Using a porous nickel electrode and at voltages that were maintained by a potentiostat, a number of reductive reactions were observed: tetrachloroethene and trichloroethene → ethane and ethene, and penta-, tetra-, tri, and dichloroethanes to ethane (Liu et al. 2000). b. Fuel cells have been used in various modiications to carry out gas-phase reductive dechlorination of trichloroethene: • Using a polymer electrolyte membrane cell in which H2 lowed through the anode chamber. The major intermediate chlorinated products from tetrachloroethene or tetrachloromethane were trichloroethene or trichloromethane, and these were inally reduced to a mixture of ethane and ethene, or methane (Liu et al. 2001). • Reduction of trichloroethene to ethane took place in a modiied fuel cell to which H2 was introduced, although the loss of catalytic activity with time could present a serious limitation (Ju et al. 2006).

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Moore DE, S Roberts-Thomson, D Zhen, CC Duke (1990) Photochemical studies on the anti-inlammatory drug diclofenac. Photochem Photobiol 52: 685–690. Mowrer J, J Nordin (1987) Characterization of halogenated organic acids in lue gases from municipal waste incinerators. Chemosphere 16: 1181–1192. Müller MD, H-R Buser (1986) Halogenated aromatic compounds in automotive emissions from leaded gasoline additives. Environ Sci Technol 20: 1151–1157. Müller SR, H-R Zweifel, DJ Kinnison, JA Jacobsen, MA Meier, MM Ulrich, RP Schwarzenbach (1996) Occurrence, sources, and fate of trichloroacetic acid in Swiss waters. Environ Toxicol Chem 15: 1470–1478. Na C, TM Olson (2006) Mechanism and kinetics of cyanogen chloride formation from the chlorination of glycine. Environ Sci Technol 40: 1469–1477. Nakagawa R, S Kitamori, K Horikawa, K Nakashima, H Tokiwa (1983) Identiication of dinitropyrenes in diesel-exhaust particles. Their probable presence as the major mutagens. Mutation Res 124: 201–211. Nélieu S, L Kerhoas, J Einhorn (2000) Degradation of atrazine into ammeline by combined ozone/hydrogen peroxide treatment in water. Environ Sci Technol 34: 430–437. Nelson L, I Shanahan, HW Sidebottom, J Treacy, OJ Nielsen (1990) Kinetics and mechanism for the oxidation of 1,1,1-trichloroethane. Int J Chem Kinet 22: 577–590. Nishioka MG, CC Howard, DA Conros, LM Ball (1988) Detection of hydroxylated nitro aromatic and hydroxylated nitro polycyclic aromatic compounds in ambient air particulate extract using bioassay-directed fractionation. Environ Sci Technol 22: 908–915. Nomiyama K, T Tanizaki, H Ishibashi, K Arizono, R Shinohara (2005) Production mechanism of hydroxylated PCBs by oxidative degradation of selected PCBs using TiO2 in water and estrogenic activity of their intermediates. Environ Sci Technol 39: 8762–8769. Nörtemann B (1992) Total degradation of EDTA by mixed cultures and a bacterial isolate. Appl Environ Microbiol 58: 671–676. Orlando JJ (2003) Atmospheric chemistry of organic bromine and iodine compounds. Handbook Environ Chem 3R: 253–299. Oturan MA, J Peiroten, P Chartin, AJ Acher (2000) Complete destruction of p-nitrophenol in aqueous medium by electro-Fenton method. Environ Sci Technol 34: 3474–3479. Paciolla MD, G Davies, SA Jansen (1999) Generation of hydroxyl radicals from metal-loaded humic acids. Environ Sci Technol 33: 1814–1818. Pakalapati SNR, BN Popov, RE White (1996) Anodic oxidation of ethylenediaminetetraacetic acid on platinum electrode in alkaline medium. J Electrochem Soc 143: 1636–1643. Pelizzetti E, V Maurino, C Minero, V Carlin, E Pramauro, O Zerbinati, ML Tosata (1990) Photocatalytics degradation of atrazine and other s-triazine herbicides. Environ Sci Technol 24: 1559–1565. Perdue EM, NL Wolfe (1982) Modiication of pollutant hydrolysis kinetics in the presence of humic substances. Environ Sci Technol 16: 847–852. Perlinger JA, W Angst, RP Schwarzenbach (1996) Kinetics of the reduction of hexachloroethane by juglone in solutions containing hydrogen sulide. Environ Sci Technol 30: 3408–3417. Pitts JN Jr, B Zielinska, JA Sweetman, R Atkinson, AM Winer (1985b) Reactions of adsorbed pyrene and perylene with gaseous N2O5 under simulated atmospheric conditions. Atmos Environ 19: 911–915. Pitts N Jr, R Atkinson, JA Sweetman, B Zielinska (1985a) The gas-phase reaction of naphthalenes with N2O5 to form nitronaphthalenes. Atmos Environ 19: 701–705. Platt UF, AM Winer, HW Biermann, R Atkinson, JN Pitts, Jr (1984) Measurement of nitrate radical concentrations in continental air. Environ Sci Technol 18: 365–369. Platz J, OJ Nielsen, J Sehested, TJ Wallington (1995) Atmospheric chemistry of 1,1,1-trichloroethane: UV absorption spectra and self-reaction kinetics of CCl3CH2 and CCl3CH2O2 radicals, kinetics of the reactions of the CCl3CH2O2 radical with NO and NO2, and the fate of alkoxy radical CCl3CH2O. J Phys Chem 99: 6570–6579. Plewa MJ, ED Wagner, SD Richardson, AD Thurston, Y-T Woo, AB McKague (2004) Chemical and biological characterization of newly discovered iodoacid drinking water disinfection byproducts. Environ Sci Technol 38: 4713–4722. Pradhan SP, JR Paterek, BY Liu, JR Conrad, VJ Srivastava (1997) Pilot-scale bioremediation of PAH-contaminated soils. Appl Biochem Biotechnol 63/65: 759–773. Quinn J, C Geiger, C Clausen, K Brooks, C Coon, S O´Hara, T Krug, D Major, W-S Yoon, A Gavskar, T Holdsworth (2005) Field demonstration of DNAPL dehalogenation using emulsiied zero-valent iron. Environ Sci Technol 39: 1309–1318.

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2 Biotic Reactions PART 1 MICROBIAL REACTIONS INTRODUCTION It is generally conceded that biotic reactions involving microorganisms are of major signiicance in determining the fate and persistence of organic compounds in aquatic and terrestrial ecosystems. The role of higher biota in carrying out important transformations is addressed in Part 2 of this chapter. Archaea, bacteria, cyanobacteria, fungi, yeasts, and algae comprise a large and diverse number of taxa. However, only a relatively small number of even the genera have been examined in the context of biodegradation, and there is no way of determining how representative these are. Care should therefore be exercised in drawing conclusions about the metabolic capability of the plethora of taxa included within these major groups of microorganisms. Attention is directed to the role of populations that are discussed in Chapter 13.

DEFINITIONS—DEGRADATION AND TRANSFORMATION It is essential to make a clear distinction between biodegradation and biotransformation in the beginning: Biodegradation. Under aerobic conditions, biodegradation results in the mineralization of an organic compound to carbon dioxide and water and—if the compound contains nitrogen, sulfur, phosphorus, or chlorine—with the release of ammonium (or nitrite), sulfate, phosphate, or chloride. These inorganic products may then enter well-established geochemical cycles. Under anaerobic conditions, methane may be formed in addition to carbon dioxide, and sulfate may be reduced to sulide. Biotransformation. In contrast, biotransformation involves only a restricted number of metabolic reactions, and the basic framework of the molecule remains essentially intact. Illustrative examples of biotransformation reactions include the following, although it should be emphasized that other microorganisms may be able to degrade the substrates: 1. The hydroxylation of 14-chlorodehydroabietic acid by fungi (Figure 2.1) (Kutney et al. 1982) 2. The epoxidation of alkenes by bacteria (Patel et al. 1982; van Ginkel et al. 1987) 3. The formation of 16-chlorohexadecyl-16-chlorohexadecanoate from hexadecyl chloride by Micrococcus ceriicans (Kolattukudy and Hankin 1968) CH3(CH2)14 –CH2Cl → ClCH2(CH2)14 –CH2–O–CO–(CH2)14 –CH2Cl 4. The O-methylation of chlorophenols to anisoles by fungi (Gee and Peel 1974; Cserjesi and Johnson 1972) and by bacteria (Suzuki 1978; Rott et al. 1979; Neilson et al. 1983; Häggblom et al. 1988) 5. The formation of glyceryl-2-nitrate from glyceryl trinitrate by Phanerochaete chrysosporium (Servent et al. 1991) 51

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HO Cl

Cl

CO 2 H

CO 2 H OH

H

OH

OH HO

HO Cl

CO 2 H

FIGURE 2.1

Cl

CO 2 H

Biotransformation of dehydroabietic acid by Mortierella isabellina.

The initial biotransformation products may, in some cases, be incorporated into cellular material. For example, the carboxylic acids formed by the oxidation of long-chain n-alkyl chlorides were incorporated into cellular fatty acids by strains of Mycobacterium sp. (Murphy and Perry 1983). The fungus Mortierella alpina, in which hexadecene was oxidized by the fungus by ω-oxidation (Shimizu et al. 1991), formed lipids that contained carboxylic acids containing both 18 and 20 carbon atoms including the unusual polyunsaturated acid 5cis, 8cis, 11cis, 14cis, 19-eicosapentaenoic acid. Metabolites of metolachlor that could only be extracted from the cells with acetone were apparently chemically bound to unidentiied sulfur-containing cellular components (Liu et al. 1989). Biodegradation and biotransformations are of course alternatives, but they are not mutually exclusive. For example, it has been suggested that for chlorophenolic compounds, the O-methylation reaction may be an important alternative to reactions that bring about their degradation (Allard et al. 1987). Apart from the environmental signiicance of biotransformation reactions, many of them have enormous importance in biotechnology for the production of valuable metabolites, for example, the synthesis of hydroxylated steroids and in reactions that take advantage of the oxidative potential of methanotrophic bacteria (Lidstrom and Stirling 1990) and rhodococci (Finnerty 1992). It is also important to consider the degradation of xenobiotics in the wider context of metabolic reactions carried out by the cell. The cell must obtain energy to carry out essential biosynthetic (anabolic) reactions for its continued existence, and to enable growth and cell division to take place. The substrate therefore cannot be degraded entirely to carbon dioxide or methane, for example, and a portion must be channeled into the biosynthesis of essential molecules. Indeed, many organisms will degrade xenobiotics only in the presence of a suitable more readily degraded growth substrate that supplies both cell carbon and the energy for growth: this is relevant to discussions of “cometabolism” and “concurrent metabolism,” which is discussed in Chapter 4. Growth under anaerobic conditions is demanding both physiologically and biochemically, since the cells will generally obtain only low yields of energy from the growth substrate, and must, in addition, maintain a delicate balance between oxidative and reductive processes. Only a few examples of mechanisms for ATP generation in anaerobes are given below: 1. Clastic reactions from 2-keto acid-CoA esters produced in a number of degradations 2. Reactions involving carbamyl phosphate in the degradation of arginine in clostridia, and the fermentation of allantoin by Streptococcus allantoicus 3. The activity of formyl THF synthase during the fermentation of purines by clostridia 4. The reductive dechlorination of 3-chlorobenzoate by Desulfomonile tiedjei DCB-1

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5. The proton pump in Oxalobacter formigenes 6. The biotin-dependent carboxylases that couple the decarboxylation of malonate to acetate in Malonomonas rubra to the transport of Na+ across the cytoplasmic membrane True fermentation implies that a single substrate is able to provide carbon for cell growth and at the same time satisfy the energy requirements of the cell. A simple example of fermentation is the catabolism of glucose by facultatively anaerobic bacteria to pyruvate that is further transformed into a variety of products including acetate, butyrate, propionate, or ethanol by different organisms. In contrast, a range of electron acceptors may be used under anaerobic conditions to mediate oxidative degradation of the carbon substrate at the expense of the reduction of the electron acceptors. For example, the following reductions may be coupled to oxidative degradation: nitrate to nitrogen (or nitrous oxide), sulfate to sulide, carbonate to methane, fumarate to succinate, trimethylamineN-oxide to trimethylamine, or dimethyl sulfoxide to dimethyl sulide, which are discussed in Chapter 3, Part 2. The environments required by the relevant organisms are determined by the redox potential of the relevant reactions, so that increasingly reducing conditions are required for reduction of nitrate, sulfate, and carbonate. Attention is drawn to the dechlorination by anaerobic bacteria of both chlorinated ethenes and chlorophenolic compounds that serve as electron acceptors with electron donors including formate, pyruvate, and acetate. This is termed dehalorespiration and is important in the degradation of a range of halogenated compounds under anaerobic conditions, and is discussed further in Chapter 3, Part 2 and Chapter 7, Part 3. Probably, most of the microbial degradations and transformations that are discussed in this book are carried out by heterotrophic microorganisms that use the xenobiotic as a source of both carbon and energy, or by cometabolism (Chapter 4). In addition, xenobiotics may serve only as sources of nitrogen, sulfur, or phosphorus. The attention is briely drawn here to those groups of organisms many of whose members are autotrophic or lithotrophic. Discussion of the complex issue of organic nutrition of chemolithotrophic bacteria, and the use of the term “autotrophy” is given in a classic review by Matin (1978). The groups of organisms that are discussed here in the context of biotransformation include 1. Ammonia-oxidizing bacteria including Nitrosomonas europaea 2. Facultatively heterotrophic thiobacilli that use a number of organic sulfur compounds as energy source 3. Oxygenic photolithotrophic algae and cyanobacteria It is important to underscore the fact that carbon dioxide is required not only for the growth of strictly phototrophic and lithotrophic organisms. Many heterotrophic organisms that are heterotrophic have an obligate requirement for carbon dioxide for their growth. Illustrative examples include the following: a. Anaerobic bacteria such as acetogens, methanogens, and propionic bacteria. b. Aerobic bacteria that degrade propane (MacMichael and Brown 1987), the branched hydrocarbon 2,6-dimethyloct-2-ene (Fall et al. 1979), or oxidize carbon monoxide (Meyer and Schlegel 1983). c. The anaerobic biotransformation of aromatic compounds may be dependent on CO2, and a review by Ensign et al. (1998) provides a brief summary of the role of CO2 in the metabolism of epoxides by Xanthobacter sp. strain Py2, and of acetone by both aerobic and anaerobic bacteria. d. The lag after diluting glucose-grown cultures of Escherichia coli into fresh medium may be eliminated by the addition of NaHCO3 and is consistent with the requirement of this organism for low concentrations of CO2 for growth (Neidhardt et al. 1974).

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BIODEGRADATION OF ENANTIOMERS The molecules of some compounds including agrochemicals such as chlorinated phenoxypropionates, certain N-substituted 2,6-dimethylanilines (e.g., metalaxyl) (Buser et al. 2002), nonplanar PCB congeners (i.e., IUPAC 91, 95, 132, 136, 149, 174, 176, 183) (Kaiser 1974), o,p′-DDT (Garrison et al. 2000), and α-hexachlorocyclohexane (Wiberg et al. 2001) are asymmetric. They may therefore exist as pairs of mirror-image enantiomers that display differential biological activity and biodegradability. Only one of them may be encountered in environmental samples, and this may plausibly be attributed to the preferential destruction or transformation of one enantiomer that is consistent with observed signiicant differences in the biodegradability of enantiomers. Different strategies for the biodegradation of racemates may be used and are illustrated in the following examples, and the pathways are discussed in the appropriate chapters: 1. Both enantiomers of mandelate were degraded through the activity of a mandelate racemase (Hegeman 1966), and the racemase (mdlA) is encoded in an operon that includes the following two enzymes in the pathway of degradation: S-mandelate dehydrogenase (mdlB) and benzoylformate decarboxylase (mdlC) (Tsou et al. 1990). 2. Only the R(+) enantiomer of the herbicide 2-(2-methyl-4-chlorophenoxy)propionic acid was degraded (Tett et al. 1994), although cell extracts of Sphingomonas herbicidovorans grown with the R(–) or S(–) enantiomer, respectively, transformed selectively the R(–) or S(–) substrates to 2-methyl-4-chlorophenol (Nickel et al. 1997). 3. Degradation of linear alkylbenzenes may produce chiral 3-phenylbutyrate. The degradation of the R(–) and R(–) enantiomers has been examined in Rhodococcus rhodochrous strain PB1 (Simoni et al. 1996). Whereas the S-enantiomer undergoes dioxygenation to the catechol that is a terminal metabolite, the R-enantiomer is degraded to 3-phenylpropionate followed by dioxygenation and ring ission. 4. The α-isomer of hexachlorocyclohexane exists in two enantiomeric forms, and both are degraded by Sphingomonas paucimobilis strain B90A by dehydrochlorination to 1,3,4, 6-tetrachlorocyclohexa-1,4-diene that is spontaneously degraded to 1,2,4-trichlorophenol. In this strain, there are two enzymes LinA1 and LinA2 that speciically accept (+)-αHCH or (–)-α-HCH to produce β-pentachlorocyclohexene-1 and -2. Both enzymes were 88% identical at the amino acid level, and LinA2 was identical to LinA of S. paucimobilis strain UT26. This implies that in strains such as UT26 that contain only a single dehydrochlorinase, enantioselective degradation may take place with enrichment of the nondegradable enantiomer (Suar et al. 2005). 5. Cells of Acinetobacter sp. NCIB 9871 grown with cyclohexanol carried out enantiomerically speciic degradation of a racemic substituted norbornanone to a single ketone having >95% enantiomeric excess (Levitt et al. 1990). 6. Bis-(1-chloro-2-propyl)ether has two chiral centers, and exists in (R,R)-, (S,S)-, and a meso form. It is degraded by Rhodococcus sp. with a preference for the S,S-enantiomer with the intermediate formation of 1-chloro-propan-2-ol and chloroacetone (Garbe et al. 2006). This enantiomeric speciicity has been of interest in other contexts, and stereospeciic biotransformation has been observed. Examples include the enantiomeric oxidation of sulides to sulfoxides (Chapter 11, Part 2) and steroid and triterpene hydroxylation (Chapter 7, Part 2). Natural systems may be quite complex. For example, the enantiomerization of phenoxyalkanoic acids containing a chiral side chain has been studied in soil using 2H2O (Buser and Müller 1997). It was shown that there was an equilibrium between the R- and S-enantiomers of both 2-(4-chloro-2methylphenoxy)propionic acid (MCPP) and 2-(2,4-dichlorophenopxy)propionic acid (DCPP) with an equilibrium constant favoring the herbicidally active R-enantiomers. The exchange reactions

Biotic Reactions

55

proceeded with both retention and inversion of coniguration at the chiral sites. This important issue will certainly attract increasing attention in the context of the preferential microbial synthesis of intermediates of speciic coniguration.

SEQUENTIAL MICROBIAL AND CHEMICAL REACTIONS Microbial activity may produce reactive intermediates that undergo spontaneous chemical transformation to terminal metabolites. This is quite a frequent occurrence, and its diversity is illustrated by the following examples: 1. A bacterial strain BN6 oxidizes 5-aminonaphthalene-2-sulfonate by established pathways to 6-amino-2-hydroxybenzalpyruvate that undergoes spontaneous cyclization to 5-hydroxyquinoline-2-carboxylate (Figure 2.2a) (Nörtemann et al. 1993). 2. The oxidation of benzo[b]thiophene by strains of pseudomonads produces the sulfoxide that undergoes an intramolecular Diels–Alder reaction followed by further transformation to benzo[b]naphtho[1,2-d]thiophene (Figure 2.2b) (Kropp et al. 1994). 3. The degradation of 4-chlorobiphenyl by Sphingomonas paucimobilis strain BPSI-3 formed the intermediates 4-chlorobenzoate and 4-chlorocatechol. Fission products from the catechol reacted with NH4+ to produce chloropyridine carboxylates (Davison et al. 1996) (Figure 2.2c). 4. 4-Nitrotoluene is degraded by a strain of Mycobacterium sp. via the corresponding 4-amino3-hydroxytoluene (Spiess et al. 1998): this is dimerized abiotically to form a dihydrophenoxazinone, and after extradiol cleavage to 5-methylpyridine -2-carboxylate (Figure 2.2d). 5. The incubation of 3,5-dichloro-4-methoxybenzyl alcohol with methanogenic sludge produced the de-O-methylated compound that was transformed to 2,6-dichlorophenol, and abiotically dimerized to bis(3,5-dichloro-4-hydroxyphenyl)methane (Verhagen et al. 1998) (Figure 2.2e). 6. The transformation of aromatic amino acids to the 2-ketoacids was mediated by Morganella morganii, and these subsequently underwent a hemin-dependent chemical transformation with the production of CO (Hino and Tauchi 1987). 7. Tetrachloroethene may be degraded by bacteria via the epoxide, and chemical hydrolysis of this produces CO and CO2 from oxalyl chloride as major products, whereas only low amounts of trichloroacetate were produced (Yoshioka et al. 2002). Nitrite (or compounds at the same or lower oxidation level) is produced microbiologically from nitrate, and may then react with the substrate to produce stable end products. The production of nitrite is the sole metabolic function of the bacteria and, in view of concern over the presence of nitrate in groundwater, the following possible environmental signiicance of these or analogous reactions should not be overlooked: 1. A strain of Escherichia coli produces a naphthotriazole from 2,3-diaminonaphthalene and nitrite that is formed from nitrate by the action of nitrate reductase. The initial product is NO, which is converted by reactions with oxygen into the active nitrosylating agent that reacts chemically with the amine (Ji and Hollocher 1988). A comparable reaction may plausibly account for the formation of dimethylnitrosamine by Pseudomonas stutzeri during growth with dimethylamine in the presence of nitrite (Mills and Alexander 1976) (Figure 2.2f ). 2. The formation of 3,3′,4,4′-tetrachloroazobenzene, 1,3-bis(3,4-dichlorophenyl)triazine and 3,3′,4,4′-tetrachlorobiphenyl from 3,4-dichloroaniline and nitrate by E. coli plausibly involved intermediate chemical formation of the diazonium compound by reaction of the amine with nitrite (Corke et al. 1979) (Figure 2.2g).

56

Environmental Degradation and Transformation of Organic Chemicals

OH

OH

SO 2 H

CO−CO2 H

(a)

N CO2 H

NH 2

NH 2

SO

(b) S

S

S

S O

O

CO2 H

OH

N

CO2 H CO2 H

CO2 H

OH OH

Cl

Cl

Cl

(c)

CO2 H OH CHO

Cl

N

CO2 H

CH3

Cl CH3

CH3

CH3

CH 3 N CHO

(d) NHOH

NO 2

NH2

CH 3

NH 2

O

CH 3 O

N

CH2 OH

CH2 OH

CO 2 H

CO 2 H

OH

CH2

Cl

CH 2

NH 2 Cl

(e) Cl

Cl

Cl

Cl

Cl

OH

OMe

OH

HO

Cl O

NH2

N

NH2

N H

(f)

Cl

Cl

N NH2

Cl Cl

(g)

N

N

Cl

Cl

+ Cl

Cl

Cl Cl

Cl

+

Cl N

N

NH

Cl Cl

Cl Cl

FIGURE 2.2 Transformation of (a) 5-aminonaphthalene-2-sulfonate, (b) benzo[b]thiophene, (c) 4-chlorobiphenyl, (d) 4-nitrotoluene, (e) 3,5-dichlor-4-methoxybenzyl alcohol, (f) 2,3-diaminonaphthalene in presence of nitrate, and (g) 3,4-dichloroaniline presence of nitrate.

Biotic Reactions

57

3. Nitro-containing metabolites have been isolated from a number of substrates when the medium contained nitrate. Reduction to nitrite is the putative source of the nitro group, and two mechanisms have been suggested: (i) nitrosation by NO+ produced from HO–NO in a slightly acidic medium followed by oxidation or (ii) nitration of an intermediate arene oxide by nitrite. Since all the primary metabolites have phenolic groups and the introduced nitro groups are ortho or para to these, the irst is probably the more attractive general reaction. In support of the alternative, however, an NIH shift has been demonstrated in the transformation of 2-chlorobiphenyl to 2-hydroxy-3-chlorobiphenyl by a methylotrophic organism, so that formation of an arene oxide cannot be excluded (Adriaens 1994). The following illustrate these reactions: a. The formation of nitro-containing metabolites during the degradation of 4-chlorobiphenyl by strain B-206 (Sylvestre et al. 1982). b. Corynebacterium sp. that utilizes dibenzothiophene as a sulfur source produced 2-hydroxybiphenyl, and subsequently nitrated this to form two hydroxynitrobiphenyls (Omori et al. 1992). c. The transformation of α-tocopherol by Streptomyces catenulae produced 5-nitrotocopherol in addition to quinones (Rousseau et al. 1997). d. The transformation of 2-hydroxybenz[1,4]oxazin-3-one with Gliocladium cibotii produced the intermediate 2-hydroxyacetanilide that was used to produce nitro derivatives (Zikmundová et al. 2002).

THE SPECTRUM OF ORGANISMS Bacteria in Their Natural Habitats Illustrations of the plethora of pathways used by bacteria for the degradation and biotransformation of xenobiotics are provided in Chapters 7 through 11. It is appropriate to say something here of the metabolic spectrum of speciic groups of organisms, in particular, those that have hitherto achieved less prominence in discussions of biodegradation and biotransformation. The application of the methodology of molecular biology has revealed new dimensions in the range of naturally occurring organisms. Further details of some of these in the context of bioremediation are given in Chapter 13. It should be appreciated that in natural situations, bacteria may be subjected to severe nutrient limitation so that they are compelled to reproduce at extremely low rates in order to conserve their metabolic energy (Kjellberg et al. 1987; Siegele and Kolter 1992). This does not necessarily mean, however, that these organisms have negligible metabolic potential toward xenobiotics. Other slowgrowing organisms may be well adapted to the natural environment (Poindexter 1981) although they may not be numerically dominant among organisms isolated by normal procedures (Schut et al. 1993). An unusual situation has been observed in Pseudomonas putida strain mt-2 that contains the TOL plasmid pWWO. After growth with 3-methylbenzoate, cells were exposed to concentrations of toluene from 4 mg/L (growth supporting) to 130 mg/L (inhibitory) to 267 mg/L (lethal). Protein synthesis was rapidly inhibited with the concomitant production of new proteins, which were characteristic of cell starvation, and which could be suppressed by the addition of 3-methylbenzoate as carbon source. Cells exposed to 4 mg/L ceased to produce “starvation proteins” within 3 h and growth was initiated. At the higher concentrations, these proteins persisted for increasing lengths of time and at 267 mg/L there was a rapid loss of viability (Vercellone-Smith and Herson 1997). An important example is provided by Lactococcus lactis that enters a resting phase after consumption of the available carbohydrates. The ensuing noncultivable state is characterized by the synthesis of 2-methylbutyrate that is derived from l-leucine, and provides the intermediate 3-hydroxy-3-methylglutarate (Ganesan et al. 2006).

58

Environmental Degradation and Transformation of Organic Chemicals

Attention is directed to organisms that have hitherto evaded isolation or are represented by only a few cultivated examples. Such organisms may well outnumber those that have been isolated as pure cultures, frequently using elective enrichment. A few illustrations are given below: 1. Archaea belonging to the kingdom Crenarchaeota deserve attention. Although it has been assumed that these are extreme thermophiles, members of this group have been identiied by molecular techniques in other habitats, for example, soils (Buckley et al. 1998), boreal forest soil (Jurgens et al. 1997), and in plant extracts (Simon et al. 2005). 2. Organisms belonging to the phylum Verrumicrobia have been detected in soil throughout the world although hitherto only a single organism Chthoniobacter lavus has been obtained in pure culture (Sangwan et al. 2004). This was made possible by the use of a dilute complex medium solidiied with gellan gum in place of agar (Janssen et al. 2002), and has been extended (Sangwan et al. 2005). Before discussing some of the larger groups of microorganisms that have been implicated in biodegradation and biotransformation, brief comments are made on other groups of organisms that have hitherto attracted somewhat limited attention: a. Typically clinical organisms in environmental samples with degradative capability that include Klebsiella pneumoniae, Mycobacterium tuberculosis, and Ochrobactrum spp. b. Marine bacteria, many of which are oligotrophic, including species of Cycloclasticus, Neptunomonas, Marinobacter, and Sulitobacter c. Gram-positive organisms belonging to the genera Mycobacterium, Rhodococcus, and Gordonia Marine and Oligotrophic Bacteria Although most illustrations have been taken from investigations of freshwater environments—lakes and rivers—fewer relate to the marine environment. In view of the area of the globe that is covered by open sea this may seem remarkable, and the degradation of xenobiotics by marine bacteria has received somewhat limited attention. Roseobacters represent one of the major groups of marine bacteria and have been found not only in a range of geographical habitats but in various degrees of association. A review provides a valuable summary, and draws attention to some of their metabolic potential including the oxidation of CO and the degradation of aromatic compounds (Buchan et al. 2005). Illustrative examples of degradation by marine bacteria are given below: 1. Strains of Marinobacter sp. that are able to degrade aliphatic hydrocarbons and related compounds have been isolated (Gauthier et al. 1992), and Marinobacter sp. strain CAB is capable of degrading 6,10,14-trimethylpentadecan-2-one under both aerobic and denitrifying conditions with the production of a range of metabolites (Rontani et al. 1997). It has been shown that Alcanivorax borkumensis is also able to degrade a number of hydrocarbons (Yakimov et al. 1998). 2. A halophilic Archaeon assigned to the genus Haloferax is able to use a restricted range of aromatic substrates including benzoate as sole sources of carbon and energy (Emerson et al. 1994). This represents an extension of the range of substrates for this genus in marine localities and has attracted attention on account of their ability to degrade polycyclic aromatic hydrocarbons (PAHs). 3. Organisms assigned to the genus Cycloclasticus have been isolated from a number of geographical locations and display a considerable metabolic versatility as follows: a. Strains were isolated from the Gulf of Mexico and from Puget Sound. In an artiicial seawater medium, they were able to degrade a range of PAHs including alkylated

Biotic Reactions

4. 5.

6.

7.

8.

59

naphthalenes, phenanthrene, anthracene, and luorene at concentrations ranging from 1 to 5 ppm (Geiselbrecht et al. 1998). Strains from both localities were numerically important, and were similar based on both 16S ribosomal DNA (rDNA) sequences and phylogenetic relationships determined from the sequences of arene dioxygenases. b. Cycloclasticus oligotrophus strain RB1 that harbors genes with a high degree of homology to that encoding xylene degradation in terrestrial pseudomonads, is able to grow at the expense of toluene, xylenes, biphenyl, naphthalene, and phenanthrene (Wang et al. 1996). c. Cycloclasticus sp. strain A5 was able to grow at the expense of naphthalenes, phenanthrenes, and luorenes—though not anthracene (Kasai et al. 2003). Bacteria isolated from marine macrofaunal burrow sediments and assigned to Lutibacterium anuloederans were able to degrade phenanthrene in a heavily contaminated sediment (Chung and King 2001). Marine bacteria were isolated from a creosote-contaminated sediment in Puget Sound by enrichment with naphthalene (Hedlund et al. 1999). It was shown that the gene encoding the naphthalene dioxygenase ISP from this strain was not closely related to those from naphthalene-degrading strains of Pseudomonas or Burkholderia. Although analysis of 16S rDNA suggested a close relation to the genus Oceanospirillum, the differences were considered suficient to assign these strains to a new taxon—Neptunomonas naphthovorans. Strains of Sagittula stellata and Sulitobacter sp. that are members of the Roseobacter group of organisms were screened for the presence of 3,4-dihydroxybenzoate dioxygenase that is involved in the degradation of several aromatic carboxylates (Buchan et al. 2000). The enzyme was widely distributed in this group, and the organisms were able to degrade a number of substrates including benzoate, anthranilate, salicylate, 4-hydroxybenzoate, and vanillate. Marine roseobacters that contain bacteriochlorophyll a have been described (Oz et al. 2005), and the bacteriochlorophyll a–containing marine bacterium Porphyrobacter sanguineus was able to degrade biphenyl and dibenzofuran, though unable to use them as sole substrates for growth (Hiraishi et al. 2002). The roseobacters Silicibacter pomeroyi and Roseovarius nubinhibens were able to carry out the degradation of dimethylsulfoniopropionate to dimethylsulide, and to methanethiol (González et al. 2003), and are discussed further in Chapter 11, Part 2.

It is necessary to take into account critical aspects of the physiology and biochemistry of these marine organisms and, although parenthetical comments on marine bacteria are made in various sections of this book, it is convenient to bring together some of their salient features. It should also be appreciated that terrestrial organisms that have a high tolerance to salinity may be isolated from inshore seawater samples. Among these are the yeasts that have been isolated from coastal marine sediments. Such organisms are excluded from the present discussion, which is restricted to oceanic water: 1. It is experimentally dificult to obtain numerical estimates of the total number of bacteria present in seawater, and the contribution of ultramicroorganisms that have a small cell volume and low concentrations of DNA may be seriously underestimated. Although it is possible to evaluate their contribution to the uptake and mineralization of readily degraded compounds such as amino acids and carbohydrates, it is more dificult to estimate their potential for degrading xenobiotics at realistic concentrations. 2. The use of conventional plating procedures may result in the isolation of only fast-growing organisms that outgrow others—which may be numerically dominant and which are unable to produce colonies on such media. The substrate concentrations used for isolation may have been unrealistically high, so that obligately oligotrophic organisms were outnumbered during attempted isolation.

60

Environmental Degradation and Transformation of Organic Chemicals

3. There is an indeterminacy in the term “oligotroph,” and the dilemma is exacerbated by the fact that it may be impossible to isolate obligate oligotrophs by established procedures. The application of DNA probes should, however, contribute to an understanding of the role of these “noncultivable” organisms. Oligotrophic bacteria in the marine environment are able to utilize low substrate concentrations, and they may be important in pristine environments. 4. During prolonged storage in the laboratory under conditions of nutrient starvation, facultatively oliogotrophic bacteria may be isolated and these display transport systems for the uptake of amino acids and glucose that are coregulated. 5. Organisms in natural ecosystems may not be actively dividing but may, nonetheless, be metabolically active. This may be particularly important for ultramicro marine bacteria in their natural habitat.

Lithotrophic Bacteria These are major groups of microorganisms that have achieved restricted prominence in discussions on biodegradation and biotransformation, and include both photolithotrophs and chemolithotrophs. Some brief comments on both are therefore justiied. These organisms use CO2 as their principal, or exclusive, source of carbon, and this is incorporated into cellular material generally by the Benson–Calvin cycle. This is distinguished from heterotrophic organisms that may incorporate CO2 during degradation, for example, CO2 in the metabolism of epoxides by Xanthobacter sp. strain Py2, and of acetone by both aerobic and anaerobic bacteria. Energy for growth is obtained either from photochemical reactions (photolithotrophs), or by chemical oxidation of inorganic substrates such as reduced forms of nitrogen or sulfur (chemolithotrophs). In some organisms, organic carbon can be taken up and incorporated during growth even in organisms that are obligately chemolithotrophic or photolithotrophic. Organic carbon may, however, have an inhibitory effect on growth. Some species and strains of these organisms may also grow heterotrophically using organic carbon as sources of both energy and cell carbon. Attention is directed to reviews that cover the sometimes controversial aspects of lithotrophy and autotrophy (Kelly 1971; Rittenberg 1972; Whittenbury and Kelly 1977; Matin 1978). It is worth noting that many aerobic bacteria that belong to groups with well-established heterotrophic activity are also chemolithoautotrophic and use the oxidation of hydrogen as their source of energy (Bowien and Schlegel 1981). Attention is drawn to the reassignment of the Pseudomonas strains P. lava, P. pseudolava, and P. palleroni to the genus Hydrogenophaga, and the degradative activity of species of Xanthobacter. Attention has been directed to obligate lithotrophs such as those that oxidize carbon monoxide or hydrogen. Analysis of DNA extracts and PCR ampliication for the cbbL gene that encodes the large subunit of ribulose-1,5-bisophosphate carboxylase/oxygenase that is typically found in obligate lithotrophs was carried out. The PCR products were cloned, sequenced, and analyzed, and the results showed that populations depended on the plant cover and land use, although the relevant populations of ammonia-oxidizing organisms were small in comparison with those of facultative lithotrophs (Tolli and King 2005). Anaerobic lithotrophs that oxidize ammonium using nitrite as electron acceptor (anammox) are noted later in the section on anaerobic bacteria. It has become increasingly clear that representatives of chemolithotrophic microorganisms may be effective in carrying out the transformation of xenobiotics. As illustration, attention is directed to three groups of organisms: (1) the ammonia-oxidizers; (2) the thiobacilli; and (3) algae and cyanobacteria. Habitats to which these organisms are physiologically adapted should therefore be considered in discussions on biodegradation and biotransformation.

61

Biotic Reactions

Phototrophic Organisms The metabolic signiicance of oxygenic algae and cyanobacteria has received relatively limited attention in spite of the fact that they are important components of many ecosystems and may, for example, in the marine environment, be of primary signiicance. Whereas the heterotrophic growth of algae at the expense of simple carbohydrates, amino acids, lower aliphatic carboxylic acids, and simple polyols is well documented (Neilson and Lewin 1974), the potential of algae for the metabolism of xenobiotics has been much less extensively explored. Among these metabolic possibilities, which have received less attention than they deserve, the following are used as illustration: 1. The transformation—though not apparently the degradation—of naphthalene has been examined in cyanobacteria and microalgae, including representatives of green, red, and brown algae, and diatoms (Cerniglia et al. 1980a, 1982). The transformation of biphenyl (Cerniglia et al. 1980b), aniline (Cerniglia et al. 1981), and methylnaphthalenes (Cerniglia et al. 1983) has been examined in cyanobacteria (Figure 2.3). Phenanthrene is metabolized by Agmenellum quadruplicatum to the trans-9,10-dihydrodiol by a monooxygenase system, and the 1-hydroxyphenanthrene that was formed transiently was O-methylated (Narro et al. 1992). The biotransformation of benzo[a]pyrene has been demonstrated in a number of green algae, though this was not metabolized by a chlamydomonad, a chrysophyte, a euglenid, or a cyanobacterium (Warshawsky et al. 1995). The relative amounts of the products depended on the light sources and their intensity, and included 9,10-, 4,5-, 11,12-, and 7,8-dihydrodiols, the toxic 3,6-quinone, and phenols. The 11,12-, 7,8-, and 4,5-dihydrodiols produced by Selenastrum capricornutum had the cis coniguration, which suggests that their formation was mediated by a dioxygenase (Warshawsky et al. 1988). It is worth noting that Ochromonas danica is able to degrade phenol by extradiol ission of the initially formed catechol (Semple and Cain 1996). 2. Some green algae are able to use aromatic sulfonic acids (Figure 2.4a) (Soeder et al. 1987) and aliphatic sulfonic acids (Figure 2.4b) (Biedlingmeier and Schmidt 1983) as sources of sulfur. Cultures of Scenedesmus obliquus under conditions of sulfate limitation metabolized naphthalene-1-sulfonate to 1-hydroxy-naphthalene-2-sulfonate and the glucoside of naphth-1-ol (Kneifel et al. 1997). These results are consistent with formation of a 1,2-epoxide followed by an NIH shift. 3. The cyanobacteria Anabaena sp. strain PCC 7120 and Nostoc ellipsosporum dechlorinated γ-hexachloro[aaaeee]cyclohexane in the light in presence of nitrate to γ-pentachlorocyclohexene (Figure 2.5), and to a mixture of chlorobenzenes (Kuritz and Wolk 1995). The reaction is dependent on the functioning of the nir operon involved in nitrite reduction (Kuritz et al. 1997). OH

(a)

(b)

FIGURE 2.3 Examples of the biotransformation of aromatic compounds by algae.

OH

62

Environmental Degradation and Transformation of Organic Chemicals SO 3 H

(a)

(b) CH 3 −CH 2 −SO 3 H

CH 3 −(CH 2 )1 2 −CH

CO 2 CH 3 SO 3 H

FIGURE 2.4 Organosulfur compounds used as sources of sulfur by algae. Cl

Cl Cl

Cl Cl

Cl

Cl

Cl Cl

Cl

Cl

OH

Cl Cl Cl

HO

Cl

OH

Cl OH

Cl

Cl

Cl

Cl

Cl

Cl

FIGURE 2.5 Transformation of γ-hexachlorocyclohexane by cyanobacteria.

4. Representatives of the major groups of algae are able to use a range of amino acids as nitrogen sources (Neilson and Larsson 1980). 5. The transformation of DDT to DDE—albeit in rather low yield—by elimination of one molecule of HCl has been observed in several marine algae (Rice and Sikka 1973). There has been a revival of interest in the metabolic potential of anaerobic phototrophic bacteria, particularly, the purple nonsulfur organisms that can degrade aromatic compounds (Khanna et al. 1992). Such organisms are widely distributed in appropriate ecosystems, and may therefore play a signiicant role in the degradation of xenobiotics. Less appears to be known of the potential of other anaerobic phototrophs such as the purple and green sulfur bacteria to degrade xenobiotics. Dehalogenation of a number of halogenated alkanoic acids has been observed with Rhodospirillum rubrum, R. photometricum, and Rhodopseudomonas palustris. Substrates include 2- and 3-chloropropionic acid for all of these organisms, chloroacetate for R. photometricum, and 2-bromopropionate for R. rubrum and Rh. palustris (McGrath and Harfoot 1997). Fe(II) (Ehrenreich and Widdel 1994) and taurine (Novak et al. 2004) may serve as electron donors for the anaerobic phototrophic growth of purple nonsulfur bacteria. Aerobic and Facultatively Anaerobic Bacteria The well-established metabolic versatility of groups such as the pseudomonads and their numerous relatives, and the methanotrophs has possibly delected attention from other groups that may be present in aquatic systems and which may play an important role in determining the fate of xenobiotics. This is increasingly being rectiied with the isolation and description of new taxa. Although the potential of other Gram-negative groups including the pseudomonads, acinetobacters, moraxellas, and species of Alcaligenes is well established, Gram-positive groups seem to have

63

Biotic Reactions

achieved generally somewhat less prominence in aquatic systems. In the succeeding paragraphs, some examples of the metabolic importance of a few of these groups of organisms are presented. Gram-Positive Aerobic Bacteria The metabolic versatility of organisms belonging to the genera Mycobacterium and Rhodococcus is becoming well established. A taxonomic word of caution is appropriate in view of the historical importance of similar organisms that were designated as mycobacteria (Gray and Thornton 1928), although they were not acid-fast, and some at least would be currently assigned to the genus Rhodococcus. This illustrates a potentially serious taxonomic pitfall that should be avoided, since the distinction between the genera Mycobacterium and Rhodococcus has not always been unequivocal in the older literature (Finnerty 1992). Indeed, the organism that is discussed in Chapter 9, Part 2, and initially described as Rhodococcus chlorophenolicus has now been transferred to the genus Mycobacterium (Häggblom et al. 1994; Briglia et al. 1994). Conversely, an organism capable of degrading acetylene and assigned (DeBont et al. 1980) to the genus Mycobacterium almost certainly belongs to the genus Rhodococcus. There has been increasing interest in both mycobacteria and rhodococci. This has been sustained by the potential application of rhodococci in biotechnology (Finnerty 1992) since they have a broad metabolic potential. The analysis of fatty acids, mycolic acids, and diaminopimelic acid has been a valuable chemotaxonomic development, in addition to the use of sequencing. Mycobacteria Alkanes and Haloalkanes

Mycobacteria can oxidize short-chain alkenes (DeBont et al. 1980), and the organism known under the invalid speciic name “Mycobacterium parafinicum” (Wayne et al. 1991) was able to degrade a number of alkanes. It has also been shown that strains of mycobacteria grown with propane are able to oxidize the apparently unrelated substrate trichloroethene (Wackett et al. 1989). Strains of mycobacteria have been shown to degrade a range of halogenated alkenes. These include (a) vinyl chloride (Hartmans and de Bont 1992; Coleman and Spain 2003) and (b) Mycobacterium sp. strain GP1 that degrades 1,2-dibromoethane by a pathway that avoids the production of the toxic 2-bromoethanol and 2-bromoacetaldehyde by formation of the epoxide (Poelarends et al. 1999). Possibly, more remarkable is the metabolic capacity of species of mycobacteria including the human pathogen M. tuberculosis strain H37Rv (Jesenská et al. 2000). On the basis of amino acid and DNA sequences, the strain that was used contained three halohydrolases and the activity of the dehalogenase for debromination of 1,2-dibromoethane by other species of mycobacteria is given in Table 2.1. The haloalkane dehalogenase gene from M. avium has been cloned and partly characterized (Jesenská et al. 2002). PAHs

There has been a revival of interest in the role of mycobacteria in the degradation of polycyclic hydrocarbons including naphthalene (Kelley et al. 1990), phenanthrene (Guerin and Jones 1988), anthracene (van Herwijnen et al. 2003), and pyrene (Heitkamp et al. 1988; Grosser et al. 1991; TABLE 2.1 Specific Activity (µmol Bromide Produced per mg Protein per min) of Dehalogenase from Selected Species of Mycobacteria toward 1,2-dibromoethane Taxon M. bovis BCG MU10 M. fortuitum MU8 M. triviale MU3 M. smegmatis CCM4622

Activity

Taxon

Activity

99 76 61 49

M.avium MU1 M. phlei CCM 5639 M. parafortuitun MU2 M. chelonae

36 22 22 20

64

Environmental Degradation and Transformation of Organic Chemicals

TABLE 2.2 Degradation of PAHs by Mycobacteria Substrate Nap, Phe, Flu, 3-Me-Chol Phe, Pyr, Flu Pyr, BaPyr, BaAnth Nap, Anth, Phe, Flu, Pyr, BaAnth, BaPyr

Organism Mycobacterium sp. Mycobacterium sp. BB1 Mycobacterium sp. RJGII-135 Mycobacterium vanbaalenii PYR-1

Reference Heitkamp et al. (1988) Boldrin et al. (1993) Schneider et al. (1996) Kim et al. (2006)

Note: Bi, biphenyl; Nap, naphthalene; Phe, phenanthrene; Anth, anthracene; Flu, luoranthene; Pyr, pyrene; Chr, chrysene; BaAnth, benz[a]anthracene; BaPyr, benzo[a]pyrene; BbFlu, benzo[b]luoranthene; DBaAnth, dibenz[a,h]anthracene; 3-Me-Chol, 3-methylcholanthrene.

Krivobok et al. 2003) (Table 2.2). Both of the pyrene-degrading strains belong to the group of fastgrowing scotochromogenic mycobacteria (Govindaswami et al. 1995). A strain of Mycobacterium sp. that is able to use all these substrates as a sole source of carbon and energy has also been isolated (Boldrin et al. 1993). Halogenated Phenols

Considerable interest has been expressed in the chlorophenol-degrading organism Mycobacterium chlorophenolicum (R. chlorophenolicus) (Apajalahti et al. 1986), partly motivated by its potential for application to bioremediation of chlorophenol-contaminated industrial sites (Häggblom and Valo 1995). Nitroarenes

The pathway used by a strain of Mycobacterium sp. for the degradation of 4-nitrotoluene is initiated by reduction to the hydroxylamine and rearrangement to 3-hydroxy-4-aminotoluene before further degradation (Spiess et al. 1998). Morpholine

This can be degraded by several mycobacteria including Mycobacterium aurum strain MO1 (Combourieu et al. 1998), Mycobacterium strain RP1 (Poupin et al. 1998), and Mycobacterium chelonae (Swain et al. 1991). The reaction is initiated by a cytochrome P450 monooxygenase that is also active against pyrrolidine and piperidine (Poupin et al. 1998). Carbon Monoxide

The degradation of carbon monoxide has attracted recent attention, and a strain of mycobacterium is able to degrade this unusual substrate (Park et al. 2003). Rhodococci

Only a selection of examples is given below to illustrate the metabolic versatility of rhodococci, and further details are given in the appropriate sections of Chapters 7 through 11: 1. A strain of Rhodococcus sp. was capable of degrading a number of chlorinated aliphatic hydrocarbons including vinyl chloride and trichloroethene, as well as the aromatic hydrocarbons benzene, naphthalene, and biphenyl (Malachowsky et al. 1994). 2. A strain of Rhodococcus opacus isolated by enrichment with chlorobenzene was able to grow at the expense of a wide range of halogenated compounds. These included 1,3- and 1,4-dichlorobenzene, 1,3- and 1,4-dibromobenzene, 2-, 3-, and 4-luorophenol, 2-, 3-, and 4-chlorophenol, 4-nitrophenol, 3- and 4-luorobenzoate, and 3-chlorobenzoate (Zaitsev et al. 1995). 3. Several rhodococci have attracted interest for their ability to degrade PCBs including an organism (Acinetobacter sp. strain P6) now assigned to Rhodococcus globerulus (Asturias

Biotic Reactions

65

and Timmis 1993), R. erythropolis (Maeda et al. 1995), and Rhodococcus sp. strain RHA1 (Seto et al. 1995). 4. The degradation of 2,4,6-trichlorophenol by Rhodococcus percolatus (Briglia et al. 1996). 5. 2,4,6-Trinitrophenol is degraded in a reaction involving ring reduction by hydride transfer from an NADPH-dependent F420 reductase (Hofmann et al. 2004). 6. The degradation of cyclopropanecarboxylate by Rhodococcus rhodochrous (Toraya et al. 2004). 7. The degradation of isoprene by Rhodococcus sp. strain AD45 involves a glutathionemediated reaction (van Hylckama Vlieg et al. 2000) and is noted again in Chapter 7, Part 1. 8. A number of aliphatic ethers can be degraded by Rhodococcus sp. strain DEE 5151 (Kim and Engesser 2004). A number of biotransformations have been accomplished by rhodococci, including, for example, the hydrolysis of nitriles including polyacronitriles (Tauber et al. 2000), and the reduction of the conjugated C=C double bond in 2-nitro-1-phenylprop-1-ene (Sakai et al. 1985). Other Gram-Positive Organisms Gordonia

A review has summarized the taxonomic status of the genus Gordonia (Arenskötter et al. 2004), and drawn attention to important degradations carried out by species of the genus. These include benzothiophene by G. desulfuricans, dibenzothiophene by G. amicalis, 3-alkylpyridines by G. nitida, hexadecane by G. alkanivorans, 2,4-dinitrophenol by G. koreensis, and cis-1,4-polyisoprene by G. polyisoprenivorans (references in Braaz et al. 2004) that is noted in Chapter 3, Part 1 on dioxygenases. Actinomycetes

The role of cytochrome P450 oxygenations in actinomycetes has been reviewed (O’Keefe and Harder 1991) and, although these organisms have been exhaustively explored as the source of clinically valuable antibiotics, their degradative capability has been less extensively examined. It has been shown that they have a virtually ubiquitous occurrence in tropical and subtropical marine sediments (Mincer et al. 2002), and all of these have been assigned to two taxa Salinispora arenicola and S. tropica (Mincer et al. 2005). Their occurrence has been explored in the marine environment as possible sources of biologically active metabolites (Magarvey et al. 2004). Streptomyces

These have been examined for the degradation of a number of contaminants, and two pathways for the introduction of oxygen have been demonstrated: 1. Cytochrome P450 monooxygenation a. The transformation by Streptomyces griseus of benzene, toluene, naphthalene, biphenyl, and benzo[a]pyrene to the corresponding phenols has been observed (Trower et al. 1989). The oxidation of phenanthrene to (–)trans-[9S,10S]-9,10-dihydrodihydroxyphenanthrene by Streptomyces lavovirens with minor amounts of 9-hydroxyphenanthrene (Sutherland et al. 1990) is plausibly carried out by epoxidation and epoxide hydrolysis rather than by typical dioxygenation. b. The transformation of sulfonylureas by Streptomyces griseolus grown in a complex medium containing glucose when the methyl group of the heterocyclic moieties is hydroxylated and, for some substrates subsequently oxidized to the carboxylic acid (Romesser and O’Keefe 1986; O’Keefe et al. 1988).

66

Environmental Degradation and Transformation of Organic Chemicals

2. Dioxygenation a. The metabolism of aromatic substrates has been examined in Streptomyces setonii, and the degradation of vanillate involved in decarboxylation to guaiacol followed by intradiol ission of the catechol that was produced (Pometto et al. 1981). This strain could also metabolize cinnamate and related carboxylic acids (Sutherland et al. 1983), and strains of Amycolatopsis sp. and Streptomyces sp. were able to metabolize benzoate and salicylate that were degraded by dioxygenation (Grund et al. 1990). b. The degradation of 4-hydroxybenzoate and vanillate has been described for Streptomyces sp. strain 2065, and the pathway involving intradiol dioxygenation of the initially formed 3,4-dihydroxybenzoate has been characterized (Iwagami et al. 2000). c. The degradation of 2,4,6-trichlorophenol has been described for Streptomyces rochei strain 303, and the dioxygenase that brings about intradiol ission of the initially formed 2,6-dichlorohydroquinone has been characterized (Zaborina et al. 1995). d. The degradation of cis-poly-1,4-isoprene has been examined in Streptomyces coelicolor 1A, and a number of oxidation products identiied (Bode et al. 2000). These were produced by oxidations of the subterminal double bonds followed by β-oxidation, hydroxylation, oxidation, and ission of the 3-ketoacids. Gram-Positive Facultatively Anaerobic Organisms The genus Staphylococcus is traditionally associated with disease in humans. The demonstration (Monna et al. 1993) that a strain of Staphylococcus auriculans—isolated by enrichment with dibenzofuran and with no obvious clinical association—could degrade this substrate and carry out limited biotransformation of luorene and dibenzo[1,4]dioxin serves to illustrate the unsuspected metabolic potential of facultatively anaerobic Gram-positive organisms. A satisfying evaluation of the metabolic potential of microorganisms in natural ecosystems should not therefore fail to consider all these organisms, which are certainly widespread, and to distinguish between rates of degradation and metabolic potential: slow-growing organisms may be extremely important in degrading xenobiotics in natural ecosystems. Gram-Negative Aerobic Bacteria A taxonomic note: there have been substantial developments in the taxonomy of pseudomonads, and many new genera have been proposed including, for example, Sphingomonas, Comamonas, and Variovorax, while denitrifying organisms described as pseudomonads have been referred to the general Thauera and Azoarcus (Anders et al. 1995). Attention is briely drawn to groups that are not only widely distributed, but which have also previously attracted attention primarily in the context of nitrogen ixation. 1. Azotobacters. Burk and Winogradsky in the 1930s showed that these could readily be obtained from soil samples by elective enrichment with benzoate. The degradative pathway for benzoate has been elucidated (Hardisson et al. 1969), and the range of substrates extended to 2,4,6-trichlorophenol (Li et al. 1992; Latus et al. 1995). The enzyme from Azotobacter sp. strain GP1 that catalyzes the formation of 2,6-dichlorohydroquinone from 2,4,6-trichlorophenol is a monooxygenase that requires NADH, FAD, and O2 (Wieser et al. 1997) and, in the absence of a substrate, results in unproductive formation of H2O2. It is also able to accept other chlorophenols with the consumption of NADH including 2,4-, 2,6-, 3,4-dichloro-, 2,4,5-trichloro-, and 2,3,4,5- and 2,3,4,6-tetrachlorophenol. 2. Rhizobia. Taxa belonging to both the genera Rhizobium and Bradyrhizobium are capable of degrading simple aromatic compounds including benzoate (Chen et al. 1984) and 4-hydroxybenzoate (Parke and Ornston 1986; Parke et al. 1991). It has been shown that 4-hydroxybenzoate hydroxylase is required for the transport of 4-hydroxybenzoate into the cell (Wong et al. 1994). In strains of Rhizobium trifolium, the metabolism of benzoate involves either 3,4-dihydroxybenzoate (protocatechuate) 3,4-dioxygenase (Chen et al. 1984), or catechol

67

Biotic Reactions

TABLE 2.3 The Major Genera within the Former Genus Sphingomonas and Their Role in Degradation Genus Sphingobium

Novosphingobium Sphingopyxis

Species herbicidovorans chlorophenolicus yanoikuyae indicum japonicum francense aromaticivorans subarctica macrogolitabida

Degradation Dichlorophenoxypropionate Chlorophenols Aromatic hydrocarbons Hexachlorocyclohexanes Hexachlorocyclohexanes Hexachlorocyclohexanes Aromatic hydrocarbons Chlorophenols Polyethylene glycol

1,2-dioxygenase (Chen et al. 1985). The degradation of the toxic N-alkylpyrid-4-one mimosine by Rhizobium sp. strain TAL1145 has been described (Awaya et al. 2005). Rhizobia have quite a broad degradative capability that is illustrated by the following examples: a. PCB congeners (Damaj and Ahmad 1996) b. Flavones (Rao et al. 1991; Rao and Cooper 1994) c. Dechlorination—though not the degradation—of atrazine (Bouquard et al. 1997) d. Phosphonomycin (1,2-epoxypropylphosphonate) as a source of carbon, energy, and phosphorus (McGrath et al. 1998) 3. Many organisms with degradative capability have been assigned to species in the genus Sphingomonas. These include the degradation of chlorophenols, aromatic hydrocarbons, 6-aminonaphthalene-2-sulfonate, and nonylphenol. The description of the genus Sphingomonas has been revised, and separated into three genera, Sphingobium, Novosphingobium, and Sphingopyxis (Table 2.3) (Takeuchi et al. 2001). Important assignments to these new genera include a number of degradations, and a strain of Novosphingobium sp. represented the dominant organisms that degraded chlorophenols in a groundwater remediation system (Tiirola et al. 2002). Gram-Negative Facultatively Anaerobic Bacteria Enterobacteriaceae

Although facultatively anaerobic bacteria and especially those belonging to the family Enterobacteriaceae have a long history as the agents of disease in man, there is increasing evidence for their importance in a wide range of environmental samples. Methods for their identiication and classiication have been extensively developed and have traditionally used the ability to ferment a wide range of carbohydrates as taxonomic characters. This has had the possibly unfortunate effect of delecting attention from the capability of these organisms to degrade other classes of substrates. Their ability to utilize, for example, 3- and 4-hydroxybenzoates (Véron and Le Minor 1975), and nicotinate (Grimont et al. 1977) under aerobic conditions has, however, been quite extensively used for taxonomic classiication. Some examples used to illustrate the metabolic capabilities of these somewhat neglected organisms that include species of the genera Citrobacter, Enterobacter, Hafnia, Klebsiella, Salmonella, and Serratia, as well as more recently described genera, are given below: 1. The degradation of DDT by organisms designated Aerobacter aerogenes (possibly Klebsiella aerogenes) (Wedemeyer 1967) (Figure 2.6), and the partial reductive dechlorination of methoxychlor by K. pneumoniae (Baarschers et al. 1982). 2. The biotransformation of methyl phenyl phosphonate to benzene by K. pneumoniae (Cook et al. 1979) (Figure 2.7a). Further examples of the cleavage of the carbon–phosphorus

68

Environmental Degradation and Transformation of Organic Chemicals CCl3

Cl

CHCl2 Cl

CH

Cl

CCl2

CH

Cl

Cl

C

Cl

FIGURE 2.6 Degradation of DDT by Aerobacter aerogenes. Cl

PO−OMe

Cl

Cl

Cl

Cl

Cl

Cl

Cl

(b)

(a)

Cl

Cl

CO 2 H CN

CO 2 H (d)

(c) Br

Br OH

Br

Br OH

OMe OH

OMe OH

FIGURE 2.7 Transformation of (a) methylphenyl phosphonate, (b) γ-hexachlorocyclohexane, (c) 3,5-dibromo4-hydroxybenzonitrile, and (d) decarboxylation.

3. 4. 5. 6.

7.

8. 9. 10.

bond by other members of the Enterobacteriaceae, and a discussion of the metabolism of phosphonates is given in Chapter 11, Part 4. The biotransformation of 2,4,6-trihydroxy-1,3,5-triazine and atrazine under anaerobic conditions by an unidentiied facultative anaerobe (Jessee et al. 1983). The biotransformation of γ-hexachloro[aaaeee]cyclohexane to tetrachlorocyclohexene by Citrobacter freundii (Figure 2.7b) (Jagnow et al. 1977). The biotransformation of 3,5-dibromo-4-hydroxybenzonitrile to the corresponding acid by a strain of K. pneumoniae ssp. ozaenae which uses the substrate as sole source of nitrogen (Figure 2.7c) (McBride et al. 1986). The decarboxylation of 4-hydroxycinnamic acid to 4-hydroxystyrene, and of ferulic acid (3-methoxy-4-hydroxycinnamic acid) to 4-vinylguaiacol by several strains of Hafnia alvei and H. protea, and by single strains of Enterobacter cloacae and K. aerogenes (Figure 2.7d) (Lindsay and Priest 1975). The decarboxylase has been puriied from Bacillus pumilis (Degrassi et al. 1995). Several taxa of Enterobacteriaceae including Morganella morganii, Proteus vulgaris, and Raoultella (Klebsiella) planticola are able to decarboxylate the amino acid histidine, which is abundant in the muscle tissue of scombroid ish (Yoshinaga and Frank 1982; Takahashi et al. 2003). The histamine produced has been associated with an incident of scombroid ish poisoning (Taylor et al. 1989). The metabolism of ferulic acid (3-methoxy-4-hydroxycinnamic acid) by Ent. cloacae to a number of products including phenylpropionate and benzoate (Figure 2.8) (Grbic-Galic 1986). Utilization of uric acid as a nitrogen source by strains of Aer. aerogenes, K. pneumoniae, and Serratia kiliensis (Rouf and Lomprey 1968). The sequential reduction of one of the nitro groups of 2,6-dinitrotoluene by Salmonella typhimurium (Sayama et al. 1992)—a taxon that is not generally noted for its metabolic activity.

69

Biotic Reactions CO 2 H CH2−CH2−CO2H

CO 2 H

+ OMe OH

FIGURE 2.8

Metabolism of ferulic acid by Enterobacter cloacae.

11. Under conditions of oxygen limitation, strains of Morganella morganii and Providencia rettgeri degraded hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) after initial reduction to the nitroso compounds (Kitts et al. 1994). 12. After growth in a medium containing suitable reductants such as glucose, a strain of Enterobacter agglomerans was able to reduce tetrachloroethene successively to trichloroethene and cis-1,2- dichloroethene (Sharma and McCarty 1996). 13. Degradation of pentaerythritol tetranitrate by Ent. cloacae (French et al. 1996) and of glyceryltrinitrate by K. oxytoca (Marshall & White 2001). 14. Degradation by Enterobacter sp. of chlorpyrifos with the formation of 3,5,6-pyridin-2-one and diethylthiophosphate that was used for growth and energy (Singh et al. 2004). 15. Degradation of naphthalene, luoranthene, and pyrene by Leclercia adecarboxylata that has hitherto been of clinical origin (Sarma et al. 2004). 16. RDX and its partial reduction product hexahydro-1-nitroso-3,5-dinitro-1,3,5-triazine were degraded by K. pneumoniae to methylenedinitramine, and then to CH2O and methanol, while abiotic reactions produced N2O (Zhao et al. 2002). 17. The taxonomic application of the ability of enteric organisms to grow with 4-hydroxyphenylacetate (Cooper and Skinner 1980) and 3-hydroxyphenylpropionic acid (Burlingame and Chapman 1983) has been established. In addition, it has been demonstrated that the enzyme that carries out the hydroxylation has a wide substrate range extending to 4-methylphenol, and even to 4-chlorophenol (Prieto and Garcis 1994). Vibrionaceae

Only a few examples have emerged of the degradative capability of these organisms, and include the following: a. An organism, tentatively identiied as a strain of Vibrio sp., was able to degrade the 2-carboxylates of furan, pyrrole, and thiophene (Evans and Venables 1990). b. A strain of Aeromonas sp. was able to degrade phenanthrene through o-phthalate (Kiyohara et al. 1976).

BACTERIAL METABOLISM OF C1 COMPOUNDS: METHANOTROPHS, METHYLOTROPHS, AND RELATED ORGANISMS Methane Monooxygenase and Related Systems A few of the reactions carried out by the monooxygenase system of methanotrophic bacteria are summarized in Figure 2.9, and it is on account of this that methylotrophs have received attention for their technological potential (Lidstrom and Stirling 1990). An equally wide metabolic potential has also been demonstrated for cyclohexane monooxygenase, which has been shown to accomplish two broad types of reaction: one in which formally nucleophilic oxygen reacts with the substrate, and

70

Environmental Degradation and Transformation of Organic Chemicals

CH 3 −Br

O

CH 3 (CH 2 )6 −CH 2OH

CH3(CH2)6−CH3

CH 3 (CH 2 )5 −CH(OH)CH 3

;

CH 2 O

;

CH 3 −CH

CH 3 CH 2 −O−CH 2 CH 3

CH 2

CH 3 −CH

CH 2

CH 3CH 2 OH

OH

; N

N

CH 3

O

CH 2OH

CH 3

CO 2H

OH

FIGURE 2.9

Reactions mediated by the monooxygenase system of methanotrophic bacteria.

CH2−O−CO−CH3

CH 2 −CO−CH 3

S

O

FIGURE 2.10

S

S O

O

Reactions mediated by cyclohexane monooxygenase.

the other in which formally electrophilic oxygen is involved (Figure 2.10) (Branchaud and Walsh 1985). In addition, it has emerged that the monooxygenase system in methanotrophs is similar to that in the nitrite-oxidizing bacteria, and that the spectrum of biotransformations is equally wide. There are also important groups of facultatively C1-utilizing bacteria: (a) members of the genus Xanthobacter (Padden et al. 1997), and (b) Methylocella silvestris that was isolated from tundra soils and had the unusual capacity to use not only methane and methanol as energy sources, but also C2 and C3 substrates such as acetate and malate (Dedysh et al. 2005). The following illustrate some of the biotransformations that have been observed with Nitrosomonas europaea. These are particularly interesting since this organism has an obligate

71

Biotic Reactions OH

OH

(a)

OH

HO 2 C

N

Cl

Cl2 CH

N

Cl

(b) Cl3 C

FIGURE 2.11

N

Cl

Metabolism by Nitrosomonas europaea (a) benzene, (b) 2-chloro-6-trichloromethylpyridine.

dependency on CO2 as carbon source, and has traditionally been considered to be extremely limited in its ability to use organic carbon for growth or transformation: 1. The oxidation of benzene to phenol and 1,4-dihydroxybenzene (Figure 2.11a) (Hyman et al. 1985), both side chain and ring oxidation of ethyl benzene, and ring-hydroxylation of halogenated benzenes and nitrobenzene (Keener and Arp 1994). 2. The oxidation of alkanes (C1–C8) to alkanols, and alkenes (C2–C5) to epoxides (Hyman et al. 1988). 3. The oxidation of methyl luoride to formaldehyde (Hyman et al. 1994), and of chloroalkanes at carbon atoms substituted with a single chlorine atom to the corresponding aldehyde (Rasche et al. 1991). 4. The oxidation of a number of chloroalkanes and chloroalkenes including dichloromethane, chloroform, 1,1,2-trichloroethane, and 1,2,2-trichloroethene (Vannelli et al. 1990). Although the rate of cometabolism of trihalomethanes increased with levels of bromine substitution so also did toxicity. Both factors must therefore be evaluated in the possible application of this strain (Wahman et al. 2005). 5. The oxidation of the trichloromethyl group in 2-chloro-6-trichloromethylpyridine to the corresponding carboxylic acid occurs at high oxygen concentrations during cooxidation of ammonia or hydrazine. At low oxygen concentrations, however, in the presence of hydrazine, reductive dechlorination to 2-chloro-6-dichloromethylpyridine occurs (Vannelli and Hooper 1992) (Figure 2.11b). 6. A range of sulides including methylsulide, tetrahydrothiophene, and phenylmethylsulide are oxidized to the corresponding sulfoxides (Juliette et al. 1993). As for methanotrophic bacteria, such transformations are probably conined neither to a single organism nor to strains of speciic taxa within the group. For example, both Nitrosococcus oceanus and Nitrosomonas europaea are able to oxidize methane to CO2 (Jones and Morita 1983; Ward 1987). The versatility of this group of organisms clearly motivates a reassessment of their ecological signiicance particularly in the marine environment where they are widely distributed. The overall similarity of these transformations to those carried out by eukaryotic cytochrome P450 systems (Guengerich 1990) is striking.

72

Environmental Degradation and Transformation of Organic Chemicals

ANAEROBIC BACTERIA There are a number of reasons for the increased interest in transformations carried out by anaerobic bacteria: a. After discharge into the aquatic environment, many xenobiotics are partitioned from the aquatic phase into the sediment phase. b. Sediments in the vicinity of industrial discharge often contain readily degraded organic matter, and the activity of aerobic and facultatively anaerobic bacteria then renders these sediments effectively anaerobic. The fate of xenobiotics in many environments is therefore signiicantly determined by the degradative activity of anaerobic bacteria. The terms anaerobic and anoxic are purely operational, and imply merely the absence of air or oxygen, and the absolute distinction between aerobic and anaerobic organisms is becoming increasingly blurred. The problem of deining anaerobic bacteria may therefore best be left to philosophers. Possibly, the critical issue is the degree to which low concentrations of oxygen are either necessary for growth or toxic. During the growth of bacteria in the absence of externally added electron acceptors, the term fermentation implies that a redox balance is achieved between the substrate (which may include CO2) and its metabolites. A few following examples are given to illustrate the apparently conlicting situations that may be encountered, and the gradients of response that may be elicited: 1. Although strictly anaerobic bacteria do not generally grow in the presence of high-potential electron acceptors such as oxygen or nitrate, an intriguing exception is provided by an obligately anaerobic organism that uses nitrate as electron acceptor during the degradation of resorcinol (Gorny et al. 1992). This isolation draws attention to the unknown extent to which such organisms exist in natural systems, since strictly anaerobic conditions are not always used for the isolation of organisms using nitrate as electron acceptor. Other formally similar organisms are either facultatively anaerobic or have a fermentative metabolism. In contrast, the normally strictly anaerobic sulfate-reducing organisms Desulfobulbus propionicus and Desulfovibrio desulfuricans may grow by reducing nitrate or nitrite to ammonia using hydrogen as electron donor (Seitz and Cypionka 1986). Desulfovibrio vulgaris Hildeborough is capable of growing at oxygen concentrations of 0.24–0.48 µM, and indeed it was suggested that this organism might protect anoxic environments from adverse effects resulting from intrusion of oxygen (Johnson et al. 1997). In the presence of nitrate, the acetogen Clostridium thermoaceticum oxidizes the O-methyl groups of vanillin or vanillate to CO2 without production of acetate, which is usually formed in the absence of nitrate (Seifritz et al. 1993). 2. Some anaerobic organisms such as clostridia are appreciably tolerant of exposure to oxygen, whereas others such as Wolinella succinogenes that have hitherto been classiied as anaerobes are in fact microaerophilic (Han et al. 1991). However, organisms such as Nitrosomonas europaea that normally obtain energy for growth by the oxidation of ammonia to nitrite, may apparently bring about denitriication of nitrite under conditions of oxygen stress (Poth and Focht 1985), or under anaerobic conditions in the presence of pyruvate (Abeliovich and Vonshak 1992). 3. It is important to note the existence of microaerotolerant or microaerophilic organisms. The example of W. succinogenes has already been noted, and another is provided by Malonomonas rubra that uses malonate as sole source of carbon and energy (Dehning and Schink 1989a). On the other hand, Propionigenium modestum that obtains its energy by the decarboxylation of succinate to propionate is a strictly anaerobic organism (Schink and Pfennig 1982).

Biotic Reactions

73

Attention is directed to two groups of anaerobic bacteria that display metabolic versatility toward structurally diverse substrates—clostridia and anaerobic sulfate reducers. Clostridia The classical studies on the anaerobic metabolism of amino acids, purines, and pyrimidines by clostridia not only set out the relevant experimental procedures and thereby laid the foundations for virtually all future investigations, but also brought to light the importance and range of coenzyme B12mediated rearrangements. These reactions were mainly carried out by species of clostridia and indeed some of these degradations belong to the classical age of microbiology in Delft (Liebert 1909). The number of different clostridia investigated may be gained from the following selected examples: 1. a. The classic purine-fermenting organisms Clostridium acidurici and Cl. cylindrosporum ferment several purines including uric acid, xanthine, and guanine. b. The degradation of pyrimidines such as orotic acid is accomplished by Cl. oroticum. 2. A large number of clostridia including Cl. perfringens, Cl. saccharobutyricum, Cl. propionicum, Cl. tetani, Cl. sporogenes, and Cl. tetanomorphum ferment a range of single amino acids, while some participate in the Stickland reaction involving two amino acids. 3. Several clostridia including Cl. tyrobutyricum, Cl. thermoaceticum, and Cl. kluyveri are able to reduce the double bond of α,β-unsaturated aldehydes, ketones, and coenzyme A thioesters (Rohdish et al. 2001), and are noted in Chapter 3, Part 3. Anaerobic Sulfate-Reducing Bacteria The spectrum of compounds degraded by anaerobic sulfate-reducing bacteria is continuously widening. It now includes, for example, alkanes (Aeckersberg et al. 1991, 1998), alkanols, alkylamines, and alkanoic acids, nicotinic acid (Imhoff-Stuckle and Pfennig 1983), indoles (Bak and Widdel 1986), methoxybenzoates (Tasaki et al. 1991), benzoate, hydroxybenzoate and phenol (Drzyzga et al. 1993), and catechol (Szewzyk and Pfennig 1987). Further details of the pathways are provided in Chapter 7, Part 1 and Chapter 8, Part 3. It should also be noted that elementary sulfur (S0) may serve as oxidant for organisms belonging to a number of genera including Desulfomicrobium, Desulfurella, Desulfuromonas, and Desulfuromusa (references in Liesack and Finster 1994). The anaerobic oxidation of propionate may be accomplished in pure cultures of Syntrophobacter wolinii and S. pfennigi at the expense of sulfate reduction (Wallrabenstein et al. 1995). Other Anaerobic Bacteria It is appropriate to mention briely some additional reactions that are brought about by anaerobic bacteria: 1. Compounds such as oxalate (Dehning and Schink 1989b) and malonate (Dehning et al. 1989; Janssen and Harfoot 1992) are degraded by decarboxylation with only a modest energy contribution. They are nevertheless able to support the growth of the appropriate organisms. The bioenergetics of the anaerobic Oxalobacter formigenes (Anantharam et al. 1989) and the microaerophilic Malonomonas rubra have been elucidated (Hilbi et al. 1993; Dimroth and Hilbi 1997). 2. Particularly extensive effort has been directed to the anaerobic dechlorination of alkenes and halogenated phenols that are discussed in Chapter 7, Part 3 and Chapter 9, Part 2. As a result of this, the range of organisms that are able to carry this out is considerable and includes a. A sulfate-reducing organism Desulfomonile tiedjei (DeWeerd et al. 1990). b. A sulite-reducing organism Desulitobacterium dehalogenans (Utkin et al. 1994).

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c. Desulitobacterium metallireducens that can use tetrachloroethene and trichlororethene as electron acceptors during growth with lactate (Finneran et al. 2002). d. The chlororespiring Anaeromyxobacter dehalogens that can use a few 2-chlorinated phenols as electron acceptors (Sanford et al. 2002), and in addition Fe(III) (He and Sanford 2003). e. Sulfurospirillum (Dehalospirillum) multivorans that accomplishes the sequential reduction of tetrachloroethene to trichloroethene and cis-1,2-dichloroethene (Neumann et al. 1994). 3. Although they have not been obtained in pure culture, chemolithotrophic anaerobic bacteria (anammox) that oxidize ammonia using nitrite as electron donor and CO2 as a source of carbon have been described. In addition, they can oxidize propionate to CO2 (Güven et al. 2005) by a pathway that has not yet been resolved. 4. Important groups of organisms belonging to the genus Geobacter are widely distributed in sediments. They are able to couple the reduction of Fe(III) to the oxidation of low molecularweight organic carboxylic acids (Coates et al. 1996), and some are able to use the humic acid model anthraquinone 2,6-disulfonate as electron acceptor. In addition to acetate and benzoate, G. metallireducens and G. grbiciae are able to use toluene as an electron donor with anthraquinone 2,6-disulfonate as an electron acceptor (Coates et al. 2001). These organisms are of considerable ecological importance since some of them are able to use humic acid as an electron acceptor. Further comments are given in Chapter 3, Part 3.

ORGANISMS FROM EXTREME ENVIRONMENTS Increasing numbers of bacteria have been isolated that are able to grow not only under high temperatures but also extremes of pH and salinity. There has been considerable interest in thermophiles as sources of enzymes, and, with increasing accessibility, studies in microorganisms from the high arctic from which signiicant features have emerged. Psychrophiles 1. Soil samples from a putatively contaminated site on Ellesmere Island (82°N, 62°W) contained bacteria belonging to the genera Pseudomonas and Sphingomonas that were psychrotolerant. They belonged to two mutually exclusive groups, one able to grow with abietanes and n-dodecane and the other with pimaranes, benzoate, and toluene. Bacteria that are able to degrade resin acids were not found in pristine tundra soils, and the isolation of the resin acid–degrading bacteria presented a conundrum (Yu et al. 2000). 2. Bacteria in thawed ice samples from Ellesmere Island (79°38′N, 74°23′W) produced CO2 and CH4 during extended incubation at 4°C in a diluted complex medium (yeast extract, casamino acids, starch, and glucose) (Skidmore et al. 2000). It was suggested that the results demonstrated that the subglacial environment beneath a polythermal glacier provided an acceptable habitat for microbial life. 3. Two different investigations have been directed to a glacial ice core (GISP2) from Greenland: a. Anomalous concentrations of methane at 2954 and 3036 m were associated with the activity of methanogens which were characterized by the luorescence of the F420 coenzyme (Tung et al. 2005). b. Thawed samples were treated by selective iltration for ultrasmall microorganisms, followed by plating and anaerobic incubation, or by cycles of iltration and enrichment for 2–8 months at –2 or +5°C in media containing low concentrations of formate or acetate. Isolates were characterized by 16S rRNA sequencing (Miteva and Brenchley 2005). A number of important conclusions could be drawn: (i) iltration increased the number of colonies that were obtained; (ii) the combination of iltration and cultivation increased

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both the number of colonies and their diversity; and (iii) spore-forming organisms were among the isolates. Thermophiles There has been increased interest in hyperthermophiles for application to biotechnology and bioremediation. The hyperthermophilic archaeon Pyrococcus furiosus is an anaerobe that grows at temperatures up to 105°C and has a requirement for tungsten that is discussed in Chapter 3, Part 5. This organism contains several tungsten-containing ferredoxin oxidoreductases—for aldehydes, glyceraldehyde-3-phosphate, and formaldehyde (Mukund and Adams 1991, 1993, 1995; Roy et al. 1999). In addition, glutamate dehydrogenase from Pyr. furiosus is inactive below 40°C, and is able to use both NAD+ and NADP + as cofactors (Klump et al. 1992). Fe(III) reductases have been described from Pyrobaculum islandicum (Childers and Lovley 2001), and from the hyperthermophilic sulfate-reducing Archaeoglobus fulgidus (Vadas et al. 1999). Illustrative examples of their biotechnological applications using metagenomes include the following: 1. A gene (erstE1) encoding a thermostable esterase was isolated from Escherichia coli cells that had been transformed by DNA libraries with metagenomes from environmental samples isolated from thermal habitats. The enzyme belonged to the hormone-sensitive lipase family, could be overexpressed in E. coli, was active between 30 and 95°C, and used 4-nitrophenyl esters with chain lengths of C4 –C16 (Rhee et al. 2005). 2. A metagenome was isolated from soil samples, a library was constructed, and was screened for amylase activity. The amlyase gene (amyM) was overexpressed and puriied. Its properties suggested that it could be regarded as a type of maltogenic amylase, α-amylase, and 4-α-glucanotransferase (Yun et al. 2004). Alkaliphiles There has been increasing interest in these on account of their potential for the synthesis of valuable enzymes that include alkaline proteases and those that degrade starch and cellulose. Strains of Bacillus sp. have been most extensively examined (Horikoshi 1999). Halophiles The organisms in a high-salinity evaporation pond were examined by plating on solid media and prolonged incubation, and by analysis of a library of PCR-ampliied 16S rRNA genes (Burns et al. 2004). The isolates were related to species of several genera including Haloferax, Halorubrum, and Natromonas. The irst of these was not, however, represented in the gene library, and it was suggested that this could be due to its ability to form colonies even though it was not a dominant group. A major group identiied in the library was the SHOW square organisms that have so far deied cultivation.

EUKARYOTIC MICROORGANISMS: FUNGI AND YEASTS Metabolism by Fungi Although the cardinal importance of fungi in the terrestrial environment is unquestioned, and some examples of the synthesis of organohalogen metabolites are given in Chapter 3, Part 1, most attention in the aquatic environment has been directed to bacteria. An important exception is provided by studies in Lake Bonney, South Australia. The microlora of the lake contained a population of fungi including Trichoderma herzianum that was able to degrade the “free” but not the associated chloroguaiacols (van Leeuwen et al. 1997). In addition, Epicoccum sp., Mucor circinelloides, and

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Penicillium expansum—which are widely distributed soil fungi and may have entered the lake from run-off—were capable of bringing about association of tetrachloroguaiacol with organic components in the aqueous phase, so that this material could subsequently enter the sediment phase (van Leeuwen et al. 1997). On account of the similarity of the metabolic systems of fungi to those of mammalian systems, it has been suggested that fungi could be used as models for screening purposes. Several relevant examples have been provided (Ferris et al. 1976; Smith and Rosazza 1983; Grifiths et al. 1992), and the fungus Cunninghamella elegans has attracted particular attention. The reactions involved in the transformation of alachlor by this organism (Pothuluri et al. 1993) are similar to those encountered in other organisms: (a) mammalian systems, (b) the biotransformation of the analogous metalochlor by bluegill sunish (Lepomis macrochirus), and (c) that carried out by a soil actinomycete, which is noted later in this chapter. A wide range of taxonomically diverse fungi has also been used for the synthesis of less readily available compounds including hydroxylated steroids (Chapter 7, Part 2). Fungi—especially white-rot and brown-rot —have attracted considerable attention in the context of bioremediation of contaminated terrestrial sites, and examples are given in Chapter 14. In the terrestrial environment—and possibly also in a few specialized aquatic ecosystems— fungi and yeasts play a cardinal role in biodegradation and biotransformation. The role of yeasts in the coastal marine environment is illustrated by results of their frequency and their potential for transformation of phenanthrene and benz[a]anthracene (MacGillivray and Shiaris 1993). The transformation of PAHs by certain fungi is analogous to that in mammalian systems so that fungal metabolism has been explored as a model for higher organisms, and extensive studies have been carried out, particularly with Cunninghamella elegans. It has been suggested that the transformations accomplished by the brown-rot fungus Gleophyllum striatum may involve hydroxyl radicals, and this is supported by the overall similarity in the structures of the fungal metabolites with those produced with Fenton’s reagent (Wetzstein et al. 1997). Biotransformation (hydroxylation) of a wide range of PAHs and related compounds including biphenyl, naphthalene, anthracene, phenanthrene, 4-, and 7-methylbenz[a]anthracene, and 7, 12-dimethylbenz[a]anthracene has been examined in a number of fungi, most extensively in species of Cunninghamella, especially C. elegans (McMillan et al. 1987). Hydroxylation of benzimidazole (Seigle-Murandi et al. 1986) by Absidia spinosa, and of biphenyl ether by C. echinulata (SeigleMurandi et al. 1991) has also been studied on account of the industrial interest in the metabolites. The biotransformation of alachlor (2-chloro-N-methoxymethyl-N-[2,6-diethylphenyl]acetamide) by C. elegans has already been mentioned, and involves primarily hydroxylation at the benzylic carbon atom and loss of the methoxymethyl group (Pothuluri et al. 1993). In all these examples, the reactions are correctly described as biotransformations since the aromatic rings of these compounds remain unaltered. Particular attention has been focused on the white-rot fungus Phanerochaete chrysosporium on account of its ability to degrade not only lignin but also to metabolize a wide range of unrelated compounds. These include PAHs (Bumpus 1989) and organochlorine compounds including DDT (Bumpus and Aust 1987), PCBs (Eaton 1985), lindane and chlordane (Kennedy et al. 1990), pentachlorophenol (Mileski et al. 1988), and 2,7-dichlorobenzo[1,4]dioxin (Valli et al. 1992b). The novel pathways for the degradation of 2,4-dichlorophenol (Valli and Gold 1991) (Chapter 9, Part 2) and 2,4-dinitrotoluene (Valli et al. 1992a) (Chapter 9, Part 5) are worth noting. The degradation of all these compounds is apparently mediated by two peroxidase systems—lignin peroxidases and manganese-dependent peroxidases—and a laccase that is produced by several white-rot fungi, though not by P. chrysosporium. A potentially serious interpretative ambiguity has, however, emerged from the observation that lignin peroxidase is able to polymerize a range of putative aromatic precursors to lignin, but that this is not the functional enzyme in the depolymerization of lignin (Sarkanen et al. 1991). The regulation of the synthesis of these oxidative enzymes is complex, and is inluenced by nitrogen limitation, the growth status of the cells, and the concentration of manganese in the medium (Perez and Jeffries 1990). In addition, it seems clear that monooxygenase and epoxide

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hydrolase activities are also involved since the biotransformation of phenanthrene takes place even in the absence of peroxidase systems (Sutherland et al. 1991). P. chrysosporium is able to degrade anthracene by oxidation to anthra-9,10-quinone, followed by ring ission to produce o-phthalate. Phanerochaete chrysosporium, which is able to degrade simultaneously chlorobenzene and toluene (Yadav et al. 1995) has achieved some importance in the context of bioremediation since the bacterial degradation of these substrates is generally restricted by the incompatibility of the degradative pathways. Clearly therefore, a number of important unresolved issues remain. In addition, attention is drawn to the role of fungal redox systems in the covalent linking of xenobiotics to aromatic components of humus in soils. The metabolic activity of other white-rot fungi including Phanerochaete chrysosporium and Pleurotus ostreacus has been discussed in the context of polycyclic aromatic hydrocarbons. For example, the mineralization potential of the manganese peroxide system from Nematoloma frowardii for a number of substrates has been demonstrated (Hofrichter et al. 1998): the formation of CO2 from labeled substrates ranged from 7% (pyrene) to 36% (pentachlorophenol), 42% (2-amino-4, 6-dinitrotoluene), and 49% (catechol). Several strains of white-rot fungi have been examined for their ability to degrade and mineralize selected PCB congeners (Beaudette et al. 1998). Mineralization of 2,4′,5 [U-14C]trichlorobiphenyl as a fraction of the substrate added ranged from ca. 4.2% for a strain of Pleurotus ostreacus, 4.9 and 6.9% for two strains of Bjerkandera adusta, to 11% for a strain of Trametes versicolor, whereas Phanerochaete chrysosporium produced only ca. 2% of 14CO2. There was no apparent correlation among levels of lignin peroxidase, manganese peroxidase, and degradative ability. The degradation of phenolic compounds by fungi may involve rather unusual features of which the following three are given as illustration: 1. Aspergillus fumigatus degrades phenol using simultaneously two pathways: irst, orthohydroxylation to catechol followed by ring cleavage to 3-ketoadipate, and second, successive hydroxylation to hydroquinone and 1,2,4-trihydroxybenzene before ring cleavage (Jones et al. 1995). The metabolism of 2-aminobenzoate (anthranilate) to 2,3-dihydroxybenzoate by A. niger is accomplished by apparent incorporation of one atom of oxygen from each of O2 and H2O, and is not a lavoprotein (Subramanian and Vaidyanathan 1984). 2. The degradation of 1,3,5-trihydroxybenzene (phloroglucinol) by Fusarium solani involves rearrangement to 1,2,3-trihydroxybenzene (pyrogallol) followed by ring cleavage to 2-ketohex-3-ene-1,6-dicarboxylate (Walker and Taylor 1983). This rearrangement is the opposite of that involved in the anaerobic degradation of 3,4,5-trihydroxybenzoate (Chapter 8, Part 4). 3. The imperfect fungus, Paecilomyces liliacinus, is able to produce mono-, di-, and trihydroxylated metabolites successively from biphenyl, and carry out intradiol ring ission of rings carrying adjacent hydroxyl groups (Gesell et al. 2001). Similarly, mono- and dihydroxylated metabolites are produced from dibenzofuran followed by intradiol ission of the ring with adjacent hydroxyl groups (Gesell et al. 2004). Metabolism by Yeasts The metabolic potential of yeasts has attracted attention in different contexts, and it has emerged that in contrast to many fungi, they are able to bring about ission of aromatic rings. Some examples that illustrate the various possibilities are given below: 1. Ring ission clearly occurs during the metabolism of phenol (Walker 1973) by the yeast Rhodotorula glutinis, and of aromatic acids by various fungi (Cain et al. 1968; Durham et al. 1984; Gupta et al. 1986). 2. Analogous ring ission reactions have also been found in studies on the metabolism of other aromatic compounds by the yeast Trichosporon cutaneum whose metabolic versatility is indeed comparable with that of bacteria. Examples include the degradation of

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phenol and resorcinol (Gaal and Neujahr 1979), tryptophan and anthranilate (Anderson and Dagley 1981a), and aromatic acids (Anderson and Dagley 1981b). 3. The ability to grow at the expense of 4-hydroxy- and 3,4-dihydroxybenzoate has been used for the classiication of medically important yeasts including Candida parapsilosis (Cooper and Land 1979). This organism degrades these substrates by oxidative decarboxylation, catalyzed by a lavoprotein monooxygenase (Eppink et al. 1997). 4. The phenol-assimilating yeast Candida maltosa degraded a number of phenols, even though these were unable to support growth. Hydroxylation of 3-chloro- and 4-chlorophenol initially produced 4-chlorocatechol and then 5-chloropyrogallol (Polnisch et al. 1992). The yeast Rhodotorula cresolica was able to assimilate phenol, 3- and 4-methylphenol, catechol and 3- and 4-methylcatechol, resorcinol and hydroquinone, and a wide range of phenolic carboxylic acids (Middelhoven and Spaaij 1997). 5. Diphenyl ether is transformed by Trichosporum beigelii through successive hydroxylation and extradiol ring ission of the resulting catechol (Schauer et al. 1995). In a formally analogous way, the metabolism of dibenzofuran by the yeast Trichosporon mucoides involves initial hydroxylation of one of the rings followed by ring ission at the 2,3-position (Hammer et al. 1998). Yeasts are also able to degrade long-chain alkanes. This is accomplished in two subcellular organelles—in microsomes, cytochrome P450 and the associated NADH reductase (Käppeli 1986) carry out hydroxylation, while the alkanols are dehydrogenated and undergo β-oxidation in peroxisomes that are induced during growth with alkanes (Tanaka and Ueda 1993). Clearly then, yeasts possess metabolic potential for the degradation of xenobiotics little inferior to that of many bacterial groups, so that their role in natural ecosystems justiies the greater attention that has been directed to them (MacGillivray and Shiaris 1993).

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Cerniglia CE, DT Gibson, C van Baalen (1982) Naphthalene metabolism by diatoms isolated from the Kachemak Bay region of Alaska. J Gen Microbiol 128: 987–990. Cerniglia CE, JP Freeman, C van Baalen (1981) Biotransformation and toxicity of aniline and aniline derivatives in cyanobacteria. Arch Microbiol 130: 272–275. Cerniglia CE, JP Freeman, JR Althaus, C van Baalen (1983) Metabolism and toxicity of 1- and 2-methylnaphthalene and their derivatives in cyanobacteria. Arch Microbiol 136: 177–183. Chen, YP, AR Glenn, MJ Dilworth (1985) Aromatic metabolism in Rhizobium trifolii—catechol 1,2-dioxygenase. Arch Microbiol 141: 225–228. Chen YP, MJ Dilworth, AR Glenn (1984) Aromatic metabolism in Rhizobium trifolii—protocatechuate 3,4dioxygenase. Arch Microbiol 138: 187–190. Childers SE, DR Lovley (2001) Differences in Fe(III) reduction in the hyperthermophilic archaeon Pyrobaculum islandicum, versus mesophilic Fe(III)-reducing bacteria. FEMS Microbiol Lett 195: 253–258. Chung WK, GM King (2001) Isolation, characterization, and polyaromatic hydrocarbon potential of aerobic bacteria from marine macrofainal burrow sediments and description of Lutibacterium anuloederans gen. nov., sp. nov., and Cycloclasticus spirillensis sp. nov. Appl Environ Microbiol 67: 5585–5592. Coates JD, EJP Phillips, DJ Lonergan, H Jenter, DR Lovley (1996) Isolation of Geobacter species from diverse sedimentary environments. Appl Environ Microbiol 62: 1531–1536. Coates JD, VK Bhupathiraju, LA Achenbach, MJ McInerney, DR Lovely (2001) Geobacter hydrogenophilus, Geobacter chapellei and Geobacter grbiciae, three new, strictly anaerobic, dissimilatory Fe(III) reducers. Int J Syst Evolut Microbiol 51: 581–588. Coleman NV, JC Spain (2003) Epoxyalkane: coenzyme M transferase in the ethene and vinyl chloride biodegradation pathways of Mycobacterium strain JS60. J Bacteriol 185: 5536–5546. Combourieu B, P Besse, M Sancelme, H Veschambre, AM Delort, P Poupin, N Truffaut (1998) Morpholine degradation pathway of Mycobacterium aurum MO1: direct evidence of intermadiates by in situ 1H nuclear magnetic resonance. Appl Environ Microbiol 64: 153–158. Cook AM, CG Daughton, M Alexander (1979) Benzene from bacterial cleavage of the carbon–phosphorus bond of phenylphosphonates. Biochem J 184: 453–455. Cooper BH, GA Land (1979) Assimilation of protocatechuate acid and p-hydroxybenzoic acid as an aid to laboratory identiication of Candida parapsilosis and other medically important yeasts. J Clin Microbiol 10: 343–345. Cooper RA, MA Skinner (1980) Catabolism of 3- and 4-hydroxyphenylacetate by the 3,4-dihydroxyphenylacetate pathway in Escherichia coli. J Bacteriol 143: 302–306. Corke CT, NJ Bunce, A-L Beaumont, RL Merrick (1979) Diazonium cations as intermediates in the microbial transformations of chloroanilines to chlorinated biphenyls, azo compounds and triazenes. J Agric Food Chem 27: 644–646. Cserjesi AJ, EL Johnson (1972) Methylation of pentachlorophenol by Trichoderma virginatum. Can J Microbiol 18: 45–49. Damaj M, D Ahmad (1996) Biodegradation of polychlorinated biphenyls by rhizobia: a novel inding. Biochem Biophys Res Commun 218: 908–915. Davison AD, P Karuso, DR Jardine, DA Veal (1996) Halopicolinic acids, novel products arising through the degradation of chloro- and bromobiphenyl by Sphingomonas paucimobilis BPS1-3. Can J Microbiol 42: 66–71. DeBont JAM, SB Primrose, MD Collins, D Jones (1980) Chemical studies on some bacteria which utilize gaseous unsaturated hydrocarbons. J Gen Microbiol 117: 97–102. Dedysh SN, C Knief, PF Dunield (2005) Methylocella species are facultatively methanotrophic. J Bacteriol 187: 4665–4670. Degrassi G, PP de Laureto, CV Bruschi (1995) Puriication and chracterization of ferulate and p-coumarate decarboxylase from Bacillus pumilis. Appl Environ Microbiol 61: 326–332. Dehning I, B Schink (1989a) Malonomonas rubra gen nov. sp. nov., a microaerotolerant anaerobic bacterium growing by decarboxylation of malonate. Arch Microbiol 151: 427–433. Dehning I, B Schink (1989b) Two new species of anaerobic oxalate-fermenting bacteria, Oxalobacter vibrioformis sp. nov., and Clostridium oxalicum sp. nov., from sediment samples. Arch Microbiol 153: 79–84. Dehning I, M Stieb, B Schink (1989) Sporomusa malonica sp. nov., a homoacetogenic bacterium growing by decarboxylation of malonate or succinate. Arch Microbiol 151: 421–426. DeWeerd KA, L Mandelco, RS Tanner, CR Woese, JM Sulita (1990) Desulfomonile tiedjei gen nov. and sp. nov., a novel anaerobic, dehalogenating, sulfate-reducing bacterium. Arch Microbiol 154: 23–30.

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PART 2 REACTIONS MEDIATED BY HIGHER ORGANISMS INTRODUCTION Very few xenobiotics remain unaltered in the environment for any length of time after their release. Although metabolism by microorganisms has already been discussed, brief comments are made here on the metabolism of contaminants by higher organisms—particularly ish. Metabolites such as conjugates may enter the aquatic environment where their ultimate fate is determined by microbial reactions. Metabolism by higher organisms is relevant to the mechanisms whereby organisms detoxify deleterious contaminants or, conversely, induce the synthesis of toxic metabolites. Some illustrations of these are briely summarized below: 1. The kinetics and products of metabolism critically inluence the nature and the concentrations of the xenobiotic and its transformation products to which the cells are exposed. Increasing evidence from different sources has shown that the effective toxicant may indeed be a metabolite synthesized from the compound originally supplied and not the xenobiotic itself. It is important to appreciate that, as with toxicity, the extent of metabolism will generally depend on the nature and position of substituents on aromatic rings as well as on their number. For example, although 2,3,4- and 3,4,5-trichloroaniline were N-acetylated in guppy, this did not occur with 2,4,5-trichloroaniline (de Wolf et al. 1993). Metabolism may also be an important determinant of genotoxic effects, estrogenic activity, and teratogenicity. 2. The classic example is that of Prontosil (Figure 2.12) in which the compound is active against bacterial infection in animals though inactive against the bacteria in pure culture. The toxicity in animals is the result of reduction to the sulfanilamide (4-aminobenzenesulfonamide) that competitively blocks the incorporation of 4-aminobenzoate into the vitamin folic acid. 3. The mechanism of luoroacetate toxicity in mammals has been extensively examined and was originally thought to involve simply initial synthesis of luorocitrate that inhibits aconitase and thereby the functioning of the TCA cycle (Peters 1952). Walsh (1982) has

NH 2

NH 2 H2 N

FIGURE 2.12

N

N

SO 2 NH 2

Metabolism of Prontosil in mammals.

H2 N

NH 2 + H 2 N

SO 2 NH 2

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FIGURE 2.13

4.

5. 6.

7.

C

S − CH 3 CH

N −O −CONHCH3

CH 3 CH 3

C

S − CH 3 CH

N−O−CONHCH3

Metabolism of aldicarb by rainbow trout.

extensively reinvestigated the problem, and revealed both the complexity of the mechanism of inhibition and the stereospeciicity of the formation of luorocitrate from luoroacetate. Considerable attention has been directed to the synthesis of the epoxides and dihydrodiol epoxides of polycyclic aromatic hydrocarbons mediated by the action of cytochrome P450 systems, and their role in inducing carcinogenesis in ish (Varanasi et al. 1987; de Maagd and Vethaak 1998). Tumors observed in feral ish exposed to PAHs may plausibly—though not necessarily—be the result of this transformation. Even though an apparently causal relationship between exposure of ish to PAHs and disease may have been established (Malins et al. 1985, 1987), caution should be exercised due to the possibility that other— and unknown—substances may have induced carcinogenesis. It is also important to appreciate that other compounds may induce induction of the metabolic system for PAHs. For example, exposure of rainbow trout to PCBs increases the effectiveness of liver enzymes to transform benzo[a]pyrene to carcinogenic intermediates (Egaas and Varanasi 1982). The carbamate insecticide aldicarb (Figure 2.13) that exerts its effect by inactivating acetylcholinesterase is metabolized by a lavin monooxygenase from rainbow trout to the sulfoxide, which is a more effective inhibitor (Schlenk and Buhler 1991). Pre-exposure to the organophosphate diazinon at exposures half the LC50 values increased the LC50 value by a factor of about ive for guppy (Poecilia reticulata), but had no effect on the value for zebra ish (Brachydanio rerio). This was consistent with the observation that during pre-exposure of guppy there was a marked inhibition in the synthesis of the toxic metabolites diazoxon and pyrimidinol, whereas this did not occur with zebra ish in which the toxicity was mediated primarily by the parent compound (Keizer et al. 1993). Pyrene is metabolized by the fungus Crinipellis stipitaria to 1-hydroxypyrene, and this has a spectrum of toxic effects substantially greater than those of pyrene: these include cytotoxicity to HeLa S3 cells, toxicity to a number of bacteria and to the nematode Caenorhabditis elegans (Lambert et al. 1995).

At the other extreme, if metabolism of the xenobiotic by the organism does not occur at all—or at insigniicant rates—after exposure, the compound will be persistent in the organism, and may therefore be consumed by predators. This is relevant to biomagniication. Most of the reactions carried out by ish and higher aquatic organisms are relatively limited transformation reactions in which the skeletal structure of the contaminants remains intact. The following three widely distributed reactions are of greatest signiicance: 1. Cytochrome P450–type monooxygenase systems, which have a generally low substrate speciicity, are widely distributed in the species of ish used for toxicity testing (Funari et al. 1987). 2. Glutathione S-transferases (Donnarumma et al. 1988; Nimmo 1987), which are important in the metabolism of highly reactive compounds containing electrophilic groups such as epoxides, and aromatic rings with several strongly electron-attracting substituents such as halogen, cyano, or nitro groups. 3. Conjugation of polar groups such as amines, carboxylic acids, and phenolic hydroxyl groups produce water-soluble compounds that are excreted and these reactions therefore function as a detoxiication mechanism.

93

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METABOLISM BY FISH The biotransformation of xenobiotics in many higher organisms is mediated by the cytochrome P450 monooxygenase system and the complexity of factors that regulate the synthesis of this in ish has been reviewed (Andersson and Förlin 1992). The metabolic potential of ish may appear restricted compared with that of microorganisms, but it may have been considerably underestimated. For example, metolachlor (2-chloro-N-[2-ethyl-6-methylphenyl]-N-[2-methoxy-1methylethyl]acetamide) is metabolized by bluegill sunish (Lepomis macrochirus) by reactions involving initially O-demethylation and hydroxylation (Cruz et al. 1993) (Figure 2.14). These are comparable to the reactions carried out by an actinomycete (Krause et al. 1985), and the benzylic hydroxylation is analogous to that involved in the biotransformation of the structurally similar alachlor by the fungus Cunninghamella elegans (Pothuluri et al. 1993). An extensive compilation of the transformation of xenobiotics by ish has been given (Sijm and Opperhuizen 1989), and only a few examples of these reactions are summarized here as illustration: 1. N-Dealkylation of dinitramine to 1,3-diamino-2,4-dinitro-6-triluoromethylbenzene (Olson et al. 1977) by carp (Cyprinus carpio) (Figure 2.15). 2. O-Demethylation of pentachloroanisole in rainbow trout (Salmo gairdneri ≡ Oncorhynchus mykiss) (Glickman et al. 1977), and of chlorinated veratroles by zebra ish (Neilson et al. 1989). 3. Acetylation of 3-amino ethylbenzoate in rainbow trout (Hunn et al. 1968). 4. Displacement of the nitro group in pentachloronitrobenzene by hydroxyl and thiol groups (Bahig et al. 1981) (Figure 2.16) in golden orfs (Idus idus). 5. Oxidation of a number of PAHs has been demonstrated in a variety of ish. A review directed to metabolism and the role of PAH metabolites in inducing tumorogenesis has been given in de Maagd and Vethaak (1998), and only two examples are given here: a. Coho salmon (Oncorhynchus kisutch) metabolized naphthalene to a number of compounds consistent with oxidation to the epoxide, hydrolysis to the dihydrodiol, and dehydration of the trans-dihydrodiol to naphth-1-ol, or by rearrangement of the epoxide (Figure 2.17) (Collier et al. 1978). b. For the carcinogen benzo[a]pyrene, a wider range of metabolites has been identiied in southern lounder (Paralichthys lethostigma) including the 4,5-, 7,8-, and 9,10diols, the 1,6-, 3,6-, and 6,12-quinones in addition to the 1-, 3-, and 9-benzopyreneols (Figure 2.18) (Little et al. 1984).

CH 3

CH 2 N

CH−CH2−O−CH3 N

COCH 2 Cl

CH−CH2OH

CH 3

N

COCH 2 Cl

CH−CH2OH COCH 2 Cl

CH 2 OH

CH 3

Metabolism of metolachlor by bluegill sunish. NH 2

NH 2 F3 C

NO 2

F3C

NO 2

Metabolism of dinitramine by carp.

NH2 NO 2

NO2

F3 C

NHEt

N(C2 H 5 )2

FIGURE 2.15

CH 2

CH 3

CH 2

CH 3

FIGURE 2.14

CH 3

CH 3

CH 3

NO 2

NH2 NO2

94

Environmental Degradation and Transformation of Organic Chemicals OH Cl

Cl

Cl

Cl

NO 2

+

Conjugate

+

Conjugate

Cl

Cl

Cl

Cl

Cl

SH

Cl

Cl

Cl

Cl

Cl Cl

FIGURE 2.16

Metabolism of pentachloronitrobenzene by golden orfs. H

OH H

O H

FIGURE 2.17

OH

OH H

Metabolism of naphthalene by coho salmon. OH OH

OH OH

OH OH

O

O

O

O

FIGURE 2.18

O

O

Metabolism of benzo[a]pyrene by southern lounder.

6. N-Hydroxylation of aniline and 4-chloroaniline by rainbow trout to hydroxylamines that could plausibly account for the subchronic toxicity of the original compounds (Dady et al. 1991). Initially formed polar metabolites such as phenols and amines may be conjugated to water-soluble terminal metabolites that are excreted into the medium and function as an effective mechanism of detoxiication. For example, pentachlorophenol and pentachlorothiophenol produced from pentachloronitrobenzene conjugated represented the major metabolites. Although the naphthalene dihydrodiol was the major metabolite produced from naphthalene, the further transformation

95

Biotic Reactions O−CH2−CO2H

O−CH2−CO−NH−CH2−CH2−SO3H

Cl

Cl

FIGURE 2.19

Cl

Cl

Conjugation of carboxylic acids with amino acids.

product naphth-1-ol was also isolated as the sulfate, glucuronate, and glucose conjugates. Diverse conjugation reactions have been described and include the following: 1. Phenolic compounds with formation of glucuronides, sulfates, or glucosides as already noted. 2. Reaction of carboxylic acids with the amino groups of glycine (Huang and Collins 1962) or taurine (Figure 2.19) (James and Bend 1976) to form the amides. 3. Reaction between glutathione and reactive chloro compounds such as 1-chloro-2,4-dinitrobenzene (Niimi et al. 1989), or the chloroacetamide group in demethylated metolachlor (Cruz et al. 1993). Important investigations have been directed to persistent halogenated aromatic compounds and different mechanisms for their metabolism have been found: 1. Hydroxylated PCBs have been found in a laboratory study using rainbow trout (Oncorhynchus mykiss), and were similar to those previously observed (Campbell et al. 2003) in wild lake trout (Salvelinus namaycush). Although it was not possible to associate the metabolites unambiguously with their precursor PCB congener, those with neighboring hydrogen atoms in the ortho/para positions were most probably transformed, putatively by CYP 2B-type isoforms of cytochrome P450 rather than by CYP 1A enzymes (Buckman et al. 2006). 2. Debromination has been examined in rainbow trout (Oncorhynchus mykiss) and carp (Cyrprinus carpio) that were fed with a diet containing decabromodiphenyl ether (BDE 209). In both of them, products from debromination were found in whole ish, whole ish homogenates, organs, and microsomal preparations. In trout, debromination produced primarily the octa and nano congeners, whereas in carp penta to octa congeners were found. This was conirmed in microsomal preparations of carp that transformed up to 63% of DBE 209 with the formation of hexa to octa congeners, whereas in trout only 23% of DBE 209 was transformed to octa and nano congeners (Stapleton et al. 2006). It was suggested that the debromination could be analogous to the deiodination of thyroxine to the more active triiodothyronine by loss of iodine from the position ortho to the hydroxyl group.

METABOLISM BY OTHER ORGANISMS Mussels 1. Mussels do not generally carry out more than the limited reactions of oxidation and conjugation, and in the common mussel, Mytilus edulis, variations between summer and winter levels for both cytochrome P450 and NADPH-independent 7-ethoxycoumarin O-deethylase have been found (Kirchin et al. 1992). Levels of cytochrome P450 and the rates of metabolism of PAHs were apparently low compared with those found in ish (Livingstone and Farrar 1984), and an investigation using subcellular extracts of the digestive glands

96

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from the mussel M. galloprovincialis showed that although the formation of diols and phenols from benzo[a]pyrene was dependent on NADPH, the quinones that were the major metabolites were produced in the absence of NADPH apparently by radical-mediated reactions involving lipid peroxidase systems (Michel et al. 1992). 2. A reaction presumably mediated by glutathione S-transferase is the replacement of the 4-chloro substitutent in octachlorostyrene in the blue mussel (Mytilus edulis) by a thiomethyl group (Figure 2.20) (Bauer et al. 1989). A similar reaction of glutathione with arene oxides produced by aquatic mammals from PCBs and DDE results ultimately in the production of methyl sulfones (Bergman et al. 1994; Janák et al. 1998). In the arctic food chain—arctic cod (Boreogadus saida), ringed seal (Phoca hispidus), polar bear (Ursus maritima)—it has been shown that levels of the dimethyl sulfones of DDE and PCB were low in cod, and that levels in polar bear were the combined result of bioaccumulation from seals and endogenous metabolism (Letcher et al. 1998). The results of these investigations suggest that caution should be exercised in interpreting not only the results of toxicity assays in which such organisms are employed but also data accumulated in monitoring studies that may not have taken into account the existence of metabolites.

INSECTS Resistance of house lies (Musca domestica) to DDT was attributed to its transformation to the nontoxic DDE, and the enzyme that carries the dehydrochlorination has been characterized in DDTresistant lies (Lipke and Kearns 1959a,b). The herbicide alachlor is transformed by chironomid larvae by O-demethylation followed by loss of the chloroacetyl group to produce 2,6-diethylaniline (Figure 2.21) (Wei and Vossbrinck 1992).

INVERTEBRATES The metabolism of xenobiotics by both terrestrial and sediment-dwelling biota has been studied, and provides illustrations of the importance of uptake by food or by sorbed sediment. Some examples of metabolism by terrestrial biota include the following.

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

SCH 3

FIGURE 2.20 Metabolism of octachlorostyrene by the blue mussel.

Et

Et

Et CH2−O −CH3 N

NH −CO −CH2Cl

N CO −CH2Cl

Et

Et

CH2−OH CO −CH2Cl Et

FIGURE 2.21 Metabolism of alachlor by chironomid larvae.

Et

NH2 Et

Biotic Reactions

97

Isopods The uptake and elimination of benzo[a]pyrene by the terrestrial isopod Porcellio scaber have been investigated (van Brummelen and van Straalen 1996), and 1-hydroxypyrene was identiied among the metabolites of pyrene in this organism (Stroomberg et al. 1996). Oligochaetes Both the (+)- and (–)- enantiomers of limonene were transformed by larvae of the cutworm Spodoptera litura (Miyazawa et al. 1998). For both of them the reactions involved are (a) dihydroxylation between C-8 and C-9 and (b) oxidation of the C-1 methyl group to carboxyl. These transformations were not dependent on the intestinal microlora in contrast to the transformation of α-terpinene to p-mentha-1,3-dien-7-ol and p-cymene whose formation could be attributed to the intestinal lora. Polychaetes Polychaete worms belonging to the genera Nereis and Scolecolepides have extensive metabolic potential. Nereis virens is able to metabolize PCBs (McElroy and Means 1988) and a number of PAHs (McElroy 1990), while N. diversicolor and Scolecolepides viridis are able to metabolize benzo[a]pyrene (Driscoll and McElroy 1996). It is worth noting that apart from excretion of the toxicant, polar, and much more water-soluble metabolites such as the glycosides formed from pyrene by Porcellio sp. (Larsen et al. 1998) may be mobile in the interstitial water of the sediment phase. It has been shown that although the marine terebellid polychaete Amphitrite ornata produced no detectable halogenated metabolites, it synthesizes a dehalogenase that is able to carry out oxidative dehalogenation of halogenated phenols, with luoro, chloro, or bromo substituents (Chen et al. 1996). One of the enzymes (DHB 1) has been puriied, and consists of two identical subunits (Mr 15,530) each containing heme and histidine as the proximal Fe ligand. In the presence of H2O2, 2,4,6-tribromophenol is oxidized to 2,6-dibromo-benzo-1,4-quinone (LaCount et al. 2000).

HIGHER PLANTS Attention is briely drawn to the metabolism of contaminants by higher plants for several reasons: a. The metabolites may be toxic to biota at higher trophic levels. b. The metabolites may be translocated into the root system and, after partition into interstitial water in the soil, exert a toxic effect on other terrestrial organisms. c. There has been interest in the use of higher plants in the bioremediation of contaminated sites. This issue is addressed in detail in Chapters 12 and 14. The detoxiication and metabolism of higher plants has been reviewed (Sandermann 1994), and a few examples are given below as illustration: 1. Pentachlorophenol is metabolized by the aquatic plant Eichhornia crassipes to a number of metabolites including di-, tri-, and tetrachlorocatechol, 2,3,5-tri- and tetrachlorohydroquinone, pentachloroanisole, and tetrachloroveratrole (Roy and Hänninen 1994). The phenolic compounds should be compared with those produced during the photochemical transformation (Figure 2.22) and the initial stages in the microbiological metabolism of pentachlorophenol, followed by O-methylation. 2. Quite complex transformations may be mediated; for example, the metabolism of phoxim by plant organs and cell suspension of soybean (Glycine max) (Höhl and Barz 1995) (Figure 2.23).

98

Environmental Degradation and Transformation of Organic Chemicals OH Cl

OH

Cl

Cl

O Cl

Cl O

OH Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

HO

Cl

O

Cl

Cl

CO2H

Cl

CO2H

O OH

FIGURE 2.22

OH

Cl

Cl

Cl

Cl

Photochemical transformation of pentachlorophenol. CH 3 N

CH 3 O

OEt P

NOH

OEt

S

CH 3 NH 2

CH 3 NH−CO−CH2−CO2H

N-malonylation

FIGURE 2.23

Metabolism of phoxim by soybean (Glycine max).

3. The uptake and biotransformation of benzene from soil and the atmosphere has been studied in a number of plants. It was shown that in leaves of spinach (Spinacia oleracea) the label in 14C-benzene was found in muconic, fumaric, succinic, malic, and oxalic acids, as well as in speciic amino acids, and that an enzyme preparation in the presence of NADH or NADPH produced phenol (Ugrekhelidze et al. 1997). 4. Hybrid poplars are able to transport and metabolize diverse xenobiotics: a. Trichloroethene was metabolized to trichloroethanol and trichloroacetate (Newman et al. 1997), and the trichloroethanol conjugated to the β-d-glucoside (Shang et al. 2001). b. Atrazine was metabolized by reactions involving dealkylation and hydrolytic dechlorination to 4,6-diamino-1,3,5-triazine (Burken and Schnoor 1997). c. Tissue cultures of poplar (Populus deltoides × nigra) metabolized the explosive hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) by partial reduction to the 1-nitroso and 1,3-dintroso derivatives, and in the light these were further metabolized to CH2O, CH3OH, and CO2 (van Aken et al. 2004). 5. 2,4,6-Trinitrotoluene (TNT) is reduced by the aquatic plant Myriophyllum spicatum to aminodinitrotoluenes (Pavlostathis et al. 1998) and, in axenic root cultures of Catharanthus roseus, the initial metabolites 2-amino-4,6-dinitrotoluene and 4-amino-2,6-dintrotoluene

99

Biotic Reactions

were conjugated probably with C6-units (Bhadra et al. 1999). There are clearly several important unresolved issues including the phytotoxicity of these metabolites before phytoremediation of TNT could be exploited. 6. Reed Canary Grass (Phalaris arundinacea) was grown in liquid culture and exposed to RDX that was metabolized to the potentially toxic 4-nitro-2,4-diazabutanal (Just and Schnoor 2004). This metabolite is also produced from RDX by strains of Rhodococcus sp. and from the homologous octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) by Phanerochaete chrysosporium. 7. Transformation of DDT to DDD by reductive dechlorination has been demonstrated in a number of aquatic plants, although the reaction appears to be abiotic mediated by some component of the plants (Garrison et al. 2000).

OTHER ORGANISMS Other groups of biota are able to bring about transformation of structurally diverse compounds and limited investigations have revealed the metabolic potential of taxonomically diverse eukaryotic organisms: a. The apochlorotic alga (protozoan) Prototheca zopii is able to degrade aliphatic hydrocarbons (Walker and Pore 1978; Koenig and Ward 1983). b. Tetrahymena thermophila transforms pentachloronitrobenzene to the corresponding aniline and pentachlorothioanisole (Figure 2.24) (Murphy et al. 1982). c. Daphnia magna has been shown to bring about dechlorination and limited oxidation of heptachlor (Figure 2.25) (Feroz et al. 1990).

NH 2

NO 2

SCH 3

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

+ Cl

FIGURE 2.24

Cl

Cl

Biotransformation of pentachloronitrobenzene by Tetrahymena thermophila. Cl

Cl Cl

Cl Cl

Cl Cl

Cl

Cl

Cl

Cl

O Cl Cl

Cl Cl

Cl Cl

Cl

OH

Cl

OH Cl

FIGURE 2.25

Biotransformation of heptachlor by Daphnia magna.

100

Environmental Degradation and Transformation of Organic Chemicals

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Newman LA, SE Strand, N Choe, J Duffy, G Ekuan, M Ruiszai, BB Shurtleff, J Wilmoth, MP Gordon (1997) Uptake and biotransformation of trichloroethylene by hybrid poplars. Environ Sci Technol 31: 1062–1067. Niimi AJ, HB Lee, GP Kissoon (1989) Octanol/water partition coeficients and bioconcentration factors of chloronitrobenzenes in rainbow trout (Salmo gairdneri) Environ Toxicol Chem 8: 817-823. Nimmo IA (1987) The glutathione S-transferases of ish. Fish Physiol Biochem 3: 163–172. Olson LE, JL Allen, JW Hogan (1977) Biotransformation and elimination of the herbicide dinitramine in carp. J Agric Food Chem 25: 554–556. Pavlostathis SG, KK Comstock, ME Jacobson, FM Saunders (1998) Transformation of 2,4,6-trinitrotoluene by the aquatic plant Myriophyllum spicatum. Environ Toxicol Chem 17: 2266–2273. Peters R (1952) Lethal synthesis. Proc Roy Soc (London) B 139: 143–170 Pothuluri JV, JP Freeman, FE Evans, TB Moorman, CE Cerniglia (1993) Metabolism of alachlor by the fungus Cunninghamella elegans. J Agric Food Chem 41: 483–488. Roy S, O Hänninen (1994) Pentachlorophenol: uptake/elimination kinetics and metabolism in an aquatic plant Eichhornia crassipes. Environ Toxicol Chem 13: 763–773. Sandermann H (1994) Higher plant metabolism of xenobiotics: the “green liver” concept. Pharmacogenetics 4: 225–241. Schlenk D, DR Buhler (1991) Role of lavin-containing monooxygenase in the in vitro biotransformation of aldicarb in rainbow trout (Oncorhyncus mykiss). Xenobiotica 21: 1583–1589. Shang TQ, SL Doty, AM Wilson, WN Howald, MP Goprdon (2001) Trichloroethylene oxidative metabolism in plants: the trichloroethanol pathway. Phytochemistry 58: 1055–1065. Sijm DTHM, A Opperhuizen (1989) Biotransformation of organic chemicals by ish: enzyme activities and reactions. Handbook Environ Chem 2E: 164–235. Stapleton HM, B Brazil, RD Holbrook, CL Mitchelmore, R Benedict, A Konstatinov, D Potter (2006) In vivo and in vitro debromination of decabromodiphenmyl ether (BDE 209) by juvenile rainbow trout and common carp. Environ Sci Technol 40: 4653–4658. Stroomberg GJ, C Reuther, I Konin, TC van Brummelen, CAM van Gestel, C Gooijer, WP Coino (1996) Formation of pyrene metabolites by the terrestrial isopod Porcello scaber. Chemosphere 33: 1905–1914. Ugrekhelidze D, F Korte, G Kvesitadze (1997) Uptake and transformation of benzene and toluene by plant leaves. Ecotoxicol Environ Saf 37: 24–29. van Aken B, JM Yoon, CL Just, JL Schnoor (2004) Metabolism and mineralization of hexahydro-1,3,5trinitro-1,3,5-triazine inside poplar tissues (Populus deltoides × nigra DN-34). Environ Sci Technol 38: 4572–4579. van Brummelen TC, NM van Straalen (1996) Uptake and elimination of benzo[a]pyrene in the terrestrial isopod Porcello scaber. Arch Environ Contam Toxicol 31: 277–285. Varanasi U, JE Stein, M Nishimoto, WL Reichert, TK Collier (1987) Chemical carcinogenesis in feral ish: uptake, activation, and detoxication of organic xenobiotics. Environ Health Perspect 71: 155–170. Walker JD, RS Pore (1978) Growth of Prototheca isolates on n-hexadecane and mixed-hydrocarbon substrate. Appl Environ Microbiol 35: 694–697. Walsh C (1982) Fluorinated substrate analogs: routes of metabolism and selective toxicity. Adv Enzymol 55: 187–288. Wei LY, CR Vossbrinck (1992) Degradation of alachlor in chironomid larvae (Diptera: Chironomidae). J Agric Food Chem 40: 1695–1699.

3 Mechanistic Aspects PART 1 INTRODUCTION OF OXYGEN This section addresses the cardinal issue of the mechanisms whereby oxygen is introduced into the substrates during degradation. A few comments are added on haloperoxidases, even though their major signiicance lies in the biogenesis of natural halogenated metabolites of bacteria, yeasts, and algae. Details of the reactions involved in degradation are covered in the appropriate parts of Chapters 7 through 11. There are several mechanisms by which oxygen is introduced during degradation: (a) molecular oxygen (dioxygen) may supply one atom of oxygen (monooxygenation), (b) dioxygen may supply both atoms of oxygen (dioxygenation), (c) the oxygen may originate from H2O (hydroxylation or hydration), and (d) by the activity of oxidases and peroxidases. A summary of oxygenation systems is given in Figure 3.1 and additional details of dioxygenases are given in Figure 3.2. The enzymes that introduce oxygen from water have been termed hydroxylases, but are more correctly termed oxidoreductases. These are particularly important in the degradation of azaarenes under both aerobic and anaerobic conditions.

MONOOXYGENATION Monooxygenases belong to a family of enzymes that introduce one atom of dioxygen into a wide range of substrates. These include aliphatic hydrocarbons and ketones, arene hydrocarbons, phenols, and hydroxybenzoates. For degradation of the aromatic compounds ission of the ring mediated by dioxygenases is necessary. These are discussed later in this section, and a comparison of the activities of monooxygenases and dioxygenases is given in Figure 3.3. Hydroxylation of Alkanes The oxidation of the simplest alkane methanol is carried out by methylotrophs that may be obligate or facultative. Only brief mention is made here of methane monooxygenase (MMO), which catalyzes the introduction of oxygen into methane. The enzyme exists in both a soluble (sMMO) and a particulate (pMMO) form of which the former has been more extensively studied. The enzyme consists of three components: a hydroxylase, a regulatory protein that is not directly involved in electron transfer between the hydroxylase, and a third protein that is a reductase containing lavin adenine dinucleotide (FAD) and a [2Fe–2S] cluster. Details of the structure of the hydroxylase and the mechanism of its action involving the FeIII–O–FeIII at the active site are given in a review (Lipscomb 1994). The particulate enzyme contains copper (Nguyen et al. 1994) or both copper and iron (Zahn and DiSpirito 1996), and the concentration of copper determines the catalytic activity of the enzyme (Sontoh and Semrau 1998). Alkane hydroxylase activity for higher alkanes is distributed among a number of Gram-negative bacteria, and sequence analysis of proteins shows that these differ widely even among pseudomonads (Smits et al. 2002). The alkane hydroxylase system for Pseudomonas putida (P. oleovorans) GPO1, which has been most extensively studied, is composed of three components: an integral membrane alkane hydroxylase (AlkB), a soluble rubredoxin (AlkG), and a soluble NADH-rubredoxin reductase (AlkT). The irst of these is a representative of a large nonheme diiron cluster (Shanklin et al. 1997), while the others are involved in electron transport. The alkane hydroxylase of Acinetobacter sp. strain ADP1 is formally similar in requiring three components (Ratajczak et al. 1998). The alkane hydroxylase belongs to a family of nonheme iron oxygenases. There is some structural similarity between the nucleotide sequence of the integral membrane alkane hydroxylase and 103

104

Environmental Degradation and Transformation of Organic Chemicals Source of oxygen O2  oxygenases 1.1

Monooxygenases

1.2

Dioxygenases

2

Source of oxygen H 2O  hydroxylases

2.1

Oxidoreductases

2.2

Hydroxylating system: chemical reaction with cation radicals produced by peroxidases

1

Oxygenases

1.1

Monooxygenases Flavoproteins introducing oxygen at site adjacent to existing hydroxy group 4-hydroxybenzoate hydroxylase Anthranilate hydroxylase in yeasts Salicylate hydroxylase Hydrocarbon hydroxylases introducing oxygen into nonoxygenated rings Toluene, ph enanthrene, pyrene monooxygenases Hydrocarbon epoxidases Fungal and yeast biotransformations of PAHs : production of phenols by NIH shift

1.2

Dioxygenases Dihydroxylating enzymes (Produce cis dihydrodiols: soluble multicomponent enzymes requiring NAD(P)H as cofactor) Benzene 1,2-dioxygenase Toluene 2, 3-dioxygenase Naphthalene 1,2-dioxygenase Biphenyl 2,3-dioxygenase Ring-cleavage enzymes (Carry out ring fission and require no cofactor) Catechol 2,3-dioxygenase (extradiol cleavage to carboxyaldehydes) Catechol 1,2-dioxygenase (intradiol cleavage to dicarboxylates) Hydroxylases

2.1

Oxidoreductases Mo multicomponent enzymes carrying out addition of H2O followed by dehydrogenation e.g., anaerobic hydratases coupled to dehydrogenases

2.2

Hydroxylation systems Secondary reaction with cation radicals formed by peroxidases

FIGURE 3.1 Bacterial oxygenation systems (excluding cytochrome P450 systems). (From Neilson, A.H. and Allard, A.-S. Microbial metabolism of PAHs and heteroarenes, The Handbook of Environmental Chemistry, Vol. 3J, pp. 1–80, Springer, 1998. With permission.)

the subunits of the monooxygenase encoded by xylA and xylM in the TOL plasmid that are involved in hydroxylation of the methyl groups in toluene and xylene in Pseudomonas putida PaW1 (Suzuki et al. 1991). Epoxidation of Alkenes The irst step in the aerobic degradation of alkenes is epoxidation. Epoxidation is then followed by several alternatives. In one of them, the epoxides may undergo carboxylation: the enzyme

105

Mechanistic Aspects Class I

Two −componentenzyme, e.g., benzoate, 4-sulfobenzoate

Class II

(1)

Reductase  flavin + [2Fe-2S] redox center

(2)

Oxygenase

Three −component enzyme, e.g., benzene and toluene

Class III

(1)

Reductase  flavoprotein

(2)

Ferrodoxin  Rieske type

(3)

Oxygenase

Three−component type, e.g., naphthalene (1)

Reductase  flavin + [2Fe−2S] redox center

(2)

[2Fe−2S] ferrodoxin

(3)

Oxygenase

Futher division may be made according to the FMN or FAD flavin r equirement, and the nature of the [2Fe−2S] protein

FIGURE 3.2 Classiication of bacterial dioxygenases. (From Neilson, A.H. and Allard, A.-S. Microbial metabolism of PAHs and heteroarenes, The Handbook of Environmental Chemistry, Vol. 3J, pp. 1–80, Springer, 1998. With permission.) Monooxygenase (a)

RH+ O 2 + H + NAD(P)H

(b)

+ O 2 + H + NAD(P)H

ROH +H 2 O +NAD(P) O + H 2 O+ NAD(P)

Dioxygenase (c)

H OH NAD(P) OH +

+ O 2 + H + NAD(P)H

H CO 2 H OH

CO 2 H

+ O2

(d) OH

FIGURE 3.3

Intradiol

Extradiol

CO 2 H OH CHO

Summary of (a,b) monooxygenase, (c,d) dioxygenase reactions.

complex has been puriied from Xanthobacter sp. strain Py2, and includes an NADPH: disulide oxidoreductase and three carboxylation components (Allen and Ensign 1997; Allen et al. 1999) (Figure 3.4). Alkene monooxygenase from this strain is closely related to the aromatic monooxygenases, and is able to hydroxylate benzene, toluene, and phenol (Zhou et al. 1999). The alkane hydroxylase from Pseudomonas oleovorans is able to carry out both hydroxylation and epoxidation (Ruettinger et al. 1977). Cycloalkanone Monooxygenases Flavoprotein 1,2-monooxygenases are used for the insertion of an atom of oxygen into the ring that is the irst step in the degradation of both cyclopentanone and cyclohexanone before hydrolysis of the resulting lactones and dehydrogenation (Figure 3.5). There are two types of cycloalkanone

106

Environmental Degradation and Transformation of Organic Chemicals NADP

FA D

NADP

NADP

FA DH

FA D

FAD

S

S

S

S

S CoM

S

S O

H

S

S

CH2

C

CoMS CH3

OH +

CH2

CH3

HO2C−CH2−COCH3

FIGURE 3.4

C

CH3COCH3

Mechanism for carboxylation of acetone involving FAD, NADP, and coenzyme M.

O

O

O

CO 2H (CH 2 )4 CH 2OH

FIGURE 3.5

Monooxygenation of cyclohexanone.

monooxygenase: one that is FAD–NADPH-dependent, whereas the other is FMN–NADH-dependent. There has been renewed interest in these reactions in view of their biotechnological importance (Iwaki et al. 2002). Cycloalkanone monooxygenase for substrates with more than seven carbon atoms is, however, different (Kostichka et al. 2001). These monooxygenases are also involved in the degradation of cyclic terpenoids, and the enzyme from Rhodococcus erythropolis strain DCL14 is able to catalyze insertions of oxygen into the cyclohexanones produced from both (+)-(4R)- and (−)-(4S)limonene by Rhodococcus erythropolis (van der Werf et al. 1999). In addition, the monooxygenase from this strain is able to insert an oxygen atom into 2-ketoterpenoids at both the 1,2 and 2,3 positions, and of a 3-ketoterpenoid at the 3,4 position (terpenoid numbering) (van der Werf 2000). Monooxygenation of Aromatic Compounds Although the bacterial degradation of aromatic compounds is most frequently initiated by dioxygenation, monooxygenases may be involved additionally or alternatively for the introduction of oxygen into the ring. An alternative pathway for the degradation of alkyl arenes involves oxidation of methyl substituents to carboxylates (Figure 3.6). This is also used for the degradation of 4-nitrotoluene by Pseudomonas sp. strain TW3. The ntnWCMAB* genes that encode the enzymes, which convert the substrate into 4-nitrobenzoate, are similar to those in the upper pathway of the TOL plasmid (Harayama et al. 1989): an alcohol dehydrogenase, benzaldehyde dehydrogenase, a two-component monooxygenase, and part of a benzyl alcohol dehydrogenase (James and Williams 1998). In this strain, however, the enzymes are chromosomal, and the benzyl alcohol dehydrogenase ntnB* differs from the corresponding xylB protein. The oxidation by strains of Pseudomonas putida of the methyl group in arenes containing a hydroxyl group in the para position is, however, carried out by a different mechanism. The initial step is dehydrogenation to a quinone methide followed by hydration (hydroxylation) to the benzyl alcohol (Hopper 1976) (Figure 3.7). The reaction with 4-ethylphenol is partially stereospeciic (McIntire et al. 1984), and the enzymes that catalyze the irst two steps are lavocytochromes (McIntire et al. 1985). The role of formal hydroxylation in the degradation of azaarenes is discussed in the section on oxidoreductases (hydroxylases).

107

Mechanistic Aspects CH 3

CO 2 H

CO 2H

CH 3

CO 2H

CO 2 H CO 2 H

OH OH

OH

OH

FIGURE 3.6 Degradation of toluene by side-chain oxidation.

FIGURE 3.7

CH3

CH2

CH2 OH

CHO

OH

O

OH

OH

Degradation of 4-methylphenol by hydroxylation.

Reactions of Aromatic Hydrocarbons Concurrent synthesis of both mono- and dioxygenases has been shown: 1. Several strains of Pseudomonas sp. that were induced for toluene dioxygenase activity catalyzed the enantiomeric monooxygenation of indane to indan-1-ol, and indene to inden-1-ol and cis-indan-1,2-diol (Wackett et al. 1988). Puriied naphthalene dioxygenase from a strain of Pseudomonas sp. catalyzed the enantiomeric monooxygenation of indane to indan-1-ol and the dehydrogenation of indane to indene (Figure 3.8) (Gibson et al. 1995). 2. By cloning genes for benzene/toluene degradative enzymes in Pseudomonas (Burkholderia) sp. strain JS150, it has been found that this strain carries genes for a monooxygenase in addition to those for a dioxygenase (Johnson and Olsen 1995). Initial products from the metabolism of toluene after dehydrogenation are, therefore, 3-methyl catechol produced by 2,3-dioxygenation, 4-methylcatechol by 4-monooxygenation, and both 3- and 4-methylcatechols by 2-monooxygenation (Johnson and Olsen 1997). 3. Sphingomonas yanoikuyae (Beijerinckia sp.) strain B1 metabolizes biphenyl by initial dioxygenation followed by dehydrogenation to 2,3-dihydroxybiphenyl. Cells of a mutant (strain B8/36) lacking cis-biphenyl dihydrodiol dehydrogenase were induced with 1,3-dimethylbenzene, and could transform dihydronaphthalene by three reactions: (i) monooxygenation to (+)-(R)-2-hydroxy-1,2-dihydronaphthalene, (ii) dioxygenation to (+)-(1R,2S)-cis-naphthalene dihydrodiol, and (iii) dehydrogenation to naphthalene followed by dioxygenation to (+)-(1R,2S)-cis-naphthalene dihydrodiol (Eaton et al. 1996). 4. The degradation of pyrene by a Mycobacterium sp. involves both di- and monooxygenase activities (Heitkamp et al. 1988). 5. Arene oxides can be intermediates in the bacterial transformation of aromatic compounds and initiate rearrangements (NIH shifts) (Dalton et al. 1981; Cerniglia et al. 1984; Adriaens 1994). The formation of arene oxides may plausibly provide one mechanism for the formation of nitro-substituted products during degradation of aromatic compounds when nitrate is present in the medium. This is discussed in Chapter 2. 6. Toluene monooxygenases provide alternatives to dioxygenation, and the ortho-monooxygenase in Burkholderia (Pseudomonas) cepacia G4 has been shown to be carried

108

Environmental Degradation and Transformation of Organic Chemicals OH

FIGURE 3.8 Transformation of indane to 3-hydroxyindane and indene.

on a plasmid TOM (Shields et al. 1995). In Pseudomonas mendocina KR1, the degradation of toluene is initiated by a three-component toluene-4-monooxygenase that converts toluene into 4-methylphenol. The formation of an intermediate arene oxide is consistent with the observation of an NIH shift in which 68% of the deuterium in 4-[2H]-toluene is retained in the 4-methyl phenol (Whited and Gibson 1991). In contrast, the enzyme that oxidizes toluene-4-sulfonate to the benzyl alcohol in the irst step of its degradation is a monooxygenase that consists of only two components: an [Fe–S] lavoprotein that serves as a reductase and an oxygenase (Locher et al. 1991b). 7. Xanthobacter sp. strain Py2 was isolated by enrichment on propene that is metabolized by initial metabolism to the epoxide. The monooxygenase that is closely related to aromatic monooxygenases is able to hydroxylate benzene to phenol before degradation, and toluene to a mixture of 2-, 3-, and 4-methylphenols that are not further metabolized (Zhou et al. 1999). 8. Toluene/o-xylene monooxygenase in P. stutzeri strain OX1 carried out successive monooxygenation of o-xylene (Bertoni et al. 1998), and the toluene-4-monooxygenase of Pseudomonas mendocina KR1 and toluene-3-monooxygenase of Ralstonia pickettii PKO1 can hydroxylate benzene, toluene, and o-xylene (Tao et al. 2004; Vardar and Wood 2004). Reactions of Hydroxybenzoates and Related Compounds 1. Hydroxybenzoates can undergo hydroxylation with or without concomitant loss of CO2. For example, salicylate → catechol + CO2 (salicylate-1-hydroxylase) (Figure 3.9a) (WhiteStevens et al. 1972) and 4-hydroxybenzoate → 1,4-dihydroxybenzene + CO2 [(4-hydroxybenzoate 1-hydroxylase (decarboxylating)] in Candida parapsilosis (Figure 3.9b) (Eppink et al. 1997). 2. Hydroxylation without elimination of CO2 is illustrated in the following examples: a. Salicylate → 2,5-dihydroxybenzoate (salicylate-5-hydroxylase) (Zhou et al. 2002) (Figure 3.10a). b. Anthranilate → 5-hydroxyanthranilate and 2,5-dihydroxybenzoate (anthranilate-5hydroxylase) in Nocardia opaca (Figure 3.10b) (Cain 1968); Anthranilate → 2,3-dihydroxybenzoate in Trichosporon cutaneum (Figure 3.10c) (Powlowski et al. 1987). c. 3-Hydroxybenzoate → 2,5-dihydroxybenzoate (3-hydroxybenzoate-6-hydroxylase) (Gao et al. 2005). d. 4-Hydroxybenzoate → 3,4-dihydroxybenzoate (4-hydroxybenzoate-3-hydroxylase) (Entsch and Ballou 1989).

109

Mechanistic Aspects OH

CO2 H

OH

OH (a)

CO2 H

OH

OH

OH

(b)

FIGURE 3.9 Monoxygenation of (a) salicylate and (b) 4-hydroxybenzoate. CO2 H

CO2 H

OH

OH (a) HO

CO2 H NH2 CO2 H NH2

(b)

HO CO2 H OH

(c) OH CO2 H

CO2 H OH

(d) NH2

H2 N

(e) N

OH

N

OH

OH

FIGURE 3.10 Monooxygenation of (a) salicylate, (b,c) 2-aminobenzoate, (d) 3-aminobenzoate, and (e) 2-hydroxyquinoline.

e. 3-Aminobenzoate → 5-aminosalicylate (3-aminobenzoate-6-hydroxylase) (Figure 3.10d) (Russ et al. 1994). f. Naphth-2-oate → 1-hydroxynaphth-2-oate (Morawski et al. 1997), or by a dioxygenation and elimination. g. Degradation of 4-hydroxybenzoate in Haloarcula sp. D1 proceeds via 2,5-dihydroxybenzoate involving an NIH shift (Fairley et al. 2002). h. 2-Hydroxyquinoline → 2,8-dihydroxyquinoline (Figure 3.10e) (Rosche et al. 1997).

110

Environmental Degradation and Transformation of Organic Chemicals HO 2C

OH

HO 2C

CO 2H

O

O

CH2CO 2H

CO 2H

CO 2H

OH

O

HO

O

FIGURE 3.11

CO 2H

CO 2H

CH2CO 2H

+ CH3CO 2H

CO 2H

CO 2H

The β-ketoadipate pathway.

CO 2 H HO 2 C

CHO

(a)

CO 2H

OH OH

OH

CO 2 H

CO 2 H

(b) OH OH

CH 3− CO −CO 2 H + H − CO 2 H

CHO

CHO

CO 2 H

CO 2 H

OH

CH 3− CO −CO 2 H + CH 3 − CHO

OH

FIGURE 3.12 Biodegradation of 3,4-dihydroxybenzoate mediated by (a) 4,5-dioxygenase in Pseudomonas acidovorans and (b) 2,3-dioxygenase in Bacillus macerans.

Degradation of the products of hydroxylation then involves ission of the catechols (or 2,5dihydroxybenzoates) that are produced. All three ission pathways have been observed for 3,4-dihydroxybenzoate: a. Intradiol 3,4-dioxygenation in Pseudomonas putida and the β-ketoadipate pathway (Figure 3.11). b. Extradiol 4,5-dioxygenation in the Pseudomonas acidovorans group (Figure 3.12a). c. Extradiol 2,3-dioxygenation in species of Bacillus (Figure 3.12b). When 1,4-dihydroxy compounds are produced by monooxygenation, these are degraded by the gentisate pathway (Figure 3.13) mediated by gentisate dioxygenase (Wergath et al. 1998). Monooxygenation of Phenols Phenols Lacking Halogen or Nitro Substituents Monooxygenases generally initiate the degradation of phenols and their ethers: 1. The 4-methoxybenzoate monooxygenase from Pseudomonas putida shows low substrate speciicity. Although it introduces only a single atom of oxygen into 3-hydroxy- and 4-hydroxybenzoate, it accomplishes the conversion of 4-vinylbenzoate into the corresponding side-chain diol (Wende et al. 1989). 2. The metabolism of 4-hydroxybenzoate involves conversion into 3,4-dihydroxybenzoate by a hydroxylase that has been puriied and characterized from a strain of Pseudomonas

111

Mechanistic Aspects H O 2C

CO2H

H O 2C

C O 2H

CO2H C O 2H C O −C O 2H

HO OH

CO −C O 2 H

OH

OH OH

C O 2H

C O 2H

FIGURE 3.13

The gentisate pathway.

luorescens (Howell et al. 1972) and from P. aeruginosa strain PAO1 (Entsch and Ballou 1989). The enzyme is a lavoprotein containing FAD and requires NADPH for activity. 3. The enzymes in a strain of Pseudomonas putida (Arunachalam et al. 1992) and in Escherichia coli strain W (Prieto and Garcia 1994), which introduce an oxygen atom into 4-hydroxyphenylacetate to produce 3,4-dihydroxyphenylacetate, are lavoprotein monooxygenases that require a further protein component (coupling protein) for activity. In the absence of this protein, oxidation of NADH produces H2O2 (Arunachalam et al. 1992). This phenomenon has also been observed with other oxygenases including salicylate hydroxylase, 2,4-dichlorophenol hydroxylase, and 2,4,6-trichlorophenol monooxygenase. 4. Salicylate is an intermediate in the metabolism of PAHs including naphthalene and phenanthrene, and its degradation involves oxidation to catechol. The hydroxylase (monooxygenase) has been extensively studied (references in White-Stevens and Kamin 1972) and in the presence of an analog that does not serve as a substrate, NADH is oxidized with the production of H2O2 (White-Stevens and Kamin 1972). This “uncoupling” is characteristic of lavoenzymes and is exempliied also by the chlorophenol hydroxylase from an Azotobacter sp. that is noted later. 5. The degradation of 2-hydroxybiphenyl by Pseudomonas azelaica HBP1 is initiated by 2-hydroxybiphenyl 3-monooxygenase (Suske et al. 1999). Chlorophenols Monooxygenases carry out the introduction of oxygen, and in the degradation of 2,4,6-trichlorophenol by Ralstonia eutropha (Louie et al. 2002) and Burkholderia cepacia (Gisi and Xun 2003), they are FADH2-dependent (Gisi and Xun 2003). There are two situations that may pragmatically be distinguished: (a) ring ission of the chlorocatechols without direct loss of chlorine and (b) reactions that result in dechlorination before ring ission. Further details are given in Chapter 9, Part 2. 1. The hydroxylase that converts 2,4-dichlorophenol into 3,5-dichlorocatechol (Figure 3.14a) before ring ission has been puriied from a strain of Acinetobacter sp. (Beadle and Smith 1982), and from Alcaligenes eutrophus JMP 134 (Don et al. 1985; Perkins et al. 1990). The reductant is NADPH, the enzyme is a lavoprotein containing FAD, and in the presence of compounds that are not substrates, NADPH and O2 are consumed with the production of H2O2.

112

Environmental Degradation and Transformation of Organic Chemicals OH

OH

OH

Cl

CO 2H CO 2H

(a) Cl

Cl

Cl

HO 2C

O

Cl

O Cl

Cl

HO 2C

HO 2C

O

HO 2C

O

O CO 2H

CO 2H

CO 2H Cl OH

OH

OH

OH

Cl

Cl

Cl

Cl

Cl

OH

Cl

Cl

Cl

Cl

Cl

Cl

OH

(b)

Cl

FIGURE 3.14

OH

OH

OH

Degradation of (a) 3,5-dichlorophenol and (b) pentachlorophenol.

2. A range of mechanisms operates for the degradation of chlorophenols with three or more substituents: a. The irst step in the degradation of pentachlorophenol by Flavobacterium sp. 39732 involves introduction of oxygen at C-4 to produce tetrachlorohydroquinone (Figure 3.14b). The enzyme is not a hydroxylase, but a lavin-containing monooxygenase that can accept a number of halogenated phenols including 2,4,6-triiodophenol (Xun et al. 1992). b. An NADH-requiring chlorophenol monooxygenase from Burkholderia cepacia AC1100 successively dehalogenates 2,4,5-trichlorophenol to 2,5-dichloro-hydroquinone and 5-chloro-1,2,4-trihydroxybenzene (Xun 1996). It is a two-component enzyme, and component A contains FAD and an NADH reductase. c. The enzyme from Azotobacter sp. strain GP1, which catalyzes the formation of 2,6-dichlorohydroquinone from 2,4,6-trichlorophenol, is also a monooxygenase that requires NADH, FAD, and O2 (Wieser et al. 1997). The enzyme is able to accept other chlorophenols with consumption of NADH including 2,4-, 2,6-, 3,4-dichloro-, 2,4,5-trichloro-, and 2,3,4,5- and 2,3,4,6-tetrachlorophenol, and in the absence of a substrate results in unproductive formation of H2O2. d. The monooxygenase involved in the degradation of 2,4,6-trichlorophenol to 6-chloro2-hydroxyhydroquinone by Ralstonia eutropha strain JMP134 combines monooxygenation with hydrolytic activity, and it was shown that oxygen is introduced from both O2 and H2O (Xun and Webster 2004). Nitrophenols Monooxygenation is involved in the degradation of 4-nitrophenol by a strain of Moraxella sp. (Spain and Gibson 1991), and the enzyme appears to be a particulate lavoprotein (Figure 3.15a). In the Gram-positive organisms Arthrobacter sp. (Jain et al. 1994) and Bacillus sphaericus strain JS905 (Kadiyala and Spain 1998), 4-nitrophenol degradation involves initial hydroxylation to 4-nitrocatechol followed by elimination of nitrite with the formation of benzene-1,2,4-triol before ring ission

113

Mechanistic Aspects OH

O

NO 2 O

(a)

(b)

OH

NO 2

OH OH

FIGURE 3.15

CO2H CO2H

OH

O

OH

O

OH

CO2H C HO

OH

OH O

OH

Alternative degradation of 4-nitrophenol.

CH 2 CH(NH 2 )CO 2 N

CH2CO−CO2H

CH2CO−CO2H OH

HO OH

FIGURE 3.16

Hydroxylation of phenylalanine followed by rearrangement to 2,5-dihydroxyphenylpyruvate.

to 3-ketoadipate (Figure 3.15b). A single two-component enzyme that consists of a lavoprotein reductase and an oxygenase carries out the irst two reactions in B. sphaericus. Other Hydroxylations/Monooxygenations 1. Phenylalanine is hydroxylated to tyrosine and then sequentially to 4-hydroxyphenylpyruvate and by dioxygenation and rearrangement to 2,5-dihydroxyphenylpyruvate (Figure 3.16) (Arias-Barrau et al. 2004). Hydroxylation involves 6,7-dimethyltetrahydrobiopterin that is converted into the 4a-carbinolamine (Song et al. 1999). Copper is not a component of the active enzyme, although there is some disagreement on whether or not Fe is involved in the reaction for the hydroxylase from Chromobacterium violaceum (Chen and Frey 1998). 2. The enzyme in Rhodococcus sp. strain IGTS8 that brings about successive oxidation of dibenzothiophene to the sulfoxide and the sulfone is a lavin mononucleotide–dependent monooxygenase that carries out both reactions by sequential incorporation of a single atom of oxygen from O2 (Lei and Tu 1996). 3. The transformations of α- and β-endosulfan with the elimination of sulite are carried out by lavin-dependent monooxygenation in Mycobacterium sp. (Sutherland et al. 2002) and Arthrobacter sp. (Weir et al. 2006).

CYTOCHROME P450 SYSTEMS These are found in bacteria, fungi, and yeasts, and mediate important hydroxylations. Reference should be made to reviews that discuss mechanistic aspects of cytochrome P450 reactions (Guengerich 1990), the reactions mediated by both eukaryotic and prokaryotic cytochrome

114

Environmental Degradation and Transformation of Organic Chemicals Class I

Class II

Two-component enzyme of eukaryotic organisms (1)

NADPH reductase containing FAD and FMN

(2)

Monooxygenase

Three-component system of prokaryotic systems (1)

NADP reductase containing FAD

(2)

Ferrodoxin

(3)

Monooxygenase

FIGURE 3.17 Cytochrome P450 systems in prokaryotes and eukaryotes. (From Neilson, A.H. and Allard, A.-S. Microbial metabolism of PAHs and heteroarenes, The Handbook of Environmental Chemistry, Vol. 3J, pp. 1–80, Springer, 1998. With permission.)

P450 systems (Sariaslani 1991), their widespread role in the transformation of xenobiotics (Smith and Davis 1968), and their occurrence and activities in yeasts (Käppeli 1986). The essential features of prokaryotic and eukaryotic cytochrome P450 systems are compared in Figure 3.17. Heme oxygenase that carries out the degradation of heme after transport into the cell is important in a range of organisms, and some opportunistic pathogenic yeasts and bacteria have an enhanced requirement for Fe that can be satisied by heme. In Gram-negative bacteria, heme is bound to outer membrane receptors and transported into the cell by the energy-transducing system TonB-ExcBExbD (Andrews et al. 2003; Wandersman and Delepelaire 2004). Heme oxygenases that have been designated HemO, HmuO, IsdG/I, and ChuZ mediate the degradation of heme with the release of Fe using an NADPH-cytochrome P450 reductase and three successive oxygenations: (a) hydroxylation at the α-meso position by the terminal oxygen of intermediate [Fe3+–O–OH], (b) release of CO and the production of verdoheme, and (c) further oxygenation to linear biliverdin with the release of Fe. Heme oxygenase has been identiied in a number of pathogenic bacteria including Corynebacterium diphtheriae (Wilks and Schmitt 1998), Staphylococcus aureus (Skaar et al. 2004), species of Neisseria (Zhu et al. 2000), enterohemorragic Escherichia coli O157:H7 (Suits et al. 2005), and Campylobacter jejeuni (Ridley et al. 2006). In Pseudomonas aeruginosa, there are two heme oxygenases that differ at the sites of the heme that are initially hydroxylated to produce biliverdins IXβ and IXδ (Wegele et al. 2004). Although reaction with dioxygen of both cytochrome P450 and heme oxygenase involves the formation of a hydroperoxy Fe3+, the subsequent reactions are different, and activation of heme oxygenase is carried out by a nearby water molecule (Matsui et al. 2005). Further comments in the context of Fe utilization are given in Part 5 of this chapter. Prokaryotic Organisms The functioning of cytochrome P450 involves both oxygenation and reduction reactions (Tyson et al. 1972), and this is consistent with its role in both hydroxylation and reductive transformations. This activity is widely distributed among both Gram-negative and Gram-positive organisms, and mediates a number of important degradations and transformations including hydroxylations at quaternary carbon atoms. Cytochrome P450 systems in actinomyces have been reviewed (O′Keefe and Harder 1991), and the systematic nomenclature of some important bacterial cytochrome P450 systems has been given (Munro and Lindsay 1996). The diversity of reactions that are catalyzed by this system is illustrated by the following examples: 1. Hydroxylation of n-octane by cell extracts of Gordonia (Corynebacterium) sp. strain 7E1C (Cardini and Jurtshuk 1968), and of some strains of Acinetobacter calcoaceticus induced with n-hexadecane (Asperger et al. 1981). 2. Hydroxylation of long-chain carboxylic acids, amides, and alcohols—but not the esters or the corresponding alkanes—at the ω-1, ω-2, and ω-3 positions by a soluble enzyme system from Bacillus megaterium (Miura and Fulco 1975; Narhi and Fulco 1986, 1987).

115

Mechanistic Aspects

3. The transformation of benzene, toluene, naphthalene, biphenyl, and benzo[a]pyrene to the corresponding phenols (Trower et al. 1989) by Streptomyces griseus, and of phenanthrene by Streptomyces lavovirens to (−)trans-[9S,10S]-9,10-dihydrodihydroxyphenanthrene with minor amounts of 9-hydroxyphenanthrene (Sutherland et al. 1990). 4. The initial hydroxylation in the degradation of some terpenes: the ring methylene group of camphor by Pseudomonas putida (Katagiri et al. 1968; Tyson et al. 1972; Koga et al. 1986), and the isopropylidene methyl group of linalool by a strain of P. putida (Ullah et al. 1990). 5. When the 5 and 6 positions of camphor are blocked by substituents, hydroxylation at other positions may take place. For example, the quaternary methyl group of 5,5-diluorocamphor is hydroxylated to the 9-hydroxymethyl compound (Figure 3.18a) (Eble and Dawson 1984). 6. The cytochrome P450cam is able to bring about the stereoselective epoxidation of cismethylstyrene to the (1S,2R) epoxide (Ortiz de Montellano et al. 1991). 7. Adamantane (A) and adamantan-4-one (B) were speciically hydroxylated at the quaternary C-1 by cytochrome P450cam to produce C and D. In contrast, the eukaryotic cytochrome P450LM2 formed in addition to the C-2 compound from adamantane, and both 5-hydroxyadamantan-1-one (D) and the 4-anti-hydroxyadamantan-1-one (E) from adamantan-4-one (Figure 3.18b) (White et al. 1984). 8. The hydroxylation of cyclohexane by a strain of Xanthobacterium sp. (Trickett et al. 1990). In cell extracts, a range of other substrates was oxidized including cyclopentane, pinane, and toluene (Warburton et al. 1990). 9. Hydroxylation of progesterone and closely related compounds at the 15-β position by cell extracts of Bacillus megaterium (Berg et al. 1976). 10. The irst step in the aerobic degradation of dehydroabietic acid by Pseudomonas abietaniphila strain BMKE-9 is hydroxylation at C-7 (Smith et al. 2004). 11. The reductive dehalogenation of polyhalogenated methanes (Castro et al. 1985) and polyhalogenated ethanes (Li and Wackett 1993) by Pseudomonas putida strain PpG786.

OH

(a)

O

O F

F

F

F

OH

(b)

A

B

O

C OH

OH

OH

D

FIGURE 3.18

O

E

O

Hydroxylation of (a) 5,5-diluorocamphor, (b) adamantane (A) and adamantan-4-one (B).

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Environmental Degradation and Transformation of Organic Chemicals

12. The oxidation of t-butyl methyl ether to t-butanol (Steffan et al. 1997), which is also mediated by the cytochrome P450 from camphor-grown Pseudomonas putida CAM, but not by that from Rhodococcus rhodochrous strain 116. 13. Initiation of the degradation of morpholine by a strain of Mycobacterium strain RP1 (Poupin et al. 1998), and additionally of pyrrolidine and piperidine. 14. The degradation of bisphenol-A by Sphingomonas sp. strain AO1 is initiated by hydroxylation to intermediates that undergo ission to 4-hydroxyacetophenone and 4-hydroxybenzoate. The components have been puriied, and consist of cytochrome P450, ferredoxin reductase, and ferredoxin (Sasaki et al. 2005). 15. The transformation of sulfonylureas by Streptomyces griseolus grown in a complex medium containing glucose when the methyl group of the heterocyclic moieties is hydroxylated, and for some substrates, subsequently oxidized to the carboxylic acid (Romesser and O′Keefe 1986; O′Keefe et al. 1988). 16. The dealkylation of S-ethyl dipropylthiocarbamate and atrazine by a strain of Rhodococcus sp. (Nagy et al. 1995a,b), and of 2-ethoxyphenol and 4-methoxybenzoate by Rhodococcus rhodochrous (Karlson et al. 1993). In R. erythropolis NI86/21, however, the thcF gene involved in the degradation of thiocarbamate herbicides is a nonheme haloperoxidase that does not occur in other strains of rhodococci that can degrade thiocarbamates (de Schrijver et al. 1997): this speciicity occurs also for the cytochrome P450 system encoded by the thcRBCD genes (Nagy et al. 1995a,b). Unusual aspects of bacterial cytochrome P450 systems are worth pointing out: a. The induction in B. megaterium by barbiturates, and the fact that the enzyme is unusual in having a single 119 kD protein-coupling NADH reduction to oxygenation (Narhi and Fulco 1986). b. The induction of the enzyme in S. griseus by genistein (5,7,4′-trihydroxyisolavone) contained in the soybean lour that is used as the growth medium (Trower et al. 1989). c. Cytochrome P450 systems may be both substrate- and organism-speciic, and multiple forms of the enzyme can be produced in the same organism. Eukaryotic Organisms Cytochrome P450 hydroxylation activity is well established in eukaryotic yeasts and some fungi, and this hydroxylation activity has attracted attention in various contexts. 1. The initial oxidation of aliphatic hydrocarbons and amines by yeasts (references in Käppeli 1986). The enzyme designated cytochrome P450aO is induced in organisms including species of Candida and Endomycopsis during growth with alkanes, and therefore differs from the enzyme (P45014DH) synthesized during the growth of saccharophilic yeasts under conditions of low oxygen concentration. 2. The aryl hydroxylase of Saccharomyces cerevisiae that transforms benzo[a]pyrene to the 3- and 9-hydroxy compounds, and the 7,8-dihydrodiol (King et al. 1984). 3. In fungi that serve as models for mammalian transformation of xenobiotics (Ferris et al. 1976; Smith and Rosazza 1983). 4. The hydroxylation of steroids at various positions is carried out by a range of fungi, and probably involves the cytochrome P450 system (Breskvar and Hudnik-Plevnik 1977). The removal of angular methyl groups is important in the transformation of steroids and related compounds. In these reactions, the methyl group is oxidized to the aldehyde before ission in which the carbonyl group oxygen is retained in formate (or acetate), and one oxygen atom from dioxygen

117

Mechanistic Aspects

is incorporated into the hydroxyl group. A group of formally analogous reactions using 18O2 has conirmed the mechanisms: 1. The oxidative removal of the 14α-methyl group in lanosterol by Saccharomyces cerevisiae with concomitant production of the ∆14–15 bond (Aoyama et al. 1984, 1987) and loss of formate (Figure 3.19a) is plausibly facilitated by formation of the conjugated 8-9,14-15-diene. The enzyme designated cytochrome P45014DM is induced under “semianaerobic” conditions during growth with glucose, and is different from both the P450aO enzyme and from P45022DS that brings about ∆22-dehydrogenation (Hata et al. 1983). The mechanism has been examined in a constructed strain containing the 14α-demethylase from Candida albicans and involves reaction of the carbonyl group with FeIII–O–OH (Shyadehi et al. 1996). 2. The conversion of androgens into estrogens involves removal of the C10 methyl group and aromatization of the A ring of ∆4,5-3-ketosterols. This is accomplished by oxidation to the C10 methyl group to the aldehyde, followed by loss of formate and aromatization of the ring to a 3-hydroxy-desmethylsterol (Figure 3.19b) (Stevenson et al. 1988). 3. Cytochrome P45017a carries out comparable reactions for removal of the C17 side chain of pregnenolone, and two reactions have been described both of which involved loss of acetate—17α-hydroxylation and formation of the 17-keto compound, and direct formation of the ∆16,17-ene (Figure 3.19c) (Akhtar et al. 1994). Most eukaryotic organisms such as yeasts and fungi contain peroxisomes, and the degradation of long-chain alkanes by yeasts is carried out in two separate organelles: hydroxylation to alkanols in microsomes (Käppeli 1986), and oxidation to the alkanoic acid CoA-esters that are further metabolized in peroxisomes. Peroxisomes are induced during growth with alkanes and

(a)

C

+ H−CO2H

D CHO CHO

(b)

A

B

+

O

O

COCH3

O

OH COCH3 (c)

C

H−CO2H

HO

+

CH3 CO2 H

D

+

CH3 CO2 H

FIGURE 3.19 Cytochrome P450 monooxygenation of (a) lanosterol, (b) aromatization of ∆4,5-3-ketosterols, and (c) pregnenolone.

118

Environmental Degradation and Transformation of Organic Chemicals

are multipurpose organelles. Some of the salient features include the following (Tanaka and Ueda 1993), which differ from the pathway for bacterial degradation of alkanoic acids: 1. In Candida sp., degradation of the CoA-alkanoic esters to the alkenoic acid esters is catalyzed by an acyl-CoA oxidase and results in the production of H2O2 that is converted into O2 by catalase activity. The enzyme from C. tropicalis contains FAD (Jiang and Thorpe 1983), and in C. lipolytica carries out a stereospeciic antielimination of hydrogen (Kawaguchi et al. 1980). 2. A bifunctional enol-CoA hydratase and 3-hydroxyacetyl-CoA dehydrogenase are used in the degradation of CoA-alkenoic esters to the β-keto acid. This is then degraded to acetylCoA and the lower alkanoate ester by 3-ketoacetyl CoA thiolase and acetyl-CoA thiolase. 3. With the exception of the acetyl-CoA thiolase, all these enzymes are located exclusively in the peroxisomes, whereas the enzymes that are involved in lipid synthesis are found in the microsomes and the mitochondrion.

DIOXYGENATION Dioxygenases Involved in Dihydroxylation of Arenes The aerobic degradation of aromatic compounds involves the introduction of oxygen into the rings as a prelude to ring ission. The most common initial reaction is dioxygenation in which both atoms of oxygen are introduced to produce cis-dihydrodiols. Catechols are formed from these either by dehydrogenation or by elimination of substituents before further dioxygenation and ission of the ring. The biochemistry, enzymology, and genetics have been enunciated in great detail. The following overview attempts to bring together the reactions for many of the compounds that are discussed in the appropriate parts of Chapter 8. Group I The dioxygenases that catalyze the initial introduction of molecular oxygen into aromatic hydrocarbons have been extensively studied, and are multicomponent enzymes that generally carry out three functions: (a) reduction of NAD by a reductase, (b) electron transport by a ferredoxin and transfer of electrons onto the substrate simultaneously with (c) the introduction of oxygen by a terminal oxygenase. In contrast, there are a number of two-component dioxygenases that consist of only a reductase and an oxygenase. These contain a lavin cofactor and a [2Fe–2S] center, but lack the ferredoxin component that is invariably required for aromatic hydrocarbon dioxygenation. Examples of these two-component dioxygenases include a. 4-sulfobenzoate-3,4-dioxygenase (Locher et al. 1991a), 2-aminobenzoate-1,2-dioxygenase (Mampel et al. 1999); b. o-phthalate 4,5-dioxygenase (Batie et al. 1987); c. benzoate 1,2-dioxygenase (Yamaguchi and Fujisawa 1982); d. 4-chlorophenylacetate-3,4-dioxygenase from Pseudomonas sp. strain CBS32 (Schweizer et al. 1987); e. 3-chlorobenzoate 3,4-dioxygenase (Nakatsu et al. 1995); f. 2-halobenzoate 1,2-dioxygenase in Pseudomonas cepacia strain 2CBS (Fetzner et al. 1992). The corresponding dioxygenase from Pseudomonas aeruginosa 142 is, however, a threecomponent enzyme (Romanov and Hausinger 1994). The main classes of bacterial dioxygenases have already been outlined in Figure 3.1. Generally the cis-dihydrodiols are dehydrogenated to the corresponding catechol. In some, dehydrogenation is not required and elimination of CO2H, NH3, Hal−, NO2−, and SO32− or exceptionally OH produces catechols directly. These are assigned to group II.

119

Mechanistic Aspects

Group II In these reactions, dehydrogenation is not required and formation of the catechol is attained with concomitant elimination of CO2, NH3, NO2−, SO32−, or halide (Figure 3.20). Illustrative examples include the following: 1. a. Amine groups in the conversion of aniline into catechol (Bachofer and Lingens 1975; Fukumori and Saint 1997). b. Both amine and carboxyl groups in the conversion of anthranilic acid into catechol by anthranilate dioxygenase (Eby et al. 2001; Chang et al. 2003; Taniuchi et al. 1964). c. 2-Aminobenzenesulfonate to catechol-3-sulfonate and ammonia (Mampel et al. 1999). However, that there are also anthranilate monooxygenases that have already been noted. 2. a. Carboxyl groups in the conversion of benzoate into catechol by benzoate dioxygenase (Neidle et al. 1991). b. The degradation of 4-methyl-o-phthalate by P. luorescens strain JT701 takes place by analogous oxidative decarboxylation with the formation of 4-methyl-2,3-dihydroxybenzoate (Ribbons et al. 1984), and of terephthalate (p-phthalate) to 3,4-dihydroxybenzoate and CO2. 3. Chloride during the conversion of 1,2,4,5-tetrachlorobenzene into 3,4,6-trichlorocatechol (Sander et al. 1991), and both chloride and carboxyl during the degradation of 2-chlorobenzoate (Fetzner et al. 1992; Romanov and Hausinger 1994). 4. Fluoride during the conversion of 3-luorotoluene into 3-methylcatechol (Renganathan 1989), and of both luoride and carboxyl during the degradation of 2-luorobenzoate (Engesser et al. 1980). 5. Nitrite during conversion of 2-nitrotoluene into catechol (An et al. 1994), 2,4-dinitrotoluene into 4-nitrocatechol (Spanggord et al. 1991), and 1,3-dinitrobenzene to 4-nitrocatechol (Dickel and Knackmuss 1991). 6. Sulite during the conversion of naphthalene-1-sulfonate into 1,2-dihydroxynaphthalene (Kuhm et al. 1991), and 4-carboxybenzenesulfonate into 3,4-dihydroxybenzoate (4-carboxycatechol) (Locher et al. 1991). Phenols may exceptionally be formed by spontaneous loss of H2O, and this is apparently favored by the presence of the electron-attracting substituents in 4-nitrotoluene, pyridine, quinoline, and indole. a. Degradation of o-xylene by Rhodococcus sp. DK17 is initiated by the formation of an unstable o-xylene cis-3,4-dihydrodiol. This may be dehydrogenated to 3,4-dimethylcatechol followed by extradiol ring ission, or undergo dehydration to produce 2,3- and 3,4-dimethylphenol (Figure 3.21a) (Kim et al. 2004). X

OH

X = Cl,

NH 2 ,

OH H

SO 3 H

OH OH

O HO

C

OH OH Y

Y = H, Cl, NH 2 , F

FIGURE 3.20 Dioxygenation with concomitant loss of substituents.

120

Environmental Degradation and Transformation of Organic Chemicals C H3 CH3 C H3

C H3

OH C H3

CH3 (a)

OH

OH OH

H

OH

OH

H

C H3 + CH3

CH3 CH3

CH3

CH3

CH3 OH

OH

H H

(b) N

N

C H3

N

OH

CH3

C H3

C H3 OH

OH

OH

H H

(c)

OH

OH NO2

N O2

NO2

NO 2

OH OH NH2

N OH H H OH

(d) N H

OH N H

H H

OH

N H

OH

FIGURE 3.21 (a) Degradation of 1,2-dimethylbenzene by dioxygenation and elimination with formation of dimethylphenols, (b) dioxygenation of 4-methylpyridine followed by elimination to 3-hydroxy-4-methylpyridine, (c) dioxygenation of 4-nitrotoluene followed by dehydrogenation or elimination, and (d) degradation of carbazole by dioxygenation followed by elimination.

b. 4-Methylpyridine → 3-hydroxy-4-methylpyridine by dioxygenation and spontaneous dehydration (Figure 3.21b) (Sakamoto et al. 2001). c. 4-Nitrotoluene → 2-methyl-5-nitrophenol + 3-methyl-6-nitrocatechol (Figure 3.21c) (Robertson et al. 1992). d. Quinoline → 3-hydroxyquinoline (Boyd et al. 1987). e. Quinol-2-one → 8-hydroxyquinol-2-one (Rosche et al. 1995). f. Degradation of carbazole by dioxygenation (Figure 3.21d) (Gieg et al. 1996).

Mechanistic Aspects

121

Arene hydrocarbon dioxygenases are capable of carrying out a number of reactions other than the introduction of both atoms of oxygen into the substrate. Illustrative examples of monooxygenation carried out by dioxygenases include the following: 1. Although naphthalene dioxygenase is enantiomer-speciic in producing the (+)-cis-(1R,2S)dihydrodiol, it also possesses dehydrogenase and monooxygenase activities (Gibson et al. 1995), so that monooxygenase and dioxygenase activities are not exclusive. a. Naphthalene dioxygenase carried out dioxygenation of indene to cis-(1R,2S)-indandiol, monooxygenation to 1S-indenol, and in addition dehydrogenation of indane to indene (Lee et al. 1997). b. Toluene is oxidized by puriied naphthalene dioxygenase from Pseudomonas sp. strain NCIB 9816-4 to benzyl alcohol and benzaldehyde, and ethylbenzene to (S)-1-phenylethanol and acetophenone. Whereas the initial reactions involve monooxygenation, oxidation to the aldehyde and ketone are dioxygen-dependent (Lee and Gibson 1996). c. Toluene dioxygenase from Pseudomonas putida strain F1 and chlorobenzene dioxygenase from Burkholderia sp. strain PS12 are involved in the degradation of toluene and chlorobenzene. In addition, they can carry out monooxygenation of 2- and 3-chlorotoluene by side chain oxidation to produce the corresponding benzyl alcohols that were slowly oxidized further (Lehning et al. 1997). 2. Naphthalene dioxygenase from P. putida strain F1 is able to oxidize a number of halogenated ethenes, propenes, and butenes, and cis-hept-2-ene and cis-oct-2-ene (Lange and Wackett 1997). Alkenes with halogen and methyl substituents at double bonds form allyl alcohols, whereas those with only alkyl or chloromethyl groups form diols. There are some metabolic similarities between naphthalene dioxygenase and 2,4-dinitrotoluene dioxygenase from Burkholderia sp. strain DNT, and it has been suggested that these enzymes may have a common ancestor (Suen et al. 1996). Protein sequences among biphenyl dioxygenases may be similar or identical, in spite of distinct differences in the range of PCB congeners that are attacked (Kimura et al. 1997; Mondello et al. 1997). The roles of the α- and β-subunits of the terminal dioxygenase (ISP) have been examined in more detail with divergent conclusions: a. Using enzymes from hybrid naphthalene dioxygenase and 2,4-dinitrotoluene dioxygenase genes introduced into Escherichia coli (Parales et al. 1998). Although the rates were different for the wild-type and hybrid enzymes, the products and the enantiomeric speciicities were the same for each. It was shown that whereas the β-subunit of the dioxygenase was necessary for activity, it was the large α-subunit containing a Rieske [2Fe–2S] center that determined substrate speciicity. b. Chimeras were constructed from the α- and β-subunits of the terminal dioxygenase proteins ISPBPH (Hurtubise et al. 1998) from two strains of PCB-degrading strains, Comamonas testosteroni strain B-356 and Pseudomonas sp. strain LB400. The enzymes were puriied, and the substrate speciicities of the puriied enzymes showed that the structures of both subunits inluenced the speciicities. c. The function of the β-subunit that contains no detectable prosthetic groups is not fully understood, although the Tod C2 subunit is needed to obtain catalytic activity of the α-subunit (Tod C1) in Pseudomonas putida F1 (Jiang et al. 1999). It is clear from the preceding comments that there is no absolute distinction between the oxygenase activities mediated by dioxygenases. This is even less clear for heteroarenes than it is for carbocyclic compounds. An illustrative example is provided by Pseudomonas putida strain 86 in which 8-hydroxy-quinol-2-one is produced from quinol-2-one (Rosche et al. 1997).

122

Environmental Degradation and Transformation of Organic Chemicals

The enzyme system consists of a reductase that transfers electrons from NADH and contains FAD and a [2Fe–2S] ferredoxin, and a high-molecular-weight oxygenase consisting of six identical subunits and six Rieske [2Fe–2S] clusters. It was suggested that this complex belonged to class IB oxygenases that include benzoate-1,2-dioxygenase. It is therefore possible that this apparent monooxygenase is, in fact, a dioxygenase introducing oxygen at the 8,8a positions followed by elimination (Rosche et al. 1995). The formation of 1-hydroxynaphthalene-2-carboxylate from naphthalene-2-carboxylate was apparently not via (1R,2S)-cis-1,2-dihydro-1,2-dihydroxynaphthalene-2-carboxylate (Morawski et al. 1997). This could have taken place either by monooxygenation that is supported by the activity of naphthalene dioxygenase in which both activities are catalyzed by the same enzyme (Gibsonet al. 1995), or by an elimination that has already been noted. Exceptionally, an acyl chloride that is spontaneously hydrolyzed to the carboxylic acid may be formed: a. Pseudomonas putida strain GJ31 is able to grow with both toluene and chlorobenzene. Degradation of chlorobenzene proceeds by formation of the dihydrodiol and dehydrogenation to 3-chlorocatechol. This is degraded by a catechol 2,3-dioxygenase (extradiol or proximal) to produce the acyl chloride that is hydrolyzed to 2-hydroxymuconate (Figure 3.22a) (Mars et al. 1997; Kaschabek et al. 1998). b. The degradation of γ-hexachlorocyclohexane by Sphingomonas paucimobilis UT 6 takes place by several steps that result in the production of 2-chlorohydroquinone (Endo et al. 2005; Miyauchi et al. 2002). This is degraded by dioxygenation to an acyl chloride that is hydrolyzed to maleylacetate (Figure 3.22b) (Miyauchi et al. 1999). c. Sphingomonas chlorophenolica ATCC 39723 degrades pentachlorophenol in a series of steps to 2,6-dichlorohydroquinone that undergoes dioxygenation to an acyl chloride that is hydrolyzed to 2-chloromaleylacetate (Figure 3.22c) (Xun et al. 1999; Ohtsubo et al. 1999).

Cl

Cl

OH (a)

COCl CO2 H

CO2 H CO2 H

CO2 H CO2 H

OH

O

O

OH

Cl Cl

OH Cl

CO2 H COCl

Cl

(b) Cl

Cl Cl

OH

OH OH

OH Cl

Cl

Cl

Cl

Cl

Cl

Cl

(c)

Cl

CO2 H COCl

CO2 H CO2 H

H

H OH

Cl

OH

O

FIGURE 3.22 Degradation involving dioxygenation via acyl chlorides of (a) chlorobenzene, (b) γ- hexachlorocyclohexane, and (c) pentachlorophenol.

123

Mechanistic Aspects

Ring-Fission Dioxygenases After dioxygenation and the formation of catechols, ring ission is mediated by a different group of dioxygenases. Group I Catechols and 2-Aminophenols

There are three possibilities, each of which has been realized (Figure 3.23), and the choice among them depends both on the substituents and on the organism. 1. Intradiol (or ortho) ission by catechol 1,2-dioxygenase breaks the bond between the atoms bearing the hydroxyl groups: a. Catechol 1,2-dioxygenase contains Fe(III), and lacks heme and sulfur–iron components. The protein consists of α- and β-subunits with masses of 30 and 32 in the combinations (α,β), (α,α), or (β,β), and the molecular mass of the enzyme is 63 kD. b. 3,4-Dihydroxybenzoate-3,4-dioxygenase is an Fe(III) protein and consists of an aggregate of α- and β-subunits with masses of 22.2 and 26.6 in an (α,β)12 structure with a molecular mass of 587. 2. Extradiol (or meta) ission by catechol 2,3-dioxygenase breaks the bond between one of the hydroxyl groups and the adjacent nonhydroxylated carbon atom. Extradiol 2,3-ission enzymes have been divided into three major classes (Table 3.1) (Spence et al. 1996; Peng et al. 1998). OH OH

Cl

(a)

(c)

(b) OH CO 2 H CHO

OH

Cl

FIGURE 3.23 and (c) distal.

CO 2 H CO 2 H Cl

CO 2 H COCl

Alternative dioxygenation pathways for 3-substituted catechols: (a) extradiol, (b) intradiol,

TABLE 3.1 Classes of Extradiol Dioxygenases Class I II

III

Organism Rhodococcus globerulus P6 Burkholderia cepacia LB 400 Pseudomonas pseudoalcaligenes KF 707 Pseudomonas sp. KKS 102 Sphingomonas paucimobilis SYK 6 Pseudomonas sp. CA 10 Escherichia coli C Escherichia coli Alcaligenes eutrophus JMP 222 Sphingomonas paucimobilis SYK 6

Substrate for Dioxygenation 2,3-Dihydroxybiphenyl 2,3-Dihydroxybiphenyl 2,3-Dihydroxybiphenyl 2,3-Dihydroxybiphenyl 3,4-Dihydroxybenzoate 4,5-dioxygenase 2′-Amino-2,3-dihydroxybiphenyl 3,4-Dihydroxyphenylacetate 2,3-dioxygenase 2,3-Dihydroxyphenylpropionate Catechol 2,3-dioxygenase I 2,2′,3-Trihydroxy-3′-methoxybiphenyl-5,5′-dicarboxylate

124

Environmental Degradation and Transformation of Organic Chemicals R= R

R

O O

R

O

O

O

CH 2 CH(NH 2 )CO 2 H COR

O

(a) N

N H OH

O

(b) OH O

O OH

O

N H

NHCHO

OH O

CO 2 H

O OH

CO 2 H

O

FIGURE 3.24

Dioxygenation of (a) catechol and (b) tryptophan.

3. Distal ission: Although substituted catechols generally undergo extradiol ission, this may produce toxic metabolites, and can be circumvented by regioselective 1,6-dioxygenation. This is rather uncommon but it has been observed in a number of degradations: a. 2-Aminophenol mediated by a 1,6-dioxygenase in Pseudomonas pseudoalcaligenes JS 45 (Lendenmann and Spain 1996) and in Comamonas CNB-1 (Wu et al. 2005). b. 3-Chlorocatechol by Sphingomonas xenophaga BN6 (Riegert et al. 2001) and 3-luorobenzoate by strain FLB300 (that does not belong to the genus Pseudomonas) (Engesser et al. 1990; Schreiber et al. 1980). 4. Tryptophan dioxygenase that mediates the conversion of tryptophan into N-formylkynurenine, contains noncovalently bound heme, and is active in the Fe(II) form. Oxygenation is initiated at C3 with the subsequent formation of a dioxetane that decomposes into products (Figure 3.24a) (Leeds et al. 1993). The reaction may formally be considered analogous to catechol extradiol ission dioxygenation (Figure 3.24b). 5. There are a few extradiol-ission dioxygenases that are dependent on metals other than Fe. Magnesium

3,4-Dihydroxyphenylacetate extradiol dioxygenase from Klebsiella pneumoniae strain M5a1 contains magnesium and is not activated by Fe2+ (Gibello et al. 1994). Manganese

a. The 3,4-dihydroxyphenylacetate-2,3-dioxygenase from Arthrobacter globiformis (Boldt et al. 1995) and the 2,3-dihydroxybiphenyl-1,2-dioxygenase from Bacillus brevis strain JFG8 (Que et al. 1981) are Mn(II) enzymes, and are neither activated by Fe(II) nor rapidly inhibited by H2O2. b. The 2,3-dihydroxybiphenyldioxygenase from Bacillus sp. strain JF8 that mediated ission of the biphenyl ring is unusual in being Mn(II)-dependent, and differs in structure from those of Burkholderia sp. strain LB400 and Pseudomonas paucimobilis strain KF707 (Hatta et al. 2003). Copper

This is an unusual component of dioxygenases but is contained in the dioxygenase from Aspergillus japonicus that brings about ission of the C ring of quercitin with the formation of carbon monoxide (Steiner et al. 2002). However, although copper can be bound quite tightly to tryptophan 2,3-dioxygenase, the evidence suggests that it probably does not play a role in the catalytic activity of the enzyme (Ishimura et al. 1980).

Mechanistic Aspects

125

Group II Hydroxybenzoates

The second large group of ring-ission dioxygenases are used for the degradation of ortho-dihydroxybenzoates including, 2,3-, 3,4-, and 4,5-dihydroxybenzoate. As for simple catechols, ission may be either intradiol or extradiol, and the choice between them depends on the organism: a. The 3,4-dihydroxybenzoate dioxygenase in Pseudomonas putida mediates intradiol ission to a muconic acid by an Fe(III) enzyme (Bull and Ballou 1981). b. The 3,4-dihydroxybenzoate in Pseudomonas testosteroni mediates extradiol ission to a muconic semialdehyde by an Fe(II) enzyme (Arciero et al. 1983). Group III Other Dioxygenases

This comprises a heterogeneous group of enzymes that is used for the degradation of substrates including gentisate, salicylate, and 1-hydroxynaphthalene-2-carboxylate by pathways that do not involve catechols: 1. 2,5-Dihydroxybenzoate (gentisate) 1,2-dioxygenase brings about ring ission between the carboxyl and hydroxyl groups, and produces maleylpyruvate without loss of the carboxyl group (Figure 3.13) (Harpel and Lipscomb 1990). It belongs to a different class of ringcleaving dioxygenases from those that have already been described, since the protein sequences of the gene product from Sphingomonas sp. strain RW5 revealed little or no similarities to those of either intradiol or extradiol dioxygenases (Wergath et al. 1998; Hintner et al. 2001). In contrast, the degradation of the analogous salicylate proceeds by hydroxylation to catechol with loss of carboxyl, followed by ring ission of the catechol. 2. There are a few dioxygenases that carry out ission of aromatic rings and do not have vicinal hydroxyl groups: a. The dioxygenase from Nocardioides sp. strain KP7 brings about ring ission of 1-hydroxynaphthalene-2-carboxylate to 2′-carboxybenzalpyruvate, and is different from the dioxygenases that catalyze ring ission of catechols (Iwabuchi and Harayama 1998b). b. The dioxygenase from Pseudaminobacter salicylatoxidans is able to carry out direct ring ission of salicylates with a range of substituents including chlorine and bromine without the formation of intermediate catechols (Hintner et al. 2004). The deduced amino acid sequence encoded a protein to which the highest degree of similarity was found in a presumptive gentisate 1,2-dioxygenase. Whereas the ring ission products from 3-halosalicylates underwent decarboxylation to 6-halo-2-keto-3,5-hexa-dienoates, the corresponding products from 5-halosalicylates were lactones that were hydrolyzed to 4-hydroxy-2-keto-3,5-hexadiendioates. 3. The dioxygenase that brings about the degradation of 2-methyl-3-hydroxypyridine-5-carboxylate to α-(N-acetylaminomethylene)succinic acid (Sparrow et al. 1969). 4. The dioxygenase that catalyzes the degradation of 2,5-dihydroxypyridine to maleamate and formate (Gauthier and Rittenberg 1971). Group IV There is a rather large and important group of dioxygenases that do not bear any similarity to the dioxygenases already described: 1. One important group is dependent on Fe2+ and 2-ketoglutarate from which succinate and CO2 are produced concomitant with dioxygenation: a. The degradation of 2,4-dichlorophenoxyacetate by Alcaligenes eutrophus strain JMP134 involves initial formation of 2,4-dichlorophenol and glyoxylate. This is

126

Environmental Degradation and Transformation of Organic Chemicals

accomplished by a dioxygenase that couples this reaction to the conversion of 2-ketoglutarate into succinate and CO2 (Fukumori and Hausinger 1993a) (Figure 3.25a). The enzyme has been puriied and characterized, and is able to accept other phenoxyacetates including 2,4,5-trichlorophenoxyacetate and 2-chloro-4-methylphenoxyacetates (Fukumori and Hausinger 1993b). In Burkholderia spp. that also degraded 2,4-dichlorophenoxyacetate by this pathway, the sequence of the chromosomal gene tfdA was, however, only 77.2% homologous to the plasmid-borne gene of A. eutrophus strain JMP 134. In contrast, it shared a 99.5% identity with the chromosomal gene from another strain of Burkholderia sp. from a geographically distinct area (Matheson et al. 1996). In Sphingomonas herbicidovorans, the 2-ketoglutaratedependent dioxygenase converted 4-chloro-2-methylphenoxypropionate (mecoprop) into 4-chloro-2-methylphenol, pyruvate, and succinate each of which were formed with incorporation of one atom of O2 (Nickel et al. 1997). b. A formally analogous reaction mediated by a dioxygenase is involved in the intramolecular dioxygenation of 4-hydroxyphenylpyruvate to 2,5-dihydroxyphenylacetate (Lindblad et al. 1970) in which both the 2-hydroxyl and the carboxylate oxygen atoms are derived from O2 (Figure 3.25b). The degradation of 4-hydroxyphenylpyruvate produced from tyrosine by Pseudomonas sp. strain PJ 874 grown at the expense of tyrosine is mediated by 4-hydroxyphenylpyruvate dioxygenase. This has been puriied (Lindstedt et al. 1977; Johnson-Winters et al. 2003), and the primary structure of the pseudomonas enzyme has been determined (Rüetschi et al. 1992). The metabolism of l-tyrosine may proceed by transamination, dioxygenation to 4-phenylpyruvate followed by either ring ission, or oxidation to 2-carboxymethyl 1,4-benzoquinone and polymerization (Denoya et al. 1994). c. The degradation of 2-aminoethanesulfonate (taurine) by Escherichia coli takes place by α-hydroxylation at the position adjacent to the sulfonate group with the production of aminoacetaldehyde and sulite, and is mediated by a 2-ketoglutarate-dependent dioxygenase (Eichhorn et al. 1997). The degradation of linear alkyl sulfate esters (C4 –C12) by Pseudomonas putida strain S-313 under sulfate limitation takes place by an analogous reaction to produce the corresponding aldehyde and sulfate. This enzyme is, however, able to use a wider range of 2-ketoacids (Kahnert and Kertesz 2000). 2. A rather heterogeneous group of reactions are carried out by dioxygenation: a. 3-Hydroxy-4-ketoquinoline dioxygenation → anthranilate + CO (Figure 3.26a) (Fischer et al. 1999). b. Quercitin dioxygenation → depside + CO (Figure 3.26b) (Krishnamurty and Simpson 1970) is mediated by a uniquely copper-dependent dioxygenase (quercitinase) (Steiner et al. 2002). c. In the methionine salvage pathway that has been elucidated in Klebsiella pneumoniae (Wray and Abeles 1995), a key intermediate is an enediol that undergoes dioxygenation. A single protein can carry out two oxygenations—the Fe-dependent enzyme carries out ission of the double bond, whereas the other enzyme that is Ni-dependent leads to the loss of CO and the formation of formate (Dai et al. 1999) (Figure 3.27). These reactions are formally analogous to the intradiol and extradiol ission of catechols. d. Dioxygenation of 2-chlorohydroquinone to produce 3-hydroxymuconate in Sphingomonas paucimobilis UT26 (Miyauchi et al. 1999, Endo et al. 2005). The product of dioxygenation is an acyl chloride that is hydrolyzed to a hydroxymuconate to avoid toxifying the dioxygenase. e. In the oxidation of n-propane to n-propanol by Nocardia parafinicum (Rhodococcus rhodochrous) ATCC 21198, the ratio of hydrocarbon to oxygen consumed was 2:1 and suggests that the reaction of two molecules of propane and one of dioxygen produced

Cl

CH2

O

H

Cl

+

CO2 H

OH

O

CH−CO2H

C

CO2 H

CO2 H

O

O

O

O

CO2

C

CH2

+

HO

O

CO2 H

CO2 H

O

O Cl

CO2 H

CH2

O

Cl

OH

O O

HO

H O CO2 H

CH2

OH

OH

CO2 H

O

Dioxygenation of (a) 2,4-dichlorophenoxyacetate and (b) 4-hydroxyphenylpyruvate.

O

O C

O

Cl

FIGURE 3.25

(b)

(a)

Cl

O

H

+

CHO−CO2H

OH

OH

CH2−CO2H

Mechanistic Aspects 127

128

Environmental Degradation and Transformation of Organic Chemicals O OH

CO 2 H

(a)

+ CO N

NH 2 OH

OH

OH

OH HO

O

HO

O

O CO 2 H

(b) OH OH

OH

O

O R C

(c)

CHOH C

RCO 2 H + CH 3 CHO

OH

Dioxygenation of (a) 3-hydroxyquinol-4-one to anthranilate, (b) rutin, and (c) enediol.

FIGURE 3.26

O R O O H

O R

C

C

C

OH

OH

O R

C

C

C

O H C

O

O CH(OH)

R

C

C

OH + H−CO2H

O

OH

O C

O

OH

O

O R

O

C C O OH

O

CH(OH) R

C

OH

+

CO + H−CO2H

FIGURE 3.27 Dioxygenation of enediol to formate + CO in the methionine salvage pathway.

two molecules of alkanol (Babu and Brown 1984). This reaction is formally comparable to the oxidation of 2-nitropropane to acetone by lavoenzymes in Hansenula mrakii (Kido et al. 1978b) and Neurospora crassa (Gorlatova et al. 1998). f. The polyisoprenoid oxygenase (Braaz et al. 2004) in Xanthomonas sp. is extracellular and functions as a heme-dependent oxygenase with the production of 12-keto-4, 8-dimethyltrideca-4,8-diene-1-al (Braaz et al. 2004). g. An unusual reaction is involved in the oxygenation of a substituted 2-chloroaniline to the corresponding nitro compound (pyrrolonitrin) that is a metabolite of Pseudomonas luorescens (Lee et al. 2005). The enzyme contains a Rieske [Fe–S] cluster and a mononuclear Fe center, and has a very limited range of anilines. 3. There are important dioxygenases from eukaryotic organisms: a. The oxidation of 2-nitropropane by the yeast Hansenula mrakii is carried out by a lavoenzyme and produces 2 mol of acetone from 2 mol of substrate and 1 molecule of O2 that is activated by conversion into superoxide (Kido et al. 1978b) (Figure 3.28). A similar enzyme for which 2-nitropropane is the optimal substrate has been puriied and characterized from the heterothallic ascomycete Neurospora crassa (Gorlatova et al. 1998).

129

Mechanistic Aspects CH 3 CH 3

H C

CH 3 CH 3

C

O

NO 2

O

O

CH 3 CH 3

O

NO 2 H

C

CH 3 CH 3

H C NO2

2CH3COCH3

FIGURE 3.28 Dioxygenation of 2-nitropropane.

b. 1,2,4-Trihydroxybenzene is an intermediate in the degradation of a number of substrates by Phanerochaete chrysosporium including vanillate, 2,4-dichlorophenol, 2,4dinitrophenol, and 2,7-dichlorodibenzo[1,4]dioxin. Its degradation is mediated by a dioxygenase that carries out intradiol ring ission (Rieble et al. 1994). c. The degradation of rutin by Aspergillus lavus proceeds by hydrolysis to the aglycone followed by degradation to a depside with the release of unusual metabolite carbon monoxide (Figure 3.26b) is accomplished by dioxygenation (Krishnamurty and Simpson 1970). In addition, the dioxygenase is unusual in containing Cu in place of the more common Fe (Steiner et al. 2002). d. Several unusual 2-ketoglutarate-dependent dioxygenations have been found in the yeast Rhodotorula glutinis: i. Conversion of deoxyuridine by 1′-hydroxylation into uracil and ribonolactone (Stubbe 1985). ii. Thymine-7-hydroxylase catalyzed the oxidation of the 5-methyl group to 5-hydroxymethyl uracil (Wondrack et al. 1978).

INCORPORATION OF OXYGEN FROM WATER: OXIDOREDUCTASES AND HYDRATASES Oxidoreductases Both aerobic and anaerobic bacteria degrade azaarenes formally by hydroxylation in which the oxygen originates from water. The reaction involves a redox reaction and is mediated by oxidoreductases (dehydrogenases), although the physiological electron acceptors have not been generally established. These enzymes contain a molybdenum cofactor, and the formation of active xanthine dehydrogenase in purinolytic clostridia requires in addition a labile cofactor containing selenium. In contrast, the enzyme that mediates the hydroxylation of a number of bicyclic azaarenes has been termed an oxidase—quinaldine 4-oxidase—since oxygen functions effectively as an electron acceptor (Stephan et al. 1996). Five-Membered Heteroarenes The aerobic degradation of the 2-carboxylates of furan, pyrrole, and thiophene is initiated by hydroxylation before ission of the rings. Although details of the enzymes are limited, it was suggested on the basis of tungstate inhibition and 185W [tungstate] labeling that the degradation of 2-furoyl-coenzyme A involves a molybdenum-dependent dehydrogenase (Koenig and Andreesen 1990). Pyridine The aerobic degradation of pyridines with carboxyl and hydroxyl substituents generally involves hydroxylation (dehydrogenation). The dehydrogenases for the degradation of pyridine-2-carboxylate by Arthrobacter picolinophilus (Siegmund et al. 1990), and for two steps in the degradation of nicotine by Arthrobacter nicotinovorans (oxidans) (Freudenberg et al. 1988; Baitsch et al. 2001) contain molybdenum, lavin, and nonheme iron–sulfur. The nicotinate dehydrogenase from Clostridium barkeri contains, in addition, a labile selenium cofactor (Dilworth 1982).

130

Environmental Degradation and Transformation of Organic Chemicals

Quinoline The quinoline enzymes have been examined in much greater detail than those for pyridines, and occur in both Gram-negative and Gram-positive organisms. The oxidoreductases have been puriied from a number of organisms that degrade quinoline. These include P. putida strain 86 (Bauder et al. 1990), Comamonas testosteroni strain 63 (Schach et al. 1995), Rhodococcus sp. strain B1 (Peschke and Lingens 1991), and Agrobacterium sp. strain 1B that degrades quinoline-4-carboxylate (Bauer and Lingens 1992). They have a molecular mass of 300–360 kDa and contain per molecule, eight atoms of Fe, eight atoms of acid-labile S, two atoms of Mo, and two molecules of FAD. The organic component of the pterin molybdenum cofactor is generally molybdopterin cytosine dinucleotide (Hetterich et al. 1991; Schach et al. 1995). The oxidoreductase that catalyzes the hydroxylation of 2-methylquinoline is able, in addition, to accept a range of other six-membered azaarenes (Stephan et al. 1996). Isoquinoline The degradation of isoquinoline by Pseudomonas diminuta strain 7 is initiated by an oxidoreductase that contains [2Fe–2S] centers and the cofactor molybdopterin cytosine dinucleotide (Lehmann et al. 1994). Purines Xanthine dehydrogenase that mediates the conversion of hypoxanthine into xanthine and uric acid has been studied extensively since it is readily available from cow’s milk. It has also been studied (Leimkühler et al. 2004) in the anaerobic phototroph Rhodobacter capsulatus, and the crystal structures of both enzymes have been solved. Xanthine dehydrogenase is a complex lavoprotein containing Mo, FAD, and [2Fe–2S] redox centers, and the reactions may be rationalized (Hille and Sprecher 1987): R−H + H2O + MoVI=S → ROH + MoIV–SH + H+ Some additional issues are worth noting: a. Xanthine dehydrogenase from the anaerobic Clostridium purinolyticum, Cl. acidi-urici, and Cl. cylindrosporum contains a labile selenium cofactor. b. In Clostridium purinolyticum, purine hydroxylase, which is a separate enzyme from xanthine dehydrogenase, hydroxylates purine to hypoxanthine (6-hydroxypurine) and xanthine (2,6-dihydroxypurine), which is then further hydroxylated to uric acid (2,6,8trihydroxypurine) by xanthine dehydrogenase (Self 2002). Like the xanthine dehydrogenases, it contains a selenium cofactor. c. Although the mammalian enzyme is synthesized in the dehydrogenase form XDH, it can readily be converted by oxidation of sulfuryl groups into the oxidase XO that exclusively uses O2 as its substrate. Hydratases These enzymes catalyze the addition of the elements of water to carbon–carbon double bonds (C=C), carbon–carbon triple bonds (C≡C), carbon–nitrogen double bonds (C=N), or carbon– nitrogen triple bonds (C≡N). These reactions are completely different from oxidoreductases since no redox reactions are involved. Illustrative examples include the following: C=C a. An alternative to monooxygenation is realized in the hydration of the substituted cyclohexanone derived from the ission product of 1,2-dihydroxynaphthalene during the degradation of 1,2,3,4-tetrahydronaphthalene (tetralin) (Figure 3.29) (Hernáez et al. 2002).

131

Mechanistic Aspects OH

OH OH

HO

O

OH O

HO

O CO 2 H

OH OH

OH

O

FIGURE 3.29 Aerobic degradation of tetralin.

(a)

H

C

C

(b)

R

N

C

H

H2 C

CHOH

CH 3 CHO

R−NH−CHO

FIGURE 3.30 (a) Hydration of acetylene to acetaldehyde and (b) transformation of an isonitrile to N-alkylformamide.

b. In addition to the oxidative pathway via (4-hydroxy-3-methoxybenzoyl)acetyl-ScoA, the degradation of feruloyl-SCoA to vanillin can be carried out by the alternative hydration followed by loss of acetate that has been found in Pseudomonas luorescens (Gasson et al. 1998). c. The degradation of phenanthrene by Nocardioides sp. strain KP7 is initiated by dioxygenation to 1-hydroxynaphthalene-2-carboxylate, which is further dioxygenated to 2′-carboxybenzalpyruvate before hydration and aldolase ission to 2-carboxybenzaldehyde (Iwabuchi and Harayama 1998a). d. One step in the anaerobic degradation of benzoyl-CoA by the denitrifying Thauera aromatica involves hydration to cyclohexa-1,5-dienecarboxylate thioester to produce the 6-hydroxy compound (Boll et al. 2000). C≡C Acetylene hydratase from the anaerobe Pelobacter acetylenicus is a tungsten–iron–sulfur enzyme that resembles molybdopterin with W replacing Mo (Meckenstock et al. 1999), and catalyzes the addition of the elements of water to acetylene (Figure 3.30a). R–C≡N and R–N≡C a. Nitriles may be degraded to carboxylic acids either directly by the activity of a nitrilase in Bacillus sp. strain OxB-1 and Pseudomonas syringae B728a, or undergo hydration to amides followed by hydrolysis in P. chlororaphis (Oinuma et al. 2003). b. The hydratase in Pseudomonas putida N19-2 converts isonitriles into N-substituted formamides, and its activity is dependent on the presence of Cys-101 (Figure 3.30b) (Goda et al. 2002).

OXIDASES, PEROXIDASES, AND HALOPEROXIDASES Oxidases These are produced by both prokaryotes and eukaryotes, and catalyze a number of important reactions. They are lavoproteins that produce potentially destructive H2O2 that is removed by the activity of catalase or peroxidase. The reactions are formally outlined in Figures 3.31a through c.

132

Environmental Degradation and Transformation of Organic Chemicals (a)

R2 CHX + H2 O + O2

(b)

RHC

R2 CO + HX + H2 O2

NH2 CO2 H (c)

FIGURE 3.31

RCO − CO2 H + NH3 + H2 O2

+ H2 O + O2

RCH2 CH2 CO2 H + O2

RCH

CH−CO2 H + H2 O2

(a–c) Overview of reactions carried out by oxidases.

1. Primary amines are widely used as a nitrogen source by bacteria, and the i rst step in their degradation involves formation of the corresponding aldehyde. Although this may be accomplished by dehydrogenation, some organisms use an amine oxidase. For example, whereas Pseudomonas putida (ATCC 12633) and P. aeruginosa (ATCC 17933) employ a dehydrogenase, Klebsiella oxytoca (ATCC 8724) and Escherichia coli (ATCC 9637) use a copper quinoprotein amine oxidase (Hacisalihoglu et al. 1997). The alternative lavoprotein oxidase is, however, used for deamination of tyramine by Sarcina lutea. The amine oxidase functions by oxidation of the amine to the aldehyde concomitant with the reduction of 2,4,5-trihydroxyphenylalanine quinone (TPQ) to an aminoquinol which, in the form of a Cu(I) radical reacts with O2 to form H 2O2 Cu(II) and the imine. Methylamine dehydrogenase, however, involves tryptophylquinone (TTQ) but does not result in formation of H 2O2 (references in Stubbe and van der Donk 1998). 2. The aerobic degradation of nicotine produces an N-methylpyrrolidine as the irst metabolite by dehydrogenation. This is then hydroxylated at the benzylic carbon atom by an FAD-containing oxidase (Dai et al. 1968), and the γ-N-methylaminobutyrate that is produced by ission of the N-methylpyrolidine ring is demethylated by an oxidase to 4-aminobutyrate (Chiribau et al. 2004). 3. Quinaldine 4-oxidase from Arthrobacter sp. Rü61a that mediates the hydroxylation of a number of bicyclic azaarenes has been termed an oxidase since oxygen functions effectively as an electron acceptor (Stephan et al. 1996). 4. Hyphomicrobium sp. strain EG is able to grow at the expense of dimethyl sulide or dimethyl sulfoxide (DMSO) and produces methanethiol initially. This is then further oxidized to formaldehyde, sulide, and H2O2 by an oxidase that has been puriied (Suylen et al. 1987). 5. The oxidation of cholesterol to cholest-4-ene-3-one is carried out by an oxidase in several bacteria. This activity has been found in Brevibacterium sterolicum and Streptomyces sp. strain SA-COO (Ohta et al. 1991), and the extracellular enzyme that has been puriied from Pseudomonas sp. strain ST-200 (Doukyu and Aono 1998) has a preference for 3βhydroxy compounds. 6. d-Aminoacid oxidase has been isolated from a number of yeasts, and the nucleotide sequence of the enzyme from Rhodotorula gracilis ATCC 26217 has been established (Alonso et al. 1998). The gene could be overexpressed in Escherichia coli, and levels of the enzyme were greater under conditions of low aeration: the enzyme isolated from the recombinant organisms was apparently the apoenzyme since maximum activity required the presence of FAD. 7. Yeasts belonging to the genera Candida and Endomycopsis are able to degrade alkanes. The initial hydroxylation is carried out by cytochrome P450 that is found in the microsome (references in Käppeli 1986). The degradation of the alkanoic acids is carried out by enzymes that are contained in peroxisomes, and are induced during growth with alkanes. Acyl-CoA oxidase carries out the irst step in the degradation of the alkanoic acid CoA-esters, and although this is formally a dehydrogenase, acyl-CoA dehydrogenase

Mechanistic Aspects

133

activity is absent (Kawamoto et al. 1978; Tanaka and Ueda 1993). The three subsequent enzymatic activities are apparently contained in a single protein. 8. Nitroalkanes are degraded by some yeasts and fungi, and the dioxygenase pathway that has already been described is not the only one. The fungus Fusarium oxysporum is able to degrade a number of nitroalkanes including 1- and 2-nitropropane, nitroethane, and nitrocyclohexane by an inducible oxidase, and the reaction rate of the enzyme is enhanced by addition of catalase and inhibited by both NADH and NADPH (Kido et al. 1978a). The oxidase is a lavoprotein that occurs in an inactive form as 5-nitrobutyl-FAD that is convertible into the active form of the enzyme (Gadda et al. 1997). This enzyme is clearly different from the dioxygenase. 9. Vanillyl-alcohol oxidase that brings about oxidation to vanillin is mediated by a lavoprotein that is reduced with production of a quinonemethine that reacts with H2O to form the aldehyde. The reduced lavoprotein is then reoxidized to produce H2O2 (Fraaije and van Berkel 1997). The enzyme is also able to accept a range of 4-alkylphenols. Two reactions occurred, and their ratio depended on the alkyl substituent: for example, whereas 4-hydroxyphenylethane produced 4-hydroxyacetophenone (76%) and 4-hydroxyphenylethene (24%), only the corresponding alkenes were produced from substrates with C4 –C7 alkyl groups (van den Heuvel et al. 1998). The reaction is formally analogous to the bacterial reaction catalyzed by 4-ethylphenol methylene hydroxylase, which proceeds by dehydrogenation followed by hydroxylation with H2O (Hopper and Cottrell 2003). Peroxidases Extracellular H2O2 is required for the activity of peroxidases in white-rot fungi, and this can be produced by several fungal reactions: a. Glyoxal oxidase is produced from Phanerochaete chrysosporium under high concentrations of oxygen, is stimulated by Cu2+, and oxidizes a range of substrates with the production of H2O2 from O2. Substrates include methylglyoxal, glyoxylic acid, and glycolaldehyde, and the pure enzyme requires activation by lignin peroxidase: under these conditions, in the presence of catalytic amounts of H2O2, pyruvate and veratraldehyde are produced, respectively, from methylglyoxal and 3,4-dimethoxybenzyl alcohol (veratryl alcohol) (the lignin peroxidase substrate) (Kersten 1990). b. An aryl-alcohol oxidase that is produced from Bjerkandera adusta optimally under carbon limitation oxidized a number of benzyl alcohols including 4-methoxybenzyl alcohol, 3,4-dimethoxybenzyl alcohol (veratryl alcohol), and 4-hydroxy-3-methoxybenzyl alcohol, with the production of H2O2 from O2: monosaccharides were not oxidized (Muheim et al. 1990). An aryl-alcohol oxidase from Pleurotus eryngii is a lavoprotein with range of substrates comparable to that from B. adusta (Guillén et al. 1992). c. Peroxide may also be produced by the manganese peroxide–dependent oxidation of glycolate and oxalate that are synthesized by Ceriporiopsis subvermispora (Urzúa et al. 1998). Two distinct extracellular enzymes are produced by white-rot fungi—lignin peroxidase (LiP) and manganese peroxidase (MnP). These are produced under speciic growth conditions that include carbon, nitrogen or sulfur limitation, manganese concentration, and increased oxygen concentration. They are involved in the degradation of lignin and in the biotransformation of xenobiotics. These enzymes require extracellular H2O2, which is produced by a number of these organisms as a result of oxidase activity that has already been noted. Details of the relevant reactions have emerged from a study of the degradation of a model lignin substrate by Phanerochaete chrysosporium (Hammel et al. 1994). 1-(3,4-Dimethyoxyphenyl)-2-phenoxypropane-1,3-diol was metabolized in the presence of H2O2 to glycolaldehyde that was identiied by 13C-NMR: the oxidase activity of glyoxal

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Environmental Degradation and Transformation of Organic Chemicals

oxidase that was synthesized simultaneously with lignin peroxidase produced oxalate and 3 mol of H2O2 that could then be recycled. In the degradation of lignin and model compounds, lignin peroxidase functions by generating cation radicals from aromatic rings. This results in ission of the alkyl side chain between C1 and C2 (Kirk and Farrell 1987, or—for substrates such as PAHs—may be followed by nonenzymatic nucleophilic reactions of the cation radical (Hammel et al. 1986; Haemmerli et al. 1986). Manganese peroxidase oxidizes Mn(II) to Mn(III), which is the active oxidant, and in the presence of H2O2 is capable of oxidizing a number of PAHs (Bogan and Lamar 1996) and mineralizing substituted aromatic compounds (Hofrichter et al. 1998). Both activities may bring about oxidation of PAHs in reactions that are mimicked by oxidation with manganese(III) acetate (Cremonesi et al. 1989) or electrochemical oxidation (Jeftic and Adams 1970). Haloperoxidases These are of primary signiicance in the biosynthesis of organohalogen compounds (Neilson 2003), which are distributed among mammals, marine biota, bacteria, and fungi. These enzymes catalyze the reaction: S–H + H2O2 + HalH → S–Hal + 2H2O where Hal may be chloride, bromide, or iodide (references in Neidleman and Geigert 1986). Haloperoxidases have been isolated and puriied from a number of organisms in which they mediate biosynthetic reactions. There are several structural groups of haloperoxidases that are summarized in Table 3.2. a. The chloroperoxidase from Caldaromyces fumago has been isolated in pure form. It is a glycoprotein containing ferroprotoporphyrin IX, and displays additionally both peroxidase and catalase activities. In the absence of organic substrates it catalyzes the formation of Cl2 and Br2 from chloride and bromide, respectively (Morris and Haeger 1966; Libby et al. 1982). b. Bromoperoxidase has been isolated from Pseudomonas aureofaciens ATCC 15926, also displays peroxidase and catalase activities, and contains ferriprotoporphyrin IX (van Pée and Lingens 1985b). Four different bromoperoxidases have been isolated from Streptomyces griseus (Zeiner et al. 1988). Only one of them, however, contains ferriprotoporphyrin IX, and displays peroxidase and catalase activities. This illustrates that there are different groups of enzymes, one of which lacks heme prosthetic groups. Chloroperoxidase activity has also been found among degradative enzymes: 1. An inducible enzyme in the bacterium Rhodococcus erythropolis NI86/21 that is involved in the degradation of thiocarbamate herbicides is a nonheme haloperoxidase, which does not occur in other strains of rhodococci that can degrade thiocarbamates (de Schrijver et al. 1997). 2. Acinetobacter calcoaceticus strain F46 was enriched with luorene that is degraded by dioxygenation, loss of C3, decarboxylation, and Baeyer–Villiger oxygenation to 3,4-dihydrocoumarin (Figure 3.32). The hydrolase for this was able to brominate monochlorodimedone in the presence of H2O2 and 3,4-dihydrocoumarin, or acetate, or butyrate (Kataoka et al. 2000). It was proposed that acyl peroxides could be produced from an acylated serine site on the enzyme by the action of H2O2 and oxidize bromide to the active brominating agent BrO−. This is analogous to the mechanism proposed earlier (Picard et al. 1997).

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TABLE 3.2 Types of Haloperoxidases Type of Enzyme

Group

Heme

Heme + f Flavin Vanadium

Nonheme/lavin Nonheme/ nonlavin Nonheme/ nonmetal

Organism

Halogen

Reference

Bacterium Streptomyces phaeochromogenes Rhodophyta Cystoclonium purpureum Chlorophyta Penicillus capitatus

Br Br Br

Fungus Polychaete Phaeophyta Phaeophyta Phaeophyta Phaeophyta Phaeophyta Rhodophyta Fungus Bacterium

Caldariomyces fumago Notomastus lobatus Ascophyllum nodosum Ecklonia stolonifera Laminaria digitata Laminaria saccharina Macrocystis pyrifera Corallina pilulifera Curvularia inequalis Pseudomonas luorescens

Cl Cl Br Br Br Br Br Br Cl Cl

van Pée and Lingens (1985a) Pedersén (1976) Baden and Corbett (1980) and Manthey and Hager (1981) Morris and Hager (1966) Chen et al. (1991) Vilter (1984) Hara and Sakurai (1998) Jordan and Vilter (1991) de Boer et al. (1986) Soedjak and Butler (1990) Krenn et al. (1989) and Itoh et al. (1988) Simons et al. (1995) Keller et al. (2000)

Bacterium

Pseudomonas putida

Br

Itoh et al. (1994)

Bacterium

Pseudomonas pyrrocinia, Streptomyces aureofaciens, and Acinetobacter calcoaceticus

Cl, Br, and Br

Wiesner et al. (1988), Weng et al. (1991), and Kataoka et al. (2000)

OH

OH

O

OH CHO

O

FIGURE 3.32

O

Degradation of luorene.

3. The gene encoding the esterase from Pseudomonas luorescens was expressed in Escherichia coli, and the enzyme displayed both hydrolytic and bromoperoxidase activity (Pelletier and Altenbuchner 1995).

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PART 2 ELECTRON ACCEPTORS OTHER THAN OXYGEN INTRODUCTION Bacteria can use a range of electron acceptors in the absence of oxygen. Although they are able to reduce a number of oxyanions, only a limited number of these can support growth under anaerobic conditions by coupling reduction to the production of energy by proton translocation. A number

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of facultatively anaerobic bacteria are, however, able to carry out a respiratory metabolism in the absence of oxygen using alternative inorganic electron acceptors. For example, the following reductions may be coupled to oxidative degradation: nitrate to nitrogen (or nitrous oxide), sulfate to sulide, carbonate to methane, fumarate to succinate, trimethylamine-N-oxide (TMAO) to trimethylamine, or dimethylsulfoxide to dimethyl sulide. Some introductory comments are given, and an attempt is made to illustrate the metabolic potential of organisms under these conditions. It is appropriate to note the metabolic potential of members of the DMSO reductase family (McEwan et al. 2002) that are able to carry out a wide range of dissimilations: Me2SO → Me2S (DMSO reductase); Me3NO → Me3N (TMAO reductase); HCO2H → CO2 + H2 (formate dehydrogenase); AsO2− → AsO43− (arsenite oxidase); SeO42− → SeO32− (selenate reductase). The conditions under which these function and their regulation depend on the organism. For example, in Escherichia coli, oxygen represses the synthesis of the other reductases, and under anaerobic conditions the reductases for fumarate, DMSO, and TMAO are repressed by nitrate. This does not apply to Wolinella succinogenes in which sulfur represses the synthesis of the more positive electron acceptors nitrate and fumarate (Lorenzen et al. 1993). The DMSO reductase from Escherichia coli (Weiner et al. 1988) has a broad substrate versatility, and is able to reduce a range of sulfoxides and N-oxides. Anaerobic sulfate reduction is not discussed here in detail.

OXYANIONS: NITRATE, SULFATE, CHLORATE, SELENATE, AND ARSENATE Nitrate and Related Compounds Nitrate can fulill several functions: (a) assimilatory as a nitrogen source after reduction, (b) dissimilatory in reduction, and (c) respiration in which the reduction is coupled to the synthesis of ATP. The structural genes for assimilatory reduction are encoded by Nas genes and contain FAD, [4Fe–4S], and bis-molybdenum guanine dinucleotide (MGD); in dissimilation, the FAD is replaced by cytochrome b or c (Moreno-Vivián et al. 1999). The membrane-bound nitrate reductase that is involved in proton translocation and energy production is encoded by the genes NarGH, and the enzyme contains molybdopterin guanine dinucleotide, [Fe–S] clusters, and diheme cytochrome b556. The periplasmic nitrate reductase encoded by NapABC is primarily involved in dissimilation. The degradation of organic compounds with nitrate in the absence of oxygen—denitriication or nitrate dissimilation—has been known for a long time and has been used as a valuable diagnostic character in bacterial classiication. The products are either dinitrogen or nitrous oxide, and the reaction is generally inhibited by oxygen, so that it occurs to a signiicant extent only under anoxic conditions. For example, although it has been reported that Thiosphaera pantotropha (Paracoccus denitriicans) is capable of both denitriication and nitriication under aerobic conditions (Robertson and Kuenen 1984), it has been shown that the suite of enzymes necessary for denitriication is not expressed constitutively. In addition, the rates of denitriication under aerobic conditions were very much slower than under anaerobic conditions (Moir et al. 1995). An important development is the appreciation of the role of anammox bacteria. These carry out the anaerobic reaction between NH4+ and NO2− in which nitrite is the electron donor with the production of N2 (Schmid et al. 2005). Several groups of bacteria have been implicated, and all of them belong to the phylum Planctomyces, although quite distinct organisms may be involved. They

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are widely distributed in habitats ranging from systems treating ammonia-rich waste to anaerobic marine environments (Tal et al. 2005). These organisms are unusual among anaerobic bacteria in many respects, and a number of procedures have been outlined to assess their contribution to nitrogen cycling, their enumeration, and their distribution. Denitriication involves the sequential formation of nitrite, nitric oxide, and nitrous oxide. Two aspects of nitric oxide have attracted attention: (a) chemical oxidation of biogenic nitric oxide to Nox in the context of increased ozone formation (Stohl et al. 1996) and (b) the physiological role in mammalian systems (Feldman et al. 1993; Stuehr et al. 2004), in parasitic infections (James 1995), and in the inhibition of bacterial respiration (Nagata et al. 1998). Nitric oxide may be produced microbiologically in widely different reactions such as a. Oxidation of l-arginine by a strain of Nocardia sp. produced nitric oxide and l-citrulline (Chen and Rosazza 1995). The enzyme (nitric oxide synthase) carries out two distinct reactions: (i) hydroxylation of l-arginine catalyzed by an enzyme analogous to cytochrome P450 and (ii) a one-electron oxidation of Nω-hydroxy-l-arginine to NO and l-citrulline. The mechanism has been reviewed (Stuehr et al. 2004). b. During the metabolism of glycerol trinitrate by Phanerochaete chrysosporium (Servent et al. 1991). Renewed interest has been focused on degradation of xenobiotics under anaerobic conditions in the presence of nitrate—possibly motivated by the extent of leaching of nitrate fertilizer from agricultural land into groundwater. In studies with such organisms, a clear distinction should be made between degradation of the substrate under three conditions that may or may not be biochemically equivalent: (a) aerobic conditions, (b) anaerobic conditions in the presence of nitrate, and (c) fermentation by strictly anaerobic conditions in the absence of any electron acceptor. Some examples are given to illustrate the diversity of degradations that have been observed with facultatively anaerobic organisms using nitrate as the electron acceptor: 1. The degradation of carbon tetrachloride to CO2 by a Pseudomonas sp. (Criddle et al. 1990), although a substantial part of the label was retained in nonvolatile water-soluble residues (Lewis and Crawford 1995). The nature of this was revealed by isolation of adducts with cysteine and N,N′-dimethylethylenediamine in which intermediates formally equivalent to COCl2 and CSCl2 were trapped, presumably formed by reaction of the substrate with water and a thiol, respectively. Further consideration of these reactions is given in Chapter 7, Part 3. 2. The nonstoichiometric production of trichloromethane from tetrachloromethane by Shewanella putrefaciens (Picardal et al. 1993). 3. The degradation of benzoate (Taylor and Heeb 1972; Williams and Evans 1975; Ziegler et al. 1987) and o-phthalate (Nozawa and Maruyama 1988; Afring and Taylor 1981). 4. The degradation of alkyl benzenes (Hutchins 1991; Evans et al. 1991a,b; Altenschmidt and Fuchs 1991). In these studies, some of the organisms referred to the genus Pseudomonas have been transferred to the genus Thauera (Anders et al. 1995). 5. The degradation of pristane in microcosms and in enrichment cultures (Bregnard et al. 1997). 6. The mineralization of cholesterol by an organism related to Rhodocyclus, Thauera, and Azoarcus (Harder and Probian 1997). It is also important to appreciate that an organism that can degrade a given substrate under conditions of nitrate dissimilation may not necessarily display this potential under aerobic conditions. For example, a strain of Pseudomonas sp. could be grown with vanillate under anaerobic conditions in the presence of nitrate but was unable to grow under aerobic conditions with vanillate.

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In contrast, cells grown anaerobically with nitrate and vanillate were able to oxidize vanillate under both aerobic and anaerobic conditions. The cells were also able to demethylate a much wider spectrum of aromatic methoxy compounds under anaerobic conditions than under aerobic conditions (Taylor 1983). Such subtleties should be clearly appreciated and taken into consideration in evaluating the degradative potential of comparable organisms under different physiological conditions. During degradation in the presence of nitrate this may be reduced, and it has been observed that nitro groups may be introduced into the substrate. Details of this have been discussed in Chapter 2. Sulfate and Related Compounds Sulfate can be either assimilated as sulfur source or dissimilated by anaerobic bacteria as an electron acceptor when it is reduced to sulide. Both reactions involve the formation of AMP anhydrides (APS) catalyzed by ATP sulfurylase. In dissimilation, this is reduced successively to sulite and sulide. In assimilation, however, the ester is phosphorylated by ATP and an APS kinase to the anhydride, which after additional phosphorylation at C3′ (PAPS), undergoes further reduction by PAPS reductase encoded by the gene cysH (Bick et al. 2000). The assimilatory sulite reductase from Escherichia coli is a complex enzyme containing two different polypeptides. The α-chain coded by the cysJ gene in Escherichia coli binds one of the lavins (FAD or FMN), while the β-chain coded by the cysI gene binds one [Fe4S4] cluster and one siroheme that is the site of sulite reduction (Eschenbrenner et al. 1995). Siroheme is an iron tetrahydroporphrrin with eight carboxylate groups and two methyl groups on the reduced rings (Murphy et al. 1973). Although the metabolism of tetrathionate has not been established in detail, it presumably takes place via thiosulfate, sulite, and sulide. Tetrathionate, which is a component of some media for enrichment of salmonellas, is able to support the anaerobic growth of Salmonella sp. using glycerol or acetate, and S. enterica with ethanolamine or propan-1,2-diol when vitamin B12 is available (Price-Carter et al. 2001). Chlorate and Perchlorate Chlorate can serve as electron acceptor under anaerobic conditions (Thorell et al. 2003; Coates et al. 1999), and chlorate reductase has been found both in organisms such as Proteus mirabilis that can reduce chlorate but is unable to use to couple this to growth, and in true chlorate-respiring organisms. Chlorate has been shown to support the growth of an anaerobic community growing at the expense of acetate (Malmqvist et al. 1991), and a pure culture designated Ideonella dechloratans has been isolated (Malmqvist et al. 1994). A number of other organisms can use chlorate as electron acceptors during anaerobic growth and all of them can carry out dismutation of the intermediate chlorite. These include strain GR-1 that is able to carry out the sequential reduction of perchlorate to chlorate, and chloride at the expense of acetate (Rikken et al. 1996). Organisms capable of dissimilatory (per)chlorate reduction are both ubiquitous and diverse, and on the basis of 16S rRNA they are distinct from the previously described Ideonella dechloratans, and have been assigned to species of Dechloromonas (Achenbach et al. 2001). They can utilize C2–C5 carboxylic acids, lactate, fumarate, and malate as electron donors using chlorate as electron acceptor. Some of them can utilize both nitrate and chlorate as electron acceptors with acetate as electron donor (Coates et al. 1999), while Dechloromonas strain RCB, which is able to degrade benzene in the presence of nitrate, is also able to use perchlorate (Chakraborty et al. 2005). Pseudomonas chloritidismutans is clearly different from these organisms and is similar to P. stutzeri, except in the ability to use chlorate as electron acceptor. It is able to use chlorate, though not perchlorate or nitrate, as electron acceptors using acetate and propionate as sources of carbon (Wolterink et al. 2002). Although some isolates are capable of high rates of growth using both perchlorate and chlorate, some are able only to use the latter (Logan et al. 2001). Chlorate reductase has been characterized in strain GR-1 where it was found in the periplasm. It is oxygen-sensitive and contains molybdenum and [3Fe–4S] and [4Fe–4S] clusters (Kengen et al. 1999).

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A different cytoplasmic reductase has been characterized from Pseudomonas chloritidismutans (Wolterink et al. 2003). Chlorate reductase from I. dechloratans has been characterized (Thorell et al. 2003), and consists of three subunits, contains heme b, and resembles enzymes belonging to the molybdopterin DMSO reductase class II family. Perchlorate reductase from Dechloromonas agitata is different from that of I. dechloratans, although the pcrAB gene products are similar to α- and β-subunits of other reductases including nitrate, selenate, and chlorate. The pcrC gene product was similar to a c-type cytochrome, and the pcrD product to the molybdenum-containing proteins of the DMSO reductase family (Bender et al. 2005). The chlorite dismutase that generates oxygen from chlorite produced by reduction of chlorate has been puriied and characterized from strain GR-1 (Van Ginkel et al. 1996) and from Ideonella dechloratans (Stenklo et al. 2001). The enzyme from Dechloromonas agitata has been suggested as a metabolic probe for chlorate reduction in the environment (Bender et al. 2002). Selenate and Arsenate Reductions in which energy is produced during reduction and supports growth of the cells should be carefully distinguished from the situation in which selenate is gratuitously reduced during aerobic growth (Maiers et al. 1988). For example, the membrane-bound selenate reductase from Enterobacter cloacae SLD1a-1 is not able to function as electron acceptor under anaerobic conditions (Ridley et al. 2006). Reductases also function in the detoxiication of arsenate and selenate. The arsenate reductase gene ArsC both in Staphylococcus aureus (Ji and Silver 1992) and in Escherichia coli (Liu et al. 1995) is a determinant of arsenate resistance, and the arsenite that is produced is extruded from the cell by the ArsA–ArsB anion-translocating ATPase (Walmsley et al. 1999). Whereas the reductase from E. coli is coupled to the glutathione and glutaredoxin system, that from S. aureus requires thioredoxin and thioredoxin reductase. The arsenate reductase from Bacillus subtilis shows structural similarity at the active site to that of low-molecular-weight tyrosine phosphatase and this enabled a mechanism for its activity to be proposed (Bennett et al. 2001). Selenate and arsenate can serve as terminal electron acceptors, and strains of anaerobic bacteria have been isolated that are able to use them during growth with lactate. These include a strain designated SES-3 (Laverman et al. 1995), and Bacillus arsenicoselenatis and Bacillus selenitriicans (Blum et al. 1998). In these strains, utilization of acetate is unusual, but acetate is used speciically by Chrysiogenes arsenatis (Macy et al. 1996). The reductase from this organism contains Mo, Fe, and acid-labile S (Krafft and Macy 1998). A facultatively anaerobic organism Thauera selenatis is able to use both selenate and selenite as electron acceptors for anaerobic growth (Macy et al. 1993). The selenate reductase has been shown to contain molybdenum, iron, acid-labile sulfur, and cytochrome b. It is located in the periplasmic space, and is speciic for selenate and nitrate, whereas neither chlorate nor sulfate was reduced at signiicant rates (Schröder et al. 1997). Reduction of selenite to Se0 can be accomplished by the periplasmic nitrite reductase that also occurs in this strain (DeMoll-Decker and Macy 1993). An organism assigned to Desulfotomaculum auripigmentum was able to grow with lactate and could use both arsenate and sulfate as terminal electron acceptors (Newman et al. 1997). Several strains of Desulitobacterium can use arsenate, generally nitrate, and exceptionally selenate as electron acceptors during growth with lactate or pyruvate as electron donors (Niggemyer et al. 2001). A strain of Shewanella ANA-3 can couple the reduction of As(V) to As(III) to the oxidation of lactate to acetate (Saltikov et al. 2003). Although this strain contains the ars operon, which confers resistance to As(III), the gene arsB that encodes the eflux system and arsC for the reductase, although advantageous, are not obligatory. Genetic analysis showed the presence of an additional gene cluster that encoded a respiratory As(V) reductase. The gene arrA is predicted to encode a molybdenum cofactor, and arrB to encode an Fe–S cluster, and are predicted to be similar to those of the DMSO reductase family (Saltikov and Newman 2003). Therefore, although there are two available mechanisms for arsenate respiration, they differ in their expression: the ars system is

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expressed under both aerobic and anaerobic conditions, whereas the arr system is expressed only anaerobically and is repressed by oxygen or nitrate (Saltikov et al. 2005). A facultative autotroph (lithotroph) strain MLHE-1 was able to oxidize arsenite under anaerobic conditions to arsenate using nitrate as electron acceptor (Oremland et al. 2002).

METAL CATIONS AND OXYANIONS Many bacteria that ferment organic substrates are able to reduce Fe(III) to Fe(II) gratuitously, but these organisms are apparently unable to use the energy of this reduction for growth and couple this to the oxidation of organic substrates. There are, however, bacteria that can accomplish this, and some of them can also effectively use Mn(IV) and U(VI) (Lovley 1991) and, occasionally, vanadate. A wide range of organisms of different taxonomic afiliation can use Fe(III) as electron acceptor during growth with acetate. They include organisms currently assigned to the genera Geobacter, Pelobacter, and Desulfuromonas (Lovley et al. 1995; Lonergan et al. 1996; Coates et al. 2001), Shewanella putrefaciens (Myers and Nealson 1990), and Pantoea (Enterobacter) agglomerans (Francis et al. 2000). The anaerobe Desulitobacter metallireducens is able to grow with lactate as electron donor using a range of electron acceptors including Fe(III) citrate, Mn(IV) oxide, 3-chloro-4-hydroxyphenylacetate, and humic substances (Finneran et al. 2002). Anaeromyxobacter dehalogenans is a chlororespiring organism that is able to couple the oxidation of acetate under anaerobic conditions to the reduction of ortho-halogenated phenols, nitrate, fumarate, and Fe(III) (He and Sanford 2003). V(V), Mn(IV), Fe(III), Tc(VII), and U(VI) There has been considerable interest in the remediation of sites contaminated with U(VI) and Tc(VII) by conversion of these soluble forms into less soluble reduced states that may be precipitated. In assessing results involving the reduction of U(VI) and Tc(VII), it is important to take into consideration (a) intermediate levels of reduction that may be critical and (b) the formation of complexes, for example, with carbonate that may determine the inal products and their association with cells or particles. The discussion is assembled by organism, since some of these are able to reduce several oxidants. Shewanella spp. Strains of Shewanella putrefaciens (Alteromonas putrefaciens) are widely distributed in environmental samples and are generally considered as aerobic organisms with the capability of reducing thiosulfate to sulide in complex media. They are also able, however, to grow anaerobically using Fe(III) as electron acceptor, and to oxidize formate, lactate, or pyruvate. These substrates cannot, however, be completely oxidized to CO2 since the acetate produced from the C2 compounds is not further metabolized. Mn[IV] may function analogously to Fe(III) (Lovley et al. 1989). The bioenergetics of the system has been examined in cells of another strain of this organism grown anaerobically with lactate using either fumarate or nitrate as electron acceptors. Respiration-linked proton translocation in response to Mn(IV), fumarate, or oxygen was clearly demonstrated (Myers and Nealson 1990). Levels of Fe(III) reductase, nitrate reductase, and nitrite reductase are elevated by growth under microaerophilic conditions, and the organism probably possesses three reductase systems, each of which apparently consists of low- or high-rate components (DiChristina 1992). Reductase activity is located on the outer membranes of Shewanella putrefaciens and has a requirement for cytochrome c (Myers and Myers 1997) and menaquinones (Saffarini et al. 2002). Another organism with hitherto unknown taxonomic afinity has been isolated (Caccavo et al. 1992), and is able to couple the oxidation of lactate to the reduction of Fe(III), Mn(IV), and U(VI). Under anaerobic conditions, Shewanella oneidensis MR1 can couple the reduction of V(V) to V(IV) to the oxidation of lactate, formate, and pyruvate (Carpentier et al. 2003). Respiration and growth can be carried out by reduction of vanadate: proton translocation across the cytoplasmic membrane takes place during the reduction and is abolished by CCCP, HOQNO, and antimycin (Carpentier et al. 2005).

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Under anaerobic conditions with H2 as electron donor—when growth did not take place—S. putrefaciens reduced Tc(VII) to Tc(IV) that was associated with the cell or with Tc(IV) complexes in the presence of carbonate (Wildung et al. 2000). Geobacter spp. A strictly anaerobic organism designated GS-15 and now assigned to the taxon Geobacter metallireducens (Lovley et al. 1993) is able to use Fe(III) as electron acceptor under anaerobic conditions for the oxidation of a number of substrates including acetate (Lovley and Lonergan 1990), and toluene and phenols (Champine and Goodwin 1991). This organism is also able to oxidize acetate by reduction of Mn(IV) and U(VI) (Lovley et al. 1993), and additional comments are given later in this chapter. Organisms belonging to the genus Geobacter are widely distributed in anaerobic environments in which Fe(III) occurs, and members of the Geobacteraceae were enriched at a site contaminated with U(VI) (Anderson et al. 2003). All species in the family are able to use Fe(III) as electron acceptor and acetate as electron donor, generally propionate and benzoate and, for G. metallireducens and G. grbiciae, additionally toluene using anthraquinone-2,6-disulfonate (AQDS) as an electron acceptor (Coates et al. 2001). The phylogenetically distinct Geovibrio ferrireducens strain PAL-1 is able to use a wide range of organic compounds as electron donors including acetate, propionate, succinate, and proline (Caccavo et al. 1996). It has been shown in Geobacter sulfurreducens that although U(VI) [UO22+] is reduced to insoluble U(IV), this occurs by initial reduction to U(V) followed by disproportionation (Renshaw et al. 2005). Therefore, it was suggested that caution be exercised in the use of microbial remediation for transuranic elements whose oxidation levels differ from those of uranium. There are other limitations to their application for bioremediation of uranium-contaminated sites: a. In long-term experiments, U(IV), which was initially produced by microbial reduction of U(VI), could be reoxidized putatively using residual Fe(III) or Mn(IV) even under anaerobic conditions (Wan et al. 2005). b. Uranium that is associated with sediments is resistant to reduction (Ortiz-Bernad et al. 2004a). It has been shown that in the presence of nitrate and an electron donor such as acetate, both U(VI) and Tc(VII) can be reduced (Istok et al. 2004). Important conclusions were that (a) whereas reduction of Tc(VII) occurred concurrently with nitrate reduction, reduction of U(VI) took place only after Fe(II) was detected and (b) reoxidation of U(IV) took place in the presence of high—though not with low—concentrations of nitrate. The reductase in Geobacter sulfurreducens is located in the outer membrane, and a soluble Fe(III) reductase has been characterized from cells grown anaerobically with acetate as electron donor and Fe(III) citrate or fumarate as electron acceptor (Kaufmann and Lovley 2001). The enzyme contained Fe, acid-labile S, and FAD. An extracellular c-type cytochrome is distributed in the membranes, the periplasm, and the medium, and functions as a reductase for electron transfer to insoluble iron hydroxides, sulfur, or manganese dioxide (Seeliger et al. 1998). The molecular mass of 9.6 kDa suggested its similarity to cytochromes from sulfate-reducing bacteria, which was consistent with the fact that it contained three hemes although there is conlicting evidence on the role of this component (Lloyd et al. 1999). In contrast, Fe(III) reduction in the hyperthermophilic archaeon Pyrobaculum islandicum and in Pelobacter carbinolicus (Lovley et al. 1995) seems not to involve cytochromes (Childers and Lovley 2001). Although the hyperthermophilic sulfate-reducing archaeon Archaeoglobus fulgidus contains an Fe(III)–EDTA reductase, this shows sequence similarity to the family of NAD(P)H:FMN oxidoreductases (Vadas et al. 1999). Cell suspensions of Geobacter sulfurreducens can couple the oxidation of hydrogen to the reduction of Tc(VII) to insoluble Tc(IV). An indirect mechanism involving Fe(II) was also observed, and was substantially increased in the presence of the redox mediator AQDS (Lloyd et al. 2000).

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Geobacter metallireducens is also able to grow by vanadate respiration supported by acetate, and it has been suggested that this could provide a new strategy for removing vanadate from groundwater (Ortiz-Bernad et al. 2004b). Other Organisms 1. Sulfate-reducing bacteria: A number of sulfate-reducing anaerobic bacteria can oxidize S0 to sulfate at the expense of Mn(IV) (Lovley and Phillips 1994), and a strain of Desulfovibrio desulfuricans was able to use hydrogen to couple the reduction of Tc(VII) to an insoluble, more reduced form that was precipitated on the periphery of the cells (Lloyd et al. 1999). Reduction of U(VI) complexes with aliphatic carboxylates was examined using Desulfovibrio desulfuricans: the acetate complex was more rapidly reduced than those of dicarboxylates such as malonate, oxalate, and citrate, and the complex with 4,5dihydroxybenzene-1,3-disulfonate was readily accessible (Ganesh et al. 1997). In the presence of H2, Desulfovibrio fructosovorans was able to reduce Tc(VII) to soluble Tc(V) or putatively to an insoluble precipitate of Tc(IV), and this was mediated by the Ni–Fe hydrogenase in the organism (De Luca et al. 2001). 2. Deinococcus radiodurans strain R1: Anaerobic cultures grown with lactate could reduce chromate, although reduction was increased by the presence of electron transfer to AQDS. Reduction of U(VI) and Tc(VII) could also be accomplished in the presence of the electron transfer agent (Fredrickson et al. 2000). 3. Pyrobaculum aerophilum: Reduction of Cr(VI) to Cr(III), U(VI) to insoluble U(IV), and Tc(VII) to insoluble Tc(IV or V) was accomplished with this hyperthermophilic organism in the presence of H2 (Kashei and Lovley 2000). 4. Cellulomonas spp.: Under anaerobic conditions, several strains could carry out reduction of Cr(VI) and U(VI) at the expense of lactate (Sani et al. 2002). 5. Desulitobacterium metallireducens: Growth occurred with lactate using Fe(III) and MnO2 as electron acceptors, and Cr(VI) is also reduced (Finneran et al. 2002). 6. Anaeromyxobacter dehalogenans: This organism that is able to use ortho-substituted phenols for chlororespiration is able to use various forms of Fe(III) (He and Sanford 2003). All these transformations illustrate important processes for the cycling of organic carbon in sediments where Fe(III) has been precipitated, and it seems likely that comparable geochemical cycles involving manganese (Lovley and Phillips 1988) will also achieve greater prominence (Lovley 1991; Nealson and Myers 1992). It has also been suggested that such organisms could be used for the immobilization of soluble U(VI) in wastewater containing both U(VI) and organic compounds by conversion into insoluble U(IV) (Lovley et al. 1991). The reductases that produce the insoluble Cr(III) from chromate are noted in Part 3 of this chapter.

HUMIC ACID AND ANTHRAQUINONE-2,6-DISULFONATE IN REDOX SYSTEMS Humic acid and the corresponding fulvic acid are complex polymers whose structures are incompletely resolved. It is accepted that the structure of humic acid contains oxygenated structures, including quinones that can function as electron acceptors, while reduced humic acid may carry out reductions. These have been observed both in the presence of bacteria that provide the electron mediator and in the absence of bacteria in abiotic reactions, for example, reductive dehalogenation of hexachloroethane and tetrachloromethane by anthrahydroquininone-2,6-disulfonate (Curtis and Reinhard 1994). Reductions using sulide as electron donor have been noted in Chapter 1. Some experimental aspects are worth noting: a. Particularly in earlier experiments, a commercial preparation of humic acids, “Aldrich humic acid,” has been used and this differs signiicantly from the naturally occurring

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complex. Pure preparations are, however, now available from the International Humic Substances Society. b. Although AQDS has been used as a surrogate for the quinone structure of humic material, it differs from this in important respects including its water solubility and its redox potential. This applies equally to hydroquinone (H2AQDS). 1. Bacterial reduction of humic acid and AQDS: a. The frequency of humic-reducing bacteria has been assessed using AQDS as a surrogate for humic material and as electron acceptor, with acetate as electron donor. The organisms that were able to grow belonged to the Geobacteraceae and were able to reduce both humic acid and Fe(III) citrate, could therefore be signiicant in environments containing humic acid and Fe(III) (Coates et al. 1998). Geobacter metallireducens and G. grbiciae that were able to couple the oxidation of acetate or toluene to the reduction of Fe(III) could also use AQDS as electron acceptor (Coates et al. 2001). Desulitobacterium metallireducens was able to grow anaerobically by coupling the reduction of AQDS to the oxidation of lactate to acetate and CO2 (Finneran et al. 2002). In addition, with lactate as electron donor, 3-chloro-4-hydroxyphenylacetae, tetrachloroethene, and trichloroethene could serve as electron acceptors. b. Fermentative bacteria including Propionibacterium freudenreichii were able to reduce humic acids and to produce relatively greater amounts of oxidized products. Speciically, during growth with lactate there was an increase in the formation of acetate at the expense of propionate. Reduction of humic acid was also observed with the fermentative Lactococcus lactis and Enterococcus cecorum (Benz et al. 1998). 2. Bacteria have been isolated using reduced anthraquinone-2,6-disulfonate (H2AQDS) as electron donor and nitrate as electron acceptor (Coates et al. 2002). The organisms belonged to the α-, β-, γ-, and δ-subdivision of the Proteobacteria, and were able to couple the oxidation of H2AQDS to the reduction of nitrate with acetate as the carbon source. In addition, a number of C2 and C3 substrates could be used including propionate, butyrate, fumarate, lactate, citrate, and pyruvate. 3. The microbial degradation of contaminants under anaerobic conditions using humic acids as electron acceptors has been demonstrated. These included the oxidations: (a) chloroethene and 1,2-dichloroethene to CO2 that was conirmed using 14C-labeled substrates (Bradley et al. 1998) and (b) toluene to CO2 with AQDS or humic acid as electron acceptors (Cervantes et al. 2001). The transformation of 1,3,5-trinitro-1,3,5-triazine was accomplished using Geobacter metallireducens and humic material with AQDS as electron shuttle (Kwon and Finneran 2006). 4. In a wider context, extracellular redox mediators have been implicated in a number of reductions. The speciic role of reductive dehalogenation by porphyrins and corrins has been discussed in Chapter 1. a. The extracellular reductase from Geobacter sulfurreducens that is a c-type cytochrome can accept not only Fe(III) but also less readily AQDS and humic acids (Seeliger et al. 1998). b. The anaerobic reduction of azo dyes can be carried out by several bacteria including Sphingomonas xenophaga BN6 and Escherichia coli strain K-12 (Rau et al. 2002). During the degradation of naphthalene-2-sulfonate by Sphingomonas xenophaga BN6, 4-aminonaphtho-1,2-quinone and 4-ethanolaminonaphtho-1,2-quinone are produced and effectively enhance reduction by functioning as redox mediators (Keck et al. 2002). Analogously, the reduction of azo compounds by Escherichia coli is promoted by 2-hydroxy-1,4-naphthoquinone (lawsone) that is reduced by the O2-insensitive reductases NfsA and NfsB (Rau and Stolz 2003).

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c. The reduction of aromatic nitro compounds by the iltrate from a strain of Streptomyces sp. that is known to synthesize 2-amino-3-carboxy-5-hydroxybenzo-1,4-quinone (cinnaquinone) and the 6,6′-diquinone (dicinnaquinone) as secondary metabolites. The hydroquinone putatively carries out the reduction (Glaus et al. 1992).

DEHALORESPIRATION Dehalorespiration in which dehalogenation of chloroethenes is coupled to the synthesis of ATP has been demonstrated in a number of bacteria for several substrates and is discussed in Chapter 7, Part 3. Organisms include Sulfurospirillum (Dehalospirillum) multivorans, Dehalobacter restrictus, Desulfuromonas chloroethenica, and strains of Desulitobacterium including Desulf. hafniense and Desulf. chlororespirans (references in Holliger et al. 1999) that can carry out reductive dechlorination of tetrachloroethene. In addition, Dehalococcoides ethenogenes is exceptional in being capable of reductively dehalogenating tetrachloroethene to ethene (Maymó-Gatell et al. 1999; Magnuson et al. 2000), while Desulitobacterium hafniense (frappieri) has a wide spectrum of substrates that can be partially dechlorinated including chlorinated phenols, catechols, anilines, pentachloronitrobenzene, and pentachloropyridine (Dennie et al. 1998). The electron donors were generally H2 or pyruvate or methanol for Dehalococcoides ethenogenes. The chloroethene reductases contain cobalamin and Fe–S clusters, and the range of substrates for trichloroethene reductase from Dehalococcoides ethenogenes includes tribromoethene and bromoethene (Magnuson et al. 2000). In addition, the TCE reductive dehalogenase from this organism is able to debrominate substrates containing C2, C3, and C4 or C5 carbon atoms albeit with decreasing facility: illustrative reactions are the debromination of tribromoethene to dibromo-ethenes, vinyl bromide, and ethene. In a wider context, attention is drawn to debrominations carried out by methanogenic bacteria—ethene from 1,2-dibromoethane and ethyne from 1,2-dibromoethene (Belay and Daniels 1987). Details of these dehalogenations have emerged from studies with methanogens. The formation of ethene from 1,2-dichloroethane with hydrogen as electron donor has been demonstrated in cell extracts of Methanobacterium thermoautotrophicum DH, and in Methanosarcina barkeri it has been shown to involve cobalamin and F430 using Ti(III) as reductant (Holliger et al. 1992).

ALKANE SULFONATES AS TERMINAL ELECTRON ACCEPTORS A few aliphatic sulfonates such as 2-hydroxyethylsulfonate, alanine-3-sulfonate, and acetaldehyde2-sulfonate are able to serve as sulfur sources and electron acceptors during anaerobic growth of some sulfate-reducing bacteria when lactate is supplied as the carbon source (Lie et al. 1996). Several sulite-reducing species of Desulitobacterium are able to use 2-hydroxyethanesulfonate as terminal electron acceptor producing acetate and sulide (Lie et al. 1999). It is relevant to note that species of Desulitobacterium are also able to use chlorinated organic compounds and arsenate as terminal electron acceptors. Conversely, a strain of Rhodopseudomonas palustris isolated by enrichment with taurine was able to use this as a source of sulfur and nitrogen, and as electron source during photoautotrophic growth in the presence of CO2 (Novak et al. 2004).

NITROALKANES AS ELECTRON ACCEPTOR An anaerobic organism isolated from the rumen by enrichment for the metabolism of the toxic aglycone of miserotoxin (3-nitro-1-propyl-β-d-glucopyramnoside) was assigned to Denitrobacterium detoxiicans (Anderson et al. 2000). It was able to use a number of nitroalkanes including 3-nitropropanol, 3-nitropropionate, nitroethane, and 2-nitrobutane as electron acceptors during growth with lactate that was converted into acetate.

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Macy JM, S Rech, G Auling, M Dorsch, E Stackebrandt, LI Sly (1993) Thauera selenatis gen. nov., sp. nov., a member of the beta subclass of Proteobacteria with a novel type of anaerobic respiration. Int J Syst Bacteriol 43: 135–142. Magnuson JK, MF Romine, DR Burris, MT Kingsley (2000) Trichlorethene reductive dehalogenase from Dehalococcoides ethenogenes: squence of tceA and substrate characterization. Appl Environ Microbiol 66: 5141–5147. Maiers DT, PL Wichlacz, DL Thompson, DF Bruhn (1988) Selenate reduction by bacteria from a seleniumrich environment. Appl Environ Microbiol 54: 2591–2593. Malmqvist Å, T Welander, L Gunnarsson (1991) Anaerobic growth of microorganisms with chlorate as an electron acceptor. Appl Environ Microbiol 57: 2229–2232. Malmqvist Å, T Wellander, E Moore, A Ternström, G Molin, I-M Stenström (1994) Ideonella dechlorans gen. nov., sp. nov., a new bacterium capable of growing anaerobically with chlorate as electron acceptor. System Appl Microbiol 17: 58–64. Maymó-Gatell X, T Anguish, SH Zinder (1999) Reductive dechlorination of chlorinated ethenes and 1,2dichlooroethane by “Dehalococcoides ethenogenes” 195. Appl Environ Microbiol 65: 3108–3113. McEwan AG, JP Ridge, CA McDevitt, P Hugenholtz (2002) The DMSO reductase family of microbial molybdenum enzymes: molecular properties and the role in the dissimilatory reduction of toxic elements. Geomicrobiol J 19: 3–21. Moir JWB, DJ Richardson, SJ Ferguson (1995) The expression of redox proteins of denitriication in Thiosphaera pantropha grown with oxygen, nitrate, and nitrous oxide. Arch Microbiol 164: 43–49. Moreno-Vivián C, P Cabello, M Martínez-Luque, R Blasco, F Castillo (1999) Prokaryotic nitrate reduction: molecular properties and functional distinction among bacterial nitrate reductases. J Bacteriol 181: 6573–6584. Murphy MJ, LM Siegel, H Kamin (1973) Reduced nicotinamide adenine dinucleotide phosphate-sulite reductase of enterobacteria. II. Identiication of a new class of heme prosthetic group: an irontetrahydroporphyrin (isobacteriochlorin type) with eight carboxylic acid groups. J Biol Chem 248: 2801–3814. Myers CR, JD Myers (1997) Cloning and sequence of cymA, a gene encoding a tetraheme cytochrome c required for reduction of iron (III), fumarate, and nitrate by Shewanella putrefaciens MR-1. J Bacteriol 179: 1143–1152. Myers CR, KH Nealson (1990) Respiration-linked proton translocation coupled to anaerobic reduction of manganese(IV) and iron (III) in Shewanella putrefaciens. J Bacteriol 172: 6232–6238. Nagata K, H Yu, M Nishikawa, M Kashiba, A Nakamura, EF Sato, T Tamura, M Inoue (1998) Helicobacter pylori generates superoxide radicals and modulates nitric oxide metabolism. J Biol Chem 273: 14071–14073. Nealson KH, CR Myers (1992) Microbial reduction of manganese and iron: new approaches to carbon cycling. Appl Environ Microbiol 58: 439–443. Newman DK, EK Kennedy, JD Coates, D Ahmann, DJ Ellis, DR Lovley, FMM Morel (1997) Dissimilatory arsenate and sulfate reduction in Desulfotomaculum auripigmentum sp. nov. Arch Microbiol 168: 380–388. Niggemyer A, S Spring, E Stackebrandt, RF Rosenzweig (2001) Isolation and characterization of a novel As(V)-reducing bacterium: implication for arsenic mobilization and the genus Desulitobacterium. Appl Environ Microbiol 67: 5568–5580. Novak, RT, RF Gritzer, ER Leadbetter, W Godchaux (2004) Phototrophic utilization of taurine by the purple nonsulfur bacteria Rhodopseudomonas palustris and Rhodobacter sphaeroides. Microbiology (UK) 150: 1881–1891. Nozawa T, Y Maruyama (1988) Anaerobic metabolism of phthalate and other aromatic compounds by a denitrifying bacterium. J Bacteriol 170: 5778–5784. Oremland RS, SE Hoeft, JM Santini, N Bano, RA Hollibaugh, JT Hollibaugh (2002) Anaerobic oxidation of arsenite in Mono Lake water and by a facultative, arsenite-oxidizing chemoauthotroph strain MLHE-1. Appl Environ Microbiol 68: 4795–4802. Ortiz-Bernad I, RT Anderson, HA Vrionis, DR Lovley (2004a) Resistance of solid-phase U(VI) to microbial reduction during in situ bioremediation of uranium-contaminated groundwater. Appl Environ Microbiol 70: 7558–7560. Ortiz-Bernad I, RT Anderson, HA Vrionis, DR Lovley (2004b) Vanadium respiration by Geobacter metallireducens: novel strategy for in situ removal of vanadium from groundwater. Appl Environ Microbiol 70: 3091–3095.

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Picardal FW, RG Arnold, H Couch, AM Little, ME Smith (1993) Involvement of cytochromes in the anaerobic biotransformation of tetrachloromethane by Shewanella putrefaciens 200. Appl Environ Microbiol 59: 3763–3770. Price-Carter M, J Tingey, TA Bobik, JR Roth (2001) The alternative electron acceptor tetrathionate supports B12-dependent anaerobic growth of Salmonella enterica serovar typhimurium on ethanolamine or 1,2propandiol. J Bacteriol 183: 2463–2475. Rau J, A Stolz (2003) Oxygen-insensitive nitroreductases NfsA and NfsB of Escherichia coli function under anaerobic conditions as lawsone-dependent azo reductases. Appl Environ Microbiol 69: 3448–3455. Rau J, H-J Knackmuss, A Stolz (2002) Effects of different quinoid redox mediators on the anaerobic reduction of azo dyes by bacteria. Environ Sci Technol 36: 1497–1504. Renshaw JC, LJC Butchins, FR Livens, I May, JR Lloyd (2005) Bioreduction of uranium: environmental implications of a pentavalent intermediate. Environ Sci Technol 39: 5657–5660. Ridley H, CA Watts, DJ Richardson, CS Butler (2006) Resolution of distinct membrane-bound enzymes from Enterobacter cloacae SKLD1a-1 that are responsible for selective reduction of nitrate and selenate anions. Appl Environ Microbiol 72: 5173–5180. Rikken GB, AGM Croon, CG van Ginkel (1996) Transformation of perchlorate into chloride by a newly isolated bacterium: reduction and dismutation. Appl Microbiol Biotechnol 45: 420–426. Robertson LA, JG Kuenen (1984) Aerobic denitriication: a controversy revived. Arch Microbiol 139: 351–354. Saffarini DA, SL Blumerman, KJ Mansoorabadi (2002) Role of menaquinones in Fe(III) reduction by membrane fractions of Shewanella putrefaciens. J Bacteriol 184: 846–848. Saltikov CW, A Cifuentes, K Venkateswaran, DK Newman (2003) The ars detoxiication system is advantageous but not required for As(V) respiration by the genetically tractable Shewanella species strain ANA-3. Appl Environ Microbiol 69: 2800–2809. Saltikov CW, DK Newman (2003) Genetic identiication of a respiratory arsenate reductase. Proc Natl Acad Sci USA 100: 10983–10988. Saltikov CW, RA Wildman, DK Newman (2005) Expression dynamics of arsenic respiration and detoxiication in Shewanella sp. strain ANA-3. J Bacteriol 187: 7390–7396. Sani RK, BM Peyton, WA Smith, WA Apekl, JN Petersen (2002) Dissimilatory reduction of Cr(VI), Fe(III), and U(VI) by Cellulomonas isolates. Appl Microbiol Biotechnol 60: 192–199. Schmid MC et al. (2005) Biomarkers for in situ detection of anaerobic ammonium-oxidizing (Anammox) bacteria. Appl Environ Microbiol 71: 1677–1684. Schröder I, S Rech, T Krafft, JM Macey (1997) Puriication and characterization of the selenate reductase from Thauera selenatis. J Biol Chem 272: 23765–23768. Seeliger S, R Cord-Ruwisch B Schink (1998) A periplasmic and extracellular c-type cytochrome of Geobacter sulfurreducens acts as a ferric iron reductase and as an electron carried to other acceptors or to partner bacteria. J Bacteriol 180: 3686–3691. Servent D, C Ducrorq, Y Henry, A Guissani, M Lenfant (1991) Nitroglycerin metabolism by Phanerochaete chrysosporium: evidence for nitric oxide and nitrite formation. Biochim Biophys Acta 1074: 320–325. Stenklo K, HD Thorell, H Bergius, R Aasa, T Nilsson (2001) Chlorite dismutase from Ideonella dechloratans. J Biol Inorg Chem 6: 601–607. Stohl A, E Williams, G Wotawa, H Kromp-Kolb (1996) A European inventory of soil nitric oxide emissions and the effect of these emissions on the photochemical formation of ozone. Atmos Environ 30: 3741–3755. Stuehr DJ, J Santolini, Z-Q Wang, C-C Wei, S Adak (2004) Update on mechanism and catalytic regulation in the NO synthases. J Biol Chem 279: 36167–36170. Tal Y, JEM Watts, HJ Svchreier (2005) Anaerobic ammonia-oxidizing bacteria and related activity in Baltimore inner harbor sediment. Appl Environ Microbiol 71: 1816–1821. Taylor BF (1983) Aerobic and anaerobic catabolism of vanillic acid and some other methoxy-aromatic compounds by Pseudomonas sp. strain PN-1. Appl Environ Microbiol 46: 1286–1292. Taylor BF, MJ Heeb (1972) The anaerobic degradation of aromatic compounds by a denitrifying bacterium. Radioisotope and mutant studies. Arch Microbiol 83: 165–171. Thorell HD, K Stenklo, J Karlsson, T Nilsson (2003) A gene cluster for chlorate metabolism in Ideonella dechloratans. Appl Environ Microbiol 69: 5585–5592. Vadas A, HG Monbouquette, E Johnson, I Schröder (1999) Identiication and characterization of a novel ferric reductase from the hyperthermophilic archaeon Archaeoglobus fulgidus. J Biol Chem 274: 36715–36721.

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PART 3 REDUCTASES AND RELATED ENZYMES Reduction is an important reaction under both aerobic and anaerobic conditions. Reductases mediate a wide variety of reactions that are summarized briely here, and have been discussed in detail in Part 2 dealing with electron acceptors and further in Part 5 with metalloenzymes. The reductases that are components of the aromatic dioxygenases and that are involved in the aerobic bacterial degradation of aromatic hydrocarbons are noted parenthetically in Chapter 8, Parts 1 and 2.

REDUCTION OF NITROARENES Nitroarene reductases catalyze the reduction of nitroarenes. They are lavoprotein (FMN) enzymes (Blehert et al. 1999) and are of two types: 1. Type I are O2-insensitive six-electron reductases that catalyze the sequential reduction of nitroarenes to nitroso, hydroxylamino, and amino arenes. They are encoded in E. coli by NfsA for the major enzyme and NfsB for the minor (Rau and Stolz 2003), and are also important in establishing resistance to nitrofuran drugs (Koziarz et al. 1998). 2. Type II are O2-sensitive two-electron reductases that catalyze the reduction to ArNO2 radicals that react with O2 to produce superoxide (Bryant and DeLuca 1991; Bryant et al. 1991).

NITRATE ESTER REDUCTASE The degradation of aliphatic nitrate esters to nitrite and the corresponding alkanol takes place by a reductive rather than a hydrolytic mechanism. The reduction of glycerol trinitrate by Agrobacterium radiobacter (Snape et al. 1997) and of pentaerythritol tetranitrate by Enterobacter cloacae strain PB2 (French et al. 1996) have been described, and of lavoprotein reductases from Pseudomonas luorescens strain I-C (Blehert et al. 1999) have been characterized. They belong to a group of lavoproteins that are related to “old yellow enzyme” with varying substrate speciicities, and can reduce pentaerythritol tetranitrate, 1-nitrocyclohexene, cyclohex-2-enone, N-ethylmaleamide, and morphinone (Williams et al. 2004). It has been shown that hydrogen transfer in the reaction with NADH in pentaerythritol tetranitrate and morphinone reductase involves hydrogen tunneling in the reaction between the reduced lavin and the substrate (Basran et al. 2003).

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ENONES (α, β-UNSATURATED KETONES) AND RELATED REDUCTASES A group of lavoenzyme reductases mediate the reduction both nitrate esters and C=C double bonds generally activated with carbonyl or nitro functions. The structures of the substrates vary widely (references in Faber 1997). Aerobic Conditions 1. The reduction of cyclohex-2-ene-1-one to cyclohexanone is highly speciic in Pseudomonas syringae (Rohde et al. 1999), whereas the reductases from Saccharomyces cerevisiae are able to accept a wide range of activated aliphatic enones (Wanner and Tressel 1998). The related “old yellow enzyme” and pentaerythritol tetranitrate reductase can carry out reduction of androsta-∆1,4-3,17-dione to androsta-∆4-3,17-dione (Vaz et al. 1995), and prednisone to pregna-∆4-17α,20-diol-3,11,20-trione (Barna et al. 2001). Old yellow enzyme is also able to bring about the unusual dismutations of several conjugated cyclohexenones and cyclodecenones (Vaz et al. 1995) that are discussed in Chapter 7, part 2. 2. A reductase in Escherichia coli can reduce N-ethylmaleamide to N-ethylsuccinimide (Miura et al. 1997). 3. Morphinone can be reduced by Pseudomonas putida M10 to hydromorphone using an enzyme of which one of the subunits contains FMN (French and Bruce 1994). 4. The reductase from Burkholderia sp. strain WS produces (S)-2-chloropropionate from 2-chloroacrylate (Kurata et al. 2005). 5. An enzyme that catalyzes the reduction of ∆1-piperidein-2-carboxylate to piperidine-2-carboxylate (l-pipecolate) in the catabolism of d-lysine by Pseudomonas putida ATCC12633 is an NADPH-dependent representative of a large family of reductases that are distributed among bacteria and archaea (Muramatsu et al. 2005). It also catalyzes the reduction of ∆1-pyrrolidine-2-carboxylate to l-proline. Anaerobic Conditions 1. The reductases from Clostridium tyrobutyricum and Cl. kluyveri can reduce both aliphatic enoates and cinnamates to the dihydro compounds (Bühler and Simon 1982). The reductase in Cl. tyrobutyricum contains iron, labile sulfur, and both FAD and FMN (Kuno et al. 1985), while electron paramagnetic resonance (EPR) measurements suggest the presence of a semiquinone radical and Mössbauer spectra the presence of a [4Fe–4S] cluster (Caldeira et al. 1996). The amino acid sequences of these enzymes show similarity to a group of oxidoreductases and dehydrogenases, including the dehydrogenase for dimethylamine in Hyphomicrobium X and trimethylamine in Methylotrophus methylophilus (Rohdich et al. 2001). 2. Important reductions are involved in the anaerobic transformations of steroid and lavanoids: a. Reduction of a steroid 3-keto-4,6-diene to the 3-keto compound involved a complex sequence of reactions in a Clostridium sp. (Wells and Hylemon 2000), which is discussed in Chapter 7, Part 2. b. The reductions of the B-ring of lavanoids have been observed in Clostridium orbiscindens (Schoefer et al. 2003) and in Eubacterium ramulus (Braune et al. 2001), and these are noted again in Chapter 10, Part 2.

AZO REDUCTASE Reduction of the azo group in dyes and colorants is the key reaction in their decolorization. Although an azo reductase mediates the reduction of azo groups to amines, the metabolic situation is quite complex. The enzyme is apparently synthesized under both aerobic (Blümel et al. 2002) and

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anaerobic conditions (Rau et al. 2002; Rau and Stolz 2003), and the anaerobic reduction is facilitated by the presence of quinonoid mediators. The enzyme from Staphylococcus aureus is tetrameric with four noncovalently bound FMN and requires NADPH as reductant for activity (Chen et al. 2005).

ALDEHYDE OXIDOREDUCTASES There are diverse reactions that are mediated by aldehyde oxidoreductases: 1. The aerobic reduction of aryl and alkyl carboxylates to the corresponding aldehydes. The reaction involves formation of an acyl-AMP intermediate by reaction of the carboxylic acid with ATP; NADPH then reduces this to the aldehyde (Li and Rosazza 1998; He et al. 2004). The oxidoreductase from Nocardia sp. is able to accept a range of substituted benzoic acids, naphthoic acids, and a few heterocyclic carboxylic acids (Li and Rosazza 1997). 2. The phenylacetaldehyde reductase involved in the degradation of styrene is also able to accept long-chain aliphatic aldehydes and ketones, and halogenated acetophenones (Itoh et al. 1997). 3. There are several 2-ketoglutarate anaerobic oxidoreductases, for example, in Thauera aromatica (Dörner and Boll 2002) and Azoarcus evansii (Ebenau-Jehle et al. 2003). Their role in the metabolism of arene carboxylates is discussed in Chapter 8, Part 3. 4. The oxidoreductase from Pseudomonas diminuta strain 7 that carries out hydroxylation of isoquinoline at C2 is a molybdenum enzyme containing [Fe–S] centers, which is comparable to the aldehyde oxidoreductase from Desulfovibrio gigas (Lehmann et al. 1994).

F420-DEPENDENT (DESAZATETRAHYDROFOLATE) REDUCTASES These reductases play a key role both in methanogenesis and in the degradation of phenols that carry several nitro groups, which is discussed further in Chapter 9, Part 5. Although these reductases are typically found in methanogens, they have been encountered in a number of other bacteria and archaea: 1. Methanogenesis from CO2 via methenyl H4MPT, methylene H4MPT, and methyl H4MPT using coenzyme F420H2 (5,6,7,8-tetrahydrofolate). 2. Degradation of 2,4,6-trinitrophenol and 2,4-dinitrophenol involving a Meisenheimer hydride complex (Vorbeck et al. 1998; Behrend and Heesche-Wagner 1999; Ebert et al. 1999; Hofmann et al. 2004; Heiss et al. 2002). 3. The sulite reductase from the hyperthermophilic methanogen Methanocaldococcus jannashii is able to reduce the otherwise toxic sulite to sulide that is required for growth. In contrast to most organisms that use nicotinamides and cytochromes as electron carriers, this organism uses a coenzyme F420 –dependent reductase (Johnson and Mukhopadhyay 2005). 4. Glucose-6-phosphate is normally dehydrogenated to 6-phosphogluconate using an NADPdependent dehydrogenase. In Mycobacterium smegmatis strain mc26, however, the reaction is mediated by coenzyme F420, and neither NAD nor NADP was effective (Purwantini and Daniels 1996).

OTHER CARBOCYCLIC AROMATIC COMPOUNDS Reduction of Carbocyclic Rings Reductases play a cardinal role in the anaerobic degradation of diverse aromatic compounds, for example, (a) the reduction of benzoyl-CoA that is a prelude to the ission of the ring (Harwood et al. 1999) (Chapter 8, Part 3) and (b) the degradation of phloroglucinol via dihydrophloroglucinol to acetate and butyrate (Haddock and Ferry 1989, 1993) (Chapter 8, Part 4).

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Dehydroxylation The anaerobic degradation of some hydroxybenzoates and phenols involves reductive removal of the phenolic hydroxyl group. The enzyme that dehydroxylates 4-hydroxybenzoyl-CoA in Thauera aromatica is a molybdenum–lavin–iron–sulfur protein (Breese and Fuchs 1998), and is similar to the enzyme from the nonsulfur phototroph Rhodopseudomonas palustris that carries out the same reaction (Gibson et al. 1997). Reduction of Azaarene Rings The aerobic degradation of several azaarenes involves reduction of the rings at some stage, and are discussed in Chapter 10, Part 1. Illustrative examples include the degradation of pyridines (3-alkylpyridine, pyridoxal) and pyrimidines (catalyzed by dihydropyrimidine dehydrogenases). Reductions are involved in both the aerobic and the anaerobic degradation of uracil and orotic acid.

METAL CATIONS AND OXYANIONS Although some metal cations and oxyanions can serve as electron acceptors for growth under anaerobic conditions, reduction may also take place gratuitously, and these reductases have been characterized in a number of organisms. Reduction has been implicated in resistance to metal cations and metalloid oxyanions, which are discussed in Part 4 of this chapter. 1. Soluble reductases with a temperature optimum of 80°C have been described from (a) Pseudomonas putida that reduces chromate to insoluble Cr(III) (Park et al. 2000) and (b) Archaeoglobus fulgidus that can reduce Fe(III)–EDTA (Vadas et al. 1999). A membrane-bound chromate reductase has been puriied from Enterobacter cloacae (Wang et al. 1990). 2. Dimeric lavoprotein chromate reductases have been puriied from Pseudomonas putida (ChrR) and Escherichia coli (YieF). The former produces a semiquinone and transiently reactive oxygen species, whereas the latter is an obligate four-electron reductant. Oneelectron reduction of Cr(VI) to Cr(V) has, however, been observed as an intermediate in the reduction by the NAD(P)H-dependent reductase of Pseudomonas ambigua strain G-1 (Suzuki et al. 1992). 3. It has been shown that the nitroreductases from Escherichia coli and Vibrio harveyi are homologous to the chromate reductase from Pseudomonas ambigua (Kwak et al. 2003). 4. Reductase activity is located on the outer membranes of Shewanella putrefaciens and has a requirement for cytochrome c (Myers and Myers 1997) and menaquinones (Saffarini et al. 2002). 5. The reductase in Geobacter sulfurreducens is located in the outer membrane and a soluble Fe(III) reductase has been characterized from cells grown anaerobically with acetate as electron donor and Fe(III) citrate or fumarate as electron acceptor (Kaufmann and Lovley 2001). The enzyme contained Fe, acid-labile S, and FAD. An extracellular c-type cytochrome is distributed in the membranes, the periplasm, and the medium, and functions as a reductase for electron transfer to insoluble iron hydroxides, sulfur, or manganese dioxide (Seeliger et al. 1998). 6. The selenate reductase from Enterobacter cloacae SLD1a-1 functions only under aerobic conditions, and is not able to serve as an electron acceptor for anaerobic growth, in contrast to the periplasmic enzyme from Thauera selenatis (Schröder et al. 1997). In E. cloacae there are separate nitrate and selenate reductases, both of which are membrane-bound. The selenate reductase is able to reduce chlorate and bromate though not nitrate, contains Mo, heme and nonheme iron, and consists of three subunits in an α3β3γ3 coniguration.

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Hofmann KW, H-J Knackmuss, G Heiss (2004) Nitrite elimination and hydrolytic ring cleavage in 2,4,6-trinitrophenol (picric acid) degradation. Appl Environ Microbiol 70: 2854–2860. Itoh N, R Morihama, J Wang, K Okada, N Mizuguchi (1997) Puriication and characterization of phenylacetaldehyde reductase from a styrene-assimilating Corynebacterium strain, ST-10. Appl Environ Microbiol 63: 3783–3788. Johnson EF, B Mukhopadhyay (2005) A new type of sulite reductase, a novel coenzyme F420 -dependent enzyme, from the methanarchaeon Methanocaldocccus jannaschii. J Biol Chem 280: 38776–38786. Kaufmann F, DR Lovley (2001) Isolation and characterization of a soluble NADPH-dependent Fe(III) reductase from Geobacter sulfurreducens. J Bacteriol 183: 4468–4476. Koziarz JWP, J Veall, N Sandhu, P Kumar, B Hoecher, IB Lambert (1998) Oxygen-insensitive nitroreductases: analysis of the roles of nfsA and nfsB in development of resistance to 5-nitrofuran derivatives in Escherichia coli. J Bacteriol 180: 5529–5539. Kuno S, A Bacher, H Simon (1985) Structure of enoate reductase from a Clostridium tyrobutyricum (C. spec. La1). Biol Chem Hoppe-Seyler 366: 463–472. Kurata A, T Kurihara, H Kamachi, N Esaki (2005) 2-haloacrylate reductase: a novel enzyme of the mediumchain dehydrogenase/reductase superfamily that catalyzes the reduction of carbon–carbon double bond of unsaturated organohalogen compounds. J Biol Chem 280: 20286–20291. Kwak YH, DS Lee, HB Kim (2003) Vibrio harveyi nitroreductase is also a chromate reductase. Appl Environ Microbiol 69: 4390–4395. Lehmann M, B Tshisuaka, S Fetzner, P Röger, F Lingens (1994) Puriication and characterization of isoquinoline 1-oxidoreductase from Pseudomonas diminuta 7, a molybdenum-containing hydroxylase. J Biol Chem 269: 11254–11260. Li T, JPN Rosazza (1997) Puriication, characterization, and properties of an aryl aldehyde oxidoreductase from Nocardia sp. strain NRRL 5646. J Bacteriol 179: 3482–3487. Li T, JPN Rosazza (1998) NMR identiication of an acyl-adeylate intermediate in the aryl-aldehyde oxidoreductase catalyzsed reaction. J Biol Chem 273: 34230–34233. Miura K, Y Tomioka, H Suzuki, M Yonezawa, T Hishinuma, M Mizugaki (1997) Molecular cloning of the nemA gene encoding N-ethylmaleimide reductase from Escherichia coli. Biol Pharm Bull 20: 110–112. Muramatsu H, H Mihara, R Kakutani, M Yasuda, M Ueda, T Kurihara, N Esaki (2005) The putative malate/ lactate dehydrogenase from Pseudomonas putida is an NADPH-dependent ∆1-piperideine-2-carboxylate/∆1-pyrroline-2-carboxylate reductase involved in the catabolism of L-lysine and D-proline. J Biol Chem 280: 5329–5335. Myers CR, JD Myers (1997) Cloning and sequence of cymA, a gene encoding a tetraheme cytochrome c required for reduction of iron (III), fumarate, and nitrate by Shewanella putrefaciens MR-1. J Bacteriol 179: 1143–1152. Park CH, M Keyhan, B Wielinga, S Fendorf, A Matin (2000) Puriication to homogeneity and characterization of a novel Pseudomonas putida chromate reductase. Appl Environ Microbiol 66: 1788–1795. Purwantini E, L Daniels (1996) Puriication of a novel coenzyme F420 -dependent glucose-6-phosphate dehydrogenase from Mycobacterium smegmatis. J Bacteriol 178: 2861–2866. Rau J, A Stolz (2003) Oxygen-insensitive nitroreductases NfsA and NfsB of Escherichia coli function under anaerobic conditions as lawsone-dependent azo reductases. Appl Environ Microbiol 69: 3448–3455. Rau J, H-J Knackmuss, A Stolz (2002) Effects of different quinoid redox mediators on the anaerobic reduction of azo dyes by bacteria. Environ Sci Technol 36: 1497–1504. Ridley H, CA Watts, DJ Richardson, CS Butler (2006) Resolution of distinct membrane-bound enzymes from Enterobacter cloacae SKLD1a-1 that are responsible for selective reduction of nitrate and selenate anions. Appl Environ Microbiol 72: 5173–5180. Rohdich F, A Wiese, R Feiucht, H Simnon, A Bacher (2001) Enoate reductases of Clostridia. Cloning, sequencing, and expression. J Biol Chem 276: 5779–5787. Rohde BH, R Schmid, MS Ullrich (1999) Thermoregulated expression and characterization of an NAD(P)Hdependent 2-cyclohexen-1-one reductase in the plant pathogenic bacterium Pseudomonas syringae pv. glycinea J Bacteriol 181: 814–822. Saffarini DA, SL Blumerman, KJ Mansoorabadi (2002) Role of menaquinones in Fe(III) reduction by membrane fractions of Shewanella putrefaciens. J Bacteriol 184: 846–848. Schoefer L, R Mohan, A Schwiertz, A Braune, M Blaut (2003) Anaerobic degradation of lavonoids by Clostridium orbiscindens. Appl Environ Microbiol 69: 5849–5854. Schröder I, S Rech, T Krafft, JM Macey (1997) Puriication and characterization of the selenate reductase from Thauera selenatis. J Biol Chem 272: 23765–23768.

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Seeliger S, R Cord-Ruwisch, B Schink (1998) A periplasmic and extracellular c-type cytochrome of Geobacter sulfurreducens acts as a ferric iron reductase and as an electron carried to other acceptors or to partner bacteria. J Bacteriol 180: 3686–3691. Snape JR, NA Walkley, AP Morby, S Nicklin, GF White (1997) Puriication, properties, and sequence of glycerol trinitrate reductase from Agrobacterium radiobacter. J Bacteriol 179: 7796–7802. Suzuki T, N Miyata, H Horitsu, K Kawai, K Takamizawa, Y Tai, M Okazaki (1992) NAD(P)H-dependent chromium (VI) reductase of Pseudomonas ambigua G-1: a Cr(V) intermediate is formed during the reduction of Cr(VI) to Cr(III). J Bacteriol 174: 5340–5345. Vaz ADN, S Chakraborty, V Massey (1995) Old yellow enzyme: aromatization of cyclic enones and the mechanism of a novel dismutation reaction. Biochemistry 34: 4246–4256. Vorbeck C, H Lenke, P Fischer, JC Spain, H-J Knackmuss (1998) Initial reductive reactions in aerobic microbial metabolism of 2,4,6-trinitrotoluene. Appl Environ Microbiol 64: 246–252. Wang P, T Mori, K Toda, H Ohtake (1990) Membrane-associated chromate reductase activity from Enterobacter cloacae. J Bacteriol 172: 1670–1672. Wanner P, R Tressel (1998) Puriication and characterization of two enone reductases from Saccharomyces cerevisiae. Eur J Biochem 255: 271–278. Wells JE, PB Hylemon (2000) Identiication and characterization of a bile acid 7α-dehydroxylation operon in Clostridium sp. strain TO-931, a highly active 7α-dehydroxylating strain isolated from human feces. Appl Environ Microbiol 66: 1107–1113. Williams RE, DA Rathbone, NS Scrutton, NC Bruce (2004) Biotransformation of explosives by the Old Yellow Enzyme family of lavoproteins. Appl Environ Microbiol 70: 3566–3574.

PART 4 MICROBIAL REACTIONS TO CHEMICAL STRESS INTRODUCTION Microbial cells may be subjected to stress from a number of sources in their environment. These include antibiotics, metal cations and metalloid oxyanions, aromatic hydrocarbons, chlorophenols, and high acidity. Tolerance and resistance can be mediated by a number of mechanisms including modiication of the toxicant and the operation of effective eflux systems. Hydrocarbon Tolerance Gram-Negative Bacteria A number of pseudomonads have been shown to tolerate high concentrations of aromatic hydrocarbons. For example, a strain of P. putida DOT-T1 was able to grow in the presence of 90% (v/v) toluene, and with a range not only of aromatic hydrocarbons including toluene, styrene, ethylbenzene, but also long-chain n-alkanes (Ramos et al. 1995). Advantage of this tolerance was taken by using the hydroxylase (tmoABCDEF) from this strain to produce 4-hydroxytoluene that could then undergo successive side-chain oxidation to 4-hydroxybenzoate (Ramos-González et al. 2003). Bacterial degradation of highly lipophilic aromatic compounds including phenol and hydrocarbons such as toluene necessitates their resistance to potentially adverse effects, and a number of mechanisms whereby toxicity is overcome have been considered (Sikkema et al. 1995). This may be accomplished by alteration of the structure of their lipid membranes although none of the mechanisms that have been proposed are entirely conclusive or exclusive. Associated Alterations in Fatty Acid and Lipid Structure It is important to distinguish short-term from long-term responses. In Pseudomonas putida DOT-T1, which is a solvent-tolerant strain, the short-term response has been associated with transformation of cis-9,10-methylene hexadecanoic acid to 9-cis-hexadecenoate and then to the trans isomer (Ramos et al. 1997). Pseudomonas putida strain S12 is able to grow with concentrations of toluene up to 50% and growth with acetate in the presence of 1% toluene was accompanied by the replacement of cis unsaturated fatty acids with the trans isomers. This was maintained during several generations even in the absence of toluene (Weber et al. 1994). Enzymes that bring about the cis/trans

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isomerization of unsaturated fatty acids (Cti) have been described in Pseudomonas oleovorans GPo12 that has been cured of the plasmid determining the degradation of octanol (Pedrotta and Witholt 1999). Although greater activity could be shown in the presence of crude membrane preparations from Pseudomonas putida DOT-T1 in the presence of alcohols, the gene cti for this enzyme was present even in solvent-sensitive strains (Junker and Ramos 1999). Therefore, although the presence of this enzyme is important in alleviating short-term damage to solvents, it cannot be the primary cause of solvent resistance in this strain. It has been pointed out that details of how the organisms are harvested and the samples prepared could jeopardize the results, and that the cis–trans isomerization is competitive with the formation of cyclopropane fatty acids from the cis isomers (Härtig et al. 2005). The synthesis of classes of phospholipid (phosphatidylethanolamine, phosphatidylglycerol, cardiolipin, phosphatidic acid, and phosphatidylserine) was examined in two strains of Pseudomonas putida, neither of which could degrade o-xylene and one of which was tolerant to o-xylene. For all strains, there were alterations in the concentration of total phospholipid, with a decrease in the sensitive strain and an increase in the tolerant strain. The fatty acid composition of the lipids was also altered in the tolerant strain, with a general decrease in cis unsaturated and increase in trans unsaturated fatty acids (this has already been noted). There was a higher rate of phospholipid biosynthesis in the tolerant strain and this suggests that the tolerant strain was able to repair membranes damaged by o-xylene more effectively than the sensitive strain (Pinkart and White 1997). In a wider context, alterations in membrane structure are generally associated with environmental stress. For example, it has been shown in the archaeon Methanococcoides burtonii that the degree of unsaturated lipids in cells grown at 4°C was higher than in cells grown at 23°C, and that the degree of unsaturation is speciic for each class of phospholipid (Nichols et al. 2004). Efflux Pumps Gram-Negative Bacteria

An alternative—and possibly complementary—mechanism that is highly attractive is the existence of an eflux pump. Evidence has been provided for an energy-dependent export system in a toluene-resistant strain of Pseudomonas putida S-12 (Isken and de Bont 1996). The genes for this system have been cloned and their nucleotide sequence determined (Kieboom et al. 1998). Proteins coded by the three genes srpA, srpB, and srpC have extensive similarity to those for proton-dependent multidrug eflux systems, which are discussed in the section dealing with antibiotic resistance. In addition, the genes could be transferred to another strain of P. putida with the development of solvent resistance. Consistent with the role of the MexA-MexB-OprM operon that is expressed in Pseudomonas aeruginosa under normal growth conditions and that mediates antibiotic resistance, these genes also contribute to tolerance to n-hexane and p-xylene—though not toluene—in this strain (Li et al. 1998). As with antibiotic resistance, tolerance is abolished in the presence of the protonophore CCCP. In the toluene-resistant Pseudomonas putida DOT-T1E, three eflux pumps have been identiied. The TtGABC and TtgGHI pumps extruded toluene, m-xylene, ethylbenzene, and styrene, whereas TtgDEF extruded only toluene and styrene (Rojas et al. 2001). In addition, mutants lacking the TtgABC pump displayed reduced resistance to nalidixic acid, chloramphenicol, and tetracycline, whereas a mutant lacking Ttg GHI was as sensitive as the parent strain. An eflux system has been characterized in a strain of Pseudomonas luorescens cLP6a (Hearn et al. 2003). This system is selective for extrusion of phenanthrene, anthracene, and luoranthene, whereas it is inactive for toluene and naphthalene. Gram-Positive Bacteria

Hydrocarbon tolerance has also been found in Gram-positive rhodococci. Tolerance to high concentrations of benzene has been demonstrated in a strain of Rhodococcus that is, in addition, tolerant of pHs in the range 2–10 (Paje et al. 1997). For Rhodococcus opacus, resistance to benzene, toluene,

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phenol, and chlorobenzene was accompanied by an increase in the synthesis of 10-methyl branched fatty acids at the putative expense of their unsaturated fatty acids (Tsitko et al. 1999). A number of factors may therefore be involved in the tolerance of bacteria to aromatic hydrocarbons, although greatest attention has hitherto been centered on Gram-negative organisms. Antibiotic Resistance Strains of Streptomyces isolated from a range of urban, agricultural, and forest soils isolated on a standard medium displayed resistance to antibiotics that were well established in clinical practice. Resistance was found among all classes of antibiotics, and a disturbing number of isolates were resistant to between 5 and 10 of them (D’Costa et al. 2006). Resistance to a range of antibiotics is of increasing concern in clinical practice since the genes are often carried on transmissible plasmids. There are different types of mechanism that confer resistance, including enzymatic covalent modiication of the antibiotic, effective eflux systems, and induction of a cellular enzyme that is resistant to the antibiotic. Examples of these are used as illustration. Enzymatic Covalent Modification of Antibiotic—The Range of Reactions 1. Hydrolysis of penicillin mediated by penicillinase that has motivated attempts to alter its structure (e.g., in semisynthetic penicillins). 2. O-acetylation of chloramphenicol (Shaw and Leslie 1991) and zwittermicin A (Stohl et al. 1999). For chloramphenicol, the reaction is complex involving three reactions: (i) acetylation at C-3, (ii) nonenzymatic acetyl migration to C-1, followed by (iii) acetylation at C-3 to the 1,3-diacetyl compound. 3. O-phosphorylation of (a) chloramphenicol (Mosher et al. 1995) and spectinomycin that lead to resistance in Legionella pneumophila (Thompson et al. 1998) and (b) erythromycin at the 2′ position (Noguchi et al. 1995). 4. O-glucosylation of telithromycin at the 2′ position in Streptomyces sp. strain Ja#7 (D′Costa et al. 2006). 5. Reduction of 5-nitrofuran derivatives associated with mutation in aryl nitroreductases (Whiteway et al. 1998). 6. Monooxygenation of tetracycline by TetX (Yang et al. 2004). In contrast, resistance to isonicotinic acid hydrazide (INH) that is the frontline drug against Mycobacterium tuberculosis and the M. tuberculosis group—though not against M. leprae—illustrates the converse. INH is a prodrug that is converted into the active form, and resistance is achieved by mutation of the gene KatG that encodes a catalase-peroxidase (Bertrand et al. 2004). Details of the mechanism of activation are complex and two possibilities have been considered: 1. Activation by KatG to a range of products including isonicotinic acid and isonicotinaldehyde. This is supported by, for example, the mechanism of enzyme-catalyzed activation in peroxidases (Pierattelli et al. 2004), and the analogous activation of ethionamide by S-monooxygenation (DeBarber et al. 2000). Remarkably, the second-tier antituberculosis drug ethionamide is also a prodrug that is oxidized by an FAD-containing enzyme (EtaA) to the S-oxide and then to the amide (Vannelli et al. 2002). The initial reaction carried out by EtaA is a Baeyer–Villiger monooxygenation that functions typically with other substrates including 4-thiomethyltoluene and ketones (Fraaije et al. 2004). 2. The role of NO is supported by several lines of evidence: a. Its formation has been shown by electron paramagnetic spin resonance using 15N-labelled INH, and CPTIO, which is a speciic scavenger of NO-provided protection against INH activity in liquid cultures of Mycobacterium tuberculosis (Timmins et al. 2004).

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b. Formation of nitrotyrosine by nitric oxide carriers during oxidation of INH (Van Zyl and van der Walt 1994). c. Incorporation into ciproloxacin of an ester with a terminal –O–NO2 group that can release NO stimulates its activity against M. tuberculosis (Ciccone et al. 2003). An alternative and not necessarily conlicting view is the formation of a free radical at a tyrosine center that was trapped by adding NO to form 3-nitrotyrosine (Zhao et al. 2004). Efflux Systems An alternative to most of these mechanisms is the existence of eficient eflux systems, so that toxic concentrations of the drug are not achieved. There are three major families of proton-dependent multidrug eflux systems: (1) the major facilitator superfamily, (2) the small multidrug resistance family, and (3) the resistance/nodulation/cell division family (Paulsen et al. 1996). It should be emphasized that several of these systems are involved not with antibiotic eflux but with, for example, acrilavine, chlorhexidine, and crystal violet. An attempt is made only to outline a few salient features of the resistance/nodulation/cell division family that mediates antibiotic eflux, and these are given in Table 3.3 (Nikaido 1996). They consist of a transporter, a linker, and an outer membrane channel. Alteration of an Essential Reaction that is Normally Inhibited The macrolide erythromycin inhibits protein synthesis and resistance is induced by N6 -dimethylation of adenine within the 23S rRNA, which results in reduced afinity of ribosomes for antibiotics related to erythromcin (Skinner et al. 1983). Sulfonamides function by binding tightly to chromosomal dihydropteroate synthetase and resistance to sulfonamides is developed in the resistance plasmid through a form of the enzyme that is resistant to the effect of sulfonamides. Antifungal Agents This is not discussed in detail since mechanisms of resistance have been carefully reviewed (Ghannoum and Rice 1999). It was pointed out that resistance has not been associated with modiication of the structure. For the 1,2,4-triazoles that have been widely used, their effect is due to inhibition of the synthesis of ergosterol that is the dominant component of fungal cell membranes. Resistance is generally associated with modiication of the target enzymes, for example, the epoxidation of squalene (Terbinaine) or 14α-demethylase (Fluconazole). Resistance of Candida albicans to the azole antifungal agent luconazole demonstrated, however, the simultaneous occurrence of several types of mechanism for resistance (Perea et al. 2001): a. Levels in expression of the genes encoding lanosterol 14α-demethylase (ERG11) both by overexpression that necessitates higher intracellular concentration of the drug and by point mutations that result in diminished afinity for the drug. b. The existence of multidrug eflux transporters including both MDR1 and CDR. TABLE 3.3 Summary of Resistance/Nodulation/–Cell Division Family Transporter

Linker

Outer Membrane Channel

Organism

Substrates

AcrB MexB MtrD

AcrA MexA MtrC

TolC OprM MtrE

E. coli P. aeruginosa Neisseria gonorrhoeae

TC, CA, FQ, ERY, NOV, RIF, β-LAC TC, CP, FQ, β-LAC TC, CP, β-LAC, RIF

Note: TC, tetracycline; CA, chloramphenicol; FQ, luoroquinoline; ERY, erythromycin; NOV, novobiocin; RIF, rifampin; and β-LAC, β-lactam.

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Many yeasts are inhibited by 5-luorocytosine and a block in the synthesis of 5-luorouridylic acid by loss of cytosine deaminase or of uracil phosphoribosyltransferase is suficient to cause resistance. Mutational loss of pyrimidine salvage enzymes has been frequently observed.

RESISTANCE TO METALS AND METALLOIDS There is concern over the toxicity of a number of metals and metalloids, and their oxyanions. As for antibiotics, the genes for resistance are often plasmid-borne. There are several mechanisms that may operate—reduction, methylation, eflux, and the synthesis of metal-binding metallothioneins. The following text illustrates aspects of these mechanisms. Reduction Reduction to less toxic forms, for example, Hg2+ to Hg0, CrO42− to Cr3+, U(VI) to U(IV), SeO32− to Se0, TeO32− to Te0, and AsO43− to AsO33−. Extrusion of the reduced form may also be involved in, for example, Se0, Te0, and AsO32− so that synthesis of the more toxic AsO32− is circumvented. Mercury Mercuric reductase is a key enzyme in detoxifying inorganic mercury (Hg2+) by reducing it to the nontoxic Hg0. The reductase in a range of rapid-growing mycobacteria from clinical sources increased from 20- to >100-fold after exposure to HgCl2 (Steingrube et al. 1991). The reductases from the plasmid-carrying Escherichia coli strain J53-1(R831) (Schottel 1978) and from Pseudomonas aeruginosa carrying the plasmid pVS1 (Fox and Walsh 1982) have been puriied and both contained FAD. The enzyme from the latter was shown to contain two thiol groups that are released after reduction with NADPH, and was considered to be similar to lipoamide dehydrogenases. The degradation of phenylmercuric acetate to benzene, methylmercuric chloride to methane, and ethylmercuric chloride to ethane and Hg2+ is apparently carried out by different enzymes from the plasmid-carrying Escherichia coli strain K12 (R831) (Schottel 1978) and Pseudomonas sp. Resistance to organic mercury compounds has also been found in clinical isolates of nontuberculous, rapidly growing mycobacteria (Steingrube et al. 1991) and can present a challenge in the clinical environment. Chromium Although reduction of chromate CrVI to CrIII has been observed in a number of bacteria, these are not necessarily associated with chromate resistance. For example, reduction of chromate has been observed with cytochrome c3 in Desulfovibrio vulgaris (Lovley and Phillips 1994), soluble chromate reductase has been puriied from Pseudomonas putida (Park et al. 2000), and a membrane-bound reductase has been puriied from Enterobacter cloacae (Wang et al. 1990). The lavoprotein reductases from Pseudomonas putida (ChrR) and Escherichia coli (YieF) have been puriied and can reduce Cr(VI) to Cr(III) (Ackerley et al. 2004). Whereas ChrR generated a semiquinone and reactive oxygen species, YieR yielded no semiquinone, and is apparently an obligate four-electron reductant. It could therefore present a suitable enzyme for bioremediation. Arsenic and Antimony A number of redox systems are involved in microbial reactions that confer resistance to inorganic arsenic (Silver and Phung 2005). The arsenate reductase gene ArsC both in Staphylococcus aureus (Ji and Silver 1992) and in Escherichia coli (Liu et al. 1995) is a determinant of arsenate resistance, and the arsenite that is produced is extruded from the cell by the ArsA–ArsB anion-translocating ATPase (Walmsley et al. 1999). In contrast, ArsB catalyzes arsenite extrusion coupled to electrochemical energy, and transport of Sb(III) into E. coli is catalyzed by the ArsB carrier protein (Meng et al. 2004). Another mechanism for detoxiication of As(III) has been found in the legume symbiont Sinorhizobium meliloti. In the operon that is involved in As(III) detoxiication, the arsb gene is replaced by aqpS that encodes an aquaglyceroporin. AqpS therefore confers resistance to arsenate

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by facilitated extrusion of arsenite produced by ArsC-catalyzed reduction of arsenate (Yang et al. 2005). In contrast, it has been proposed that in Escherichia coli the polyol transporter GlpF accumulates both arsenite and the analogous antimonite. Arsenite is also an intermediate in the fungal biomethylation of arsenic (Bentley and Chasteen 2002) and oxidation to the less toxic arsenate can be accomplished by heterotrophic bacteria including Alcaligenes faecalis. Exceptionally, arsenite can serve as electron donor for chemolithotrophic growth of an organism designated NT-26 (Santini et al. 2000), and both selenate and arsenate can be involved in dissimilation reactions as alternative electron acceptors. In a wider context, reduction of Sb(V) in the native drug to Sb(III) is required for the activity of preferred drugs for the treatment of leishmaniasis, and is supported by the following evidence. The sequence for the arsenate reductase ScAcr2p in Saccharomyces cerevisiae was used to clone the homolog LmACR2 in Leishmania major, and it was shown that the puriied enzyme was able to reduce both As(V) and Sb(V). In addition, transfection of L. infantum with LmACR2 increased the sensitivity of amastigotes to the Sb(V) drug Pentostam (Zhou et al. 2004). Selenium and Tellurium Whereas selenium is a necessary trace element particularly for anaerobic bacteria, tellurium is not known to play an essential role. Both selenite (SeO32−) and tellurite (TeO32−) can be toxic, and in Escherichia coli, selenite is able to induce the genes for Mn and Fe superoxide dismutases that may be protective under aerobic conditions (Bébien et al. 2002). Resistance to selenite and tellurite can be developed in a range of bacteria. A number of controversial mechanisms have been proposed for the reduction of SeO32− to Se0, and the involvement of glutathione has been suggested on the plausible basis of a chemical analogy (Kessi and Hanselmann 2004). In resistant bacteria related to the genus Pseudoalteromonas (Rathgeber et al. 2002) and in Shewanella oneidensis (Klonowska et al. 2005), the selenite that has been reduced to Se0 can be extruded from the cells, whereas the Te0 that is produced from tellurite is located within the cells. As for the mechanism of reduction, several reasons have been adduced for resistance to selenite and tellurite. In Escherichia coli, tellurite resistance has been associated with the activity of nitrate reductase (Avazéri et al. 1997; Sabaty et al. 2001). The ars operon on the plasmid R773, which functions as an anion-translocating ATPase for arsenite, arsenate, and antimonite, provides moderate resistance also to tellurite (Turner et al. 1992). In the Gram-positive Geobacillus stearothermophilus, which is naturally resistant to tellurite, transfer of the iscS gene that encodes cysteine desulfurase into E. coli confers tellurite resistance (Tantaleán et al. 2003). Detoxiication of tellurite has also been attributed to methyltransferase activity involving S-adenosymethionine (Liu et al. 2000) or thiopurine methyltransferase (Cournoyer et al. 1998), even when the expected methylated products were not observed (Liu et al. 2000). Selenate can be reduced to Se0 via selenite in Enterobacter cloacae SLD1a-1 (Losi and Frankenberger 1997), although it cannot be used as an electron acceptor for anaerobic growth (Ridley et al. 2006). Selenate can also serve as an electron acceptor, which is discussed in Part 2 of this chapter. Although in Rhodobacter sphaeroides (Van Fleet-Stalder et al. 2000) and in the metal-resistant Ralstonia metallidurans CH34 (Sarret et al. 2005), both reduction of selenite to Se0 and formation of organic selenium may take place, reduction appears to be the dominant reaction. Methylation Methylation of both metals and metalloids has been observed for both fungi and bacteria. These metabolites may, however, be toxic to higher biota as a result of their volatility. The Minamata syndrome represents the classic example of the toxicity of forms of methylated Hg to man, even though the formation of Hg(CH3)2 was probably the result of both biotic and abiotic reactions. Transmethylation is important not only in the biosynthesis of cellular components but also in detoxiication. Although the resulting metabolites are less toxic to the cell, they are often more lipophilic and may have serious adverse effects on other biota. Toxic volatile arsenic compounds

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produced from inorganic. As were among the irst examples, and methylmercury is a well-established toxicant both to wildlife and humans. Transmethylation is also involved in the degradation of methyl halides by the corrinoid pathway. Alkylated compounds were previously of industrial importance, for example, tetraethyl lead as an antiknock in gasoline engines and butyltin compounds as biocides. Biogeochemical cycles must take into account biogenic and anthropogenic inputs as well as biogenic and abiotic degradation and transformation. Monitoring has revealed the presence in the environment of a wide variety of methylated metals and metalloids. In the following summary, however, attention is directed only to results that conclusively demonstrate methylation under controlled laboratory conditions. Reference should be made to substantive reviews with extensive bibliographies dealing with methylation of metals and metalloids (Thayer 2002; Chasteen and Bentley 2002; Bentley and Chasteen 2003). A cardinal issue is the species of the metal or metalloid that is examined. Metals such as mercury or tin are methylated from cationic Hg2+ or Sn4+, whereas the metalloids are transformed from the oxyanions of As, Sb, Se, or Te. The classical Challenger mechanism that involves sequential reductions and methylations is well established, at least for fungal methylation of the oxyanions of As (Bentley and Chasteen 2002), and Se—and is assumed to be—for Te (Chasteen and Bentley 2003). Methylation may take place under aerobic conditions for fungi or anaerobic conditions for bacteria. Formation of methylated derivatives may occur in metals and metalloids belonging to groups 15 and 16, and a few of group 14 of the periodic table, and have been discussed in a critical review (Thayer 2002). Although bacteria can carry out several of the methylations, fungal methylation is probably most widely distributed, for example, of As and Sb (Tamaki and Frankenberger 1992; Bentley and Chasteen 2002), and Se and Te (Chasteen and Bentley 2003). Although the mechanism has not been established for all methylations, methyl transferases generally use either S-adenosylmethionine or methylcobalamin as methyl donors. In contrast, methylation of selenite in Escherichia coli is carried out by the activity of thiopurine methyltransferase (Ranjard et al. 2003). Methylation of mercury seems, however, to be carried out only by bacteria, although the mechanisms for methylation under anaerobic conditions have not been inally resolved (Bentley and Chasteen 2002). Sulfate-reducing bacteria are generally presumed to be the primary source of HgCH3 under anaerobic conditions (Choi et al. 1994; King et al. 2000), and generally use methylcobalamin as methyl donor. Methylation may also take place by reactions, which do not involve methylcobalamin (Ekstrom et al. 2003). It has been shown that Geobacter strain CLFeRB was able to carry out methylation of Hg2+ at a rate comparable to that of Desulfobulbus propionicus strain Ipr3 (Fleming et al. 2006). Under anaerobic conditions, methanogenic archaeons use pathways that probably involve methylcobalamin for the methylation of arsenate to dimethylarsine (McBride and Wolfe 1971); arsenate to mono-, di-, and trimethylarsines; SbCl3 to trimethylstibine; and Bi(NO3)3 to trimethylbismuth (Michalke et al. 2000). Conversely, among the organic arsenic compounds that were evaluated, only methylarsine appreciably inhibited acetoclastic methanogenesis (SierraAlvarez et al. 2004). Under aerobic conditions, S-adenosylmethionine is the methyl donor for methylation of methanethiol and methaneselenol (Drotar et al. 1987), and probably for the bacterial methylation of halogenated phenols and thiophenols (Neilson et al. 1988). It is also the probable methyl donor for fungal methylation of the oxyanions of As and Sb (Bentley and Chasteen 2002). Although the pathway has not been established, relatively high yields of trimethyltin from inorganic tin have been observed in yeast concomitant with the degradation of butyltin compounds (Errécalde et al. 1995). Exceptionally, methionine transferase may carry out the methylation of Hg in Neurospora crassa (Landner 1971) and thiopurine methyltransferase the methylation of inorganic Se in Escherichia coli (Ranjard et al. 2003). Although their source has not been identiied, it has been shown that volatile compounds from landills contain carbonyls of Mo and W in addition to the known hydrides and methylated derivatives of As, Se, Sn, Sb, Te, Hg, Pb, and Bi (Feldmann and Cullen 1997).

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Efflux Systems As for antibiotics, resistance to toxic cations may be mediated by the existence of eflux systems that have been discussed in reviews (Silver and Phung 1996; Mergeay et al. 2003; Nies 2003). A great deal of attention has been directed to Ralstonia metallidurans that has masqueraded under several names—Alcaligenes eutropha, Ralstonia eutropha, and Achromobacter xylosoxidans—and details of the mechanisms have been presented in a review (Mergeay et al. 2003). In this brief summary of eflux systems that alleviate heavy metal toxicity, the convenient system of classiication used by Nies (2003) will be adopted. The range of metals in this section is restricted to resistance to the divalent cations of Zn, Cd, Co, and Ni, and the monovalent Cu and Ag, and occurs in a range of bacteria and a few yeasts. Mechanisms for resistance to mercury have already been discussed, and chromate resistance in Pseudomonas aeruginosa is achieved by an eflux system that is driven by the membrane potential (Alvarez et al. 1999). a. The resistance–nodulation–cell division (RND) family of proteins. In Ralstonia metallidurans the CzcA protein mediates resistance to Zn2+, Cd2+, Co2+, and Ni2+ in two megaplasmids, one associated (pMOL30) with resistance to Cd2+, Zn2+, and Co2+, the other (pMOL28) with increased resistance to Co2+ and Ni2+. In Escherichia coli, resistance to copper is mediated by a periplasmic protein (CusF). b. Cation-diffusion facilitators (CDF). The primary substrate for the protein is Zn2+, although other divalent cations including Ni2+ and Co2+, may also be effective. Transport is driven by gradients of several types—concentration, chemiosmotic ∆ψ or ∆pH, or potassium, and most studies have examined R. metallidurans in which the encoding genes are chromosomal, although species of Saccharomyces have also been included. c. P-type ATPases. These function both as uptake and as eflux mediators, and one family is involved in the speciic eflux of monovalent Cu+ and Ag+, but not Cu2+, and has been examined in Gram-positive bacteria and the archaeon Archaeoglobus fulgidus. Another family that is involved in eflux of Zn2+/Cd2+/Pb2+ has been found in Gram-negative bacteria and yeast. Polyphosphates There is some evidence for the role of phosphate produced by hydrolysis of polyphosphates in metal tolerance and remediation. Polyphosphates are accumulated by many bacteria and serve as an energy source and for chelating metal cations. Their biosynthesis is mediated by a kinase ppk that catalyzes their formation from the terminal phosphate of ATP, while an exopolyphosphatase ppx brings about their hydrolysis to inorganic phosphate. It has been suggested that the extruded phosphate could bind metal cations and therefore lead to the development of resistance to the toxic cation. For example, the thermophilic archaeon Sulfolobus metallicus was highly resistant to Cu2+ during the concomitant decrease in the level of polyphosphate, increase in the level of exopolyphosphatase, and the eflux of phosphate (Remonsellez et al. 2006). Overexpression of the polyphosphate kinase gene in Pseudomonas aeruginosa induced accumulation of polyphosphate that could be mobilized under conditions of carbon starvation with the release of phosphate into the medium. Phosphate was utilized to remove UO22+ from solution that was initially precipitated on the cell walls (Renninger et al. 2004). Metallothionein Metallothioneins are proteins that are rich in cysteine residues, and the genes encoding them are found in eukaryotes and a few prokaryotes. Although they have been found in a wide range of biota, their function has not been inally resolved, and different roles have been assigned to them (Palmiter 1998). To demonstrate their function in metal resistance, it is necessary to show not only their presence, but also that the genes encoding them are ampliied after exposure to the metal. Resistance has been explored extensively for copper that can produce reactive oxygen species with

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consequent cellular damage. At the same time, copper is necessary for the functioning of several cellular enzymes. Homeostasis is maintained by regulation. Whereas this can be maintained in prokaryotes by P1-type ATPases in combination with a regulatory protein, for example, in Pseudomonas putida (Adaikkalam and Swarup 2002), tolerance may also be mediated by metallothioneins. They have been found in a few cyanobacteria within the genus Synechococcus (Turner and Robinson 1992), and the structure in strain Tx-20 has been elucidated (Olafson et al. 1988). It has been shown in a culture of Synechococcus PCC 6301 adapted to Cd2+ that ampliication of the smtAB genes took place, and that multiple copies of them were found after exposure to Cd2+ to which the cells are resistant (Gupta et al. 1992). Genes homologous to these have also been found in Cd-resistant strains of sulfate-reducing bacteria. Metal-translocating ATPases were, however, also found in two of the strains (Naz et al. 2005), so that several mechanisms of resistance could be involved. Substantial studies have been directed to yeasts. Several studies have examined the resistance to Cu2+ and Ag+ in the yeast Candida. In C. albicans, genes encoding a P1-type ATPase, and one encoding a metallothionein were cloned, and their expression studied in response to Cu2+. Transcription of only the former increased with increasing levels of Cu2+, so that this was putatively the primary determinant of resistance (Riggle and Kumamoto 2000). A similar study showed that extracellular Cu2+ induced the genes for a metallothionein (CaCUP1) and a P-type ATPase (CaCRP1). The former was responsible for the unusual resistance of C. albicans to copper, whereas the latter was essential for survival under conditions of low copper concentration (Weissman et al. 2000). In Candida glabrata, whereas glutathione-related (γEC)nF peptides are induced by Cd2+, metallothioneins encoded by the genes MT-1 and MT-2 are induced by Cu2+. In cells induced by increasing concentrations of Cu, chromosomal ampliication of the MT-II took place, whereas the MT-I gene remained as a single copy and was shown to map on different chromosomes (Mehra et al. 1990). Although protection from copper toxicity in Saccharomyces cerevisiae involves a metallothionein encoded by CUP1, an additional element encoded by CRS5 that is regulated by both Cu2+ and by oxidative stress possesses a metallothionein-like amino acid sequence (Culotta et al. 1994). It is therefore clear that care should be exercised in assigning metallothioneins to a cardinal role in conferring resistance to metals. Chlorophenol Tolerance There are two putative mechanisms whereby bacteria become resistant to polychlorinated phenols. These are illustrated by the following examples: 1. Two strains of Sphingomonas sp. that could degrade pentachlorophenol maintained their levels of ATP even in the presence of high concentrations of pentachlorophenol. Analysis of the lipids using 31P NMR showed that this could be attributed to the increased levels of cardiolipin (Lohmeier-Vogel et al. 2001). 2. O-methylation has been shown in a range of halogenated phenols and thiophenols (Neilson et al. 1988), thiophenols (Drotar and Fall 1985), and methanethiol and methaneselenol (Drotar et al. 1987). Methylation has been putatively attributed to reaction with S-adenosylmethionine. Resistance to High Acidity Some bacteria are able to withstand high acidity in their surroundings, and for some pathogens this is critical for their survival. Some details of this are given in Chapter 7, Part 1, and it is suficient here to merely note the existence of mechanisms whereby the decarboxylation of aminoacids serves to remove protons from the medium.

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Santini JM, LI Sly, RD Schnagl, JM Macy (2000) A new chemolithoautotrophic arsenite-oxidizing bacterium isolated from a gold mine: phylogenetic, physiological and preliminary biochemical studies. Appl Environ Microbiol 66: 92–97. Sarret G, L Avoscan, M Carrière, R Collins, N Geoffroy, F Carrot, J Covès, B Gouget (2005) Chemical forms of selenium in the metal-resistant bacterium Ralstonia metallireducens CH34 exposed to selenite and selenate. Appl Environ Microbiol 71: 231–2337. Schottel JL (1978) The mercuric and organomercurial detoxifying enzymes from a plasmid-bearing strain of Escherichia coli. J Biol Chem 253: 4341–4349. Shaw WV, AGW Leslie (1991) Chloramphenicol acetyltransferase. Annu Rev Biophys Chem 20: 363–386. Sierra-Alvarez R, I Cortinas, U Venal, JA Field (2004) Methanogenesis inhibited by arsenic compounds. Appl Environ Microbiol 70: 5688–5691. Sikkema J, JAM de Bont, B Poolman (1995) Mechanisms of membrane toxicity of hydrocarbons. Microbiol Rev 59: 201–222. Silver S, LT Phung (1996) Bacterial heavy metal resistance: new surprizes. Annu Rev Microbiol 50: 753–789. Silver S, LT Phung (2005) Genes and enzymes in bacterial oxidation and reduction of inorganic arsenic. Appl Environ Microbiol 71: 599–608. Skinner R, E Cundliffe, FJ Schmidt (1983) Site of action of a ribosomal RNA methylase responsible for resistance to erythromycin and other antibiotics. J Biol Chem 258: 12702–12706. Steingrube VA, RJ Wallace, LC Steele, Y Pang (1991) Mercuric reductase activity and evidence of broadspectrum mercury resistance among clinical isolates of rapidly growing mycobacteria. Antimicrob Agents Chemother 35: 819–823. Stohl EA, SF Brady, J Clarty, J Handelsman (1999) ZmaR, a novel and widespread antibiotic resistance that acetylates zwittermicin A. J Bacteriol 181: 5455–5460. Tamaki S, WT Frankenberger (1992) Environmental biochemistry of arsenic. Rev Environ Contam Toxicol 124: 79–110. Tantaleán JC, MA Araya. CP Saavedra, DE Fuementes, JM Pérez, IL Calderón, P Youderian, CC Vásquez (2003) The Geobacillus stearothermophilus V iscS gene, encoding cysteine desulfurase, confers resistance to potassium tellurite in Escherichia coli. J Bacteriol 185: 5831–5837. Thayer JS (2002) Biological methylation of less-studied elements. Appl Organometal Chem 16: 677–691. Thompson PR, DW Hughes, NP Cianciotto, GD Wright (1998) Spectinomycin kinase from Legionella pneumoniae. J Biol Chem 273: 14788–14795. Timmins GS, S Master, F Rusnak, V Deretic (2004) Nitric oxide generated from isoniazid activation by KatG: source of nitric oxide and activity against tunerculosis. Antimicrob Agents Chemother 48: 3006–3009. Tsitko IV, GM Zaitsev, AG Lobanok, MS Salkinoja-Salonen (1999) Effect of aromatic compounds on cellular fatty acid composition of Rhodococcus opacus. Appl Environ Microbiol 65: 853–855. Turner JS, NJ Robinson (1992) Cyanobacterial metallothioneins: biochemistry and molecular genetics. J Ind. Microbiol 14: 119–125. Turner RJ, Y Hou, JH Weiner, DE Taylor (1992) The arsenical APTase eflux pump mediates tellurite resistance. J Bacteriol 174: 3092–3094. Van Fleet-Stalder V, TG Chasteen, IJ Pickering, GN George, RC Prince (2000) Fate of selenate and selenite metabolized by Rhodobacter sphaeroides. Appl Environ Microbiol 66: 4849–4853. Van Zyl JM, BJ van der Walt (1994) Apparent hydroxyl radical generation without transition metal catalysts and tyrosine nitration during oxidation of the anti-tubercular drug, isonicotinic acid hydrazide. Biochem Pharmacol 48: 2033–2042. Vannelli TA, A Dykman, PR Ortiz de Montellano (2002) The antituberculosis drug ethionamide is activated by a lavin monooxygenase. J Biol Chem 277: 12824–12829. Walmsley AR, T Zhou, MI Boirges-Walmsley, BP Rosen (1999) The ATPase mechanism of ArsA, the catalytic subunit of the arsenite pump. J Biol Chem 274: 16153–16161. Wang P, T Mori, K Toda, H Ohtake (1990) Membrane-associated chromate reductase activity from Enterobacter cloacae. J Bacteriol 172: 1670–1672. Weber FJ, S Isken, JAM de Bont (1994) Cis/trans isomerization of fatty acids as a defence mechanism of Pseudomonas putida strains to toxic concentrations of toluene. Microbiology (UK) 140: 2013–2017. Weissman Z, I Berdicevsky, BZ Cavari, D Kornotzer (2000) The high copper tolerance of Candida albicans is mediated by a P-type ATPase. Proc Natl Acad Sci USA 97: 3520–3525 Whiteway J, P Koziarz, J Veall, N Sandhu, P Kumar, B Hoecher, IB Lambert (1998) Oxygen-insensitive nitroreductases: analysis of the roles of nfsA and nfsB in development of resistance to 5-nitrofuran derivatives in Escherichia coli. J Bacteriol 180: 5529–5539.

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PART 5 ENZYMES CONTAINING MANGANESE, IRON, NICKEL, COPPER, MOLYBDENUM, TUNGSTEN, AND VANADIUM This short section attempts to bring together the range of metalloenzymes that are encountered in biodegradation and biotransformation. Fe is the most common component of enzymes, and is followed in frequency by zinc and molybdenum, while some important enzymes contain nickel, copper, manganese, tungsten, or vanadium.

MANGANESE The role of manganese concentration has seldom been explicitly examined in the context of biodegradation. It is a component of the oxygen-evolving complex containing the Mn4Ca cluster in oxygenic phototrophs, and it is essential for the growth of the purple nonsulfur anaerobic phototrophs Rhodospirillum rubrum and Rhodopseudomonas capsulata during growth with N2—though not with glutamate (Yoch 1979). 1. A few extradiol dioxygenases contain Mn in place of Fe: a. 3,4-Dihydroxyphenylacetate-2,3-dioxygenase from Arthrobacter globiformis (Boldt et al. 1995) and from Bacillus brevis (Que et al. 1981) are Mn(II) enzymes, and are neither activated by Fe(II) nor rapidly inhibited by H2O2. b. The 2,3-dihydroxybiphenyl dioxygenase from Bacillus sp. strain JF8 that mediates ission of the biphenyl ring is unusual in being Mn(II)-dependent, and differs in structure from the analogous enzymes in Burkholderia sp. strain LB400 and Pseudomonas paucimobilis strain KF707 (Hatta et al. 2003). 2. The aerobic and anaerobic degradation of acetone is initiated by carboxylation to acetoacetate. The involvement of manganese has been examined in photoheterotrophically grown Rhodobacter capsulatus strain B10 and the presence of Mn veriied from the X-band EPR spectrum (Boyd et al. 2004). 3. There are several peroxidases produced by fungi including manganese peroxidase. This plays an essential role in the metabolic capability of the white-rot fungus Phanaerochaete chrysosporium. Two groups of peroxidases are produced during secondary metabolism— lignin peroxidases and manganese-dependent peroxidases. Both are synthesized when only low levels of Mn(II) are present in the growth medium, whereas high concentrations of Mn result in the repression of the synthesis of the lignin peroxidases and an enhanced synthesis of manganese-dependent peroxidases (Bonnarme and Jeffries 1990; Brown et al. 1990). Experiments with a nitrogen-deregulated mutant have shown that nitrogen regulation of both these groups of peroxidases is independent of Mn(II) regulation (van der Woude 1993).

IRON Cells require Fe, which is a component of cytochromes and of enzymes that carry out degradation by oxygenation. Its concentration within the cell must, however, be controlled to avoid the

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production of deleterious hydroxyl radicals from molecular oxygen (Touati et al. 1995). Under Fe limitation, transport of Fe into Gram-negative bacteria is controlled by speciic Fe(III) siderophores containing catechol, α-hydroxycarboxylate, and hydroxamate groups in which the Fe occurs as a hexadentate octahedral complex. These are synthesized within the cell and excreted into the medium. They are bound by speciic outer membrane receptors and cross the cytosolic membrane potential using the energy-transducing system TonB-ExcB-ExbD. In Gram-positive bacteria, however, ABC permeases are used (Andrews et al. 2003; Wandersman and Delepelaire 2004). Some organisms including pathogenic bacteria and fungi are able to make use of heme as a source of Fe, and this is noted in Part 1 of this chapter.

NICKEL Nickel exists in the tunicate Trididemnum solidum as the nickel complex of a modiied chlorin (Bible et al. 1988) and is a component of a number of enzymes. Urease is the classic example of a nickel-containing enzyme, and several enzymes contain both nickel and iron. Details of enzymes that contain nickel have been provided in a review (Mulrooney and Hausinger 2003), and only brief summaries are provided: 1. Urease catalyzes the two-stage hydrolysis of urea to ammonia and bicarbonate, and is involved in the pathogenesis of reactive arthritis following infection with Yersinia enterocolitica, in urinary tract infection, and in exacerbating the function of Helicobacter pylori by increasing the pH. The enzyme is found in several Enterobacteriaceae—including Escherichia coli, and species of Proteus and Providencia—in which it is induced by urea, although in Klebsiella aerogenes its synthesis is regulated by nitrogen limitation. The enzyme contains two nickel atoms coordinated with His134, 136, 246, and 272 and the carboxylate of Asp360 (Mobley et al. 1995). 2. Glyoxalase I is involved in the detoxiication of methylglyoxal (Figure 3.33) that is produced during unregulated metabolism of carbohydrates. It is a widely distributed and is typically a Zn-containing enzyme. The enzyme from Escherichia coli is, however, activated by Ni (Clugston et al. 1998), and the basis of metal ion activation has been examined (He et al. 2000). 3. Superoxide dismutase is important for the detoxiication of the superoxide radical (O2−) by reacting with protons to produce H2O2: 2O2− + 2H+ → O2 + H2O2. Although the enzyme generally contains Mn and Fe, or Cu and Zn, the enzyme from Streptomyces seoulensis contains Ni(III) (Wuerges et al. 2004). 4. Exceptionally, in Escherichia coli acireductone dioxygenase (enediol dioxygenase) carries out two enzymatic activities that are responsible for the salvage of methionine, but are encoded by the same gene. Whereas one enzyme is dependent on Fe and produces the ketoacid and formate (Figure 3.34a), the other that is nickel-dependent produces the carboxylic acid, formate, and CO (Figure 3.34b) (Dai et al. 1999). 5. Methyl coenzyme M reductase plays a key role in the production of methane in archaea. It catalyzes the reduction of methyl-coenzyme M with coenzyme B to produce methane and the heterodisulide (Figure 3.35). The enzyme is an α 2β2γ2 hexamer, embedded between two molecules of the nickel-porphinoid F430 and the reaction sequence has been delineated (Ermler et al. 1997). The heterodisulide is reduced to the sulides HS-CoB and HS-CoM by a reductase that has been characterized in Methanosarcina thermophila, and involves low-potential hemes, [Fe4S4] clusters, and a membrane-bound methanophenazine that contains an isoprenoid chain linked by an ether bond to phenazine (Murakami et al. 2001).

183

Mechanistic Aspects GSH OH CH3−CO−CHO CH3−CO−CH SG

FIGURE 3.33

CH3

C

HO

C

O

R

C

O O H C

C

OH

O R

C

O H C O

OH

C

SG

C

O C

(a)

H

O SG

C

CH3

OH CO2 H

O

O R

CH(OH)

C

C

OH + H−CO2H

O

OH

O OH (b)

O R

FIGURE 3.34

CH3−CH(OH)−C

Degradation of methylglyoxal by glyoxylase I.

R O

OH

O

O

CH(OH)

C C O OH

R

C

OH

+ CO + H−CO2H

(a,b) Alternative dioxygenations of an enediol.

O CH3

SO3

S

+ HS

N

H

H

H CO2

CH4 + S

SO3

H

S

N

CH3

P O

O H P O

CH4

S

CoM

FIGURE 3.35

CoB

S

H

CoM

S

S

H CO2 CH3

CoB

Biosynthesis of methane from S-methylcoenzyme M by methyl coenzyme reductase.

6. The acetyl-coenzyme A decarbonylase synthase complex contains ive polypeptide subunits and in acetate-degrading methanotrophs, such as Methanosarcina barkeri and M. thermophila, catalyzes the formation of methane and CO2 from acetyl-CoA: CH3–CO–S–CoA + Co(I)-FeS-protein ⇔ CH3–Co(III)-FeS-protein + CO + CoA The methyl group is subsequently transferred to a tetrahydropterin and coenzyme M. The β-subunit contains Ni and an Fe/S center, and an Ni2[4Fe–4S] arrangement at the active site has been proposed (Gencic and Grahame 2003). 7. Carbon monoxide dehydrogenase can participate in different reactions. Both aerobic and anaerobic organisms can oxidize CO using the reaction CO + H2O → CO2 + H2. Whereas the former uses an Mo-[2Fe–2S]-FAD enzyme, the enzyme from the latter contains Fe and Ni. Carbon monoxide dehydrogenase occurs in several anaerobic bacteria including the homoacetate-fermenting Clostridium thermoaceticum (Drake et al. 1980) and the acetate-utilizing methanogen Methanosarcina thermophila (Lu et al. 1994). It has been suggested that in Carboxydothermus hydrogenoformans there are two forms of the enzyme, both of which contain Ni, one involved in energy generation and one in biosynthetic reactions (Svetlitchnyi et al. 2001). Carboxydothermus hydrogenoformans contains several [4Fe–4S] metal clusters and the active site contains an asymmetrical [Ni–4Fe–5S] cluster in which three of the Fe atoms and the Ni atom are coordinated with cysteine (Dobbek

184

(1)

(2)

(3)

Environmental Degradation and Transformation of Organic Chemicals

F + P

E

E

FIGURE 3.36

cys

cys

C

S

S

O NH 2

C

C

AMP

F

O

E

NH 2

N

E

O

cys

cys

C

S

O

E

NH 2

C

O P

E

NH

SH + Fe

C

cys

S

cys

C

S

O NH 2

C

N

N

Synthesis of Fe–C≡N ligand.

et al. 2001). In contrast, an [Ni–3Fe–4S] cluster was found in Rhodospirillum rubrum (Drennan et al. 2001). 8. Hydrogenase catalyzes the reaction H2 ⇔ 2H+ + 2e and is found in a diverse range of organisms: (a) anaerobes including species of Desulfovibrio, (b) the aerobe Rhizobium leguminosarum, (c) the facultative anaerobe Escherichia coli, and (d) hyperthermophilic archaea including Thermococcus kodakaraensis and Pyrococcus furiosus. There are three groups of hydrogenases distinguished by the presence of (i) Ni–Fe, (ii) Fe–Fe with a dinuclear iron center in anaerobic organisms, or (iii) unrelated with an Fe–S clusterfree enzyme. Both the Ni–Fe and Fe–Fe hydrogenases have CO and CN ligands at the active site. Exceptionally, in Desulfovibrio baculatus, the active site contained [Ni–Fe–Se] (Wang et al. 1992). Nickel is required for the anaerobic growth of Escherichia coli, and there are four [Ni–Fe] hydrogenases whose genes occur in operons (references in Blokesch et al. 2004). The hydrogenases fulill a range of functions. Two of the operons hya and hyb are induced under anaerobic conditions and allow the cells to utilize hydrogen as a source of energy, while hyc is part of the formate hydrogen lyase that converts formate into CO2 and hydrogen. In addition, synthesis of the active nickel enzyme requires the cooperation from several other proteins that bind zinc at a site apparently different from the Ni-binding site (Blokesch et al 2004). In Ni–Fe hydrogenases, the Fe is coordinated with one CO and two CN ligands, and synthesis of the latter involves two proteins HypF and HypE that carry out the consecutive reactions (Figure 3.36) (Reissmann et al. 2003). The analogous active site in the Fe–Fe hydrogenase of the hyperthermophilic Thermotoga maritima contains CO and CN ligands at both Fe atoms that are linked by an additional CO and sulfur ligands, one of which contains the [4Fe–4S] center. The maturation protein HydF is able to bind GTP and catalyze GTP hydrolysis, and contains an [4Fe–4S] cluster with an unusual EPR signal, which suggests that only three cysteines are coordinated (Brazzolotto et al. 2006). In hyperthermophilic archaea, hydrogenases are also involved in the reduction of S0 to H2S (Laska et al. 2003; Ma et al. 2000). It has been suggested that the subunits of hydrogenase and sulfur reductase in the acidophilic Acidianus ambivalens are similar to their homologs from Wolinella succinogenes (Laska et al. 2003).

COPPER Copper is a component of several enzymes that have quite different catalytic properties: 1. Methane monooxygenase may exist in either soluble (sMMO) or particulate (pMMO) forms. These display different substrate ranges and different rates of transformation rates, and most methanotrophs express only the latter form of the enzyme (Hanson and Hanson 1996). The particulate form of methane monooxygenase contains copper, or both copper

185

Mechanistic Aspects

2. 3.

4.

5. 6.

7.

and iron, and the concentration of copper determines the catalytic activity of the enzyme (Sontoh and Semrau 1998). Although various dioxygenases generally contain Fe(II) or Fe(III), copper replaces Fe in the dioxygenase from Aspergillus japonicus that brings about ission of the C-ring of quercitin with the formation of carbon monoxide (Steiner et al. 2002). The carbon monoxide dehydrogenase of the aerobe Oligotropha carboxidovorans contains both Cu and Mo in the form of a cluster in which the Mo is bound to the thiol groups of molybdopterin cytosine nucleotide, and the Cu to cysteine residue in the form of a Cu–S–Mo(=O)OH cluster (Dobbek et al. 2002). Glyoxal oxidase that is required to produce the H2O2 required for the activity of lignin peroxidase carries out the reaction RCHO + O2 + H2O → RCO2H + H2O2, and requires Cu for full activity. It is a radical-copper oxidase closely resembling galactose oxidase (Whittaker et al. 1996). Copper is a component of the oxalate decarboxylase in Bacillus subtilis that converts oxalate into formate and CO2 (Tanner et al. 2001). The deamination of primary amines such as phenylethylamine by Escherichia coli (Cooper et al. 1992) and Klebsiella oxytoca (Hacisalihoglu et al. 1997) is carried out by an oxidase. This contains copper and topaquinone (TPQ), which is produced from tyrosine by dioxygenation. TPQ is reduced to an aminoquinol that in the form of a Cu(I) radical reacts with O2 to form H2O2, Cu(II), and the imine. The mechanism has been elucidated (Wilmot et al. 1999), and involves formation of a Schiff base followed by hydrolysis in reactions that are formally analogous to those involved in pyridoxal-mediated transamination. Superoxide dismutases may contain a range of metals: Mn, Fe, or both Cu and Zn, and representatives of all these are found in prokaryotes. The nickel enzyme is noted later.

MOLYBDENUM Molybdopterin Oxidoreductases The molybdenum cofactor (molybdopterin) consists of a dihydropteridine fused to a dihydropyran ring containing a −CH2OPO32− group and an enedithiol that is coordinated to the molybdenum. In prokaryotes, the cofactor is formed by coupling to a nucleoside phosphate (generally cytidine or guanidine) forming a pyrophosphate (Llamas et al. 2004) (Figure 3.37). The biosynthesis of molybdopterin is catalyzed by at least six gene products, and is initiated from guanosine triphosphate by guanosine hydrolase I that provides the pteridine nucleus, while the C5 of ribose and the purine C8 provide the dihydropyran ring. Molybdopterin is a component of four enzyme families all of which contain Mo(VI): the xanthine oxidase and the sulite oxidase families with one molybdopterin and the DMSO family with two molybdopterins. There are a number of tungsten-containing enzymes with structures analogous

O H

NH 2

H

S Mo S

N

N N

N H

NH 2

O

N O

O P O

O

O P

O

O

O

N

O OH OH

FIGURE 3.37

Structure of molybdopterin conjugated with cytidine diphosphate.

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Environmental Degradation and Transformation of Organic Chemicals

to molybdopterin in which W(VI) replaces Mo(VI) (Hille 2002). Molybdopterin is a structural part of the important oxidoreductases that are involved in the aerobic degradation of azaarenes. Using a bioinformatics screen, a molybdenum-containing oxidoreductase has also been found in the majority of Gram-negative bacteria (Loschi et al. 2004). It contains one molybdopterin, and the soluble subunit designated YedY functions as a reductase for TMAO and some sulfoxides. These oxidoreductases are widely used for the introduction of the oxygen atom from H2O into heteroarenes, especially azaarenes including pyridine, quinoline, pyrimidine, and purine, and they generally contain molybdenum. Heteroarenes The degradation of the ive-membered heteroarenes furan-2-carboxylate and pyrrole-2-carboxylate is initiated by the corresponding hydroxylases (Hormann and Andreesen 1991; Koenig and Andreesen 1990, 1991). Pyridine

The degradation of several pyridine carboxylates is initiated by hydroxylation. In Arthrobacter picolinophilus, pyridine-2-carboxylate is hydroxylated to 3,6-dihydroxypyridine-2-carboxylate (as for 2-hydroxypyridine) and this is carried out by a particulate enzyme that introduces oxygen from H2O (Tate and Ensign 1974), has a molecular mass of 130 kDa, and contains Mo (Siegmund et al. 1990). Pyridine-4-carboxylate is hydroxylated by Mycobacterium sp. strain INA1 to the 2,6-dihydroxy-4-carboxylate. Two different hydroxylation enzymes were involved and were apparently Mo-dependent (Kretzer and Andreesen 1991). The degradation of nicotine by Arthrobacter nicotinovorans involves two dehydrogenations by enzymes containing Mo, Fe–S, and FAD (Baitsch et al. 2001). Quinoline

Experiments with H218O using Pseudomonas putida strain 86 (Bauder et al. 1990) showed that the oxygen incorporated into quinol-2-one originates from water. The oxidoreductases have been puriied from a number of organisms that degrade quinoline including P. putida (Bauder et al. 1990), Rhodococcus sp. strain B1 (Peschke and Lingens 1991), Comamonas testosteroni (Schach et al. 1995), and Agrobacterium sp. strain 1B that degrades quinoline-4-carboxylate (Bauer and Lingens 1992). They have a molecular mass of 300–360 kDa, and contain per molecule, eight atoms of Fe, eight atoms of acid-labile S, two atoms of Mo, and two molecules of FAD. The organic component of the pterin molybdenum cofactor is generally molybdopterin cytosine dinucleotide (Hetterich et al. 1991; Schach et al. 1995). The metabolism of 2-methylquinoline in Arthrobacter sp. strain Rü 61a is comparable, with introduction of oxygen at C4 (Hund et al. 1990). The enzymes (oxidoreductases) that introduce oxygen into the azaarene rings in Rhodococcus sp. strain B1, Arthrobacter sp. strain Rü61a, and Pseudomonas putida strain 86 are virtually identical and, like those already noted have molecular masses of 300–320 kDa and contain Mo, Fe, FAD, and acid-labile sulfur (De Beyer and Lingens 1993). The enzymes from Comamonas testosteroni for hydroxylation of quinoline to quinol-2-one (quinoline 2-oxidoreductase) and the dioxygenase responsible for the introduction of oxygen into the benzenoid ring (2-oxo-1,2-dihydroquinoline 5,6-dioxygenase) have been described (Schach et al. 1995). Isoquinoline

The degradation of isoquinoline by Alcaligenes faecalis strain Pa and Pseudomonas diminuta strain 7 (Röger et al. 1990, 1995) is mediated by an oxidoreductase that produces 1,2-dihydroisoquinoline-1-one, followed by ring ission with the production of o-phthalate and oxidation to 3,4-dihydroxybenzoate (Figure 3.38). The oxidoreductase is puriied and like most typical azarene oxidoreductases contains, per mole, 0.85 g atoms of Mo, 3.9 g atoms of Fe, and acid-labile S (Lehmann et al. 1994).

187

Mechanistic Aspects NH 2

CO 2 H CO 2 H

N

NH

CO 2 H

CO 2 H

O

FIGURE 3.38

OH OH

Degradation of isoquinoline initiated by an oxidoreductase.

Reductases a. The dehydroxylase in Thauera aromatica that brings about dehydroxylation of 4-hydroxybenzoyl-CoA to benzoyl-CoA is a molybdenum–lavin–iron–sulfur enzyme (Breese and Fuchs 1998). b. The DMSO reductase family contains molybdenum generally in the form of bis (molybdopterin guanine nucleotide) (references in McEwan et al. 2002). In addition to DMSO reductase, they include TMAO reductase, (per)chlorate reductase, selenate reductase, and arsenate reductase that are able to couple the reduction to the generation of energy (dissimilatory reduction). They catalyze the following reactions that have been noted in Part 2 of this chapter: Me2SO → Me2S (DMSO reductase); Me3NO → Me3N (TMAO reductase); HCO2H → CO2 + H2 (formate dehydrogenase); ClO4− → ClO3− → ClO− ([per]chlorate reductase); SeO42− → SeO32− (selenate reductase); AsO2− → AsO43− (arsenite oxidase). The chlorate reductase has been characterized in strain GR-1 where it was found in the periplasm, is oxygen-sensitive, and contains molybdenum, and both [3Fe–4S] and [4Fe–4S] clusters (Kengen et al. 1999). The arsenate reductase from Chrysiogenes arsenatis contains Mo, Fe, and acid-labile S (Krafft and Macy 1998), and the reductase from Thauera selenatis that is speciic for selenate, is located in the periplasmic space, and contains Mo, Fe, acid-labile S, and cytochrome b (Schroeder et al. 1997). In contrast, the membrane-bound selenate reductase from Enterobacter cloacae SLD1a-1 that cannot function as an electron acceptor under anaerobic conditions contains Mo and Fe and is distinct from nitrate reductase (Ridley et al. 2006). In the anaerobic photoheterotroph Rhodobacter (Rhodopseudomonas) spheroides, a molybdenum enzyme in which the metal is coordinated by two equivalents of a pyranopterin cofactor is involved in sequential oxidations and reductions involving Mo(VI), Mo(V), and Mo(IV) (Cobb et al. 2005).

TUNGSTEN Tungsten-containing enzymes have been found to mediate a variety of reactions both in aerobic and anaerobic bacteria, and their structure may plausibly be assumed to be analogous to the molybdopterins: 1. Acetylene hydratase from the anaerobe Pelobacter acetylenicus is a tungsten– iron–sulfur enzyme that resembles molybdopterin in which W replaces Mo (Meckenstock

188

2.

3.

4.

5.

Environmental Degradation and Transformation of Organic Chemicals

et al. 1999), and catalyzes the addition of the elements of water to acetylene HC≡CH → CH2=CHOH≡CH3CHO. Oxidoreductases: A number of these have been characterized and include the following: a. Aldehyde oxidoreductase from Desulfovibrio gigas (Hensgens et al. 1995). b. An aldehyde dehydrogenase from Desulfovibrio simplex is stimulated by tungsten and oxidizes aliphatic and aromatic aldehydes using lavins (Zellner and Jargon 1997). c. Aldehyde oxidoreductase from Clostridium thermoaceticum (Strobl et al. 1992). Several tungsten-containing oxidoreductases have attracted attention in the biochemistry of the extreme thermophile Pyrococcus furiosus: (a) aldehyde ferredoxin oxidoreductase (Mukund and Adams 1991), (b) glyceraldehyde ferredoxin oxidoreductase (Mukund and Adams 1995), (c) formaldehyde ferredoxin oxidoreductase (Mukund and Adams 1993; Roy et al. 1999), (d) an aldehyde oxidoreductase with a broad substrate speciicity that probably involves ferredoxin (Bevers et al. 2005), and (e) an enzyme that may be involved in the reduction of S0 (Roy and Adams 2002). Carboxylic acid reductase: Anaerobic reduction of aryl and alkyl carboxylates to the corresponding aldehydes has been demonstrated in a few tungsten-containing reductases and dehydrogenases. In Clostridium formicoaceticum the enzyme catalyzes the reduction of propionate, butyrate, and benzoate to the corresponding aldehydes RCO2H → RCHO. The enzyme contains, per dimer, 11 iron, 16 acid-labile sulfur, and 1.4 tungsten + molybdopterin (White et al. 1991). In addition, an Mo oxidoreductase has been described from Cl. formicoaceticum (White et al. 1993). Formate dehydrogenase from Moorella (Clostridium) thermoaceticum catalyzes the reduction of CO2 to formate and contains W, Se, Fe, and S (Yamamoto et al. 1983), and the FDH-II enzyme from Eubacterium acidamophilum that uses formate as electron donor during aminoacid fermentations contains W, Se, and Fe (Graentzdoerffer et al. 2003). The formate dehydrogenase involved in the oxidation of formate to CO2 in E. coli is, however, an Mo, Se, (Fe4S4) enzyme (Boyington et al. 1997). Hydrogenase: Thermotoga maritima grows at the expense of carbohydrates producing lactate, acetate, CO2, and H2. Although production of the hydrogenase and its in vitro activity is greatly stimulated by the presence of tungstate, the puriied enzyme contains only Fe and acid-labile S, and tungsten is absent (Juszczak et al. 1991). This is also true for pyruvate: ferredoxin oxidoreductase from the same organism.

VANADIUM 1. Three enzymes in Azotobacter vinelandii (Rüttimann-Johnson et al. 2003) and Rhodopseudomonas palustris (Oda et al. 2005) are capable of reducing dinitrogen: the nifencoded enzyme containing molybdenum and iron, the vnf that encodes a vanadium and iron enzyme, and the anf that is an iron-only enzyme. 2. Some haloperoxidases contain vanadium and a review of vanadium peroxidases has been given (Butler 1998). The structure of the vanadium enzyme in the terrestrial fungus Curvularia inaequalis has been determined by x-ray analysis (Messerschmidt et al. 1997), and the apochloroperoxidase possesses, in addition, phosphatase activity that can be rationalized on the basis of the isomorphism of phosphate and vanadate (Renirie et al. 2000).

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Meckenstock RU, R Krieger, S Ensign, PMH Kroneck, B Schink (1999) Acetylene hydratase of Pelobacter acetylenicus. Molecular and spectroscopic properties of the tungsten iron-sulfur enzyme. Eur J Biochem 264: 176–182. Messerschmidt A, L Prade, R Wever (1997) Implications for the catalytic mechanism of the vanadiumcontaining enzyme chloroperoxodase from the fungus Curvularia inaequalis by X-ray structures of the native and peroxide form. Biol Chem 378: 309–315. Mobley HLT, MD Island, RP Hausinger (1995) Molecular biology of microbial ureases. Microbiol Rev 59: 451–480. Mukund S, MWW Adams (1991) The novel tungsten-iron-sulfur protein of the hyperthermophilic archaebacterium, Pyrococcus furiosus, is an aldehyde ferredoxin oxidoreductase J Biol Chem 266: 14208–14216. Mukund S, MWW Adams (1993) Characterization of a novel tungsten-containing formaldehyde oxidoreductase from the extremely thermophilic archaeon, Thermococcus litoralis. J Biol Chem 268: 13592–13600. Mukund S, MWW Adams (1995) Glyceraldehyde-3-phosphate ferredoxin oxidoreductase, a novel tungstencontaining enzyme with a potential glycolytic role in the hyperthermophilic archaeon, Pyrococcus furiosus. J Biol Chem 270: 8389–8392. Mulrooney SB, RP Hausinger (2003) Nickel uptake and utilization by microorganisms. FEMS Microbiol Rev 27: 239–261. Murakami E, U Deppenmeier, SW Ragsdale (2001) Characterization of the intramolecular electron transfer pathway from 2-hydroxyphenazine to the heterodisulide reductase from Methanosarcina thermophila. J Biol Chem 276: 2432–2439. Oda Y, SK Samanta, FE Rey, L Wu, X Liu, T Yan, J Zhou, CS Harwood (2005) Functional genomic analysis of three nitrogenase isoenzymes in the photosynthetic bacterium Rhodopseudomonas palustris. J Bacteriol 187: 7784–7794. Peschke B, F Lingens (1991) Microbial metabolism of quinoline and related compounds XII. Isolation and characterization of the quinoline oxidoreductase from Rhodococcus spec. B1 compared with the quinoline oxidoreductase from Pseudomonas putida 86. Biol Chem Hoppe-Seyler 370: 1081–1088. Que L, J Widom, RL Crawford (1981) 3,4-dihydroxyphenylacetate 2,3-dioxygenase : a manganese(II) dioxygenase from Bacillus brevis. J Biol Chem 256: 10941–10944. Reissmann S, E Hochleitner, H Wang, A Paschos, F Lottspeich, RS Glass, A Böck (2003) Taming of a poison: biosynthesis of the NiFe-hydrogenase cyanide ligands. Science 299: 1067–1070. Renirie R, W Hemrika, R Wever (2000) Peroxidase and phosphatase activity of active-site mutants of vanadium chloroperoxidase from the fungus Curvularia inaequalis. J Biol Chem 275: 11650–11657. Ridley H, CA Watts, DJ Richardson, CS Butler (2006) Resolution of distinct membrane-bound enzymes from Enterobacter cloacae SKLD1a-1 that are responsible for selective reduction of nitrate and selenate anions. Appl Environ Microbiol 72: 5173–5180. Röger P, A Erben, F Lingens (1990) Microbial metabolism of quinoline and related compounds IV. Degradation of isoquinoline by Alcaligenes faecalis Pa and Pseudomonas diminuta 7. Biol Chem Hoppe-Seyler 370: 1183–1189. Röger P, G Bär, F Lingens (1995) Two novel metabolites in the degradation pathway of isoquinoline by Pseudomonas diminuta 7. FEMS Microbiol Lett 129: 281–286. Roy R, MWW Adams (2002) Characterization of a fourth tungsten-containing enzyme from the hyperthermophilic Pyrococcus furiosus. J Bacteriol 184: 6952–6956. Roy R, S Mukund, GJ Schut, DM Dunn, R Weiss, MWW Adams (1999) Puriication and molecular characterization of the tungsten-containing formaldehyde ferredoxin oxidoreductase from the hyperthermophilic archaeon Pyrococcus furiosus: the third of a putative ive-member tungstoenzyme family. J Bacteriol. 181: 1171–1180. Rüttimann-Johnson C, LM Rubio, DR Dean, PW Ludden (2003) VnfY is required for full activity of the vanadium-containing dinitrogenase in Azotobacter vinelandii. J Bacteriol 185: 2383–2386. Schach S, B Tshisuaka, S Fetzner F Lingens (1995) Quinoline 2-oxidoreductase and 2-oxo-1,2-dihydroquinoline 5,6-dioxygenase from Comamonas testosteroni 63. The irst two enzymes in quinoline and 3-methylquinoline degradation. Eur J Biochem 232: 536–544. Schroeder I, S Rech, T Krafft, JM Macey (1997) Puriication and characterization of the selenate reductase from Thauera selenatis. J Biol Chem 272: 23765–23768. Siegmund I, Koenig K, Andreesen JR (1990) Molybdenum involvement in aerobic degradation of picolinic acid by Arthrobacter picolinophilus FEMS Microbiol Lett 67: 281–284.

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4 Determinants and Interactions This section addresses the conditions under which the degradation of organic compounds is carried out, the factors that determine their success, and attempts to provide a background for experimental aspects, which are discussed in Chapters 5 and 6, illustrations of the reactions are given in Chapters 7 through 11.

SINGLE SUBSTRATES: SEVERAL ORGANISMS Cultures of a single microorganism may occur naturally only in circumstances where extreme selection pressure operates. Generally, however, many different organisms with diverse metabolic potential will exist side by side. Therefore, metabolic interactions are probably the rule rather than the exception in natural ecosystems and biological treatment systems. Both the nature and the tightness of the association may vary widely, and the degradation of a single compound may necessitate the cooperation of two (or more) organisms. Some well-deined interactions and the different mechanisms underlying the cooperation are illustrated by the following examples: 1. One of the organisms fulills the need for a growth requirement by the other, for example, vitamin requirements of one organism that is provided by the other. Examples are provided by biotin in cocultures of Methylocystis sp. and Xanthobacter sp. (Lidstrom-O’Connor et al. 1983), and thiamin in cocultures of Pseudomonas aeruginosa and an undeined Pseudomonas sp. that degraded the phosphonate herbicide glyphosate (Moore et al. 1983). 2. One organism may be able to carry out only a single step in biodegradation. Many examples among aerobic organisms have been provided (Reanney et al. 1983; Slater and Lovatt 1984) so that this is probably a widespread situation. The following three examples are given as illustration: a. The degradation of parathion was carried out by a mixed culture of Pseudomonas stutzeri and P. aeruginosa (Daughton and Hsieh 1977) in which the 4-nitrophenol initially formed by the former is metabolized by the latter (Figure 4.1). b. The degradation of 4-chloroacetophenone was accomplished by a mixed culture of an Arthrobacter sp. and a Micrococcus sp. The irst organism was able to carry out all the degradative steps except the conversion to 4-chlorocatechol of the intermediate 4-chlorophenol that is toxic to this organism (Havel and Reineke 1993). c. A consortium of a Flavobacterium sp. and a Pseudomonas sp. could carry out the aerobic degradation of polyethylene glycol. The latter was required for the degradation of the glycollate produced by the former (Kawai and Yamanaka 1986). HO–(CH2–CH2O)n –CH2–CH2–O–CH2–CH2OH → HO–(CH2–CH2O)n –CH2–CH2–O –CH2–CO2H → HO–(CH2–CH2O)n.CH2–CH2–OH + HO–CH2–CO2H

3. Two organisms are required to maintain the redox balance. Among anaerobic bacteria, hydrogen transfer is important since the redox balance must be maintained, and the hydrogen concentration in mixed cultures may be critical. Interspecies hydrogen transfer has been demonstrated especially among populations of rumen bacteria containing methanogens where the concentration of hydrogen must be limited for effective functioning of the consortia. Illustrative examples have been summarized (Wolin 1982), and some additional 193

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EtO P EtO

OH

S EtO EtO

P

O

NO 2 OH

OH OH

NO2

NO2

FIGURE 4.1 Degradation of parathion by a mixed culture of two pseudomonads.

comments on degradative reactions that are dependent on hydrogen transfer mediated by one of the cooperating organisms are added here. Stable metabolic associations generally between pairs of anaerobic bacteria have been termed syntrophs, and these are effective in degrading a number of aliphatic carboxylic acids or benzoate under anaerobic conditions. These reactions have been discussed in reviews (Schink 1991, 1997; Lowe et al. 1993) that provide lucid accounts of the role of syntrophs in the degradation of complex organic matter. Two examples are given here to illustrate the experimental intricacy of the problems besetting the study of syntrophic metabolism under anaerobic conditions: 1. Oxidation under anaerobic conditions of long-chain aliphatic carboxylic acids was established in syntrophic cultures of Clostridium bryantii, Desulfovibrio sp. (Stieb and Schink 1985); Syntrophomonas sapovorans, Methanospirillum hungatei (Roy et al. 1986); and Syntrophomonas wolfei in coculture with H2-utilizing anaerobic bacteria (McInerney et al. 1981). The role of the second syntroph was to metabolize the reducing equivalents produced by oxidation of the carboxylic acids. S. wolfei was subsequently, however, adapted to grow with crotonate in pure culture (Beaty and McInerney 1987), and this procedure was also used for Cl. bryantii. 16S rRNA sequence analysis was then used to show the close relationship of these two organisms and to assign them to a new genus Syntrophospora (Zhao et al. 1990). However, anaerobic oxidation of carboxylic acids with chain lengths of up to 10 has been demonstrated in pure cultures of species of Desulfonema (Widdel et al. 1983), and aliphatic hydrocarbons may be completely oxidized to CO2 by a sulfate-reducing bacterium (Aeckersberg et al. 1991, 1998). 2. There has been considerable interest in the anaerobic degradation of propionate that is a fermentation product of many complex substrates, and syntrophic associations of acetogenic and methanogenic bacteria have been obtained. During the metabolism of propionate in a syntrophic culture (Houwen et al. 1991), the methanogens serve to remove hydrogen produced during the oxidation of propionate to acetate. The growth of syntrophic propionate-oxidizing bacteria in the absence of methanogens has, however, been accomplished using fumarate as the sole substrate (Plugge et al. 1993). Fumarate played a central role in the metabolism of this organism since it is produced from propionate via methylmalonate and succinate, and is metabolized by the acetyl-CoA cleavage pathway via malate, oxalacetate, and pyruvate. Pure cultures of organisms that can oxidize propionate either in the presence of a methanogen or using sulfate as electron acceptor have been obtained. These include both Syntrophobacter wolinii and Syntrophobacter pfenigii (Wallrabenstein et al. 1995). The interaction of two organisms, therefore, is clearly not obligatory for the ability to degrade these carboxylic acids under anaerobic conditions.

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COMETABOLISM AND RELATED PHENOMENA In natural ecosystems, it is indeed seldom that either a pure culture or a single substrate exists. In general, several substrates will be present, and these will include compounds of widely varying susceptibility to microbial degradation. The phenomenon where degradation occurs in the presence of two substrates has been termed “cooxidation” or, less speciically, “cometabolism” or “concurrent metabolism.” Unfortunately, the term cometabolism (Horvath 1972) has been used in different and conlicting ways. Since the preix “co” implies “together,” it should not therefore be used when only a single substrate is present. The term “biotransformation” is unambiguous, and seems appropriate and entirely adequate. Detailed discussions have been presented (Dalton and Stirling 1982), and some of the conlicting aspects have been briely summarized (Neilson et al. 1985). Whereas probably most aerobic bacteria that have been used in experiments on biodegradation were obtained by elective growth using the chosen substrate as sole source of both carbon and energy, anaerobic bacteria are often more fastidious in their nutritional demands. The addition of nutrient supplements, such as yeast extract or ruminant luid, may be needed to stimulate or maintain growth. Although the metabolic conclusions from such laboratory experiments are unambiguous, care should be exercised in uncritically extrapolating the results to natural ecosystems that are unlikely to provide such a nutritious environment. In such experiments, unequivocal results may often advantageously be obtained by using suspensions of washed cells. Cometabolism merits, however, careful analysis since important metabolic principles underlie most of the experiments, even though confusion may have arisen as a result of ambiguous terminology. An attempt is therefore made to ignore semantic implications and to adopt a broad perspective in discussing this environmentally important issue. A pragmatic point of view has been adopted, and the following examples attempt to illustrate the kinds of experiments, which have been carried out under various conditions.

INDUCTION OF CATABOLIC ENZYMES PRE-EXPOSURE TO AN ANALOG SUBSTRATE Organisms may be obtained after elective enrichment with a given substrate but are subsequently shown to be unable to use the substrate for growth, although they are able to accomplish its incomplete metabolism. These situations should rather be termed biotransformation. A typical example is the partial oxidation of 2,3,6-trichlorobenzoate to 3,5-dichlorocatechol (Figure 4.2) (Horvath 1971). The catabolic enzymes may, however, be induced by pre-exposure to an analog substrate. Cells may be grown with this before exposure to the xenobiotic. Although the xenobiotic is extensively degraded, it cannot be used alone to support the growth of cells. When both substrates are simultaneously present, the term cometabolism is appropriate, but this term is quite unjustiiable for the situation in which cells grown with a given inducing substrate are then used for studying the metabolism of a single xenobiotic. The following examples are given as illustration: a. Several strains of bacteria grown with nonchlorinated substrates such as phenol, naphth-2-ol, or naphthalene were able to oxidize 4-chlorophenol to 4-chlorocatechol, or 3-chlorobenzoate to 3-chloro-5,6-dihydroxybenzoate (Figure 4.3) even though they were unable to use them for growth (Spokes and Walker 1974). b. The oxidation of nitrobenzene to 3-nitrocatechol by strains of Pseudomonas sp. grown with toluene or chlorobenzene (Haigler and Spain 1991). c. The oxidation of 2-chloronaphthalene to chloro-2-hydroxy-6-ketohexa-2,4-dienoic acids (Figure 4.4) by cells in which biotransformation of the substrate was induced by growth with naphthalene (Morris and Barnsley 1982).

196

Environmental Degradation and Transformation of Organic Chemicals CO2H Cl

CO2H Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

OH

OH

OH

OH

FIGURE 4.2 Biotransformation of 2,3,6-trichlorobenzoate. OH

OH

CO 2 H

CO 2 H

OH

CO 2 H

HO

HO

; Cl Cl

Cl

HO

Cl

Cl

FIGURE 4.3 Biotransformation of 4-chlorophenol and 3-chlorobenzoate. Cl

Cl

CO 2 H

OH CO 2 H CHO

OH Cl

or Cl

OH

CO 2 H

FIGURE 4.4

Cl

CHO CO 2 H OH

Biotransformation of 2-chloronaphthalene.

d. The degradation of polychlorinated biphenyls has been established in a number of organisms enriched with biphenyl as carbon source, for example, Pseudomonas sp. strain LB400 (Bopp 1986), Alcaligenes eutrophus strain H850 (Bedard et al. 1987), and P. pseudoalcaligenes (Furukawa and Arimura 1987). e. The use of brominated biphenyls has been examined to induce anaerobic dechlorination of highly chlorinated biphenyls including the hepta-, hexa-, and pentachloro congeners (Bedard et al. 1998). Di- and tribromo congeners were the most effective and were themselves reduced to biphenyl. f. The oxidation of methylbenzothiophenes by cells grown with 1-methylnaphthalene (Salic et al. 1992). g. The mineralization of benz[a]anthracene, chrysene, and benzo[a]pyrene by organisms isolated by enrichment with and grown at the expense of phenanthrene (Aitken et al. 1998). Comparable situations could be encountered during experiments on bioremediation in which it may be experimentally expedient to grow cells on a suitable analog (Klecka and Maier 1988), or to introduce the organisms into the contaminated site (Harkness et al. 1993). There are, however, inherent dangers in this procedure. For example, cells able to degrade 5-chlorosalicylate (Crawford et al. 1979), 2,6dichlorotoluene (Vandenbergh et al. 1981) and pentachlorophenol (Stanlake and Finn 1982) were unable to degrade the nonhalogenated analogs. Further, the degradation of 4-nitrobenzoate was inhibited by benzoate even though the strain could use either substrate separately (Haller and Finn 1978).

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Determinants and Interactions

ENZYME INDUCTION BY GROWTH ON STRUCTURALLY UNRELATED COMPOUNDS Enzymes necessary for the metabolism of a substrate may be induced by growth on structurally unrelated compounds. In the examples used for illustration, monooxygenases play a cardinal role as a result of the versatility of methane monooxygenase, while monooxygenases that may be involved in toluene degradation are discussed in Chapter 3, Part 1 and Chapter 8, Part 1. 1. Trichloroethene and aromatic compounds. A striking example is the degradation of trichloroethene by different strains of Pseudomonas sp. grown with phenol (Folsom et al. 1990) or with toluene. This capability has attracted attention for the bioremediation of sites contaminated with chloroethenes (Hopkins and McCarty 1995). Conversely, toluene degradation is induced (a) by trichloroethene in a strain of P. putida (Heald and Jenkins 1994) and (b) in P. mendocina (though not in Burkholderia [Pseudomonas] cepacia or P. putida strain F1) by trichloroethene, pentane, and hexane (McClay et al. 1995). This metabolic versatility may be consistent with the different pathways that are followed in toluene degradation (Figure 4.5): a. P. putida F1 by the classical toluene dioxygenase system (Zylstra et al. 1989) b. B. cepacia G4 by monooxygenation to 2-methylphenol (Shields et al. 1989) c. P. mendocina KR by monooxygenation to 4-methylphenol (Whited and Gibson 1991) d. P. pickettii PKO1 by monooxygenation to 4-methylphenol (Olsen et al. 1994) The last example is mediated by a monooxygenase that can be induced by benzene, toluene, and ethylbenzene, and also by xylenes and styrene. A plausibly analogous situation exists for strains of Pseudomonas sp. and Rhodococcus erythropolis that were obtained by enrichment with isopropylbenzene, and that could be shown to oxidize trichloroethene (Dabrock et al. 1992). In addition, one of the pseudomonads could oxidize 1,1-dichloroethene, vinyl chloride, trichloroethane, and 1,2-dichloroethane. 2. Methane, butane, and chloroform. Cells of Methylosinus trichosporium grown with methane and of Pseudomonas butanovora and Mycobacterium vaccae grown with butane were able to partially degrade chloroform (Hamamura et al. 1997). Again this may be the result of the induction of monooxygenase activity.

CH 3

CH 3

CH 3

CH 3

CH 2 OH

H

OH

OH OH

OH

H CO 2 H

FIGURE 4.5 Pathways for the biotransformation of toluene.

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Environmental Degradation and Transformation of Organic Chemicals

3. Strain G4/PR1 of Burkholderia cepacia in which the synthesis of toluene-2-monooxygenase is constitutive is able to degrade a number of ethers including diethyl ether and n-butyl methyl ether but not t-butyl methyl ether (Hur et al. 1997). 4. A good example is provided by DDE, which is the irst metabolite in the conventional degradation pathway of DDT and is apparently persistent in the environment. Pure cultures of aerobic and anaerobic bacteria that were able to degrade 1,1-dichloroethene and 4,4′-dichlorobiphenyl, which were considered to represent important structural features of DDE, were, however, unable to degrade DDE even during incubation with dense cell suspensions (Megharaj et al. 1997). Cell extracts of the aerobic organisms were also ineffective, and it was therefore concluded that recalcitrance lay in the structure of 1,1-diphenyl-2,2-dichloroethene since 1,1-diphenylethene could be used as sole substrate for the growth of styrene-degrading strains of Rhodococcus sp. (Megharaj et al. 1998). In contrast, cells of Pseudomonas acidovorans strain M3GY during growth with biphenyl have been shown to degrade DDE with the ission of one ring and production of 4-chlorobenzoate (Hay and Focht 1998). This situation may be of widespread occurrence and further examples of its existence will be facilitated by insight into the mechanisms of pathways for biodegradation.

ROLE OF READILY DEGRADED SUBSTRATES Results from experiments on biodegradation in which readily degraded substrates such as glucose are added have probably restricted relevance to natural ecosystems in which such substrates exist in negligible concentration. However, readily degraded substrates in addition to those less readily degradable undoubtedly occur in biological-waste-treatment systems. In these circumstances, at least three broadly different metabolic situations may exist: 1. The presence of glucose may suppress degradation of a recalcitrant compound: a. Strains of Pseudomonas pickettii degrade 2,4,6-trichlorophenol, and its degradation is induced by several other chlorophenols, but is repressed in the presence of glucose or succinate (Kiyohara et al. 1992). b. The presence of glucose decreased the rate of degradation of phenol in a natural lake-water community, though the rate was increased by arginine (Rubin and Alexander 1983). 2. The presence of glucose may, however, enhance the degradation of a recalcitrant compound. Several different metabolic situations may be discerned, each probably representing a different mechanism for the stimulation: a. Experiments in which degradation of luorobenzoates by a mixed bacterial lora was enhanced by the presence of glucose might plausibly be attributed to an increase in the cell density of the appropriate organism(s) (Horvath and Flathman 1976). A comparable conclusion could also be drawn from the data for the degradation of 2,4dichlorophenoxyacetate and O,O-dimethyl-O-[3-methyl-4-nitrophenyl] phosphorothioate in cyclone fermentors (Liu et al. 1981). b. The presence of readily degraded substrates such as glutamate, succinate, or glucose had a stimulatory effect on the degradation of pentachlorophenol by a Flavobacterium sp., and could be attributed to ameliorating the toxic effects of pentachlorophenol (Topp et al. 1988). These additional substrates also enhanced the ability of natural communities to degrade a number of xenobiotics (Shimp and Pfaender 1985a). c. The presence of glucose facilitated the anaerobic dechlorination of pentachlorophenol and may plausibly be attributed to the increased level of reducing equivalents

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Determinants and Interactions

(Henriksen et al. 1991). A comparable phenomenon is the enhanced dechlorination of tetrachloroethene in anaerobic microcosms by the addition of carboxylic acids including lactate, propionate, butyrate, and crotonate (Gibson and Sewell 1992). 3. The xenobiotic may be degraded in preference to glucose, which is not a universal growth substrate. This situation is encountered in a phenol-utilizing strain of the yeast Trichosporon cutaneum that possesses a partially constitutive catechol 1,2-dioxygenase (Shoda and Udaka 1980), and illustrates the importance of regulatory mechanisms in determining the degradation of xenobiotics. Constitutive synthesis of the appropriate enzyme systems may indeed be of determinative signiicance in many natural ecosystems, and merits investigation. In some circumstances, therefore, the presence of readily degraded substrates may clearly facilitate the degradation of recalcitrant xenobiotics, although a generally valid mechanism for these positive effects has not emerged. Whereas the addition of metabolizable analogs may increase the overall rates of degradation (Klecka and Maier 1988), it should be emphasized that the presence of readily degraded substrates in enrichments would generally be expected to be counterselective to the development of organisms that could degrade a speciic xenobiotic. In addition, the observed enhancements summarized earlier were generally observed during relatively short time intervals. Simultaneous metabolism of two structurally related substrates in which only one of them serves as growth substrate during biotransformation of the other may exist. A simple example is the O-demethylation of 4,5,6-trichloroguaiacol to 3,4,5-trichlorocatechol followed by successive O-methylation during the growth of a strain of Rhodococcus sp. at the expense of vanillate (Figure 4.6) (Allard et al. 1985). The results of experiments with mixtures of benzoate and 2,5-dichlorobenzoate using variants of a strain of Pseudomonas aeruginosa grown in chemostat cultures have revealed the following important aspects of environmental signiicance (van der Woude et al. 1995): a. Variants that formed stable cultures could be obtained by growth limitation with both benzoate and 2,5-dichlorobenzoate. b. One of these variants was capable of 2,5-dichlorobenzoate-limited growth at an oxygen concentration of 11 µM, although the presence of benzoate increased the residual concentration of 2,5-dichlorobenzoate from 0.05 to 1.27 µM. A number of factors may be responsible for these observations, including the oxygen gradient within the cell and the oxygen concentration required for synthesis of the degradative oxygenases. It was concluded that under the low oxygen tensions that might exist in natural ecosystems, the presence of the more readily degraded benzoate necessitated high oxygen afinity for organisms to achieve complete degradation of the 2,5-dichlorobenzoate. In this case, it is relevant to note that the organism was originally isolated after enrichment at high oxygen concentrations. The issue of oxygen concentration is discussed in a wider context later in this chapter.

OH Cl

OCH 3

Cl

Cl

OH

Cl

Cl

OCH 3 OH

Cl

Cl Cl

OCH 3

OH

Cl

OCH 3

Cl Cl

Cl

FIGURE 4.6 Biotransformation of 4,5,6-trichloroguaiacol by Rhodococcus sp. during growth with vanillate.

200

Environmental Degradation and Transformation of Organic Chemicals

PHYSICAL PARAMETERS Physical parameters such as temperature, salinity, pH, and oxygen concentration may critically determine the persistence or otherwise of a xenobiotic under natural conditions, and these should therefore be critically evaluated. Laboratory experiments can be carried out under any of the conditions that simulate the natural environment, and these can be imposed during isolation of the organisms by enrichment and incorporated into the design of subsequent experiments on biodegradation and biotransformation. In practice, most experiments are carried out with mesophiles and at pH values in the vicinity of pH 7, presumably motivated by the fact that these are, or are assumed to be, prevalent in natural ecosystems. It should be emphasized that soil and water temperatures during the winter in high latitudes of both the northern and southern hemispheres are low—probably below 10°C. Greater advantage should therefore be taken of psychrophiles, particularly in investigations aimed at providing realistic estimates of rates for microbial transformation under natural conditions. With the notable exception of the anaerobic sulfate-reducing bacteria, surprisingly few investigations have used truly marine bacteria in spite of the fact that substantial quantities of xenobiotics are discharged into the open sea either directly or via input from rivers. These issues are discussed in the next section.

TEMPERATURE The role of temperature may be of particular signiicance for mixed cultures of organisms in the natural environment, or when they are used in laboratory studies. Temperature may effect important changes both in the composition of the microbial lora and on the rates of reaction. Greatest attention has hitherto been directed to hydrocarbons and PCBs. Some illustrative examples of important issues that are especially relevant to bioremediation include the following: 1. An anaerobic sediment sample was incubated with 2,3,4,6-tetrachlorobiphenyl at various temperatures between 4 and 66°C (Wu et al. 1997a). The main products were 2,4,6- and 2,3,6-trichlorobiphenyl, and 2,6-dichlorobiphenyl. The irst was produced maximally and discontinuously at 12 and 34°C, the second maximally at 18°C, and the third was dominant from 25 to 30°C. Dechlorination was not observed above 37°C. In a further comparable study with Arochlor 1260, hexa- to nanochlorinated congeners were dechlorinated with a corresponding increase in tri- and tetrachloro congeners, and four dechlorination patterns associated with different temperature ranges could be distinguished (Wu et al. 1997b). 2. Sediment samples from a contaminated site were spiked with Arochlor 1242 and incubated at 4°C for several months (Williams and May 1997). Degradation by aerobic organisms in the upper layers of the sediment—but not in those at >15 mm from the surface—occurred with the selective production of di- and trichlorobiphenyls. Some congeners, including 2,6- and 4,4-dichlorobiphenyls and a range of trichlorobiphenyls, were not found. 3. The enrichment of arctic soils from Northwest Territories, Canada with biphenyl yielded organisms that were assigned to the genus Pseudomonas (Master and Mohn 1998). Rates of removal of individual congeners of Arochlor 1242 were examined at 7°C, and compared with those for the mesophilic Burkholderia cepacia strain LB400. The spectrum of rates for all congeners was similar for the arctic strains and those for some of the trichlorinated congeners was considerably greater than those obtained for Burkholderia cepacia strain LB400. 4. The mineralization of 14C-ring-labeled toluene was examined in contaminated and uncontaminated samples from an aquifer in Alaska and one in South Carolina (Bradley and Chapelle 1995). A number of important facts emerged: a. Rates for organisms from South Carolina were greater for the contaminated sample than for the uncontaminated sample, and for the uncontaminated sample were zero at 5°C.

Determinants and Interactions

201

b. Rates for organisms from the contaminated site in Alaska were highly sensitive to temperature, and showed a distinct maximum at 20°C that was not apparent for those from the uncontaminated site. In contrast, rates for both groups of organisms were virtually identical at 5 and 35°C. 5. The aerobic degradation of hydrocarbons has been examined in many cold-temperature regions—Arctic (Whyte et al. 1996; Yu et al. 2000), Alpine (Margesin et al. 2003), and Antarctic (Ruberto et al. 2003; Aislabie et al. 2004)—and in both terrestrial and marine environments. A number of psychotrophic organisms that were isolated from various sites in northern Canada were capable of mineralizing naphthalene, toluene, and linear dodecane and hexadecane at 5°C. Although some of the positive strains possessed genes homologous with those required for metabolism of the substrates by established pathways—nahB for naphthalene and xylE and todC1 for toluene—others showed only low homologies and may have possessed novel catabolic genes (Whyte et al. 1997). Two organisms assigned to the genus Pseudomonas degraded alkanes (C5–C12), and toluene, and naphthalene at both 5°C and 25°C (Whyte et al. 1998). It was shown by PCR and DNA sequence analysis that the plasmid-borne catabolic genes were comparable to those for the alk pathway in P. oleovorans and the nah pathway in P. putida G7. 6. Anaerobic psychrophilic sulfate-reducing bacteria isolated using lactate as substrate were assigned to the genera Desulfofrigus, Desulfofaba, and Desulfotalea, and could grow at temperatures down to –1.8°C. Most strains were able to use Fe(III)citrate as electron acceptors as well as sulfate, and a range of C1–C4 carboxylates as electron donors (Knoblauch et al. 1999). 7. Experiments using a luidized-bed reactor showed that the removal of chlorophenols could be accomplished by organisms adapted to a temperature of 5–7°C (Järvinen et al. 1994).

OXYGEN CONCENTRATION The question of oxygen concentration is a good deal more complex. The extreme conditions in which oxygen concentration is high, for example in well-mixed surface waters, or essentially absent, for example, in organic-rich deep sediments, are readily visualized. Although these conditions can be realized in laboratory experiments, it is worth drawing attention to a number of less clear-cut situations: 1. Under conditions of oxygen limitation in continuous culture, mixed populations of aerobic bacteria and the strictly anaerobic Methanobacterium formicicum and Methanosarcina barkeri could be maintained (Gerritse and Gottschal 1993a). 2. The existence of microaerophilic organisms such as Wolinella succinogenes that was formerly considered an anaerobe or, conversely, the oxygen tolerance of many clostridia, suggests that such organisms may occupy an ecological niche between the two extremes already noted. 3. Although Pseudomonas aeruginosa is normally considered an aerobic organism, growth can take place by denitriication or by fermentation of arginine. There are also several lines of evidence that support its tolerance of oxygen limitation that may be relevant to its survival in bioilms and it role in pathogenesis: a. Under oxygen stress, Pseudomonas aeruginosa strain PAO1 produces polysaccharide on the cell surface that may limit the diffusion of oxygen into the cell (Sabra et al. 2002). b. Pseudomonas aeruginosa strain PAO1 was able to survive anaerobic conditions by the fermentation of pyruvate. Although pyruvate is incapable of supporting growth, it is transformed under anaerobic conditions to lactate, acetate, and succinate (Eschbach et al. 2004).

202

Environmental Degradation and Transformation of Organic Chemicals

c. During pyruvate fermentation in a complex medium, arginine deiminase (ArcA), catabolic ornithine carbamoyltransferase (ArcB) and carbamate kinase (ArcC) were induced, and survival of the organism was dependent on a protein (PA3309) related to universal stress proteins (Schreiber et al. 2006). Oxygen concentration is important in a range of contexts, for example, (a) regulating the synthesis of peroxidases in white-rot fungi, (b) determining the outcome of the degradation of the trichloromethyl group in a substituted pyridine by Nitrosomonas europaea, and (c) inducing cytochrome P45014DH in Saccharomyces cerevisiae. Anaerobic Bacteria It is well established from laboratory practice that anaerobic microorganisms differ widely in their oxygen tolerance, ranging from the strictly anaerobic methanogens to the more tolerant clostridia. Although strictly anaerobic bacteria do not generally grow in the presence of high-potential electron acceptors such as oxygen or nitrate, there are a number of intriguing exceptions. For example, an obligately anaerobic organism uses nitrate as electron acceptor during the degradation of resorcinol (Gorny et al. 1992). The normally strictly anaerobic sulfate-reducing organisms Desulfobulbus propionicus and Desulfovibrio desulfuricans may grow by reducing nitrate or nitrite to ammonia using hydrogen as the electron donor (Seitz and Cypionka 1986). This draws attention to the unknown extent to which such organisms exist in natural systems, since strictly anaerobic conditions are not always used for the isolation of organisms using nitrate as an electron acceptor. A few examples illustrate the occurrence of oxygen tolerance among bacteria that are normally considered as strictly anaerobic: a. Desulfovibrio vulgaris Hillsborough is capable of growth at oxygen concentrations of 0.24–0.48 µM, and it was suggested that this organism might protect anoxic environments from adverse effects resulting from the intrusion of oxygen (Johnson et al. 1997). b. The anaerobic Geobacter sulfurreducens is able to use oxygen as terminal electron acceptor, and can grow at oxygen concentrations up to 10% (Lin et al. 2004). It was suggested that this would contribute to its survival under oxic conditions. c. Although bacteria belonging to the genus Clostridium are generally considered to be obligate anaerobes, there are important exceptions. Clostridium acetobutylicum and Cl. aminovalericum can grow under microaerophilic conditions and consume oxygen. The gene that encoded NADH oxidase was unregulated in Cl. aminovalericum when microaerophilic conditions were attained, and a number of NAD(P)H-dependent enzyme activities were induced in Cl. acetobutylicum (Kawasaki et al. 2005). d. Among bacteria considered strict anaerobes, cytochrome bd-oxidases have been found, and these enable the organisms to tolerate and reduce low levels of oxygen. Such cytochromes have been found in Bacteroides fragilis (Baughn and Malamy 2004), Desulfovibrio gigas (Lemos et al. 2001), and Moorella thermoacetica (Das et al. 2005). Aerobic and Facultatively Anaerobic Organisms 1. Facultatively anaerobic organisms can employ either fermentative or oxidative modes for the metabolism of appropriate substrates such as carbohydrates, while others can use nitrate as an alternative electron acceptor in the absence of oxygen. Such organisms have, therefore, two metabolic options, even though they may often be mutually exclusive. An illustrative example of the metabolic lexibility of facultatively anaerobic organisms is provided by the type strains of all the species of the enteric genus Citrobacter. These organisms were able to degrade a number of amino acids including glutamate using either respiratory or fermentative metabolism, and they could rapidly switch between these alternatives (Gerritse and Gottschal 1993b). Under anaerobic conditions, the initial steps of

Determinants and Interactions

203

glutamate degradation involved the formation of 3-methylaspartate, mesaconate, and citramalate, which are typical of clostridial fermentations. Although the oxygen concentration in natural environments may be highly variable, organisms with such a high degree of metabolic lexibility may reasonably be presumed to be at an advantage. 2. Oxygen toxicity under aerobic conditions may result from the synthesis of toxic compounds including superoxide, hydrogen peroxide, or hydroxyl radicals. Further details have emerged from observations that the Fe isoenzyme of superoxidase dismutase is synthesized by Escherichia coli under anaerobic conditions, in contrast to the Mn isoenzyme that is produced only under aerobic conditions. The synthesis of the former facilitates the transition from anaerobic to aerobic conditions by destroying the superoxide radical generated after exposure to oxygen (Kargalioglu and Imlay 1994). This lexibility is important in environments where luctuating oxygen concentrations prevail. Studies with mutants of Pseudomonas aeruginosa in which the synthesis of Mn superoxide dismutase and Fe superoxide dismutase were impaired showed that growth in a complex medium or in a deined glucose medium was adversely affected by the latter but only insigniicantly by the former (Hassett et al. 1995). Concentrations of Fe must be regulated, since excess of Fe within the cell would result in the production of deleterious hydroxyl radicals from molecular oxygen (Touati et al. 1995). The transport of Fe into the cell is regulated by Fe(III) high-afinity siderophores which are synthesized within the cell and excreted into the medium before transport of the complexes into the cell by speciic membrane transporters (Wandersman and Delepelaire 2004). In this way, homeostasis is achieved. 3. There is substantial evidence that organisms that are strictly dependent on the aerobic metabolism of substrates for growth and replication may nonetheless accomplish biodegradations and biotransformations under conditions of low oxygen concentration. Indeed, such conditions may inadvertently prevail in laboratory experiments using dense cell suspensions; it is important to appreciate that the growth of these aerobic organisms may be limited by the availability of oxygen. A number of examples are given below to illustrate the environmental role of putatively aerobic organisms under conditions of low oxygen concentration: a. The rate of biodegradation of hexadecane in a marine enrichment culture was unaffected until oxygen concentrations were lower than 1% saturation (Michaelsen et al. 1992). b. It has been shown that the degradation of pyrene by a strain of Mycobacterium sp. can take place at low oxygen concentrations (Fritzsche 1994). c. Alcaligenes sp. strain L6 that was obtained after enrichment with 3-chlorobenzoate in an atmosphere of only 2% oxygen in the gas phase possessed both 2,5- and 3,4dihydroxybenzote dioxygenase activities although it lacked catechol dioxygenase activity that would be required for ission of the aromatic ring (Krooneman et al. 1996). The afinity for the substrate of cells grown under oxygen limitation was three times greater than was observed under excess oxygen, and exceeded values for other bacteria growing with benzoate or 2,5-dichlorobenzoate. This strain that metabolized 3-chlorobenzoate by the gentisate pathway was, under low oxygen concentrations, able to compete successfully with a Pseudomonas sp. strain A that used the catechol pathway (Krooneman et al. 1998). d. Further details emerged from the results of experiments that compared the kinetic properties of catechol-2,3-dioxygenases from toluene-degrading pseudomonads isolated from aquifer sands or groundwater (strains W 31 and CFS 215) with other strains (P. putida F1). This revealed a number of signiicant differences that may plausibly be associated with the low oxygen concentrations pertaining in the environment from which the strains were isolated. For strains that degraded toluene via cis-toluene2,3-dihydrodiol and 3-methylcatechol, lower values of Km were observed for O2 and 3-methylcatechol, whereas higher values of Vmax for O2 and 3-methylcatechol were found (Kukor and Olsen 1996) (Table 4.1).

204

Environmental Degradation and Transformation of Organic Chemicals

TABLE 4.1 Values of Km and Vmax for O2 and 3-Methylcatechol in Strains F1, W31, and CFS 215 Km Substrate

Vmax Substrate

Strain

O2

3-Methylcatechol

O2

3-Methylcatechol

F1 W31 CFS 215

9.7 2.0 0.9

16.9 0.3 0.5

4.3 293 400

17 125 180

e. The growth of Pseudomonas putida strains KT2442 and mt-2 on aromatic carboxylates decreased with O2 concentrations 4 (Käppeli 1986; Tanaka and Ueda 1993). The alkane hydroxylase of Candida tropicalis is located within the microsomes that contain cytochrome P450 and NADPH-cytochrome c reductase (references in Käppeli 1986). In contrast, degradation of the alkanoate is carried out in peroxisomes that contain the β-oxidation enzymes—alkanoate oxidase, enoyl-CoA hydratase, and 3-hydroxyacylCoA dehydrogenase. Yeasts of the genus Candida excrete α,ω-dicarboxylates during growth on n-alkanes as the carbon source, and the cytochrome P450 gene family (CYP52) in Candida tropicalis is a determinant of this transformation (Craft et al. 2003). 3. In the hydroxylation of n-propane to n-propanol by Nocardia parafinicum (Rhodococcus rhodochrous) ATCC 21198, the ratio of hydrocarbon to oxygen consumed was 2:1 and this suggests that the reaction of two molecules of propane and one molecule of dioxygen

304

Environmental Degradation and Transformation of Organic Chemicals R

FIGURE 7.10

CH2

CH3

R CH

CH2

R CH2 CH2OH

R CH2 CO2H

Biodegradation of an alkane under anaerobic conditions.

produced two molecules of alkanol (Babu and Brown 1984). This reaction is formally analogous to the oxidation of 2-nitropropane to acetone by lavoenzymes in Hansenula mrakii (Kido et al. 1978) and Neurospora crassa (Gorlatova et al. 1998). 4. An unusual pathway has been proposed for the degradation of n-decane to the carboxylic acid by Pseudomonas sp. strain 196Aa under anaerobic conditions, apparently in the absence of an electron acceptor. This involved initial dehydrogenation, followed by hydroxylation and dehydrogenation (Figure 7.10), and was supported by puriication of an NAD-linked alkane dehydrogenase, an NADPH-linked alkene hydroxylase, and an FAD Fe-dependent alcohol dehydrogenase (Parekh et al. 1977). Possibly this organism is not, in fact, an aerobic pseudomonad, although the survival of Pseudomonas aeruginosa under anaerobic conditions by pyruvate fermentation has been observed (Schreiber et al. 2006). 5. It is worth noting that the aerobic degradation of hexadecane may be accomplished at quite low oxygen concentrations (Michaelsen et al. 1992). Anaerobic Conditions Considerable effort has been directed to the anaerobic degradation of alkanes. There has been renewed interest in the anaerobic degradation of methane since this represents an important sink for methane in anaerobic sediments where it is produced by methanogenesis. Although the organisms responsible have not hitherto been isolated in pure culture, the anaerobic oxidation of methane probably involves consortia of archaea and sulfate-reducing bacteria (Teske et al. 2002; Schouten et al. 2003; Girguis et al. 2005), and may possibly occur by reverse methanogenesis (Hallam et al. 2004). Genes for both anaerobic methane oxidation and methanogenesis were found together with those for aerobic methane oxidation at the surface of a single site in Japan (Inagaki et al. 2004). There is evidence for the anaerobic degradation of alkanes to CO2, plausibly under conditions of sulfate reduction. In experiments with sediment slurries from contaminated marine areas, 14CO2 was recovered from 14C-hexadecane (Coates et al. 1997), and was inhibited by molybdate that is consistent with the involvement of sulfate reduction. Under sulfate-reducing conditions 14CO2 was produced from 14C[14,15]octacosane (C28H58) (Caldwell et al. 1998). Different mechanisms have been elucidated for the anaerobic degradation of higher alkanes, and both occurred simultaneously in a sulfate-reducing consortium (Callaghan et al. 2006): 1. Reaction at the subterminal position with fumarate can be initiated by a free-radical reaction (Rabus et al. 2001). In a denitrifying organism that degraded n-hexane (Figure 7.11) (Wilkes et al. 2002) and a sulfate-reducing organism that degraded hexadecane (Callaghan et al. 2006), this is followed by a rearrangement analogous to that of succinate → malonate and sequential loss of acetate. Comparable reactions have been described for a sulfate-reducing enrichment culture (Davidova et al. 2005), and the sulfate-reducing Desulfatibacillum aliphaticivorans that can oxidize C13 to C18 alkanes (Cravo-Laureau et al. 2005). An analogous pathway is used for the degradation of ethylcyclopentane by a sulfate-reducing enrichment culture, which is discussed in Part 2 of this chapter. 2. An alternative involved carboxylation at C3 followed by loss of the C1–C2 fragment and further degradation of the resulting terminal carboxylate by β-oxidation (So et al. 2003) (Figure 7.12).

305

Aliphatic Compounds

CH 3 (CH 2 )3 CH 2 CH 3

CH 3 CO 2 H

CH 3 (CH 2 )3 CH

CH 3

CO 2 H

CH 3 (CH 2 )3 CH−CH2CH COSCoA

CO 2 H CH 3 CH 3 (CH 2 )3 CH−CH

FIGURE 7.11

CH−COSCoA

CH 3 CO−SCoA

Anaerobic degradation of alkanes. CO 2 H

CH 3 (CH 2 )n CH 2 CH 2 CH 3

FIGURE 7.12

CH 3 (CH 2 )n CH

CH 2 CH 3

CH 3 (CH 2 )n CH 2 CO 2 H + C 2

Anaerobic degradation of n-alkanes.

ALKENES Aerobic Conditions Two kinds of investigations have been carried out (a) growth of microorganisms at the expense of alkenes and (b) biotransformations resulting in the synthesis of epoxides. For example, growth has been demonstrated at the expense of propene and butene (Van Ginkel and de Bont 1986). An interesting observation is the pathway for the degradation of intermediate n-alkenes produced by an aerobic organism under anaerobic conditions (Parekh et al. 1977). Although the generality of this pathway remains unknown, it is clearly possible that even aerobic bacteria under anoxic conditions might accomplish comparable degradations. Attention is drawn to the possibility that intermediate metabolites may be incorporated into biosynthetic pathways. For example, hexadecene is oxidized by the fungus Mortierella alpina by ω-oxidation (Shimizu et al. 1991), but the lipids contain carboxylic acids with both 18 and 20 carbon atoms including the unusual polyunsaturated acid 5-cis, 8-cis,11-cis,14-cis,19-eicosapentaenoic acid. Direct ission of the double bond by oxidation exempliies the simplest, though less common reaction. A few illustrations are given: 1. The degradation of squalene by Marinobacter sp. strain 2sq31 (Rontani et al. 2002) is initiated by oxidative ission, although the subsequent steps are carried out by β-oxidation and carboxylation that are comparable to those used for branched alkanes. 2. An extracellular enzyme from Xanthomonas sp. is able to degrade poly(cis-1,4-isoprene) with the production of 12-keto-4,8-dimethyltrideca-4,8-diene-1-al (Braaz et al. 2004), and functions as a heme-dependent oxygenase (Braaz et al. 2005). The irst step in the aerobic degradation of alkenes is, however, generally epoxidation. Alkene monooxygenase is closely related to the aromatic monooxygenases, and is able to hydroxylate benzene, toluene, and phenol (Zhou et al. 1999), while the alkane hydroxylase from Pseudomonas oleovorans is able to carry out both hydroxylation and epoxidation (Ruettinger et al. 1977). In Xanthobacter sp. strain Py2, which can carry out epoxidation of alkenes from C2 to C6, the monooxygenase has been characterized, and consists of an oxygenase, a ferredoxin, and a reductase (Small and Ensign 1997). Epoxidation may be followed by several alternatives, which may be summarized before further discussion: (a) hydrolysis to a 1,2-diol, (b) nucleophilic attack by coenzyme M followed by dehydrogenation, and (c) a reductive glutathione-mediated reaction. In detail, the degradation of epoxides is quite varied and several different pathways have been observed. 1. Degradation of epichlorohydrin (1-chloro-2,3-epoxypropane) may proceed by hydrolysis of the epoxide to 3-chloro-1,2-propanediol that is then converted successively into

306

Environmental Degradation and Transformation of Organic Chemicals

3-hydroxy-1,2-epoxypropane (glycidol) followed by hydrolysis to glycerol before degradation (van den Wijngaard et al. 1989). Epoxide hydrolases have been isolated and characterized from bacteria that are able to use epoxides as growth substrates. A Corynebacterium sp. is able to grow with alicyclic epoxides, and the sequence of the hydrolase (Misawa et al. 1998) is similar to the enzyme from Agrobacterium radiobacter strain AD1 that used epichlorohydrin (1-chloro-2,3-epoxypropane) as growth substrate (Rink et al. 1997). Examination of mutants of this strain prepared by site-directed mutagenesis showed that the mechanism involves nucleophilic attack by Asp107 at the terminal position of the substrate followed by hydrolysis of the resulting ester mediated by His275. Analogy may be noted with the inversion accompanying hydrolysis of 2-haloacids mediated by l-2-haloacid hydrolase. Limonene-1,2-epoxide hydrolases from Rhodococcus erythropolis DCL14 that are intermediates in the degradation of both (+)-(4R)- and (−)-(4S)-limonene (Van der Werf et al. 1999) differ from these groups of enzymes, and do not involve the catalytic function of histidine residues (Van der Werf et al. 1998). 2. Hydrolysis to the diol followed by dehydration to the aldehyde and oxidation to the carboxylic acid is used by a propene-utilizing species of Nocardia (de Bont et al. 1982). Although an ethene-utilizing strain of Mycobacterium sp. strain E44 degrades ethane-1,2-diol by this route, the diol is not an intermediate in the metabolism of the epoxide (Wiegant and de Bont 1980). 3. The aldehyde may also be produced directly from the epoxide. This occurs in the metabolism of ethene by Mycobacterium sp. strain E44 (Wiegant and de Bont 1980), of styrene by a strain of Xanthobacter sp. strain 124X (Hartmans et al. 1989), and by Corynebacterium sp. strains ST-5 and AC-5 (Itoh et al. 1997). The reductase in the coryneforms has a low substrate speciicity, and is able to reduce acetophenone to 3-phenylethan-2-ol with an enantiomeric excess >96%. In Rhodococcus rhodochrous, however, styrene is degraded by ring dioxygenation with the vinyl group intact (Warhurst et al. 1994): 2-vinyl-cis, cis-muconate is produced by catechol 1,2-dioxygenase as a terminal metabolite and complete degradation is carried out by catechol 2,3-dioxygenase activity that is also present. 4. Xanthobacter sp. strain Py2 may be grown with propene or propene oxide. On the basis of amino acid sequences, the monooxygenase that produces the epoxide was related to those that catalyzes the monooxygenation of benzene and toluene (Zhou et al. 1999). The metabolism of the epoxide is initiated by nucleophilic reaction with coenzyme M followed by dehydrogenation (Figure 7.13a). There are alternative reactions, both of which are dependent on a pyridine nucleotide-disulide oxidoreductase (Swaving et al. 1996; Nocek et al. 2002): a. In the absence of CO2, by transformation to acetone that is not further degraded. b. In the presence of CO2 by carboxylation to 3-ketobutyrate (acetoacetate) (Allen et al. 1999; Krum and Ensign 2001). Acetoacetate is used partly for cell growth and partly converted into the storage product poly-β-hydroxybutyrate (Small and Ensign 1995). Kinetic and 13C NMR experiments conirmed that acetoacetate was the irst product from which β-hydroxybutyrate is formed as a secondary metabolite with acetone as the terminal metabolite (Allen and Ensign 1996). The epoxide carboxylase consists of a three-component enzyme—all three of which are necessary for activity (Allen and Ensign 1997). Coenzyme M (2-mercaptoethanesulfonate) is required, component II is a lavin containing NADPH: disulide oxidoreductase (Nocek et al. 2002), and the interactions involving NADP+, FAD, the disulide, and the 2-ketopropyl-CoM are shown in Figure 7.13b (Clark et al. 2000; Boyd et al. 2006). An analogous mechanism operates in the degradation of epichlorohydrin (1-chloro-2,3-epoxypropane) by the same strain (Small et al. 1995). c. The metabolism of acetone that converges with the metabolism of propene oxides in Xanthobacter sp. strain Py2 is accomplished by an ATP-dependent carboxylase with production of acetoacetate (Sluis et al. 1996, 2002).

307

Aliphatic Compounds O

CH 3 C

CH 3

O

H

C

C

H

H C

H

H

CH 3

OH CoM

S

CH 2

OH

CH 3

C

H CoM

S

CH 2

C

H

CH 3 NAD

NAD

CoM

S

CH 2

CO CH3

CO 2

HO2C CH 2 COCH3

FIGURE 7.13

Reaction of epoxide with coenzyme M.

CH 3

C CH CH 2

FIGURE 7.14

CH 2 OH

CH 2

CH 2 CH 3

C

O

CH 3

CH CH 2

C

SGl

CH CH 2

CH 2 OH CH 3

CH CH CH 2

Glutathione-mediated degradation of isoprene.

5. Rhodococcus sp. strain AD45 carried out the transformation of 2-methyl-1,3-butadiene (isoprene), and both cis- and trans-dichloroethenes to the epoxides (van Hylckama Vlieg et al. 1998). Degradation of the diene (Figure 7.14) takes place by a pathway involving a glutathione S-transferase that is able to react with the epoxides and a conjugate-speciic dehydrogenase that produces 2-glutathionyl-2-methylbut-3-enoate (van Hylckama Vlieg et al. 1999, 2000). 6. The degradation of vinyl chloride and ethene has been examined in Mycobacterium sp. strain JS 60 (Coleman and Spain 2003) and in Nocardioides sp. strain JS614 (Mattes et al. 2005). For both substrates, the initially formed epoxides underwent reaction with reduced coenzyme M and, after dehydrogenation and formation of the coenzyme A esters, reductive loss of coenzyme M acetate resulted in the production of S-acetyl-coenzyme A. The reductive ission is formally analogous to that in the glutathione-mediated reaction. Epoxides may be formed from alkenes during degradation by Pseudomonas oleovorans, although octan-1,2-epoxide is not further transformed, and degradation of oct-1-ene takes place by ω-oxidation (May and Abbott 1973; Abbott and Hou 1973). The ω-hydroxylase enzyme is able to carry out either hydroxylation or epoxidation (Ruettinger et al. 1977). Considerable attention has been directed to the epoxidation of alkenes on account of interest in the epoxides as industrial intermediates. The wide metabolic capability of MMO, which has already been noted, has been applied to the epoxidation of C2, C3, and C4 alkenes (Patel et al. 1982). A large number of propane-utilizing bacteria are also effective in carrying out the epoxidation of alkenes (Hou et al. 1983). Especially valuable is the possibility of using microorganisms for resolving racemic mixtures of epoxides. For example, this has been realized for cis- and trans-2,3-epoxypentanes

308

Environmental Degradation and Transformation of Organic Chemicals CH 3 O

CH 3

C2 H5

O

H

;

H

H

(2S, 3S)

O

H

C2 H5

H

(2S, 3R)

H

O

H

C2 H5

;

CH 3

C2 H5

(2R, 3S)

FIGURE 7.15

CH 3

H

(2R, 3S)

Biodegradability of enantiomeric of epoxides of cis- and trans-pent-2-enes.

using a Xanthobacter sp., which is able to degrade only one of the pairs of enantiomers leaving the other intact (Figure 7.15) (Weijers et al. 1988). Bacterial epoxidation of alkenes and fungal enzymatic hydrolysis of epoxides have been reviewed in the context of their application to the synthesis of enantiomerically pure epoxides and their derivatives (Archelas and Furstoss 1997). One of the disadvantages of using bacteria, which may carry out undesirable degradation, may sometimes be overcome by the use of fungi (Archelas and Furstoss 1992), although the initially formed epoxides are generally hydrolyzed by fungal epoxide hydrolase activities. Other aspects of epoxide formation and degradation are worth noting, particularly on account of their biotechnological relevance. a. Although Mycobacterium sp. strain E3 is able to degrade ethene via the epoxide, the epoxide-degrading activity is highly speciic for epoxyethane and degradation requires reductant generated from glycogen or trehalose storage material (de Haan et al. 1993). b. In Xanthobacter sp. strain Py2 both the alkene monooxygenase and the epoxidase are induced by C2, C3, and C4 alkenes, and also by chlorinated alkenes including vinyl chloride, cis- and trans-dichloroethene, and 1,3-dichloropropene (Ensign 1996). As an alternative to epoxidation of alkenes, hydration is occasionally used, for example in degradation of the ring-ission products from dioxygenation and dehydrogenation of tetralin (Figure 7.16) (Hernáez et al. 2000, 2002). Although the aerobic degradation of squalene involves oxidation and ission at ∆10–11, degradation under anaerobic conditions involves hydration and carboxylation (Rontani et al. 2002) (Figure 7.17). Anaerobic Conditions Degradation of hex-1-ene has been observed in a methanogenic consortium (Schink 1985a) that converted the substrate into methane, and a plausible pathway involving hydration and oxidation was suggested.

ALKYNES The degradation of alkynes has been the subject of sporadic interest during many years, and the pathway has been clearly delineated. It is quite distinct from those used for alkanes and alkenes, and is a relection of the enhanced nucleophilic character of the alkyne C≡C bond. The initial step is hydration of the triple bond followed by ketonization of the initially formed enol. This reaction operates during the degradation of acetylene itself (de Bont and Peck 1980), acetylene carboxylic acids (Yamada and Jakoby 1959), and more complex alkynes (Figure 7.18) (Van den Tweel and de Bont 1985). It is also appropriate to note that the degradation of acetylene by anaerobic bacteria proceeds by the same pathway (Schink 1985b).

309

Aliphatic Compounds OH

OH OH

OH

O HO2C

CO2H OH

OH CO2H CO2H

HO2C OH

FIGURE 7.16

O

CHO + CH3CO−CO2H

HO2C

Aerobic degradation of tetralin by hydration.

CH 2 CH 2

HO CH 2 CH 2

CO 2

O CH 2 CH 2

FIGURE 7.17

Aerobic degradation of squalene.

FIGURE 7.18

Aerobic biodegradation of but-3-ynol.

+

HO 2 C

Acetylene is able to support the growth of the anaerobe Pelobacter acetylenicus (Schink 1985b), and undergoes initial hydration to acetaldehyde followed by dismutation into acetate and ethanol. Although the enzyme is stable in air, it requires a strong reductant such as Ti(III) or dithionite for its activity (Rosner and Schink 1995). The hydratase is a tungsten iron–sulfur protein with a [4Fe–4S] cluster in the reduced state and contains a molybdopterin cofactor conjugated with guanosine monophosphate (Meckenstock et al. 1999).

ALKANOLS Aerobic Conditions Essential aspects of the aerobic degradation of alkanols have already been covered in the context of the degradation of alkanes. Only one additional comment is added: the initial reactions involved

310

Environmental Degradation and Transformation of Organic Chemicals

in the metabolism of higher alkanes (>C1) are formally similar to those used for the metabolism of methane, and the soluble alkanol dehydrogenases also contain PQQ (references in Anthony 1992). Enzymatically, however, the details may be more complex since, for example, a number of distinct alcohol and fatty acid dehydrogenases have been isolated from an Acinetobacter sp. during the metabolism of hexadecane (Singer and Finnerty 1985a,b). Anaerobic Conditions Anaerobic oxidation of methanol—though not incorporation into cellular material—has been observed in a sulfate-reducing bacterium (Braun and Stolp 1985). Ethanol may be converted into methane by Methanogenium organophilum (Widdel 1986; Frimmer and Widdel 1989), and oxidation of primary alkanols has been demonstrated in Acetobacterium carbinolicum (Eichler and Schink 1984). Secondary alcohols such as propan-2-ol and butan-2-ol may be used as hydrogen donors for methanogenesis with concomitant oxidation to the corresponding ketones (Widdel et al. 1988). An NAD-dependent alcohol dehydrogenase has been puriied from Desulfovibrio gigas that can oxidize ethanol, and it has been shown that the enzyme does not bear any relation to classical alcohol dehydrogenases (Hensgens et al. 1993). The metabolism of 1,2-diols has attracted considerable attention, and in particular that of glycerol in view of its ubiquity as a component of lipids. Widely different pathways have been found of which two are given as illustration: a. Anaerovibrio glycerini ferments glycerol to propionate (Schauder and Schink 1989) and Desulfovibrio carbinolicus to 3-hydroxypropionate (Nanninga and Gottschal 1987). b. Desulfovibrio alcoholovorans converts glycerol into acetate, and 1,2-propandiol to acetate and propionate (Qatibi et al. 1991).

ALKANONES These may be degraded under aerobic conditions by a sequence involving Baeyer–Villiger monooxygenation to lactones followed by hydrolysis. The resulting alkanols are then degraded to α,ω-carboxylic acids by the reactions following terminal hydroxylation, which have already been described (Figure 7.4). This is used in one of the pathways used for the degradation of 6,10,14-trimethylpentadecan-2-one by Marinobacter sp. strain CAB that involves insertion of an oxygen atom between C2 and C3 and subsequent hydrolysis and oxidation with loss of C2 and C3 (Rontani et al. 1997). The aerobic metabolism of acetone by Xanthobacter sp. strain Py2 involves at ATP-dependent carboxylation (Sluis et al. 1996), with the direct formation of acetoacetate. The carboxylase has been characterized from Xanthobacter autotrophicus strain Py2, and from the anaerobic phototroph Rhodobacter capsulatus strain B10 (Sluis et al. 2002). It has an α2β2γ2 subunit composition and EPR measurements conirm the presence of Mn2+ (Boyd et al. 2004). The anaerobic degradation of ketones also involves carboxylation followed by hydrolysis (Platen and Schink 1990; Hirschler et al. 1998) (Figure 7.19). There are two subsequent pathways in anaerobes: (1) oxidation to CO2 in denitrifying and sulfate reducing bacteria by the acetyl-CoA-CO dehydrogenase pathway and (2) an anabolic pathway by a modiied tricarboxylate-glyoxylate cycle (Janssen and Schink 1995a). Methylglyoxal is a metabolite of unregulated carbohydrate metabolism that is toxic to the cell. Detoxiication in Escherichia coli can be achieved by several mechanisms (Ko et al. 2005): (a) by successive reduction to hydroxyacetone and 1,2-propandiol, (b) by reduction to 2-hydroxyacetaldehyde, and (c) by the activity of glyoxalase to d-lactate (Figure 7.20) (Clugston et al. 1998). In Clostridium beijerinckii, however, detoxiication is carried out only by reduction to 1,2-propandiol (Liyanage et al. 2001).

311

Aliphatic Compounds CO2H RCH2COCH3

FIGURE 7.19

RCH2CO2 H + CH3CO2H

RCH−COCH3

Anaerobic degradation of ketones. GSH

OH SG

CH 3 HO

C

C

OH

O

SG

SG

H CH3

C

OH CO2H

FIGURE 7.20 Conversion of methylglyoxal into d-lactate.

ALKYLAMINES AND AMINO ACIDS Aerobic Conditions Alkylamines The initial reaction in the biodegradation of primary alkylamines is conversion into the aldehyde and subsequent reactions converge on those for the degradation of primary alkanes. There are a number of important details in this apparently straightforward reaction: 1. The conversion of alkylamines into aldehydes may be accomplished by different mechanisms: (a) by oxidases that convert molecular oxygen to H2O2 or (b) by dehydrogenases. Which of these is used depends on the organism. For example, the dehydrogenase is used by Pseudomonas aeruginosa ATCC 17933, P. putida ATCC 12633, and the methylotroph Paracoccus versutus ATCC 25364. In contrast, Klebsiella oxytoca ATCC 8724, Escherichia coli ATCC 9637, and Arthrobacter sp. NCIB 11625 use a copper-quinoprotein amine oxidase (Hacisalihoglu et al. 1997) that contains copper at the active site (Wilmot et al. 1999). An inducible primary amine dehydrogenase in a strain of Mycobacterium convolutum had diverse degradative capability with a broad speciicity, and was involved in the degradation of 1- and 2-aminopropane and 1,3-diaminopropane. The products were assimilated by the methylmalonate pathway, or by formation of C2 + C1 fragments (Cerniglia and Perry 1975). 2. An alternative pathway for methylamine in Pseudomonas sp. strain MA and Hyphomicrobium is initiated by the formation of N-methylglutamate with the loss of NH4+, and is mediated by an FMN-containing synthetase (Pollock and Hersh 1973). This is dehydrogenated by a lavoprotein to glutamate and formaldehyde (Bamforth and Large 1977), while established pathways metabolize the resulting formaldehyde. 3. The transformation of 2-aminopropane to alaninol by a strain of Pseudomonas sp. KIE171 involves reaction with glutamate in an ATP-dependent reaction to produce a γ-glutamide. Introduction of a hydroxyl group into the methyl group is followed by hydrolysis to regenerate glutamate, and dehydrogenation to alanine (Wäsch et al. 2002). 4. Species of Pseudomonas can utilize the α,ω-diamines putrescine, spermidine, and spermine as sources of carbon and nitrogen, and putrescine can be produced from the secondary amine spermidine together with 1,3-diaminopropane (Dasu et al. 2006). Putrescine (1,4-diaminobutane) is an intermediate in the arginine decarboxylase (ADC) pathway of l-arginine degradation, which is described later, and can be degraded, by two pathways: a. In Pseudomonas aeruginosa via the analogous intermediates used for primary amines— oxidative deamination to 4-aminobutyraldehyde, followed by dehydrogenation to 4-aminobutyrate and oxidative deamination to succinate semialdehyde (Lu et al. 2002) b. In Escherichia coli by an ATP-dependent production of γ-glutamyl putrescine followed by conversion of the terminal–CH2NH2 group into carboxylate and removal of glutamate (Kurihara et al. 2005). Succinate semialdehyde is then produced by reactions, which have already been outlined.

312

Environmental Degradation and Transformation of Organic Chemicals

The degradation of secondary or tertiary amines has been examined most extensively with dimethylamine and trimethylamine. The latter can be degraded by two mechanisms—dehydrogenation to dimethylamine and formaldehyde or monooxygenation to the N-oxide followed by demethylation. The resulting dimethylamine can then be degraded by dehydrogenation. Species of Paracoccus able to degrade tetramethylammonium hydroxide have been assigned to the species Pa. kocurii (Ohara et al. 1990), and those degrading N,N′-dimethylformamide to Pa. aminophilus and Pa. aminovorans (Urakami et al. 1990). Although Aminobacter aminovorans (Pseudomonas aminovorans) was able to utilize methylamine and trimethylamine, it was unable to use methane, methanol, or dimethylamine (Urakami et al. 1992). Considerable effort has been directed to the degradation of complexing agents. The degradation of nitrilotriacetate (NTA), ethylenediamine tetraacetate (EDTA), and related compounds display some important features: a. The degradation of NTA takes place by successive loss of glyoxylate (Cripps and Noble 1973; Firestone and Tiedje 1978), and the monooxygenase system consists of two components, both of which are necessary for hydroxylation (Uetz et al. 1992); b. The irst step in the degradation of EDTA is carried out by a lavin-dependent monooxygenase, which has been puriied (Witschel et al. 1997; Payne et al. 1998), and results in the formation of glyoxal and N,N-ethylenediaminediacetate (EDDA). The ultimate formation of ethylenediamine and glyoxylate is, however, carried out by an oxidase (Liu et al. 2001). It may be assumed that an analogous pathway exists for the degradation of triethylenediaminepentaaacetic acid (DTPA); c. Iminodisuccinate, which is a potential replacement for ETDA, has two asymmetric centers and, since the C−N lyase that cleaves it to d-aspartate and fumarate is stereospeciic, degradation is initiated by the activity of epimerases to the R,S-enantiomer. d-Aspartate is then isomerized to l-aspartate that undergoes elimination to fumarate (Figure 7.21) (Cokesa et al. 2004). The degradation of morpholine has been described in several strains of Mycobacterium, including M. chelonae (Swain et al. 1991), M. aurum strain MO1 (Combourieu et al. 1998), and Mycobacterium strain RP1 (Poupin et al. 1998). Initiation of the degradation of the cyclic secondary amines morpholine, piperidine, and pyrrolidine by the strain of Mycobacterium RP-1 is carried out by cytochrome P450 hydroxylation (Poupin et al. 1998). The irst step in the degradation of the tertiary amine nicotine by Arthrobacter nicotinovorans involves hydroxylation to 6-hydroxynicotine, which is followed by ission of the N-methylpyrrolidine ring by an oxidase (Dai et al. 1968) and is discussed in Part 1 of Chapter 10. Amino acids A number of factors complicate the aerobic metabolism of amino acids—different enzymes may be used even for the same amino acid; the enzymes may be inducible or constitutive depending on their function; α-ketoacids may be produced by deamination or amines by decarboxylation. 1. Pyridoxal 5′phosphate enzymes are generally used when amino acids are supplied as sources of carbon or nitrogen. An aldimine is produced initially and is isomerized to HO2C−CH2 HO 2 C

HH N H

CH 2 CO 2 H

HO 2 C

H +

CO 2 H H

H2 N H

CO 2 H

CH 2

CH 2 CO 2 H

HO 2 C

H

H CO 2H

D-asp

FIGURE 7.21 Aerobic degradation of iminodisuccinate.

CO 2 H

H2 N

CO 2H L-asp

H

CO 2 H

313

Aliphatic Compounds

the corresponding ketimine through loss of the α-proton that is facilitated by a lysine group on the enzyme. The ketimine is then hydrolyzed to pyridoxamine phosphate and an α-ketocarboxylic acid that is incorporated into established catabolic pathways. There are some additional important features: a. Lysine. In pseudomonads, there are different pathways for the degradation of l-lysine (Figure 7.22a) and d-lysine (Figure 7.22b) (Muramatsu et al. 2005). Genetic evidence suggests their connection in Pseudomonas putida strain KT2440 (Revelles et al. 2005), which is an eficient colonizer of important commercial plants in the rhizosphere (Molina et al. 2000). b. L- and D-Leucines are degraded by Pseudomonas aeruginosa in a pathway analogous to that for branched-chain alkanes. This involves formation of isovaleryl-CoA, dehydrogenation to methylcrotonly-CoA that is degraded by terminal carboxylation to 3-methylgutaconyl-CoA before hydroxylation, and ission to acetyl-CoA and acetoacetate (Figure 7.23a) (Massey et al. 1974; Höschle et al. 2005). c. 1-Aminocyclopropane-1-carboxylate. This somewhat unusual amino acid is the immediate precursor of the important plant hormone ethene, and the bacterial deaminase in the rhizosphere has therefore attracted considerable attention (Belimov et al. 2001). Unlike other amino acids, 1-aminocyclopropane-1-carboxylate does not contain the α-proton that is required for conventional deamination, and its degradation involves concomitant ission of the cyclopropane ring to α-ketobutyrate (Figure 7.23b). The mechanism has been examined and several possibilities have been put forward that are consistent with the x-ray structure of the enzyme (Karthikeyan et al. 2004) and with isotopic evidence (Walsh et al. 1981). d. L-Arginine. The degradation of arginine can be accomplished by no less than four different mechanisms depending on the circumstances (Nakada and Itoh 2002). The deiminase pathway enables organisms to grow anaerobically with l-arginine, and includes Bacillus licheniformis, Halobacterium halobium, Streptococcus faecalis, and to a limited extent Pseudomonas aeruginosa. The four pathways are summarized:

CH 2 NH 2 (a)

CH 2 NH 2

(CH 2 )3 CH

(CH 2 )3

NH 2

CONH 2

CO 2 H

CH 2 NH 2 (CH 2 )3

(CH 2 )3

CO 2 H

CO 2 H

CO 2 H L-lysine

CH 2 NH 2 (b) H2 N

(CH 2 )3

CH 2 NH 2 (CH 2 )3

CH

CO

CO 2 H

CO 2 H

N

CO 2 H

D-lysine

CO 2 H

CO 2 H

CO 2 H

(CH 2 )3

(CH 2 )3

(CH 2 )3

CH

NH 2

CO 2 H

FIGURE 7.22

CO

CO 2 H

CO 2 H

Degradation of (a) l-lysine and (b) d-lysine.

N H

CO 2 H

N

CO 2 H

CO 2 H

CH 3

CH 3

CH 2 O

CH 3

CH 3

OH

HO2C−CH2−C−CH2−COSCoA

CH 3

CH−CH2−CO−CO2H

CO 2 H

CH−COSCoA

CH 3

CH 3

CH 3

CH 3

CH

CH−COSCoA

HO2C−CH2−CO−CH3 + CH 3 COSCoA

CH−CH2−COSCoA

Degradation of (a) d- and l-leucine, (b) 1-aminocyclopropane-1-carboxylate.

CO 2 H

NH 2

HO2C−CH2−C

CH 3

NH 2

CH 3

FIGURE 7.23

(b)

(a)

314 Environmental Degradation and Transformation of Organic Chemicals

Aliphatic Compounds

315

Arginine deiminase (ADI) pathway (Mercenier et al. 1980); arginine → citrulline → ornithine + carbamoyl phosphate (ADC) pathway (Lu et al. 2002); arginine → agmatine → N-carbamoylputrescine → putrescine → 4-aminobutyrate Arginine dehydrogenase (ADH) pathway (Nakada and Itoh 2002); 4-aminobutyrate + urea

arginine → 2-ketoarginine →

Arginine succinyltransferase (AST) pathway (Schneider et al. 1998); arginine → N 2 succinylarginine → N 2-succinylornithine → N 2-succinylglutamate → glutamate 2. As an alternative to oxidative deamination, decarboxylation is involved in polyamine biosynthesis and in the protection of enteric bacteria from acidic conditions. Under these conditions, the electrons used to form the ketimine are provided by decarboxylation in place of those from the α-methine group. a. In Escherichia coli—and probably other Enterobacteriaceae—amino acids play a role in the resistance to extremely acid conditions through removal of intracellular protons by decarboxylation. Tolerance is mediated by decarboxylase antiporter systems including arginine/agmatine, glutamate/γ-aminobutyrate, and lysine/cadaverine (Iyer et al. 2003). The irst of these also is involved in the acid resistance of Salmonella enterica serovar Typhimurium under anaerobic conditions (Kieboom and Abee 2006). b. Polyamines have an important function in contributing to the stability of molecular complexes in the cell. The biosynthesis of putrescine generally involves the decarboxylation of arginine or ornithine. There are two decarboxylases for arginine and ornithine, both of which are dependent on pyridoxal 5′-phosphate and Mg2+ (references in Tabor and Tabor 1985), and probably also for lysine (Lemonnier and Lane 1998; Kikuchi et al. 1997). The synthesis of these alternative enzymes is controlled by the conditions under which the cells are grown—aeration at neutral pH, or semianaerobic at low pH. Exceptionally a pyruvoyl-dependent ADC in Methanococcus jannaschii functions in polyamine synthesis (Graham et al. 2002). The 3-aminopropyl group in spermine and spermidine is produced by decarboxylation of S-adenosylmethionine, which is explained in the next paragraph. 3. A completely distinct enzyme has been found in a number of organisms, which carry out the metabolism of amino acids. In this group, a pyruvoyl group is covalently bound to the active enzyme that is produced from a proenzyme in a self-maturation process (Toms et al. 2004). The proenzyme contains a serine residue that undergoes rearrangement to an ester followed by conversion into the β-chain of the enzyme and a dehydroalanine residue that forms the N-terminal pyruvoyl group of the α-chain. This type of enzyme has been found for a number of important decarboxylations: a. Histidine decarboxylation in Lactobacillus including L. buchneri (Huynh and Snell 1985; Martín et al. 2005), which is the most extensively studied. b. Arginine decarboxylation in Methanococcus jannaschii (Graham et al. 2002). c. S-adenosylmethionine carboxylase in Escherichia coli (Markham et al. 1982; Anton and Kutny 1987), Sulfolobus solfataricus (Cacciapuoti et al. 1991), M. jannaschii (Lu and Markham 2004), and Thermotoga maritima (Toms et al. 2004). S-adenosylmethionine carboxylase is the source of the propylamine in the polyamines spermine and spermidine. The activity of spermine synthase introduces this into spermidine and spermine, which has already been noted. It is worth pointing out that, whereas the inducible histidine decarboxylase

316

Environmental Degradation and Transformation of Organic Chemicals

from Gram-positive bacteria belongs to the pyruvoyl group, those from the Gram-negative Enterobacteriaceae including Klebsiella planticola and Enterobacter aerogenes are pyridoxal 5′-phosphate-dependent (Kamath et al. 1991). Anaerobic Conditions A range of C1 compounds such as methylamine, trimethylamine, and betaine can be used by methanogens for the synthesis of methane. Anaerobic degradation of some amino acids by clostridia involves rearrangements and dismutation between pairs, and the biogenic formation of toluene from phenylalanine and of p-cresol from tyrosine is worth noting. Few investigations have been devoted to the anaerobic degradation of alkylamines, though there has been considerable interest in the metabolism of trimethylamine, choline, and glycine betaine as a source of methane in marine sediments (King 1984). Some aspects of the metabolism of alkylamines are used as illustration: 1. Methane formation from trimethylamine by Methanosarcina barkeri has been demonstrated (Hippe et al. 1979; Patterson and Hespell 1979), and the metabolically versatile organisms Methanococcoides methylutens (Sowers and Ferry 1983) and Methanolobus tindarius (Konig and Stetter 1982), which use methylamines and methanol for methane formation, have been described. The methanogen Methanomethylovorans hollandica is able to use a range of methyl substrates including mono-, di-, and trimethylamine as well as dimethyl sulide and methanethiol (Lomans et al. 1999). 2. The metabolism of betaine, which is an important osmoregulatory solute in many organisms, has been studied and different metabolic pathways have been revealed. a. Demethylation to dimethylglycine by Eubacterium limosum (Müller et al. 1981) and by strains of Desulfobacterium sp. (Heijthuijsen and Hansen 1989a). b. Fermentation by a strain of Desulfuromonas acetoxidans with the production of trimethylamine and acetate (Heijthuijsen and Hansen 1989b), while the same products are formed by Clostridium sporogenes in a Stickland reaction with alanine, valine, leucine, or isoleucine (Naumann et al. 1983). 3. The degradation of amino acids has been examined in detail, particularly in clostridia (Barker 1981), and these investigations have revealed a number of important reactions not encountered in other degradations. a. Coenzyme B12–mediated rearrangements have been elucidated as an important reaction in the degradation of glutamate and ornithine, and subsequently, led to a detailed investigation into the role of this rearrangement in other reactions (Barker 1972). An outline of the β-methylaspartate pathway for the degradation of glutamate by Clostridium tetanomorphum is given in Figure 7.24. The involvement of radicals in a number of rearrangements carried out by clostridia during fermentation of amino acids has been discussed in a review (Buckel and Golding 1999). These include S-lysine to

CH 3−CH(CO2H)−CH(NH 2)−CO2H

HO 2C−CH 2−CH2−CH(NH 2)−CO2H

HO 2C

H

OH HO 2C−C−CH 2CO 2H

CH 3

FIGURE 7.24

CO 2H

CH 3−CO2H

CH 3

Biodegradation of glutamate by Clostridium tetanomorphum.

+

CH3−CO−CO2H

317

Aliphatic Compounds CH 2−CH(NH2)CO2H

FIGURE 7.25

N H

CH3

CH2−CO2H

Metabolism of phenylalanine.

CO2H

FIGURE 7.26

CH2−CO−CO2H

+

CO2H NH2

+

+

CO2 + NH3

Stickland reaction between l-proline and l-alanine.

S-β-lysine (lysine 2,3-aminomutase), S-glutamate to (2S,3S)-3-methylaspartate (glutamate mutase), and 2-methyleneglutarate—produced during the fermentation of nicotinate by Clostridium barkeri—to (R)-3-methylitaconate (2-methyleneglutarate mutase). b. The transformation of aromatic amino acids has been examined, and it has been shown (Elsden et al. 1976; D′Ari and Barker 1985) that in Cl. dificile these compounds are possible biogenic sources of 4-methyl phenol. In an organism designated “Cl. aerofoetidum” toluene may be produced from phenylalanine (Pons et al. 1984) and the postulated reactions are schematically shown in Figure 7.25. c. An unusual dismutation reaction involving pairs of amino acids has been studied extensively in Cl. sporogenes (Stickland 1934, 1935a,b). The reaction can be carried out by many other clostridia and has been summarized (Barker 1961). The products from proline and alanine (Stickland 1935a) illustrate the reaction and are shown in Figure 7.26, and the mechanism whereby glycine is reduced to acetate by glycine reductase from Cl. sticklandii has been elucidated (Arkowitz and Abeles 1989). The involvement of betaine in the reaction has already been noted.

ALKANOIC ACIDS Aerobic Conditions Oxalate and Glyoxylate Oxalate is synthesized from acetyl-CoA and oxalacetate in Burkholderia glumae (Li et al. 1999) and in the wood-rotting basidiomycete Fomitopsis palustris (Munir et al. 2001). Oxalate is also produced in a few degradations, although details of its metabolism are not fully resolved. Oxalate decarboxylase produces formate and CO2, and although its physiological signiicance in bacteria is not fully resolved, the enzyme in Bacillus subtilis requires manganese for activity (Tanner et al. 2001), and is induced not by oxalate, but by an acidic pH (Tanner and Bornemann 2000). Glyoxylate is produced during several aerobic degradations: a. 1,2-Dichloroethane by both the hydrolytic (Janssen et al. 1985) and oxidative (Hage and Hartmans 1999) pathways b. Allantoate that is a product of purine metabolism (Cusa et al. 1999) c. Morpholine by Mycobacterium aurum strain MO1 (Combourieu et al. 1998) d. Cyclic ethers by the fungus Cordyceps sinensis (Nakamiya et al. 2005). The pathway for bacterial degradation of glyoxylate involves condensation to tartronic semialdehyde by glyoxylate carboligase, reduction to glycerate, and elimination of 3-phosphoglycerate to produce pyruvate (Ornston and Ornston 1969) (Figure 7.27). In the brown-rot fungus Tyromyces

318

Environmental Degradation and Transformation of Organic Chemicals O HO 2 CCH(OH)CHO

CHO C

HO 2 CCH(OH)CH 2 OH

CH 3 COCO 2 H

OH O CH CO 2 H

FIGURE 7.27 Aerobic degradation of glyoxylate.

palustris, however, glyoxylate is dehydrogenated to oxalate by a cytochrome c–dependent enzyme (Tokimatsu et al. 1998). Anaerobic Conditions Oxalate, Malonate, and Glycolate Although these are rather unusual substrates, their degradation by anaerobic bacteria has been described. 1. Oxalobacter vibrioformis uses oxalate as sole source of energy using acetate as principal carbon source (Dehning and Schink 1989a). In O. formigenes, oxalate is metabolized to formate and CO2 by the coupled reaction of formyl-CoA transferase and a thiamin diphosphate–dependent oxalyl-CoA decarboxylase, which is activated by adenosine diphosphate (Berthold et al. 2005). Oxalate and formate form a one-to-one antiport system, which involves the consumption of an internal proton during decarboxylation, and serves as an indirect proton pump (Ruan et al. 1992) to generate ATP by decarboxylative phosphorylation (Anantharam et al. 1989). Cell-free extracts contain the enzymes of the biosynthetic glycerate pathway via glyoxylate and tartronic semialdehyde (Cornick and Allison 1996). Oxalyl-CoA decarboxylase has been characterized from several species of Biidobacterium including B. lactis, B. animalis, B. longum, and B. adolescens (Federici et al. 2004), and it was suggested that such strains could be important in the intestinal degradation of oxalate. 2. Malonomonas rubra is a microaerotolerant fermenting organism that decarboxylates malonate to acetate (Dehning and Schink 1989b). The organism contains high concentrations of c-type cytochromes that are not involved in the metabolism of the substrate, and are presumably remnants of the sulfur-reducing relatives of the organism (Kolb et al. 1998). Biotin-dependent carboxylases couple the decarboxylation to the transport of Na+ across the cytoplasmic membrane and use the electrochemical potential ∆µ Na+ to mediate the synthesis of ATP (Dimroth and Hilbi 1997). 3. Glycolate or fumarate is fermented by an organism belonging to the family Lachnospiraceae to acetate, succinate, and CO2 without the formation of hydrogen (Janssen and Hugenholtz 2003). Higher Carboxylic Acids The aerobic degradation of these has been covered in the discussion on alkanes and need not be repeated here. Anaerobic Conditions The anaerobic degradation of aliphatic carboxylic acids is of great ecological importance, since compounds such as acetate, propionate, or butyrate may be the terminal fermentation products of organisms degrading more complex compounds including carbohydrates, proteins, and lipids, while long-chain acids are produced by the hydrolysis of lipids (Zeikus 1980; Mackie et al. 1991). Degradation of aliphatic carboxylic acids by sulfate-reducing bacteria was traditionally restricted to

Aliphatic Compounds

319

lactate and its near relative, pyruvate, but recent developments have radically altered the situation and increased the spectrum of compounds which can be oxidized to CO2 at the expense of sulfate reduction. In the following paragraphs, an attempt will be made to present a brief summary of the anaerobic degradation of the main groups of aliphatic compounds. Studies on the anaerobic degradation of alkanoic acids have been carried out using both pure cultures and syntrophic associations. Acetate For the degradation of acetate, two different reactions may take place: oxidation to CO2 or dismutation to methane and CO2. To some extent, as it will emerge, segments of both pathways are at least formally similar, although the mechanisms for anaerobic degradation of these apparently simple compounds are quite subtle. Degradation of acetate and butyrate can be accomplished by Desulfotomaculum acetoxidans (Widdel and Pfennig 1981) and of acetate by Desulfuromonas acetoxidans (Pfennig and Biebl 1976) and species of Desulfobacter (Widdel 1987), while propionate is degraded by species of Desulfobulbus (Widdel and Pfennig 1982; Samain et al. 1984). A sulfur-reducing organism with a much wider degradative capability than Desulfuromonas acetoxidans has been isolated (Finster and Bak 1993), and this organism is capable of accomplishing the complete oxidation of, for example, propionate, valerate, and succinate. The oxidation of acetate under anaerobic conditions can take place by different pathways, both of which have been investigated in detail and their enzymology delineated (Thauer et al. 1989). 1. Oxidation may take place by a modiied tricarboxylic acid cycle in which the production of CO2 is coupled to the synthesis of NADPH and reduced ferredoxin, and the dehydrogenation of succinate to fumarate is coupled to the synthesis of reduced menaquinone. This pathway is used, for example, by Desulfuromonas acetoxidans and in modiied form by Desulfobacter postgatei. 2. In contrast, dissimilation of acetate may take place by reversal of the pathway used by organisms such as Clostridium thermoaceticum for the synthesis of acetate from CO2. In the degradation of acetate, the pathway involves a dismutation in which the methyl group is successively oxidized via methyl THF to CO2 while the carbonyl group is oxidized via bound carbon monoxide. Such THF-mediated reactions are of great importance in the anaerobic degradation of purines, which is discussed in Chapter 10, Part 1. Acetate may also be converted into methane by a few methanogens belonging to the genus Methanosarcina. The methyl group is initially converted into methyltetrahydromethanopterin (corresponding to methyltetrahydrofolate in the acetate oxidations discussed above) before reduction to methane via methyl-coenzyme M; the carbonyl group of acetate is oxidized via bound CO to CO2. Propionate, Succinate, and Long-Chain Carboxylic Acids Degradation of propionate is an intermediate step in the decomposition of organic matter in anaerobic environments, and growth at the thermodynamic limit is facilitated by syntrophy with methanogenic bacteria. For example, the syntrophic population of anaerobic organisms that carried out the oxidation of propionate in a rice ield was examined and showed the presence of the genera Syntrophobacter, Smithella, and Pelotomaculum. Among the archaea, species of Methanobacterium, Methanosarcina, and members of the Rice Cluster I were found (Lueders et al. 2004). A number of important aspects are noted: 1. Both the synthesis of propionate and its metabolism may take place under anaerobic conditions. In Desulfobulbus propionicum, degradation could plausibly take place by reversal of the steps used for its synthesis from acetate (Stams et al. 1984)—carboxylation of propionate to methylmalonate followed by coenzyme B12–mediated rearrangement to succinate, which then enters the tricarboxylic acid cycle. The converse decarboxylation of succinate to propionate has been observed in Propionigenium modestum (Schink and Pfennig 1982),

320

Environmental Degradation and Transformation of Organic Chemicals 2CH3CH2CO2H

CH3CH2COCHCO2H

CH3CH2COCH2CH2CO2H

CH3CH2 CH CH

CH 2 CO 2 H

CH 3 CH3CH2CH2CH(OH)CH2CO2H

CH3CH2CH2COCH2CO2H

CH3CH2CH2CO2H + CH3CO2H

FIGURE 7.28 Anaerobic degradation of propionate by Smithella propionica.

Sporomusa malonica (Dehning et al. 1989), Selenomonas acidaminovorans (Guangsheng et al. 1992), and Propionigenium maris (Janssen and Liesack 1995). 2. Growth of syntrophic propionate-oxidizing bacteria in the absence of methanogens has been accomplished using fumarate as the sole substrate (Plugge et al. 1993). Fumarate plays a central role in the metabolism, since it is produced from propionate via methylmalonate and succinate, while fumarate itself is metabolized by the acetyl-CoA cleavage pathway via malate, oxalacetate, and pyruvate. 3. The pathways and mechanism of interspecies transfer have been examined in syntrophic propionate-oxidizing organisms. a. Two pathways for propionate degradation have been proposed. In Pelotomaculum thermopropionicum the methylmalonyl-CoA pathway is used, and stringent regulation of fumarase is exerted (Kosaka et al. 2006). In Smithella propionica, which produces acetate and butyrate, however, the pathway is initiated by condensation of two molecules of propionate. This is followed by rearrangement—putatively by a coenzyme B12–dependent mutase—to 3-ketohexanoate, and ission to butyrate and acetate (Figure 7.28) (de Bok et al. 2001). b. Although it has been generally assumed that interspecies transfer in propionateoxidizing syntrophs involved H2, there is increasing evidence that formate transfer is actually involved. Components of the syntrophic culture of Syntrophobacter fumaroxidans and Methanospirillum hungatei that degrade propionate were separated by Percoll gradient centrifugation. Levels of formate dehydrogenase, hydrogenase, and formatehydrogen lyase in the components were examined, and it was showed that interspecies electron transfer was carried out primarily via formate (de Bok et al. 2002). The degradation of long-chain carboxylic acids is important in the anaerobic metabolism of lipids and an extensive compilation of the organisms that can accomplish this has been given (Mackie et al. 1991). This capability has been demonstrated in syntrophic bacteria in the presence of hydrogen-utilizing bacteria; for example, β-oxidation of C4 to C8, C5, and C7 carboxylic acids was carried out by the Syntrophomonas wolfei association (McInerney et al. 1981), and of C4 to C10, and C5 to C11 by the Clostridium bryantii syntroph (Stieb and Schink 1985). Acetate and propionate were the respective terminal products from the even- and odd-numbered acids. Single cultures of many sulfate-reducing bacteria are also able to carry out analogous reactions (Mackie et al. 1991). For example, Desulfobacterium cetonicum degrades butyrate to acetate by a typical β-oxidation pathway (Janssen and Schink 1995b). Long-Chain Dicarboxylic Acids Long-chain dicarboxylic acids are produced by a number of reactions: a. The C12 dicarboxylate by α,ω-oxidation of dodecane (Broadway et al. 1993) b. The C7 dicarboxylate (pimelate) as an intermediate in the anaerobic degradation of benzoate (Harwood et al. 1999) c. As intermediates in the degradation of cycloalkanones (Kostichka et al. 2001) d. Atmospheric oxidation of unsaturated fatty acids (Stephanou and Stratigakis 1993). The degradation of pimelate is initiated by formation of the coenzyme A ester and is followed by a series of steps with the production of glutaryl-CoA that is decarboxylated to crotonyl-CoA

321

Aliphatic Compounds

(Härtel et al. 1993; Gallus and Schink 1994; Harrison and Harwood 2005). This produces two molecules of acetate or, in strictly fermenting organisms butyrate and isobutyrate (Matties and Schink 1992). The genetics of the degradation has been explored (Parke et al. 2001) in Acinetobacter sp. strain ADP1 that is able to degrade dicarboxylic acids up to C14, and the enzymes for the degradation of pimelate in Rhodopseudomonas palustris are contained in an operon in which the PimA ligase that catalyzes the irst step is able to accept an unusually wide range of dicarboxylic acids as substrates (Harrison and Harwood 2005). In summary, the anaerobic degradation of alkanoic acids may truly be described as ubiquitous and is carried out by organisms with widely different taxonomic afinity both in pure culture and in syntrophic associations.

AMIDES AND RELATED COMPOUNDS Amides Aromatic amides, carbamates, and ureas are components of a number of important agrochemicals, and the irst step in their biodegradation is mediated by the activities of amidases, ureases, and carbamylases with the production of amines (Figures 7.29a through c). The chloroanilines that are formed from many of them as initial products may, however, be substantially more resistant to further degradation. Application of assays for amidase activity, particularly for pyrazinamidase, has been widely used in the classiication of mycobacteria (Wayne et al. 1991). Sequential hydrolysis of nitriles to amides and carboxylic acids is well established both in aliphatic (Miller and Gray 1982; Nawaz et al. 1992) and aromatic compounds (Harper 1977; McBride et al. 1986). Degradation of the herbicide bromoxynil may, however, take place by the elimination of cyanide from the ring with the initial formation of 2,6-dibromohydroquinone (Topp et al. 1992) (Figure 7.30). There may be a high

O C2H5O (a)

P

C2H5O

NO 2

O

C2H5O

O

P

NO 2

C2H5O O (C2H5O)P−OH +

HO

NO 2

NH 2

NH−CO−CH 2−CH3

+

(b) Cl

Cl

Cl

Cl

Cl

NH−CO−N

CH 3

NH 2

O−CH 3

(c) Cl

CH 3−CH2−CO2H

+

CH 3−NH−OCH3

Cl Cl

FIGURE 7.29 Hydrolysis of (a) acetanilides, (b) phenylureas, and (c) carbamates.

322

Environmental Degradation and Transformation of Organic Chemicals CN

Br

OH

Br OH

FIGURE 7.30

Br

Br OH

Metabolism of bromoxynil.

degree of speciicity in the action of these nitrilases and this may have considerable signiicance in biotechnology. Some examples are given as illustrations: 1. Racemic 2-(4′-isobutylphenyl)propionitrile is converted by a strain of Acinetobacter sp. into S-(+)-2-(4′-isobutylphenyl)propionic acid with an optical purity > 95% (Yamamoto et al. 1990). 2. The nitrilase from a number of strains of Pseudomonas sp. mediated an enantiomerically selective hydrolysis of racemic O-acetylmandelonitrile to d-acetylmandelic acid R-(−)acetylmandelic acid (Layh et al. 1992). 3. The amidase from Rhodococcus erythopolis strain MP50 was used to selectively convert racemic 2-phenylpropionamide into S-2-phenylpropiohydroxamate. This was converted into the isocyanate by Lossen rearrangement and then by hydrolysis to S-(−)-phenylethylamine (Hirrlinger and Stolz 1997). 4. An amidase from Ochrobactrum anthropi strain NCIMB 40321 has a wide substrate versatility for l-amides, primarily those with an α-amino group (Sonke et al. 2005), while the condensation product of urea and formaldehyde H2N–[CONH–CH2NH]n –CONH2 is hydrolyzed by another strain of O. anthropi (Jahns et al. 1997).

NITRILES There are two pathways for the degradation of nitriles: (a) direct formation of carboxylic acids by the activity of a nitrilase, for example, in Bacillus sp. strain OxB-1 and P. syringae B728a (b) hydration to amides followed by hydrolysis, for example, in P. chlororaphis (Oinuma et al. 2003). The monomer acrylonitrile occurs in wastewater from the production of polyacrylonitrile (PAN), and is hydrolyzed by bacteria to acrylate by the combined activity of a nitrilase (hydratase) and an amidase. Acrylate is then degraded by hydration to either lactate or β-hydroxypropionate. The nitrilase or amidase is also capable of hydrolyzing the nitrile group in a number of other nitriles (Robertson et al. 2004) including PAN (Tauber et al. 2000).

ISONITRILES Isonitriles are widespread metabolites in marine organisms, although little attention has been paid to their degradation. Pseudomonas putida strain N-19-2 can hydrolyze isonitriles to N-substituted formamides (Goda et al. 2001), and the enzyme is active toward cyclohexyl isonitrile and benzyl isonitrile.

SULFONYLUREAS AND THIOCARBAMATES 1. Sulfonylureas are the basis of a large group of herbicides. Cytochrome P450 enzymes in Streptomyces griseolus transform the sulfonylureas by hydroxylation (Omer et al. 1990) leaving the –SO2NHCONH– part of the structure unaltered (Harder et al. 1991). 2. Substantial effort has been given to the degradation of thiocarbamates and the expression of the thcB gene encoding cytochrome P450 in strains of Rhodococcus is expressed constitutively (Shao and Behki 1996). The degradation of S-ethyl N,N′-dipropylthiocarbamate

323

Aliphatic Compounds CH 3 CH 2 CH 2

CH 3 CH 2 CH 2 N−CO−S−CH 2CH 3

CH 3 CH 2 CH 2

N−CO−S−CH 2CH 3 CH 3 CH 2 CH OH

CH 3 CH 2 CHO + CH 3CH 2CH 2−NH−CO−S−CH 2CH 3 CH 3 CH 2 CH 2 NH 2 + HO 2C−S−CH 2CH 3

FIGURE 7.31

HO 2C−S−CH 3

CO 2 + CH 3 SH

Aerobic degradation of S-ethyl N,N′-dipropylthiocarbamate.

(EPTC) has been examined in a number of rhodococci and in one of them (strainTE1 given as a species of Arthrobacter sp.) degradation is associated with a 50.5 mDa plasmid (Tam et al. 1987). The principal pathway in Rhodococcus sp. strain JE1 involves hydroxylation of the propyl group followed by loss of propionaldehyde and degradation of N-depropyl EPTC to S-ethylformate and propylamine (Figure 7.31) (Dick et al. 1990). Two of the genes induced by EPTC encode a cytochrome P450 system that carries out the initial hydroxylation with formation of the N-depropylated product and an aldehyde dehydrogenase that converts the aldehyde produced into the corresponding carboxylic acid (Nagy et al. 1995). In addition to these mechanisms, the degradation of thiocarbamates may be carried out in Rhodococcus erythropolis NI86/21 by a herbicide-inducible nonheme haloperoxidase (de Schrijver et al. 1997). Although it is moot whether carbon monoxide, cyanide, and thiocyanate should be included as organic compounds, brief comments on their biodegradation are summarized.

CARBON MONOXIDE Carbon monoxide is produced biotically from hemin and amino acids and in soil, and during fossil fuel incomplete combustion. Although normally toxic to aerobic organisms, microorganisms have been isolated that are able to degrade it, and in a bound form it is an important intermediate in anaerobic reactions. Some aerobic bacteria are able to use carbon monoxide as a source of energy and cell carbon (Meyer and Schlegel 1993), and mycobacteria are able to utilize both carbon monoxide and methanol (Park et al. 2003). CO2 is formed by a carbon monoxide dehydrogenase and is incorporated into biosynthetic reactions by the ribulosebisphosphate pathway (Park et al. 2003). Carbon monoxide is also an important metabolite in reactions carried out by anaerobic bacteria including the degradation of acetate by a pathway that involves a dismutation in which the methyl group is successively oxidized via methyltetrahydrofolate to CO2, while the carbonyl group is oxidized via bound carbon monoxide. Acetate may also be converted into methane by a few methanogens belonging to the genus Methanosarcina. The methyl group is initially converted into methyltetrahydromethanopterin (corresponding to methyltetrahydrofolate in the acetate oxidations) before reduction to methane via methyl coenzyme M; the carbonyl group of acetate is oxidized via bound CO to CO2.

CYANIDE Cyanide is a component of plant cyanogenic glycosides such as amygdalin and linamarin, while a range of structurally diverse diterpenoid isonitriles is produced by marina biota. Cyanide is a toxic waste from the mining and electroplating industries and, although normally toxic to aerobic organisms, microorganisms have been isolated that are able to degrade it. Two mechanisms have emerged for the degradation of cyanide (Fernandez et al. 2004) and the corresponding nitriles: a. Hydrolysis by nitrilase to the carboxylic acid and ammonia b. Hydratases that catalyze the formation of the amides

324

Environmental Degradation and Transformation of Organic Chemicals

The mechanism of the irst reaction in Pseudomonas luorescens NCIMB 11764 is complex, and involves both monooxygenation and hydrolysis. Oxygenation is carried out by reduced pterins and is analogous to the hydroxylation of phenylalanine to tyrosine. The overall reaction involves monooxygenation to cyanate followed by reduction to formamide and hydrolysis to formate and NH4+. An alternative degradation for cyanate has, however, been shown in Escherichia coli when an inducible cyanase brings about a recycling reaction between bicarbonate and cyanate to form formamide that is hydrolyzed to CO2 and NH4+ (Johnson and Anderson 1987). A strain of Pseudomonas pseudoalcaligenes isolated by enrichment with cyanide as sole source of nitrogen was able to utilize, in addition, ferrocyanide, nitroferricyanide, and cuprocyanide, and may involve cyanate (Luque-Almagro et al. 2005). Noncyanogenic fungi can degrade cyanide to formamide followed by hydrolysis by a hydratase to formate and ammonia (Dumestre et al. 1997). This pathway is also used by some bacteria (Jandyala et al. 2003). Bacteria also use a number of reactions for the detoxiication of cyanide, including monooxygenation to CO2 and ammonia (Wang et al. 1996).

THIOCYANATE Although the degradation of thiocyanate is accomplished by a few bacteria, the chemolithoautrophic Thiobacillus thioparus strain THI 115 is unusual in being able to use this as an energy source. The hydrolase that converts the substrate into NH4+ and COS has been puriied, and consists of three subunits (Katayama et al. 1998). The hydrolase showed a high homology to nitrile hydrolase, which suggests a close similarity in the pathways for their degradation—hydrolysis to the amines followed by deamination.

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Swaving J, JAM de Bont, A Westphal, A de Kok (1996) A novel type of pyridine nucleotide-disulide oxidoreductase is essential for NAD+- and NADPH-dependent degradation of epoxyalkanes by Xanthobacter strain Py2. J Bacteriol 178: 6644–6646. Tabor CW, H Tabor (1985) Polyamines in microorganisms. Microbiol Revs 49: 81–99. Tam AC, RM Behki, SU Khan (1987) Isolation and characterization of an S-ethyl-N,N-dipropylthiocarbamatedegrading Arthrobacter strain and evidence for plasmid-associated S-ethyl-N,N-dipropylthiocarbamate degradation. Appl Environ Microbiol 53: 1088–1093. Tanaka A, M Ueda (1993) Assimilation of alkanes by yeasts: functions and biogenesis of peroxisomes. Mycol Res 98: 1025–1044. Tanner A, L Bowater, SA Fairhurst, S Bornemann (2001) Oxalate decarboxylase requires manganese and dioxygen for activity. J Biol Chem 276: 43627–43634. Tanner A, S Bornemann (2000) Bacillius subtilis YvrK is an acid-induced oxalate decarboxylase. J Bacteriol 182: 5271–5273. Tauber MM, A Cavaco-Paulo, K-H Robra, GM Gübitz (2000) Nitrile hydratase and amidase from Rhodococcus rhodochrous hydrolyze acrylic ibers and granular polyacrylonitrile. Appl Environ Microbiol 66: 1634–1638. Teske A, K-U Hinrichs, V Edgcomb, A de Vera Gomez, D Kysela, SP Sylva, ML Sogin, HW Jannasch (2002) Microbial diversity of hydrothermal sediments in the Guaymas Basin: evidence for anaerobic methanotrophic communities. Appl Environ Microbiol 68: 1994–2007. Textor S, VF Wendich, AA De Graaf, U Müller, MI Linder, D Linder, W Buckel (1997) propionate oxidation in Escherichia coli: evidence for operation of a methylcitrate cycle in bacteria. Arch Microbiol 168: 428–436. Thauer RK, D Möller-Zinjhan, AM Spormann (1989) Biochemistry of acetate catabolism in anaerobic chemotrophic bacteria. Annu Rev Microbiol 43: 43–67. Tokimatsu T, Y Nagai, T Hattori, M Shimada (1998) Puriication and characteristics of a novel cytochrome c dependent glyoxylate dehydrogenase from a wood-rotting fungus Tyromyces palustris. FEBS Lett 437: 117–121. Toms AV, C Kinsland, DE McCloskey, AE Pegg, SE Ealick (2004) Evolutionary links as revealed by the structure of Thermotoga maritima S-adenosylmethionine decarboxylase. J Biol Chem 279: 33837–33846. Topp E, L Xun, CS Orser (1992) Biodegradation of the herbicide bromoxynil (3,5-dibromo-4-hydroxybenzonitrile) by puriied pentachlorophenol hydroxylase and whole cells of Flavobacterium sp. strain ATCC 39723 is accompanied by cyanogenesis. Appl Environ Microbiol 58: 502–506. Uetz T, R Schneider, M Snozzi, T Egli (1992) Puriication and characterization of a two-component monooxygenase that hydroxylates nitrilotriacetate from “Chelatobacter” strain ATCC 29600. J Bacteriol 174: 1179–1188. Urakami T, H Araki, H Oyanagi, K-I Suzuki, K Komagata (1990) Paracoccus aminophilus sp. nov. and Paracoccus aminovorans sp. nov., which utilize N,N′-dimethylformamide. Int J Syst Bacteriol 40: 287–291. Urakami T, H Araki, H Oyanagi, K-I Suzuki, K Komagata (1992) Transfer of Pseudomonas aminovorans (den Dooren de Jong 1926) to Aminobacter gen. nov. as Aminobacter aminovorans comb. nov. and description of Aminobacter aganoensis sp. nov. and Aminobacter niigataensis sp. nov. Int J Syst Bacteriol 42: 84–92. van Beilin J, EG Funhoff, A van Loon, A Just, L Kaysser, M Bouza, R Holtackers, M Röthlisberger, Z Li, B Witholt (2006) Cytochrome P450 alkane hydroxylases of the CYP153 family are common in alkane-degrading eubacteria lacking integral membrane alkane hydroxylases. Appl Environ Microbiol 72: 59–65. Van den Tweel WJJ, JAM de Bont (1985) Metabolism of 3-butyl-1-ol by Pseudomonas BB1. J Gen Microbiol 131: 3155–3162. Van den Wijngaard AJ, DB Janssen, B Withold (1989) Degradation of epichlorohydrin and halohydrins by bacterial cultures isolated from freshwater sediment. J Gen Microbiol 135: 2199–2208. Van der Werf MJ, HJ Swarts, JAM de Bont (1999) Rhodococcus erythopolis DCL14 contains a novel degradation pathway for limonene. Appl Environ Microbiol 65: 2092–2102. Van der Werf MJ, KM Overkamp, JAM de Bont (1998) Limonene-1,2-epoxide hydrolase from Rhodococcus erythropolis DCL14 belongs to a novel class of epoxide hydrolases. J Bacteriol 180: 5052–5057. Van Ginkel CG, JAM de Bont (1986) Isolation and characterization of alkene-utilizing Xanthobacter spp. Arch Microbiol 145: 403–407.

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PART 2 CYCLOALKANES The aerobic degradation of cycloalkanes has been examined in both monocyclic and polycyclic substrates. In all of them, monooxygenation is the irst step and this is sometimes accomplished by cytochrome P450 systems. Reviews of the degradation of alicyclic compounds including monoterpenes

337

Aliphatic Compounds OH

O

O O HO2C

FIGURE 7.32

[CH2]4

CO2H

Biodegradation of cyclohexane.

have been given by one of the pioneers (Trudgill 1978, 1984, 1994) and these should be consulted for further details. Only a bare outline with some newer developments will therefore be given here. Hydroxylation by cycloalkane monooxygenase and dehydrogenation to the cycloalkanone are the irst steps in the oxidation of cycloalkanes, and are formally similar to those used for the degradation of linear alkanes. It was some time, however, before pure strains of microorganisms were isolated that could grow with cycloalkanes or their simple derivatives. The degradation of cyclohexane has been examined in detail (Stirling et al. 1977; Trower et al. 1985). There are ive steps in its degradation: (1) hydroxylation of the ring by monooxygenation, (2) dehydrogenation to the ketone, (3) insertion of one atom of oxygen into the ring in a reaction formally analogous to the Baeyer– Villiger persulfate oxidation, (4) hydrolysis of the lactone, and (5) dehydrogenation to an α,ωdicarboxylate. The pathway is illustrated for cyclohexane in Figure 7.32 (Stirling et al. 1977), and a comparable one operates also for cyclopentanol (Grifin and Trudgill 1972). The enantiomeric speciicity of this oxygen-insertion reaction has been examined in a strain of camphor-degrading Pseudomonas putida (Jones et al. 1993). Both cyclohexanone monooxygenase (Branchaud and Walsh 1985) and cyclopentanone monooxygenase exhibit a substrate versatility (Iwaki et al. 2002) that is reminiscent of that of MMO, and has attracted interest in them as biocatalysts. There has been interest in Baeyer–Villiger monooxygenation of higher cycloalkanones and important issues have emerged: a. Cyclododecanone monooxygenase from Rhodococcus ruber SC1 is different from those already mentioned, and is active towards substrates with more than seven carbon atoms (Kostichka et al. 2001). b. The enzyme derived from Pseudomonas sp. strain HI-70 is able to oxidize a wide range of substrates including C12–C15 ketones, C5 and C6 ketones with methyl substituents, and some bicyclic ketones including decalones (Iwaki et al. 2006). Attention has also been directed to the degradation of cycloalkane carboxylic acids: 1. Cyclopropane carboxylic acid is degraded via 3-hydroxybutyrate by both the bacterium Rhodococcus rhodochrous (Toraya et al. 2004) (Figure 7.33) and by fungi (Schiller and Chung 1970), although the mechanism for ring ission has not been determined. 2. The degradation of 11,12-methyleneoctadecanoate is carried out in Tetrahymena pyriformis by a modiied β-oxidation pathway with the formation of propionate and acetate (Figure 7.34a) (Tipton and Al-Shather 1974). 3. Cyclohexylacetate is degraded to cyclohexanone by elimination of the side chain after hydroxylation at the ring junction (Figure 7.34b) (Ougham and Trudgill 1982). An alternative to monooxygenation is realized in the hydration of the substituted cyclohexanone derived from the ission product of 1,2-dihydroxynaphthalene during the degradation of 1,2,3,4tetrahydronaphthalene (tetralin) (Hernáez et al. 2002) (Figure 7.35). A less common pathway for the degradation of cyclohexanecarboxylate has been found in which the ring is dehydrogenated to 4-hydroxybenzoate before ission (Figure 7.36) (Blakley 1974; Taylor and Trudgill 1978). The degradation of polyhydroxylated cyclohexanes such as quinate and shikimate also involves aromatic intermediates (Ingledew et al. 1971), though in these examples a

338

Environmental Degradation and Transformation of Organic Chemicals OH

O CO2H

CO2H CO2H

CO2H

FIGURE 7.33 (a)

Aerobic degradation of cyclopropanecarboxylate. CH 2

CH 3−(CH2)5−CH

(b)

CH 2−CO2H

CH−(CH 2)9−CO2H

CH 2 CH 3−(CH2)5−CH

CH−CH 2−CO2H CH−CO 2H

CH 2 CH 3−(CH2)5−CH

C CH−CO 2H HO

CH 2 CH 3−(CH2)5−CH

CH 2−CO2H

CH 2−CO2H C OH

O

+

CH 3−CO2H

CH 3−(CH2)5−CH2−CH2−CO−CH2−CO2H

FIGURE 7.34

Degradation of (a) 11,12-methyleneoctadecanoate and (b) cyclohexylacetate.

OH

OH OH

OH

O HO2C OH CO2H

CO2H

HO2C OH

FIGURE 7.35

O

Aerobic degradation of tetralin.

H O2C

CHO + CH3CO−CO2H

CO2H OH

339

Aliphatic Compounds CO2H

CO2H

CO2H

CO2H

OH OH

O

FIGURE 7.36

Alternative pathway for the biodegradation of a cyclohexane carboxylate. CO 2 H

CO 2 H

HO

HO

OH OH

FIGURE 7.37

OH

HO

CO 2 H

OH OH

CO 2 H

OH

O OH

HO OH

Biodegradation of quinate.

mechanism for the formation of the aromatic ring by elimination reactions is more readily rationalized (Figure 7.37). The interrelation between the metabolism cyclohexane carboxylates and their benzenoid analogs may be seen in the pathways for the anaerobic degradation of cyclohexane carboxylate by Rhodopseudomonas palustris. This takes place by the action of a ligase (AliA) to form the coenzyme ester, followed by a dehydrogenase (BadJ) to produce cyclohex-1-ene-1-carboxy-CoA, which is then fed into the pathway used for the anaerobic degradation of benzoyl-CoA (Egland and Harwood 1999), which is discussed in Chapter 8, Parts 1 and 3. An unusual reaction was been observed in the reaction of “old yellow enzyme” with α,β-unsaturated ketones. A dismutation took place under aerobic or anaerobic conditions, with the formation from cyclohex-1-keto-2-ene of the corresponding phenol and cyclohexanone, and an analogous reaction from representative cyclodec-3-keto-4-enes—putatively by hydride-ion transfer (Vaz et al. 1995). Reduction of the double bond in α,β-unsaturated ketones has been observed, and the enone reductases from Saccharomyces cerevisiae have been puriied and characterized. They are able to carry out reduction of the C=C bonds in aliphatic aldehydes and ketones, and ring double bonds in cyclohexenones (Wanner and Tressel 1998). Reductions of steroid 1,4-diene-3-ones can be mediated by the related old yellow enzyme and pentaerythritol tetranitrate reductase, for example, androsta-∆1,4-3,17-dione to androsta-∆4-3,17-dione (Vaz et al. 1995) and prednisone to pregna-∆4-17α, 20-diol-3,11,20-trione (Barna et al. 2001) respectively. Numerous single-step transformations—generally hydroxylations, oxidations of alcohols to ketones or dehydrogenations—of both terpenes and sterols have been accomplished using microorganisms especially fungi. This interest has been motivated by the great interest of the pharmaceutical industry in the products (Smith et al. 1988), and in fungal metabolism as a model for that of higher organisms (Smith and Rosazza 1983). Reactions catalyzed by cytochrome P450 mediated in both prokaryotes and eukaryotes have been discussed in Chapter 3, Part 1. Anaerobic degradation of cycloalkanes has seldom been reported. The pathway used for the degradation of ethylcyclopentane by a sulfate-reducing enrichment is analogous to the fumarate pathway used for n-alkanes (Part 1 of this chapter) with the formation of 3-ethylcyclopentanecarboxylate followed by ring ission to 3-ethylpentan-1,5-dioate (Rios-Harnandez et al. 2003).

MONOTERPENES Hydroxylation and Baeyer–Villiger reactions carried out by monooxygenation are important in the degradation of a range of terpenoids and steroids. The aerobic degradation of limonene can take place by a number of reactions several of which involve hydroxylation at allylic positions

340

Environmental Degradation and Transformation of Organic Chemicals

O

O

HO2C

O

O

O

O

O HO2C OH

O

O

O

CO2H HO2C

FIGURE 7.38

Degradation of camphor by Pseudomonas putida.

O

O

O

O

CO2H

FIGURE 7.39

OH

O

O

O

COCH3

CO2H

HO2C

CO2H

Degradation of camphor by Mycobacterium rhodochrous.

(terpene numbering): C-7 to perillyl alcohol, C-6 to carveol, C-4 to α-terpineol, and C-3 to isopiperitenol (references in van der Werf et al. 1999). Oxidations analogous to Baeyer–Villiger reactions are employed in the degradation of alicyclic compounds containing several rings. The degradation of the monoterpenoid camphor has attracted particular attention since the initial hydroxylation in a plasmid-bearing pseudomonad is carried out by a cytochrome P450 enzyme (designated P450cam) (Schlichting et al. 2000). This enzyme displays a wide versatility, which is noted later in the degradation of luorinated alkanes, of abietic acid, in the hydroxylation of 1,4-luorobenzene, and in the fungal metabolism of styrene. In Pseudomonas putida ATCC 17453 carrying the CAM plasmid degradation involves an initial cytochrome P450 hydroxylation at C-5 followed by oxidation, and the introduction of an oxygen atom adjacent to the quaternary methyl group (Figure 7.38) (Ougham et al. 1983). In an organism designated Rhodococcus rhodochrous strain NCIMB 9784, hydroxylation occurs, however, at C-6, followed by ring ission of the 1,3-diketone (Figure 7.39) (Chapman et al. 1966). The hydrolase that carries out ission of the cyclic 1,3-diketone has been characterized, and was comparable to those carried out by the enoyl-CoA hydratase superfamily (Grogan et al. 2001; Whittingham et al. 2003). The enzyme from Rhodococcus erythropolis strain DCL14 is able to catalyze insertions of oxygen into the cyclohexanones produced by epoxidation, hydrolysis, and oxidation from both (+)-(4R)- and (−)-(4S)-limonene (van der Werf et al. 1999). In addition, the

341

Aliphatic Compounds

O

FIGURE 7.40

CHO

Degradation of α-pinene.

monooxygenase from this strain is able to insert an oxygen atom into 2-ketomonoterpenoids at both the 1,2 and 2,3 positions, and into a 3-ketomonoterpenoid at the 3,4 position (terpenoid numbering) (van der Werf 2000). The biodegradation of cyclic monoterpenes has been investigated under both aerobic and denitrifying conditions (Foss and Harder 1998), and may involve key reactions other than the Baeyer–Villiger-type ring cleavage of ketones (Trudgill 1994). For example, although some strains of Pseudomonas sp. degrade α-pinene by rearrangement to limonene, oxidation, and β-oxidation, in others the initial reaction was formation of the epoxide that produced a carbonium ion at C-1 followed by sequential ring ission of the cyclobutane and cyclohexane rings to produce 2-methyl5-isopropylhexa-2,5-dienal (Best et al. 1987; Grifiths et al. 1987a,b) (Figure 7.40). Bacterial hydroxylation by cytochrome P450 systems is well established in actinomyces (O′Keefe and Harder 1991). Stereospeciic hydroxylation of α-ionone—though not β-ionone—has been observed with strains of Streptomyces sp. (Lutz-Wahl et al. 1998), and the racemic substrate is hydroxylated to the (3R,6R)and (3R,6S)-hydroxy-α-ionones.

STEROIDS Hydroxylation Microorganisms, particularly fungi, are able to hydroxylate sterols at the 11α-, 12β-, 15-, 17, 19, and 21 positions (references in Hudlický 1990), although the product even from the same substrate may depend on the organism: a. Calonectria decora, Rhizopus nigricans, and Aspergillus ochraceus produce the 12β,15α-; 11α,16β-; and 6β,11α-diols from 3-keto-5α-androstane (Bird et al. 1980). b. The biotransformation of pregna-4,17(20)-cis-diene-3,16-dione by Aspergillus niger produced metabolites with hydroxyl groups at the 7β, or 7β and 15β positions, whereas Cephalosporium aphidicola produces metabolites with hydroxyl groups at the 11α, or 11α and 15β positions (Atta-ur-Rahman et al. 1998). An interesting development has been the need for unusual products that may be sterol metabolites. Studies have been directed to the biosynthesis, for example, of the otherwise rare and inaccessible derivatives of progesterone hydroxylated at the 6, 9, 14, or 15 positions that could be accomplished by incubating progesterone in a complex medium with the fungus Apiocrea chrysosperma (Smith et al. 1988). The hydroxylation of progesterone and closely related compounds at the 15β position has been observed in cell extracts of Bacillus megaterium (Berg et al. 1976). Other Aerobic Transformations and Degradation Attention has been directed to the reactions catalyzed by cytochrome P450s that bring about important reactions leading to the loss of angular methyl groups at C-10 (with concomitant aromatization of ring A) and C-14, and the C-17 –COCH3 side chain. These reactions are discussed further in Chapter 3, Part 1. The transformations of steroids and their precursor lanosterol have been extensively

342

Environmental Degradation and Transformation of Organic Chemicals CO2H HO (a) O

HO

O

(b) HO

O

HO (c)

A O

A

A O

HO

A

A

A

A

O

HO

O

HO OH

C B

C

C B

OH

B

C B

FIGURE 7.41 Demethylation of angular methyl groups: (a) in steroids and related compounds, (b) in lanosterol derivative and (c) summary of reactions for the formation of CH2O.

examined as sources of estrone and related compounds. In all of them, the essential reactions involve loss of the angular methyl groups and cytochrome P450–mediated reactions have already been noted in Chapter 3, Part 1. In Nocardia sp., demethylation of steroids is accomplished by sequential formation of the 1,4-diene-3-ones, hydroxylation at C-10, and a dienone-phenol transformation (Figure 7.41a) (Sih et al. 1968). In a lanosterol derivative, Mycobacterium sp. carries out analogous reactions for the loss of the C-29, C-30, and C-28 methyl groups by hydroxylation (Figure 7.41b) (Wang et al. 1995). Plausible reactions for the formation of CH2O from the quaternary methyl groups are outlined in Figure 7.41c), although formate is produced in cytochrome P450–mediated reactions. The degradation of sterols and the related bile acids oxygenated at C-3 is also initiated by formation of the 1,4-diene-3-ones. In these, the critical reaction is, however, hydroxylation at C-9 that results in ission of the B-ring with formation of the 9,10-seco compound under the driving force of aromatization of the A-ring by a dienone-phenol reaction (Leppik 1989). The pathway is exempliied in the degradation of testosterone by a strain of Comamonas testosteroni (Horinouchi et al. 2003a, 2005) (Figure 7.42), and is presumptively used for the degradation of androsterone after initial dehydrogenation (Horinouchi et al. 2003b).

343

Aliphatic Compounds O

O

O

O O

O

H

O

O

O

O

O

O

OH

O

O

O

HO 2 C OH

OH

OH

FIGURE 7.42

HO

H

CO 2 H

O

Aerobic degradation of testosterone.

OH

O

O

OH

H

O H

O

HO

OH

O

H

FIGURE 7.43 Anaerobic biotransformation of 3α,7α-cholic acid.

Anaerobic Transformation This has been examined quite extensively in the context of the intestinal metabolism of bile acids and a number of reactions that are otherwise quite unusual have been observed, most frequently in organisms belonging to the genera Eubacterium or Clostridium. Illustrative examples include the following: a. Reduction of the ∆4,5 bond with production of 5β-reduced compounds (Mott et al. 1980). b. Reductive dehydroxylation of 7α-hydroxy bile acids (Masuda et al. 1984) that has been extensively studied, and both the genetics and the complex of pathways have been elucidated for cholic acid (Wells and Hylemon 2000). These reactions involve a complex sequence of reactions: (i) dehydrogenation to the 3-keto-4,5-ene, (ii) dehydration to the 3-keto-4,6-diene, and (iii) successive reduction to the 3-keto and the 3-hydroxy compounds, which are illustrated in Figure 7.43 (Wells and Hylemon 2000). In addition, dehydroxylation of 16α- and 21-hydroxy corticosteroids has been observed with fecal bacteria (Bokkenheuser et al. 1980).

344

Environmental Degradation and Transformation of Organic Chemicals

(a)

A

B

B

A

A

B O

OH CO 2 H

CO 2 H

OH

CO 2 H

HO O A

B

A

CO 2 H

B

O

O

CO 2 H

CO 2 H CO 2 H

CO 2 H

OH HO

(b)

A

A

B

B

O

A

B O

CO 2 H

A HO

FIGURE 7.44

CO 2 H

Pathways for aerobic degradation of dehydroabietic acid.

DITERPENOIDS The degradation of the diterpenoid derivative dehydroabietic acid has been examined in several different strains of bacteria. In Pseudomonas abietaniphila strain BKME-9, it is degraded by initial cytochrome P450 hydroxylation at C-7 (Smith et al. 2004), oxidation to the 7-keto compound followed by dioxygenation to the 7-keto-11,12-diol that undergoes meta ission (Martin and Mohn 1999, 2000). Further degradation then takes place by dioxygenation of ring C and ring ission (Figure 7.44a) (Biellmann et al. 1973b) or by an alternative (Figure 7.44b) (Biellmann et al. 1973a).

POLYCYCLIC SUBSTRATES The following illustrate the variety of hydroxylations of structurally diverse polycyclic substrates: 1. P450cam is able to hydroxylate the –CH3 group of the quaternary methyl group of 5,5diluorocamphor (Figure 7.45a) to the 9-hydroxymethyl compound (Eble and Dawson 1984), and both adamantane and adamantan-4-one at the -CH quaternary carbon atom (Figure 7.45b) (White et al. 1984). 2. Patchoulol is transformed by Botrytis cinerea to a number of products principally to those involving hydroxylation at the C-5 and C-7 quaternary atoms (Aleu et al. 1999) (Figure 7.45c).

345

Aliphatic Compounds OH

O

O

(a) F

F

F

F OH

(b)

14

HO

1

13

4

5

12

(1 )

FIGURE 7.45

OH

HO

6

10 9

HO

3 7

8

(c)

15 2

11

OH (2 )

(3)

Hydroxylation of (a) 5,5-diluorocamphor, (b) adamantane, and (c) patchoulol.

HO

O

N CH 2

FIGURE 7.46

O

N CH 2

Hydroxylation of azabrendane derivative.

3. Cells of Acinetobacter sp. NCIB 9871 grown with cyclohexanol carried out enantiomerically speciic degradation of 5-bromo-7-luoronorbornanone and production of a lactone with >95% enantiomeric excess (Levitt et al. 1990). 4. Bauveria sulfurescens stereospeciically hydroxylated an azabrendane at the quaternary carbon atom (Figure 7.46) (Archelas et al. 1988). 5. Penicillium lilacinum transformed testosterone successively to androst-4-ene-3,17-dione and testololactone (Prairie and Talalay 1963): once again the oxygen atom is introduced into ring D at the quaternary position between C13 and C17. 6. An illustration of the plethora of reactions that may occur is afforded by the transformation of caryophyllene oxide by Botrytis cinerea. Although most of the reactions were hydroxylations or epoxidations, two involved transannular reactions: (a) between the C4-epoxide oxygen and C7 and (b) between the C4-epoxide and C13 with formation of a caryolane (Figure 7.47) (Duran et al. 1999). 7. The degradation of atropine has been examined in Pseudomonas sp. strain AT3 and produces tropine as the initial metabolite. The degradation of this proceeds by oxidative

346

Environmental Degradation and Transformation of Organic Chemicals

O O

OH +

HO

FIGURE 7.47

Transformation of caryophyllene oxide by Botrytis cinerea.

CH 3

H

N

N

O

O O

O

O

CO 2 H CH 3

OH

FIGURE 7.48

OH

OH

O

O

Degradation of tropine.

loss of the N-methyl group and elimination of ammonia to form 6-hydroxy-cyclohepta-1,4dione, followed by ission of the 1,3-diketone to produce 4,6-diketoheptanoate (Figure 7.48) (Bartholomew et al. 1996). Although the enzymology was unresolved, loss of ammonia presumably occurs either by successive hydroxylation at the tertiary carbon atoms adjacent to the –NH group or by successive dehydrogenations. Hydroxylation of other natural products such as a. A synthetic diterpenoid butenolide by Cunninghamella elegans at 5α, and both 7α and 7β positions as well as on the isopropyl side chain (Milanova et al. 1994). b. Sclareol by Cunninghamella elegans at the 2α, 3β, 18, and 19 positions (Abraham 1994). c. Stemodin by Cephalosporium aphidicola at the 7α 7β, 8β, 18, and 19 positions (Hanson et al. 1994). The spectrum of substrates has been extended to xenobiotics, and a single example may sufice. The fungus Beauveria bassiana metabolized the hydroxycoumarin rodenticide warfarin to the hydroxylated and oxidized metabolites, which have already been established in mammalian systems or mediated by fungal cytochrome P450 monooxygenase systems. In addition, novel products were produced from the reduction of the keto group in the 4-hydroxyl group (Grifiths et al. 1992).

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PART 3 ALKANES, CYCLOALKANES AND RELATED COMPOUNDS WITH CHLORINE, BROMINE, OR IODINE SUBSTITUENTS Particularly the chlorinated compounds have enjoyed range of applications: vinyl chloride (chloroethene) as monomer for the production of PVC, tetra- and trichloroethenes as solvents for degreasing, and the insecticides 1,1,1-trichloro-2,2-bis(p-chlorophenyl)ethane (DDT) and isomers of hexachlorocyclohexane (HCH) (benzene hexachloride). The biodegradation of luorinated aliphatic compounds is generally different from the outlines that have emerged from investigations on their chlorinated, brominated, and even iodinated analogues. They are therefore treated separately in Part 4 of this chapter.

CHLORINATED, BROMINATED, AND IODINATED ALKANES, ALKENES, AND ALKANOATES A range of mechanisms has been found for the biodegradation of halogenated alkanes, alkenes, and alkanoates: 1. Elimination including dehydrohalogenation 2. A corrinoid pathway for C1 halides, which operates under both aerobic and anaerobic conditions 3. Nucleophilic displacement including hydroxylation, hydrolysis, and glutathione-mediated reactions 4. Reduction in which a halogen atom is replaced by hydrogen including dehalorespiration 5. Cytochrome P450–mediated reactions.

350

Environmental Degradation and Transformation of Organic Chemicals

Elimination Reactions In contrast to chemical reactions in which elimination and nucleophilic displacement are alternatives and may occur simultaneously, microbial elimination is less common. This term is also used for the reaction in which, for example, 1,2-dihaloethanes are transformed to ethene, in contrast to dehydrohalogenation in which a haloethene is produced or reductive hydrogenolysis to a haloethane. Degradation involving elimination is found in several degradations: a. Several steps in the degradation of DDT by the facultatively anaerobic bacterium Aerobacter aerogenes involve elimination (Figure 7.49) (Wedemeyer 1967), while a range of products from transformation of the trichloromethyl groups have been isolated (Schwartzbauer et al. 2003). The recovery of the elimination product 1,1-dichloro-2,2-bis(p-chlorophenyl)ethene (DDE) from environmental samples long after restriction on the use of DDT suggests a high degree of persistence. DDE can, however, be degraded by ring dioxygenation and extradiol ring ission to 4-chlorobenzoate in cells of Pseudomonas acidovorans M3GY grown with biphenyl (Hay and Focht 1998) and Terrabacter sp. strain DDE-1 induced with biphenyl (Aislabie et al. 1999). An alternative pathway for the transformation of DDT involves hydroxylation of the ring and displacement of the aromatic ring chlorine atom by hydroxyl (Figure 7.50) (Massé et al. 1989). Bis(p-chlorophenyl)acetic acid (DDA) is a polar metabolite that is apparently persistent in the environment (Heberer and Dünnbier 1999). In higher organisms, DDE can be metabolized by formation of sulfones (Letcher et al. 1998). b. Growth of a range of bacteria including Escherichia coli, Bacillus subtilis, and Streptococcus pyogenes is inhibited by 3-chloro-d-alanine and extracts of the irst two of these inactivate alanine racemase (Manning et al. 1974). The enzyme that brings about degradation by elimination to pyruvate, ammonia, and chloride has been puriied from Pseudomonas putida strain CR 1-1 and contains 2 mol pyridoxal 5′phosphate per mole of enzyme. The enzyme is induced by 3-chloro-d-alanine and also catalyzes the analogous degradation of d-cysteine to pyruvate, sulide, and ammonia, although this activity could not be detected in medium supplemented with d-cysteine (Nagasawa et al. 1982). There are important differences in the effects of d- and l-3-chloroalanine on membrane transport of proline that are relections of their metabolism. Whereas in membrane vesicles from E. coli B, the l-enantiomer can undergo elimination to pyruvate catalyzed by pyridoxal phosphate, the d-enantiomer brings about irreversible inactivation of membrane transport by dehydrogenation to chloropyruvate (Kaczorowski et al. 1975). Aerobic Conditions A great deal of effort has been expended in elucidating the details of the degradation of HCH isomers that differ both in their toxicity and their biodegradability. This has been examined mostly in strains originally classiied as Sphingomonas paucimobilis, and to a lesser extent in Rhodobacter lindaniclasticus (Nalin et al. 1999), though this strain apparently no longer exists. Although many of the reactions are biotransformations in which the ring is retained, evidence for ission of the ring has been obtained for Sphingobium japonicum strain UT26 that is noted below. 1. Bacteria that degrade or transform HCH isomers have been described. They vary in selectivity towards the isomers and the β-isomer that has only equatorial substituents is generally the most recalcitrant. Three strains, which have been most studied belong to the genus Sphingobium, Sph. indicum B90A, Sph. japonicum UT26, and Sph. francese sp+ (Pal et al. 2005). All have the genes for linA, linD, linC, and linDER, which are discussed later, but they differ in the ease with which they transform the HCH isomers (Table 7.1) (Sharma et al. 2006).

FIGURE 7.49

Cl

Cl

Cl

Cl

Biotransformations of DDT.

DDMS

CH 2 Cl

CH

DDT

CCl3

CH

Cl

Cl

Cl

Cl

DDA

CO 2 H

CH

DDNU

CH 2

C

DDD

CHCl2

CH

CCl2

C

DDE

Cl

Cl

Cl

Cl

Cl

CO

Cl

Cl

DDMU

CHCl

C

Cl

Aliphatic Compounds 351

352

Environmental Degradation and Transformation of Organic Chemicals CCl3 CH

Cl

CCl3 Cl

Cl

CH

OH

OH

OH

FIGURE 7.50 Alternative pathway for biodegradation of DDT.

TABLE 7.1 Relative Transformation of Hexachlorocyclohexane Isomers Hexachlorocyclohexane Isomer Sphingobium Strain α γ B90A +++ +++ sp+ ++ ++ UT26 ++ ++ A strain of Pandoraea sp. was also able to degrade the γ-isomer (Okeke et al. 2002).

β +++ ++ +

δ +++ ++ ++

2. There are seven isomers of HCH that differ in their conformations: α-isomer, aaaaee; β-isomer, eeeeee; γ-isomer, aaaeee; δ-isomer, aeeeee; ε-isomer, aeeaee; η-isomer, aaeaee; and φ-isomer, aeaeee (Willett et al. 1998). Their degradation is initiated by dehydrochlorination that is dependent on the stereochemistry of the isomer. For example, the β-isomer that lacks 1,2-diaxial hydrogen and chlorine groups is not a substrate for the LinA dehydrohalogenase (Nagata et al. 1993) and as a consequence this isomer is less readily degraded. Strain Sphingobium japonicum UT26 is, however, capable of converting the persistent β-isomer only into pentachlorocyclohexanol by the activity of the dehalogenase lin B (Nagata et al. 2005). 3. In strains of S. paucimobilis, most of the genes (linA-E) encoding the degradative enzymes are associated with an insertion sequence (IS6100) that mediated horizontal gene transfer (Dogra et al. 2004). In another strain that is able to degrade γ-HCH, the enzymes involved in dehydrochlorination were apparently extracellular (Thomas et al. 1996). 4. a. The irst two steps in the biotransformation of HCH involve eliminations (dehydrochlorinations), for example, in the degradation of γ-hexachloro(aaaeee)cyclohexane from which pentachlorobenzene (Tu 1976) or γ-2,3,4,6-tetrachlorocyclohex-1-ene are formed (Jagnow et al. 1977) (Figure 7.51). The formation of 2,5-dichlorophenol and 2,4,5-trichlorophenol during the aerobic degradation of γ-hexachloro(aaaeee)cyclohexane by Sphingomonas (Pseudomonas) paucimobilis putatively involves comparable elimination reactions (Sendoo and Wada 1989). The transformation by Sphingobium japonicum (Pseudomonas paucimobilis) strain UT26 produced 1,2,4-trichlorobenzene as a terminal metabolite by sequential diaxial dehydrochlorinations (Nagasawa et al. 1993a,b). Further details have been given of the stereochemistry of the initial reactions that involve 1,2-diaxial dehydrochlorination to pentachlorocyclohexane followed by sequential 1,4-anti dehydrochlorinations to 1,2,4,5-tetrachlorocyclohex-2,5-diene and 1,2,4-trichlorobenzene (Figure 7.52) (Trantírek et al. 2001). b. In the degradation by Sphingobium japonicum strain UT26, the genes leading to 2,5-dichlorohydroquinone have been designated linA, linB, and linC. They encode enzymes that carry out two successive dehydrochlorinations (LinA), two successive dehalogenations (hydrolytic dechlorinations) (LinB), and a dehydrogenase (LinC) (Nagata et al. 1999). Further steps involving linD, linE, and linF in this strain have been described. They comprise dioxygenation of 2-chlorohydroquinone, followed by

353

Aliphatic Compounds Cl

Cl Cl

Cl

Cl

Cl Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl Cl

FIGURE 7.51

Pathway for biotransformation of γ-hexachlorocyclohexane.

H

H

Cl

Cl

H Cl

FIGURE 7.52

Cl

Cl

Cl

H

H

H

Cl

Cl Cl

Cl H

H

H

Cl H

H Cl

Cl

H

Cl

Cl

Cl

Stereochemistry of irst steps in the biotransformation of γ-hexachlorocyclohexane.

hydrolysis of the acyl chloride to 3-hydroxymuconate that is mediated by an unusual metacleavage enzyme encoded by linE (Figure 7.53) (Miyauchi et al. 1999; Endo et al. 2005). Since the elimination reactions that are involved are not themselves dependent on the presence of oxygen, they may occur under anaerobic conditions. 5. Whereas strain UT26 is capable of converting the β-isomer of HCH only into pentachlorocyclohexanol by the activity of the dehalogenase lin B (Nagata et al. 2005), Sphingobium indicum (Sphingomonas paucimobilis) strain B90A is able to degrade all four isomers (α-, β-, γ-, and δ-) of HCH mediated by linA1, linA2, linB, linC, linD, and linE (Suar et al. 2004). 6. Strain B90A contains two copies of linA that have important consequences. The corresponding dehydrochlorinases LinA1 and LinA2 are speciic for the (+) and (−) enantiomers of α-HCH (Suar et al. 2005), and the presence of both makes possible the degradation of racemic HCH. In strains with only a single copy of the enzyme, however, degradation of only one of the enantiomers will take place with consequent enrichment of the nondegradable enantiomer. Anaerobic Conditions Elimination is rather exceptional under anaerobic conditions although there are some examples that involve additionally dehydrogenation. 1. Elimination, dehydrogenation, and hydrogenolysis may take place during biotransformation of HCH isomers. a. A strain of Clostridium rectum (Ohisa et al. 1980) converted γ-HCH into 1,2,4-trichlorobenzene, while γ-1,3,4,5,6-pentachlorocyclohexene produced 1,4-dichlorobenzene (Figure 7.54). It was suggested (Ohisa et al. 1982) that this reductive dechlorination and

LinE

LinA

HO

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

CO 2 H

OH

Cl

Cl

COCl HO

Cl

Cl

CO 2 H

LinB

Cl

CO 2 H

Cl

Cl

LinA

Cl

FIGURE 7.53 Aerobic degradation of γ-hexachlorocyclohexane.

OH

OH Cl

Cl

Cl

Cl

Cl

Cl

Cl

LinF

LinB

O

Cl

Cl

Cl

Cl

CO 2 H

CO 2 H

OH

OH

Cl

LinC Cl OH

OH Cl LinD

354 Environmental Degradation and Transformation of Organic Chemicals

355

Aliphatic Compounds Cl

Cl

Cl

Cl

Cl

Cl

Cl Cl

Cl

Cl ;

Cl

Cl

Cl

Cl Cl

Cl

FIGURE 7.54 Anaerobic biotransformation of γ-hexachlorocyclohexene and γ-1,3,4,5,6-pentachlorocyclohexene. Br CH2 CH2 Br

FIGURE 7.55

CH2

CH2

;

Br CH

CH Br

CH

CH

Metabolism of 1,2-dibromoethane.

elimination was coupled to the synthesis of ATP, and this possibility has been amply conirmed in a number of anaerobic dehalogenations of polychlorinated ethenes and some chlorophenols. b. During anaerobic incubation of [36Cl]-γ-hexachlorocyclohexane, dechlorination with tetrachlorocyclohexene as an intermediate was demonstrated in Cl. butyricum, Cl. pasteurianum, and Citrobacter freundii (Jagnow et al. 1977). c. A methanogenic enrichment culture dehydrochlorinated β-hexachlorocyclohexane to δ-tetrachlorocyclohexene by elimination and hydrogenolysis, with the formation of chlorobenzene and benzene as the stable end product. The α-isomer was dechlorinated at a comparable rate, and the γ- and δ-isomers more slowly (Middeldorp et al. 1996). 2. Analogous reactions have been shown to occur with aliphatic halides: a. Pure cultures of strictly anaerobic methanogenic bacteria transformed 1,2-dibromoethane to ethene and 1,2-dibromoethene to ethyne (Figure 7.55) (Belay and Daniels 1987). b. A nonmethanogenic culture produced propene from 1,2-dichloropropane plausibly via the reductive formation of monochloropropanes followed by elimination (Löfler et al. 1997). c. The dehalorespiring Desulitobacterium dichloroeliminans strain DCA1 carried out exclusive antielimination of vicinal dichloroethane, and all the vicinal dichlobutanes (de Wildeman et al. 2003). d. The reductive dehalogenase from Desulitobacterium sp. strain Y51 carried out not only the dehalogenation of tetrachloroethene to trichloroethene and cis-1,2-dichloethene, but also the elimination of a number of polyhalogenated ethanes, for example, hexachloroethane to cis-1,2-dichloroethene (Suyama et al. 2002). Corrinoid Pathways The existence of corrinoids in anaerobic bacteria in substantial concentrations is well established, and their metabolic role in acetogenesis and in methanogenesis has been elucidated. Their involvement in degradation pathways of aerobic organisms is more recent, and it has emerged that their role under these different conditions is similar. These issues are explored in the following paragraphs with a view to illustrating the similar metabolic pathways used by both aerobes and anaerobes. Corrinoids are involved in aerobic degradation of methyl chloride by the aerobic Methylobacterium sp. strain CM4, and also in the degradation of other C1 compounds by Methylobacterium extorquens (Christoserdova et al. 1998). Methyl corrins are key components in transmethylation and examples illustrating the similarity of pathways in aerobic and anaerobic metabolism will be summarized. In the following discussion, THF or tetrahydromethanopterin (Figure 7.56) are implicated in the form of their methyl (CH3), methylene (CH2), methine (CH), and formyl (CHO) derivatives (Figure 7.57). The formation of a CH3–Co bond is central to activity, and generally the 5,6-dimethylbenziminazole is replaced by histidine.

356

Environmental Degradation and Transformation of Organic Chemicals H

O

N

HN H2N

CH 2

NHΦ

N

N H Tetrahydrofolate H4F

H N

4 3

2

N

CH 3

O N

HN H2 N

N

CH

NHΦ

N H

Tetrahydromethanopterin H 4 MPT N

5

10

CH 2 9 H 4 F 6

N 1

8

7

N H

FIGURE 7.56 Partial structures of tetrahydrofolate (H4F) and tetrahydromethanopterin (H4MPT). (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

O N H 2N

H N

CH 2 NHΦ H4F

H

N H CH 3 N

CH 2 NHΦ CH 3

H4F

CH 2

H4F

N H CH 2 N N

Φ

CH 2

N H Φ

CH

N

N

CH 2 CH

H 4F

N H CHO N

CH 2 NHΦ CHO

H4F

N H

FIGURE 7.57 Dehydrogenation of CH3-tetrahydrofolate to CHO-tetrahydrofolate. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

357

Aliphatic Compounds

Strain IMB-1 is able to grow at the expense of methyl bromide (Woodall et al. 2001) and belongs to a group of organisms that can also degrade methyl iodide, but are unable to use formaldehyde or methanol (Schaefer and Oremland 1999). It was postulated that the pathway for chloromethane degradation in this strain was similar to that in Methylobacterium chloromethanicum (McAnulla et al. 2001a). Aerobic Degradation of Methyl Chloride Methylotrophic bacteria have been isolated that are able to use methyl chloride aerobically as the sole source of energy and carbon, and bacteria that can utilize methyl chloride are apparently widely distributed and several belong to strains of Hyphomicrobium (McAnulla et al. 2001b). The substrate is metabolized to formaldehyde and subsequently oxidized either to formate and CO2, or incorporated via the serine pathway. A study using strain CC495 that is similar to the strain IMB-1 already noted revealed the complexity of this reaction (Coulter et al. 1999), while details had emerged from a somewhat earlier study of methyl chloride degradation by the aerobic Methylobacterium sp. strain CM4 (Methylobacterium chloromethanicum). Cobalamin was necessary for growth with methyl chloride, though not for growth with methylamine, and the use of mutants containing a miniTn5 insertion and enzyme assays revealed that the mechanism involved initial methyl transfer to a Co(I) corrinoid followed by oxidation via THFs to formytetrahydrofolate and thence to formate with production of ATP (Figure 7.58) (Vannelli et al. 1999). Anaerobic Degradation of Methyl Chloride The anaerobic methylotrophic homoacetogen Acetobacterium dehalogenans is able to grow with methyl chloride and CO2, and uses a pathway comparable to that noted above for the aerobic

CH 3 Cl CmuA III

CH 3

Co

CH 3

H 4F

CH 2

H 4F

E

CmuB

MetF

FolD CH

H 4F

FolD CHO

H 4F

PurU 2H

Methylobacterium chloromethanicum

FIGURE 7.58 Degradation of methyl chloride by Methylobacterium chloromethanicum. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

358

Environmental Degradation and Transformation of Organic Chemicals CH 3 Cl

CH 3

H4F

CH 2

H4F

CH 3

Co I

E

CO 2 CO

CH

H4F

CHO

H4F

CH 3CO−SCoA

CH 3 CO 2 H

H−CO 2H

FIGURE 7.59

Degradation of methyl chloride by Acetobacterium halogenans.

degradation: dehydrogenation of the methyl group involving THF and a corrinoid coenzyme. Acetate is simultaneously produced from CO2 by the activity of CO dehydrogenase and the methyltetrahydrofolate (Figure 7.59) (Meβmer et al. 1993). Some of the gene products are shared with those involved in metabolism of methyl chloride (Vannelli et al. 1999). The methyl transfer reactions and those involved in the subsequent formation of acetate have been explored for the demethylase of this strain (Kaufmann et al. 1998), and resemble closely those for the aerobic metabolism of methyl chloride by aerobic methylotrophs. Anaerobic Degradation of Polyhalogenated Methanes Acetobacterium dehalogenans is able to degrade dichloromethane and the pathway formally resembles that for the anaerobic degradation of methyl chloride. A strain of Dehalobacterium formicoaceticum is able to use only dichloromethane as a source of carbon and energy forming formate and acetate (Mägli et al. 1998). The pathway involves initial synthesis of methylenetetrahydrofolate of which two-thirds is degraded to formate with generation of ATP, while the other third is dehydrogenated, transmethylated, and after incorporation of CO forms acetate with production of ATP (Figure 7.60). The formation of [13C]formate, [13C]methanol, and [13CH3]CO2H was elegantly conirmed using a cell suspension and [13C]CH2Cl2. It was suggested that a sodium-independent F0F1-type ATP synthase exists in this organism in addition to generation of ATP from formyltetrahydrofolate. A strain of Acetobacterium woodii strain DSM 1930 dehalogenated tetrachloromethane to dichloromethane as the inal chlorinated product, while the carbon atom of [14C]tetrachloromethane was recovered as acetate (39%), CO2 (13%), and pyruvate (10%) (Egli et al. 1988). Since the transformation of tetrachloromethane to chloroform and CO2 is a nonenzymatic corrinoid-dependent reaction (Egli et al. 1990; Hasham and Freedman 1999), it seems safe to assume operation of the acetyl-CoA synthase reaction. The synthesis of acetate that also takes place during the degradation of dichloromethane by Dehalobacterium formicoaceticum involves CO2 that originates from the medium (Mägli et al. 1996). Nucleophilic Substitution: Hydrolytic Reactions of Halogenated Alkanes and Alkanoates Alkanes Displacement of halogen by hydroxyl is a widely distributed reaction in the degradation of haloalkanes and haloalkanoates. Although an apparently simple pathway involving two displacement

359

Aliphatic Compounds CH2Cl2 + H4F

CH 2

H 4F

CH 2

H 4F

CH

H 4F

CH 3

H 4F

CHO

H 4F

CH 3

Co I

E

CO 2 CO

H−CO 2H CH 3 C O SCoA

CH 3 C O PO 4

CH3CO2H

FIGURE 7.60 Degradation of methylene chloride by Dehalobacterium formicoaceticum. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.) Cl−CH 2−CH2−Cl

FIGURE 7.61

Cl−CH 2−CH2OH

Cl−CH 2CHO

Cl−CH 2−CO2H

HOCH 2−CO2H

Biodegradation of 1,2-dichloroethane.

steps is illustrated in Figure 7.61 (Janssen et al. 1985), it should be emphasized that the enzymology of hydrolytic dehalogenation is quite complex. For example, two different dehalogenases are involved in the dechlorination of 1,2-dichloroethane and chloroacetate (van den Wijngaard et al. 1992). A number of distinct dehalogenases exist, and they may differ signiicantly in their substrate speciicity in respect of chain length and the inluence of halogen atoms at the ω-position (Scholtz et al. 1988; Sallis et al. 1990). The degradation of 1,2-dichloroethane may also be initiated by monooxygenation (Hage and Hartmans 1999), and the pathways for hydrolysis and monooxygenation converge with the production of glyoxylate. The degradation of 2-chloroethylvinyl ether by Ancylobacter aquaticus is initiated by a dehalogenase, although ission of the C–O–C bond is nonenzymatic (van den Wijngaard et al. 1993). Pseudomonas sp. strain ES-2 was able to grow with a range of brominated alkanes that greatly exceeded the range of chlorinated or unsubstituted alkanes, and bromoalkanes with chain lengths of C6 –C16 and C18 could be utilized (Shochat et al. 1993). A range of chlorinated, brominated, and iodinated alkanes C4 –C16 was incubated with resting cells of Rhodococcus rhodochrous NCIMB 13064 (Curragh et al. 1994), and dehalogenation was assessed from the concentration of halide produced. The range of substrates is impressive and the yields were approximately equal for chloride and bromide, and greater for iodide. Signiicant differences between the degradation of

360

Environmental Degradation and Transformation of Organic Chemicals

chlorine- and bromine-substituted alkanes may, however, exist. For example, although Xanthobacter autotrophicus is able to grow with 1,2-dichloroethane and the dehalogenases can debrominate 1,2dibromoethane and bromoacetate, these substrates are unable to support growth of the organism. Several reasons have been suggested including the toxicity of bromoacetaldehyde (van der Ploeg et al. 1995). This is consistent with the observations that in this strain, the initially produced 2chloroethanol is oxidized to the aldehyde by an alkanol dehydrogenase and then to chloroacetate before loss of chloride and mineralization. In contrast, Mycobacterium sp. strain GP1,which belongs to the group of fast-growing mycobacteria, was able to use 1,2-dibromoethane as a source of carbon and energy. Although a hydrolytic haloalkane dehalogenase produced 2-bromoethanol, this was converted into the epoxide that was used for growth by a pathway that was not established. In this way, production of toxic bromoacetaldehyde was circumvented (Poelarends et al. 1999). The metabolic capacity of species of mycobacteria including the human pathogen Mycobacterium tuberculosis strain H37Rv is remarkable (Jesenská 2000). Extracts of M. avium and M. smegmatis were able to dehalogenate a range of halogenated alkanes with chlorine, bromine, and iodine terminal substituents. On the basis of amino acid and DNA sequences, the strain that was used contained three halohydrolases, and the debromination capability of a selected number of other species of mycobacteria is given in Table 7.2. The haloalkane dehalogenase gene from M. avium has been cloned and partly characterized (Jesenská et al. 2002), and it has been shown that there are two dehalogenase genes dmbA and dmbB that are widely distributed in bacteria of the Mycobacterium tuberculosis complex (Jesenská et al. 2005). Some strains of bacteria are able to use α,ω-dichlorinated long-chain alkanes for growth, and the activity of the hydrolase from Rhodococcus erythropolis strain Y2 was high for 1,2-dibromoethane, 1,2-dibrompropane, and the α,ω-dichloroalkanes (Sallis et al. 1990). In contrast, the range of α,ω-dichlorinated alkanes that was used for growth of Pseudomonas sp. strain 273 was limited to the C9 and C10 substrates (Wischnak et al. 1998). Dehalogenase activity was demonstrated in a strain of Acinetobacter GJ70 that could degrade some α,ω-dichloroalkanes, and 1-bromo- and 1-iodopropane. Although 1,2-dibromoethane could be converted into 2-bromoethanol, this could not be used for growth plausibly due to the toxicity of bromoacetaldehyde that has already been noted, and the inability to use dihydroxyethane as growth substrate (Janssen et al. 1987). In a later study, the enzyme from this strain showed dehalogenase activity towards a wide range of substrates including halogenated alkanes, alkanols, and ethers (Janssen et al. 1988). A brief summary of the degradation of 1,2-dichloroethane by Xanthobacter autotrophicus strain GJ10 is given, since this strain has been used to delineate all stages of the metabolism and the appropriate enzymes have been demonstrated (Janssen et al. 1987) (Figure 7.62). The activity of a haloalkane dehalogenase initiates degradation and is discussed in this section, while the alkanol dehydrogenase, the aldehyde dehydrogenase, and the haloacetate dehalogenase are discussed subsequently. The enzyme responsible for dehalogenase activity has been puriied from Xanthobacter autotrophicus strain GJ10, consists of a single polypeptide chain with a molecular mass of 36 kDa, and was able to dehalogenate chlorinated, and both brominated and iodinated alkanes

TABLE 7.2 Specific Activity (µmol bromide produced/mg protein/min) of Dehalogenase from Selected Species of Mycobacterium towards 1,2-Dibromoethane Taxon M. bovis BCG MU10 M. fortuitum MU8 M. triviale MU3 M. smegmatis CCM4622

Activity

Taxon

Activity

99 76 61 49

M. avium MU1 M. phlei CCM 5639 M. parafortuitun MU2 M. chelonae

36 22 22 20

361

Aliphatic Compounds

FIGURE 7.62 Degradation of 1,2-dichloroethane by Xanthobacter autotrophicus strain GJ10. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

Trp 75 N H

Phe 172

C2

Phe 128

Cl

Cl

1

C1

2

H N O

O

Trp 125

H N

O

O

HN

Asp 260

N

H

O H

O

O

Asp 124

H N

His 289 Glu 56 O

O

FIGURE 7.63 Mechanism of dehalogenation. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

(Keuning et al. 1985). Details of the mechanism have been explored using an ingenious method of producing crystal at different stages of the reaction (Verschuren et al. 1993). The overall reaction involves a catalytic triad at the active site: Asp124 binds to one of the carbon atoms, and hydrolysis with inversion is accomplished by cooperation of Asp260 and His289 with a molecule of water bound to Glu56 (Figure 7.63). Intermediate Epoxides

The conversion of vicinal haloalkanols into epoxides is of considerable interest and was apparently irst recognized in a strain of Flavobacterium (Castro and Bartnicki 1968). The trans-epoxide from erythro-3-bromobutan-2-ol and the cis-epoxide from threo-3-bromobutan-2-ol were formed stereospeciically, and the epihalohydrins were able to react with halide to produce 2-hydroxy-1,3dihalobutanes (Bartnicki and Castro 1969). Haloalkanol dehalogenase activity has since been found in a number of different bacteria (Slater et al. 1997). The enantioselective halohydrin hydrogen lyase (alkanol dehalogenase) has been characterized from Corynebacterium sp. strain N-1074 (Nakamura et al. 1994a), as well as two different epoxide hydrolases that produce 3-chloropropane-1,2-diol from the same strain (Nakamura et al. 1994b). The haloalkanol dehalogenase has been characterized from Arthrobacter sp. strain AD2 that is able to utilize 3-chloro-1,2-propandiol for growth (van den Wijngaard et al. 1991). It has a molecular mass of 29 Da and consists of two equal subunits. The x-ray structure of the epoxide hydrolase from Agrobacterium radiobacter strain AD2 has been

362

Environmental Degradation and Transformation of Organic Chemicals

carried out and provided details of its mode of action (Nardini et al. 1999). Haloalkanol dehalogenase from this strain is able to form epoxides from a number of vicinal chlorinated and brominated alkanols (van den Wijngaard et al. 1991), and is also able to carry out transhalogenation between epihalohydrins and halide ions. The activities of both haloalkanol dehalogenase (halohydrin hydrogen lyase) that catalyzes the formation of epoxides from alkanes with vicinal hydroxyl and halogen groups, and epoxide hydrolase that brings about hydrolysis of epoxyalkanes to diols are involved in a number of degradations that involve their sequential operation. a. In the degradation of epichlorohydrin (3-chloro-1,2-epoxyethane) (van den Wijngaard et al. 1989), the epoxide hydrolase produced 3-chloropropan-1,2-diol that was dehalogenated to glycidol by the dehydrogenase, followed by hydrolysis of the epoxide with the production of glycerol. b. The degradation of trihalogenated propanes by Agrobacterium radiobacter into which dehalogenases in plasmids from Rhodococcus sp. strain m15-3 were incorporated (Bosma et al. 1999) involved a sequence of steps, two of which involve the formation and hydrolysis of epoxides with the ultimate production of glycerol. Halogenated Alkanoates Halogenated alkanoic acids are produced from the corresponding aldehydes during the degradation of 1,2-dihaloethanes by Xanthobacter autotrophicus (Janssen et al. 1985) and the facultative methanotroph Ancylobacter aquaticus (van den Wijngaard et al. 1992), and are degraded by haloacetate dehalogenases. The aerobic degradation of halogenated alkanoic acids has been extensively investigated, and is generally carried out by halohydrolases that have variable speciicity for the halogen, its position, and for different enantiomers. The dehalogenases have been grouped according to their reactions with 2-chloropropionate in carrying out hydrolysis with or without inversion—and the effect of sulfhydryl inhibitors (Fetzner and Lingens 1994). The enzymology of 2-haloalkanoate dehalogenases has been discussed in detail (Slater et al. 1997). The crystal structures of the complexes between the l-2-haloacid dehalogenase from Pseudomonas sp. strain YL and 2-chloroalkanoates have been determined (Li et al. 1998). They reveal that the hydrolytic inversion involves the Arg41 and Asp10 sites as electrophiles and nucleophiles, respectively, followed by interaction of the Asp10 ester with Ser118. The enantiomeric speciic dehalogenase from Pseudomonas sp. strain DL-DEX is able to use both enantiomers of 2-haloalkanoic acids as substrates forming products with inversion of the coniguration (Nardi-Del et al. 1997). The degradation of 2,2dichloropropionate involves dehalogenation to pyruvate but even here two different dehalogenases are synthesized (Allison et. al. 1983). Di- and trichloroacetate are degradable, though not apparently by the same groups of organisms. Mono- and dichloroacetate were effectively degraded by a strain of “Pseudomonas dehalogenans” that had only limited effect on trichloroacetate, whereas conversely, strains of Arthrobacter sp. readily degraded trichloroacetate—though not monochloroacetate (Jensen 1960). An organism that was able to grow with trichloroacetetae, though not with mono- or dichloroacetate was similar to Acinetobacter calcoaceticus on the basis of 16S rDNA (Yu and Welander 1995). The anaerobic degradation of halogenated alkanoic acids has, however, been much less exhaustively examined. Geobacter (Trichlorobacter) thiogenes was able to transform trichloroacetate to dichloroacetate by coupling the oxidation of acetate to CO2 with the reduction of sulfur to sulide that carries out the dechlorination (De Wever et al. 2000). Halogenated Alkenoates The degradation of 2- and 3-chloroacrylate displays novel features. The degradation of 2-chloroacrylate by Burkholderia sp. strain WS is initiated by a 2-haloacrylate reductase with the formation of (S)-2-chloropropionate that undergoes dehalogenation to (R)-lactate (Kurata et al. 2005). The degradation of 1,3-dichloropropene by Pseudomonas pavonaceae (cichorii) strain 170 involves a series of steps by which trans-3-chloroacrylate is formed (Poelarends et al. 1998). This was degraded

363

Aliphatic Compounds O

O

C

C

S N O C S

Cu

CCl4

O C S

C S +CCl3 Lg

N Ligand

O

Cu Cl

N O C S

COS S CCl3 Lg

Cl3CSH

Cl2

Cu

CO2

S CS2

Cl

FIGURE 7.64 Degradation of tetrachloromethane (CCl4) mediated by pyridine-2,6-dithiocarboxylate.

by dehalogenation to malonate semialdehyde (Poelarends et al. 2001), and it has been shown that this is accomplished by hydration of trans-3-chloroacrylate to an unstable halohydrin that collapses to form malonate semialdehyde (De Jong et al. 2004). The malonate semialdehyde decarboxylase (Poelarends et al. 2003) has been characterized. Glutathione-Mediated and Other Reactions Involving Nucleophilic Sulfur Although the reactions described above are formally nucleophilic displacements of the chlorine atoms by hydroxyl groups, a different mechanism clearly operates in the degradation of dichloromethane by Hyphomicrobium sp. The enzyme is glutathione-dependent (Stucki et al 1981; Kohler-Staub et al. 1986) and the reaction presumably involves at least two steps. Glutathionedependent reactions are also involved in the transformation and detoxiication of alkenes including isoprene, and both cis- and trans-1,2-dichloroethene in Rhodococcus sp. strain AD45 (van Hylckama Vlieg et al. 1998). For cis-1,2-dichloroethene, the initially formed epoxide is transformed by reaction with glutathione followed by chemical reactions with the inal production of glyoxal. Glutathione S-transferase and a glutathione dehydrogenase have been characterized in this strain (van Hylckama Vlieg et al. 1999). The degradation of tetrachloromethane by a strain of Pseudomonas sp. presents a number of exceptional features. Although 14CO2 was a major product from the metabolism of 14CCl4, a substantial part of the label was retained in nonvolatile water-soluble residues (Lewis and Crawford 1995). The nature of these was revealed by the isolation of adducts with cysteine and N,N′-dimethylethylenediamine, when the intermediates that are formally equivalent to COCl2 and CSCl2 were trapped—presumably formed by reaction of the substrate with water and a thiol, respectively. Further examination of this strain classiied as Pseudomonas stutzeri strain KC has illuminated novel details of the mechanism. The metabolite pyridine-2,6-dithiocarboxylic acid (Lee et al. 1999) plays a key role in the degradation. Its copper complex produces trichloromethyl and thiyl radicals, and thence the formation of CO2, CS2, and COS (Figure 7.64) (Lewis et al. 2001). Monooxygenation Halogenated Alkanes A number of halogenated—including polyhalogenated—alkanes are degraded by hydroxylation mediated by MMO. 1. The soluble MMO from Methylococcus capsulatus (Bath) is able to oxidize chloro- and bromomethane—but not iodomethane—with the presumptive formation of formaldehyde (Colby et al. 1977). 2. The methane degrading Methylosinus trichosporium OB3b has been shown to degrade both methyl bromide and dibromomethane (Bartnicki and Castro 1994; Streger et al. 1999), and the propane-degrading Mycobacterium vaccae JOB5 can degrade methyl bromide (Streger et al. 1999). 3. A number of haloalkanes including dichloromethane, chloroform, 1,1-dichloroethane and 1,2-dichloroethane may be degraded by the soluble MMO system of Methylosinus trichosporium (Oldenhuis et al. 1989).

364

Environmental Degradation and Transformation of Organic Chemicals

4. The metabolism of chloroform has been studied in several organisms (Hamamura et al. 1997), and from the inhibitory effect of acetylene it was concluded that a monooxygenase was involved: a. Cells of Methylosinus trichosporium strain OB3b grown with methanol and incubated with formate as electron donor degraded chloroform with the release of 2.1 mol of chloride per mole substrate and at substrate concentrations up to 38.6 µM. b. Cells of Pseudomonas butanovora grown with butane and incubated with butyrate as electron donor degraded chloroform with the release of 1.7 mol chloride per mole substrate and degradation was incomplete even at concentrations of 12.9 µM. Butane inhibited the degradation. This organism also partially degraded other chloroalkanes and chloroalkenes including chloroethene (vinyl chloride), 1,2-trans-dichloroethene and trichloroethene. c. Butane-grown cells of Mycobacterium vaccae strain JOB5 were able to degrade chloroform without addition of an electron donor. 5. The degradation of 1,2-dichloroethane by Pseudomonas sp. strain DCA1 was initiated not by hydrolysis, but by monooxygenation with the direct formation of 1,2-dichloroethanol that spontaneously decomposed to chloroacetaldehyde (Hage and Hartmans 1999). The cometabolism of halogenated methanes has been examined in Nitrosomonas europaea and may putatively be mediated by ammonia monooxygenase. a. Oxidation of methyl luoride to formaldehyde has been demonstrated (Hyman et al. 1994), and of chloroalkanes at carbon atoms substituted with a single chlorine atom to the corresponding aldehyde (Rasche et al. 1991). b. Oxidation of a number of chloroalkanes and chloroalkenes including dichloromethane, chloroform, 1,1,2-trichloroethane, and 1,2,2-trichloroethene has been demonstrated (Vannelli et al. 1990). Although the rate of cometabolism of trihalomethanes increased with levels of bromine substitution, so also did the toxicity. Both factors must therefore be evaluated (Wahman et al. 2005). Halogenated Alkenes Although degradation of halogenated alkenes by direct displacement of halogen is not expected on purely chemical grounds, this reaction apparently occurs during the degradation of vinyl chloride by a strain of Pseudomonas sp. that carries out the direct hydrolysis to acetaldehyde followed by mineralization to CO2 (Castro et al. 1992a). The degradation of 3-trans-3-chloroacrylate, however, involves dehalogenation by hydration to an unstable halohydrin (De Jong et al. 2004). The regulation of the synthesis of the soluble and particulate monooxygenase enzymes is illustrated by the degradation of trichloroethene by Methylosinus trichosporium strain OB3b. During copper limitation, the soluble monooxygenase is formed, but not during copper suficiency when the particulate form is synthesized (Oldenhuis et al. 1989). Epoxidation is the irst reaction in the degradation of chlorinated ethenes including chloroethene (vinyl chloride) (Coleman et al. 2002a; Coleman and Spain 2003; Danko et al. 2004) and cis-dichloroethene that is a recalcitrant intermediate in the anaerobic dechlorination of tetra- and trichloroethene (Coleman et al. 2002b). The epoxides formed by monooxygenation are toxic to cells and mechanisms must exist for their removal. Although evidence for the existence of epoxide hydrolases is well established in mammalian systems, this has not been so widely observed in bacteria. Some aspects of the pathways are summarized: 1. The degradation of trichloroethene (Figure 7.65) provides a good example of the monooxygenation of haloalkenes (Little et al. 1988). 2,2,2-Trichloroacetaldehyde is produced during oxidation of trichloroethene by several methanotrophs and undergoes a dismutation to form trichloroethanol and trichloroacetate (Newman and Wackett 1991). At least formally, this transformation is analogous to an NIH shift. The particulate enzyme contains

365

Aliphatic Compounds

Hal Hal

C

C

O

Hal

Hal

H

Hal

C

C

Hal H

Hal Hal C Hal Hal Hal

CHO

CH−CO 2H

+

HO 2C−CHO

HCO 2 H + C

O

FIGURE 7.65 Generalized degradation of trihaloethenes by methanotrophs. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

copper, or both copper and iron, and the concentration of copper determines the catalytic activity of the enzyme (Sontoh and Semrau 1998). 2. The degradation of 1,2,3-trichloropropane by Agrobacterium radiobacter strain AD1 involves hydrolysis of an intermediate epichlorohydrin (3-chloroprop-1-ene) to the diol (Bosma et al. 1999, 2002). An enzyme from this strain has been modiied from the use of epichlorohydrin that is its normal substrate to accept cis-1,2-dichloroethene with the release of chloride and the presumptive formation of glyoxal (Rui et al. 2004). 3. The aerobic degradation of chloroethene (vinyl chloride) by Mycobacterium aurum strain L1 proceeded by initial formation of an epoxide mediated by an alkene monooxygenase (Hartmans and de Bont 1992). This reaction has also been demonstrated to occur with Methylosinus trichosporium, even though subsequent reactions were purely chemical (Castro et al. 1992b). 4. The degradation of chloroethene by Mycobacterium sp. strain JS60 involved epoxidation followed by reaction with coenzyme M and loss of chloride in formation of the aldehyde. Subsequent steps involved reductive loss of coenzyme M and the production of acetate (Coleman and Spain 2003) and were analogous to those in Nocardioides sp. strain JS614 (Mattes et al. 2005). The reductive loss of coenzyme M is formally analogous to that involved in the degradation of isoprene by Rhodococcus sp. strain AD45 (van Hylckama Vlieg et al. 2000). The coenzyme M pathway is not limited to Gram-positive organisms and has also been demonstrated in Pseudomonas putida strain AJ and Ochrobactrum sp. strain TD (Danko et al. 2006). Induction of Monooxygenation by Non-Halogenated Substrates

An important observation is the transformation of chlorinated ethenes by monooxygenases induced by a range of “cosubstrates” including toluene, phenol, and methane or propane (references in Kageyama et al. 2005). Advantage has been taken of this for bioremediation of contaminated sites when both aromatic and chlorinated aliphatic contaminants are present. Factors determining the effectiveness of toluene as an inducer of monooxygenase have been examined (Leahy et al. 1996), although strains of Wautersia sp. can degrade trichloroethene in the absence of a cosubstrate (Kageyama et al. 2005). The degradation of trichloroethenes has also been examined by strains in which the relevant dioxygenase has been induced with a range of cosubstrates. These include (a) phenol or benzoate (Nelson et al. 1987), (b) toluene (Wackett and Gibson 1988), (c) isopropylbenzene (Plugmacher et al. 1996), or (d) in a hybrid dioxygenase using elements of the toluene and biphenyl dioxygenase operons (Furukawa et al. 1994). Degradation seems to be limited to trichloroethene and cis-1,2-dichloroethene and the toxicity of the substrates is a limiting factor (Wackett and Gibson 1988). It seems possible that monooxygenation might be involved in view of the demonstrated existence of this activity in naphthalene dioxygenase (Gibson et al. 1995).

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Environmental Degradation and Transformation of Organic Chemicals

Although monooxygenases can be involved in the degradation of toluene, there is a complex relation between toluene monooxygenase activity and the degradation of chlorinated hydrocarbons. Although toluene oxidation is accomplished by Pseudomonas mendocina strain KR1, P. putida strain F1, P. picketii strain PKO1, and Burkholderia cepacia strain G4 that possess toluene monooxygenase activities, the degradation of chloroform and 1,2-dichloroethane is carried out by only strains with the facility of toluene-4-monooxygenation—P. mendocina KR1 and Pseudomonas sp. strain ENVPC5 (McClay et al. 1996). In these strains, toluene oxidation could be induced by trichloroethene, which was subsequently degraded, whereas trichloroethene did not induce toluene oxidation in B. cepacia strain G4 or P. putida strain F1 (McClay et al. 1995). The degradation of trichloroethene by the three components of toluene 2-monooxygenase of B. cepacia involves initial formation of the epoxide followed by spontaneous decomposition to carbon monoxide, formate, and glycolate (Newman and Wackett 1997). In contrast to the degradation by MMO or cytochrome P450 monooxygenase, chloral hydrate was not formed. Reductive Reactions: Dehalogenation Including Dehalorespiration Cytochrome P450 reduction of polyhalogenated alkanes has been demonstrated. For example, cells of Pseudomonas putida G786 containing cytochrome P450cam genes on the CAM plasmid were able to carry out the reductive dehalogenation of a number of halogenated alkanes and for some substrates also oxidations. Illustrative examples include the following: 1. Selective reductive debromination of polyhalogenated methanes (Castro et al. 1985; Li and Wackett 1993). 2. Both aerobic and reductive pathways were suggested for the degradation of 1,1,2-trichloroethane (Castro and Belser 1990)—a dominant aerobic pathway to chloroacetate and glyoxylate, and simultaneously a minor reductive reaction, which must also involve an elimination reaction with the formation of chloroethene (Figure 7.66). 3. Under anaerobic conditions, various reactions can occur, and the following are illustrative: (a) trichloroluoromethane → carbon monoxide; (b) hexachloroethane → tetrachloroethene; (c) 1,1,1-trichloro-2,2,2-triluoroethane → 1,1-dichloro-2,2-diluoroethene (Hur et al. 1994). 4. When a plasmid containing genes encoding toluene dioxygenase was incorporated into this modiied strain of P. putida, complete degradations that involved both reductive and oxidative steps were accomplished, for example, the degradation of pentachloroethane via trichloroethene to glyoxylate, and of 1,1-dichloro-2,2-diluoroethene to oxalate (Wackett et al. 1994). Anaerobic Dehalogenation of Polyhalogenated Alkenes Considerable effort has been devoted to the anaerobic transformation of polychlorinated C1 alkanes and C2 alkenes in view of their extensive use as industrial solvents and their identiication as widely distributed groundwater contaminants. Early experiments, which showed that tetrachloroethene was transformed into chloroethene (Vogel and McCarty 1985) (Figure 7.67), aroused concern; though it has now been shown that complete dechlorination can be accomplished by some organisms.

Cl Cl

Cl CH2 CO2H CH

CH2Cl CH2

CHCl

FIGURE 7.66 Biodegradation of trichloroethane by Pseudomonas putida.

367

Aliphatic Compounds Cl

H C

C

Cl

Cl

Cl C

Cl

C Cl

H

Cl C Cl

H

Cl

C

H C

Cl

H

Cl

H

H

H C

C H

C Cl

CO2

H C

Cl

C Cl

FIGURE 7.67 Anaerobic dechlorination of tetrachloroethene.

The dechlorination of polychlorinated ethenes by a number of bacteria can be coupled to the synthesis of ATP and has been designated dehalorespiration (Holliger et al. 1999; Drzyzga and Gottschal 2002; Sun et al. 2002). Dehalorespiration has been demonstrated in Sulfurospirillum (Dehalospirillum) multivorans, Dehalobacter restrictus, Desulfuromonas chloroethenica, and some strains of Desulitobacterium sp. (references in Holliger et al. 1999), and in Dehalococcoides ethenogenes that is capable of reductively dehalogenating tetrachloroethene to ethene (Magnuson et al. 2000; Maymó-Gatell et al. 1999). The electron donors were generally H2 or pyruvate, or methanol for Dehalococcoides ethenogenes. The chloroethene reductases contain corrinoid cofactors and [Fe–S] clusters, and the trichloroethene reductase from Dehalococcoides ethenogenes is able to debrominate substrates containing two, three, four, or ive carbon atoms, albeit with decreasing ease (Magnuson et al. 2000). Further examples include the following dechlorinations: a. Polychlorinated ethenes to cis-1,2-dichloroethene, chloroethene (vinyl chloride), and ethene or ethane, and of chloroethene (vinyl chloride) to ethene (He et al. 2003; Müller et al. 2004). b. Tetrachloroethene to trans-1,2-dichloroethene (Grifin et al. 2004). c. Tetra- and trichloroethene at the expense of acetate or pyruvate and H2, to cis-dichloroethene by Geobacter lovleyi, which is a relative of Geobacter thiogenes that can couple growth from the dechlorination of trichloroacetate to dichloroacete (Sung et al. 2006). Among organisms that can dechlorinate tetrachloroethene, several types of reductase have been found. In Sulfurospirillum (Dehalospirillum) multivorans, Desulitobacterium sp. strain PCE-S, Desulitobacterium hafniense (frappieri) strain TCE-1, and Dehaloccoides ethenogenes, it consists of a peptide with a single corrinoid cofactor and two [Fe–S] centers. There is considerable interest in the dechlorination of tetrachloroethene and organisms that are able to do so include the following: 1. A strain of Sulfurospirillum (Dehalospirillum) multivorans transformed tetrachloroethene to trichloroethene and cis-1,2-dichloroethene (Neumann et al. 1994) using pyruvate as electron donor, and some properties of the dehalogenase have been reported (Neumann et al. 1995). One mol of the dehalogenase contained 1 mol of corrinoid, 9.8 mol of Fe, and 8.0 mol of acid-labile sulfur (Neumann et al. 1996), and the genes have been cloned and sequenced (Neumann et al. 1998). Although comparable values have been reported for the enzyme from Desulitobacterium sp. strain PCE-S (Miller et al. 1997), the N-terminal sequence of the enzyme showed little similarity to that of Sulfurospirillum multivorans (Miller et al. 1998). The cardinal role of a corrinoid was proposed for both organisms (Neumann et al. 1996; Miller et al. 1997). A comparable reductive dehalogenation— though only as far as trichloroethene—is carried out by Desulfomonile tiedjei in which

368

2.

3.

4. 5. 6.

7.

8.

9.

10.

Environmental Degradation and Transformation of Organic Chemicals

the reductase is a heme protein that is similar to that involved in dehalogenation of 3-chlorobenzoate (Townsend and Sulita 1996). Dehalococcoides ethenogenes is unusual among the dehalorespiring strains in its capability to reductively dehalogenate tetrachloroethene to ethene using methanol as substrate (Magnuson et al. 2000; Maymó-Gatell et al. 1999). It is also capable, though less readily, of reductively dehalogenating a few halogenated propenes including 3-chloropropene and 1,3-dichloropropene with the formation of propene (Magnuson et al. 2000). The membrane-bound dehalogenase from Dehalobacter restrictus contained (per mole of subunit) 1 mol of cobalamin, 0.6 mol cobalt, 7 mol iron, and 6 mol acid-labile sulfur. It carried out dechlorination of tetra- and trichloroethene to cis-1,2-dichloroethene, and had a substrate spectrum that included tetrachloromethane, hexachloroethane, and 1,1,1trichloro-2,2,2-triluorarethane although the products from these were not apparently identiied (Maillard et al. 2003). Two strains of Desulfuromonas michiganensis carried out the partial dechlorination of tetrachloroethene to cis-1,2-dichloroethene using acetate as the electron donor (Sung et al. 2003). The reduction of tetrachloroethene to cis-1,2-dichloroethene by the enteric organism Pantoea (Enterobacter) agglomerans may be noted (Sharma and McCarty 1996) as one of the few examples of the ability of Enterobacteriaceae to carry out reductive dechlorination. A nonfermentative organism putatively assigned to Desulfuromonas acetexigens reduced tetrachloroethene to cis-dichloroethene using acetate as electron donor (Krumholz et al. 1996), and a similar species D. chloroethenica used both tetra- and trichloroethene as electron acceptors with the production of cis-dichloroethene using acetate or pyruvate as electron donors (Krumholz 1997). Clostridium bifermentans can dechlorinate tetrachloroethene to cis-dichloroethene (Chang et al. 2000; Okeke et al. 2001). The enzyme has been puriied and contains a corrinoid cofactor, although the complete nucleotide sequence of the gene encoding the reductase showed no homology with existing dehalogenases. The enzyme was most active with tetrachloroethene and trichloroethene, although lower rates were also observed with other chlorinated ethenes except chloroethene (vinyl chloride). Under methanogenic conditions, a strain of Methanosarcina sp. transformed tetrachloroethene to trichloroethene (Fathepure and Boyd 1988). In the presence of suitable electron donors such as methanol, complete reduction of tetrachloroethene to ethene may be achieved in spite of the fact that the dechlorination of vinyl chloride appeared to be the rate-limiting step (Freedman and Gossett 1989). Tetrachloroethene can be dechlorinated to trichloroethene as the sole product by the homoacetogen Sporomusa ovata using methanol as the electron donor, and cell extracts of other homoacetogens including Clostridium formicoaceticum and Acetobacterium woodii were able to carry this out using CO as electron donor (Terzenbach and Blaut 1994). Complete dechlorination of high concentrations of tetrachloroethene in the absence of methanogenesis has been achieved using methanol as electron donor (DiStefano et al. 1991).

There has been substantial interest in the complete dechlorination of chloroethene to ethene, since chloroethene is an undesirable product of partial dechlorination of polychlorinated ethenes. Strains of Dehalococcoides sp., and especially D. ethenogenes that is possibly unique in being able to carry out the dechlorination of tetrachloroethene to chloroethene and ethene (Magnuson et al. 2000; Maymó-Gatell et al. 1999), have attracted particular attention: a. It has been shown that the gene bvcA that is putatively involved in the reduction of chloroethene to ethene by Dehalococcoides sp. strain BAC1 was present in strains that could

369

Aliphatic Compounds BrCH2CH2Br BrCH

CH2 CH2

CHBr

HC

BrCH2CH2SO3H

CH

CH2 CH2

FIGURE 7.68 Reductive debromination by methanogenic bacteria. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

Cl

Cl

Cl

Cl

Cl

Cl

Cl Cl

Cl

Cl ;

Cl

Cl Cl

Cl Cl

Cl

FIGURE 7.69 Biotransformation of γ-hexachlorocyclohexene and γ-1,3,4,5,6-pentachlorocyclohexene. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, pp. 1–74, Springer, 2002. With permission.)

carry out chloroethene respiration, but was absent in those that could not (KrajmalnikBrown et al. 2004). b. The genes for the reductase designated vcrAB were detected at sites with established chloroethene contamination and it was suggested that this could serve as monitoring probe (Müller et al. 2004). Further examples include the debromination of 1,2-dibromoethane to ethene, and 1,2-dibromoethene to ethyne by methanogenic bacteria (Figure 7.68) (Belay and Daniels 1987). Details of these dehalogenations have emerged from studies with methanogens. The formation of ethene from 1,2-dichloroethane using hydrogen as electron donor has been demonstrated in cell extracts of Methanobacterium thermoautotrophicum DH and in Methanosarcina barkeri has been shown to involve cobalamin and F430 using Ti(III) as reductant (Holliger et al. 1992). Some additional comments on abiotic reactions are given in Chapter 1. Other Substrates 1. Reductive dehalogenation is one of the series of reactions involved in the degradation of γ-HCH (aaaeee) (Nagata et al. 1999): (a) initial elimination catalyzed by LinA, (b) hydrolysis by LinB, and (c) glutathione-mediated reductive loss of chloride from 2,5-dichlorohydroquinone catalyzed by LinD, which has already been noted (Figure 7.53) The last reaction also occurs during the degradation of pentachlorophenol (Xun et al. 1992). 2. Reductive dechlorination in combination with the elimination of chloride has been demonstrated in a strain of Clostridium rectum (Ohisa et al. 1982): γ-hexachlorocyclohexene formed 1,2,4-trichlorobenzene and γ-1,3,4,5,6-pentachlorocyclohexene formed 1,4dichlorobenzene (Figure 7.69). It was suggested that this reductive dechlorination is coupled to the synthesis of ATP, and this possibility has been clearly demonstrated during the dehalogenation of 3-chlorobenzoate coupled to the oxidation of formate in Desulfomonile tiedjei (Mohn and Tiedje 1991). Combined reduction and elimination has also been demonstrated in methanogenic cultures that transform 1,2-dibromoethane to ethene and 1,2dibromoethene to ethyne (Belay and Daniels 1987).

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Environmental Degradation and Transformation of Organic Chemicals

3. Both the active enzyme, the heat-inactivated enzyme from Sulfurospirillum (Dehalospirillum) multivorans, and cyanocobalamin are capable of dehalogenating haloacetates (Neumann et al. 2002), and the rate of abiotic dehalogenation depends on the catalyst that is used. 4. An organism that is able to use methyl chloride as energy source and converting this into acetate has been isolated (Traunecker et al. 1991). 5. Cultures of a number of anaerobic bacteria are able to dechlorinate tetrachloromethane and Acetobacterium woodii formed dichloromethane as the inal chlorinated metabolite by successive dechlorination, although CO2 was also produced by an unknown mechanism (Egli et al. 1988). 6. A strain of Clostridium sp. transformed 1,1,1-trichloroethane to 1,1-dichloroethane, and tetrachloromethane successively to trichloromethane and dichloromethane (Gälli and McCarthy 1989). 7. Although dichloromethane is a terminal metabolite in some transformations, an organism assigned to Dehalobacterium formicoaceticum is able to use this as a source of carbon and energy (Mägli et al. 1996). Dichloromethane was converted into methylenetetrahydrofolate from which formate is produced by oxidation and acetate by incorporation of CO2 catalyzed by CO dehydrogenase and acetyl-coenzyme A synthase. 8. Toxaphene is a complex mixture of compounds prepared by chlorinating camphene, and contains several hundred polychlorinated bornanes. After incubation with Sulfurospirillum (Dehalospirillum) multivorans only the hexa- (B6-923) and the heptachlorinated (B7-1001) remained. The nonachlorinated congener B9-1679 could be transformed by preferential dechlorination of the gem-dichloro groups with formation of the heptachlorinated B7-1001 (Ruppe et al. 2003). Further examination showed that this congener could be dechlorinated to penta- and hexachlorinated bornanes (Ruppe et al. 2004).

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Aliphatic Compounds

377

Traunecker J, A Preub, G Diekert (1991) Isolation and characterization of a methyl chloride utilizing, strictly anaerobic bacterium. Arch Microbiol 156: 416–421. Tu CM (1976) Utilization and degradation of lindane by soil microorganisms. Arch Microbiol 108: 259–263. van den Wijngaard AJ, PTW Reuvenkamp, DB Janssen (1991) Puriication and characterization of haloalcohol dehalogenase from Arthrobacter sp. strain AD2. J Bacteriol 173: 124–129. van den Wijngaard, AJ, DB Janssen, B Withold (1989) Degradation of epichlorohydrin and halohydrins by bacterial cultures isolated from freshwater sediment. J Gen Microbiol 135: 2199–2208. van den Wijngaard, AJ, J Prins, AJAC Smal, DB Janssen (1993) Degradation of 2-chloroethylvinyl ether by Ancylobacter aquaticus AD25 and AD27. Appl Environ Microbiol 59: 2777–2783. van den Wijngaard, AJ, KWHJ van der Kamp, J van der Ploeg, F Pries, B Kazemier, DB Janssen (1992) Degradation of 1,2-dichloroethane by Ancyclobacter aquaticus and other facultative methylotrophs. Appl Environ Microbiol 58: 976–983. van der Ploeg, M Willemsen, G van Hall, DB Janssen (1995) Adaptation of Xanthobacter autotrophicus GJ10 to bromoacetate due to activation and mobilization of the haloacetate dehalogenase gene by insertion element IS1247. J Bacteriol 177: 1348–1356. van Hylckama Vlieg JET, H Leemhuis, JHL Spelberg, DB Janssen (2000) Characterization of the gene cluster involved in isoprene metabolism in Rhodococcus sp. strain AD45. J Bacteriol 182: 1956–1963. van Hylckama Vlieg JET, J Kingma, AJ van den Wijngaard, DB Janssen (1998) A gluathione S-transferase with activity towards cis-1,2-dichloroepoxyethane is involved in isoprene utilization by Rhodococcus strain AD 45. Appl Environ Microbiol 64: 2800–2805. van Hylckama Vlieg JET, J Kingma, W Kruizinga, DB Janssen (1999) Puriication of a glutathione S-transferase and a glutathione conjugate-speciic dehydrogenase is involved in isoprene metabolism by Rhodococcus sp. strain AD 45. J Bacteriol 181: 2094–2101. Vannelli T, M Logan, DM Arciero, AB Hooper (1990) Degradation of halogenated aliphatic compounds by the ammonia-oxidizing bacterium Nitrosomonas europaea. Appl Environ Microbiol 56: 1169–1171. Vannelli T, M Messmer, A Studer, S Vuilleumier, T Leisinger (1999) A corrinoid-dependent catabolic pathway for growth of a Methylobacterium strain with chloromethane. Proc Natl Acad Sci USA 96: 4615–4620. Verschuren KHG, F Seljée, HJ Rozeboom, KH Kalk, BW Dijkstra (1993) Crystallographic analysis of the catalytic mechanism of haloalkane dehalogenase. Nature 363: 693–698. Vogel TM, PL McCarty (1985) Biotransformation of tetrachloroethylene to trichloroethylene, dichloroethylene, vinyl chloride, and carbon dioxide under methanogenic conditions. Appl Environ Microbiol 49: 1080–1083. Wackett LP, DT Gibson (1988) Degradation of trichloroethylene by toluene dioxygenase in whole-cell studies with Pseudomonas putida F1. Appl Environ Microbiol 54: 1703–1708. Wackett LP, MJ Sadowsky, LM Newman, H-G Hur, S Li (1994) Metabolism of polyhalogenated compounds by a genetically engineered bacterium. Nature 368: 627–629. Wahman DG, LE Katz, GE Speitel (2005) Cometabolism of trihalomethanes by Nitrosomonas europaea. Appl Environ Microbiol 71: 7980–7986. Wedemeyer G (1967) Dechlorination of 1,1,1-trichloro-2,2-bis[p-chlorophenyl]ethane by Aerobacter aerogenes. I. Metabolic products. Appl Microbiol 15: 569–574. Willett KL, EM Ulrich, RA Hites (1998) Differential toxicity and environmental fates of hexachlorocyclohexane isomers. Environ Sci Technol 32: 2197–2207. Wischnak C, FE Löfler, J Li, JW Urbance, R Müller (1998) Pseudomonas sp. strain 273, an aerobic α,ωdichloroalkane-degrading bacterium. Appl Environ Microbiol 64: 3507–3511. Woodall CA, KL Warner, RS Oremland, JC Murrell, IR McDonald (2001) Identiication of methyl halideutilizing genes in the methyl bromide-utilizing bacterial strain IMB-1 suggests a high degree of conservation of methyl halide-speciic genes in Gram-negative bacteria. Appl Environ Microbiol 67: 1959–1963. Xun L, E Topp, CS Orser (1992) Diverse substrate range of a Flavobacterium pentachlorophenol hydroxylase and reaction stoichiometries. J Bacteriol 174: 2898–2902. Yu P, T Welander (1995) Growth of an aerobic bacterium with trichloroacetic acid as the sole source of energy and carbon. Appl Microbiol Biotechnol 42: 769–774.

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PART 4 FLUORINATED ALIPHATIC COMPOUNDS There has been increase in the application of these compounds since the synthesis of luorinated alkanes and related compounds in the 1930s. These include luorinated hydrocarbons that were formerly used as propellants, polymerized tetraluoroethene, and the polyluorinated C4 –C8 carboxylates and sulfonates. All of them are notable for their inertness under normal conditions. Aromatic luorinated compounds are discussed in Chapter 9, Part 3.

ALKANES AND ALKENES The biodegradation of hydrochloroluorocarbons and hydroluorocarbons has attracted considerable attention on account of their presumptive adverse effect on ozone depletion and climate alteration (references in Fabian and Singh 1999). Valuable background on chloroluorocarbons has been given (Elliott 1994) and on alternatives to them (Rao 1994). The perluorinated compounds including diluoromethane (HFC-32), triluoroethane (HFC-143a), tetraluoroethane (HFC-134a), hexaluoropropane (HFC-236ea), and heptaluoropropane (HFC-227ea) are, however, of potential interest as environmentally acceptable (Harnisch 1999). A list of acronyms is given in Table 7.3 (Midgley and McCulloch 1999). Further details of their degradation are given in a review (Neilson and Allard 2002). Fluorohydrocarbons Fluoromethane has been used as a selective inhibitor of ammonium oxidation and nitriicationlinked synthesis of N2O in Nitrosomonas europaea (Miller et al.1993), while diluoromethane has been proposed as a reversible inhibitor of methanotrophs (Miller et al. 1998). Monooxygenation is distributed among a variety of bacteria and several have been examined for their potential to degrade luorinated alkanes: 1. Ammonia monooxygenase in Nitrosomonas europaea is able to oxidize luoromethane to formaldehyde (Hyman et al. 1994). 2. The methanotroph Methylosinus trichosporium strain OB3b that produces the soluble MMO system consisting of a 40 kDa NADH oxidoreductase, a 245 kDa hydroxylase, and a 16 kDa protein termed component B has a low substrate speciicity (Sullivan et al. 1998). It has been shown to metabolize triluoroethene to glyoxylate, diluoroacetate, and the rearranged product triluoroacetaldehyde (Fox et al. 1990). The last reaction is analogous to the formation of trichloroacetaldehyde from trichloroethene by the same strain (Oldenhuis et al. 1989).

TABLE 7.3 Acronyms for chlorofluorocarbons (CFCs), hydrochlorofluorocarbons (HCFCs), and hydrofluorocarbons (HFCs) Acronym CFC-11 CFC-12 CFC-113 CFC-114 CFC-115

Structure CCl3F CCl2F2 CCl2F–CClF2 CClF2–CClF2 CClF3–CF3

Acronym HCFC-123 HCFC-22 HCFC-141b HCFC-142b HCFC-124 HCFC-225ca HCFC-225cb

Structure CHCl2–CF3 CHClF2 CH3–CCl2F CH3–CClF2 CHClF–CF3 CHCl2–CF2–CF3 CHFCl–CF2–CF3Cl

Acronym HFC-134a HFC-227ea HFC-152a HFC-143a HFC-125 HFC-32 HFC-23 HFC-245ca

Structure CH2F–CF3 CF3–CHF–CF3 CH3–CHF2 CH3–CF3 CHF2–CF3 CH2F2 CHF3 CHF2–CF2–CH2F

379

Aliphatic Compounds

3. This strain and Mycobacterium vaccae strain JOB 5 that produces propane monooxygenase has been used to examine the degradation of a number of hydrochloroluorocarbons and hydroluorocarbons (Streger et al. 1999). It was shown that during complete degradation by M. trichosporium and M. vaccae, this was accompanied by release of luoride. It is worth noting, however, that the methylotrophs IMB-1 (Schaefer and Oremland 1999) and CC495 (Coulter et al. 1999) are able to oxidize chloromethane, bromomethane, and iodomethane, though not luoromethane. On the basis of their 16S rRNA sequences, these organisms are related to those classiied as Pseudaminobacter sp., and more distantly related to the nitrogen-ixing rhizobia (Coulter et al. 1999). Chlorofluorocarbons and Hydrochlorofluorocarbons In general, halogen is last from organic substrates in the order I > Br > Cl > F. Considerable effort has been directed to degradation and transformation by methylotrophic bacteria. As a generalization, the HCFCs are more readily degraded that the corresponding compounds lack hydrogen. The soluble MMO from Methylosinus trichosporium OB3b that has a wide substrate spectrum is able to oxidize some hydrochloroluoroethanes including 1,1,2-trichloro-2-2-luororethane and 1,1,2-triluoroethane, though neither trichloroluoromethane (CFC-11) nor any hydrochloroluoroethane with three luorine substituents on the same carbon atom were oxidized (DeFlaun et al. 1992). Although quantitative loss of luoride and chloride was shown for dichloroluoromethane, none of the organic products of oxidation were identiied for the others. Reductive dechlorination of luorinated substrates has been observed for both methanogens and sulfate-reducing bacteria. 1. The methanogen Methanosarcina barkeri is able to transform trichloroluoromethane (CFC-11) by successive loss of chlorine to produce chloroluoromethane (Figure 7.70a) (Krone and Thauer 1992). A similar transformation has been demonstrated in the presence of sulfate and butyrate with a mixed culture containing putatively Desulfovibrio baarsii and Desulfobacter postgatei (Sonier et al. 1994). 2. In anaerobic microcosms, 1,1,2-trichloro-1,2,2-triluoroethane (CFC-113) was transformed by successive reductive dechlorination to 1,2-dichloro-1,2,2-triluoroethane (HCFC-123a), and under methanogenic conditions to 1-chloro-1,2,2-triluoroethane (HCFC-133) and 1-chloro-1,1,2-triluoroethane (HCFC-133b) without evidence for the reductive replacement of luorine (Figure 7.70b) (Lesage et al. 1992). 3. 1,1,1-Triluoro-2,2-dichloroethane (HCFC-123) was recalcitrant in aerobic soils, but underwent reductive dechlorination anaerobically to produce 1,1,1-triluoro-2-chloroethane (Oremland et al. 1996). Cytochrome P450cam is a monooxygenase that can be induced in Pseudomonas putida G786 by growth on camphor, and is responsible for the introduction of a hydroxyl group at C5 as the irst step in the degradation of camphor. This enzyme is also able to carry out nonphysiological reductive dehalogenation (Castro et al.1985), and it has been shown (Li and Wackett 1993) that the electrons for reduction can be supplied by putidaredoxin. These alternatives are summarized: Monooxygenation Reductive dehalogenation

R–H + O2 + 2H+ + 2e → R–OH + H2O R–Hal + 2H+ + 2e → R–H + H–Hal

The production of carbon monoxide from trichloroluoromethane catalyzed by cytochrome P450cam proceeded through intermediate formation of the dichloroluorocarbene (Li and Wackett 1993) (Figure 7.70c). Other reactions included β-elimination from 1,1,1-trichloro-2,2,2-triluorethane (Figure 7.70c). Pseudomonas putida strain G786 (pGH-2) was constructed to contain both the

380

Environmental Degradation and Transformation of Organic Chemicals

Cl (a) Cl Cl

C

F

Cl (b) Cl F

C

C

Cl (c) Cl Cl

C

F

Cl Cl Cl

C

C

Cl H H

Cl F F

C

F

Cl F H

C

Cl Cl

F F

C

C

Cl

F C

F + H F

F

C F

H

CO

H

F

F F

[ Cl2 CF ]

H

Cl F H

Cl C

F C

C

F

Cl F

C

C F

Cl

F

FIGURE 7.70 (a) Metabolism of trichloroluoromethane by Methanosarcina barkeri, (b) transformation of 1,1,2-trichloro-1,2,2-triluoroethane (CFC-113) under anaerobic conditions, (c) dehalogenation by cytochrome P450cam of trichloroluoromethane and 1,1,1-trichloro-2,2,2-triluoroethane. Cl

Cl Cl Cl

C

C

F F

(a)

F

Cl C

C

+

Cl

F

Cl

Cl

Cl C H

C

F F

(b) HO2C−CO2H

(a) anaerobic,

(b) aerobic

FIGURE 7.71 Combined dehalogenation of 1,1,1,2-tetrachloro-2,2-diluoroethane by cytochrome P450cam and oxidation with toluene 2,3-dioxygenase.

cytochrome P450cam genes on the CAM plasmid and the tod C1, tod C2, tod b, and tod A genes of toluene dioxygenase. Toluene dioxygenase was constitutively expressed and cytochrome P450cam after induction by camphor (Wackett et al. 1994). Under anaerobic conditions 1,1,1,2-tetrachloro2,2-diluoroethane was dehalogenated to 1,1-chloro-2,2-diluoroethene that could be oxidized by the dioxygenase under aerobic conditions to oxalate (Figure 7.71) (Hyman et al. 1994). Carboxylic Acids Fluorinated aliphatic carboxylic acids are produced by some plants including species of Dichapetalum (Gribble 2002), and several mechanisms have been suggested for the biosynthesis of luorinated metabolites (Harper et al. 2003). The mechanism of luoroacetate toxicity in mammals has been extensively examined and was originally thought to involve simply initial synthesis of luorocitrate that inhibits aconitase and thereby functioning the TCA cycle. Walsh has extensively reinvestigated the problem, and revealed both the complexity of the mechanism of inhibition and the stereospeciicity of the formation of luorocitrate from luoroacetate (Walsh 1982).

381

Aliphatic Compounds CO 2 H

F

CO 2 H F

F

O

HO 2C

CO 2H

OH

CH(F)CO 2 H CO 2H

OH

NO 2

O

CO 2H

F O

CO 2 H CO 2 H

FIGURE 7.72

+

Degradation of 2-luoro-4-nitrobenzoate by Nocardia erythropolis.

Fluoroacetate As might be expected, bacteria have been isolated from the plants that produce luoroacetate, and these include an unidentiied Pseudomonas sp. (Goldman 1965), a strain of Burkholderia (Pseudomonas) cepacia from Dichapetalum cymosum (Meyer et al. 1990), and a strain of Moraxella sp. (Kawasaki et al. 1981). In addition, luoroacetate is an unusual product of microbial metabolism: a. It is a terminal metabolite formed during the metabolism of 2-luoro-4-nitrobenzoate by Nocardia erythropolis (Figure 7.72) (Cain et al. 1968). b. It is formed together with 4-luorothreonine during the late-stage growth of Streptomyces cattleya on a deined medium in the presence of luoride (Reid et al. 1995). It has been shown (Hamilton et al. 1998) that glycine is an effective precursor of both luoroacetate and 4-luorothreonine, and that glycine is metabolized via N5,N10 -methylenetetrahydrofol ate to serine and thence to pyruvate. However, details of the mechanism for the incorporation of luoride remain incompletely resolved. The metabolism of luoroacetate results in the production of luoride and glycolate, and the use of H218O showed that the oxygen atom was introduced from water by a hydroxylase (Goldman 1966). The enzyme has been puriied from the unidentiied pseudomonad (Goldman 1965), and is speciic for luoroacetate: it is inactive towards 2- and 3-luoropropionate, di- and triluoroacetates, and luorobenzoates. It is rapidly inhibited by 4-chloromercuriphenylsulfonate and slowly by N-methylmaleimide, and this suggests the involvement of an active thiol group in the enzyme. Strains of Moraxella sp. have also been shown to assimilate luoroacetate using plasmid-determined dehalogenase activities (Kawasaki et al. 1981). One of these (strain H-1) was active towards both luoroacetate and chloroacetate, whereas the other (strain H-2) was active only towards chloroacetate. Further investigation (Au and Walsh 1984) of the haloacetate hydrolase H-1 from Pseudomonas sp. strain A used 1H NMR of the (−)-α-methoxyl-α-(triluoromethyl) phenylacetic acid ester of the phenacyl ester of the glycolate produced from (S)-2-[2H1]luoroacetate. This established that the major metabolite was the (R)-enantiomer of 2-[2H1]glycolate and that the reaction proceeded with inversion of the coniguration at C-2. The mechanism for the hydrolysis of luoroacetate by Moraxella sp. strain B has been examined and conirmed the involvement of Asp105 as nucleophile with inversion of the coniguration at C2 (Liu et al. 1998). Di- and Trifluoroacetate The soluble MMO from Methylsosinus trichosporium OB3 produced diluoroacetate as one of the main products from the oxidation of triluoroethene and a low yield of triluoroacetaldehyde by rearrangement (Fox et al. 1990).

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Environmental Degradation and Transformation of Organic Chemicals

Chlorodiluoroacetic acid has been identiied in rain and snow samples (Martin et al. 2000) and may plausibly be an atmospheric degradation product of 1,1,2-trichloro-1,2,2-triluoroethane. Triluoroacetate has been found in a wide range of environmental samples (Key et al. 1997), and attention has been directed to its origin, its toxicity, and its recalcitrance. Compared with chloroacetates, however, it is only mildly phytotoxic to algae (Berends et al. 1999) and higher plants (Boutonnet et al. 1999). It is worth noting its formation during the photochemical degradation of 3-triluoromethyl-4-nitrophenol (Ellis and Mabury 2000). Concern has been expressed over its biodegradability and conlicting results over its recalcitrance under anaerobic conditions have been reported. This has been resolved by the results of a chemostat study using a mixed ethanol-degrading culture (Kim et al. 2000). Clear evidence for anaerobic degradation was produced on the basis of luoride release and formation of acetic acid and methane. Perfluoroalkyl Carboxylates and Sulfonates There has been increasing interest in perluoroalkyl sulfonates and carboxylates (Key et al. 1997). The sulfonates are valuable surface protectors and surfactants under extreme conditions, and are components of ire ighting foams (Moody and Field 2000). Perluorooctane carboxylates and sulfonates have a global distribution in wildlife and humans (Houde et al. 2006). Low levels of perluoro compounds have been carefully quantiied in samples of human sera (Hansen et al. 2001) and determination of perluorinated surfactants in surface water samples has been described. Two independent analytical techniques—liquid chromatography/tandem mass spectrometry and 19F NMR were used—and a summary of analytical methods was included (Moody et al. 2001). References to toxicological studies in rats and epidemiological studies in man have been given (Hansen et al. 2001), and the biochemical toxicology of the related perluorooctanoic acid has been discussed (DePierre 2002). Concern with their apparent persistence has motivated investigations of their potential sources including luorotelomer alcohols. A strain of Pseudomonas sp. strain D2 was used to evaluate the degradation of a range of luorinated sulfones (Key et al. 1998). Although the fully luorinated perluorooctane sulfonate was resistant to deluorination by an aerobic bacterium, the presence of hydrogen substituents in 1H,1H,2H,2H-perluorooctane sulfonate made it possible for the organism to carry out partial deluorination. For growth and deluorination of diluoromethane sulfonate, acetate or glucose were supplied as the source of carbon, ammonium as the source of nitrogen, and the substrate as the source of sulfur. It should be noted that perluoro analogs that lacked hydrogen substituents did not support growth of this strain. These considerations apply also to the luorotelomer alcohol CF3(CF2)7–CH2CH2OH that was degraded in a mixed culture obtained by enrichment with ethanol. Terminal dehydrogenation followed by elimination of luoride, hydration and further loss of luoride produced perluorooctanoate (Dinglasan et al. 2004). CF3(CF2)7CH2–CH2OH → CF3(CF2)7CH2CO2H → CF3(CF2)6 –CF=CHCO2H → CF3(CF2)6COCH2CO2H → CF3(CF2)6CO2H An exhaustive study with activated municipal sludge using the telomer alcohol labeled with 14C at the terminal CF2 established the formation of a range of products that involved ission of several C–F bonds (Wang et al. 2005). Perluorooctanoate is also formed during simulated atmospheric reactions of the luorotelomer alcohol (Ellis et al. 2004) and it is suggested that all these reactions are the possible sources of perluorocarboxylic acids.

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Liu J-Q, T Kurihara, S Ichiyama, M Miyagi, S Tsunasawa, H Kawasaki, K Soda, N Esaki (1998) Reaction mechanism of luoroacetate dehalogenase from Moraxella sp. B. J Biol Chem 273: 30897–30902. Martin JW, J Franklin, ML Hanson, KR Solomon, SA Mabury, DA Ellis, BF Scott, and DCG Muir (2000) Detection of chlorodiluoroacetic acid in precipitation: a possible product of luorocarbon degradation. Environ Sci Technol 34: 274–281. Meyer JJM, N Grobbelaar, PL Steyn (1990) Fluoroacetate-metabolizing pseudomonad isolated from Dichapetalum cymosum. Appl Environ Microbiol 56: 2152–2155. Midgley PM, A McCulloch (1999) Properties and applications of industrial halocarbons. In Reactive Halogen Compounds in the Atmosphere (Eds P Fabian and ON Singh). Springer, Berlin. Miller LG, C Sasson, RS Oremland (1998) Diluoromethane, a new and improved inhibitor of methanotrophy. Appl Environ Microbiol 64: 4357–4362. Miller LG, MD Coutlakis, RS Oremland, BB Ward (1993) Selective inhibition of ammonium oxidation and nitriication-linked N2O formation by methyl luoride and dimethyl ether. Appl Environ Microbiol 59: 2457–2464. Moody CA, JA Field (2000) Perluorinated surfactants and environmental implications of their use in i reighting foams. Environ Sci Technol 34: 3864–3870. Moody CA, WC Kwan, JW Martin, DCG Muir, SA Mabury (2001) Determination of perluorinated surfactants in surface water samples by two independent analytical techniques: liquid chromatography/ tandem mass spectrometry and 19F NMR. Anal Chem 73: 2200–2206. Neilson AH, A-S Allard (2002) Degradation and transformation of organic luorine compounds. Handbook Environ Chem 3N: 138–202. Oldenhuis R, RLJM Vink, DB Janssen, B Witholt (1989) Degradation of chlorinated aliphatic hydrocarbons by Methylosinus trichosporium OB3b expressing soluble methane monooxygenase. Appl Environ Microbiol 55: 2819–2826. Oremland RS, DJ Lonrergan, CW Culbertson, DR Lovley (1996) Microbial degradation of hydrochloroluorocarbons (CHCl2F and CHCl2CF3) in soils and sediments. Appl Environ Microbiol 62: 1818–1821. Rao VNM (1994) Alternatives to chloroluorocarbons (CFCs). In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, and JC Tatlow), pp. 159–175. Plenum Press, New York. Reid KA, JTG Hamilton, RD Bowden, DO′Hagan, L Dasaradhi, MR Amin, DB Harper (1995) Biosynthesis of luorinated secondary metabolites by Streptomyces cattleya. Microbiology (UK) 141: 1385–1393. Schaefer JK, RS Oremland (1999) Oxidation of methyl halides by the facultative methylotroph strain IMB-1. Appl Environ Microbiol 65: 5035–5041. Sonier DN, NLDuran, GB Smith (1994) Dechlorination of trichloroluoromethane (CFC-11) by sulfatereducing bacteria from an aquifer contaminated with halogenated aliphatic compounds. Appl Environ Microbiol 60: 4567–4572. Streger SH, CW Condee, AP Togna, MF Delaun (1999) Degradation of halohydrocarbons and brominated compounds by methane- and propane-oxidizing bacteria. Environ Sci Technol 33: 4477–4482. Sullivan JP, D Dickinson, HA Chase (1998) Methanotrophs, Methylosinus trichosporíum OB3b, sMMO, and their application to bioremediation. Crit Rev Microbiol 24: 335–373. Wackett LP, M J Sadowsky, LM Newman, H-G Hur, S Li (1994) Metabolism of polyhalogenated compounds by a genetically engineered bacterium. Nature (London) 368: 627–629. Walsh C (1982) Fluorinated substrate analogs: routes of metabolism and selective toxicity. Adv Enzymol 55: 187–288. Wang N, B Szostek, RC Buck, PW Folsom, LM Sulecki, V Capka, , MR Berti, JT Gannon (2005) Fluorotelomer alcohol biodegradation—direct evidence that perluorinated carbon chains breakdown. Environ Sci Technol 39: 7516–7628.

Aromatic 8 Carbocyclic Compounds without Halogen Substituents Before the advent of the petrochemical industry carbocyclic aromatic compounds, such as naphthalene, phenol, and pyridine, provided the source of many important industrial chemicals including dyestuffs, while the monocyclic compounds continue to play an important role as fuels and starting materials.

PART 1 MONOCYCLIC AROMATIC HYDROCARBONS INTRODUCTION The degradation of aromatic compounds including hydrocarbons and phenols has attracted interest over many years, for several reasons: 1. They are components of unreined oil, and there has been serious concern over the hazard associated with their discharge into the marine environment after accidents at sea. 2. A number of the polycyclic representatives have been shown to be human procarcinogens that require metabolic activation. 3. There has been increased concern over air pollution as a result of their presence in the atmosphere from incomplete combustion. 4. The corresponding phenols are signiicant components of creosote and tar, which have traditionally been used for wood preservation. Although aerobic growth at the expense of aromatic hydrocarbons has been known for many years (Söhngen 1913; Tausson 1927; Gray and Thornton 1928), it was many years later before details of the ring-ission reactions began to emerge. Two converging lines of investigations have examined them in detail: (a) the degradation of the monocyclic aromatic hydrocarbons benzene, toluene, and the xylenes and (b) the degradation of oxygen-substituted compounds such as benzoate, hydroxybenzoates, and phenols. As a result of this activity, the pathways of degradation and their regulation are now known in considerable detail, and ever-increasing attention has been directed to the degradation of polycyclic aromatic hydrocarbons. Since many of these metabolic sequences recur in the degradation of a wide range of aromatic compounds, a brief sketch of the principal reactions may conveniently be presented here. Reviews that include almost all aspects have been given, for example, by Hopper (1978), Cripps and Watkinson (1978), Ribbons and Eaton (1982), Gibson and Subramanian (1984), Smith (1996), and Neilson and Allard (1998). In addition, developments in regulatory aspects have been presented in Rothmel et al. (1991), van der Meer et al. (1992), and Parales and Harwood (1993).

MONOCYCLIC ARENES Aerobic Conditions It is important at the outset to appreciate two important issues. 1. For complete degradation of an aromatic hydrocarbon to occur, it is necessary that the products of ring oxidation and ission can be further degraded to molecules that enter anabolic and energy-producing reactions. 385

386

Environmental Degradation and Transformation of Organic Chemicals H

OH OH H

(a) H

(b)

OH H OH

FIGURE 8.1 Alternative pathways for the oxidative metabolism of naphthalene by (a) bacteria and (b) fungi. CO2H

OH

OH

OCH3

OCH3

OH

OH

OH

O

O O

O

OH

CO2H CO2H

CO2H CO2H

OH

FIGURE 8.2 Biodegradation of vanillic acid by fungi.

2. Essentially different mechanisms operate in bacteria and fungi, and these differences have important consequences. In bacteria, the initial reaction is carried out by dioxygenation and results in the synthesis of a cis-1,2-dihydro-1,2-diol, which is then dehydrogenated to a catechol before ring ission mediated by dioxygenases. However, in fungi, the irst reaction is monooxygenation to an epoxide followed by hydrolysis to a trans-1,2-dihydro-1,2-diol and rearrangement to a phenol. Ring ission of polycyclic aromatic hydrocarbons does not generally occur in fungi, so that these reactions are essentially biotransformations. These reactions are schematically illustrated in Figure 8.1. 3. However, both fungi and yeasts are able to degrade simpler substituted aromatic compounds such as 3,4-dihydroxybenzoate (Cain et al. 1968), which can be produced as intermediates. The pathways that are used differ from those used by bacteria. Two examples are given, both of which involve concomitant hydroxylation and decarboxylation: (a) the degradation of 3,4dihydroxybenzoate by the yeast Trichosporon cutaneum produces 1,2,4-trihydroxybenzene prior to ring ission (Anderson and Dagley 1980), and (b) the pathway used for vanillate (Figure 8.2) (Ander et al. 1983). The oxidative decarboxylation of a range of 4-hydroxybenzoates to 1,4-dihydroxy compounds has been examined in yeasts, and is carried out by an FAD-dependent monooxygenase in Candida parapsilosis CBS604 (Eppink et al. 1997). Benzene Benzene is one of a group of related aromatic monocyclic hydrocarbons (BTEX—benzene, toluene, ethylbenzene, and xylene), and since these are water soluble, there has been concern for their dissipation and persistence in groundwater under both aerobic and anaerobic conditions. Although aerobic growth at the expense of benzene was established many years ago, the pathway for its degradation was established only much later. The aerobic degradation of benzene by bacteria is

Carbocyclic Aromatic Compounds without Halogen Substituents

387

initiated by formation of a cis-dihydrodiol, followed by dehydrogenation to catechol (Gibson et al. 1968). In a strain of Moraxella sp., subsequent intradiol ission by catechol-1,2-dioxygenase produced muconate that was degraded by the 3-ketoadipate pathway to succinate and acetate (Högn and Jaenicke 1972). In other organisms including Pseudomonas putida, extradiol ring ission by catechol-2,3-dioxygenase produced 2-hydroxymuconate semialdehyde that was degraded to pyruvate and acetaldehyde. Formation of the dihydrodiol in a mutant strain of Pseudomonas putida involves incorporation of both atoms of 18O2 (Gibson et al. 1970). It is mediated by a dioxygenase that has been puriied and shown to be a soluble enzyme consisting of three protein components (Axcell and Geary 1975) encoded by the genes bedA, bedB, and bedC. A lavoprotein reductaseBED containing FAD accepts electrons from NADH and transfers them to a [2Fe–2S] Rieske ferredoxinBED, while the terminal oxygenase is a high-molecular-weight protein consisting of two large subunits containing two [2Fe–2S] Rieske ferredoxins (ISPBED) (Crutcher and Geary 1979). The dihydrodiol dehydrogenase that converts the dihydrodiol into catechol is a large enzyme with a molecular weight of 440,000 (Axcell and Geary 1973). In Pseudomonas putida ML2, the genes encoding benzene dioxygenase are carried on a 112-kb plasmid (Tan and Mason 1990). As an alternative, successive monooxygenation of benzene to phenol, catechol, and 1,2,3trihydroxybenzene may be accomplished by the toluene 4-monooxygenase of Pseudomonas mendocina strain JKR1 and the 3-monooxygenase of Ralstonia (Pseudomonas) pickettii strain PKO1 (Tao et al. 2004). Toluene The degradation of toluene has been studied extensively in strains of Pseudomonas putida, and details of the three different pathways have been resolved. 1. In strains containing the TOL plasmid, degradation proceeds by successive oxidation of the methyl group to hydroxymethyl, aldehyde, and carboxylate, followed by dioxygenation of benzoate to catechol and extradiol ring ission (Figure 8.3a) (Keil and Williams 1985). The TOL plasmid also carries the genes for the degradation of 1,3- and 1,4-dimethylbenzenes (Assinder and Williams 1990), and involves comparable oxidations of a single methyl group (Davey and Gibson 1974; Williams and Worsey 1976). These carboxylic acids are then converted into catechols by benzoate dioxygenase and then undergo extradiol ring ission (Williams and Worsey 1976). In Pseudomonas desmolytica, n-propyl benzene is degraded by alternative pathways, both of which terminate in ring ission: (a) oxidation of the side chain to produce benzoate or (b) by dioxygenation and dehydrogenation to 3-n-propyl catechol (Jigami et al. 1979). 2. The genes for toluene degradation may also be located on the chromosome, when a different pathway is followed—dioxygenation by toluene 2,3-dioxygenase to (+)-cis-(2R,3S) 2,3-dihydro-2,3-dihydroxytoluene (Boyd et al. 1992; Ziffer et al. 1977), dehydrogenation to 3-methyl catechol followed by extradiol ring ission (Figure 8.3b). The multicomponent dioxygenase enzymes encoded by the genes todA, todB, todC1, and todC2 are analogous to those involved in benzene degradation: a lavoprotein reductaseTOL that accepts electrons from NADH, and a ferredoxinTOL that transfers them to the terminal dioxygenase (ISPTOL) which consists of two subunits (Zylstra and Gibson 1989). The dihydrodiol dehydrogenase has, however, a much lower molecular weight (104 kDa) than that for the corresponding benzene dihydrodiol dehydrogenase (Rogers and Gibson 1977). 3. Degradation of toluene may also take place in different species of Pseudomonas by initial monooxygenation at the 2-, 3-, or 4-positions. The situation for toluene monooxygenases has been confusing. However, it is now recognized that only the following two initial reactions take place: a. Toluene-2-monooxygenase of Burkholderia cepacia G4 hydroxylates toluene at the ortho position (Shields et al. 1995) and then further to 3-methylcatechol.

388

Environmental Degradation and Transformation of Organic Chemicals CH3

CH2OH

CHO

CO2H

OH

OH OH

(a)

CO2H CHO

CH3

CH3

CH3

H OH

CH3 OH

O OH

(b) OH H CH3

CH3

OH

CO2H

CO2H

CO2H

CO2H

(c) OH OH

OH

CO2H CO2H

OH

FIGURE 8.3 Aerobic degradation of toluene by (a) side-chain oxidation, (b) dioxygenation of the ring, and (c) monooxygenation. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

b. The formation of 4-methylphenol by the three-component monoxygenase in P. mendocina strain KR1 plausibly involves an arene oxide intermediate since it takes place with an NIH shift of a proton to the 3-position (Whited and Gibson 1991a,b). Further degradation involves oxidation to 4-hydroxybenzoate, hydroxylation to 3,4dihydroxybenzoate followed by intradiol ring ission (Figure 8.3c). c. Although the monooxygenase from Ralstonia pickettii was originally reported to form 3-hydroxytoluene, it has been shown that 4-hydroxytoluene is produced as the major product (Fishman et al. 2004). Other examples of monooxygenation of arenes include the following: a. The soluble methane monooxygenase from Methylococcus capsulatus produced 4-ethylphenol and 1-phenylethanol from ethylbenzene, and both 1- and 2-hydroxynaphthalene from naphthalene (Dalton et al. 1981); the formation of the 4-ethylphenol is accompanied by an NIH shift suggesting the involvement of an intermediate arene oxide. b. Under conditions of active NH4+ oxidation, cells of Nitrosomonas europaea can transform ethylbenzene to 4-ethylphenol and acetophenone (Keener and Arp 1994). c. In cell extracts, the cytochrome P450 system of Streptomyces griseus transforms benzene to phenol, toluene to 2-methylphenol, biphenyl to 2- and 4-hydroxybiphenyl, styrene to 4-hydroxystyrene, and naphthalene to naphth-1-ol (Sariaslani et al. 1989). Xylenes The pathway for the degradation of the xylenes depends critically on the orientation of the methyl groups, and o-xylene is considered to be the most recalcitrant since xylene monooxygenase cannot hydroxylate one of its methyl groups: a. The degradation of m- and p-xylene in organisms carrying the TOL plasmid is initiated, as for toluene, by oxidation of one of the methyl groups to m- or p-toluic acid. These are then degraded to 3- or 4-methylcatechol by dioxygenation and decarboxylation (Davey and Gibson 1974).

Carbocyclic Aromatic Compounds without Halogen Substituents

389

b. The degradation of o-xylene by chromosomal genes in Pseudomonas stutzeri OX1 takes place, however, by successive hydroxylation to 3,4-dimethylcatechol (Bertoni et al. 1998) that is degraded by dioxygenation and ring ission, with the loss of acetate to propionaldehyde and pyruvate. c. Degradation of o-xylene by Rhodococcus sp. DK17 is initiated by dioxygenation to an unstable o-xylene cis-3,4-dihydrodiol. This may be dehydrogenated to 3,4-dimethylcatechol followed by extradiol ring ission, or undergo dehydration to produce 2,3- and 3,4dimethylphenol (Kim et al. 2004). The degradation of BTEX both individually or in admixture has been shown in a lignindegrading white-rot fungus under nonlignolytic conditions, and was conirmed with ring-labeled toluene (Yadav and Reddy 1993). Interest in fungal transformation of PAHs is noted in the next part of this chapter, and illustrative examples of the hydroxylation of monocyclic arenes include the following (Smith and Rosazza 1983): a. Benzene to phenol by Penicillium chrysogenum, Cunninghamella blakesleeana, C. baineri, and Gliocladium deliquens b. Toluene to 2- and 4-methylphenol by Penicillium chrysogenum, Rhizopus stolonifer, and C. baineri c. Trans-stilbene to 4-hydroxy- and 4,4′-dihydroxystilbene by C. baineri Anaerobic Conditions Concern has arisen that leakage of BTEX from gasoline may reach groundwater where its fate is determined by anaerobic reactions. Although the degradation of benzene can occur anaerobically under sulfate-reducing, denitrifying, methanogenic, and iron (III)-reducing conditions (Mancini et al. 2003), the complete pathway for these reactions has not been established. Details of intermediates have been obtained using enrichment cultures using 13C6 -benzene: labeled phenol, benzoate, and toluene were detected and the kinetics of their formation were determined (Ulrich et al. 2005). The pathway for Dechloromonas aromatica strain RCB involves established reactions—hydroxylation to phenol followed by carboxylation and dehydroxylation to benzoate (Chakraborty and Coates 2005). The last two reactions are analogous to those involved in the anaerobic degradation of phenol by Thauera aromatica (Breese and Fuchs 1998; Schühle and Fuchs 2004). Dechloromonas aromatica strain RCB is also able to degrade toluene, ethylbenzene, and xylenes partially (Chakraborty et al. 2005). Perchlorate could also be used as an electron acceptor for the degradation of benzene, while benzene and toluene could be degraded concurrently. The anaerobic mineralization of BTEX in Fe-reducing cultures has been observed (Jahn et al. 2005). The pathways for the degradation of toluene and xylene under denitrifying and sulfatereducing conditions have been studied most extensively, and they take place by reactions quite different from those used by aerobic bacteria. As an example, two anaerobes afiliated with known sulfate-reducing bacteria isolated from enrichments with crude oil were able to grow at the expense of a number of alkylated benzenes—strain oXyS1 with toluene, o-xylene, and o-ethyltoluene and strain mXyS1 with toluene, m-xylene, and m-ethyltoluene (Harms et al. 1999). Several mechanisms have been established for the anaerobic degradation of toluene: 1. Dehydrogenation of the methyl group. Strains of denitrifying bacteria have been shown to degrade toluene in the absence of oxygen using N2O as electron acceptor (Schocher et al. 1991), and the data are consistent with a pathway involving successive oxidation of the ring methyl group with the formation of benzoate. The details of this pathway involving benzyl alcohol and benzaldehyde have been clearly demonstrated with a strain of Thauera (Pseudomonas) sp. under denitrifying conditions (Altenschmidt and Fuchs 1992).

390

Environmental Degradation and Transformation of Organic Chemicals

This pathway is supported by the demonstration of benzyl alcohol dehydrogenase, benzaldehyde dehydrogenase, benzoyl-CoA ligase, and benzoyl-CoA reductase activities in cell extracts (Biegert and Fuchs 1995). The benzyl alcohol dehydrogenase from benzyl alcohol–grown cells was similar in many of its properties to those from the aerobic bacteria Acinetobacter calcoaceticus and Pseudomonas putida (Biegert et al. 1995). 2. Condensation reactions. It has been suggested that the degradation of toluene could proceed by condensation with acetate to form phenylpropionate and benzoate before ring ission (Evans et al. 1992). These are produced as terminal metabolites during anaerobic degradation of toluene by sulfate-reducing enrichment cultures (Beller et al. 1992). A mechanism for the oxidation of the methyl group has been proposed for Azoarcus tolulyticus, and involves a condensation reaction with acetyl-CoA followed by dehydrogenation to cinnamoyl-CoA (Migaud et al. 1996). This is then either transformed into benzylsuccinate and benzylfumarate, which are apparently terminal metabolites that have also been isolated from a denitrifying organism (Evans et al. 1992), or by further degradation to benzoyl-CoA, which is the substrate for the ring reductase (Figure 8.4). The later reactions are also parts of the fumarate pathway. 3. Reactions with fumarate. An alternative sequence involves the direct formation of benzylsuccinate by the reaction of toluene with fumarate in Thauera aromatica (Biegert et al. 1996), and in a strain designated Pseudomonas sp. strain T2 (Beller and Spormann 1997a,b). It has been shown in the denitrifying strain T2 that the reaction between toluene and fumarate is stereospeciic, yielding (+)-benzylsuccinate, and that the proton abstracted from toluene is incorporated into the benzylsuccinate (Figure 8.5) (Beller and Spormann 1998). The synthesis of benzylsuccinate during the anaerobic degradation of toluene under denitrifying conditions involves activation of toluene to a benzyl radical by a mechanism involving glycyl radical catalysis (Leuthner et al. 1998; Verfürth et al. 2004). The amino HO2C CH2

CH3

CO2H

CO−SCoA

HO2C + CO2H

FIGURE 8.4

Anaerobic degradation of toluene via benzylsuccinate.

CO2H

COSCoA HO

CH3

CHO

CO2H

CO−SCoA HO

CO2H

CO2H

CO−SCoA HO

O

HO CO2H

FIGURE 8.5 Anaerobic degradation of toluene.

CO−SCoA

391

Carbocyclic Aromatic Compounds without Halogen Substituents

acid sequence of the large subunit of the puriied enzyme from Thauera aromatica showed a high level of homology to glycine radical enzymes and particularly to pyruvate formate lyase. It has been shown (Coschigano et al. 1998) in two mutants of strain T1 that the genes tutD and tutE involved in the anaerobic degradation of toluene encode proteins with molecular masses of 97.6 and 41.3 kDa, which possess homologies to pyruvate formate lyase and its activating enzyme, respectively. A free radical at Gly734 is involved in the operation of pyruvate formate lyase (Wagner et al. 1992) and there is, therefore, a formal similarity in at least one step in the two reaction pathways. The resulting benzylsuccinate is then metabolized to benzoyl-CoA followed by its metabolism, which has already been noted. Comparable pathways are used by Thauera aromatica and Azoarcus sp. for the degradation of m-xylene under denitrifying conditions (Verfürth et al. 2004). A sulfate-reducing bacterium strain PRTOL1 also catalyzes the reaction between toluene and fumarate with the formation of benzylsuccinate, so that this is apparently a widespread reaction (Beller and Spormann 1997a,b). It is also used by Desulfobacula toluolytica (Rabus and Heider 1998), for the degradation of o- and m-xylene by a sulfate-reducing strain of Desulfotomaculum (Morasch et al. 2004), and for xylene and ethylbenzene under sulfate-reducing conditions (Kniemeyer et al. 2003). The analogous succinates and fumarates that would be produced from dimethyl benzenes have been used as markers for the anaerobic degradation of these substrates in an aquifer (Beller et al. 1995; Beller 2002). Strains may be able to regulate the pathway of degradation of toluene to the availability of oxygen: aerobic degradation by dioxygenation or, in the absence of oxygen and under denitrifying conditions, by the benzylsuccinate pathway (Shinoda et al. 2004). 4. Other reactions. a. Under denitrifying conditions that have been extensively examined in strain EbN1, whereas the degradation of toluene proceeds via the fumarate pathway, the degradation of ethylbenzene involves dehydrogenation at the benzylic carbon atom, dehydrogenation, carboxylation, and hydrolysis (Rabus et al. 2002; Kühner et al. 2005) (Figure 8.6). The dehydrogenase is a soluble periplasmic trimeric enzyme that contains molybdenum, iron, acid-labile sulfur, and the molybdopterin cofactor (Johnson et al. 2001). b. Anaerobic hydroxylation of toluene to 4-hydroxytoluene followed by oxidation of the methyl group and dehydroxylation to benzoate has been suggested (Rudolphi et al. 1991). Although the role of these in degradation has not been clearly established, at least two analogies can be suggested: (i) carboxylation and dehydroxylation to 3methylbenzoate that is produced from 1,3-dimethylbenzene by Thauera sp. strain K172 under denitrifying conditions (Biegert and Fuchs 1995) and (ii) oxidation to 4hydroxybenzoate and further degradation. c. An alternative pathway for toluene includes side-chain carboxylation to phenyl acetate and oxidation via phenylglyoxylate to benzoate, which is an established pathway for phenyl acetate itself (Dangel et al. 1991).

O CH3 CH2

HO

CH3

CH3 CO

FIGURE 8.6 Anaerobic degradation of ethylbenzene.

O

C

O

CH2

O

SCoA

392

Environmental Degradation and Transformation of Organic Chemicals

Styrene This is used in large amounts for the production of polymers, and attention has been directed to the degradation of the volatile monomer that may be discharged into the environment or collected in bioilters. The bacterial degradation and transformation of styrene has attracted considerable attention (Warhurst and Fewson 1994), and several pathways have been described for bacteria: 1. In several bacteria, ring dioxygenation with the production of the cis-2,3-dihydrodiol takes place, leaving the vinyl group intact. In Rhodococcus rhodochrous strain NCIMB 13259, 2-vinyl-cis,cis-muconate is then produced by catechol 1,2-dioxygenase as a terminal metabolite, although complete degradation is possible owing to the existence of catechol 2,3-dioxygenase activity that is present (Warhurst et al. 1994). 2. Naphthalene dioxygenase from Pseudomonas sp. strain NCIB 9816-4 produces (R)-1phenyl-1,2-ethandiol by stereospeciic dioxygenation of the vinyl group (Lee and Gibson 1996). In a formally analogous reaction, the 4-methoxybenzoate monooxygenase from Pseudomonas putida strain DSM 1868 brings about dioxygenation of 4-vinyl benzoate to 4-(1,2-dihydroxyethyl)benzoate (Wende et al. 1989). 3. Monooxygenation of the vinyl group with formation of the epoxide takes place with a number of bacteria including Methylococcus capsulatus strain Bath (Colby et al. 1977) and Nitrosomonas europaea (Keener and Arp 1994, p. 202). The degradation of styrene oxide by Xanthobacter sp. strain 124X produced phenylacetaldehyde by the activity of an isomerase (Hartmans et al. 1989), and in an unclassiied Gram-positive organism—though not in the 124X strain—the degradation of styrene is accomplished by an FAD-dependent monooxygenase (Hartmans et al. 1990). Further metabolism of phenylacetaldehyde in Corynebacterium sp. strain ST-10 is carried out by an aldehyde reductase that is able to accept a wide range of aldehyde substrates (Itoh et al. 1997). In Pseudomonas sp. strain Y2, phenylacetaldehyde enters the lower pathway for degradation of phenylacetate via the coenzyme A-ester (del Peso-Santos et al. 2006). 4. The initial steps in the degradation of 2′-methyl-4-methoxystyrene (trans-anethole) by a strain of Arthrobacter aurescens are comparable to those already noted, except that the epoxide is hydrolyzed to a diol to produce 4-methoxybenzoate (Shimoni et al. 2002). It is appropriate here to note that styrene is transformed by the black yeast Exophilia jeanselmei to phenylacetate by a pathway similar to that of the Xanthobacter sp. already noted. The initial monooxygenation was carried out by a cytochrome P450, and phenylacetate was further metabolized to 2-hydroxy- and 2,5-dihydroxyphenylacetate (Cox et al. 1996). Stilbene Substituted stilbenes are formed during the production of wood pulp, and are components of luorescent whiting agents. The latter are considered recalcitrant although there are a few examples of their biodegradation. The degradation of stilbenes by oxidative ission of the Ar–C=C–Ar bond has been described for a lignin model compound (Habu et al. 1989b) putatively by dioxygenation (Habu et al. 1989a), and presumptively for α-methyl-4,4′-dihydroxy stilbene that is an intermediate in the degradation of bisphenol-A (Spivack et al. 1994). Synthetic Applications It has already been shown that biodegradation of many aromatic compounds proceeds by initial dioxygenation to cis-dihydrodiols, followed by dehydrogenation and ring ission. The high enantiomeric purity of cis-dihydrodiols produced by bacterial dioxygenases has been emphasized. Mutant strains that lack dehydrogenase activity produce only dihydrodiols, and there has been increasing interest in developing the use of these as synthons for the production of novel compounds that would not be readily available by conventional chemical synthesis.

393

Carbocyclic Aromatic Compounds without Halogen Substituents

For dihydrodiols derived from substituted benzenes, the key to their signiicance lies in the availability of two adjacent chiral centers with an established absolute stereochemistry. The dihydrodiol from benzene is, of course, the meso compound, although enantiomers produced by subsequent reaction with a chiral reagent are readily separated. There are useful reviews containing numerous applications (Carless 1992; Ribbons et al. 1989), many of which involve, in addition, the use of cis-luoro-, cis-chloro-, or cis-bromobenzene-2,3-dihydrodiols. Only a few illustrative syntheses using benzene and toluene cis-dihydrodiols are given below: 1. Although the product from the transformation of toluene by mutants of Pseudomonas putida lacking dehydrogenase activity is the cis-2R,3S dihydrodiol, the cis-2S,3R dihydrodiol has been synthesized from 4-iodotoluene by a combination of microbiological and chemical reactions. P. putida strain UV4 was used to prepare both enantiomers of the cis-dihydrodiol, and iodine was chemically removed using H2 -Pd/C. Incubation of the mixture of enantiomers with P. putida NCIMB 8859 selectively degraded the 2R,3S compound to produce toluene cis-2S,3R dihydrodiol (Allen et al. 1995). 2. Racemic pinitol from benzene cis-dihydrodiol benzoate by successive epoxidation and osmylation (Figure 8.7a) (Ley et al. 1987). 3. Conduramine A1 tetraacetate using an activated nitroso-mannose derivative (Figure 8.7b) (Werbitzky et al. 1990). 4. (–)-Laminitol from toluene cis-dihydrodiol by successive epoxidations (Figure 8.7c) (Carless and Oak 1991). 5. Analogs of conduritols from toluene cis-dihydrodiol by reaction with singlet oxygen followed by scission with thiourea (Figure 8.7d) (Carless et al. 1989). OH

O

OBz

OBz

MeO

OH OBz

MeO

OH

OBz

HO

OH

(a) OBz

OBz

NH

NHAc

O OAc

OH OAc

+

(b) OAc

OAc

Cl

OAc OAC

OAc OMe O

O

Me

HO O

Me

HO

HO

Me

OH

HO

OH

OH

HO

OH

(c) O

O

OH Me

Me OH

O

(d) OH

O

HO

Me OH

OH OH

OH OH

FIGURE 8.7 Examples of chemical syntheses based on cyclohexadiene cis dihydrodiols: (a) pinitol, (b) conduramine A, (c) (–)-laminitol, and (d) conduritol analogs. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

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There is clearly enormous potential using other cis dihydrodiols produced from benzocycloalkenes, or from the numerous dihydrodiols produced from polycyclic carbocyclic and heterocyclic substrates.

REFERENCES Allen CCR, DR Boyd, H Dalton, ND Sharma, I Brannigan, NA Kerley, GN Sheldrake, SC Taylor (1995) Enantioselective bacterial biotransformation routes to cis-diol metabolites of monosubstituted benzenes, naphthalene and benzocycloalkenes of either absolute coniguration. J Chem Soc Chem Commun 117–118. Altenschmidt U, G Fuchs (1992) Anaerobic toluene oxidation to benzylalcohol and benzaldehyde in a denitrifying Pseudomonas sp. J Bacteriol 174: 4860–4862. Ander P, K-E Eriksson, H-S Yu (1983) Vanillic acid metabolism by Sporotrichium pulverulentum: evidence for demethoxylation before ring-cleavage. Arch Microbiol 136: 1–6. Anderson JJ, S Dagley (1980) Catabolism of aromatic acids in Trichosporon cutaneum. J Bacteriol 141: 534–543. Assinder SJ, PA Williams (1990) The TOL plasmids: determinants of the catabolism of toluene and the xylenes. Adv Microb Physiol 31: 1–69. Axcell BC, PJ Geary (1973) The metabolism of benzene by bacteria. Puriication and some properties of the ezyme cis-1,2-dihydroxycyclohexa-3,5-diene (nicotinamide adenine dinucleotide) oxidoreductase (cis-benzene glycol dehydrogenase). Biochem J 136: 927–934. Axcell BC, PJ Geary (1975) Puriication and some properties of a soluble benzene-oxidizing system from a strain of Pseudomonas. Biochem J 146: 173–183. Beller HR (2002) Analysis of benzylsuccinates in groundwater by liquid chromatography/tandem mass spectrometry and its use for monitoring in situ BTEX biodegradation. Environ Sci Technol 36: 2724–2728. Beller HR, AM Spormann (1997a) Anaerobic activation of toluene and o-xylene by addition to fumarate in denitrifying strain T. J Bacteriol 179: 670–676. Beller HR, AM Spormann (1997b) Benzylsuccinate formation as a means of anaerobic toluene activation by sulfate-reducing strain PRTOL1. Appl Environ Microbiol 63: 3729–3731. Beller HR, AM Spormann (1998) Analysis of the novel benzylsuccinate synthase reaction for anaerobic toluene activation based on structural studies of the product. J Bacteriol 180: 5454–5457. Beller HR, M Reinhard, D Grbic-Galic (1992) Metabolic by-products of anaerobic toluene degradation by sulfate-reducing enrichment cultures. Appl Environ Microbiol 58: 3192–3195. Beller HR, W-H Ding, M Reinhard (1995) Byproducts of anaerobic alkylbenzene metabolism useful as indicators of in situ bioremediation. Environ Sci Technol 29: 2864–2870. Bertoni G, M Martino, E Galli, P Barbieri (1998) Analysis of the gene cluster encoding toluene/o-xylene monooxygenase from Pseudomonas stutzeri OX1. Appl Environ Microbiol 64: 3626–3632. Biegert T, G Fuchs (1995) Anaerobic oxidation of toluene (analogues) to benzoate (analogues) by whole cells and by cell extracts of a denitrifying Thauera sp. Arch Microbiol 163: 407–417. Biegert T, G Fuchs, J Heider (1996) Evidence that anaerobic oxidation of toluene in the denitrifying bacterium Thauera aromatica is initiated by formation of benzylsuccinate from toluene and fumarate. Eur J Biochem 238: 661–668. Biegert T, U Altenschmidt, C Eckerskorn, G Fuchs (1995) Puriication and properties of benzyl alcohol dehydrogenase from a denitrifying Thauera sp. Arch Microbiol 163: 418–423. 1 Boyd DR, ND Sharma, R Boyle, RAS McMordie, J Chima, H Dalton (1992) A H NMR method for the determination of enantiomeric excess and absolute coniguration of cis-dihydrodiol metabolites of polycyclic arenes and heteroarenes. Tetrahedron Lett 33: 1241–1244. Breese K, M Boll, J Alt-Mörbe, H Schäggrer, G Fuchs (1998) Genes encoding the benzoyl-CoA pathways of anaerobic aromatic metabolism in the bacterium Thauera aromatica. Eur J Biochem 256: 148–154. Cain RB, RF Bilton, JA Darrah (1968) The metabolism of aromatic acids by micro-organisms. Metabolic pathways in the fungi. Biochem J 108: 797–828. Carless HAJ (1992) The use of cyclohexa-3,5-diene-1,2-diols in enantiospeciic synthesis. Tetrahedron Asymmetry 3: 795–826. Carless HAJ, Billinge JR, Oak OZ (1989) Photochemical routes from arenes to inositol intermediates: the photo-oxidation of substituted cis-cyclohexane-3,5-diene-1,2-diols. Tetrahedron Lett 30: 3113–3116.

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Hartmans S, MJ van der Werf, JAM de Bont (1990) Bacterial degradation of styrene involving a novel lavin adenenine dinucleotide-dependent styrene monooxygenase. Appl Environ Microbiol 41: 1045–1054. Harwood CS, G Burchardt, H Herrmann, G Fuchs (1999) Anaerobic metabolism of aromatic compounds via the benzoyl-CoA pathway. FEMS Microbiol Rev 22: 439–458. Högn T, L Jaenicke (1972) Benzene metabolism of Moraxella species. Eur J Biochem 30: 369–375. Hopper DJ (1978) Microbial degradation of aromatic hydrocarbons. In Developments in biodegradation of hydrocarbons-1 (Ed RJ Watkinson), pp. 85–112. Applied Science Publishers Ltd, London. Itoh N, R Morihama, J Wang, K Okada, N Mizuguchi (1997) Puriication and characterization of phenylacetaldehyde reductase from a styrene-assimilating Corynebacterium strain, ST10. Appl Environ Microbiol 63: 3783–3788. Jahn MK, SB Haderlin, RU Meckenstock (2005) Anaerobic degradation of benzene, toluene, ethylbenzene, and o-xylene in sediment-free iron-reducing enrichment cultures. Appl Environ Microbiol 71: 3355–3358. Jigami Y, Y Kawasaki, T Omori, Y Minoda (1979) Coexistence of different pathways in the metabolism of n-propylbenzene by Pseudomonas sp. Appl Environ Microbiol 38: 783–788. Johnson HA, DA Pelletier, AM Spormann (2001) Isolation and characterization of anaerobic ethylbenzene dehydrogenase, a novel Mo-Fe-S enzyme. J Bacteriol 183: 4536–4542. Keener WK, DJ Arp (1994) Transformations of aromatic compounds by Nitrosomonas europaea. Appl Environ Microbiol 60: 1914–1932. Keil H, PA Williams (1985) A new class of TOL plasmid deletion mutants in Pseudomonas putida MT15 and their reversion by tandem gene ampliication. J Gen Microbiol 131: 1023–1033. Kim D, J-C Chae, GJ Zylstra, Y-S Kim, MH Nam, YM Kim, E Kim (2004) Identiication of a novel dioxygenase involved in metabolism of o-xylene, toluene, and ethylbenzene by Rhodococcus sp. strain DK17. Appl Environ Microbiol 70: 7086–7092. Kniemeyer O, T Fischer, H Wilkes, FO Glöckner, F Widdel (2003) Anaerobic degradation of ethylbenzene by a new type of marine sulfate-reducing bacterium. Appl Environ Microbiol 69: 760–768. Kühner S, L Wöhlbrand, I Fritz, W Wruck, C Hultschig, P Hufnagel, M Kube, R Reinhardt, R Rabus (2005) Substrate-dependent regulation of anaerobic degradation pathways for toluene and ethylbenzene in a denitrifying bacterium strain EbN1. J Bacteriol 187: 1493–1503. Lee K, DT Gibson (1996a) Stereospeciic dihydroxylation of the styrene vinyl group by puriied naphthalene dioxygenase from Pseudomonas sp. strain NCIB 9816-4. J Bacteriol 178: 3353–3356. Leuthner B, C Leutwein, H Schulz, P Hörth, W Haehnel, E Schiltz, H Schägger, J Heider (1998) Biochemical and genetic characterisation of benzylsuccinate synthase from Thauera aromatica: a new glycyl-radical catalysing the irst step in anaerobic toluene degradation. Mol Microbiol 28: 515–628. Ley SV, F Sternield, S Taylor (1987) Microbial oxidation in synthesis: a six step preparation of (+/–)-pinitol from benzene. Tetrahedron Lett 28: 225–226. Mancini SA, AC Ulrich, G Lacrampe-Couloume, B Sleep, EA Edwards, BS Lollar (2003) Carbon and hydrogen isotopic fractionation during anaerobic biodegradation of benzene. Appl Environ Microbiol 69: 191–198. Migaud ME, JC Chee-Sandford, JM Tiedje, JW Frost (1996) Benzylfumaric, benzylmaleic, and Z- and E-phenylitaconic acids: synthesis, characterization, and correlation with a metabolite generated by Azoarcus tolulyticus Tol-4 during anaerobic toluene degradation. Appl Environ Microbiol 62: 974–978. Morasch B, B Schink, CC Tebbe, RU Meckenstock (2004) Degradation of o-xylene and m-xylene by a novel sulfate-reducer belonging to the genus Desulfotomaculum. Arch Microbiol 181: 407–417. Neilson AH, A-S Allard (1998) Microbial metabolism of PAHs and heteroarenes. Handb Environ Chem 3J: 1–80. Parales RE, CS Harwood (1993) Regulation of the pcaIJ genes for aromatic acid degradation in Pseudomonas putida. J Bacteriol 175: 5829–5838. Rabus R, J Heider (1998) Initial reactions of anaerobic metabolism of alkylbenzenes in denitrifying and sulfate-reducing bacteria. Arch Microbiol 170: 377–384. Rabus R, M Kube, A Beck, F Widdel, R Reinhardt (2002) Genes involved in the anaerobic degradation of ethylbenzene in a denitrifying bacterium, strain EbN1. Arch Microbiol 178: 506–516. Ribbons DW, RW Eaton (1982) Chemical transformations of aromatic hydrocarbons that support the growth of microorganisms. In Biodegradation and detoxiication of environmental pollutants (Ed AM Chakrabarty), pp. 59–84. CRC Press, Boca Raton.

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Ribbons DW, SJC Taylor, CT Evans, SD Thomas, JT Rossiter, DA Widdowson, DJ Williams (1989) Biodegradations yield novel intermediates for chemical synthesis. In Biotechnology and Biodegradation (Eds D Kamely, A Chakrabarty, GS Omenn), pp. 213–245. Gulf Publishing Company, Houston, Texas. Rogers JE, DT Gibson (1977) Puriication and properties of cis-toluene dihydrodiol dehydrogenase from Pseudomonas putida. J Bacteriol 130: 1117–1124. Rothmel, RK, DL Shinbarger, MR Parsek, TL Aldrich, AM Chakrabarty (1991) Functional analysis of the Pseudomonas putida regulatory protein CatR: transcriptional studies and determination of the CatR DNA-binding site by hydroxyl-radical footprinting. J Bacteriol 173: 4717–4724. Rudolphi A, A Tschech, G Fuchs G (1991) Anaerobic degradation of cresols by denitrifying bacteria. Arch Microbiol 155: 238–248. Sariaslani FS, MK Trower, SE Buchloz (1989) Xenobiotic transformations by Streptomyces griseus. Dev Ind Microbiol 30: 161–171. Schocher RJ, B Seyfried, F Vazquez, J Zeyer (1991) Anaerobic degradation of toluene by pure cultures of denitrifying bacteria. Arch Microbiol 157: 7–12. Schühle K, G Fuchs (2004) Phenylphosphate carboxylase: a new C–C lyase involved in anaerobic phenol metabolism in Thauera aromatica. J Bacteriol 186: 4556–4567. Shields MS, MJ Reagin, RR Gerger, R Campbell, C Somerville (1995) TOM, a new aromatic degradative plasmid from Burkholderia (Pseudomonas) cepacia G4. Appl Environ Microbiol 61: 1352–1356. Shimoni E, T Baasov, U Ravid, Y Shoham (2002) The trans-anethole degradation pathway in an Arthrobacter sp. J Biol Chem 277: 11866–11872. Shinoda Y, Y Sakai, H Uenishi, Y Uchihashi, A Hiraishi, H Yukawa, H Yurimoto, N Kato (2004) Aerobic and anaerobic toluene degradation by a newly isolated denitrifying bacterium Thauera sp. strain DNT-1. Appl Environ Microbiol 70: 1385–1392. Smith MR (1994) The physiology of aromatic hydrocarbon degrading bacteria. In Biochemistry of Microbial Degradation (Ed C Ratledge), pp. 347–378. Kluwer Academic Publishers, Dordrecht, The Netherlands. Smith RV, JP Rosazza (1983) Microbial models of mammalian metabolism. J Nat Prod 46: 79–91. Söhngen NL (1913) Benzin, Petroleum, Parafinöl und Parafin als Kohlenstoff- und Energiequelle für Mikroben. Centralbl Bakteriol Parasitenkd Infektionskr (2 Abt) 37: 595–609. Spivack J, TK Leib, JH Lobos (1994) Novel pathway for bacterial metabolism of bisphenol A. Rearrangements and stilbene cleavage in bisphenol A metabolism. J Biol Chem 269: 7323–7329. Tan H-M, JR Mason (1990) Cloning and expression of the plasmid-encoded benzene dioxygenase from Pseudomonas putida ML2. FEMS Microbiol Lett 72: 259–264. Tao Y, A Fishman, WE Bentley, TK Wood (2004) Oxidation of benzene to phenol, catechol, and 1,2,3trihydroxybenzene by toluene 4-monooxygenase of Pseudomonas mendocina KR 1 and toluene 3-monooxygenase of Ralstonia pickettii PKO1. Appl Environ Microbiol 70: 3814–3820. Tausson WO (1927) Naphthalin als Kohlenstoffquelle für Bakterien. Planta 4: 214–256. Ulrich AC, HR Beller, EA Edwards (2005) Metabolites detected during biodegradation of 13C6 -benzene in nitrate-reducing and methanogenic enrichment cultures. Environ Sci Technol 39: 6681–6691. van der Meer, WM de Vos, S Harayama, AJB Zehnder (1992) Molecular mechanisms of genetic adaptation to xenobiotic compounds. Microbiol Revs 56: 677–694. Verfürth K, AJ Pierik, C Leutwein, S Zorn, J Heider (2004) Substrate speciicities and electron paramagnetic resonance properties of benzylsuccinate synthesis in anaerobic toluene and m-xylene metabolism. Arch Microbiol 181: 155–162. Wagner AFV, M Frey, FA Neugebauer, W Schäfer, J Knappe (1992) The free radical in pyruvate formate-lyase is located on glycine-734. Proc Natl Acad USA 89: 996–1000. Warhurst AM, CA Fewson (1994) Microbial metabolism and biotransformations of styrene. J Appl Bacteriol 77: 597–606. Warhurst AM, KE Clarke, RA Hill, RA Holt, CA Fewson (1994) Metabolism of styrene by Rhodococcus rhodochrous NCIMB 13259. Appl Environ Microbiol 60: 1137–1145. Wende P, F-H Bernhardt, K Pleger (1989) Substrate-modulated reactions of putidamonooxin. The nature of the active oxygen species formed and its reaction mechanism. Eur J Biochem 181: 189–197. Werbitzky O, K Klier, H Felber H (1990) Asymmetric induction of four chiral cenbters by hetero Diels–Alder reaction of a chiral nitrosodienmophile. Liebigs Ann Chem 267–270. Whited GM, DT Gibson (1991a) Separation and partial characterization of the enzymes of the toluene-4monooxygenase catabolic pathway in Pseudomonas mendocina KR1. J Bacteriol 173: 3017–3020.

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PART 2 POLYCYCLIC AROMATIC HYDROCARBONS (PAHS) INTRODUCTION Aromatic hydrocarbons are components of petroleum and are produced during the gasiication of coal, while naturally occurring partially aromatized steroids and terpenoids which occur in sediments and coal have been used as biomarkers (Simoneit 1998). Concern with polycyclic aromatic hydrocarbons has centered on those that display carcinogenicity to mammals after metabolic activation. Since anoxic sediments may be a sink for PAHs, degradation and biodegradation have been examined under both aerobic and anaerobic conditions. Biochemical aspects of the biodegradation of PAHs have been given in a classic review in Gibson and Subramanian (1984), Smith (1994), and Kanaly and Harayama (2000), while speciic aspects of sphingomonads have been presented in Pinyakong et al. (2003). The biodegradation of benzo[a]pyrene by bacteria, fungi, and algae has been addressed in a review within the context of remediation (Juhasz and Naidu 2000). Attention is directed to marine organisms that are able to degrade PAHs, and which generally belong to the genus Cycloclasticus (Geiselbrecht et al. 1998; Kasai et al. 2003; Wang et al. 1996). The aerobic degradation of naphthalene was described many years ago (Tausson 1927; Gray and Thornton 1928). As for the degradation of benzene, it was, however, many years later that the details of the reaction involved were elucidated. Since then, the degradation of naphthalene, anthracene, phenanthrene, luoranthene, and pyrene has been described in a number of organisms, that of benzo[a]pyrene, benz[a]anthracene, and dibenz[a]anthracene less often, and that of chrysene (Demanèche et al. 2004) and coronene (Juhasz et al. 1997) only occasionally. It should be realized that growth at the expense of PAHs may require only a contribution from the products of partial degradation. Care should therefore be exercised in the interpretation of experiments using partially labeled substrates (Ye et al. 1996). Aerobic degradation is generally initiated by dioxygenation followed by dehydrogenation to catechols that undergo ring ission. For polycyclic arenes, repetition of these reactions is then used for the successive degradation of the other rings, for example, o-phthalate is produced from anthracene (van Herwijnen et al. 2003), phenanthrene (Moody et al. 2001), and pyrene (Vila et al. 2001; Krivobok et al. 2003). Exceptionally, elimination rather than dehydrogenation takes place. For example, the dioxygenation of 7,4′-dihydroxyisolavone by biphenyl-2,3-dioxygenase from Burkholderia sp. strain LB400 is followed by elimination to the phenol 7,2′,4′trihydroxyisolavone rather than by dehydrogenation (Seeger et al. 2003). Substantial attention has been directed to details of the degradation of naphthalene on account of interest in the synthesis of chiral compounds using naphthalene-1,2-dioxygenase, and of biphenyl, since biphenyl-2,3-dioxygenase induced by growth with biphenyl has a broad substrate range including congeners of PCBs. Genes for the degradation of naphthalene may be carried on plasmids, for example, in pseudomonads (Dunn and Gunsalus 1973; Dunn et al. 1980; Yen et al. 1988), Novosphingobium aromaticivorans (Romine et al. 1999), and some species of Rhodococcus (Kulakov et al. 2005).

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Aerobic Reactions Carried Out by Bacteria Naphthalene The aerobic degradation of naphthalene and its derivatives has been extensively examined, so that the pathway, biochemistry, and genetics are well established. Naphthalene is readily degraded by many bacteria including Gram-negative pseudomonads, Gram-positive rhodococci, and marine bacteria belonging to the genus Cycloclasticus. Both the details of the initial steps and their enzymology have been elucidated. Genes for the degradation of naphthalene and the intermediate metabolite salicylate are generally carried on plasmids in pseudomonads (Dunn and Gunsalus 1973; Dunn et al. 1980; Yen et al. 1988), and in some species of Rhodococcus (Kulakov et al. 2005). The overall pathway of degradation is shown in Figure 8.8, and is carried out by a sequence of enzymes. The enzymes for the complete sequence of enzymes involved in the oxidative degradation of naphthalene to catechol and for the extradiol (meta) ission pathway for degradation of the catechol are inducible by growth with salicylate in Pseudomonas putida (Austen and Dunn 1980). The genes for degradation in Pseudomonas putida G7 are organized in two operons, the upper encoding those for the conversion of naphthalene into salicylate, and the lower those for the degradation of salicylate to pyruvate and acetate. The nah genes encoding the enzymes on the plasmid NAH7 for conversion of naphthalene into salicylate have been cloned from Pseudomonas putida G1064: nahA, nahB, nahC, nahD, nahE, and nahF for naphthalene dioxygenase, naphthalene cis-dihydrodiol dehydrogenase, 1,2-dihydroxynaphthalene dioxygenase, 2-hydroxychromene-2-carboxylate isomerase, and salicylaldehyde dehydrogenase, respectively (Yen and Serdar 1988). The initial product of naphthalene oxidation in Pseudomonas putida by naphthalene dioxygenase is naphthalene (+)-cis-(1R,2S)-1,2-dihydro-1, 2-diol (Jeffrey et al. 1975). Naphthalene dioxygenase (Patel and Barnsley 1980; Ensley and Gibson 1983), cis-naphthalene dihydrodiol dehydrogenase (Patel and Gibson 1974), and 1,2-dihydroxynaphthalene dioxygenase (Kuhm et al. 1991) have been puriied, while further details of the subsequent steps have been added (Eaton and Chapman 1992). The degradation of naphthalene has also been studied in strains of Rhodococcus sp., and two groups of strains have been examined. Differences from pseudomonads have been observed in strain NCIMB 12038, in which the genes are carried on a plasmid: (a) naphthalene is the sole inducer of the whole pathway and (b) the degradation of salicylate proceeds from the activity of salicylate 5-hydroxylase to 2,5-dihydroxybenzoate (gentisate) (Grund et al. 1992; Larkin et al. 1999). In other strains including strain P200, the genes are chromosomal (Kulakov et al. 2005).

H

OH

OH OH

OH

H

OH

OH CO2H

OH

OH

CO2H

OH

OH HO

CO2H

FIGURE 8.8 Degradation of naphthalene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

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Further details merit brief comment: a. In some strains of pseudomonads, the degradation of the intermediate catechol produced by the activity of salicylate hydroxylase may proceed either by the extradiol or the alternative intradiol ission pathway (Barnsley 1976). b. In Ralstonia (Pseudomonas) sp. strain U2 (Fuenmayor et al. 1998; Zhou et al. 2002), the alternative gentisate pathway for the degradation of the intermediate salicylate is used. c. In a strain of Mycobacterium sp., both dioxygenation to cis-naphthalene-1,2-dihydrodiol and monooxygenation and hydrolysis to trans-naphthalene-1,2-dihydrodiol were encountered, with the latter dominating 25-fold (Kelley et al. 1990). d. In the context of biotechnology, naphthalene dioxygenase from a strain of Pseudomonas sp. also carried out enantiomeric monooxygenation of indan and dehydrogenation of indene (Gibson et al. 1995), and the stereospeciic hydroxylation of (R)-1-indanol, (S)-1-indanol to cis-indan-1,3-diol, and trans (1S,3S)-indane-1,3-diol (Lee et al. 1997); the indantriols are also formed by further reactions. Essentially comparable reactions have been observed with Rhodococcus sp. strain NCIMB 12038 (Allen et al. 1997). e. Sphingomonas aromaticivorans carries catabolic genes for the degradation of aromatic hydrocarbons on a plasmid. It is able to degrade not only naphthalene and biphenyl by dioxygenation, but also initiate the degradation of xylenes by monooxygenation of the methyl groups, followed by dioxygenation of the resulting benzoates (Romine et al. 1999). Naphthalene dioxygenase from Pseudomonas putida consists of three proteins: the reductaseNAP (Haigler and Gibson 1990b), a ferredoxinNAP (Haigler and Gibson 1990a), and the two-subunit terminal oxygenase ISPNAP (Ensley and Gibson 1983). They are analogous to those involved in the degradation of benzene and toluene, and are encoded by the genes nadAa, nadAb, and nadAc/nadAd (Simon et al. 1993). However, the reductaseNAD component of naphthalene dioxygenase contains both FAD and a [2Fe–2S] ferredoxin (Haigler and Gibson 1990a), so that naphthalene is unusual in requiring three redox centers to transfer electrons from NADH to the terminal dioxygenase. Although naphthalene dioxygenase is enantiomer-speciic in producing the (+)-cis-(1R,2S)dihydrodiol, it also possesses dehydrogenase and monooxygenase activities (Gibson et al. 1995), so that monooxygenase and dioxygenase activities are not exclusive. Exclusive monooxygenation has been observed; for example, the transformation of naphthalene by Bacillus cereus yielded naphth-1-ol with retention of the deuterium after incubation with 1[2H]- and 2-[2H]naphthalene, which is consistent with involvement of an arene oxide and an NIH shift (Cerniglia et al. 1984). Alkylated Naphthalenes Methylnaphthalenes are important components of crude oils, and their degradation follows the initial stages used for alkylated benzenes. The degradation of 2,6-dimethylnaphthalene by lavobacteria involves a pathway analogous to that for dimethylbenzenes—successive oxidation of one methyl group to carboxylate, decarboxylative dioxygenation to 1,2-dihydroxy-6-methylnaphthalene, ring ission to 5-methylsalicylate, followed by further degradation by pathways established for naphthalene itself (Barnsley 1988). Degradation of both 1-methyl- and 2-methylnaphthalene was initiated by 7,8-dioxygenation (Mahajan et al. 1994). Whereas 1-methylnaphthalene produced only 3-methyl catechol, 2-methylnaphthalene produced both 4-hydroxymethylcatechol and 4-methylcatechol. The catechols then underwent extradiol ission. The oxidation of 1,5-, 2,6-, 2,7-, and 1,8-dimethyl naphthalene by a recombinant strain of Pseudomonas aeroginosa PAO1 involved successive oxidation of only a single methyl group to the monocarboxylates, except for 1,8-dimethylnaphthalene in which both methyl groups were oxidized to the dicarboxylate (Selifonov et al. 1996). The oxidation of a wide range of dimethyl naphthalenes has been examined in Sphingomonas paucimobilis strain 2322 (Dutta et al. 1998). Degradative pathways involved successive oxidation to the corresponding

Carbocyclic Aromatic Compounds without Halogen Substituents

401

carboxylate of a methyl group in one of the rings. Further degradation involved the following alternative pathways: a. Decarboxylative dioxygenation to a 1,2-dihydroxynaphthalene followed by 1:1a extradiol ission and formation of salicylate b. Hydroxylation to a 1-hydroxynaphthalene-2-carboxylate and 1:2-intradiol ring ission with the formation of o-phthalate Naphthols and Naphthalene Carboxylates Less attention has been devoted to the degradation of naphthols and naphthalene carboxylates: 1. a. The degradation of naphth-1-ol has been described (Bollag et al. 1975), and the speciicity of oxygen uptake in whole cells—though not in cell-free extracts—has been studied (Larkin 1988). Two strains, Pseudomonas sp. strain 12043 and Rhodococcus sp. strain NCIB 12038, were less versatile, whereas Pseudomonas sp. strain 12042 was more versatile, showing oxygen uptake with both 1- and 2-naphthols, 1,5- and 2,7dihydroxynaphthalene and naphthalene itself. The subsequent degradation of the 1,2dihydroxynaphthalene formed from the naphthols may plausibly be assumed to proceed by ring ission and subsequent established reactions that produce salicylate and then catechol (strain 12042) or gentisate (strains 12043 and 12038). b. Naphthalene-1-hydroxy-2-carboxylate is an intermediate in the degradation of phenanthrene, and it has been proposed that as a β-ketoacid, it is decarboxylated to naphth-1-ol followed by pathways leading to salicylate or o-phthalate (Samanta et al. 1999). c. Naphthalene 1,8-dicarboxylate and naphthalene 1-carboxylate are intermediates in the degradation of acenaphthylene by Rhizobium sp. strain CU-A1. They are formed from acenaphthenequinone, and then degraded to salicylate and 2,5-dihydroxybenzoate (Poonthrigpun et al. 2006). 2. Although the degradation of naphthalene-2-carboxylate by Burkholderia sp. strain JT 1500 involves the formation of 1-hydroxy naphthalene-2-carboxylate, this is not formed from the expected (1R,2S)-cis-1,2-dihydrodiol-2-naphthoate. Possibly, therefore, the reaction is carried out by a monooxygenase, or a dehydration step is involved. Subsequent reactions produced pyruvate and o-phthalate that was degraded via 4,5-dihydroxyphthalate (Morawski et al. 1997). Degradation of naphthalene carboxylates formed by oxidation of methyl groups has already been noted. Biphenyl The degradation of biphenyl is known in considerable detail on account of interest in the degradation of PCBs, and virtually all bacteria that degrade PCBs have been isolated after enrichment with biphenyl (Pellizari et al. 1996). Although the degradative pathways of naphthalene and biphenyl are broadly similar, dioxygenation of chlorinated biphenyls by Pseudomonas sp. strain LB400 may occur at either the 2,3- or the 4,5-positions (Haddock et al. 1995). A strain of Pseudomonas paucimobilis, which also degrades toluene, and 1,3- and 1,4-dimethylbenzene, carries out dioxygenation and dehydrogenation of biphenyl followed by ring ission to benzoate, which is further degraded by intradiol ring ission (Figure 8.9) (Furukawa et al. 1983). The three-component biphenyl dioxygenase consists of a reductaseBPH, a ferredoxinBPH, and a terminal dioxygenase ISPBPH. The dioxygenase contains two subunits and a Rieske-type [2Fe–2S] center that are encoded by the genes bphA4 (bphG), bphA3 (bphF), and bphA1bph/A2 (bphA/bphE) (Erickson and Mondello 1992). The dioxygenase has been puriied from Pseudomonas sp. strain LB400 (Haddock and Gibson 1995). All the components from Comamonas testosteroni strain B-356, which degrades 4-chlorobiphenyl, have been isolated. Puriication of the reductaseBPH and ferredoxinBPH proteins was made possible by using His-tagged components produced from

402

Environmental Degradation and Transformation of Organic Chemicals HO

OH

H

HO

HO

H

OH O

CO2H

OH CO2H

OH

FIGURE 8.9 Degradation of biphenyl. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

recombinant strains of Escherichia coli (Hurtubise et al. 1995). The reductaseBPH contains 1 Mol of FAD, the ferredoxinBPH a Rieske [2Fe–2S] center, and together with the terminal oxygenase ISPBPH, both biphenyl-2,3-dihydrodiol and biphenyl-3,4-dihydrodiol were produced from biphenyl. It has been shown that the product of dioxygenation of biphenyl by Sphingomonas yanoikuyae strain B1 (Beijerinckia sp. B1) is biphenyl cis-(2R,3S)-2,3-dihydrodiol (Ziffer et al. 1977). This is then converted into 2,3-dihydroxybiphenyl by a dehydrogenase encoded by the bphB gene followed by ring ission by 2,3-dihydroxybiphenyl 1,2-dioxygenase encoded by the bphC gene. The ring ission dioxygenase has been examined in a number of organisms, and although polyclonal antibodies from the enzymes from P. paucimobilis strain Q1 and from P. pseudoalcaligenes strain KF707 do not cross-react (Taira et al. 1992), there is a high degree of homology between the bphC gene in P. putida strain OU 83 and those from P. cepacia strain LB400 and P. pseudoalcaligenes strain KF707 (Khan et al. 1996). Greater complexity has been observed in Gram-positive strains: in Rhodococcus globerulus strain P6, there are three genes encoding 2,3-dihydroxybiphenyl-1,2dioxygenase (Asturias and Timmis 1993), and in Rhodococcus erythropolis strain TA421, four (Maeda et al. 1995). Although toluene-2,3-dioxygenase, naphthalene-1,2-dioxygenase, and bipheny-2,3-dioxygenase are broadly similar, an interesting difference has emerged in the products formed from benzocycloheptene by bacterial strains that express these activities (Resnick and Gibson 1996). Fungal hydroxylation and subsequent ring ission has only seldom been reported. The imperfect fungus Paecilomyces liliacinus is able to produce successively mono-, di-, and trihydroxylated metabolites from biphenyl and carry out intradiol ring ission of rings carrying adjacent hydroxyl groups (Gesell et al. 2001). PAHs with Three or More Rings The aerobic degradation of a wide range of PAHs with three or more rings has been described, and the pathways are analogous to those outlined for naphthalene and biphenyl—though sometimes they have been covered in less detail. These reactions have been reviewed (Kanaly and Harayama 2000), and only salient features with some exceptions are briely noted. The lexibility of some organisms—including several mycobacteria—to degrade or metabolize a range of PAHs and the apparently unique metabolic versatility of a strain of Enterobacter sp. is particularly striking. Some illustrative examples are given in Table 8.1.

403

Carbocyclic Aromatic Compounds without Halogen Substituents

TABLE 8.1 Bacterial Degradation of PAHs Substrate Nap, Phe, Flu, 3-Me-Chol Nap, Phe, Anth, Flu Nap, Flu, Pyr Phe, Pyr, Flu Nap, Phe, Anth, Fl Nap, Phe, Anth, Pyr, BaPyr, BaAnth Flu, Pyr, BaAnth, DBaAnth Bi, Phe, Anth, Flu, BbFlu, Chr, Pyr Flu, Pyr, BaAnth, Chr, BaPyr Nap, Anth, Phe, Flu, Pyr, BaAnth, BaPyr Note:

Organism Mycobacterium sp. Alcaligenes denitriicans Enterobacter sp. Mycobacterium sp. BB1 Pseudomonas cepacia F297 Pseudomonas putida GZ44 Mycobacterium sp. RJGII-135 Burkholderia cepacia Pseudomonas paucimobilis Pseudomonas paucimobilis Mycobacterium vanbaalenii PYR-1

Reference Heitkamp et al. (1988a,b) Weissenfels et al. (1991) Sarma et al. (2004) Boldrin et al. (1993) Grifoll et al. (1994, 1995) Goyal and Zylstra (1996) Schneider et al. (1996) Juhasz et al. (1997) Mueller et al. (1990) Ye et al. (1996) Kim et al. (2006)

Bi, biphenyl; Nap, naphthalene; Phe, phenanthrene; Anth, anthracene; Fl, luoranthene; Pyr, pyrene; Chr, chrysene; BaAnth, benz[a]anthracene; BaPyr, benzo[a]pyrene; BbFlu, benzo[b]luoranthene; DbaAnth, dibenz[a,h]anthracene; 3-Me-Chol, 3-methylcholanthrene.

The stereospeciic dioxygenation of several PAHs by bacteria has been described, and includes the following illustrative examples: a. Anthracene to cis-(1R,2S)-anthracene-1,2-dihydrodiol (Akhtar et al. 1975) b. Phenanthrene to cis-(1R,2S)-phenanthrene-1,2-dihydrodiol and cis-(3S,4R)-phenanthrene3,4-dihydrodiol (Koreeda et al. 1978) c. Benz[a]anthracene to benz[a]anthracene-cis-(1R,2S)-1,2-dihydrodiol, cis-(8R,9S)-8,9dihydrodiol, and cis-(10S,11R)-10,11-dihydrodiol (Jerina et al. 1984) Further degradation of the dihydrodiols involves dehydrogenation to the catechols followed by ring ission and oxidative degradation of the ission product. However, for higher PAHs, degradation may be more complex. Other issues that intrude include dioxygenation at different positions of the rings, and the alternative of monooxygenation. A great deal of attention has been given to the degradation of higher PAHs, and only selected examples are given as illustration. Anthracene and Phenanthrene The degradation of these was described many years ago (Evans et al. 1965), and details have since been added (Figure 8.10a) (van Herwijnen et al. 2003). Phenanthrene is more readily degraded than anthracene, and both can be degraded to o-phthalate. After ission of the peripheral ring in phenanthrene, several pathways have been demonstrated: a. The naphthalene pathway via salicylate (Evans et al. 1965) b. The o-phthalate pathway followed by ission of 3,4-dihydroxybenzoate (Kiyohara and Nagao 1978; Kiyohara et al. 1976; Barnsley 1983) (Figure 8.10b) c. Degradation to diphenyl-6,6′-dicarboxylate (Figure 8.10c) (Moody et al. 2001) d. A pathway that involves naphth-1-ol, which has already been noted (Samanta et al. 1999) The enzymes involved in the degradation of phenanthrene by Nocardioides sp. strain KP7 have been characterized. In this strain, the genes are chromosomal, and phdA and phdB encoding the α- and β-subunits of the dioxygenase, phdC and phdD that encode the ferredoxin, and ferredoxin reductase have been cloned and sequenced (Saito et al. 2000). The order of the genes

404

Environmental Degradation and Transformation of Organic Chemicals OH OH

OH

CO2H

CO 2 H

CO2H

(a) OH HO

OH CO2H

CO2H

(b) CO2H (c) CO2H CO2H

OH OH

FIGURE 8.10

Degradation of (a) anthracene, (b,c) alternative pathways for phenanthrene.

O

O

OH H OH

CO2H CO2H OH OH CHO O

O

FIGURE 8.11 Pathways for degradation of luorene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.) OH

OH OH CHO

O

O

O

FIGURE 8.12 Degradation of luorene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

405

Carbocyclic Aromatic Compounds without Halogen Substituents

was different from that in pseudomonads, and there was only moderate similarity to the sequence for other dioxygenase subunits. 1-Hydroxy-2-naphthoate dioxygenase (Iwabuchi and Harayama 1998a), trans-2′-carboxybenzalpyruvate hydratase-aldolase (Iwabuchi and Harayama 1998b), and 2-carboxybenzaldehyde dehydrogenase, which catalyzes the formation of o-phthalate (Iwabuchi and Harayama 1997), have been puriied and characterized. The puriied dioxygenase was used to determine further details of the degradation pathways (Adachi et al. 1999). The initial product from ring ission is in equilibrium with the lactone formed by reaction between the carboxyl group and the activated double bond of the benzalpyruvate in a reaction formally comparable to the formation of muconolactones during degradation of monocyclic aromatic compounds. An important exception to the generalization that bacterial dioxygenation is used for aromatic hydrocarbons is provided by Streptomyces lavovirens in which cytochrome P450 produces (–)-trans-[9S,10S]-9,10-dihydrodihydroxyphenanthrene with minor amounts of 9-hydroxyphenanthrene (Sutherland et al. 1990). Fluorene Several pathways have been reported including oxidation to luoren-9-one and dioxygenation at the ring junction followed by degradation of the oxygenated ring by extradiol ission to yield phthalate (Grifoll et al. 1994; Trenz et al. 1994). In one variant, an 8-hydroxy benzo[c]coumarin is produced (Figure 8.11). Alternatively, dioxygenation may take place to produce 3,4-dihydroxyluorene followed by extradiol ring ission and further degradation to 3,4-dihydrocoumarin (Grifoll et al. 1992) (Figure 8.12). A strain of Pseudomonas cepacia F297 that was able to grow with a range of PAHs including luorene, anthracene, and phenanthrene degraded luorene via 3,4-dihydroxyluorene and extradiol ission to indan-1-one as terminal metabolite (Grifoll et al. 1994). Fluoranthene Degradation by Mycobacterium sp. strain PYR-1 involves dioxygenation at both the 1,2-, and 7, 8-positions, producing after ring ission luorene-9-one (Figure 8.13a), or acenaphthene-7-one (Figure 8.13b) (Kelley et al. 1993). In a strain of Alcaligenes denitriicans, acenaphthene-7-one is further

OH

OH (a)

O HO

O

CO2H

O

HO (b)

(c)

O O

O

OH

CH2CO2H

FIGURE 8.13 Degradation of luoranthene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

406

Environmental Degradation and Transformation of Organic Chemicals

oxidized by a Baeyer—Villiger-type oxidation to 3-hydroxymethyl-3,4-dihydro-benzo[d,e]coumarin before further oxidation (Weissenfels et al. 1991) (Figure 8.13c). The unusual transformation products luoranthene-2,3- and 1,5-quinone have been identiied in several strains of bacteria (Kazunga et al. 2001). Both were terminal metabolites and since the 2,3-quinone inhibited the degradation of other PAHs, its formation could have an adverse effect on attempts at bioremediation of PAH-contaminated sites. Benz[a]anthracene Transformation by Sphingomonas yanoikuyae strain B1 (Beijerinckia sp. strain B 1) involves dioxygenation at the 1,2-, 8,9-, or 10,11-positions with production of the cis-[1R,2S], cis-[8R,9S], or cis[10S,11R] dihydrodiols of which the irst is the dominant (Jerina et al. 1984). These are then further degraded to 1-hydroxy-2-carboxyanthracene, or the corresponding phenanthrenes (Mahaffey et al. 1988) (Figures 8.14a through 8.14c). In contrast, Mycobacterium sp. strain RJGII-135 forms the 5,6- and 10,11-dihydrodiols (Schneider et al. 1996), so that four different pathways for degradation are possible. Exceptionally, monooxygenation may occur concomitant with dioxygenation; for example, the transformation of 7,12-dimethylbenz[a]anthracene by Mycobacterium vanbaalenii PYR-1 takes place by monooxygenation to epoxides followed by hydration to trans-dihydrodiols, and also by dioxygenation to cis-dihydrodiols (Moody et al. 2003). Pyrene Degradation by a Mycobacterium sp. involves both monooxygenation and dioxygenation at the 4,5-position with production of the trans- and cis-dihydrodiols, respectively, which are degraded to phenanthrene-4-carboxylate and ultimately to o-phthalate. 4-Hydroxyperinaphthenone was also produced, presumably by initial dioxygenation at the 1,2-positions (Heitkamp et al. 1988a) (Figure 8.15). This is consistent with the structure of the intermediate from the degradation of pyrene by Rhodococcus sp. strain UW1 (Walter et al. 1991). Alternatively, degradation by Mycobacterium sp. OH HO

OH CO2H

(a)

CO2H OH

(b) HO OH OH (c) OH HO CO2H

FIGURE 8.14 Pathways for partial degradation of benz[a]anthracene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

407

Carbocyclic Aromatic Compounds without Halogen Substituents HO2C CO2H OH

CO2H

OH OH O

OH

OH

FIGURE 8.15

Degradation of pyrene.

OH

OH

OH

OH CO2H + CO2H CO2H

CO2H CO2H HO OH

CO2H CO2H

FIGURE 8.16

Degradation of pyrene.

strain AP1 produced both cis- and trans-4,5-dihydrodiols (Vila et al. 2001). The former was degraded further to phenanthrene-4,5-dicarboxylic acid, phenthanrene-4-carboxylate and phthalate, and 6,6′-dihydroxy-biphenyl-2,2′-dicarboxylate (Figure 8.16). Bacterial formation of pyrene-4,5quinone has been reported (Kazunga and Aitken 2000). Although the degradation of pyrene by Mycobacterium sp. strain A1-PYR was restricted with the formation of several oxygenated metabolites, complete degradation without their formation was accomplished when phenanthrene or luoranthene was also present (Zhong et al. 2006). This is particularly relevant to the degradation of mixtures of PAHs, for example, in bioremediation (Chapter 14, Part 2).

408

Environmental Degradation and Transformation of Organic Chemicals

OH

CO2H CO2H

OH

FIGURE 8.17 Products produced by partial degradation of benzo[a]pyrene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

Benzo[a]pyrene Mycobacterium sp. strain RJGH-135, which was able to metabolize pyrene, benz[a]anthracene, and benzo[a]pyrene, degraded the last by dioxygenation at the 4,5-, 7,8-, and 9,10-positions (Schneider et al. 1996). Chrysene-4,5-dicarboxylate was presumptively formed by intradiol ission of the 4, 5-benzo[a]pyrene-4,5-diol, while the 7,8- and 9,10-dihydrodiols underwent extradiol ission to 7- and 8-dihydropyrene carboxylates (Figure 8.17). Mycobacterium vanbaalenii strain PYR1 carried out both monooxygenation with the formation of benzo[a]pyrene trans-11,12-dihydrodiol and dioxygenation to cis-dihydrodiols at the 4,5- and 11,12-positions. The former was then degraded further to chrysene-4,5-dicarboxylic acid (Moody et al. 2004). A soil strain of Rhodanobacter sp. in a consortium could degrade [7-14C]benzo[a]pyrene apparently using metabolites produced by other organisms, since the pure cultures were unable to degrade the substrate (Kanaly et al. 2002). This may be a widespread phenomenon for complex mixtures such as those that were used in that study. Anaerobic Reactions Carried Out by Bacteria The anaerobic degradation of a few PAHs has been examined, generally using mixed cultures from widely different habitats, and investigations have been limited hitherto to naphthalene and phenanthrene. Although no pathway was established, the degradation has been assessed from the diminishing substrate concentration of anthracene, phenanthrene, and pyrene by denitrifying pseudomonads isolated from diverse environments under both aerobic and anaerobic denitrifying conditions (McNally et al. 1998). Under sulfate-reducing conditions, [1-14C]naphthalene and [9-14C]phenanthrene were oxidized to 14CO2 (Coates et al. 1996, 1997), and a pure culture NaphS2b that belongs to the δ-subclass of the Proteobacteria has been isolated, which can degrade naphthalene, naphthalene-2-carboxylate, benzoate, and acetate (Galushko et al. 1999). Under anaerobic nitrate-reducing conditions, both [ring 14C]toluene and [1-14C]naphthalene were oxidized to 14CO2 (Bregnard et al. 1996), and pure cultures of denitrifying organisms could mineralize [U14C]naphthalene under anaerobic conditions, although a substantial fraction of the label was recovered in cell biomass (Rockne et al. 2000). Although carboxylated intermediates of naphthalene and phenanthrene have been identiied in a sulidogenic mixed culture (Zhang and Young 1997), these are not the primary metabolites. Details of the pathway emerged using a sulfate-reducing enrichment culture that was able to grow at the expense of naphthalene and 2-methylnaphthalene. It was shown (Sainowski and Meckenstock 2006) that transformation of naphthalene is initiated by the formation of 2-methylnaphthalene, which is able to support the growth of this enrichment culture. Its transformation is initiated by reaction with fumarate analogous to that used for the activation of toluene. The pathway involves successive formation of naphthyl-2-methylsuccinate, naphthyl-2-methylenesuccinate, and naphth2-oate, followed by subsequent steps to 2-carboxycyclohexylacetate (Figure 8.18) (Annweiler et al. 2002) by the reduction of both rings (Meckenstock et al. 2000) and hydroxylation; these steps are analogous to those for benzoate. In cometabolism with 2-methylnaphthalene, analogous

409

Carbocyclic Aromatic Compounds without Halogen Substituents CH3

CH2

CO 2 H

CO2H

CO2H

CO 2 H

CO2H OH

FIGURE 8.18

CO2H CO2H

CO2H CO2H

Anaerobic degradation of 2-methylnaphthalene.

reactions were shown to operate with benzothiophene and benzofuran (Sainowski et al. 2006). It was suggested that these polar metabolites could be used to assess degradation of these arenes in anaerobic groundwater, analogous to the use of benzylsuccinates from monocyclic arenes (BTEX), which has already been demonstrated (Beller et al. 1995, 2002). An analogous pathway that produced decahydronaphthalene-2-carboxylate has been demonstrated for another sulfate-reducing consortium in which reduction of the A-ring and carboxylation of the B-ring of 2-methylnaphthalene was also observed (Sullivan et al. 2001). Fungal Transformations In contrast to the degradations carried out by bacteria, eukaryotic organisms such as yeasts and fungi often accomplish only biotransformation. The aryl hydrocarbon monooxygenase in Cunninghamella baineri is a cytochrome P450 (Ferris et al. 1976) in which the [FeO]3+complex with the substrate may carry out either direct hydroxylation of the substrate by elimination of a proton, or produce an epoxide or a rearranged (NIH shift) monohydroxy (phenolic) compound (Guengerich 1990). Isotope experiments clearly show that the phenols are generally not produced by either a direct substitution reaction or elimination from the trans-dihydrodiols. Epoxide hydrolases produce phenols from the trans-dihydrodiols, and can then be conjugated to sulfate or glucuronide esters (Cerniglia et al. 1982b), or O-methylated. Monooxygenation of methyl groups to carboxyl groups has also been reported. C. elegans has been used to examine the transformation of a number of polycyclic aromatic hydrocarbons. Reactions are generally conined to oxidation of the rings with the formation of phenols, catechols, and quinones, and ring ission does not generally take place. Different rings may be oxygenated, for example, in 7-methylbenz[a]anthracene (Cerniglia et al. 1982c) (Figure 8.19) or oxidation may take place in several rings, for example, in luoranthene (Pothuluri et al. 1990) (Figure 8.20). Since fungal metabolism of PAHs has been suggested as a model for mammalian metabolism (Smith and Rosazza 1983), particular attention has been directed to the stereochemistry and absolute coniguration of the trans-dihydrodiols produced by monooxygenation. There is one very signiicant difference between the trans-dihydrodiols produced by fungi and those from mammalian systems—the absolute coniguration of the products. Although trans-1,2-dihydroxy-1, 2-dihydroanthracene and trans-1,2-dihydroxy-1,2-dihydrophenanthrene are formed from anthracene by C. elegans, these dihydrodiols have the S,S coniguration in contrast to the R,R coniguration of the metabolites from rat liver microsomes (Cerniglia and Yang 1984). It has become clear, however, that the situation among a wider range of fungi is much less straightforward. For example, the trans-9,10-dihydrodiol produced by Phanerochaete chrysosporium was predominantly the 9S,10S enantiomer, whereas those produced by Cunninghamella elegans and Syncephalastrum racemosum were dominated by the 9R,10R enantiomers (Sutherland et al. 1993). Comparable differences were also observed for the trans-1,2-dihydrodiols and trans-3,4-dihydrodiols, so that generalizations on the enantiomeric selectivity of these reactions should be viewed with caution.

410

Environmental Degradation and Transformation of Organic Chemicals OH H OH H

CH2OH

CH3 HO H HO H

FIGURE 8.19

CH2OH

Biotransformation of 7-methylbenz[a]anthracene by Cunninghamella elegans.

OH HO

H

H

HO

OH HO

H

H

FIGURE 8.20 Alternative pathways for the biotransformation of luoranthene by Cunninghamella elegans.

There are two issues that recur in fungal transformations, and these have been extensively documented: 1. The phenol, which is formed by rearrangement from the initially produced transdihydrodiol, may be conjugated to form sulfate esters or glucuronides (Cerniglia et al. 1982b; Golbeck et al. 1983; Cerniglia et al. 1986; Lange et al. 1994). The less-common glucosides have also been identiied: 1-phenanthreneglucopyranoside is produced from phenanthrene by Cunninghamella elegans (Cerniglia et al. 1989) and 3-(8-hydroxyluoranthene)lucopyranoside from luoranthene by the same organism (Pothuluri et al. 1990). The xylosylation of 4-methylguaiacol and vanillin by the basidiomycete Coriolus versicolor (Kondo et al. 1993) represents an even less-common alternative. 2. In reactions involving monooxygenase systems with the formation of intermediate arene oxides, rearrangement of substituents may take place (Figure 8.21a). This is an example of the NIH shift that plays an important role in the metabolism of xenobiotics by mammalian systems (Daly et al. 1972). It has also been observed in fungal (Figure 8.21b) (Faulkner and Woodcock 1965; Smith et al. 1981; Cerniglia et al. 1983) and bacterial systems

411

Carbocyclic Aromatic Compounds without Halogen Substituents R

R

R H

(a) x

CH2−CO2H O

O

X

O X

O

OH

CH2−CO2H

O

Cl

Cl

R H X

CH2−CO2H Cl

(b) Cl

HO Cl

Cl

CH2−CH3

OH

CH2−CH3

(c) D

H D

H

FIGURE 8.21 Examples of the NIH shift.

(Figure 8.21c) (Dalton et al. 1981; Cerniglia et al. 1984a,b; Adriaens 1994) including the marine cyanobacterium Oscillatoria sp. (Narro et al. 1992a,b). The transformation of naphthalene by a large number of fungi has been examined, including representatives of the Mucorales such as Cunninghamella, Syncephalastrum, and Mucor, which were the most active. The principal product was naphth-1-ol, with lesser amounts of 2-naphthol, 4-hydroxytetral-1-one, trans-naphthalene-1,2-dihydrodiol, and the 1,2- and 1,4-quinones (Cerniglia et al. 1978). The results of detailed study (Cerniglia et al. 1983) of the transformation of naphthalene by Cunninghamella elegans illustrate most of the basic principles involved in the fungal transformation of all PAHs: a. The initial product is naphthalene-1,2-epoxide, which is converted into the trans-dihydrodiol with the (+)-(1S,2S) coniguration. b. The trans-dihydrodiol is formed by introduction of a single atom of 18O2 at C1 while that at C2 comes from H218O. c. The naphth-1-ol formed from [1-2H]-naphthalene retains 78% of the deuterium so that an NIH shift is involved. Similar experiments with 1-methyl- and 2-methylnaphthalene involved oxidation of the methyl group to hydroxymethyl and carboxyl groups (Cerniglia et al. 1984a,b). The transformation of biphenyl is analogous to that of naphthalene, with the production of hydroxylated biphenyls as the major metabolites: 4-hydroxybiphenyl from C. echinulata, 2-hydroxybiphenyl from Helicostylum piriforme, 4,4′-dihydroxybiphenyl from Aspergillus parasiticus (Golbeck et al. 1983; Smith et al. 1980), and 2-, 3-, and 4-hydroxybiphenyl, and 4,4′-dihydroxybiphenyl from C. elegans (Dodge et al. 1979). During the formation of 4-hydroxybiphenyl from [U-2H]-biphenyl by C. echinulata, 20% of the deuterium was retained, which is consistent with formation of an arene oxide followed by an NIH shift (Smith et al. 1981).

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Environmental Degradation and Transformation of Organic Chemicals

H

OH

H HO

HO HH

OH O

O

O

O

FIGURE 8.22 Products produced by fungal transformation of benzo[a]pyrene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

Higher PAHs may produce a number of products. For example, 7,12-dimethylbenz[a] anthracene gives rise to a range of metabolites including both hydroxymethyl compounds and several trans-dihydrodiols. The 7-hydroxymethyl-12-methylbenz[a]anthracene-trans-5,6-dihydrodiols produced by C. elegans and S. racemosum were mixtures of the R,R and S,S enantiomers with the former predominating (McMillan et al. 1987). This is, however, contrary to the products from mammalian systems. From luoranthene, C. elegans produces both the trans-2,3-dihydrodiol as well as the 8-hydroxy-3-hydroxyglucoside, and the 8- and 9-hydroxy-3,4-dihydrodiols (Pothuluri et al. 1990). The metabolism of pyrene and benzo[a]pyrene by C. elegans is increasingly complex. Pyrene is transformed by hydroxylation at the 1-, 1- and 6-, and 1- and 8- positions, and the bisphenols were glucosylated at the 6- and 8-positions; the 1,6- and 1,8-pyrenequinones were also formed (Cerniglia et al. 1986). The same organism transformed benzo[a]pyrene to the trans-7,8- and trans9,10-diols, the 3- and 9-hydroxy compounds, and the 1,6- and 3,6-quinones (Cerniglia and Gibson 1979) (Figure 8.22). In addition, C. elegans formed sulfate conjugates of polar metabolites, and one of these was identiied as the 7b,8a,9a,10b-tetrahydrotetrol formed sequentially from the 7b,8bepoxide, the 7b,8a-dihydrodiol, and the 7b,8a-dihydrodiol-9a,10a-epoxide (Cerniglia and Gibson 1980a). Tetrahydrotetrols were also formed by metabolism of both diastereomers of (+/–)-trans9,10-dihydrodiol including the 7b,8a,9b,10a- and 7b,8a,9a,10b-compounds; a dihydrodiol epoxide was also isolated that could be hydrolyzed to the former (Cerniglia and Gibson 1980b). The transformation of 3-methylcholanthrene by C. elegans was exceptional in that 1-hydroxy-trans-9,10dihydrodiol was formed in only trace amounts, and benzylic oxidations at C1 and C2 dominated (Cerniglia et al. 1982d). The metabolism of pyrene by the basidiomycete fungus Crinipellis stipitaria strain JK 364 illustrates a hitherto largely neglected possibility: biosynthesis from the products of metabolism. This strain can transform pyrene to 1-hydroxypyrene, and trans-4,5-dihydro-4,5-dihydroxypyrene. Simultaneously, the secondary metabolite 3-methyl-6,8-dihydroxyisocoumarin is produced, which is synthesized from acetate produced by ring ission (Lange et al. 1995). The biosynthesis of the isocoumarin was also induced by chrysene, though not by anthracene, phenanthrene, or luoranthene. Most of the foregoing studies were conducted with C. elegans or S. racemosum, but results have been presented showing that a wide range of nonbasidiomycete soil fungi are capable of oxidizing both pyrene and benzo[a]pyrene (Launen et al. 1995). Those with high activity included Penicillium janthinellum that produced 1-hydroxypyrene as a major metabolite, together with the 1,6- and 1,8-quinones.

Carbocyclic Aromatic Compounds without Halogen Substituents

413

Yeasts and Algae A cytochrome P450 has been puriied from Saccharomyces cerevisiae that has benzo[a]pyrene hydroxylase activity (King et al. 1984), and metabolizes benzo[a]pyrene to 3- and 9hydroxybenzo[a]pyrene and benzo[a]pyrene-7,8-dihydrodiol (Wiseman and Woods 1979). The transformation of PAHs by Candida lipolytica produced predominantly monohydroxylated products: naphth-1-ol from naphthalene, 4-hydroxybiphenyl from biphenyl and 3- and 9hydroxybenzo[a]pyrene from benzo[a]pyrene (Cerniglia and Crow 1981). The transformation of phenanthrene was demonstrated in a number of yeasts isolated from littoral sediments and of these, Trichosporum penicillatum was the most active. In contrast, biotransformation of benz[a]anthracene by Candida krusei and Rhodotorula minuta was much slower (MacGillivray and Shiaris 1993). Naphthalene, biphenyl, and phenanthrene may be transformed in low yield by oxygenic phototrophs (algae and cyanobacteria) with the formation of several metabolites. A range of algae produced naphth-1-ol from naphthalene (Cerniglia et al. 1980a,b; 1982a), while biphenyl was transformed by a strain of the cyanobacterium Oscillatoria sp. to 4-hydroxybiphenyl (Cerniglia et al. 1984a). A study with the same strain showed that the naphth-1-ol formed from [1-2H]- and [2-2H]naphthalene retained 68% and 74% of the deuterium. This shows that the reaction proceeded by initial formation of naphthalene-1,2-epoxide followed by an NIH shift (Narro et al. 1992a). The transformation of phenanthrene by the unicellular cyanobacterium Agmenellum quadruplicatum involved monooxygenation to produce the trans 9,10-dihydrodiol and lesser amounts of 3-methoxyphenanthrene. The dihydrodiol which has an enantiomeric excess of the (–)-[9S,10S] enantiomer was produced by the introduction of a single atom of 18O2 (Narro et al. 1992b), and is formally analogous to the transformation of naphthalene to naphth-1-ol by a strain of Oscillatoria sp., which has already been noted. The products from the metabolism of benzo[a]pyrene by the green alga Selenastrum capricornutum strain UTEX 1648 are unexpected, since the cis-dihydrodiols at the 11,12-, 7,8-, and 4,5-positions were apparently produced by dioxygenation (Warshawsky et al. 1995b). The light conditions determine both the preferred site of dioxygenation and the relative contribution of the phytotoxic benzo[a]pyrene-3,6-quinone (Warshawsky et al. 1995a). An interesting and exceptional example of ring ission by algae is afforded by the degradation of phenol by Ochromonas danica via catechol followed by extradiol ission (Semple and Cain 1996). White-Rot Fungi There has been considerable interest in white-rot fungi since they are capable of degrading not only lignin but also a wide range of other substrates including PAHs. They are discussed separately since the mechanisms whereby they accomplish degradation or transformation of PAHs differ signiicantly from the fungi already discussed. Although considerable attention has been directed to Phanerochaete chrysosporium, the degradation and transformation of PAHs is not limited to this taxon (Ferris et al. 1976). Investigations with Ph. laevis and Pleurotus ostreatus (Bezalel et al. 1996a) have brought to light signiicantly different metabolic pathways. It should be pointed out that ten different strains of Ph. chrysosporium have been shown to harbor bacteria, although only a few of these have been identiied (Seigle-Murandi et al. 1996). The metabolic consequence of this association is apparently unresolved. The mechanism and enzymology of transformations by white-rot fungi are complicated for several issues: a. The synthesis of the lignin and Mn peroxidases is regulated by several factors including the nitrogen status of the cells, the oxygen concentration, and the concentration of Mn2+ in the growth medium. b. The dependence of enzyme activity on the growth phase of the cells. The results of experiments with whole cells may, therefore, differ from those obtained with pure enzymes or cell extracts. c. The range of oxygenation mechanisms that has emerged.

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Environmental Degradation and Transformation of Organic Chemicals

A brief summary of these factors includes the following issues: 1. Peroxidase systems. There are at least three of these extracellular enzyme systems: (a) lignin peroxidase (LiP), (b) manganese-dependent peroxidase (MnP), and (c) manganese peroxide-dependent lipid peroxidase. The irst functions by formation of a cation radical that undergoes further reaction, the second by formation of Mn3+ that brings about oxidation of the substrate, and the third probably by proton abstraction followed by the introduction of oxygen. The enzyme system responsible for lignin degradation is expressed during idiophasic growth as a result of nitrogen limitation. The regulation of the synthesis of LiP and MnP is complex, and depends on the Mn2+ concentration in the medium (Bonnarme and Jeffries 1990; Brown et al. 1990), although it is not apparently subject to carbon substrate regulation (van der Woude et al. 1993). However, the synthesis of manganese peroxidase is regulated by concentrations of H2O2 and O2 (Li et al. 1995). 2. Monooxygenases. Under nonlignolytic conditions, arene monooxygenase and epoxide hydrolase systems may function to produce trans-dihydrodiols. Hydrogen abstraction mediated by the lipid peroxidase system may operate, for example, in the formation of luorene-9-one from luorene by Ph. chrysosporium (Bogan et al. 1996). 3. Hydroxylases. Some substrates are activated to cation radicals that react further with H2O to ultimately produce quinones. This is particularly prevalent in 4- and 5-ring compounds, though important alternatives exist. 4. Dioxygenase. Although it is not involved in the transformation of PAHs, it may be noted for the sake of completeness that a catechol intradiol dioxygenase is involved in the ission of 1,2,4-trihydroxybenzene that is formed from a number of aromatic substrates (Rieble et al. 1994). Although a number of white-rot fungi have been examined and shown to degrade PAHs (Field et al. 1992), greatest attention has probably been directed to Phanerochaete chrysosporium and Pleurotus ostreatus, and to the PAHs anthracene, phenanthrene, pyrene, and benzo[a]pyrene that will be used to illustrate the cardinal principles. A substantial fraction of PAHs may also be sorbed to the biomass—40% for phenanthrene and 22% for benzo[a]pyrene (Barclay et al. 1995). The degree of mineralization of PAHs by white-rot fungi may sometimes be quite low, for example, for Pleurotus ostreatus, yields were 3.0, 0.44, 0.19, and 0.19% for phenanthrene, pyrene, luorene, and benzo[a]pyrene, respectively (Bezalel et al. 1996a). Anthracene Degradation by Ph. chrysosporium took place by initial formation of anthra-9,10-quinone followed by ring ission to phthalate (Figure 8.23) (Hammel et al. 1991). This pathway is completely different from that used by both bacteria and fungi, and the ission of the quinone might plausibly involve a Baeyer–Villiger-type insertion of oxygen. In contrast, P. ostreatus formed both anthra-9,10-quinone and anthracene trans-1,2-dihydrodiols as terminal metabolites, with an S,S- to R,R- ratio of 58:42 in the latter (Bezalel et al. 1996c).

O CO2H

O

CO2H

FIGURE 8.23 Degradation of anthracene by Phanerochaete chrysosporium. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

415

Carbocyclic Aromatic Compounds without Halogen Substituents

CO2H CO2H

O O

OH H OH H

+ H OH

3-ol+4-ol

H

OH

9-ol

FIGURE 8.24 Alternative pathways for transformation of phenanthrene by Phanerochaete chrysosporium. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

Phenanthrene There are different pathways that have been delineated and these are considered separately as follows: 1. The transformation of phenanthrene has been extensively studied and illustrates the operation of alternative pathways that depend on the status of the cells. During cell growth of Ph. chrysosporium, the trans-3,4- and trans-9,10-diols were formed and rearranged to produce 3-, 4-, and 9-phenanthrenols (Figure 8.24). Since lignin peroxidase activity was not observed, it was suggested that the trans-diols were formed by monooxygenase and epoxide hydrolase activities (Sutherland et al. 1991). 2. In conditions under which lignin degradation is induced, phenanthrene is oxidized by cell suspensions of Ph. chrysosporium to phenanthrene-9,10-quinone, which is then issioned to biphenyl-2,2′-dicarboxylate (Hammel et al. 1992) (Figure 8.24). Cytochrome P450 activation was not apparently involved, and extracellular ligninases were inactive in vitro. The same products, with a preponderance of the intermediate trans-[R,R]-9,10-dihydrodiol, were produced by P. ostreacus, and it was suggested that a cytochrome P450 system was involved (Bezalel et al. 1996b, 1997). 3. Biphenyl-2,2′-dicarboxylate was formed by Ph. chrysosporium in a reaction mixture with manganese peroxidase, O2, and unsaturated lipid, and it was suggested that a MnPmediated lipid peroxidation was involved (Moen and Hammel 1994). A synthesis of these results has been presented, and evidence presented for the role of alkoxy radicals generated during lipid oxidation (Bogan and Lamar 1995; Tatarko and Bumpus 1993). Pyrene and Benzo[a]pyrene Puriied ligninase H8 produced by P. chrysosporium in stationary cultures oxidized pyrene to pyrene-1,6- and pyrene-1,8-quinones in high yield, and experiments with H218O showed that both quinone oxygen atoms originated in water (Figure 8.25). It was suggested that initial one-electron abstraction produced cation radicals at the 1 and 6 or 8-positions (Hammel et al. 1986), whereas in

416

Environmental Degradation and Transformation of Organic Chemicals O

O

+

O

O

O

O

+

O

O

FIGURE 8.25 Quinones produced from pyrene and benzo[a]pyrene. (From Neilson, A.H. and Allard, A.-S. The Handbook of Environmental Chemistry, Springer, 1998. With permission.)

P. ostreacus that produced the trans-4,5-dihydrodiols with a 63:37 ratio of the R,R and S,S enantiomers, a cytochrome P450 monooxygenase was involved (Bezalel et al. 1996b). In analogy with the transformation of pyrene, the 1,6-, 3,6-, and 6,12-quinones were formed from benzo[a]pyrene by Ph. chrysopsporium (Haemmerli et al. 1986). These reactions are analogous to those involved in the electrochemical oxidation of benzo[a]pyrene (Jeftic and Adams 1970), and oxidation by Mn(III) acetate (Cremonesi et al. 1989), while substantial evidence supports the role of cation radicals as intermediates in biological oxidations and the tumorogenic properties of some PAHs (Cavalieri and Rogan 1998). In most of the above illustrations, quinones have been formed and they may be terminal metabolites or only transient intermediates that are produced, for example, during mineralization by the basiomycete Stropharia coronillla (Steffen et al. 2003). Degradation was stimulated by addition of Mn2+, and could be attributed to elevated levels of the lignolytic manganese peroxidase. Experiments with Ph. laevis strain HHB-1625 have revealed some additional features (Bogan and Lamar 1996): a. Under conditions of nitrogen limitation in the presence of Mn2+, manganese peroxidase activity was induced although no lignin peroxidase activity could be demonstrated. b. Transformation of anthracene, phenanthrene, benz[a]anthracene, and benzo[a]pyrene was demonstrated without the accumulation of quinones that were, at best, transient metabolites. c. In comparison with Ph. chrysosporium, Ph. laevis was more effective in mineralizing [5,6-14C]benz[a]anthracene-7-12-quinone. In summary, it may be stated that for a wide range of PAHs, the speciic association of dioxygenation to give cis-dihydrodiols by prokaryotes and of monooxygenation to epoxides and thence to trans-dihydrodiols by eukaryotes is generally valid. The absolute stereochemistry of the transdihydrodiols produced by fungi is highly variable, and there are frequently signiicant differences between the products of fungal monooxygenation and those carried out by rat-liver microsomes. Although quinone are frequently formed as metabolites of the white-rot fungus Ph. chrysosporium, these are only transiently formed by Ph. laevis, so that care should be exercised in making generalizations on the basis the results obtained for a single species or strain. The intermediate epoxides may rearrange to produce phenols that are generally conjugated.

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Brown JA, JK Glenn, MA Gold (1990) Manganese regulates expression of manganese peroxidase by Phanerochaete chrysosporium. J Bacteriol 172: 3125–3130. Cavalieri E, E Rogan (1998) Mechanisms of tumor initiation by polycyclic aromatic hydrocarbons in mammals. Handbook Environ Chem 3J: 82–117. Cerniglia CE, DT Gibson (1979) Oxidation of benzo[a]pyrene by the ilamentous fungus Cunninghamella elegans. J Biol Chem 254: 12174–12180. Cerniglia CE, DT Gibson (1980a) Fungal oxidation of benzo[a]pyrene and (+/–)-trans-7,8-dihydroxy-7,8dihydrobenzo[a]pyrene: evidence for the formation of a benzo[a]pyrene 7,8-diol-9,10-epoxide. J Biol Chem 255: 5159–5163. Cerniglia CE, DT Gibson (1980b) Fungal oxidation of (+/–)-9,10-dihydroxy-9-10-dihydrobenzo[a]pyrene: formation of diastereomeric benzo[a]pyrene 9,10-diol-7,8-epoxides. Proc Natl Acad USA 77: 4554–4558. Cerniglia CE, DT Gibson, C van Baalen (1980a) Oxidation of naphthalene by cyanobacteria and microalgae. J Gen Microbiol 116: 495–500. Cerniglia CE, DW Kelley, JP Freeman, DW Miller (1986) Microbial metabolism of pyrene. Chem-Biol Interactions 57: 203–216. Cerniglia CE, DT Gibson, C van Baalen (1982a) Naphthalene metabolism by diatoms isolated from the Kachemak Bay region of Alaska. J Gen Microbiol 128: 987–990. Cerniglia CE, JP Freeman, FE Evans (1984a) Evidence for an arene oxide-NIH shift pathway in the transformation of naphthalene to 1-naphthol by Bacillus cereus. Arch Microbiol 138: 283–286. Cerniglia CE, JP Freeman, RK Mitchum (1982b) Glucuronide and sulfate conjugation in the fungal metabolism of aromatic hydrocarbons. Appl Environ Microbiol 43: 1070–1075. Cerniglia CE, JR Althus, FE Evans, JP Freeman, RK Mitchum, SK Yang (1983) Stereochemistry and evidence for an arene oxide-NIH shift pathway in the fungal metabolism of naphthalene. Chem-Biol Interactions 44: 119–132. Cerniglia CE, KL Lambert, DW Mille, JP Freeman (1984b) Transformation of 1- and 2-methylnaphthalene by Cunninghamella elegans. Appl Environ Microbiol 47: 111–118. Cerniglia CE, PP Fu, SK Yang (1982c). Metabolism of 7-methylbenz[a]anthracene and 7-hydroxymethylbenz [a]anthracene by Cunninghamella elegans. Appl. Environ. Microbiol. 44: 682–689. Cerniglia CE, RH Dodge, DT Gibson (1982d) Fungal oxidation of 3-methylcholanthrene: formation of proximate carcinogenic metabolites of 3-methylcholanthrene. Chem-Biol Interactions 38: 161–173. Cerniglia CE, RL Herbert, PJ Szaniszlo, DT Gibson (1978) Fungal metabolism of naphthalene. Arch Microbiol 117: 135–143. Cerniglia CE, SA Crow (1981) Metabolism of aromatic hydrocarbons by yeasts. Arch Microbiol 129: 9–13. Cerniglia CE, SK Yang (1984) Stereoselective metabolism of anthracene and phenanthrene by the fungus Cunninghamella elegans. Appl. Environ. Microbiol. 47: 119–124. Cerniglia CE, C van Baalen, DT Gibson (1980b) Oxidation of biphenyl by the cyanobacterium, Oscillatoria sp. strain JCM. Arch Microbiol 125: 203–207. Cerniglia CE, WL Campbell, JP Freeman, FE Evans (1989) Identiication of a novel metabolite in phenanthrene metabolism by the fungus Cunninghamella elegans. Appl Environ Microbiol 55: 2275–2279. Coates JD, J Woodward, J Allen, P Philip, DR Lovley (1997) Anaerobic degradation of polycyclic aromatic hydrocarbons and alkanes in petroleum-contaminated marine harbor sediments. Appl Environ Microbiol 63: 3589–3593. Coates JD, RT Anderson, DR Lovley (1996) Oxidation of polycyclic aromatic hydrocarbons under sulfatereducing conditions. Appl Environ Microbiol 62: 1099–1101. Cremonesi P, EL Cavalieri, EG Rogan (1989) One-electron oxidation of 6-substituted benzo[a]pyrenes by manganic acetate : a model for metabolic activation. J Org Chem 54: 3561–3570. Dalton H, BT Gording, BW Watyers, R Higgins, JA Taylor (1981) Oxidations of cyclopropane, methylcyclopropane, and arenes with the monooxygenase system from Methylococccus capsulatus. J Chem Soc Chem Commun 482–483. Daly JW, DM Jerina, B Witkop (1972) Arene oxides and the NIH shift: the metabolism, toxicity and carcinogenicity of aromatic compounds. Experientia 28: 1129–1149. Demanèche S, C Meyer, J Micoud, M Louwagie, JC Wilson, Y Jouanneau (2004) Identiication and functional analysis of two ring-hydroxylating dioxygenases from a Sphingomonas strain that degrades various polycyclic aromatic hydrocarbons. Appl Environ Microbiol 70: 6714–6725. Dodge RH, CE Cerniglia, DT Gibson (1979) Fungal metabolism of biphenyl. Biochem J 178: 223–230. Dunn NW, HM Dunn, RA Austen (1980) Evidence for the existence of two catabolic plasmids coding for the degradation of naphthalene. J Gen Microbiol 117: 529–533.

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PART 3 AROMATIC CARBOXYLATES, CARBOXALDEHYDES, AND RELATED COMPOUNDS INTRODUCTION Catechols, benzoates, and hydroxylated benzoates are intermediates in the aerobic degradation of aromatic hydrocarbons. The irst stage in their degradation is the introduction of the elements of dioxygen into the ring, either both atoms by dioxygenation or only one atom by monooxygenation. The second stage involves ission of the ring by another group of dioxygenases. Details of these oxygenases are given in Chapter 3, Part 1. The anaerobic degradation of benzoate is carried out by different reactions involving hydrogenation of the ring.

BENZOATES Aerobic Conditions Mechanisms for the Initial Oxygenation Benzoate is generally degraded to catechol by dioxygenation with loss of the carboxyl group. For benzoates substituted at the ortho position with amino or halogen groups, dioxygenation involves the loss of both the carboxyl and amino groups or both the carboxyl and halogen groups. In contrast to arene hydrocarbons, dehydrogenation is not, therefore, required for the formation of catechols. The formation of 1-hydroxynaphthalene-2-carboxylate from naphthalene-2-carboxylate was apparently not via (1R,2S)-cis-1,2-dihydro-1,2-dihydroxynaphthalene-2-carboxylate (Morawski et al. 1997). This is supported by the activity of naphthalene dioxygenase in which both activities are catalyzed by the same enzyme (Gibson et al. 1995). The degradation of halogenated benzoates, arenesulfonates, and nitroarenes, by dioxygenation is discussed in Chapter 9, Parts 1, 3 through 5. Benzoate Dioxygenase In Acinetobacter calcoaceticus, the enzyme is chromosomal and consists of a hydroxylase and an electron transport protein that have been designated benAB and benC (Neidle et al. 1991). The corresponding genes are designated xylXY and xylZ in the plasmid-encoded toluate dioxygenase in Pseudomonas putida, and this dioxygenase accepts a much wider range of substrates.

Carbocyclic Aromatic Compounds without Halogen Substituents

425

Anthranilate-1,2-Dioxygenase In Acinetobacter sp. strain ADP1 (Eby et al. 2001), this enzyme catalyzes the dioxygenation of anthranilate with the loss of both the amino and carboxyl groups. This, like the enzyme from Pseudomonas putida and P. aeruginosa, is a two-component enzyme consisting of an oxygenase and a reductase, whereas the enzyme from Burkholderia cepacia DBO1 consists of three components—a two-subunit oxygenase, a ferredoxin, and a reductase (Chang et al. 2003). Anthranilate may also be hydroxylated to 5-hydroxyanthranilate, and 2,5-dihydroxybenzoate by anthranilate-5-hydroxylase in Nocardia opaca (Cain 1968) and in Ralstonia sp. strain U2 (Zhou et al. 2002), or to 2,3-dihydroxybenzoate in Trichosporon cutaneum (Powlowski et al. 1987) and Aspergillus niger (Subramanian and Vaidyanathan 1984). 2-Halobenzoate 1,2-Dioxygenases These are multicomponent enzymes that catalyze dioxygenation with the loss of the halogen and the carboxyl groups, and are discussed in Chapter 9, Part 1. The application of cis-arene dihydrodiols has been noted in Part 1 of this chapter, and it is suficient to note here the application of a mutant of Alcaligenes eutrophus strain B9 that is blocked in the degradation of benzoate (and some halogenated benzoates). This produced the cis-1,2-dihydrodiol (Reiner and Hegeman 1971), and has been used as the source of ring B for the synthesis of a range of tetracyclines (Charest et al. 2005). A range of substituted cis-dihydrodiols has been produced, and it has been shown that for 3-substituted benzoates both 3- and 5-substituted cis-dihydrodiols were formed (Reineke et al. 1978).

HYDROXYBENZOATES AND RELATED COMPOUNDS Phenols and hydroxybenzoates are generally degraded by monooxygenation. Illustrative examples include the following: 1. The degradation of salicylate to catechol is initiated by monooxygenation accompanied by decarboxylation (salicylate-1-hydroxylase), and two different and independent salicylate hydroxylases have been found in the naphthalene-degrading Pseudomonas stutzeri AN10 (Bosch et al. 1999). Alternatively, in Rhodococcus sp. strain B4, salicylate is hydroxylated to 2,5-dihydroxybenzoate by salicylate-5-hydroxylase (Grund et al. 1992). An alternative occurs for 5-hydroxy- and 5-aminosalicylate in Pseudaminobacter salicylatoxidans in which ring ission is accomplished directly (Hintner et al. 2001). 2. The monooxygenase from Pseudomonas luorescens that converts 4-hydroxybenzoate into 3,4-dihydroxybenzoate before ring ission has been characterized (Howell et al. 1972). 3. In Pseudomonas putida, the hydroxylation of 4-hydroxyphenylacetate to 3,4-dihydroxyphenylacetate is carried out by an enzyme that consists of a lavoprotein and a coupling factor (Arunachalam et al. 1992). At least in Escherichia coli, it has been suggested that the large component is an FADH2-utilizing monooxygenase (Xun and Sandvik 2000; Chaiyen et al. 2001). 4. The irst enzyme in the degradation of 2-hydroxybiphenyl by Pseudomonas azelaica strain HBP1 is an FAD-dependent monooxygenase that produces 2,3-dihydroxybiphenyl (Suske et al. 1999). Hydroxylation to 1,4-dihydroxy compounds may also activate the ring to oxidative ission. This is illustrated by the following examples of the gentisate pathway: a. The degradation of 3-methylphenol, 3-hydroxybenzoate and salicylate can be initiated by hydroxylation to 2,5-dihydroxybenzoate (gentisate). The range of organisms includes species of Pseudomonas, and Bacillus (Crawford 1975a), and the enteric bacteria Salmonella typhimurium (Goetz and Harmuth 1992) and Klebsiella pneumoniae

426

Environmental Degradation and Transformation of Organic Chemicals HO2C

CO2H

CO−CO2H

CO2H

CO2H CO2H CO−CO2H

HO OH

HO2C

OH

OH OH CO2H CO2H

FIGURE 8.26

The gentisate pathway.

(Jones and Cooper 1990). Gentisate dioxygenase carries out ission of the ring to produce pyruvate, and fumarate or maleate (Figure 8.26). Its distribution is noted later. b. The gentisate pathway is used for the degradation of salicylate produced from naphthalene by a Rhodococcus sp. strain B4 (Grund et al. 1992), rather than by the more usual sequence involving the hydroxylative decarboxylation of salicylate to catechol. c. An analogous pathway is used for the degradation of 5-aminosalicylate that is an intermediate in the degradation of 6-aminonaphthalene-2-sulfonate. Direct ring ission of both 5-aminosalicylate and 5-hydroxysalicylate can be accomplished by a salicylate 1,2-dioxygenase in Pseudaminobacter salicylatoxidans (Hintner et al. 2001). d. The gentisate pathway may plausibly be involved in the degradation of benzoate by a denitrifying strain of Pseudomonas sp. in which the initial reaction is the formation of 3-hydroxybenzoate (Altenschmidt et al. 1993). Unusual pathways have been found in the bacterial degradation of a number of 4-hydroxybenzoates and related compounds, and in some of them rearrangements (NIH shifts) are involved: 1. In Pseudomonas putida, l-phenylalanine is hydroxylated to tyrosine by a reaction that involves 6,7-dimethyltetrahydrobiopterin, which is converted into 4a-carbinolamine (Song et al. 1999). Tyrosine is then transformed to 2,5-dihydroxyphenylacetate followed by ring ission (Arias-Barrau et al. 2004). 2. Gentisate is formed by a strain of Bacillus sp. in an unusual rearrangement from 4-hydroxybenzoate (Crawford 1976) that is formally analogous to the formation of 2,5-dihydroxyphenylacetate from 4-hydroxyphenylacetate by Pseudomonas acidovorans (Hareland et al. 1975). Similarly, the metabolism of 4-hydroxybenzoate by the archaeon Haloarcula sp. strain D1 involves the formation of 2,5-dihydroxybenzoate (Fairley et al. 2002). All these reactions putatively involve an NIH shift. 3. The degradation of 4-hydroxyphenylacetate by Pseudomonas acidovorans takes place by hydroxylation with the production of 2,5-dihydroxyphenylacetate in a reaction involving an NIH shift. The inal products are fumarate and acetate, and the enzyme has been characterized (Hareland et al. 1975). In contrast, the degradation of 3,4-dihydroxyphenylacetate by the same organism takes place by extradiol ission to produce pyruvate and succinate semialdehyde (Sparnins and Dagley 1975). 4. Pseudomonas sp. strain P.J. 874 grown with tyrosine carried out dioxygenation of 4hydroxyphenylpyruvate to 2,5-dihydroxyphenylacetate accompanied by an NIH shift (Lindstedt et al. 1977). The involvement of a high-spin ferric center coordinated with tyrosine is conclusively revealed in the primary structure of the enzyme (Rüetschi et al. 1992).

427

Carbocyclic Aromatic Compounds without Halogen Substituents

5. The chlorophenol-4-hydroxylase from Burkholderia cepacia strain AC1100 is able to bring about not only the transformation of 4-hydroxybenzaldehydes to the expected 4-hydroxybenzoates, but also rearrangement to 2,5-dihydroxybenzaldehydes (Martin et al. 1999) (Figure 8.27). 6. The degradation of nonylphenol isomers with quaternary side chains in strains of Sphingomonas sp. displays unusual features that involve rearrangement of the side chain (Corvini et al. 2004; Gabriel et al. 2005a,b). This is discussed in Part 4 of this chapter. Both fungi and yeasts are able to degrade simpler substituted aromatic compounds such as vanillate (Ander et al. 1983) (Figure 8.28) and 3,4-dihydroxybenzoate (Anderson and Dagley 1981), both of which involve concomitant decarboxylation and hydroxylation. The oxidative decarboxylation of a range of 4-hydroxybenzoates to 1,4-dihydroxy compounds has been examined, and is carried out by an FAD-dependent monooxygenase in Candida parapsilosis CBS604 (Eppink et al. 1997). The yeast Trichosporon cutaneum is able to metabolize phenol and a number of other aromatic compounds. The pathways by which this is accomplished differ, however, from those that are operative in most bacteria. Illustrative examples include the following (Anderson and Dagley 1980): a. Benzoate is degraded by successive hydroxylation at the 4- and 3-positions followed by concomitant hydroxylation and decarboxylation to benzene-1,2,4-triol, while an analogous pathway is used for 2,5-dihydroxybenzoate. In contrast, 2,3-dihydroxybenzoate is decarboxylated to catechol without hydroxylation. b. The benzene-1,2,4-triol undergoes intradiol ring ission followed by reduction to 3-ketoadipate and incorporation into the TCA cycle.

OH

OH R

R

R

OH R

R

R

or CHO OH

CH O

CO2H

FIGURE 8.27 Anaerobic rearrangement of 4-hydroxybenzaldehydes.

CO2H

OH

OCH3

OH

OCH3

OH

OH

OH

O

O O

O

OH

CO2H CO2H

OH

FIGURE 8.28 Biodegradation of vanillic acid by fungi.

CO2H CO2H

428

Environmental Degradation and Transformation of Organic Chemicals

c. Analogous hydroxylations are used to initiate the metabolism of phenylacetate and 4hydroxyphenyl acetate. Fission of the rings takes place between the ortho hydroxyl group and the –CH2–CO2H group to produce acetoacetate, and fumarate or oxalacetate. Mechanisms for Fission of Oxygenated Rings Catechols In the degradation of the catechols, the next step is the dioxygenation and ission of the ring, either by extradiol (2:3) or intradiol (1:2) ring ission. The intradiol and extradiol enzymes are quite speciic for their respective substrates, and whereas all of the irst group contain Fe3+, those of the latter contain Fe2+ (Wolgel et al. 1993). Although the extradiol 2,3-dihydroxybiphenyl 1,2-dioxygenases in Rhodococcus globerulus strain P6 are typical in containing Fe (Asturias et al. 1994), the enzyme from Bacillus sp. strain JF8 is manganese-dependent (Hatta et al. 2003). A few other manganesedependent ring-ission dioxygenases have been observed for 3,4-dihydroxyphenylacetate in Arthrobacter globiformis (Boldt et al. 1995) and Bacillus brevis (Que et al. 1981). After formation of the 1,2-dihydroxy compounds, ring ission is mediated by 1:2 (intradiol ission) or 2:3 (extradiol and distal ission) dioxygenases. There are, however, important variations in the pathways used by various groups of microorganisms: 1. The pathways and their regulation during the degradation of catechol and 3,4-dihydroxybenzoate in Pseudomonas putida have been elucidated in extensive studies (Ornston 1966). In this organism, intradiol ring ission is carried out by a 3,4-dioxygenase to produce 3-ketoadipate (Figure 8.29). The stereochemistry of the reactions after ring ission has been examined in detail (Kozarich 1988), and the regulation and genetics in a range of organisms have been reviewed (Harwood and Parales 1996). In contrast, 3,4,5-trihydroxybenzoate (gallate) is degraded in P. putida by extradiol ission with the production of 2 moles of pyruvate (Sparnins and Dagley 1975). 2. In the degradation of 3-hydroxybenzoate, divergent pathways are used by different groups of pseudomonads: a. Pseudomonas testosteroni uses 4,5-dioxygenase to produce pyruvate and formate from 3,4-dihydroxybenzoate by extradiol ission (Figure 8.30a) (Wheelis et al. 1967). The degradation involves pyrone-4,6-dicarboxylate that was converted by a hydrolase into the open-chain 2-hydroxy-4-carboxymuconic acid that was produced directly by extradiol ission from gallate by the same enzyme (Kersten et al. 1982); b. Pseudomonas acidovorans produces 2,5-dihydroxybenzoate that is degraded by gentisate 1,2-dioxygenase to fumarate and pyruvate, which has already been noted (Figure 8.26), and two different gentisate dioxygenases have been characterized (Harpel and Lipscomb 1990). 3. The third alternative for ring ission of 3,4-dihydroxybenzoate is exempliied by Bacillus macerans and B. circulans that use a 2,3-dioxygenase to accomplish this (Figure 8.30b) HO2C

OH

HO2C

CO2H

OH

HO

O

O

O

CO2H

CO2H

CH2CO2H O

FIGURE 8.29 The β-ketoadipate pathway.

CO2H

CH2CO2H CO2H

CO2H + CO2H

CH3CO2H

429

Carbocyclic Aromatic Compounds without Halogen Substituents CO2H HO2C

CHO

(a)

CO 2 H

OH

OH

OH CO2H

CO2H

(b) OH OH

CH3−CO−CO2H + H−CO2H

OH

CHO

CHO

CO2H

CO2H

CH3−CO−CO2H + CH3−CHO

OH

FIGURE 8.30 Biodegradation of 3,4-dihydroxybenzoate mediated by (a) 4,5-dioxygenase in Pseudomonas testosteroni and (b) 2,3-dioxygenase in Bacillus macerans.

(Crawford 1975a,b, 1976). In addition, a 2,3-dioxygenase is elaborated by Gram-negative bacteria for the degradation of 3,4-dihydroxyphenylacetate (Sparnins et al. 1974), and by Gram-positive bacteria for the degradation of l-tyrosine via 3,4-dihydroxyphenylacetate (Sparnins and Chapman 1976). 4. The enzymes of alternative pathways may be induced in a given strain by growth with different substrates; for example, growth of Pseudomonas putida R1 with salicylate induces enzymes of the extradiol ission pathway, whereas growth with benzoate induces those of the intradiol pathway (Chakrabarty 1972). As a broad generalization, the extradiol ission is preferred for the degradation of more complex compounds such as toluene, naphthalene, and biphenyl (Furukawa et al. 1983). Methoxybenzoates and Related Compounds Studies on the degradation of lignin have attracted interest in the degradation of the monomeric vanillate and syringate, and mechanisms for their de-O-methylation are given in Chapter 11, Part 2. For substrates such as vanillate and isovanillate, degradation is initiated by de-O-methylation, followed in Comamonas testosteroni by extradiol ission (Providenti et al. 2006). 3-O-methylgallate occupies a central position in several degradations such as that of (a) 4-hydroxy-3-methoxymandelate by Acinetobacter lwofii (Sze and Dagley 1987), (b) syringate by Sphingomonas paucimobilis SYK-6 (Kasai et al. 2004), and (c) 3,4,5-trimethoxybenzoate by Pseudomonas putida (Donnelly and Dagley 1980). In all of them, dioxygenation carries out extradiol ring ission to an ester that may undergo cyclization to 2-pyrone-4,6-dicarboxylate with the loss of methanol, and degradation of 4-oxalomesaconitate to pyruvate and oxalacetate (Figures 8.31a through 8.31c). 2-Hydroxybenzoate and 1-Hydroxynaphthalene-2-Carboxylate Salicylate is generally degraded by monooxygenation and decarboxylation mediated by salicylate1-hydroxylase to catechol (White-Stevens et al. 1972 a,b), although monooxygenation without decarboxylation can be carried out by salicylate-5-hydroxylase to produce 2,5-dihydroxybenzoate (Zhou et al. 2002). The degradation of naphthalene-2-carboxylate by Burkholderia sp. strain JT 1500 involves the formation of 1-hydroxynaphthalene-2-carboxylate rather than initial oxidative decarboxylation. Naphthalene-1,2-dihydrodiol-2-carboxylate is not, however, involved; hence, the reaction is possibly carried out either by a monooxygenase, or a dehydration step is involved. Subsequent reactions produced pyruvate and o-phthalate, which was degraded via 4,5dihydroxyphthalate (Morawski et al. 1997).

430

Environmental Degradation and Transformation of Organic Chemicals CH−CO2H

CH(OH)CO2H

OMe

CO2H

MeO

OH

CH

OMe

MeO

OH (a)

OMe MeO

(b)

(c)

CO2H

HO

OMe OH

CO2H

OH

HO2C

CO2Me

HO2C−CO

CO2H

HO2C

O

FIGURE 8.31

CO2H

CO2H

CH3COCO2H

+

HO2C−CO−CH2CO2H

O

Degradation of 3-O-methylgallate.

Fission of 1,4-Dihydroxybenzoates Gentisate (2,5-dihydroxybenzoate) is produced from a range of substrates and has already been noted. Fission of the ring is carried out by gentisate 1,2-dioxygenase that has been characterized from a range of organisms including Moraxella osloensis (Crawford et al. 1975); Pseudomonas testosteroni and P. acidovorans (Harpel and Lipscomb 1990); P. alcaligenes and P. putida (Feng et al. 1999); Sphingomonas sp. strain RW 5 (Wergath et al. 1998); and Klebsiella pneumoniae (Suárez et al. 1996). Nonoxidative Decarboxylation of Benzoate and Related Compounds Although benzoate is generally metabolized by simultaneous dioxygenation and decarboxylation to catechol followed by ring ission, nonoxidative decarboxylation of hydroxybenzoates has been observed. Important issues include the following: (a) the reaction is carried out both by aerobic and anaerobic bacteria, (b) it may be reversible, (c) some of the enzymes—even from aerobes—are oxygen-sensitive, and (d) a high degree of speciicity is often observed. 1. Strains of Bacillus megaterium and Streptomyces sp. strain 179 transformed vanillate to guaiacol by decarboxylation (Crawford and Olson 1978), and the gene cluster encoding decarboxylation in Streptomyces sp. strain m D7 has been characterized (Chow et al. 1999). 2. Decarboxylation of aromatic carboxylic acids has been encountered extensively in facultatively anaerobic Enterobacteriaceae. For example, 4-hydroxycinnamic acid is

Carbocyclic Aromatic Compounds without Halogen Substituents

431

CO2H

OMe

OMe OH

FIGURE 8.32

OH

Decarboxylation of ferulic acid (3-methoxy-4-hydroxycinnamic acid).

decarboxylated to 4-hydroxystyrene, and ferulic acid (3-methoxy-4-hydroxycinnamic acid) to 4-vinylguaiacol by several strains of Hafnia alvei and H. protea, and by single strains of Enterobacter cloacae and K. aerogenes (Figure 8.32) (Lindsay and Priest 1975). The enzyme has been puriied from Bacillus pumilis (Degrassi et al. 1995). 3. The degradation of 2,2′-dihydroxy- 3,3′-dimethoxybiphenyl-5,5′-dicarboxylate (5,5′-dehydrodivanillate) by Sphingomonas paucimobilis SYK-6 proceeds by partial de-O-methylation followed by extradiol ission of the catechol to 2-hydroxy-3-methoxy-5-carboxybenzoate. Diversion of this into central metabolic pathways involves decarboxylation to vanillate by two separate decarboxylases LigW1 and LigW2 (Peng et al. 2005). 4. Decarboxylation is an important step in the degradation of phthalates. The degradation of o- and p-phthalate (terephthalate) has been examined in strains of both Gram-negative and Gram-positive bacteria, and the genetics has been established (references in Sasoh et al. 2006). In summary, degradation is accomplished by dioxygenation followed by dehydrogenation and decarboxylation: a. Dioxygenation initiates the degradation of o-phthalate by Pseudomonas cepacia. A two-component enzyme consisting of a nonheme iron oxygenase and an NADH-dependent oxidoreductase containing FMN and a [2Fe–2S] ferredoxin (Batie et al. 1987) produces the 4,5-dihydrodiol. Degradation is completed by dehydrogenation, decarboxylation (Pujar and Ribbons 1985) to 3,4-dihydroxybenzoate, and ring ission to 2-carboxymuconate. The pathway for the degradation of o-phthalate in Micrococcus sp. strain 12B differs by the initial formation of the 3,4-dihydrodiol followed by dehydrogenation and decarboxylation to 3,4-dihydroxybenzoate (Eaton and Ribbons 1982). The degradation of 4-methyl-o-phthalate by P. luorescens strain JT701 follows the same pathway by formation of the 2,3-dihydrodiol, followed by decarboxylation with the formation of 4-methyl-2,3-dihydroxybenzoate and extradiol ring ission (Ribbons et al. 1984). b. 3,4-dihydroxybenzoate is produced by an analogous pathway during the degradation of p-phthalate by Comamonas sp. strain T-2 via (Schäli et al. 1994), and of 5-hydroxyisophthalate via 4,5-dihydroxyisophthalate (Elmorsi and Hopper 1979). The phthalate dioxygenase from Pseudomonas cepacia is also active with pyidine-2,3and 3,4-dicarboxylates (Batie et al. 1987), and this is substantiated in growth experiments in which different strains were able to metabolize pyridine-2,6-, 2,5-, and 2,3-dicarboxylate (Taylor and Amador 1988). It has been shown that there are two regions of DNA that encode the enzymes for o-phthalate degradation, with the gene encoding quinolinate phosphoribosyl transferase located between them, and insertional knockout mutants with elevated levels of this enzyme enhanced growth on o-phthalate (Chang and Zylstra 1999). 5. The reversible decarboxylation of 4-hydroxybenzoate and 3,4-dihydroxybenzoate has been described in Sedimentibacter (Clostridium) hydroxybenzoicum (He and Wiegel 1996), and the oxygen-sensitive enzyme has been puriied. The decarboxylase from Pantoae

432

Environmental Degradation and Transformation of Organic Chemicals

agglomerans, which is speciic for 3,4,5-trihydroxybenzoate (gallate), is also oxygensensitive (Zeida et al. 1998). 6. The decarboxylase in Clostridium thermoceticum produces CO2 that is essential for growth, and under CO2 limitation, CO2 provides both the methyl and the carboxyl groups of acetate (Hsu et al. 1990). Alternative Pathways for the Degradation of Benzoates and Related Compounds Unusual reactions have been encountered in the aerobic degradations carried out by Azoarcus evansii and Geobacillus stearothermophilus (Zaar et al. 2001). The anaerobic degradation of benzoate by Azoarcus evansii (Ebenau-Jehle et al. 2003) and Thauera aromatica (Dörner and Boll 2002), and of 3-hydroxybenzoate by Th. aromatica (Laempe et al. 2001) is discussed later. 1. a. Aerobic degradation of benzoate in Azoarcus evansii takes place via the CoAester to produce ∆1,2-adipate and 3-ketoadipate, that is degraded to CoA-esters of succinate and acetate (Zaar et al. 2001; Gescher et al. 2002) (Figure 8.33). The initial dihydrodiol has been characterized using 13C NMR, and the enzyme that carries this out consists of two components: BoxA that is an Fe-S protein and functions as a reductase, and BoxB that functions as an oxygenase (Zaar et al. 2004). Fission of the dihydrodiol is mediated by a lyase BoxC that is not dependent on oxygen and results in the production of formate from C-2 (Gescher et al. 2005). The product from dehydrogenation by BoxD is then converted into 3-ketoadipate by conventional steps (Gescher et al. 2006). b. Burkholderia xenovorans strain LB400 uses several pathways for the degradation of the benzoate produced by degradation of biphenyl. One of them is the classical benzoate dihydroxylation/catechol intradiol ission pathway, while another resembles the pathway that is used by Azoarcus evansii. The genes for this pathway occur both in the chromosome when they are expressed during growth with biphenyl, and in a megaplasmid copy where they were detected only in benzoate-grown cells in the transition to the stationary phase (Denef et al. 2005). 2. Novel pathways for the aerobic degradation of anthranilate (2-aminobenzoate) were described several years ago in a strain then designated as a Pseudomonas sp. (Lochmeyer et al. 1992; Altenschmidt and Fuchs 1992), and now reassigned to Azoarcus evansii. The pathway is analogous to that used for benzoate by this strain. This is initiated by formation of the benzoyl SCoA-ester followed by monooxygenation/ reduction to 2-amino-5-ketocyclohex-1-ene that undergoes β-oxidation with a concomitant NIH shift of the hydrogen at C5 to C6 (Hartmann et al. 1999; Schühle et al. 2001) (Figure 8.34).

CO−SCoA

CO−SCoA

CO−SCoA

CO−SCoA

OH CHO

OH

CO2H

CO−SCoA

CO−SCoA O CO2H

FIGURE 8.33

CO2H

Alternative aerobic degradation of benzoyl-CoA by Azoarcus evansii.

433

Carbocyclic Aromatic Compounds without Halogen Substituents R N

N H

CoS−SCoA N

NH2

O

H

N

HO

O O OH

Co−SCoA H

NH2 +

NADH

O

NH2

H

H

O H

FIGURE 8.34

NH2 H

Co−SCoA H

CoS−CoA

H

H

Aerobic degradation of 2-aminobenzoate by Azoarcus evansii.

AEROBIC REDUCTION OF ARENE CARBOXYLATES The reduction of aromatic carboxylic acids to the corresponding aldehydes under aerobic conditions is of interest in biotechnology, since the oxidoreductase from Nocardia sp. is able to accept a range of substituted benzoic acids, naphthoic acids, and a few heterocyclic carboxylic acids (Li and Rosazza 1997). The reaction involves formation of an acyl-AMP intermediate by reaction of the carboxylic acid with ATP; NADPH then reduces this to the aldehyde (Li and Rosazza 1998; He et al. 2004). A comparable reaction for aromatic carboxylates has been demonstrated in Neurospora crassa (Gross 1972).

ARENES WITH AN OXYGENATED C2 OR C3 SIDE CHAIN Several pathways are used for the aerobic degradation of aromatic compounds with an oxygenated C2 or C3 side chain. These include acetophenones and reduced compounds that may be oxidized to acetophenones, and compounds including tropic acid, styrene, and phenylethylamine that can be metabolized to phenylacetate, which has already been discussed. 1. The mandelate pathway in Pseudomonas putida involves successive oxidation to benzoyl formate and benzoate, which is further metabolized via catechol and the 3-ketoadipate pathway (Figure 8.35a) (Hegeman 1966). Both enantiomers of mandelate were degraded through the activity of a mandelate racemase (Hegeman 1966), and the racemase (mdlA) is encoded in an operon that includes the next two enzymes in the pathway—S-mandelate dehydrogenase (mdlB) and benzoylformate decarboxylase (mdlC) (Tsou et al. 1990). A formally comparable pathway is used by a strain of Alcaligenes sp. that degrades 4-hydroxyacetophenone to 4-hydroxybenzoyl methanol, which is oxidized in an unusual reaction to 4-hydroxybenzoate and formate. The 4-hydroxybenzoate is then metabolized to 3-ketoadipate via 3,4-dihydroxybenzoate (Figure 8.35b) (Hopper et al. 1985). 2. Although the metabolism of vanillate generally involves de-O-methylation to 3,4-dihydroxybenzoate followed by intradiol ring ission, in Acinetobacter lwofii vanillate is hydroxylated to 3-O-methyl gallate, which produces pyruvate and oxalacetate in reactions that have already been noted (Sze and Dagley 1987). 3. The metabolism of ferulate to vanillin by Pseudomonas luorescens strain AN103 is carried out by an enoyl-SCoA hydratase/isomerase rather than by oxidation, and the enzyme belongs to the enoyl-CoA hydratase superfamily (Gasson et al. 1998).

434

Environmental Degradation and Transformation of Organic Chemicals CO2H

CO2H

CH(OH)

CO

CO2H

OH OH

(a)

CH3

CH2OH

CO

CO

CO2H

CO2H

OH

OH

OH

OH

(b) OH

CH3 CO

O−COCH3

OH

(c)

FIGURE 8.35 Degradation of (a) mandelate, (b) 4-hydroxyacetophenone by side-chain oxidation pathways, (c) acetophenone by Baeyer–Villiger monooxygenation.

4. A strain of Pseudomonas sp. AT3 degraded tropic acid, which has a –CH–(CH2OH)– CO2H side chain to phenylacetate (Long et al. 1997). 5. Baeyer–Villiger-type oxidations initiate the degradation of acetophenone by strains of Arthrobacter sp. and Nocardia sp. (Cripps et al. 1978), and of 4-hydroxyacetophenone by Pseudomonas putida strain JD1 (Darby et al. 1987). Acetophenone is converted into phenyl acetate, which is hydrolyzed to phenol and then hydroxylated to catechol before ring ission (Figure 8.35c). Similarly, 4-hydroxyacetophenone is oxidized to 4hydroxyphenyl acetate, which is hydrolyzed to 1,4-dihydroxybenzene before ring ission to 3-ketoadipate. The 4-hydroxyacetophenone monooxygenase from Pseudomonas luorescens has been puriied from recombinant Escherichia coli, and was able to carry out Baeyer–Villiger oxidation of a range of substituted acetophenones, bicyclic cyclobutanones, and the enantiomerically speciic oxidation of methyl aryl sulides to sulfoxides (Kamerbeek et al. 2003). The metabolism of chloroacetophenones takes place by analogous monooxygenation to the corresponding chlorophenylesters. Some ortho-substituted chlorophenols are, however, inhibitory, and only low rates of oxidation have been encountered with di- and trichlorinated acetophenones, so that growth with them is not possible (Higson and Focht 1990). However, degradation of 4-chloroacetophenone has been demonstrated with a mixed culture of an Arthrobacter sp. and a Micrococcus sp. (Havel and Reineke 1993). 6. Phenylalanine-ammonia lyase (PAL), which catalyzes the nonoxidative deamination of l-phenylalanine to trans-cinnamate, is widespread among plants as a precursor of lignins, lavanoids, and coumarins but is uncommon among bacteria. The gene has been characterized in “Streptomyces maritimus” (Xiang and Moore 2002), and the homologous l-histidine ammonia lyase that produces trans-urocanate from l-histidine is the irst enzyme in the pathway for the bacterial degradation of l-histidine.

435

Carbocyclic Aromatic Compounds without Halogen Substituents CO2H

CH2

COSCoA COSCoA OH OH

COSCoA

COSCoA CH3COSCoA +

O

FIGURE 8.36

CO2H

CO2H

Aerobic degradation of phenylacetate.

7. Some unusual reactions have emerged in the degradation of phenylacetate and 3-phenyl butyrates: a. The degradation of hydroxylated phenylacetates and related compounds such as tyrosine has been described. These include 3,4-dihydroxyphenylacetate by Escherichia coli (Cooper and Skinner 1980), and 2,5-dihydroxyphenylacetate produced by rearrangement of 4-hydroxyphenylacetate in Xanthobacter sp. strain 124X (van der Tweel et al. 1986). However, these are not intermediates in the degradation of phenylacetate, and an important alternative for this has been described. The degradation of phenylacetate by Escherichia coli is carried out by a pathway, which has been elucidated in detail using 13C NMR of the labeled substrate (Ismail et al. 2003). It is initiated by the formation of the coenzyme A-ester, and continues with the formation of a 1,2-diol, which undergoes reduction and ission of the ring (Figure 8.36) in reactions that are formally analogous to the oxygenation/reduction in the degradation of benzoate by Azoarcus evansii. This pathway is also followed by Escherichia coli strain W (Fernández et al. 2006) and Rhodococcus sp. strain RHA1, which has an established ability to degrade PCBs and a wide range of monocyclic aromatic compounds (Navarro-Llorens et al. 2005). b. Although the aerobic degradation of 3-phenylpropionate by Escherichia coli proceeded as expected by ring dioxygenation, dehydrogenation, and ring ission to pyruvate, succinate, and acetate (Díaz et al. 1998), the degradation of iboprofen (2-[4-isobutylphenyl]-propionic acid) with a −CH(CH3)CO2H side chain was different. The catechol produced by dioxygenation and dehydrogenation was succeeded exceptionally by loss of the side chain (Murdoch and Hay 2005), involving a hitherto unresolved mechanism. c. i. The degradation of 3-phenylbutyrate was examined in a strain of Pseudomonas sp. (Sariaslani et al. 1982). The formation of the expected catechol was proved by NMR analysis of its nonenzymatic transformation to a dihydrocoumarin, and characterization of the ring ission product by reaction with NH3 to produce a pyridine. In addition, however, products that were identiied by mass spectrometry (MS) included 3-phenylpropionate and 3-phenylacetate. It was tentatively suggested that the irst of these was produced by oxidation of the methyl group followed by decarboxylation, although the expected phenylsuccinate could not be utilized. ii. The degradation of (R)- and (S)-3-phenyl butyrate has been examined in Rhodococcus rhodochrous strain PB1. Whereas the (S)-enantiomer was dioxygenated to the 2,3dihydroxy compound that was not metabolized further, the (R)-enantiomer was converted into 3-phenylpropionate by a mechanism that was not established. This was followed by dioxygenation and ission of the ring to succinate (Simoni et al. 1996). Anaerobic Metabolism Considerable effort has been devoted to the anaerobic degradation of aromatic compounds. It is important to note that several distinct groups of organisms are involved: (a) strictly anaerobic

436

Environmental Degradation and Transformation of Organic Chemicals

fermentative bacteria, (b) strictly anaerobic photoheterotrophic bacteria, (c) anaerobic sulfate-reducing bacteria, and (d) organisms using nitrate as electron acceptor under anaerobic conditions. Pragmatically, these organisms generally belong to the following groups: methanogenic, sulidogenic, denitrifying, and phototrophic. Although the greatest attention is given here to studies using pure cultures and investigations in which the relevant enzymes have been characterized, some valuable examples from studies using mixed cultures are provided. Bacteria Using Nitrate Electron Acceptor under Anaerobic Conditions, and Anaerobic Phototrophs It has become clear that benzoate occupies a central position in the anaerobic degradation of both phenols and alkylated arenes such as toluene and xylenes, and that carboxylation, hydroxylation, and reductive dehydroxylation are important reactions for phenols that are discussed in Part 4 of this chapter. The simplest examples include alkylated benzenes, products from the carboxylation of napthalene and phenanthrene (Zhang and Young 1997), the decarboxylation of o-, m-, and p-phthalate under denitrifying conditions (Nozawa and Maruyama 1988), and the metabolism of phenols and anilines by carboxylation. Further illustrative examples include the following: 1. Under denitrifying conditions, 2-aminobenzoate is degraded by a Pseudomonas sp. to benzoate, which is then reduced to cyclohexene-1-carboxylate (Lochmeyer et al. 1992). 2. The metabolism of cinnamate and ω-phenylalkane carboxylates has been studied in Rhodopseudomonas palustris (Elder et al. 1992), and for growth with the higher homologs additional CO2 was necessary. The key degradative reaction was β-oxidation, for compounds with chain lengths of three, ive, and seven carbon atoms, benzoate was formed and further metabolized, but for the even-numbered compounds with four, six, and eight carbon atoms phenylacetate was a terminal metabolite. 3. The anaerobic metabolism of l-phenylalanine by Thauera aromatica under denitrifying conditions involves several steps that result in the formation of benzoyl-CoA: (a) conversion to the CoA-ester by a ligase, (b) transamination to phenylacetyl-CoA, (c) α-oxidation to phenylglyoxalate, and (d) decarboxylation to benzoyl-CoA (Schneider et al. 1997). An analogous pathway is used by Azoarcus evansii (Hirsch et al. 1998). The membrane-bound phenylacetyl-CoA: acceptor oxidoreductase that is induced under denitrifying conditions during growth with phenylalanine or phenylacetate has been puriied (Schneider and Fuchs 1998). The level of the enzyme was low in cells grown with phenylglyoxalate, the enzyme was insensitive to oxygen, and was absent in cells grown aerobically with phenylacetate. 4. Phenylacetate and 4-hydroxyphenylacetate are oxidized sequentially under anaerobic conditions by a denitrifying strain of Pseudomonas sp. to the phenylglyoxylates and benzoate (Mohamed et al. 1993). Benzoate The pathway for the anaerobic degradation of benzoate is entirely different from that used under aerobic conditions, and in contrast to degradation under aerobic conditions (with the exception of those carried out by Azoarcus evansii in which this is used under aerobic conditions), it invariably involves initial formation of the CoA-esters. The coenzyme A-ester is an inducer for both the anaerobic and aerobic pathways depending on the absence or presence of oxygen (Schüle et al. 2003). The pathway for its anaerobic degradation under denitrifying or phototrophic conditions involves three cardinal reactions: (1) formation of benzoyl-CoA, (2) partial reduction of the ring, and (3) ring ission (references in Harwood et al. 1999) (Figures 8.37a and 8.37b). The designation of the enzymes corresponds to those for the genes discussed below: 1. Formation of the coenzyme A thioester is mediated by a ligase, which has been demonstrated in a number of organisms including Pseudomonas sp. strain K172

437

Carbocyclic Aromatic Compounds without Halogen Substituents O

SCoA C

O

SCoA C

(b)

(a) O

SCoA

Dch

O

SCoA C

C HO

BadK

Had O

O

SCoA

SCoA C

C

OH

O

BadH O

O

SCoA C

O

SCoA C

OH

O

BadI

Oah

CO−SCoA CO2H CO−SCoA HO

FIGURE 8.37

Anaerobic degradation of benzoate.

CO2H

438

2.

3. 4.

5.

6.

Environmental Degradation and Transformation of Organic Chemicals

(Thauera sp. strain K172) (Dangel et al. 1991) and Rhodopseudomonas palustris (Egland et al. 1995). A benzoyl-CoA reductase reduces one or more of the double bonds in the aromatic ring (Gibson and Gibson 1992; Koch and Fuchs 1992). In Thauera aromatica, the reduction is mediated by a 2-ketoglutarate: ferredoxin oxidoreductase (Dörner and Boll 2002), whereas in Azoarcus evansii, a 2-ketoglutarate, NADP+ oxidoreductase is involved (Ebenau-Jehle et al. 2003). This has been suggested as a biomarker for the anaerobic degradation of aromatic compounds by developing degenerate primers from the established genes of Thauera aromatica and Azoarcus evansii. The isolated clones were then assigned to the bcr or bzd type of the reductase (Song and Ward 2005). The cyclohexa-1,5-dienecarboxylate thioester is hydrated to produce the 6-hydroxy compound (Boll et al. 2000). The pathways in T. aromatica and Rh. palustris differ slightly in details. a. In T. aromatica strain K172, the gene sequence for the following enzymes has been determined: bcrCBAD for the benzoyl-CoA reductase, dch for the dienyl-CoA hydratase, and had for 6-hydroxycyclohex-1-ene-1-carboxy-CoA dehydrogenase, and they occur in the order had, dch, bcrCBAD (Breese et al. 1998). b. In Rh. palustris, the genes are badDEFG for the benzoyl-CoA reductase, badK for the cyclohex-1ene-1-carboxyl-CoA hydratase, badH for the 2-hydroxycyclohexane1-carboxyl-CoA dehydrogenase, and badL for the ketohydrolase. They occur in the order badK, badL, badH, badD, badE, badF, badG, the irst three transcribing in the direction opposite to the others (Harwood et al. 1999; Egland and Harwood 1999). Fission of the ring: In T. aromatica, the initial ring ission product is hepta-3-ene-1,7dicarboxylyl-CoA formed by 3-ketoacyl-CoA hydrolase, which is encoded by oah that lies immediately to the right of had. The resulting 3-hydroxpimelyl-CoA is degraded by β-oxidation to glutaryl-CoA. With the minor modiications noted above, the same pathway has been demonstrated in Rhodopseudomonas palustris, and the ring ission enzyme 2-ketocyclohexanecarboxyl-CoA hydrolase that produces pimelyl-CoA has been puriied (Pelletier and Harwood 1998). The gene for the ring-ission enzyme badL lies to the left of badH. It has been shown in Rh. palustris that the suit of enzymes in the sequence from cyclohexen1-carboxylate onward was induced during growth on benzoate, though not on succinate (Perrotta and Harwood 1994). The further degradation of glutarate takes place through a pathway involving dehydrogenation and decarboxylation to crotonyl-CoA and subsequent formation of acetate (Härtel et al. 1993). After the growth of a denitrifying organism with either benzoate or pimelate, both glutaryl-CoA dehydrogenase and glutaconyl-CoA decarboxylase activities were induced—though not the enzymes leading from pimelyl-CoA to glutaryl-CoA. This is consistent with the involvement of 3-hydroxypimelyl-CoA in the degradation of benzoyl-CoA (Gallus and Schink 1994). The initial steps in the degradation of glutarate involving dehydrogenation, decarboxylation, and the β-oxidation pathway have also been demonstrated in other organisms that produce butyrate and isobutyrate (Matties and Schink 1992). Details of the various pathways for the anaerobic metabolism of acetate have been reviewed (Thauer et al. 1989).

Hydroxybenzoates There are different pathways for the degradation of hydroxybenzoates: 1. For hydroxybenzoates with hydroxyl groups at the ortho or meta positions, degradation is initiated by decarboxylation. a. For 2,6- and 3,5-dihydroxybenzoates, a denitrifying organism initiates degradation by decarboxylation to 1,3-dihydroxybenzene followed by the reduction of the ring to cylohexan-1,3-dione (Kluge et al. 1990);

Carbocyclic Aromatic Compounds without Halogen Substituents

439

b. For 3,4,5- and 2,4,6-trihydroxybenzoate, Pelobacter acidigalli carries out decarboxylation to 1,3,5-trihydroxybenzene followed by reduction of the ring (Brune and Schink 1992). 2. The degradation of 4-hydroxybenzoate by Thauera aromatica (Brackmann and Fuchs 1993) and by the anaerobic phototroph Rhodopseudomonas palustris (Gibson et al. 1997) is initiated by formation of the CoA-ester. The next step involves dehydroxylation to benzoate by a reductase that been characterized in both Thauera aromatica (Breese and Fuchs 1998) and Rh. palustris (Gibson et al. 1997). The benzoate that is produced then enters the established pathway for reduction of the ring (Heider et al. 1998). The degradation of 3-hydroxybenzoate by Sporotomaculum hydroxybenzoicum uses an analogous pathway (Müller and Schink 2000). 3. The fermentation of 3-hydroxybenzoate by Sporotomaculum hydroxybenzoicum produces acetate, butyrate, and CO2, with benzoate as a transient intermediate (Brauman et al. 1998). However, although the degradation of 3-hydroxybenzoate by Thauera aromatica begins with the formation of the CoA-ester, this is followed by the reduction of the ring with retention of the original hydroxyl group (Laempe et al. 2001).

ALDEHYDES The reductive transformation of arene carboxylates to the corresponding aldehydes under aerobic conditions has already been noted. In addition, aromatic aldehydes may undergo both reductive and oxidative reactions, with the possibility of decarboxylation of the carboxylic acid formed: a. Oxidation of substituted benzaldehydes to benzoates at the expense of sulfate reduction has been demonstrated in strains of Desulfovibrio sp., although the carboxylic acids produced were apparently stable to further degradation (Zellner et al. 1990). Vanillin was, however, used as a substrate for growth by a strain of Desulfotomaculum sp. and was metabolized via vanillate and catechol (Kuever et al. 1993). Vanillin is transformed by Clostridium formicoaceticum sequentially to vanillate and 3,4-dihydroxybenzoate, while the methyl group is converted into acetate via acetyl coenzyme A (Göbner et al. 1994). b. Reduction of benzoates to the corresponding benzyl alcohols has been observed in several organisms: (i) cell extracts of Clostridium formicoaceticum at the expense of carbon monoxide (Fraisse and Simon 1988), (ii) Desulfomicrobium escambiense at the expense of pyruvate that was oxidized to acetate, lactate, and succinate (Sharak Genther et al. 1997). Oxidoreductases mediate the transfer of electrons between aldehydes and carboxylates. In Clostridium formicoaceticum, there are two oxidoreductases. One contains Mo, is reversible, and active toward a range of both aliphatic and aromatic carboxylic acids and aldehydes (White et al. 1993), whereas the other is a W-containing enzyme (White et al. 1991). In addition, there exists a different enzyme that carries out the same reaction in C. thermoaceticum (White et al. 1989). Different aldehyde oxidoreductases have been isolated from Clostridium thermoaceticum and Cl. formicoaceticum (White et al. 1993). Whereas however, both cinnamate and cinnamaldehyde were good substrates for the Mo-containing enzyme from the latter, benzoate was an extremely poor substrate. The W-containing enzyme from Cl. formicoaceticum, however, displays high activity toward a greater range of substituted benzoates (White et al. 1991).

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Crawford RL (1976) Pathways of 4-hydroxybenzoate degradation among species of Bacillus. J Bacteriol 127: 204–290. Crawford RL, PP Olson (1978) Microbial catabolism of vanillate: decarboxylation to guaiacol. Appl Environ Microbiol 36: 539–543. Crawford RL, SW Hutton, PJ Chapman (1975) Puriication and properties of gentisate 1,2-dioxygenase from Moraxella osloensis. J Bacteriol 121: 794–799. Cripps RE, PW Trudgill, JG Whateley (1978) The metabolism of 1-phenylethanol and acetophenone by Nocardia T5 and an Arthrobacter species. Eur J Biochem 86: 175–186. Dangel W, R Brackmann, A Lack, M Mohamed, J Koch, B Oswald, B Seyfried, A Tschech, G Fuchs (1991) Differential expression of enzyme activities initiating anoxic metabolism of various aromatic compounds via benzoyl-CoA. Arch Microbiol 155: 256–262. Darby JM, DG Taylor, DJ Hopper (1987) Hydroquinone as the ring-ission substrate in the catabolism of 4-ethylphenol and 4-hydroxyacetophenone by Pseudomonas putida D1. J Gen Microbiol 133: 2137–2146. Degrassi G, PP de Laureto, CV Bruschi (1995) Puriication and chracterization of ferulate and p-coumarate decarboxylase from Bacillus pumilis. Appl Environ Microbiol 61: 326–332. Denef VJ, MA Patrauchan, C Florizone, J Park, TV Tsoi, W Verstraete, JM Tiedje, LD Eltis (2005) Growth substrate- and phase-speciic expression of biphenyl, benzoate, and C1 metabolic pathways in Burkholderia xenovorans LB400. J Bacteriol 187: 7996–8005. Díaz E, A Ferrández, JL Garcia (1998) Characterization of the hca cluster encoding the dioxygenolytic pathway for initial catabolism of 3-phenylpropionic acid in Escherichia coli K-12. J Bacteriol 180: 2915–2923. Donnelly MI, S Dagley (1980) Production of methanol from aromatic acids by Pseudomonas putida. J Bacteriol 142: 916–924. Dörner E, M Boll (2002) Properties of 2-oxoglutarate: ferredoxin oxidoreductase from Thauera aromatica and its role in enzymatic reduction of the aromatic ring. J Bacteriol 184: 3975–3983. Eaton RW, DW Ribbons (1982) Metabolism of dibutylphthalate and phthalate by Micrococcus sp. strain 12B. J Bacteriol 151: 48–57. Ebenau-Jehle C, M Boll, G Fuchs (2003) 2-oxoglutarate: NADP+ oxidoreductase in Azoarcus evansii: properties and function in electron transfer reactions in aromatic ring reduction. J Bacteriol 185: 6119–6129. Eby DM, ZM Beharry, ED Coulter, DM Kurtz, EL Neidle (2001) Characterization and evolution of anthranilate 1,2-dioxygenase from Acinetobacter sp. strain ADP1. J Bacteriol 183: 109–118. Egland PG, CS Harwood (1999) BadR, a new MarR family member regulates anaerobic benzoate degradation by Rhodopseudomonas palustris in concert with AadR, an Fnr family member. J. Bacteriol. 181: 2102–2109. Egland PG, J Gibson, CS Harwood (1995) Benzoate-coenzyme A ligase, encoded badA, is one of three lighases to catalyze benzoyl-coenzyme A formation during anaerobic growth of Rhodopseudomonas palustris on benzoate. J Bacteriol 177: 6545–6551. Elder DJE, P Morgan, DJ Kelly (1992) Anaerobic degradation of trans-cinnamate and ω-phenylalkane carboxylic acids by the photosynthetic bacterium Rhodopseudomonas palustris: evidence for a betaoxidation mechanism. Arch Microbiol 157: 148–154. Elmorsi EA, DJ Hopper (1979) The catabolism of 5-hydroxyisophthalate by a soil bacterium. J Gen Microbiol 111: 145–152. Eppink MHM, SA Boeren, J Vervoort, WJH van Berkel (1997) Puriication and properties of 4-hydroxybenzoate 1-hydroxylase (decarboxylating), a novel lavin adenine dinucleotide-dependent monooxygenase from Candida parapilosis CBS604. J Bacteriol 179: 6680–6687. Fairley DJ, DR Boyd, ND Sharma, CCR Allen, P Morgan, MJ Larkin (2002) Aerobic metabolism of 4hydroxybenzoic acid in Archaea via an unusual pathway involving an intramolecular migration (NIH shift). Appl Environ Microbiol 68: 6246–6255. Feng Y, HE Khoo, CL Poh (1999) Puriication and characterization of gentisate 1,2-dioxygenases from Pseudomonas alcaligenes NCIB 9867 and Pseudomonas putida NCIB 9869. Appl Environ Microbiol 65: 946–950. Fernández C, A Ferrández, B Minambres, E Diaz, JL Gardia (2006) Genetic characterization of the phenylacetyl-coenzyme A oxygenase from the aerobic phenylacetic acid degradation pathway of Escherichia coli. Appl Environ Microbiol 72: 7422–7426.

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PART 4 NONHALOGENATED PHENOLS AND ANILINES Although phenols and anilines have similar electronic structures, the initial step in their aerobic degradation is different. Whereas the degradation of phenols is initiated by monooxygenation, dioxygenation with loss of the amino group is used for anilines. Catechols are then produced from both of them. The degradation of halogenated phenols and anilines is discussed in Chapter 9, Part 2.

PHENOLS Aerobic Degradation The degradation of phenol is initiated by hydroxylation using a single-component NAD(P)H-dependent monooxygenase encoded by pheA (Nurk et al. 1991). In Bacillus thermoglucosidasius, however, the hydroxylase is a two-component system encoded by pheA1 and pheA2, and hydroxylation requires supplementation by the second component with FAD(NADH) (Kirchner et al. 2003). For alkylated phenols, there are different pathways for degradation depending on whether or not oxidation of the alkyl group precedes oxygenation and ission of the ring: a. The degradation of cresols and xylenols by strains of Pseudomonas putida is initiated by oxidation of one of the methyl groups to carboxylate before ring hydroxylation and ring

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ission (Bayly et al. 1988). For example, 4-methyl phenol is oxidized to 4-hydroxybenzoate, which is hydroxylated to 3,4-dihydroxybenoate and undergoes ring ission to 3-ketoadipate. For 3-methylphenol, degradation of the 3-hydroxybenzoate involves hydroxylation to 2,5dihydroxybenzoate (gentisate), which is degraded to pyruvate and maleate (Hopper and Chapman 1971). b. Pseudomonas sp. strain KL 28 is able to degrade 4-n-alkylphenols with chain lengths of one to ive carbon atoms. Degradation of both the 3-n-alkyl and 4-n-alkylphenols is initiated by hydroxylation to 3,4-dihydroxy compounds that are degraded by extradiol ission followed by dehydrogenation to 2-hydroxy-5-n-alkylmuconates with the alkyl groups intact (Jeong et al. 2003). Some unusual reactions have been encountered in the degradation of substituted phenols: 1. The degradation of bisphenol-A involves a rearrangement—analogous to those described for compounds with quaternary carbon atoms in Chapter 7, Part 1—followed by oxidative ission of the stilbene produced (Lobos et al. 1992; Spivack et al. 1994) (Figure 8.38). 2. The degradation of 4-ethylphenol and related compounds is initiated not by oxygenation but by dehydrogenation to a quinone methide followed by hydroxylation (Hopper and Cottrell 2003) (Figure 8.39), and the lavocytochrome 4-ethylphenol methylene hydroxylase in Pseudomonas putida stain JD1 has been characterized (Reeve et al. 1989). CH3

CH3

CH3

HO

OH

CH2OH

HO

OH

OH

OH CH2 OH

CH3

HO

HO

OH

CO2H

COCH2OH

OH

OH

CH3

HO

FIGURE 8.38

CH2OH

HO

CO2H

COCH3

OH

OH

Degradation of bisphenol-A.

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Environmental Degradation and Transformation of Organic Chemicals CH(OH)CH3 CH3

CH3

CH2

OH

O

OH

OH

FIGURE 8.39

Aerobic degradation of 4-ethylphenol. OH

OH

H C

C OH

O

O

OH

(a)

O C

OH

C

O

(b)

OH

O

O C

HO

FIGURE 8.40

OH O

O

O

C

OH + O

C

Biotransformations of nonylphenol.

3. The degradation of nonylphenol isomers with quaternary side chains in a strain of Sphingomonas xenophaga displays unusual features (Corvini et al. 2004; Gabriel et al. 2005a,b). These may be described formally as oxygenation at the position para to the phenol group, followed by either of two rearrangements: a. Migration of the alkyl group to C-3 of the phenolic ring with the formation of an alkylated hydroquinone (Figure 8.40a); b. Rearrangement by insertion of an oxygen atom from the hydroxyl group between the terminal position of the alkyl group and C-4 of the phenolic ring, followed by further oxygenation with the loss of the tertiary alkanol and formation of benzoquinone (Figure 8.40b). Analogous reactions may be presumed to have taken place in the transformation of a tert-octylphenol by a strain of Sphingomonas sp. in which 2,4,4-trimethylpent-2-anol was produced (Tanghe et al. 2000). The degradation of polyhydroxybenzenes has been examined rather seldom. 1. The degradation of resorcinol can take place by several pathways that are initiated by hydroxylation. 1,2,4-Trihydroxybenzene is degraded by (a) 1:2 dioxygenation and

Carbocyclic Aromatic Compounds without Halogen Substituents

449

ring ission to maleylacetate and 3-ketoadipate or 1:6 dioxygenation and ring ission to acetylpyruvate in strains of Pseudomonas putida (Chapman and Ribbons 1976), or (b) 1:2 dioxygenation and ring ission in Corynebacterium glutamicum (Huang et al. 2006). In contrast, degradation by Azotobacter vinelandii involved hydroxylation to pyrogallol that was degraded by intradiol ission to 2-hydroxymuconate and pyruvate (Groseclose and Ribbons 1981). 2. The metabolism of phloroglucinol (1,3,5-trihydroxybenzene) by Fusarium solani produced 1,2,3-trihydroxybenzene (pyrogallol) as an unexpected intermediate, which was degraded by intradiol ission to vinylpyruvate, and then to acetaldehyde and pyruvate (Walker and Taylor 1983). Under anaerobic conditions, Pelobacter massiliensis uses the transhydroxylation pathway for the degradation of all the trihydroxbenzenes (Brune et al.1992). 3. 2,4-Diacetylphloroglucinol, which is a secondary metabolite produced by Pseudomonas luorescens CHA0, is the effective biocontrol agent for fungal pathogens. As a 1:3-diketone, it can be hydrolyzed to the monoacetyl compound, which is much less toxic to Fusarium oxysporum, and inally to phloroglucinol (Schouten et al. 2004). The hydrolase has been characterized from Pseudomonas luorescens CHA0, is peciic for 2,4-diacetylphloroglucinol, and was unreactive against 2-acetyl- and 2,4,6-triacetylphloroglucinol (Bottiglieri and Keel 2006). Anaerobic Degradation The anaerobic degradation of phenols is dependent on two reactions—carboxylation of the ring to hydroxybenzoates and dehydroxylation to benzoates. Ring carboxylation is a key reaction in the anaerobic degradation of both phenols and anilines. In Thauera aromatica, the carboxylation of phenol is carried out in two steps: AMP-dependent phosphorylation by a synthase followed by carboxylation with the production of 4-hydroxybenzoate (Schühle and Fuchs 2004; Narmandakh et al. 2006). Catechol and aniline can be degraded to CO2 by Desulfobacterium anilini (Schnell et al. 1989), and catechol is slowly degraded by D. catecholicum (Szewzyk and Pfennig 1987), and by a strain of Desulfotomaculum sp. (Kuever et al. 1993). Analogy with phenol and consistent with the CO2 dependence of the catechol-degrading Desulfotomaculum sp. (Kuever et al. 1993), catechol is carboxylated to 3,4-dihydroxybenzoate by a strain of Desulfobacterium sp. (Gorny and Schink 1994b). This is then dehydroxylated to benzoate before further degradation. The reversible decarboxylation of 3,4-dihydroxybenzoate has been described in Sedimentibacter (Clostridium) hydroxybenzoicum (He and Wiegel 1996), and the enzyme has been puriied. 4-HydroxybenzoylCoA plays a central role in the metabolism of phenol, 4-methylphenol, 4-hydroxyphenylacetate, and related aromatic compounds by a denitrifying strain of Pseudomonas sp. (now classiied as Thauera aromatica). This is supported by the isolation and puriication of the dehydroxylating enzyme (Brackmann and Fuchs 1993), and the characterization of the enzyme as a molybdenumlavin-iron-sulfur protein (Breese and Fuchs 1998). A similar dehydroxylase is also involved in the metabolism of 4-hydroxybenzoate by Rhodopseudomonas palustris (Gibson et al. 1997), and is also a molybdenum-containing enzyme. The degradation of 3-methylphenol by oxidation to 3-hydroxybenzoate followed by analogous dehydroxylation has been observed in a “Pseudomonas-like” organism under denitrifying conditions (Bonting et al. 1995), and in Desulfotomaculum sp. strain Gross (Londry et al. 1997). The oxidation is formally comparable to the reactions in the metabolism of alkylarenes, and a carboxylation pathway is apparently not involved. The degradation of phenol is initiated by formation of phenylphosphate followed by carboxylation and dehydroxylation to benzoate. Benzoyl CoA is then degraded to acetate (Breinig et al. 2000) or—under methanogenic conditions to methane. An analogous pathway to benzoyl CoA has been demonstrated for hydroquinone (Gorny and Schink 1994a). In contrast, the degradation of 1,3-dihydroxybenzene (resorcinol) by Azoarcus anaerobius under denitrifying conditions apparently proceeds by hydroxylation to 1,2,4-trihydroxybenzene followed by oxidation at the expense

450

Environmental Degradation and Transformation of Organic Chemicals

of nitrate to 2-hydroxybenzoquinone. Putative enzymes for established ring-ission reactions or hydrolysis could not be found, and the reactions leading to ission of the aromatic ring remain to be elucidated (Phillip and Schink 1998). The initial reactions involved in the degradation of 2-, 3-, or 4-methylphenol (o-, m-, p-cresol) are quite different. Degradation in Desulitobacterium cetonicum is initiated by reaction with fumarate catalyzed by benzylsuccinate synthase—analogous to that already noted for the anaerobic degradation of toluene and xylenes (Verfürth et al. 2004). For m- and p-cresol, this is followed by dehydrogenation to 3- or 4-hydroxybenzoyl-CoA and dehydroxylation to benzoyl-CoA (Figure 8.41) (Müller et al. 2001). The degradation of 3-methylphenol (m-cresol) may alternatively proceed by oxidation to 3-hydroxybenzoate followed by dehydroxylation to benzoate (Londry et al. 1997). Gallate (3,4,5-trihydroxybenzoate) can be degraded by Pelobacter acidigallici to acetate and CO2 (Schink and Pfennig 1982), and by Eubacterium oxidoreducens in the presence of exogenous H2 or formate to acetate, butyrate, and CO2 (Krumholz et al. 1987). The degradation has been studied in detail, and takes place by this unusual pathway (Figure 8.42) (Brune and Schink 1992; Krumholtz and Bryant 1988). The formation of phloroglucinol in P. acidigallici involves a series of intramolecular hydroxyl transfer reactions with regeneration of 1,2,3,5-tetrahydroxybenzene (Brune and Schink 1990) (Figure 8.43), and in Eubacterium oxidoreducens the reaction is catalyzed by an isomerase that contains Fe, acid-labile sulfur, and Mo (Krumholtz and Bryant 1988). Although CoSCoA

CoSCoA

CoSCoA

CH2

CH3

CO2H

FIGURE 8.41

CO2H

CO2H

OH

OH

OH

OH

OH

Anaerobic degradation of 4-methylphenol. CO2H

HO

OH

OH

HO

OH

HO

O

OH HO

CH3−CO−CH2−CH(OH)−CH2−CO2H

3CH3−CO2H

CH3−CO−CH2−CO−CH2−CO2H

Pathway for the biodegradation of 3,4,5-trihydroxybenzoate. OH

OH

OH

+ HO

OH OH

FIGURE 8.43

O

OH

OH

FIGURE 8.42

CoSCoA

CoSCoA

CO

+ HO

OH OH

HO

OH

HO

OH

OH

Intramolecular hydroxyl group transfers in the biodegradation of 1,2,3-trihydroxybenzoate.

451

Carbocyclic Aromatic Compounds without Halogen Substituents

the reaction is a transhydroxylase, it does not involve hydroxylation by water, which is found in many other molybdenum enzymes (Reichenbecher et al. 1996). An analogous reaction occurs in E. oxidoreducens and also involves 1,2,3,5-tetrahydroxybenzene, although details of the pathway may be different (Haddock and Ferry 1989, 1993). Subsequent reduction to dihydrophloroglucinol is followed by ring ission to 3-hydroxy-5-ketohexanoate and, inally, to formation of butryrate and acetate (Krumholz et al. 1987). This pathway is comparable to that involved in the degradation of resorcinol by the species of Clostridium (Tschech and Schink 1985), although an alternative pathway involving direct hydrolysis has been observed in denitrifying bacteria (Gorny et al. 1992). P. massiliensis is able to degrade all three trihydroxybenzenes (1,2,3-, 1,3,5-, and 1,2,4-) by the transhydroxylation pathway (Brune et al. 1992), whereas Desulfovibrio inopinatus degrades 1,2,4trihydroxybenzene by a different pathway (Reichenbecher and Schink 1997). The degradation of phenols has also been examined in mixed cultures, and embodies some of the features that have been observed in pure cultures, in particular, the signiicance of carboxylation. The following examples illustrate some additional details of these reactions. It is worth noting that metabolism of the methylphenols (cresols) by mixed cultures may proceed by ring carboxylation in contrast to the oxidation pathway that has been demonstrated in pure cultures: 1. Phenol is carboxylated by a deined obligate syntrophic consortium to benzoate, which is then degraded to acetate, methane, and CO2 (Knoll and Winter 1989). 2. 2-Methylphenol is carboxylated by a methanogenic consortium to 4-hydroxy-3-methylbenzoate that was dehydroxylated to 3-methylbenzoate, which was the stable end product (Bisaillon et al. 1991). 3. 3-Methylphenol is carboxylated to 2-methyl-4-hydroxybenzoate by a methanogenic-enrichment culture before degradation to acetate (Figure 8.44a) (Roberts et al. 1990): 14C-labeled bicarbonate produced carboxyl-labeled acetate, while 14C-methyl-labeled 3-methylphenol yielded methyl-labeled acetate. However, 2-methylbenzoate formed by dehydroxylation of 2-methyl-4-hydroxybenzoate was not further metabolized (Figure 8.44b). A similar reaction occurs with a sulfate-reducing mixed culture (Ramanand and Sulita 1991). 4. An unusual reaction occurred during the degradation of 3-methylphenol by a methanogenic consortium (Londry and Fedorak 1993). Although carboxylation to 2-methyl-4hydroxybenzoate took place as in the preceding example, further metabolism involved loss of the methyl group with the formation of methane before dehydroxylation to benzoate (Figure 8.44c).

CH3−CO2H (a)

OH

OH

(b) CH3

CH3

CH3

(c)

CO2H

CO2H OH

CO2H

FIGURE 8.44

Anaerobic biodegradation of 3-methylphenol.

CO2H

452

Environmental Degradation and Transformation of Organic Chemicals

It can be concluded from these observations that whereas benzoate produced by the carboxylation of phenols can be degraded, dehydroxylation with the formation of substituted benzoates may produce stable terminal metabolites. Anilines Aerobic The aerobic degradation of anilines is, in principle, straightforward and involves deamination in a strain of Nocardia sp. by a dioxygenase (Bachofer and Lingens 1975), although details of the enzyme have not been fully resolved (Fukumori and Saint 1997). This is followed by ring ission of the resulting catechols by either intradiol or extradiol ring ission. Analogous mechanisms are used for anthranilic acid by deamination and decarboxylation (Chang et al. 2003), and 2-aminobenzenesulfonate to catechol-3-sulfonate with concomitant deamination (Junker et al. 1994). The degradation of 3- and 4-methylanilines by Pseudomonas putida mt-2 has been described (McClure and Venables 1986, 1987). It is important to emphasize that since anilines may be incorporated into humic material, their fate is not determined solely by biodegradation. The aerobic degradation of aminobenzenesulfonates that are produced from azobenzenes by reduction and scission is discussed in Chapter 9, Part 4. Anaerobic In analogy with phenol, aniline is carboxylated to 4-aminobenzoate followed by reductive deamination to benzoate (Schnell and Schink 1991), which is degraded by pathways that have already been elaborated.

REFERENCES Bachofer R, F Lingens (1975) Conversion of aniline into pyrocatechol by a Nocardia sp. : incorporation of oxygen-18. FEBS Lett 50: 288–290. Bayly R, R Jain, CL Poh, R Skurry (1988) Unity and diversity in the degradation of xylenols by Pseudomonas spp.: a model for the study of microbial evolution. In Microbial Metabolism and the Carbon Cycle (Eds SR Hagedorn, RS Hanson, DA Kunz) pp. 359–379. Harwood Academic Publishers, Chur, Switzerland. Bisaillon J-G, F Lépine, R Beaudet, M Sylvestre (1991) Carboxylation of o-cresol by an anaerobic consortium under methanogenic conditions. Appl Environ Microbiol 57: 2131–2134. Bonting CFC, S Schneider, G Schmidtberg, G Fuchs (1995) Anaerobic degradation of m-cresol via methyl oxidation to 3-hydroxybenzoate by a denitrifying bacterium. Arch Microbiol 164: 63–69. Bottiglieri M, C Keel (2006) Characterization of PhlG, a hydrolase that speciically degrades the antifungal compound diacetylphloroglucinol in the biocontrol agent Pseudomonas luorescens CHA0. Appl Environ Microbiol 72: 418–427. Brackmann R, G Fuchs (1993) Enzymes of anaerobic metabolism of phenolic compounds 4-hydroxy benzoyl-CoA reductase (dehydroxylating) from a denitrifying Pseudomonas sp. Eur J Biochem 213: 563–571. Breese K, G Fuchs (1998) 4-hydroxybenzoyl-CoA reductase (dehydroxylating) from the denitrifying bacterium Thauera aromatica: prosthetic groups, electrom donor, and genes of a member of the molybdenumlavin-iron-sulfur proteins. Eur J Biochem 251: 916–923. Breinig S, E Schiltz, G Fuchs (2000) Genes involved in anaerobic metabolism of phenol in the bacterium Thauera aromatica. J Bacteriol 182: 5849–5863. Brune A, B Schink (1990) Pyrogallol-to-phloroglucinal conversion and other hydroxyl-transfer reactions catalyzed by cell extracts of Pelobacter acidigallici. J Bacteriol 172: 1070–1076. Brune A, B Schink (1992) Phloroglucinol pathway in the strictly anaerobic Pelobacter acidigallici fermentation of trihydroxybenzenes to acetate via triacetic acid. Arch Microbiol 157: 417–424. Brune A, S Schnell, B Schink (1992) Sequential transhydroxylations converting hydroxyhydroquinone to phloroglucinol in the strictly anaerobic, fermentative bacterium. Pelobacter massiliensis. Appl Environ Microbiol 58: 1861–1868.

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Chang H-K, P Mohseni, GJ Zylstra (2003) Characterization and regulation of the genes for a novel anthanilate 1,2 dioxygenase from Burkholderia cepacia DBO 1. J Bacteriol 185: 5871–5881. Chapman PJ, DW Ribbons (1976) metabolism of resorcinylic compounds by bacteria: alternative pathways fore resorcinol catabolism in Pseudomonas putida. J Bacteriol 125: 985–998. Corvini PFX, RJW Meesters, A Schäffer, HF Schröder, R Vinken, J Hollender (2004) Degradation of a nonylphenol single isomer by Sphingomonas sp. strain TTNP3 leads to a hydroxylation-induced migration product. Appl Environ Microbiol 70: 6897–6900. Fukumori F, CP Saint (1997) Nucleotide sequences and regulational analysis of genes involved in conversion of aniline to catechol in Pseudomonas putida UCC22 (pTDN1). J Bacteriol 179: 399–408. Gabriel FLP, A Heidlberger, D Rentsch, W Giger, K Guenther, H-P E Kohler (2005b) A novel metabolic pathway for degradation of 4-nonylphenol environmental contaminants by Sphingomonas xenophaga Bayram. J Biol Chem 280: 15526–15533. Gabriel FLP, W Giger, K Guenther, H-P E Kohler (2005a) Differential degradation of nonylphenol isomers by Sphingomonas xenophaga Bayram. Appl Environ Microbiol 71: 1123–1129. Gibson J, M Dispensa, CS Harwood (1997) 4-hydroxybenzoyl coenzyme A reductase dehydroxylating is required for anaerobic degradation of 4-hydrozybenzoate by Rhodopseudomonas palustris and shares features with molybdenum-containing hydroxylases. J Bacteriol 179: 634–642. Gorny N, B Schink (1994a) Hydroquinone degradation via reductive dehydroxylation of gentisyl-CoA by a strictly anaerobic fermenting bacterium. Arch Microbiol 161: 25–32. Gorny N, B Schink (1994b) Anaerobic degradation of catechol by Desulfobacterium sp strain cat2 proceeds via carboxylation to protocatechuate. Appl Environ Microbiol 60: 3396–3400. Gorny N, G Wahl, A Brune, B Schink (1992) A strictly anaerobic nitrate-reducing bacterium growing with resorcinol and other aromatic compounds. Arch Microbiol 158: 48–53. Groseclose EE, DW Ribbons (1981) Metabolism of resorcinolic compounds by bacteria: a new pathway for resorcinol catabolism in Azotobacter vinelandii. J Bacteriol 146: 460–466. Haddock JD, JG Ferry (1989) Puriication and properties of phloroglucinol reductase from Eubacterium oxidoreducens G-41. J Biol Chem 264: 4423–4427. Haddock JD, JG Ferry (1993) Initial steps in the anaerobic degradation of 3,4,5-trihydroxybenzoate by Eubacterium oxidoreducens: characterization of mutants and role of 1,2,3,5-tetrahydroxybenzene. J Bacteriol 175: 669–673. He Z, J Wiegel (1996) Puriication and characterization of an oxygen-sensitive, reversible 3,4-dihydroxybenzoate decarboxylase from Clostridium hydroxybenzoicum. J Bacteriol 178: 3539–3543. Hopper DJ, L Cottrell (2003) Alkylphenol biotransformations catalyzed by 4-ethylphenol methylenehydroxylase. Appl Environ Microbiol 69: 3650–3652. Hopper DJ, PJ Chapman (1971) Gentisic acid and its 3- and 4-methyl-substituted homologues as intermediates in the bacterial degradation of m-cresol, 3,5-xylenol and 2,4-xylenol. Biochem J 122: 19–28. Huang Y, K-X Zhao, X-H Shen, MT Chaudhry, C-Y Jiang, S-J Liu (2006) Genetic characterization of the resorcinol catabolic pathway in Corynebacterium glutamicum. Appl Environ Microbiol 72: 7238–7245. Jeong JJ, JH Kim, C-K Kim, I Hwang, K Lee (2003) 3- and 4-alkylphenol degradation pathway in Pseudomonas sp. strain KL28: genetic organization of the lap gene cluster and substrate speciicities of phenol hydroxylase and catechol 2,3-dioxygenase. Microbiology (UK) 149: 3265–3277. Junker F, T Leisinger, AM Cook (1994) 3-sulfocatechol 2,3-dioxygenase and other dioxygenases (EC 1.13.11.2 and EC 1-14-12) in the degradative pathways of 2-aminobenzenesulfonic, benzenesulphonic and 4-toluenesulfonic acids in Alcaligenes sp. strain O-1. Microbiology U.K. 140: 1713–1722. Kirchner U, AH Westphal, R Müller, WJH van Berkel (2003) Phenol hydroxylase from Bacillus thermoglucosidasius A7, a two-component monooxygenase with a dual role for FAD. J Biol Chem 278: 47545–47553. Knoll G, J. Winter (1989) Degradation of phenol via carboxylation to benzoate by a deined, obligate syntrophic consortium of anaerobic bacteria. Appl. Microbiol. Biotechnol. 30: 318–324. Krumholz LR, MP Bryant (1988) Characterization of the pyrogallol–phloroglucinol isomerase of Eubacterium oxidoreducens. J Bacteriol 170: 2472–2479. Krumholz LR, RL Crawford, ME Hemling, MP Bryant (1987) Metabolism of gallate and phloroglucinol in Eubacterium oxidoreducens via 3-hydroxy-5-oxohexanoate. J Bacteriol 169: 1886–1890. Kuever J, J Kulmer, S Janssen, U Fischer, K-H Blotevogel (1993) Isolation and characterization of a new spore-forming sulfate-reducing bacterium growing by complete oxidation of catechol. Arch Microbiol 159: 282–288. Lobos JH, TK Leib, T-M Su (1992) Biodegradation of bisphenol A and other bisphenols by a gram-negative aerobic bacterium. Appl Environ Microbiol 58: 1823–1831.

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Londry KL, PM Fedorak (1993) Use of luorinated compounds to detect aromatic metabolites from m-cresol in a methanogenic consortium: evidence for a demethylation reaction. Appl Environ Microbiol 59: 2229–2238. Londry KL, PM Fedorak, JM Sulita (1997) Anaerobic degradation of m-cresol by a sulfate-reducing bacterium. Appl Environ Microbiol 63: 3170–3175. McClure NC, WA Venables (1986) Adaptation of Pseudomonas putida mt-2 to growth on aromatic amines. J Gen Microbiol 132: 2209–2218. McClure NC, WA Venables (1987) pTDN1, a catabolic plasmid involved in aromatic amine catabolism in Pseudomonas putida mt-2. J Gen Microbiol 133: 2073–2077. Müller JA, AS Galuschko, A Kappler, B Schink (2001) Initiation of anaerobic degradation of p-cresol by formation of 4-hydroxybenzylsuccinate in Desulitobacterium cetonicum. J Bacteriol 183: 752–757. Narmandakh A, N Gad′on, F Drepper, B Knapp, W Haehnel, G Fuchs (2006) Phosphorylation of phenol by phenylphosphate synthase: role of histidine phosphate in catalysis. J Bacteriol 188: 7815–7822. Phillip B, B Schink (1998) Evidence of two oxidative reaction steps initiating anaerobic degradation of resorcinol (1,3-dihydroxybenzene) by the denitrifying bacterium Azoarcus anaerobius. J Bacteriol. 180: 3644–3649. Ramanand K, JM Sulita (1991) Anaerobic degradation of m-cresol in anoxic aquifer slurries: carboxylation reactions in a sulfate-reducing bacterial enrichment. Appl. Environ. Microbiol. 57: 1689–1695. Reeve CD, MA Carver, DJ Hopper (1989) The puriication and characterization of 4-ethylphenol methylene hydroxylase, a lavocytochrome from Pseudomonas putida JD1. Biochem J 263: 431–437. Reichenbecher W, A Rüdiger, PMH Kroneck, B Schink (1996) One molecule of molybdopterin guanine dinucleotide is associated with each subunit of the heterodimeric Mo-Fe-S protein transhydroxylase of Pelobacter acidigallici as determined by SDS (PAGE) and mass spectrometry. Eur J Biochem 237: 406–413. Reichenbecher WW, B Schink (1997) Desulfovibrio inopinatus sp nov, a new sulfate-reducing bacterium that degrades hydroxyhydroquinone (1,2,4-trihydroxybenzene). Arch Microbiol 168: 338–344. Roberts DJ, PM Fedorak, SE Hrudey (1990) CO2 incorporation and 4-hydroxy-2-methylbenzoic acid formation during anaerobic metabolism of m-cresol by a methanogenic consortium. Appl Environ Microbiol 56: 472–478. Schink B, N Pfennig (1982) Fermentation of trihydroxybenzenes by Pelobacter acidigallici gen nov sp nov, a new strictly anaerobic, non-sporeforming bacterium. Arch Microbiol 133: 195–201. Schnell S, B Schink (1991) Anaerobic aniline degradation via reductive deamination of 4-aminobenzoyl-CoA in Desulfobacterium anilini. Arch Microbiol 155: 183–190. Schnell S, F Bak, N Pfennig (1989) Anaerobic degradation of aniline and dihydroxybenzenes by newly isolated sulfate-reducing bacteria and description of Desulfobacterium anilini. Arch Microbiol 152: 556–563. Schouten A, G van den Berg, C Edel-Hermann, C Steinberg, N Gautheron, C Alabouvette, CH de Vos, P Lemanceau, JM Raaijmakers (2004) Defense responses of Fusarium oxysporum to 2,4-diacetylphloroglucinol, a broad-spectrum antibiotic produced by Pseudomonas luorescens. Mol Plant–Microbe Interact 17: 1201–1211. Schühle K, G Fuchs (2004) Phenylphosphate carboxylase: a new C–C lyase involved in anaerobic phenol metabolism in Thauera aromatica. J Bacteriol 186: 4556–4567. Spivack J, TK Leib, JH Lobos (1994) Novel pathway for bacterial metabolism of bisphenol A. Rearrangements and stilbene cleavage in bisphenol A metabolism. J Biol Chem 269: 7323–7329. Szewzyk R, N Pfennig (1987) Complete oxidation of catechol by the strictly anaerobic sulfate-reducing Desulfobacterium catecholicum sp. nov. Arch Microbiol 147: 163–168. Tanghe T, W Dhooge, W Verstraete (2000) Formation of the metabolic intermediate 2,4,5-trimethyl2-pentanol during incubation of a Sphingomonas sp. strain with the xeno-estrogenic octylphenol. Biodegradation 11: 11–19. Tschech A, B Schink (1985) Fermentative degradation of resorcinol and resorcylic acids. Arch Microbiol 143: 52–59. Verfürth K, AJ Pierik, C Leutwein, S Zorn, J Heider (2004) Substrate speciicities and electron paramagnetic resonance properties of benzylsuccinate synthesis in anaerobic toluene and m-xylene metabolism. Arch Microbiol 181: 155–162. Walker JRL, BG Taylor (1983) Metabolism of phloroglucinol by Fusarium solani. Arch Microbiol 134: 123–126.

Carbocyclic 9 Substituted Aromatic Compounds PART 1 HALOGENATED ARENES AND CARBOXYLATES WITH CHLORINE, BROMINE, OR IODINE SUBSTITUENTS These industrial chemicals are widely used as the precursors for a wide range of products, which include agrochemicals, pharmaceutical products, polychlorinated biphenyls (PCBs), and polybrominated diphenyl ether lame retardants. For almost all of them, serious concern has arisen over their adverse environmental effects.

INTRODUCTION Since the aerobic degradation of halogenated phenols takes place by monooxygenation and is discussed in Part 2 of this chapter, it is not discussed here except to note the production of chlorocatechols from chlorophenols and chloroanilines. Emphasis is placed on chlorinated substrates, and reference may be made to a review (Allard and Neilson 2003) for details of their brominated and iodinated analogs. The degradation of aromatic luorinated compounds is discussed in Part 3 of this chapter. Aerobic degradation of chlorinated arene hydrocarbons, including the important group PCBs, and chlorobenzoates that are produced from them as metabolites, is generally initiated by dihydroxylation of the rings to dihydrodiols followed by dehydrogenation to catechols. Halide may be lost simultaneously and for 2-halogenated benzoates, both halide and carboxyl. Salient aspects are summarized, and attention drawn to selected aspects of enzyme inhibition. Halogenated catechols play a central role in the degradation of halogenated aromatic hydrocarbons, carboxylates, phenols, and amines. Fission of 3-substituted catechols may take place by extradiol, intradiol, or distal ission (Figure 9.1). To avoid the production of toxic metabolites, the halogenated catechols generally use both intradiol (1:2) and—exceptionally—distal (1:6) ission, whereas the alkylated catechols generally involve extradiol ission (2:3) (Figure 9.2). Further details are given later in this section.

HALOGENATED ARENE HYDROCARBONS Aerobic Conditions 1. Initial dioxygenation. Although degradation generally proceeds by dioxygenation followed by dehydrogenation of the cis-dihydrodiols that are formed, dehydrogenation may be replaced by elimination to produce catechols directly, for example, in the degradation of 1,2,4,5-tetrachlorobenzene (Sander et al. 1991), and chlorinated biphenyls with chlorine at the 2-positions when 2:3 dioxygenation has taken place (Seeger et al. 2001). Analogously, 2-halogenated benzoates generally undergo dioxygenation with concomitant decarboxylation and loss of halide, whereas other isomers are degraded by dioxygenation followed by dehydrogenation to chlorocatechols. 2. Ring ission. Ring ission of substituted catechols may take place by three pathways: intradiol (ortho), extradiol (meta), or distal (1:6) ission. Although extradiol ission is generally preferred for substituted catechols, the product from extradiol ission of 3-chlorocatechol is normally inhibitory since the acyl chloride reacts with the enzyme 455

456

Environmental Degradation and Transformation of Organic Chemicals OH OH

Cl

(a)

(c)

(b) OH CO 2 H CHO

OH

CO 2 H CO 2 H

Cl

Cl

CO 2 H COCl

FIGURE 9.1 Alternative dioxygenation pathways for 3-substituted catechols (a) distal (b) intradiol (c) extradiol.

R CO 2 H R

CHO

1,2

OH R OH CO 2 H CHO

FIGURE 9.2

2,3

Ring-cleavage pathways for the biodegradation of 3-substituted catechols.

producing it. Degradation then takes place by what has been termed the “modiied ortho pathway” with the production of chloromuconates. As an alternative, spontaneous hydrolysis of the acyl chloride is able to relieve the inhibition so that the extradiol pathway is available, for example, in Pseudomonas putida strain GJ31 (Mars et al. 1997; Kaschabek et al. 1998). An analogous example is found in the degradation of 2-chlorohydroquinone (Endo et al. 2005). Further examples are given in Chapter 3, Part 1. 3. Additional limitations. Other limitations have been encountered: (a) the formation of the inhibitory protoanemonin from 4-chlorocatechols (Blasco et al. 1995) and (b) the ineffectiveness of cycloisomerases required for effective degradation of 2-chlorotoluene (Pollmann et al. 2005). An example of this limitation is given later, and in the degradation of 3-luorobenzoate in Part 3 of this chapter.

MONOCYCLIC CHLORINATED ARENES Ultimately, ring cleavage of halogenated aromatic hydrocarbons must occur if aerobic degradation—rather than merely biotransformation—is to be accomplished. The pathways outlined for unsubstituted hydrocarbons generally followed are formation of a cis-dihydrodiol followed by dehydrogenation to the catechol and ring cleavage to muconic acids or hydroxymuconate semialdehydes. Dioxygenation, dehydrogenation, and intradiol ission of the resulting catechols are used in the degradation of 1,2,4-trichlorobenzene (Figure 9.3) and 1,2,3,4-tetrachlorobenzene by Pseudomonas chlororaphis strain RW71 (Potrawfke et al. 1998). A strain of Pseudomonas sp. PS12 can degrade 1,2,4-trichlorobenzene by a comparable pathway, although chloride is lost before the production of 3,4,6-trichlorocatechol during the degradation of 1,2,4,5-tetrachlorobenzene (Figure 9.4) (Sander et al. 1991). The genes encoding the α- and β-subunits of the terminal oxidase, the ferredoxin, and

457

Substituted Carbocyclic Aromatic Compounds Cl

Cl

Cl

Cl OH

Cl

Cl

Cl OH

Cl

H H Cl

Cl

Cl

Cl

Cl HO 2 C

HO 2 C

HO 2 C O

O

CO 2 H

OH

OH Cl

CO 2 H

O

CO 2 H

O

Cl

Cl

CO 2 H

Cl

FIGURE 9.3 Biodegradation of 1,2,4-trichlorobenzene.

Cl

Cl Cl

Cl

Cl

OH

H Cl Cl Cl

FIGURE 9.4

Cl OH

OH

OH Cl

Cl

Biodegradation of 1,2,4,5-tetrachlorobenzene.

the reductase from this strain now designated Burkholderia sp. have been cloned into Escherichia coli (Beil et al. 1997). It was conirmed that whereas metabolism of 1,2- and 1,4-dichlorobenzene and 1,2,4-tri- and 1,2,3,4-tetrachlorobenzene produced stable cis-dihydrodiols, dechlorination concomitant with dioxygenation took place with 1,2,4,5-tetrachlorobenzene, and was conirmed using 18 O2. In addition, dioxygenation of biphenyl, dibenzo [1,4]dioxin, dibenzofuran, and naphthalene was observed in this constructed strain. An additional example of simultaneous dechlorination and dioxygenation in the degradation of PCB congeners is given later. The importance of both the number and the position of chlorine substituents is illustrated by the results of a study with Xanthobacter lavus strain 14p1. The strain grew only with 1,4-dichlorobenzene, which was degraded by dioxygenation, dehydrogenation, and intradiol ring ission, whereas 1,3-dichlorobenzene did not induce dioxygenase activity (Sommer and Görisch 1997). Although chlorobenzene induced several of the enzymes essential for degradation, its inability to support growth was assumed to be the result of the accumulation of toxic intermediates. The transformation of chlorotoluenes has been studied in Ralstonia (Pseudomonas) sp. strain PS12, and important reasons that limit their biodegradability have emerged (Pollmann et al. 2001). a. Whereas 2,4-, 2,5-, and 3,4-dichlorotoluenes were dioxygenated and dehydrogenated to the corresponding catechols—and were therefore potentially degradable, 2,3-, 2,6-, and 3,5-dichlorotoluenes and 2,4,5-trichlorotoluene were only monooxygenated at the methyl group to the benzyl alcohols. b. Although the 2,3-, 2,4-, 2,5-, and 2,6-dichlorobenzyl alcohols could be oxidized to the benzoate, these apparently could not be degraded for unresolved reasons. c. 2-Chlorotoluene appears to be recalcitrant in this strain, although dioxygenation and dehydrogenation to chloromethylcatechols took place: the cycloisomerases were unable to degrade effectively the muconolactones produced by intradiol ring ission (Pollmann et al. 2005).

458

Environmental Degradation and Transformation of Organic Chemicals CCl3 CH

Cl

CCl3 Cl

OH

Cl

CH

OH

OH

FIGURE 9.5 Alternative degradation of DDT.

Although 1,1-dichloro-2,2-bis(p-chlorophenyl)ethene (DDE) is appreciably recalcitrant, it can be degraded by dioxygenation and extradiol ring ission to chlorobenzoate by cells of Pseudomonas acidovorans M3GY grown with biphenyl (Hay and Focht 1998; Aislabie et al. 1999). Bis (p-chlorophenyl)acetic acid (DDA), which is a polar metabolite, is apparently persistent in the environment (Heberer and Dünnbier 1999). Alternatively, degradation of DDT may take place by hydroxylation of the ring and displacement of the aromatic ring chlorine atom by hydroxyl (Figure 9.5) (Massé et al. 1989). Mutations at the active site of CYP101 (cytochrome P450cam) from a strain of Pseudomonas putida made possible the monooxygenation of chlorinated benzenes with less than three substituents to chlorophenols, with concomitant NIH shifts for 1,3-dichlorobenzene (Jones et al. 2001). Further mutations made it possible to oxidize even pentachlorobenzene and hexachlorobenzene to pentachlorophenol (Chen et al. 2002). Integration of the genes encoding cytochrome P450cam into Sphingobium chlorophenolicum enabled this strain to partially transform hexachlorobenzene to pentachlorophenol (Yan et al. 2006). Anaerobic Conditions Attention has been directed to the dechlorination of polychlorinated benzenes by strains that use them as an energy source by dehalorespiration. Investigations using Dahalococcoides sp. strain CBDB1 have shown its ability to dechlorinate congeners with three or more chlorine substituents (Hölscher et al. 2003). Although there are minor pathways, the major one for hexachlorobenzene was successive reductive dechlorination to pentachlorobenzene, 1,2,4,5-tetrachlorobenzene, 1,2,4trichlorobenzene, and 1,4-dichlorobenzene (Jayachandran et al. 2003). The electron transport system has been examined by the use of speciic inhibitors. Ionophores had no effect on dechlorination, whereas the ATP-synthase inhibitor N,N′-dicyclohexylcarbodiimide (DCCD) was strongly inhibitory (Jayachandran et al. 2004).

POLYCHLORINATED BIPHENYLS Aerobic Degradation This is discussed in some detail both on account of the importance of the degradation of PCBs, which are widely distributed contaminants, and since it illustrates a number of important principles. Overview The degradation of PCBs has attracted enormous attention. Although impressive investigation has been directed to Burkholderia xenovorans strain LB400 on account of the wide spectrum of PCBs that are oxidized, there are a number of factors that determine PCB biodegradability. These include (a) both the number and position of the chlorine substituents, (b) the positions at which dioxygenation occurs, (c) whether or not the initially formed dihydrodiol can be dehydrogenated, and (d) the degradability of the metabolites produced by ring ission. Considerable effort has been made to enlarge the range of strains that are susceptible to degradation by genetic manipulation. Because PCBs are lipophilic contaminants, a range of biota including ish, ish-eating birds, and mammals can accumulate PCBs. In contrast to the reactions described in this section, these are metabolized by the formation of sulfones in mammals (Letcher et al. 1998) or by monooxygenation with the

Substituted Carbocyclic Aromatic Compounds

459

production of hydroxylated PCBs in ish (Buckman et al. 2006). The anaerobic dechlorination of these metabolites has been described (Wiegel et al. 1999) in the context of the degradation of halogenated phenols. In this section, the strains used have been given to minimize confusion because there have been a number of changes in the nomenclature of some organisms, for example, Acinetobacter sp. strain P6 → Rhodococcus globerulus strain P6 Pseudomonas sp. strain LB400 → Burkholderia xenovorans strain LB400 Pseudomonas pseudoalcaligenes KF707 → Pseudomonas paucimobilis KF707 The assignments by the original authors have been used, with the alternatives in parentheses. A range of organisms able to degrade PCB congeners has been isolated, generally from biphenyl enrichments. These include a. Gram-negative strains—Alcaligenes eutrophus strain H850 (Bedard et al. 1987a), Pseudomonas pseudoalcaligenes strain KF707 (Furukawa and Miyazaki 1986), Pseudomonas (Burkholderia) sp. strain LB400 (Bopp 1986), and P. testosteroni (Ahmad et al. 1990) b. Gram-positive strains—Rhodococcus globerulus strain P6 (Acinetobacter sp. strain P6) (Furukawa et al. 1979; Asturias and Timmis 1993), Rhodococcus erythropolis strain TA421 (Maeda et al. 1995), Rhodococcus sp. strain RHA1 (Seto et al. 1995), and Bacillus sp. strain JF8 (Shimura et al. 1999) There are considerable differences in the oxidative activity of these organisms toward PCB congeners. For example, (a) Burkholderia (Pseudomonas) sp. strain LB400 has a much greater versatility than P. pseudoalcaligenes strain KF707 (Gibson et al. 1993) or P. testosteroni (Ahmad et al. 1990) and (b) the range of congeners transformed by Rhodococcus sp. strain RHA1 differs from that of Burkholderia sp. strain LB400 and Pseudomonas paucimobilis strain KF707 (Seto et al. 1995). Degradation of PCBs is carried out by a suite of enzymes comprising biphenyl-2,3-dioxygenase, biphenyl-2,3-dihydrodiol dehydrogenase, 2,3-dihydroxybiphenyl dioxygenase, and the hydrolytic enzymes that produce benzoate encoded by the genes bphA, bphB, bphC, and bphD (Furukawa and Miyazaki 1986; Ahmad et al. 1991; Taira et al. 1992). Degradation Is Initiated by Dioxygenation Dioxygenation generally takes place at the 2,3-position, or less commonly, at the 3,4-position, to produce cis-2,3-dihydrodiols or cis-3,4-dihydrodiols. For example, a strain of Pseudomonas sp. that was able to degrade a range of PCB congeners had both 2,3-dioxygenase and 3,4-dioxygenase activity, and four of the open reading frames were homologous to components of toluene dioxygenase (Erickson and Mondelo 1992). It was not resolved whether a single dioxygenase was able to introduce oxygen at the 2,3- or the 3,4-positions, or whether there were two different enzymes. The dioxygenase has been puriied and characterized from several organisms including Burkholderia (Pseudomonas) sp. strain LB400 (Haddock and Gibson 1995) and Comomonas testosteroni strain B-356 (Hurtubise et al. 1995). Dioxygenation required three components—a [2Fe–2S] oxygenase ISPBDH, a [2Fe–2S] ferredoxin (FER BPH), and a lavin reductase (FERBPH). These are encoded by bphA (α-subunit), bphE (β-subunit), bphF, and bphG. The iron–sulfur protein consists of a large subunit (α) with a molecular mass of 51–52 kDa and a small subunit (β) with a molecular mass of 22–27 kDa. Whole-cell studies using oxygen uptake by Burkholderia (Pseudomonas) sp. strain LB400 had clearly shown the versatility of this organism in the degradation of PCB congeners containing up

460

Environmental Degradation and Transformation of Organic Chemicals

to four chlorine substituents. The biphenyl 2,3-dioxygenase from this strain has been puriied and revealed additional mechanistic details (Haddock et al. 1995): a. The dihydrodiol was produced from all congeners, and as an alternative to dehydrogenation, an ortho-chlorine substituent could be eliminated from the 2,3-dihydrodiol to produce the catechol. b. 4,5-Dihydrodiols were produced from 3-3 (3,3′), (25-2) 2,2′,5, and the (25-25) 2,2′,5,5′ congeners, although these are not substrates for the dihydrodiol dehydrogenase. These results are consistent with the results accumulated over many years, and with the most frequent operation of a single dioxygenase enzyme. Several issues determine the speciicity of strains for the degradation of PCBs, and extensive efforts have been made to increase the range of strains that can be degraded. The speciicity relects differences in the protein sequences in two regions (III and IV) of the BphA large α-subunit of the dioxygenase (Kimura et al. 1997; Mondello et al. 1997), and this offers the possibility of expanding the range of degradable PCBs by alterations of speciic amino acids. The puriied dioxygenase from Burkholderia sp. strain LB400—whicht is one of the most versatile—has been examined in the presence of electron-transport proteins and cofactors for its reactivity toward congeners (Arnett et al. 2000). Reactivity depended both on the number and position of substituents, and some congeners were recalcitrant, including (24-4) 2,4,4′-trichloro-, (24-24) 2,4,2′,4′-tetrachloro-, and (345-25) 3,4,5,2′,5′-pentachlorobiphenyl. Substantial effort has therefore been directed to elucidating determinants of the speciicity for degradation, and to procedures for increasing the range of substrates that can be accepted. The ortho-substituted congeners are particularly recalcitrant. a. It has been suggested that the substrate speciicity of the dioxygenase is determined by the α-subunit of the dioxygenase. In contrast, the substrate speciicities of the four chimeras constructed from the respective α- and β-subunits of the terminal dioxygenase ISPBPH of Pseudomonas sp. strain LB400 and Comamonas (Pseudomonas) testosteroni strain B-356 were dependent on the presence of both proteins (Hurtubise et al. 1998). In addition, the catalytic activity of hybrid dioxygenases comprising α- and β-subunits from distant biphenyl dioxygenases is not determined speciically by one or other of the subunits (Chebrou et al. 1999). There is therefore a complex dependency on the presence of both subunits. b. Shufling the genes in a fragment of the bphA gene in Burkholderia sp. strain LB400, Comamonas testosteroni strain B-356, and Rhodococcus globerulus strain P6 resulted in variants that had high activity toward the generally persistent 2,6-dichloro- and 2,4,4′trichlorobiphenyls (Barriault et al. 2002). c. Site-directed mutants of amino acids that coordinate the catalytic iron center of Pseudomonas pseudoalcaligenes strain KF707 were produced and expressed in Escherichia coli. One mutant was able to degrade (25-25) 2,5,2′,5′-tetrachlorobiphenyl by 3,4-dioxygenation and displayed 2,3- and 3,4-dioxygenase activities for 2,5,2′- and 2,5,4′-trichlorobiphenyls (Suenaga et al. 2002). d. Efforts have been made to increase the range of substrates accepted by the dioxygenase by mutagenesis of multiple sites in region III (Barriault and Sylvestre 2004). The changes were in the positions at which dioxygenation took place: • 2-2 (2,2′)-Dichloro from the 2:3 position with loss of chloride, to the 3,4-dihydrodiol that is a terminal metabolite • 23-23 (2,2′,3,3′)-Tetrachloro to the 4,5-dihydrodiol without dechlorination • 2,2′,5,5′-Tetrachloro to the 3,4-dihydrodiol without dechlorination e. An attractive suggestion has been made to improve the spectrum of PCBs that are degraded by Pseudomonas sp. strain KKS102 by altering the promoter of the bph operon

Substituted Carbocyclic Aromatic Compounds

461

(Ohtsubo et al. 2003). By this means, strains were obtained that showed enhanced degradation of tri-, tetra-, and pentachlorobiphenyl. The next step in degradation is generally dehydrogenation that results in the production of the dihydroxybiphenyl, which is the substrate for ring ission. Alternatively, in the degradation of 2,4′- and 4,4′-dichlorobiphenyl by Pseudomonas testosteroni strain B-356 involving 3,4-dioxygenation, this is accomplished by loss of chloride (Ahmad et al. 1991), as in Burkholderia (Pseudomonas) sp. strain LB400 with congeners carrying ortho-chlorine substituents (Haddock et al. 1995; Seeger et al. 1999). Ring Fission by 2,3-Dihydroxybiphenyl Dioxygenase Degradation of the initially formed 2,3-dihydroxybiphenyl is carried out by extradiol ission, and 2,3-dihydroxybiphenyl 1,2-dioxygenase has been puriied and characterized from several organisms including Pseudomonas pseudoalcaligenes strain KF707 (Furukawa and Arimura 1987), Pseudomonas paucimobilis strain Q1 (Taira et al. 1988), Burkholderia (Pseudomonas) sp. strain LB400 (Haddock et al. 1995), and the Gram-positive Rhodococcus sp. strain RHA1 (Hauschild et al. 1996). In Rhodococcus globerulus strain P6 (Acinetobacter sp. strain P6), there are several nonhomologous 2,3-dihydroxybiphenyl-1,2-dioxygenases with a narrow substrate speciicity (Asturias and Timmis 1993), and one of them encoded by bphC2 was appreciably different from other extradiol dioxygenases (Asturias et al. 1994). The enzyme from Bacillus sp. strain JF8 is unusual in being Mn(II)-dependent and differs in structure from those of Burkholderia sp. strain LB400 and Pseudomonas paucimobilis strain KF707 (Hatta et al. 2003). Detailed investigations have revealed a number of important conclusions that affect the degradability of PCB congeners: 1. In Burkholderia sp. strain LB400, which is one of the most versatile, dioxygenation at C-2 and C-3 is preferred, and hydroxylation at atoms bearing chlorine substituents is restricted to the ortho positions with elimination of chloride in place of dehydrogenation (Seeger et al. 1999). The preferred site also depends, however, on the substitution pattern of the other ring, and 2′- and 2′,6′-dichlorobiphenyls seriously inhibit the activity of dihydroxybiphenyl dioxygenase (Dai et al. 2002). It had been suggested that substrate inhibition of the dioxygenase was a result of enzyme inactivation, and a general mechanism for inhibition of the dioxygenase by catechols involving formation of the complex between the substrate and the Fe(II) enzyme has been suggested (Vaillancourt et al. 2002). This has been explored further (Fortin et al. 2005) using extradiol dioxygenases from organisms with established ability to degrade PCBs—Burkholderia sp. strain LB400, two isoenzymes from Rhodococcus globerulus strain P6, and Sphingomonas sp. strain RW1. Rates of dioxygenation were measured from the rate of formation of the ission product 2-hydroxy-6-keto-6phenylhexa-2,4-dienoate. Important conclusions emerged: (i) rates for the monochlorinated isomers were lower than those for the nonchlorinated 2,3-dihydrodihydroxybenzoate and (ii) among polychlorinated congeners, the rate for the recalcitrant 2′,6′dichloro-dihydroxybiphenyl was the lowest. 2. The next step in degradation involves hydrolysis of 2-hydroxy-6-keto-6-phenylhexa-2, 4-dienoate to benzoate and 2-hydroxy-penta-2,4-dienoate encoded by the hydrolase BphD. A study of the hydrolase in Burkholderia cepacia LB 400 has revealed signiicant details (Seah et al. 2000) (Figure 9.6a): a. There are substantial differences in the rates of hydrolysis by the hydrolase. b. The 4-chloro compound is hydrolyzed nonenzymatically to the 4-hydroxy compound, which may undergo cleavage to acetophenone and 3-ketoadipate (Figure 9.6b). c. The 3-chloro compound is stable to enzymatic hydrolysis and strongly inhibits the hydrolase.

462

Environmental Degradation and Transformation of Organic Chemicals OH

OH

(a)

O O H CO 2H

OH

CO 2H

O O H CO 2H

HO

Cl

Cl

OH 2 5 8 9

(b) Cln

Cln

6

Cl

Co 2H

OH

4 3 2 O O H CO 2H 1

O O H CO 2H Cln

10 OH

O O H CO 2H Cln O CH3 HO 2C CH2 O O H CO 2H

O

COO−CO 2H

Cln

FIGURE 9.6 Aerobic degradation of (a) biphenyl by biphenyl-2,3-dioxygenase, (b) a polychlorinated 4′-chlorobiphenyl.

3. The hydrolase is competitively inhibited by 3-chloro- and 4-chloro-2-hydroxy-6-keto6-phenylhexa-2,4-dienoate (Seah et al. 2000), and a cardinal role has been assigned to a glutathione S-transferase BphK that had not hitherto been assigned a speciic function. The bphK gene does not occur in all bacteria that are recognized as being able to degrade PCBs, and it has been shown in Burkholderia (Pseudomonas) xenovorans strain LB400 that the transferase has the ability to dechlorinate 3-chloro-, 5-chloro-, and 3,9,11trichloro-2-hydroxy-6-keto-6-phenylhexa-2,4-dienoate in reactions involving addition of GS−, elimination of Cl−, followed by generation of GSSG (Fortin et al. 2006). These observations contribute to understanding the relative recalcitrance of PCB congeners, rationalize the formation of the metabolites, and focus attention on the formation of the 3- and 4-chlorohexadienoates that would be produced from 3- and 4-chlorinated biphenyls by 2-hydroxy-6-keto-6-phenylhexa-2,4-dienoate hydrolases. Collectively, these conclusions are supported by the results of a study of 33 congeners using Acinetobacter sp. strain P6 (Rhodococcus globerulus) (Asturias and Timmis 1993). The extradiol

463

Substituted Carbocyclic Aromatic Compounds

ission product greatly exceeded the chlorobenzoates for the 2,5,4′- and 2,4,4′-trichlorobiphenyls (Furukawa et al. 1979). In this strain, however, although the speciicities of the hydrolases in Burkholderia cepacia LB 400 and Rhodococcus globerulus P6 were essentially similar, signiicant differences have been observed (Seah et al. 2001). In the former, inhibition by 3-chlorohexadienoate exceeded that of 4-chlorohexadienoate, whereas the opposite was found in the latter. Metabolites Chlorobenzoates and Catechols a. Total degradation of PCBs necessitates degradation of the chlorobenzoates produced by the foregoing reactions. It has been suggested that the inability of strains to degrade chlorobenzoates produced from some PCB congeners may be related to the restricted metabolism of chlorobenzoate ission products (Hernandez et al. 1995). The distribution of chlorobenzoates has indeed been suggested as biomarkers for the aerobic degradation of PCBs (Flanagan and May 1993). The inhibitory nature of chlorocatechols that are metabolites of chlorobenzoates has already been noted. b. Another metabolic limitation involves the formation of protoanemonin (4-methylenebut2-ene-4-olide) as an intermediate in the degradation of 4-chlorobenzoate formed by partial degradation of 4-chlorobiphenyl. This is formed by the intradiol ission of 4-chlorocatechol to 3-chloro-cis,cis-muconate followed by loss of CO2 and chloride (Blasco et al. 1995) (Figure 9.7). The synthesis of this metabolite adversely affects the survival of organisms that metabolize 4-chlorobiphenyl in soil microcosms, although its formation can be obviated by organisms using a modiied pathway that produces the cis-dienelactone (Blasco et al. 1997). Acetophenones Quite different metabolites may also be formed. Although the ultimate products from the degradation of PCBs are generally chlorinated muconic acids, the unusual metabolite 2,4,5-trichloroacetophenone has been isolated (Bedard et al. 1987b) from the degradation of 2,4,5,2′,4′,5′-hexachlorobiphenyl (Figure 9.8) by Alcaligenes eutrophus H850, which has an unusually wide spectrum of degradative activity for PCB congeners. The mechanism for the formation of 2,4,5-trichloroacetophenone may be analogous to the formation of acetophenones by nonenzymatic hydrolysis of the 4′-chlorinated compound. The metabolism of chloroacetophenones takes place by monooxygenation to the corresponding chlorophenylesters. Some ortho-substituted chlorophenols are, however, inhibitory, and only low rates of oxidation have been encountered with di- and trichlorinated

O CO 2 H CO 2 H

O

OH OH

O

CO 2 H

CH 3 CO 2 H Cl

Cl

Cl

O CO 2 H O O CO 2 H

FIGURE 9.7

Formation of protoanemonin from 4-chlorobenzoate.

CO 2 H

464

Environmental Degradation and Transformation of Organic Chemicals Cl Cl

Cl Cl

Cl Cl

Cl COCH 3

Cl Cl

FIGURE 9.8

Biodegradation of 2,4,5,2′,4′,5′-hexachlorobiphenyl.

acetophenones, so that growth with them is not possible (Higson and Focht 1990). However, degradation of 4-chloroacetophenone has been demonstrated with a mixed culture of an Arthrobacter sp. and a Micrococcus sp. (Havel and Reineke 1993). The NIH Shift A rearrangement (NIH shift) occurred during the transformation of 2-chlorobiphenyl to 2-hydroxy3-chlorobiphenyl by a methanotroph, and is consistent with the formation of an intermediate arene oxide (Adriaens 1994). The occurrence of such intermediates also offers plausible mechanisms for the formation of nitro-containing metabolites that have been observed in the degradation of 4-chlorobiphenyl in the presence of nitrate (Sylvestre et al. 1982). Induction of PCB Metabolism

Apart from induction of degradative enzymes by growth with biphenyl, nonrelated naturally occurring substrates have been shown to induce the enzymes for PCB degradation. a. A range of related compounds was examined (Donnelly et al. 1994) for their capacity to support the growth of Alcaligenes eutrophus H850, Pseudomonas putida LB400, and Corynebacterium sp. MB1. For strains H850 and MB1, growth with biphenyl equaled that using a wide range of substrates including naringin, catechin, and myricitin (Figure 9.9). These results suggest that natural plant metabolites are able to mediate the growth of PCBdegrading organisms. In addition, the pattern of metabolism of PCB congeners was identical using biphenyl or the naturally occurring plant metabolites. b. Cells of Arthrobacter sp. strain B1B were grown in a mineral medium with fructose and carvone (50 mg/L). Effective degradation of a number of congeners in Arochlor 1242 was induced by carvone that could not, however, be used as a growth substrate, and was toxic at high concentrations (>500 mg/L). Other structurally related compounds including limonene, p-cymene, and isoprene were also effective (Gilbert and Crowley 1997). These results may be particularly relevant in the context of bioremediation, and lend support to the potential role of the rhizosphere and of plants (Chapters 12 and 14, Part 4). There are other changes that are involved in the metabolism of biphenyls and PCBs. A study of the degradation of biphenyl by Burkholderia xenovorans LB400 showed that elevated levels of the enzymes involved in the upper Bph pathway were induced by growth with biphenyl, whereas those for benzoate degradation were upregulated by growth on benzoate. Enzymes for the latter involved conversion to benzoyl-CoA and use of the pathway delineated for Azoarcus evansii (Denef et al. 2004). Accumulation of inorganic polyphosphate is induced in cells exposed to stress, and has been observed during the growth of Pseudomonas sp. strain B4 in a deined medium with biphenyl, and on changing the growth substrate from glucose to biphenyl (Chávez et al. 2004).

465

Substituted Carbocyclic Aromatic Compounds OH

O

HO

OH

HO

O

O

HO

Esculetin

O Quercitin

OH OH

OH

OH

O

O

OH HO

OH

O Myricitin

HO

O Naringenin

OH

OH

OH OH OH

HO

O

O Catechin

OH OH

FIGURE 9.9

Carvone

Limonene

Naturally occurring products used as substrates or inducers.

FUNGAL DEHALOGENATION Dehalogenation of commercial PCB mixtures has been observed using Phanerochaete chrysosporium in different media including low nitrogen, high nitrogen, and complex malt extract (Yadav et al. 1995). Dechlorination of congeners with ortho, meta, and para substituents occurred. Maximal dechlorination ranged from 61% for Arochlor 1242 to 18% for Arochlor 1260, and although it was greatest in malt extract medium, it also occurred in low- and high-nitrogen media.

REDUCTIVE DEHALOGENATION The anaerobic dechlorination of PCBs has been extensively studied both in laboratory microcosms and in ield samples from heavily contaminated sites in the United States. A complex pattern of dechlorination has been described that depends on the site and environmental factors such as concentration of organic carbon and sulfate (Bedard and Quensen 1995). In a study where dechlorination was stimulated by addition of brominated biphenyls (Bedard et al. 1998; Wu et al. 1999), three main patterns were found—N that removed lanked meta chlorines, P that removed para chlorines, and LP that removed unlanked para chlorines. The example of the 2,2′,3,4,4′,5,5′-heptachloro (2345-245) congener is given in Figure 9.10. For the heptachloro congener 2,2′,3,3′,4,4′,5 (2345234), a combination of processes N, P, and LP resulted in the production of the 2,2′-dichloro- and 2,2′,5-trichloro congeners (Bedard et al. 2005). In contrast, ortho chlorines were more recalcitrant. An important study using sediment contaminated with Arochlor 1260 was initiated by priming with 2,6-dibromobiphenyl to select for N dechlorination. Successive dilution produced sedimentfree cultures that grew with acetate, butyrate or pyruvate, and H2 and resulted in a range of bacteria. These were able to dechlorinate hexa- through nonachlorinated congeners to tri- through

466

Environmental Degradation and Transformation of Organic Chemicals 2345-245-CB

Process N

Process P

Cl

Cl

Cl

Cl

Cl

Cl Cl

Cl

Cl 235-25-CB

24-24-CB

Cl

Cl 2-2-CB

FIGURE 9.10 Anaerobic dechlorination of 2,2′,3,4,4′,5,5′-heptachlorobiphenyl. (From Neilson, A.H. and Allard, A.-S., The Handbook of Environmental Chemistry, Vol. 3R, Springer Verlag, 2002, pp. 1–74. With permission.)

pentachlorinated congeners, and dechlorination of heptachloro congeners produced the 2,2′,4′,5 (25-24), 2,2′,4,6′ (24-26) and 2,2′,5,6′ (25-26) tetrachloro congeners with retention of the ortho substituents (Bedard et al. 2006). It is important to appreciate important factors that affect the relative effectiveness of dechlorination: (a) temperature (Wu et al. 1997b) that is discussed in greater detail below and (b) the nature of the PCB congener that primes the dehalogenation (Wu et al. 1997a). In contrast to the results discussed above, an enrichment culture supplemented with acetate was able to dechlorinate 2,3,5,6-tetrachlorobiphenyl to 3,5-dichlorobiphenyl with the removal of ortho chlorines (Holoman et al. 1998), and success is being achieved in deining the organisms responsible. For example, a nonmethanogenic mixed culture containing strain o-17 was able to bring about dechlorination of ortho-halogenated congers 2,3,5,6-tetrachlorobiphenyl to 3,5-dichlorobiphenyl (May et al. 2006). Substantial attention has been given to organisms within the Dehalococcoides group and the green nonsulfur phylum Chlorolexi (Fagervold et al. 2005). Examples include the following: (a) laboratory studies using enriched cultures speciically dechlorinated PCBs with doubly lanked chlorines (Wu et al. 2002), (b) cultures containing Dehalococcoides ethenogenes carried out sequential dechlorination of 2,3,4,5,6-pentachlorobiphenyl to 2,4,6-trichlorobiphenyl (Fennell et al. 2004), and (c) it has been shown that individual species of Chlorolexi have different speciicities (Fagervold et al. 2005). The Role of Temperature This is an important parameter particularly for naturally occurring mixed cultures of organisms in the natural environment: temperature may result in important changes in the composition of the microbial lora as well as on the rates for different processes. An illustrative example of its importance includes the following. An anaerobic sediment sample was incubated with

Substituted Carbocyclic Aromatic Compounds

467

2,3,4, 6-tetrachlorobiphenyl at various temperatures between 4 and 66°C (Wu et al. 1997a,b). The main products were 2,4,6- and 2,3,6-trichlorobiphenyl and 2,6-dichlorobiphenyl; the irst was produced maximally and discontinuously at 12 and 34°C, the second maximally at 18°C, and the third was dominant from 25 to 30°C. Dechlorination was not observed above 37°C. Collectively, there is therefore extensive evidence for the anaerobic dechlorination of PCBs but the extent and speciicity of this depends on both the organism and the degree and pattern of substituents in the congener. Polybrominated Biphenyls and Diphenylmethanes

Mixed cultures of organisms that were isolated from sediments contaminated with PCBs and polybrominated biphenyls (PBBs) were shown to debrominate PBBs under anaerobic conditions (Morris et al. 1992), and the dominant congener—2,2′,4,4′,5,5′(245-245)-hexabromobiphenyl—could be successively debrominated to 2,2′-dibromobiphenyl. However, in sediments from the most heavily contaminated site containing contaminants in addition to PBBs, very little debromination occurred and the recalcitrance was attributed to the toxicity of the other contaminants (Morris et al. 1993). Ingenious experiments to which reference has already been made have used addition of speciic PCB congeners that are more readily dechlorinated to “prime” dechlorination at speciic positions (Bedard and Quensen 1995). They have been extended to the use of dibrominated biphenyls in the presence of malate to stimulate dechlorination of the hexachloro- to nanochlorobiphenyls (Bedard and Quensen 1995). Results from these experiments provide valuable evidence of important differences between anaerobic dechlorination and anaerobic debromination, and the greater facility of the latter. The use of brominated biphenyls to induce dechlorination of highly chlorinated biphenyls has been examined in detail. Di- and tribromobiphenyls were the most effective in dechlorinating the PCBs including the heptachloro, hexachloro, and pentachloro congeners, and were themselves reduced to biphenyl (Bedard et al. 1998). In addition, 2,6-dibromobiphenyl stimulated the growth of anaerobes that effectively dechlorinated hexa-, hepta-, octa-, and nanochlorobiphenyls over the temperature range 8–30°C (Wu et al. 1999). In anaerobic sediment microcosms, a range of tribrominated biphenyls was successively debrominated to dibromo- and monobromo compounds before complete debromination to biphenyl. Of particular interest, both the 2,2′,4′,5 (25-24) and 2,2′,5,5′ (25-25) tetrabromo congeners were debrominated to the 2,2′-dibromo congener that was slowly and completely debrominated to biphenyl within 54 weeks (Bedard and van Dort 1998). The pathways for debromination of 2,2′,4,5′- and 2,2′,5,5′-tetrabromobiphenyls are shown in Figure 9.11. In comparable microcosm experiments, a number of important features were observed: a. All the tribrominated congeners were debrominated to products including biphenyl in acclimation times between 5— although organisms have been isolated that degrade short-chain (C1–C4) primary alkyl sulfates (White et al. 1987). Pseudomonas sp. strain C12B produces two primary (P1 and P2) and three secondary (S1, S2, and S3) alkylsulfatases, and hydrolysis by the P1 enzyme takes place by O–S bond ission. The S1 and S2 enzymes are constitutive, and for chiral compounds such as octan-2-yl 569

570

Environmental Degradation and Transformation of Organic Chemicals

(a)

CH3 CH3

(b)

FIGURE 11.1

CH−O−SO3H2

CH3−O−SO3H2

CH3−CH−CO2H O−SO3H2

HO−CH2−O−SO3H2

CH3−CH(OH)−CO2H

CH2O

Degradation of (a) propan-2-yl sulfate and (b) methyl sulfate.

sulfate, hydrolysis proceeds with inversion of coniguration by cleavage of the alkyl–oxygen bond (Bartholomew et al. 1977). For example, hydrolysis of (R)-2-octyl sulfate by Rhodococcus ruber DSM 44541 proceeded with inversion to (S)-2-octanol (Pogorevc and Faber 2003). As an alternative pathway for degradation, oxidation may precede elimination of sulfate. Examples include the degradation of propan-2-yl sulfate (Crescenzi et al. 1985) and of monomethyl sulfate (Davies et al. 1990; Higgins et al. 1993) (Figure 11.1). Under sulfate limitation, Pseudomonas putida strain S-313 degraded alkyl sulfates (C4 –C12) to sulfate and the corresponding aldehyde by a 2-ketoaciddependent reaction in the presence of Fe2+. Exceptionally, other 2-ketoacids could be used including 2-ketoglutarate, 2-ketovalerate, and 2-ketoadipate (Kahnert and Kertesz 2000). For alkylethoxy sulfates, a greater range of possibilities exist including ether-cleavage reactions, while direct removal of sulfate may be of lesser signiicance (Hales et al. 1986). It should be noted, however, that an unusual reaction may occur simultaneously: chain elongation of the carboxylic acid. For example, during degradation of dodecyl sulfate, lipids containing 14, 16, and 18 carbon atoms were synthesized (Thomas and White 1989). Transformations by monooxygenation rather than hydrolysis have been described for the organochlorine insecticides endosulfan and endosulfate in organisms that use them as sources of sulfur in the absence of inorganic sulfur. Hydroxylation at the position adjacent to the oxygen is mediated by a monooxygenase and a reduced lavin, and results in the production of sulite from β-endosulfan by Mycobacterium sp. strain ESD (Sutherland et al. 2002). Analogous monooxygenation of α- and β-endosulfan, and endosulfate can be carried out by a species of Arthrobacter (Weir et al. 2006). Aryl sulfates are widely synthesized from phenolic substrates and serve as a detoxiication mechanism both for microorganisms and for ish. Hydrolysis of aryl esters takes place with ission of the O–S bond (Recksiek et al. 1998), whereas for aliphatic sulfates, ission of the C–O bond takes place. In addition, utilization of aryl sulfate may be mediated by an arylsulfotransferase (Kahnert et al. 2000). As for alkyl sulfates, sulfate is formed from aryl sulfates and, for aryl sulfates the pathway of degradation is controlled by the source of sulfur (Cook et al. 1999). The hydrolysis of aryl sulfates has traditionally been a useful taxonomic character in the genus Mycobacterium (Wayne et al. 1991). A positive result in the 3-d aryl sulfatase test based on the hydrolysis of phenolphthalein sulfate has been particularly valuable for distinguishing members of the rapidly growing M. fortuitum group, which are potentially pathogenic to man, whereas the slow-growing M. tuberculosis and M. bovis are negative even after 10 d. Regulation of the synthesis of tyrosine sulfate sulfohydrolase has been examined in a strain of Comamonas terrigena (Fitzgerald et al. 1979), and both inducible and constitutive forms of the enzyme exist. These are, however, apparently distinct from the aryl sulfate sulfohydrolase, which has found application in taxonomic classiication.

PHOSPHATES Aryl phosphates and thiophosphates, and alkyl dithiophosphates are important agrochemicals, while phosphoroluoridates have been prepared as chemical warfare agents. Concern over the persistence and the biodegradability of organophosphate and organophosphorothioates, which are used as agrochemicals, has stimulated studies into their degradation. Considerable attention has been

571

Miscellaneous Compounds

directed to biodegradation of all of them, and references may be found in Munnecke et al. (1982), DeFrank and White (2002), and Singh et al. (2004). The hydrolytic enzyme(s)—organophosphorus acid anhydrase (OPA)—responsible for deluorination of phospholuoridates are noted in Chapter 14, Part 6. These studies have revealed the widespread distribution of bacterial triesterases, whereas diesterases are less common, although an enzyme from Delftia acidovorans has been described (Tehara and Keasling 2003). The irst step in the degradation of phosphate and phosphorothioate esters is hydrolysis, and substantial effort has been directed to all groups. Investigations have also been directed to the use of their degradation products as a source of phosphate for the growth of bacteria, and a wide range of phosphates, dialkylphosphates, and phosphorothioates has therefore been examined as sources of phosphorus (Cook et al. 1978). It is important to emphasize that the initial metabolites after hydrolysis may be both toxic and sometimes resistant to further degradation. Examples include nitrophenols, whose degradation is discussed in Chapter 9, Part 5; and 3,5,6-trichloropyridin-2-ol (Feng et al. 1997), which is produced by the hydrolysis of chlorpyrifos (O,O-diethyl-O-[3,5,6-trichlo-2-pyridyl]phosphorothioate).

NITRATES Compared with the fairly numerous investigations on the microbial degradation of carboxylic acid, sulfate, and phosphate esters, data on the degradation of nitrate esters are more fragmentary. This has been clearly revealed in a review (White and Snape 1993), which summarized existing knowledge on the microbial degradation of nitrate esters including glycerol trinitrate and its close relatives, and the pharmaceutical products pentaerythritol tetranitrate and isosorbide 2,5-dinitrate. Examples include glycerol trinitrate (Marshall and White 2001) and pentaerythritol tetranitrate (French et al. 1996), which are important explosives. Reactions involving glutathione transferases are important in eukaryotic microorganisms (White et al. 1996). In bacteria, however, the degradation of nitrate esters takes place by reduction with loss of nitrite (Figure 11.2), and pentaerythritol tetranitrate reductase, which is related to “old yellow enzyme” (French et al. 1996), and glycerol trinitrate reductase (Snape et al. 1997) have been puriied. The reductase from E. cloacae is strongly inhibited by steroids and is capable of the reduction of cyclohex-2-ene-1-one (French et al. 1996). The biotransformation of gylcerol trinitrate by strains of Bacillus thuringiensis/cereus or Enterobacter agglomerans (Meng et al. 1995), by strains of Pseudomonas sp., and some Enterobacteriaceae (Blehert et al. 1997) involves the expected successive loss of nitrite with the formation of glycerol. The biotransformation of pentaerythritol tetranitrate by Enterobacter cloacae proceeds comparably with metabolism of two hydroxymethyl groups produced by loss of nitrite to the aldehyde (Binks et al. 1996). In a medium containing glucose and ammonium nitrate, glyceryl trinitrate is degraded by Penicillium corylophilum to the di- and mononitrate before complete degradation. In contrast, the metabolism of glyceryl trinitrate by Phanerochaete chrysosporium involves the production of nitric oxide (Servent et al. 1991). Nitric oxide is produced during conversion of l-arginine into l-citrulline by a strain of Nocardia sp. (Chen and Rosazza 1995), and a summary of the mechanism, which includes both prokaryotic and mammalian systems, has been given (Stuehr et al. 2004).

O2NOCH2 O2NOCH2

FIGURE 11.2

C

CH2O−NO2 CH2−O−NO2

O2NOCH2 HOCH2

Reductive degradation of pentaerythritol tetranitrate.

C

CH2OH CH2−O−NO2

572

Environmental Degradation and Transformation of Organic Chemicals

REFERENCES Akutsu Y, T Nakajima-Kambe, N Nomura, T Nakahara (1998) Puriication and properties of a polyester polyurethane-degrading enzyme from Comamonas acidovorans TB-35. Appl Environ Microbiol 64: 62–67. Bartholomew B, KS Dodgson, GWJ Matcham, DJ Shaw, GF White (1977) A novel mechanism of enzymatic hydrolysis. Inversion of coniguration and carbon–oxygen bond cleavage by secondary alkylsulphohydrolases from detergent-degrading micro-organisms. Biochem J 165: 575–580. Binks PR, CE French, S Nicklin, NC Bruce (1996) Degradation of pentaerythritol tetranitrate by Enterobacter cloacae PB2. Appl Environ Microbiol 62: 1214–1219. Blehert DS, KL Knoke, BG Fox, GH Cambliss (1997) Regioselectivity of nitroglycerine denitration by lavoprotein nitroester reductases puriied from two Pseudomonas species. J Bacteriol 179: 6912–6920. Britt AJ, NC Bruce, CR Lowe (1992) Identiication of a cocaine esterase in a strain of Pseudomonas maltophilia. J Bacteriol 174: 2087–2094. Cain RB (1981) Microbial degradation of surfactants and “builder” components. In Microbial Degradation of Xenobiotics and Recalcitrant Compounds (Eds T Leisinger, AM Cook, R Hütter, and J Nüesch), pp. 325–370. Academic Press, London. Chen Y, JPN Rosazza (1995) Puriication and characterization of nitric oxide synthase NOSNoc from a Nocardia sp. J Bacteriol 177: 5122–5128. Cook AM, CG Daughton, M Alexander (1978) Phosphorus-containing pesticide breakdown products: quantitative utilization as phosphorus sources by bacteria. Appl Environ Microbiol 36: 668–672. Cook AM, H Laue, F Junker (1999) Microbial desulfonation FEMS Microbiol Rev 22: 399–419. Crescenzi AMV, KS Dodgson, GF White, WJ Payne (1985) Initial oxidation and subsequent desulphation of propan-2-yl sulphate by Pseudomonas syringae strain GG. J Gen Microbiol 131: 469–477. Davies I, GF White, WJ Payne (1990) Oxygen-dependent desulphation of monomethyl sulphate by Agrobacterium sp. M3C. Biodegradation 1: 229–241. DeFrank JJ, WE White (2002) Phosphoroluoridates: biological activity and biodegradation. Handbook Environ Chem 3N: 295–343. Dodson KS, GF White (1983) Some microbial enzymes involved in the biodegradation of sulfated surfactants. In Topics in Enzyme and Fermentation Technology (Ed A Wiseman), Vol 7, pp. 90–155. Ellis-Horwood, Chichester. Eaton RW, DW Ribbons (1982) Metabolism of dibutylphthalate and phthalate by Micrococcus sp. strain 12B. J Bacteriol 151: 48–57. Ellis AW, SG Hales, NGA Ur-Rehman, GF White (2002) Novel alkylsulfatases required for biodegradation of the branched primary alkyl sulfate surfactant 2-butyloctyl sulfate. Appl Environ Microbiol 68: 31–36. Feng Y, KD Racke, J-M Bollag (1997) Isolation and characterization of a chlorinated-pyridinol-degrading bacterium. Appl Environ Microbiol 63: 4096–4098. Fitzgerald JW (1976) Sulfate ester formation and hydrolysis: a potentially important yet often ignored aspect of the sulfur cycle of aerobic soils. Bacteriol Rev 40: 698–721. Fitzgerald JW, HW Maca, FA Rose (1979) Physiological factors regulating tyrosine-sulphate sulphohydrolase activity in Comamonas terrigena: occurrence of constitutive and inducible enzymes. J Gen Microbiol 111: 407–415. French CE, S Nicklin, NC Bruce (1996) Sequence and properties of pentaerythritol tetranitrate reductase from Enterobacter cloacae PB 2. J Bacteriol 178: 6623–6627. Hales SG, GK Watson, KS Dodson, GF White (1986) A comparative study of the biodegradation of the surfactant sodium dodecyltriethoxy sulphate by four detergent-degrading bacteria. J Gen Microbiol 132: 953–961. Higgins TP, JR Snape, GF White (1993) Comparison of pathways for biodegradation of monomethyl sulphate in Agrobacterium and Hyphomicrobium species. J Gen Microbiol 139: 2915–2920. Kahnert A, MA Kertesz (2000) Characterization of a sulfur-regulated oxygenative alkylsulfatase from Pseudomonas putida S-313. J Biol Chem 275: 31661–31667. Kahnert A, P Vermeli, C Wietek, P James, T Leisinger, MA Kertesz (2000) The ssu locus plays a key role in organosulfur metabolism in Pseudomonas putida S-313. J Bacteriol 182: 2869–2878. Kertesz MA (1999) Riding the sulfur cycle—metabolism of sulfonates and sulfate esters by Gram-negative bacteria. FEMS Microbiol Rev 24: 135–175. Li J, J-D Gu, L Pan (2005) Transformation of dimethyl phthalate, dimethyl isophthalate, and dimethylterephthalate by Rhodococcus rubber Sa and modeling the process using the modiied Gompertz model. Int Biodet Biodeg 55: 223–232.

Miscellaneous Compounds

573

Marshall SJ, GF White (2001) Complete denitration of nitroglycerin by bacteria isolated from a washwater soakaway. Appl Environ Microbiol 67: 2622–2626. Meng M, W-Q Sun, LA Geelhaar, G Kumar, AR Patel, GF Payne, MK Speedie, JR Stacy (1995) Denitration of glycerol trinitrate by resting cells and cell extracts of Bacillus thuringiensis/cereus and Enterobacter agglomerans. Appl Environ Microbiol 61: 2548–2553. Munnecke DM, LM Johnson, HW Talbot, S Barik (1982) Microbial metabolism and enzymology of selected pesticides. In Biodegradation and Detoxiication of Environmental Pollutants (Ed AM Chrakrabarty), pp. 1–32. CRC Press, Boca Raton, FL. Pogorevc M, K Faber (2003) Puriication and characterization of an inverting stero- and enantioselective sec-alkylsulfatase from the Gram-positive bacterium Rhodoccus ruber DSM 44541. Appl Environ Microbiol 69: 2810–2815. Recksiek M, T Selmer, T Dierks, B Schmidt, K von Figura (1998) Sulfatases, trapping of the sulfonated enzyme intermediate by substituting the active site formylglycine. J Biol Chem 273: 6096–6103. Servent D, C Ducrorq, Y Henry, A Guissani, M Lenfant (1991) Nitroglycerin metabolism by Phanerochaete chrysosporium: evidence for nitric oxide and nitrite formation. Biochim Biophys Acta 1074: 320–325. Singh BK, A Walker, JAW Morgan, DJ Wright (2004) Biodegradation of chloropyrifos by Enterobacter strain B-14 and its use in bioremediation of contaminated soils. Appl Environ Microbiol 70: 4855–4863. Snape JR, NA Walkley, AP Morby, S Nicklin, GF White (1997) Puriication, properties, and sequence of glycerol trinitrate reductase from Agrobacterium radiobacter. J Bacteriol 179: 7796–7802. Stuehr DJ, J Santolini, Z-Q Wang, C-C Wei, S Adak (2004) Update on mechanism and catalytic regulation in the NO synthases. J Biol Chem 36167–36170. Sutherland TD, I Horne, RJ Russell, JG Oakeshott (2002) Gene cloning and molecular characterization of a two-enzyme system catalyzing the oxidative detoxiication of β-endosulfan. Appl Environ Microbiol 68: 6237–6245. Tehara SK, JD Keasling (2003) Gene cloning, puriication, and characterization of a phosphodiesterase from Delftia acidovorans. Appl Environ Microbiol 69: 504–508. Thomas ORT, GF White (1989) Metabolic pathway for the biodegradation of sodium dodecyl sulfate by Pseudomonas spC12B. Biotechnol Appl Biochem 11: 318–327. Wayne LG et al. (1991) Fourth report of the cooperative, open-ended study of slowly growing mycobacteria by the international working group on mycobacterial taxonomy. Int J Syst Bacteriol 41: 463–472. Weir KM, TD Sutherland, I Horne, RJ Russell, JG Oakshott (2006) A singe monooxygenase, Ese, is involved in the metabolism of the organochlorines endosulfan and endosulfate in an Arthrobacter sp. Appl Environ Microbiol 72: 3524–3530. White GF, JR Snape (1993) Microbial cleavage of nitrate esters: defusing the environment. J Gen Microbiol 139: 1947–1957. White GF, JR Snape, S Nicklin (1996) Bacterial biodegradation of glycerol trinitrate. Int Biodet Biodeg 38: 77–82. White GF, KS Dodson, I Davies, PJ Matts, JP Shapleigh, WJ Payne (1987) Bacterial utilisation of short-chain primary alkyl sulphate esters. FEMS Microbiol Lett 40: 173–177. White GF, NJ Russell (1994) Biodegradation of anionic surfactants and related molecules. In Biochemistry of Microbial Degradation (Ed C Ratledge), pp. 143–177. Kluwer Academic Publishers, Dordrecht, The Netherlands.

PART 2 ETHERS AND SULFIDES The degradation of a structurally wide range of ethers under both aerobic and anaerobic conditions is covered in a review (White et al. 1996), which should be consulted for details, particularly of polyethers.

ALIPHATIC AND BENZYLIC ETHERS Aliphatic and benzylic ethers are degraded by hydroxylation of the α-methylene group followed by scission of the ether bond with the formation of an aldehyde and an alkanol (White et al. 1996; Kim and Engesser 2004). In contrast, the degradation of 2-chloroethylvinyl ether by Ancylobacter

574

Environmental Degradation and Transformation of Organic Chemicals

aquaticus is initiated by a dehalogenase, although ission of the C–O–C bond is nonenzymatic (van den Wijngaard et al. 1993). 1. The monooxygenase from Burkholderia cepacia G4/PR1 in which the synthesis of toluene2-monooxygenase is constitutive is able to degrade a number of ethers including diethyl ether and n-butyl methyl ether, though not tert-butyl methyl ether (Hur et al. 1997). 2. tert-Butyl methyl ether (MTBE) has been used as a gasoline additive, and concern has arisen over its biodegradability in view of its water solubility that facilitates dispersion in aquatic systems (Johnson et al. 2000). Although pure cultures have been isolated that are able to mineralize MTBE (Hanson et al. 1999; Hatzinger et al. 2001), there are a number of issues that determine its biodegradation and the pathway that is used: this has been evaluated in dicyclopropylketone-induced and n-octane-grown cells of Pseudomonas putida Gpo1 (Smith and Hyman 2004). Propane-grown cells of Mycobacterium vaccae JOB5 and a strain ENV425 obtained by propane enrichment transformed MTBE to tert-butanol or, by hydroxylation (monooxygenation) of the quaternary methyl group to 2-hydroxyisobutyric acid, which was not, however, used as a growth substrate for the organisms (Figure 11.3) (Steffan et al. 1997). In contrast, Mycobacterium austroafricanum strain IFP 2012 transformed MTBE to tert-butanol, 2-methyl-1,2-propandiol, and 2-hydroxyisobutyrate that was degraded (Ferreira et al. 2006). A pathway for its degradation was proposed that involved a cobalamin-dependent mutase, which converted 2-hydroxyisobutyrate-CoA into 3-hydroxybutyryl-CoA (Rohwerder et al. 2006). 3. Degradations of symmetrical long-chain dialkyl ethers are used to illustrate an entirely different metabolic pathway. The di-n-heptyl-, di-n-octyl-, di-n-nonyl-, and di-n-decyl ethers are degraded by a strain of Acinetobacter sp. to two different groups of metabolites (Figure 11.4): a. To n-heptan-, n-octan-, n-nonan-, and n-decanol-1-acetic acids, which were not metabolized further. b. To glutaric (C5), adipic (C6), pimelic (C7), and suberic (C8) acids, which served as sources of carbon and energy. These compounds were formed by terminal oxidation

CH3

CH3 CH3 CH3

FIGURE 11.3

C

OCH3

CH3

C

OH

+ CH2O

CH3

CH3 CH3

Degradation of methyl tert-butyl ether.

CH3−(CH2)n −O−CH2−CH2−(CH2)n −2 −CH3

CH3−(CH2)n −O−CH2−CH2−(CH2)n −2 −CO2H

CH3−(CH2)n −O−CH2−CO2H

FIGURE 11.4

HO2C−CH2−(CH2)n −3 −CO2H

Biodegradation of di-n-heptyl ether by Acinetobacter sp.

C

OH CO2H

575

Miscellaneous Compounds

4. 5.

6. 7.

8.

9.

followed by an unusual oxidation at the carbon atom β to the ether bond (Modrzakowski and Finnerty 1980). A less usual reaction is involved in the degradation of succinyloxyacetate by Zoogloea sp. (Peterson and Llaneza 1974), which is accomplished by a lyase that produced fumarate and glycolic acid. Bis-(1-chloro-2-propyl)ether has two chiral centers and exists in (R,R)-, (S,S)-, and a meso form. It is degraded by Rhodococcus sp. with a preference for the (S,S) enantiomer with the intermediate formation of 1-chloro-propan-2-ol and chloroacetone (Garbe et al. 2006). Although hydrolysis of alkyl sulfates by sulfatases is noted in Part 1 of this chapter, ether cleavage has been shown to be the major pathway for the degradation of dodecyltriethoxy sulfate (Hales et al. 1986). Polyethylene glycol can be metabolized and used for growth by a number of bacteria, and degraded aerobically by sphingomonads including species of Sphingopyxis. Aerobic degradation is generally initiated by oxidation and an unusual lavoprotein dehydrogenase has been characterized from Sphingopyxis (Sphingomonas) terrae (Sugimoto et al. 2001). The mechanism of degradation has not, however, been resolved (White et al. 1996). In contrast, anaerobic degradation involves rearrangement. This has been investigated in a variety of organisms including Pelobacter venetianus (Schink and Stieb 1983), an Acetobacterium sp. (Schramm and Schink 1991), Desulfovibrio desulfuricans, and Bacteroides sp. (Dwyer and Tiedje 1986). The initial product is acetaldehyde, which is formed in two stages by the action of a diol dehydratase and a polyethylene glycol acetaldehyde lyase (Figure 11.5), which is apparently found in all PGE-degrading anaerobic bacteria (Frings et al. 1992). Alkylphenol polyethoxylates, which are widely used as nonionic surfactants, are partially degradable by oxidation and loss of ethoxyethyl groups. Concern has arisen, since, although the number of the ethoxy groups is reduced from about nine or more to two or three (Figure 11.6) (Maki et al. 1994; John and White 1998; Fenner et al. 2002), the metabolites are both appreciably persistent and toxic. Although the alkyl phenols may be formed from the complete oxidation of the polyethoxylate side chains, partially degraded metabolites may apparently be resistant to further degradation (Ball et al. 1989). The degradation of a highly branched nonylphenol polyethoxylate by Pseudomonas putida isolated from activated sludge involved the loss of single ethoxylate groups as acetaldehyde until two ethoxylate residues remained (John and White 1998). The mechanism is reminiscent of that involved in the anaerobic degradation of polyethylene glycols. The metabolism of diethyl ether has been studied in the fungus Graphium sp. strain ATCC 58400, which was able to use this as sole source of carbon and energy. When grown with n-butane, the fungus was able to transform—though not to degrade—tert-butyl methyl HO−(CH2−CH2−O)n −CH2−CH2−OH

HO−(CH2−CH2−O)n −CH(OH)−CH3

HO−(CH2−CH2−O)n -1−CH2−CH2OH + CH3−CHO

FIGURE 11.5 Ar ArO

FIGURE 11.6

Anaerobic biodegradation of polyethylene glycol. O

(CH2CH2O)n (CH2CH2O)n −1

CH2CH2OH CH2CH2OH

ArO ArO

(CH2CH2O)n

(CH2CH2O)n −1

Partial degradation of alkylphenol polyethoxylates.

CH2CO2H CH2CO2H

576

Environmental Degradation and Transformation of Organic Chemicals

ether to tert-butanol and tert-butyl formate (Hardison et al. 1997). The former is biodegradable under aerobic, and some anaerobic, conditions (Bradley et al. 2002). 10. Rhodococcus sp. strain 219 (Bernhardt and Dickmann 1991) and Pseudonocardia sp. strain K1 (Thiemer et al. 2003) are able to grow at the expense of tetrahydrofuran. It was suggested that degradation was initiated by monooxygenation to 2-hydroxytetrahydrofuran. Mineralization of 1,4-dioxane by Pseudonocardia dioxanivorans strain CB1190 has been described (Parales et al. 1994). Although Pseudonocardia sp. strain ENV4789 that was isolated by enrichment with tetrahydrofuran was unable to grow with 1,4-dioxan, it produced 2-hydroxyethoxyacetate as a metabolite, analogous to that produced from tetrahydrofuran (Vainberg et al. 1994). The fungus Cordyceps sinensis degraded 1,4-dioxane and other cyclic ethers including 1,3-dioxane and tetrahydrofuran. The pathway for 1,4-dioxane involved reductive formation of ethylene glycol, glycolate, and oxalate, although details of the mechanism were not presented (Nakamiya et al. 2005).

ARYL ETHERS Diaryl Ethers Halogenated derivatives of diphenyl ether have been used as herbicides (Scalla et al. 1990) and lame retardants (references in Sellström et al. 1998), and also occur naturally (Voinov et al. 1991). Attention has therefore been directed to this class of compounds that formally includes dibenzofurans and dibenzo[1,4]dioxins, which are discussed in Chapter 10, Part 2. The degradation of diphenyl ether itself by Pseudomonas cepacia has been examined (Pfeifer et al. 1989, 1993) and yields 2-pyrone-6-carboxylate as a stable end product. This may be formed from the initially produced 2,3-dihydroxydiphenyl ether in a reaction formally analogous (Figure 11.7) to that, whereby 3-O-methylgallate is converted into 2-pyrone-4,6-dicarboxylate by 3,4-dihydroxybenzoate 4,5dioxygenase in pseudomonads (Kersten et al. 1982). The degradation of diphenyl ether by a strain of Sphingomonas sp. strain SS33 took place with the ission of both rings (Schmidt et al. 1992), and cells grown with diphenyl ether were able to oxidize dibenzo[1,4]dioxin to 2-(2-hydroxyphenoxy)cis,cis-muconate. After adaptation to growth with 4,4′-diluorodiphenyl ether, the organism grew with the chlorinated, but not the brominated analogs (Schmidt et al. 1993). In general some degree of recalcitrance seems to be associated with halogenated diaryl ethers. Aryl-Alkyl Ethers 1. Phenoxyalkanoates. There has been considerable interest in the persistence of chlorinated phenoxyalkanoates—and particularly of phenoxyacetates and phenoxypropionates, which have been used as herbicides. This has therefore stimulated studies on the degradation of these aryl-alkyl ethers. Considerable effort has been directed to elucidating the subsequent

O

O OH

OH OH

CO2H

+ O

FIGURE 11.7

O

Biodegradation of diphenyl ether.

OH

O

O

CO2H

Miscellaneous Compounds

577

steps that culminate in the ission of the aromatic ring and have been discussed in Chapter 9, Part 2. The irst step in the degradation of phenoxyalkanoates is dealkylation to the corresponding phenol with the formation of glyoxylate from phenoxyacetates or acetoacetate and acetone from phenoxypropionates. This reaction is mediated by an α-ketoglutaratedependent dioxygenase (Fukumori and Hausinger 1993), and it has been shown that one atom of this is incorporated into pyruvate and succinate in cell extracts of Sphingomonas herbicidovorans by using 18O2 (Nickel et al. 1997). This strain is able to degrade both enantiomers of the racemate (R,S)-4-chloro-2-methylphenoxypropionate (mecoprop) (Zipper et al. 1996), and dioxygenases speciic for the R and S enantiomers are induced by growth of cells with the respective enantiomer (Nickel et al. 1997). Enantiospeciic dioxygenases involved in the degradation of 2-(2,4-dichlorophenoxy)propionate in Delftia acidovorans have been characterized (Schleinitz et al. 2004). The resulting chlorophenols are then degraded by intradiol ission of 2,4-dichlorocatechol and established pathways (Müller et al. 2004). 2. Aryl methyl ethers. A great deal of attention has been directed to the demethylation of aryl methyl ethers on account of interest in the degradation of lignin and related compounds by both aerobic and anaerobic organisms. a. In aerobic bacteria, the degradation of vanillate, isovanillate, and syringate is initiated by de-O-methylation, and the resulting catechols are then degraded by extradiol dioxygenation (Kasai et al. 2004; Providenti et al. 2006). Three mechanisms for the demethylation of aryl O-methyl ethers have been identiied, and are involved in the degradation of methoxylated benzoates. i. The methyl group is converted into CH2O by a dioxygenase vanA and a reductase vanB in Pseudomonas sp. strain HR199 (Priefert et al. 1997) and Acinetobacter sp. (Segura et al. 1999). The sequences of van B have been divided into three clusters (Civolani et al. 2000). ii. A tetrahydrofolate (THF) pathway in which the methyl group is transferred to 5-CH3-THF and then to 5,10-CH2-THF. For example, in Sphingomonas paucimobilis strain SYK-6, the demethylase LigM is required for the degradation of both vanillate and the product of partial O-demethylation of syringate (Abe et al. 2005). In this strain, however, the initial de-O-methylation of 2,2′dihydroxy-3,3′-dimethoxy4,4′-dicarboxybiphenyl is mediated by an unstable oxygenase (Sonoki et al. 2000), so that both mechanisms operate in the same organism. iii. In the degradation of substrates such as syringate (Kasai et al. 2004) and 3,4,5trimethoxybenzoate (Donnelly and Dagley 1980) from which 3-O-methylgallate is formed, the methyl group may be lost as methanol produced by hydrolysis of an intermediate methyl ester. This is discussed in Chapter 7, Part 3. b. Several mechanisms have been elucidated for anaerobic bacteria: i. Different organisms are able to utilize the methyl of the methoxy group for growth, for example, the acetogenic Acetobacterium woodii, although this organism is unable to degrade the aromatic ring (Bache and Pfennig 1981). In Clostridium pfennigii, the methyl group may alternatively be converted into butyrate (Krumholz and Bryant 1985), and Desulfotomaculum thermobenzoicum is able to use methoxylated benzoates in the presence or absence of sulfate (Tasaki et al. 1992). The pathways of de-O-methylation have been elucidated in A. woodii (Berman and Frazer 1992), Sporomusa ovata (Stupperich and Konle 1993), Acetobacterium dehalogenans (Kaufmann et al. 1998), and Moorella thermoacetica, and all of them involve an intermediate THF. The O-demethylase of M. thermoacetica consists of three components: MtvB carries out the O-demethylation, MtvC carries out transfer of the methyl group to Co(III) and MtvA the transmethylation to THF with production

578

Environmental Degradation and Transformation of Organic Chemicals

HO HO

HO O

O

O

O

OMe

OMe

GSH

OH

OH

FIGURE 11.8

Biotransformation of a β-aryl ether.

O

SG GSH

+

OMe

OMe

HO

HO

OMe

OMe OH

+ GSSG

OH

OMe OH

of CH3-THF that is then metabolized to acetate after incorporation of CO from CO2 (Naidu and Ragsdale 2001). ii. Methanethiol is produced by de-O-methylation in a few organisms. Sporobacterium olearium is able to use a wide range of hydroxylated and methoxylated aromatic compounds for growth (Mechichi et al. 1999). Methanethiol was produced from the methoxy groups and acetate and butyrate from the resulting 3,4,5-trihydroxylated compounds. Sulide-dependent de-O-methylation has been demonstrated in Parasporobacterium paucivorans that is able to degrade syringate with the production of both methanethiol and dimethyl sulide, while gallate that is produced from 3,4,5-trimethoxybenzoate is degraded to butyrate and acetate (Lomans et al. 2001). 3. Fission of the aryl–O bond in a β-aryl ether by Sphingomonas paucimobilis SYK-6 involves the operation of four genes: LigD, a dehydrogenase; and three tandem-located glutathione S-transferase genes LigE, LigF, a β-etherase, and LigG, a glutathione lyase (Figure 11.8) (Masai et al. 2003).

SULFIDES, DISULFIDES, AND RELATED COMPOUNDS Interest in the possible persistence of aliphatic sulides has arisen since they are produced in marine anaerobic sediments, and dimethylsulide may be implicated in climate alteration (Charlson et al. 1987). Dimethylsulfoniopropionate is produced by marine algae as an osmolyte, and has aroused attention for several reasons. It can be the source of climatically active dimethylsulide (Yoch 2002), so the role of speciic bacteria has been considered in limiting its lux from the ocean and delecting the products of its transformation into the microbial sulfur cycle (Howard et al. 2006). Sulides and related compounds may be degraded by a range of different pathways, which are illustrated in the following examples: 1. Bacteria selected for growth with bis-(3-pentluorophenylpropy)-sulide as sulfur source are able to use dimethyl sulfoxide, dibenzyl sulide, and some long-chain disulides as sources of sulfur (van Hamme et al. 2004). Degradation takes place by oxidation to the sulfone, scission of the C–S bond to an alkanol, and an alkyl sulinate that is degraded with loss of the sulfur, which is used for growth. 2. The anaerobic reduction of dimethyl sulide to methane (Oremland et al. 1989), and of dibenzyl disulide to toluenethiol and inally toluene (Miller 1992) has been described. Methanomethylovorans hollandica is able to grow anaerobically with both dimethyl sulide and methanethiol (Lomans et al. 1999); whereas dimethyl sulide, which is used as an electron donor for the growth of Rhodobacter sulidophilus, is converted into dimethyl sulfoxide (Hanlon et al. 1994).

579

Miscellaneous Compounds (a)

HS−CH2−CH(NH2)−CO2H

CH2

C

NH2 CO2H

CH3−CO−CO2H S

CH2−CH(NH2)−CO2H

NH

CH3

CH3−C(NH2)−CO2H

CO2H

S

CO2H (b) CH3−S−CH2−CH2−CH(NH2)−CO2H CH2 + (c) (CH3)2S−CH2−CH2−CO2H

CH2

CH3−S−CH2−CH2−CO−CO2H

+ CH3SH + CO2 (CH3)2S + CH2

CH−CO2H

FIGURE 11.9 Elimination reactions during metabolism of aliphatic sulfur compounds: (a) cysteine, (b) methionine, and (c) 2-dimethylsulfoniopropionate.

3. Elimination reactions have been implicated in the degradation of a variety of simple sulfur compounds: a. The desulfhydrase that brings about the degradation of l-cysteine to pyruvate was characterized in Salmonella typhimurium. The low yield of the expected pyruvate could be explained by the formation of 2-methylthiazolidine-2,4-dicarboxylate by reaction of the initially produced 2-aminoacrylate with the substrate (Kredich et al. 1973). d-Cysteine inhibits the growth of Escherichia coli but can be degraded to pyruvate, sulide, and ammonia by a desulfhydrase that is found in other enteric bacteria including Klebsiella pneumoniae, Enterobacter cloacae, and Citrobacter freundii (Nagasawa et al. 1985). Enzymatic activity involves pyridoxal phosphate, and is able to bring about elimination reactions from other d-cysteine derivatives and from 3-chloro-d-alanine (Nagasawa et al. 1988) (Figure 11.9a). Pyruvate is also formed from l-cysteine by tryptophanase (Newton et al. 1965), and in an analogous reaction from S-(2-aminoethyl)-l-cysteine by Corynebacterium glutamicum (Rossol and Pühler 1992) and Streptococcus anginosus (Yoshida et al. 2002). Exceptionally in a few bacteria, cysteine can apparently be dioxygenated to the sulinic acid from which pyruvate and sulite are produced (Dominy et al. 2006). This may putatively be carried out by a lyase that is analogous to that involved in the degradation of the corresponding sulfonate cysteate (Denger et al. 2006). b. The formation of ethene from methionine by Escherichia coli takes place by an elimination reaction (Ince and Knowles 1986) (Figure 11.9b), although considerable complexities have emerged in the control and regulation of this reaction (Mansouri and Bunch 1989). It should be noted that the synthesis of ethene in plants proceeds by an entirely different reaction via S-adenosyl methionine and 1-aminocyclopropane-1carboxylate (Kende 1989). c. Elimination is used for the degradation of dimethylsulfoniopropionate to acrylate and dimethyl sulide. This has been observed in a strain of Clostridium sp. (Wagner and Stadtman 1962) (Figure 11.9c), and in Alcaligenes sp. strain M3A and Pseudomonas doudorofii (de Souza and Yoch 1995b). The lyase has been puriied from a strain of

580

Environmental Degradation and Transformation of Organic Chemicals

an Alcaligenes-like organism (de Souza and Yoch 1995a). The acrylate is metabolized by Alcaligenes sp. strain M3A to β-hydroxypropionate (Ansede et al. 1999, 2001) and by Desulfovibrio acrylicus to propionate. This organism can use both sulfate and acrylate as electron acceptors and a range of electron donors including lactate, succinate, ethanol, propanol, glycerol, glycine, and alanine (van der Maarel et al. 1996a). It is worth noting that whereas this mechanism provides a source of dimethyl sulide in marine environments, in anaerobic freshwater habitats methyl sulide (methanethiol) and dimethyl sulide can be produced by the reaction of sulide with methoxylated aromatic compounds (Lomans et al. 2001). 4. An alternative pathway for the degradation of dimethylsulfoniopropionate involves successive de-S-methylation to 3-thiomethylpropionate and 3-mercaptopropionate: (CH3)2S+–CH2–CH2–CO2– → CH3–S–CH2–CH2–CO2H → HS–CH2–CH2–CO2H This has been observed in strain BIS-6 that was a versatile methylotroph (Visscher and Taylor 1994) and in strains of Desulfobacterium sp. (van der Maarel et al. 1996b). Exceptionally, both elimination to dimethylsulide and de-S-methylation to methanethiol have been observed in the roseobacters Silicibacter pomeroyi and Roseovarius nubinhibens. Whereas S. pomeroyi could grow at the expense of dimethylsulfoniopropionate and a number of putative degradation products including acrylate, R. nubinhibens was unable to grow with acrylate and neither strain could utilize 3-mercaptopropionate for growth (González et al. 2003). 5. Dimethyldisulide is degraded by autotrophic sulfur bacteria with the formation of sulfate and CO2, which then enters the Benson–Calvin cycle (Smith and Kelly 1988). In contrast, dimethyl sulide and dimethyl sulfoxide are degraded by a strain of Hyphomicrobium sp. by pathways involving the formation from both carbon atoms of formaldehyde, which subsequently enters the serine pathway (Suylen et al. 1986) (Figure 11.10). The key enzyme is methanethiol oxidase, which converts methanethiol into formaldehyde, sulide, and peroxide (Suylen et al. 1987). A strain of Thiobacillus sp. metabolizes dimethyl sulide by an alternative pathway involving transfer of the methyl group probably to THF by a cobalamin carrier (Visscher and Taylor 1993). Oxygen is not involved in the removal of the methyl groups, so that the reaction may proceed anaerobically. 6. Strains of some facultatively heterotrophic and methylotrophic bacteria can use CS2 as sole energy source, and under aerobic conditions also COS, dimethyl sulide, dimethyl disulide, and thioacetate (Jordan et al. 1995). It was proposed that the strains belonged to the genus Thiobacillus, though they are clearly distinct from previously described species, and they have now been assigned to Paracoccus denitriicans (Jordan et al. 1997). There has been considerable interest in the enantiomeric oxidation of sulides to sulfoxides and illustrative examples include the following: 1. Enantiomerically pure alkyl aryl sulfoxides have been obtained by the microbial oxidation of the corresponding sulides (Holland 1988). Both Corynebacterium equi, and fungi

O CH3−S−CH3

CH3−SH CH3−S−CH3 CH2O

FIGURE 11.10

H−CO2H

Biodegradation of dimethyl sulide by Hyphomicrobium sp.

CO2

Miscellaneous Compounds

581

including Aspergillus niger, species of Helminthosporium, and Mortierella isabellina were effective. The same fungi were not, however, able to carry out enantiomeric-selective oxidation of ethylmethylphenyl phosphine apparently due to the intrusion of nonselective chemical autoxidation (Holland et al. 1993). 2. The oxidation of a series of substituted phenylmethyl sulides was examined in two strains of putatively the same organism—Pseudomonas frederiksbergensis. Two signiicant features emerged: (a) the enantioselectivity varied widely among the substrates and (b) one of the strains consistently produced sulfoxides with the S coniguration, whereas the other produced those with the R coniguration (Adam et al. 2005). This is unique among sulfoxide-producing strains.

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Miscellaneous Compounds

583

Krumholz LR, MP Bryant (1985) Clostridium pfennigi sp. nov. uses methoxyl groups of monobenzenoids and produces butyrate. Appl Environ Microbiol 35: 454–456. Lomans BP, P Leijdekkers, J-P Wesselink, P Bakkes, A Pol, C van der Drift, HJP op den Camp (2001) Obligate sulide-dependent degradation of methoxylated aromatic compounds and formation of methanethiol and dimethyl sulide by a freshwater sediment isolate, Parasporobacterium paucivorans gen. nov., sp. nov. Appl Environ Microbiol 67: 4017–4203. Lomans BP, R Maas, R Luderer, HJP op den Camp, A Pol, C van der Drift, GD Vogels (1999) Isolation and characterization of Methanomethylovorans hollandica gen. nov., sp. nov., isolated from freshwater sediment, a methylotrophic methanogen able to grow with dimethyl sulide and methanethiol. Appl Environ Microbiol 65: 3641–3650. Maki H, N Masuda, Y Fujiwara, M Ile, M Fujita (1994) Degradation of alkylphenol ethoxylates by Pseudomonas sp strain TR01. Appl Environ Microbiol 60: 2265–2271. Mansouri S, AW Bunch (1989) Bacterial synthesis from 2-oxo-4-thiobutyric acid and from methionine. J Gen Microbiol 135: 2819–2827. Masai E, A Ichimura, Y Sato, K Miyauchi, Y Katayama, M Fukuda (2003) Roles of enantioselective glutathione S-transferases in cleavage of β-aryl ether. J Bacteriol 185: 1768–1775. Mechichi T, M Labat, J-L Garcia, P Thomas, BKC Patel (1999) Sporobacterium olearium gen. nov., sp. nov., a new methanethiol-producing bacterium that degrades aromatic compounds, isolated from an olive mill wastewater treatment digester. Int J Syst Bacteriol 49: 1741–1748. Miller KW (1992) Reductive desulfurization of dibenzyldisulide. Appl Environ Microbiol 58: 2176–2179. Modrzakowski MC, WR Finnerty (1980) Metabolism of symmetrical dialkyl ethers by Acinetobacter sp HO1-N. Arch Microbiol 126: 285–290. Müller TA, SM Byrde, C Werlen, JR van der Meer, H-P Kohler (2004) Genetic analysis of phenoxyalkanoic acid degradation in Sphingomonas herbicidovorans MH. Appl Environ Microbiol 70: 6066–6075. Nagasawa T, T Ishii, H Kumagai, H Yamada (1985) d-Cysteine desulfhydrase of Escherichia coli. Eur J Biochem 153: 541–551. Nagasawa T, T Ishii, H Yamada (1988) Physiological comparison of d-cycteine desulfhydrase of Escherichia coli with 3-chloro-d-alanine dehydrochlorinase of Pseudomonas putida CR 1-1. Arch Microbiol 149: 413–416. Naidu D, SW Ragsdale (2001) Characterization of a three-component vanillate O-demethylase from Moorella thermoacetica. J Bacteriol 183: 3276–3281. Nakamiya K, S Hashimoto, H Ito, JS Edmonds (2005) Degradation of 1,4-dioxane and cyclic ethers by an isolated fungus. Appl Environ Microbiol 71: 1254–1258. Newton WA, Y Morino, EE Snell (1965) Properties of crystalline tryptophanase. J Biol Chem 240: 1211–1218. Nickel K, MJ-F Suter, H-PE Kophler (1997) Involvement of two β-ketoglutarate-dependent dioxygenases in enantioselective degradation of (R)- and (S)-mecoprop by Sphingomonas herbicidovorans MH. Appl Environ Microbiol 63: 6674–6679. Oremland RS, RS Kiene, I Mathrani, MJ Whiticar, DR Boone (1989) Description of an estuarine methylotrophic methanogen which grows on dimethyl sulide. Appl Environ Microbiol 55: 994–1002. Parales RE, JE Adanus, N White, HD May (1994) Degradation of 1,4-dioxane by an actinomycete in pure cultures. Appl Environ Microbiol 60: 4527–4530. Peterson D, J Llaneza (1974) Identiication of a carbon-oxygen lyase activity cleaving the ether linkage in carboxymethyloxysuccinic acid. Arch Biochem Biophys 162: 135–146. Pfeifer F, HG Trüper, J Klein, S Schacht (1993) Degradation of diphenylether by Pseudomonas cepacia Et4: enzymatic release of phenol from 2,3-dihydroxydiphenylether. Arch Microbiol 159: 323–329. Pfeifer F, S Schacht, J Klein, HG Trüper (1989) Degradation of diphenyl ether by Pseudomonas cepacia. Arch Microbiol 152: 515–519. Priefert H, J Rabenborst, A Steinbüchek (1997) Molecular characterization of genes of Pseudomonas sp. strain HR199 involved in bioconversion of vanillin to protocatechuate. J Bacteriol 179: 2595–2607. Providenti MA, JM O′Brien, J Ruff, AM Cook, IB Lambert (2006) Metabolism of isovanillate, vanillate, and veratrate by Comamonas testosteroni strain BR6020. J Bacteriol 188: 3862–3869. Rohwerder T, U Breuer, D Benndorf, U Lechner, RH Müller (2006) The alkyl tert-butyl ether intermediate 2-hydroxyisobutyrate is degraded via a novel cobalamin-dependent mutase pathway. Appl Environ Microbiol 72: 4128–4135. Rossol I, A Pühler (1992) The Corynebacterium glutamicum aecD gene encodes a C-S lyase with alpha-betaelimination activity that degrades aminoethylcysteine. J Bacteriol 174: 2968–2977. Scalla R, M Matringe, J-M Camadroo, P Labbe (1990) Recent advances in the mode of action of diphenyl ethers and related herbicides. Z Naturforsch 45c: 503–511.

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Environmental Degradation and Transformation of Organic Chemicals

Schink B, M Stieb (1983) Fermentative degradation of polyethylene glycol by a strictly anaerobic, Gram-negative, nonsporeforming bacterium, Pelobacter venetianus sp. nov. Appl Environ Microbiol 45: 1905–1913. Schleinitz KM, S Kleinsteuber, T Vallaeys, W Babel (2004) Localization and characterization of two novel genes encoding stereospeciic dioxygenases catalyzing 2(2,4-dichlorophenoxy)propionate cleavage in Delftia acidovorans MC1. Appl Environ Microbiol 70: 5357–5365. Schmidt S, P Fortnagel, R-M Wittich (1993) Biodegradation and transformation of 4,4′- and 2,4-dihalodiphenyl ethers by Sphingomonas sp. strain SS33. Appl Environ Microbiol 59: 3931–3933. Schmidt S, R-M Wittich, D Erdmann, H Wilkes, W Francke, P Fortnagel (1992) Biodegradation of diphenyl ether and its monohalogenated derivatives by Sphingomonas sp. strain SS3. Appl Environ Microbiol 58: 2744–2750. Schramm E, B Schink (1991) Ether-cleaving enzyme and diol dehydratase involved in anaerobic polyethylene glycol degradation by a new Acetobacterium sp. Biodegradation 2: 71–79. Segura A, PV Bünz, DA D′Argenio, LN Ornston (1999) Genetic analysis of a chromosomal region containing van A and van B, genes required for conversion of either ferulate or vanillate to protocatechuate in Acinetobacter. J Bacteriol 181: 3494–3504. Sellström U, A Kierkegaard, C de Witt, B Jansson (1998) Polybrominated diphenyl ethers and hexabromocyclododecane in sediment and ish from a Swedish river. Environ Toxicol Chem 17: 1065–1072. Smith CA, MR Hyman (2004) Oxidation of methyl tert-butyl ether by alkane hydroxylase in dicyclopropylketone-induced and n-octane-grown Pseudomonas putida Gpo1. Appl Environ Microbiol 70: 4544–4550. Smith NA, DP Kelly (1988) Isolation and physiological characterization of autotrophic sulphur bacteria oxidizing dimethyl disulphide as sole source of energy. J Gen Microbiol 134: 1407–1417. Sonoki T, T Obi, S Kubota, M Higashi, E Masai, Y Katayama (2000) Coexistence of two different O demethylation systems in lignin metabolism by Sphingomonas paucimobilis SYK-6: cloning and sequencing of the lignin biphenyl-speciic O-demthylase4 (LigX) gene. Appl Environ Microbiol 66: 2125–2132. Steffan RJ, K McClay, S Vainberg, CW Condee, D Zhang (1997) Biodegradation of the gasoline oxygenates methyl tert-butyl ether, ethyl tert-butyl ether, and amyl tert-butyl ether by propane-oxidizing bacteria. Appl Environ Microbiol 63: 4216–4222. Stupperich E, R Konle (1993) Corrinoid-dependent methyl transfer reactions are involved in methanol and 3,4-dimethoxybenmzoate metabolism by Sporomusa ovata. Appl Environ Microbiol 59: 3110–3116. Sugimoto M, M Tanaba, M Hataya, S Enokibara, JA Duine, F Kawai (2001) The i rst step in polyethylene glycol degradation by sphingomonads proceeds via a lavoprotein alcohol dehydrogenase containing lavin adenine dinucleotide. J Bacteriol 183: 6694–6698. Suylen GMH, GC Stefess, JG Kuenen (1986) Chemolithotrophic potential of a Hyphomicrobium species, capable of growth on methylated sulphur compounds. Arch Microbiol 146: 192–198. Suylen GMH, PJ Large, JP van Dijken, JG Kuenen (1987) Methyl mercaptan oxidase, a key enzyme in the metabolism of methylated sulphur compounds by Hyphomicrobium EG. J Gen Microbiol 133: 2989–2997. Tasaki M, Y Kamagata, K Nakamura, E Mikami (1992) Utilization of methoxylated benzoates and formation of intermediates by Desulfotomaculum thermobenzoicum in the presence or absence of sulfate. Arch Microbiol 157: 209–212. Thiemer B, JR Andreesen, T Schrader (2003) Cloning and characterization of a gene cluster involved in tetrahydrofuran degradation in Pseudonocardia sp. strain K1. Arch Microbiol 179: 266–277. Vainberg S, K McClay, H Masuda, D Root, C Condee, GJ Zylstra, RJ Steffan (2006) Biodegradation of ether pollutants by Pseudonocardia sp. strain ENV478. Appl Environ Microbiol 72: 5218–5224. van den Wijngaard AJ, J Prins, AJAC Smal, DB Janssen (1993) Degradation of 2-chloroethylvinyl ether by Ancylobacter aquaticus AD25 and AD27. Appl Environ Microbiol 59: 2777–2783. van der Maarel MJEC, M Jansen, R Haanstra, WG Meijer, TA Hansen (1996b) Demethylation of dimethylsulfoniopropionate to 3-S-methylmercaptopropionate by marine sulfate-reducing bacteria. Appl Environ Microbiol 62: 3978–3984. van der Maarel MJEC, S van Bergeijk, AF van Werkhoven, AM Laverman, WG Maijer, WT Stam, TA Hansen (1996a) Cleavage of dimethylsulfoniopropionate and reduction of acrylate by Desulfovibrio acrylicus sp. nov. Arch Microbiol 166: 109–115. van Hamme JD, PM Fedorak, JM Foght, MR Gray, HD Dettman (2004) Use of novel luorinated organosulfur compound to isolate bacteria capable of carbon–sulfur bond ission. Appl Environ Microbiol 70: 1487–1493. Visscher PT, BF Taylor (1993) A new mechanism for the aerobic catabolism of dimethyl sulide. Appl Environ Microbiol 59: 3784–3789.

585

Miscellaneous Compounds

Visscher PT, BF Taylor (1994) Demethylation of dimethylsulfoniopropionate to 3-mercaptopropionatre by an aerobic bacterium. Appl Environ Microbiol 60: 4617–4619. Voinov VG, YuN El′kin, TA Kuznetsova, II Mal′tsev, VV Mikhailov, VA Sasunkevich (1991) Use of mass spectrometry for the detection and identiication of bromine-containing diphenyl ethers. J Chromatogr 586: 360–362. Wagner C, ER Stadtman (1962) Bacterial fermentation of dimethyl-β-propiothetin. Arch Biochem Biophys 98: 331–336. White GF, NJ Russell, EC Tidswell (1996) Bacterial scission of ether bonds. Microbiol Rev 60: 216–232. Yoch D (2002) Dimethylsulfoniopropionate: its sources, role in the marine food web, and biological degradation to dimethylsulide. Appl Environ Microbiol 68: 5804–5815. Yoshida Y, Y Nakano, A Amano, M Yoshimura, H Fukamachi, T Oho, Y Koga (2002) lcd from Streptoccus anginosus encodes a C-S lyase with α,β-elimination activity that degrades l-cysteine. Microbiology (UK) 148: 3961–3970. Zipper C, K Nickel, W Angst, H-PE Kohler (1996) Complete microbial degradation of both enantiomers of the chiral herbicide Mecoprop [(R,S)-2-(4-chloro-2-methylphenoxy)]propionic acid in an enantioselective manner by Sphingomonas herbicidovorans sp. nov. Appl Environ Microbiol 62: 4318–4322.

PART 3 ALIPHATIC NITRAMINES AND NITROALKANES NITRAMINES Aliphatic nitramines based on oligomers of –CH2–N–NO2– have been used extensively as explosives. Hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) can be used as a source of nitrogen by several bacteria, including Stenotrophomonas maltophilia strain PB1 (Binks et al. 1995). In Rhodococcus sp. this was accomplished by reduction of the ring, loss of nitrite, and formation of 4-nitro-2,4-diazabutanal as a terminal metabolite that retained one of the nitro groups (Figure 11.11) (Seth-Smith et al. 2002; Fournier et al. 2002). This metabolite is also produced from octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) by Phanerochaete chrysosporium (Fournier et al. 2004), although it can be used as a nitrogen source by the facultative methylotroph Methylobacterium sp. strain JS178 (Fournier et al. 2005). RDX can be degraded via methylenedinitramine to CH2O, CH3OH, and CO2 by Klebsiella pneumoniae strain SCZ-1 (Zhao et al. 2002). The use of RDX as a source of both carbon and nitrogen is less common, but this has been observed in Williamsia sp. strain KTR4 and Gordonia sp. strain KTR9 (Thompson et al. 2005). Under anaerobic conditions, the formation of methylenedinitramine is followed by abiotic loss of formaldehyde. Bacterial degradation of the polyazapolycyclic-caged polynitramine (2,4,6,8,10,12-hexanitro-2,4,6,8,10,12-hexaazaisowurtzitane), which will probably displace RDX, has been accomplished when it is used as a source of nitrogen (Trott et al. 2003; Bhushan et al. 2003). Its degradation by salicylate 1-monooxygenase from Pseudomonas sp. strain ATCC 29352 involved successive loss of nitrite followed by hydrolytic reactions and abiotic reactions (Bhushan et al. 2004).

NITROALKANES These contain C–NO2 bonds in contrast to the nitrate esters of, for example, glycerol and pentaerythritol with O–NO2 bonds. Nitroalkanes have been used as solvents, and there are a few naturally occurring nitroalkanes such as the glycoside of the toxic 3-nitropropionic acid and the O-methyl

O2N

N

N

NO2

N NO2

FIGURE 11.11

Degradation of RDX.

O2N

N

N N

CH2 O2N

NH

NHCHO +

H2N−CHO

586

Environmental Degradation and Transformation of Organic Chemicals CH3 CH3

H C

CH3 CH3

FIGURE 11.12

C

O

NO2

O NO2

O

CH3 CH3

O H

C

H C

NO2

CH3 CH3

2 CH3COCH3

Metabolism of 2-nitropropane.

ethers of aci-nitro compounds such as enteromycin. It has been suggested that degradation of nitroalkanes may have developed in fungi as a protection against defensive plant toxins. The structurally related aliphatic azoxy compounds are represented by the toxic macrozamin that occurs in plants as a glucoside, the antibiotic elaiomycin, and the microbial metabolite jietacin A that is an insecticide. Only limited attention has been devoted to their biodegradation and is accomplished by different types of oxidation: a. Dioxygenation of 2-nitropropane to acetone has been observed in the yeast Hansenula mrakii (Figure 11.12) (Kido et al. 1978b) and in Neurospora crassa (Gorlatova et al. 1998). Both the neutral and the aci-nitronate may react, and it has been proposed that in N. crassa the reaction proceeds via a lavosemiquinone involving the nitronate radical (Francis et al. 2005). b. A monoxygenase (oxidase) from Fusarium oxysporum oxidized nitroalkanes to the aldehyde with production of H2O2 (Kido et al. 1978a; Gadda et al. 1997), and belongs to the acyl-coenzyme A dehydrogenase superfamily (Daubner et al. 2002). It is also worth drawing attention to the plant metabolites miserotoxin that is a glycoside of nitropropanol, and karakin that is a glucose ester of 3-nitropropionate (Anderson et al. 2005). These exert their toxicity by hydrolysis to nitropropionic acid that is a suicide inactivator of succinate dehydrogenase (Alston et al. 1977). Exceptionally, the aglycones can be used as electron acceptors by Denitrobacterium detoxiicans during growing with lactate that is converted into acetate (Anderson et al. 2000). The enantiomeric reduction of 2-nitro-1-phenylprop-1-ene has been studied in a range of Gram-positive organisms including strains of Rhodococcus rhodochrous (Sakai et al. 1985). The enantiomeric purity of the product depended on the strain used, the length of cultivation, and the maintenance of a low pH that is consistent with the later results of Meah and Massey (2000). It has been shown that an NADPH-linked reduction of α,β-unsaturated nitro compounds may also be accomplished by old yellow enzyme via the aci-nitro form (Meah and Massey 2000). This is formally analogous to the reduction and dismutation of cyclic enones by the same enzyme (Vaz et al. 1995), and the reductive ission of nitrate esters by an enzyme homologous to the old yellow enzyme from Saccharomyces cerevisiae (Snape et al. 1997). The transformation of N-nitrosodimethylamine by Pseudomonas mendocina KR1 that has toluene-4-monoxygenase activity was initiated by monooxygenation to the N-nitro compound, which produced N-nitromethylamine and formaldehyde, presumably by hydroxylation of the methyl group (Fournier et al. 2006).

REFERENCES Alston TA, L Mela, HJ Bright (1977) 3-Nitropropionate, the toxic substance of Indigofera, is a suicide inactivator of succinate dehydrogenase. Proc Natl Acad USA 74: 3767–3771.

Miscellaneous Compounds

587

Anderson RC, MA Rasmussen, NS Jensen, MJ Allison (2000) Denitrobacterium detoxiicans gen. nov., sp. nov., a ruminal bacterium that respires on nitrocompounds. Int J Syst Evol Microbiol 50: 633–638. Anderson RC, W Majak, MA Rasmussen, TR Callaway, RC Beier, DJ Nisbet, MJ Allison (2005) Toxicity and metabolism of the conjugates of 3-nitropropanol and 3-nitropropionioc acid in forage poisonous to livestock. J Agric Food Chem 53: 2344–2350. Bhushan B, A Halasz, J Spain, J Hawari (2004) Initial reaction(s) in biotransformation of CL-20 is catalyzed by salicylate 1-monooxygenase from Pseudomonas sp. strain ATCC 29352. Appl Environ Microbiol 70: 4040–4047. Bhushan B, L Paquet, JC Spain, J Hawari (2003) Biotransformation of 2,4,6,8,10,12-hexanitro-2,4,6,8,10,12hexaazaisowurtzitane (CL-20) by denitrifying Pseudomonas sp. strain FA1. Appl Environ Microbiol 69: 5216–5221. Binks PR, S Nicklin, NC Bruce (1995) Degradation of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) by Stenotrophomonas maltophilia PB1. Appl Environ Microbiol 61: 1318–1322. Daubner SC, G Gadda, Mp Valley, PF Fitzpatrick (2002) Cloning of nitroalkane oxidase from Fusarium oxysporum identiies a new member of the acyl-CoA dehydrogenase superfamily. Proc Natl Acad Sci USA 99: 2702–2707. Fournier D, A Halasz, J Spain, P Fiurasek, J Hawari (2002) Determination of key intermediates during biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine with Rhodococcus sp. strain DN 22. Appl Environ Microbiol 68: 166–172. Fournier D, A Halasz, S Thiboutot, G Ampleman, D Manno, J Hawari (2004) Biodegradation of octahydro1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) by Phanerochaete chrysosporium: new insight into the degradation pathway. Environ Sci Technol 38: 4130–4133. Fournier D, J Hawari, SH Streger, K McClay, PB Hatzinger (2006) Biotransformation of N-nitrosodimethylamine by Pseudomonas mendocina KR1. Appl Environ Microbiol 72: 6693–6698. Fournier D, S Trott, J Hawari, J Spain (2005) Metabolism of the aliphatic nitramine 4-nitro-2,4-diazabutranal by Methylobacterium sp. strain JS 178. Appl Environ Microbiol 71: 4199–4202. Francis K, B Russell, G Gadda (2005) Involvement of a lavosemiquinone in the enzymatic oxidation of nitroalkenes catalyzed by 2-nitropropane dioxygenase. J Biol Chem 280: 5195–5204. Gadda G, RD Edmonson, DH Russell, PF Fitzpatrick (1997) Identiication of the naturally occurring lavin of nitroalkane oxidase from Fusarium oxysporum as a 5-nitrobutyl-FAD and conversion of the enzyme to the active FAD-containing form. J Biol Chem 272: 5563–5570. Gorlatova N, M Tchorzewski, T Kurihara, K Soda, N Esaki (1998) Puriication, characterization, and mechanism of a lavin mononucleotide-dependent 2-nitropropane dioxygenase from Neurospora crassa. Appl Environ Microbiol 64: 1029–1033. Kido T, K Hashizume, K Soda (1978a) Puriication and properties of nitroalkane oxidase from Fusarium oxysporium. J Bacteriol 133: 53–58. Kido T, K Sida, K Asada (1978b) Properties of 2-nitropropane dioxygenase of Hansenula mrakii. J BiolChem 253: 226–232. Meah Y, V Massey (2000) Old yellow enzyme: stepwise reduction of nitrooleins and catalysis of acid-nitro tautomerization. Proc Natl Acad Sci USA 97: 10733–10738. Sakai K, A Nakazawa, K Kondo, H Ohta (1985) Microbial hydrogenation of nitrooleins. Agric Biol Chem 49: 2231–2236. Seth-Smith HMB, SJ Rosser, A Basran, ER Travis, ER Dabbs, S Nicklin, NC Bruce (2002) Cloning, sequencing, and characterization of the hexahydro-1,3,5-trinitro-1,3,5-triazine degradation gene cluster from Rhodococcus rhodochrous. Appl Environ Microbiol 68: 4764–4771. Snape JR, NA Walkley, AP Morby, S Nicklin, GF White (1997) Puriication, properties, and sequence of glycerol trinitrate reductase from Agrobacterium radiobacter. J Bacteriol 179: 7796–7802. Thompson KT, FH Crocker, HL Fredrickson (2005) Mineralization of the cyclic nitramine explosive hexahydro-1,3,5-trinitro-1,3,5-triazine by Gordonia and Williamsia spp. Appl Environ Microbiol 71: 8265–8272. Trott S, SF Nishino, J Hawari, JC Spain (2003) Biodegradation of the nitramine explosive CL-20. Appl Environ Microbiol 69: 1871–1874. Vaz ADN, S Chakraborty, V Massey (1995) Old yellow enzyme: aromatization of cyclic enones and the mechanism of a novel dismutation reaction. Biochemistry 34: 4246–4256. Zhao J-S, A Halasz, L Paquet, C Beaulieu, J Hawari (2002) Biodegradation of hexahydro-1,3,5-trinitro-1,3,5triazine and its mononitroso derivative hexahydro-1-nitroso-3,5-dinitro-1,3,5-triazine by Klebsiella pneumoniae strain SCZ-1 isolated from an anaerobic sludge. Appl Environ Microbiol 68: 5336–5341.

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PART 4 ALIPHATIC PHOSPHONATES AND SULFONATES INTRODUCTION Organic phosphonates are both anthropogenic and biogenic. They have been incorporated into household detergents and synthesized as antiviral compounds (acyclic nucleoside phosphonates): they exist in naturally occurring compounds including antibiotics (phosphonomycin [fosfomycin], alaphosphin [alafosfalin], and plumbemycin), in the microbial herbicide bialaphos (phosphinothricin), and in complex cell components. Although alkyl sulfonates have been used as detergents and the aromatic analogs have a number of applications, there are also biogenic alkyl sulfonates including the metabolically important coenzyme M (2-mercaptoethanesulfonate), taurine (2-aminoethanesulfonate) derived from cysteine, and sulfonolipids. It has been shown that sulfonates, which are present in agricultural soil, are important for the survival of Pseudomonas putida in the soil and the rhizosphere (Mirleau et al. 2005). Both phosphonates and sulfonates can be degraded, and the mechanisms of their degradation generally depend on the absence of alternative sources of inorganic phosphorus or sulfur. There are only a few naturally occurring organic compounds containing boron, and these are borate complexes with tetradentate oxygen ligands containing substituted 1,2-dihydroxyethanes. Organic boronates with C–B bonds, particularly aryl boronates are, however, important intermediates in organic synthesis.

PHOSPHONATES Phosphonates can serve as sources of phosphorus, generally in the absence of inorganic phosphate (Cook et al. 1978), although only a single strain may not be able to use all the phosphonates that have been examined (Schowanek and Verstraete 1990). Degradation of phosphonates involves cleavage of the C–P bond with the formation of inorganic phosphate, and may be accomplished by a carbon–phosphorus lyase, although the enzymology and its regulation are extremely complex (Chen et al. 1990). The gene cluster required for the utilization of phosphonates is induced in Escherichia coli by phosphate limitation, and genetic evidence suggests a connection between the metabolism of phosphonates and phosphites. On the basis of this, the interesting suggestion has been made that there may exist a phosphorus redox cycle and that phosphorus is involved not only at the +5 oxidation level, but also at lower oxidation levels (Metcalf and Wanner 1991). Two main pathways are used for the degradation of phosphonates that are initiated by a lyase or a hydrolase (Wanner 1994): 1. C–P lyase has a broad substrate speciicity and, for example, dimethyl phosphonate is degraded to methane, methylphenyl phosphonate to benzene, and the degradation of the widely used herbicide glyphosate may follow alternative pathways both of which involve C–P ission. 2. The phosphonatase (hydrolase) pathway is less widely used, typically for the degradation of 2-aminoethylphosphonate via phosphonoacetaldehyde to acetaldehyde, and the degradation of phosphonoacetate that involves a speciic hydrolase (Kulakova et al. 2001). Different enzymatic activities have, however, been shown in species of Campylobacter in which these are exceptionally expressed in the presence of high concentrations of phosphate (Mendz et al. 2005). In enteric bacteria and pseudomonads, both or only one of the pathways may be expressed (Jiang et al. 1995), and further examples are given in the illustrations. Examples of the various mechanisms available for the metabolism of phosphonates include the following: 1. In Bacillus cereus, 2-aminoethylphosphonate is initially oxidized to 2-phosphonoacetaldehyde (La Nauze and Rosenberg 1968) before cleavage of the C–P bond (La Nauze et al. 1970) (Figure 11.13). The degradation of 2-aminoethylphosphonate by Pseudomonas

589

Miscellaneous Compounds O H2N−CH2−CH2−P

FIGURE 11.13

O OH

OH

CHO−CH2−P

OH

OH

CH3−CHO + Pi

Biodegradation of 2-aminomethylphosphonate. O CH3 CH3

FIGURE 11.14

O

OH

P

P

CH3

OH

OH

+

CH4

Pi

+ CH4

Reductive biodegradation of alkyl phosphonates and phosphites.

O

O (a)

HO2C−CHO +

OH

HO2C−CH2−NH−CH2−P

H2N−CH2−P

OH

OH

OH CH3−NH2 + Pi

O (b)

HO2C−CH2−NH−CH2−P

OH

HO2C−CH2−NH−CH3 + Pi

OH HO2C−CH2−NH2 + CH2O

FIGURE 11.15

Alternative pathways for the biodegradation of glyphosate.

putida strain NG2 is carried out even in the presence of phosphate, and is mediated by pyruvate aminotransferase and phosphonoacetaldehyde hydrolase activities that are induced by 2-aminoethylphosphonate (Ternan and Quinn 1998). In contrast, in Enterobacter aerogenes strain IFO 12010, these activities are induced only under conditions of phosphate limitation. 2. Reductive pathways have been observed in a number of degradations. Klebsiella pneumoniae metabolized methylphenylphosphonate to benzene (Cook et al. 1979). Alkyl phosphonates and phosphites are degraded by a number of bacteria including species of Klyvera and Klebsiella (Wackett et al. 1987a) (Figure 11.14), and by Escherichia coli (Wackett et al. 1987b) using a pathway in which the alkyl groups are reduced to alkanes. 3. In view of its importance as a herbicide, the degradation of glyphosate has been investigated in a number of organisms and two pathways have been elucidated, differing in the stage at which the C–P bond undergoes ission: a. Loss of a C2 fragment—formally glyoxylate—with the formation of aminomethylphosphonate (Pipke and Amrhein 1988), which may be further degraded by cleavage of the C–P bond to methylamine and phosphate (Jacob et al. 1988) (Figure 11.15a). b. Initial cleavage of the C–P bond with the formation of sarcosine, which is then metabolized to glycine (Pipke et al. 1987; Liu et al. 1991) (Figure 11.15b).

SULFONATES Methane sulfonic acid is produced by tropospheric oxidation of methyl sulides, and there are naturally occurring sulfonates including derivatives of taurine and of glucose-6-sulfonate (sulfoquinovose),

590

Environmental Degradation and Transformation of Organic Chemicals

which are widely distributed in the sulfonolipids of algae and some cyanobacteria. Sulfonates can be degraded by a range of mechanisms, both aerobically and anaerobically (Cook et al. 1999): 1. Strains of methylotrophic bacteria degrade methane sulfonate by initial oxidation to formaldehyde and sulite (Kelly et al. 1994; Thompson et al. 1995; Baxter et al. 2002). A formally analogous reaction is used in the biodegradation of sulfosuccinate to oxalacetate (Quick et al. 1994). The aerobic strains capable of degrading methanesulfonate have been assigned to the genera Methylosulfonomonas and Marinosulfonomonas (Holmes et al. 1997). Degradation by Methylosulfonomonas methylovora strain M2 is initiated by monooxygenation (hydroxylation) by a multicomponent enzyme. One component is an electron transfer protein of which the larger subunit contains a Rieske [2Fe–2S] center, and both this and the small subunit show a high degree of homology with those of dioxygenase enzymes (De Marco et al. 1999). The degradation of C2 to C10 unsubstituted alkyl sulfonates also takes place by monooxygenation with the formation of sulite and the corresponding aldehyde (Eichorn et al. 1999). 2. Taurine is degraded aerobically either by a 2-ketoglutarate-dependent dioxygenation to aminoacetaldehyde (Kertesz 1999) (cf. degradation of 2,4-dichlorophenoxyacetate) or by transamination and ission by a lyase that is also used anaerobically with the formation of acetate (Cook et al. 1999). 3. Sulfoacetaldehyde is a central metabolite in the degradation of a number of C2 sulfonates (Cook and Denger 2002), including ethane-1,2-disulfonate by Ralstonia sp. strain EDS1 (Denger and Cook 2001), and taurine by dehydrogenation and transamination (references in Cook and Denger 2002). Degradation of sulfoacetaldehyde is carried out by sulfoacetaldehyde acetyl transferase, also termed sulphoacetaldehyde sulpholyase. The enzyme has been puriied and characterized from cells of Alcaligenes defragrans grown with taurine using nitrate as electron acceptor. Its activity required thiamine pyrophosphate, phosphate, and Mg2+ (Ruff et al. 2003), and the reaction involves the C-2 anion of the thiazolium ring and results in the formation of sulite and acetyl phosphate in a reaction that is formally analogous to the conversion of pyruvate into acetyl-CoA. 4. The aerobic degradation of l-cysteate by Paracoccus pantotrophus is carried out by deamination to 3-sulfolactate from which sulite is lost with the formation of pyruvate (Cook et al. 2006). The activity of the lyase (3-l-sulfolactatesulfolyase) has been shown to involve pyridoxal 5′-phosphate, and the enzyme has been found in a number of organisms using l-cysteate either as a source of carbon or as an electron acceptor (Denger et al. 2006). 5. a. When lactate is supplied as the carbon source, a few aliphatic sulfonates such as 2-hydroxyethylsulfonate, alanine-3-sulfonate, and acetaldehyde-2-sulfonate are able to serve as sulfur sources and electron acceptors during the anaerobic growth of some sulfate-reducing bacteria (Lie et al. 1996). Several sulite-reducing species of Desulitobacterium were able to use 2-hydroxyethanesulfonate as terminal electron acceptor producing acetate and sulide (Lie et al. 1999). It is relevant to note that species of Desulitobacterium are also able to use widely different terminal electron acceptors including chlorinated organic compounds, acrylate, and arsenate. b. Anaerobic degradation of alkylsulfonates has been demonstrated in a strain of Bilophila wadsworthia (Desulfovibrio sp.) strain GRZCYSA by different pathways: i. Fermentation of cysteate with the formation of acetate, NH4+, and equimolar amounts of sulide and sulfate (Laue et al. 1997a). ii. Utilization of aminomethansulfonate and taurine with lactate as electron donor (Laue et al. 1997b). 6. A strain of Rhodopseudomonas palustris, which was isolated by enrichment with taurine, could use this as electron source, and as a source of sulfur and nitrogen during photoautotrophic growth with CO2. Taurine was metabolized to sulfoacetaldehyde and acetyl phosphate by a pathway, which has already been noted (Novak et al. 2004).

Miscellaneous Compounds

591

It has already been noted (Chapter 9, Part 4) that the degradation of aromatic sulfonates when they are used as source of carbon involves dioxygenation, whereas when they serve as a source of sulfur in the absence of sulfate, degradation takes place by monooxygenation to produce the corresponding phenol and sulite (Kertesz 1999).

BORONATES The C–B bond in boronates is issioned by monooxygenases in both alkyl (Latham and Walsh 1986), and in aryl boronates including substituted phenylboronates and naphthylboronates with production of the corresponding phenols (Negrete-Raymond et al. 2003).

REFERENCES Baxter NJ, J Scanlan, P De Marco, AP Wood, JC Murrell (2002) Duplicate copies of genes encoding methanesulfonate monooxygenase in Marinosulfonomonas methylotrophica strain TR3 and detection of methanesulfonate utilizers in the environment. Appl Environ Microbiol 68: 289–296. Chen C-M, Q-Z Zhuang, Z Zhu, BL Wanner, CT Walsh (1990) Molecuar biology of carbon-phosphorus bond cleavage Cloning and sequencing of the phn (psiD) genes involved in alkylphosphonate uptake and C-P lyase activity in Escherichia coli. J Biol Chem 265: 4461–4471. Cook AM, CG Daughton, M Alexander (1978) Phosphonate utilization by bacteria. J Bacteriol 133: 85–90. Cook AM, CG Daughton, M Alexander (1979) Benzene from bacterial cleavage of the carbon-phosphorus bond of phenylphosphonates. Biochem J 184: 453–455. Cook AM, H Laue, F Junker (1999) Microbial desulfonation FEMS Microbiol Rev 22: 399–419. Cook AM, K Denger (2002) Dissimilation of the C2 sulfonates. Arch Microbiol 179: 1–6. Cook AM, K Denger, THM Smits (2006) Dissimilation of C3-sulfonates. Arch Microbiol 185: 83–90. De Marco P, P Moradas-Ferreira, TP Higgins, I McDonald, EM Kenna, JC Murrell (1999) Molecular analysis of a novel methanesulfonic acid monooxygenase from the methylotroph Methylosulfonomonas methylovora. J Bacteriol 181: 2244–2251. Denger K, AM Cook (2001) Ethanedisulfonate is degraded via sulfoacetaldehyde in Ralstonia sp. strain EDS1. Arch Microbiol 176: 89–95. Denger K, THM Smits, AM Cook (2006) l-Cysteate sulpho-lyase, a widespread pyridoxal 5′-phosphatecoupled desulfonative enzyme puriied from Silicibacter pomeroyi DSS-3. Biochem J 394: 657–664. Eichorn E, JR van der Ploeg, T Leisinger (1999) Characterization of a two-component alkanesulfonate monooxygenase from Escherichia coli. J Biol Chem 274: 26639–26646. Holmes AJ, DP Kelly, SC Baker, AS Thompson, P de Marco, EM Kenna, JC Murrell (1997) Methylosulfonomonas methylovora gen. nov., sp. nov., and Marinosulfonomonas methylotropha gen. nov., sp. nov.: novel methylotrophs able to grow on methansulfonic acid. Arch Microbiol 167: 46–53. Jacob GS, JR Garbow, LE Hallas, NM Kimack, GN Kishore, J Schaefer (1988) Metabolism of glyphosate in Pseudomonas sp strain LBr. Appl Environ Microbiol 54: 2953–2958. Jiang W, WW Metcalf, K-S Lee, BL Wanner (1995) Molecular cloning, mapping, and regulation of the pho regulon genes for phosphonate breakdown by the phosphonatase pathway of Salmonella typhimurium LT2. J Bacteriol 177: 6411–6421. Kelly DP, SC Baker, J Trickett, M Davey, JC Murrell (1994) Methanesulphonate utilization by a novel methylotrophic bacterium involves an unusual monooxygenase. Microbiology (UK) 140: 1419–1426. Kertesz MA (1999) Riding the sulfur cycle—metabolism of sulfonates and sulfate esters by Gram-negative bacteria. FEMS Microbiol Rev 24: 135–175. Kulakova AN, LA Kulakov, NY Akulenko, VN Ksenzenko, JTG Hamilton, JP Quinn (2001) Structural and functional analysis of the phosphonoacetate hydrolase (phnA) gene region in Pseudomonas luorescens 23F. J Bacteriol 183: 3268–3275. La Nauze JM, H Rosenberg (1968) The identiication of 2-phosphonoacetaldehyde as an intermediate in the degradation of 2-aminoethylphosphonate by Bacillus cereus. Biochim Biophys Acta 165: 438–447. La Nauze JM, H Rosenberg, DC Shaw (1970) The enzymatic cleavage of the carbon–phosphorus bond: puriication and properties of phosphonatase. Biochim Biophys Acta 212: 332–350. Latham J, AC Walsh (1986) Retention of coniguration in oxidation of a chiral boronic acid by the lavoenzyme cyclohexanone oxygenase. J Chem Soc Chem Commun 527–528. Laue H, K Denger, AM Cook (1997a) Fermentation of cysteate by a sulfate-reducing bacterium. Arch Microbiol 168: 210–214.

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Laue H, K Denger, AM Cook (1997b) Taurine reduction in anaerobic respiration of Bilophila wadsworthia RZATAU. Appl Environ Microbiol 63: 2016–2021. Lie TJ, T Pitta, ER Leadbetter, W Godchaux, JR Leadbetter (1996) Sulfonates: novel electron acceptors in anaerobic respiration. Arch Microbiol 166: 204–210. Lie TJ, W Godchaux, JR Leadbetter (1999) Sulfonates as terminal electron acceptors for growth of sulite-reducing bacteria (Desulitobacterium spp.) and sulfate-reducing bacteria: effects of inhibitors of sulidogenesis. Appl Environ Microbiol 65: 4611–4617. Liu C-M, PA McLean, CC Sookdeo, FC Cannon (1991) Degradation of the herbicide glyphosate by members of the family Rhizobiaceae. Appl Environ Microbiol 57: 1799–1804. Mendz GL, F Megraud, V Korolik (2005) Phosphonate catabolism by Campylobacter spp. Arch Microbiol 183: 113–120. Metcalf WW, BL Wanner (1991) Involvement of the Escherichia coli phn (psiD) gene cluster in assimilation of phosphorus in the form of phosphonates, phosphite, Pi esters, and Pi. J Bacteriol 173: 587–600. Mirleau P, R Wogelius, A Smith, MA Kertesz (2005) Importance of organosulfur utilization for survival of Pseudomonas putida in soil and rhizosphere. Appl Environ Microbiol 71: 6571–6577. Negrete-Raymond AC, B Weder, LP Wackett (2003) Catabolism of arylboronic acids by Arthrobacter nicotinovorans strain PBA. Appl Environ Microbiol 69: 4263–4267. Novak, RT, RF Gritzer, ER Leadbetter, W Godchaux (2004) Phototrophic utilization of taurine by the purple nonsulfur bacteria Rhodopseudomonas palustris and Rhodobacter sphaeroides. Microbiology (UK) 150: 1881–1891. Pipke R, N Amrhein (1988) Degradation of the phosphonate herbicide glyphosate by Arthrobacter atrocyaneus ATCC 13752. Appl Environ Microbiol 54: 1293–1296. Pipke R, N Amrhein, GS Jacob, J Schaefer, GM Kishore (1987) Metabolism of glyphosate in an Arthrobacter sp GLP-1. Eur J Biochem 165: 267–273. Quick A, NJ Russell, SG Hales, GF White (1994) Biodegradation of sulphosuccinate: direct desulphonation of a secondary sulphonate. Microbiology (UK) 140: 2991–2998. Ruff J, K Denger, AM Cook (2003) Sulphoacetaldehyde acetyltransferase yields acetyl phosphate: puriication from Alcaligenes defragrans and gene clusters in taurine degradation. Biochem J 369: 275–285. Schowanek D, W Verstraete (1990) Phosphonate utilization by bacterial cultures and enrichments from environmental samples. Appl Environ Microbiol 56: 895–903. Ternan NG, JP Quinn (1998) Phosphate starvation-independent 2-aminoethylphosphonic acid biodegradation in a newly isolated strain of Pseudomonas putida, NG2. System Appl Microbiol 21: 346–352. Thompson AS, NJP Owens, JC Murrell (1995) isolation and characterization of methansulfonic acid-degrading bacteria from the marine environment. Appl Environ Microbiol 61: 2388–2393. Wackett LP, BL Wanner, CP Venditti, CT Walsh (1987b) Involvement of the phosphate regulon and the psiD locus in carbon-phosphorus lyase activity of Escherichi coli K-12. J Bacteriol 169: 1753–1756. Wackett LP, SL Shames, CP Venditti, CT Walsh (1987a) Bacterial carbon-phosphorus lyase: products, rates and regulation of phosphonic and phosphinic acid metabolism. J Bacteriol 169: 710–717. Wanner BL (1994) Molecular genetics of carbon–phosphorus bond cleavage in bacteria. Biodegradation 5: 175–184.

PART 5 DEGRADATION OF ORGANIC COMPOUNDS OF METALS AND METALLOIDS Although knowledge on the biodegradation of these compounds is sparse, a number of them are important in industrial processes. Formation of methylated derivatives may take place in metals and metalloids belonging to groups 15 and 16 of the periodic table, and a few of group 14. These have been discussed in a critical review (Thayer 2002) and in Chapter 3, Part 4, and they have been noted in the context of the bacterial resistance to metals and metalloids. Since carbon monoxide has been considered as an organic compound (Chapter 7, Part 1), it is consistent to make brief comments on metal carbonyls. There are distinct structural types of organic compounds containing metals and metalloids. The irst contain covalent carbon–metal bonds and are strictly organometallic compounds, for example, the alkylated compounds of Hg, Sn and Pb, and of Li, Mg, and Al (and formerly Hg), which have been extensively used in laboratory organic synthesis, and Al(C2H5)3 that is a component of the

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Ziegler–Natta catalyst for polymerization of alkenes. Considerable attention has been directed to double-bonded Fischer carbenes of Cr and W, the Schrock carbenes of Ta and Ti, and cyclic polyene ligands of Fe, Co, Cr, and U. Carbonyls of transition metals from groups 6 to 10 of the periodic table include both the monomeric compounds such as Cr(CO)6, Fe(CO)5, Ni(CO)4 and those with two metal groups such as Mn2(CO)10 and Co2(CO)8, which is used industrially for hydroformylation. Although their source has not been identiied, it has been shown that volatile compounds from landills contain carbonyls of Mo and W (Feldmann and Cullen 1997). Metals may also be linked through an oxygen or nitrogen atom to form a stable metal complex without a carbon–metal bond. These include metal complexes of ethylenediamine tetraacetate (EDTA), diethylenetriamine pentaacetate (DTPA), or ethylenediamine tetramethylphosphonate (EDTMP). Metalloid compounds include antimonyl gluconate and bismuth salicylate. Organic compounds of metals and metalloids are both anthropogenic and produced naturally as methylated compounds of which methylmercury has received considerable attention in view of its established toxicity. In addition, resistance to toxic metal cations and metalloid oxyanions by methylation is well established and is discussed in Chapter 3, Part 4. Phenylmercury and organic tin compounds have been used as biocides; methylcyclopentadienyl manganese tricarbonyl has been proposed as a fuel additive. Methylarsonate and dimethylarsinate have been used as herbicides and insecticides, and several organic arsenic compounds have been examined as chemotherapeutic agents. These include phenylarsonic acids and arsenobenzene of which the 3,3′-diamino-4,4′-dihydroxy derivative known as Salvarsan occupied an important place in the history of chemotherapy. A range of organoarsenic compounds including arsenolipids and arsenocarbohydrates that are degraded to arsenobetaine is found in marine biota. A number of the less common metals including Gd, Sm, In, Tc, Au, and the platinum metals have achieved importance in clinical medicine, and include the γ-emitters 99mTc, 111In, and 153Sm with short half-lives (6.0 h, 2.8 d, and 1.93 d, respectively). They are generally administered as organic complexes— the DTPA of 111In in brain imaging and of Gd that is used in MRI; the EDTMP of 153Sm; the cis-diammine-(1,1-cyclobutanedicarboxylato)platinum (carboplatin); and the gold complex of (Et3P)=Au–X, where X is 1-β-thiopenta-O-acetylglucose (auranoin) (Thompson and Orvig 2003). Little is known, however, of the ultimate fate of these metal complexes (Kümmerer and Helmers 2000). Although the degradation or transformation of some organometallic compounds has been examined, only a few of the pathways and the enzymology have been unambiguously established. Only a brief account of the important issues is attempted, but coverage of essentially ecological aspects has not been attempted. Redox systems that are involved in bacterial reactions involving inorganic arsenic have been reviewed (Silver and Phung 2005), and reactions in which selenate and arsenate serve as electron acceptors for growth in the absence of oxygen have been discussed in Chapter 3, Part 2.

TIN The aerobic transformation of tributyltin by bacteria takes place by successive loss of butyl groups to monobutyltin and eventually to inorganic tin (Kawai et al. 1998). A comparable degradation takes place with fungi and yeasts, but is complicated by the simultaneous methylation of the products (Errécalde et al. 1995). Triphenyltin chloride is degraded to diphenyltin and benzene (Inoue et al. 2000), apparently mediated by pyoverdine siderophores produced by the luorescent pseudomonad (Inoue et al. 2003). The analogous pyochelin has been implicated in the degradation of triphenyltin chloride by Pseudomonas aeruginosa (Sun et al. 2006), and the role of the ferric complex of pyochelin in generating hydroxyl radicals has been demonstrated using EPR (Sun and Zhong 2006).

LEAD It has been shown using (1-14C-ethyl) tetraethyl lead that this was biodegradable, and that the rate of mineralization was adversely affected by the presence of hydrocarbons that are generally simultaneous contaminants (Mulroy and Ou 1998).

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MERCURY In Hg-resistant bacteria that are resistant to organic forms of Hg such as phenylmercuric acetate and methylmercury chloride, lyases are involved in the ission of the C–Hg to form Hg2+ and benzene or methane, and the enzyme has been partly puriied (Schottel 1978). The Hg2+ may then be reduced to nontoxic Hg0. The situation under anaerobic conditions for sulfate-reducing bacteria is complicated by the possibility of both methylation and demethylation in the same strain (Pak and Bartha 1998), plausibly by operation of the acetyl-CoA pathway (Choi et al. 1994; Ekstrom et al. 2003). Under anaerobic conditions, demethylation, though not methylation, has been reported for a methanogen (Pak and Bartha 1998).

ARSENIC Tamaki and Frankenberger (1992) quote the degradation of methanearsonic acid to arsenate and CO2 by aerobic bacteria, and growth at the expense of organoarsenic compounds has been reported. Growth with 2-aminoethylarsonic acid has been demonstrated and the products identiied as alanine and arsonoacetaldehyde, the latter decomposing spontaneously by hydrolysis (Lacoste et al. 1992). Growth on arsenoacetate has also been reported without, however, identifying the enzyme responsible for scission of the C–As bond (Quinn and McMullen 1995), and strains of Campylobacter degraded both phenylphosphonate and phenylarsonate (Mendz et al. 2005). Dimethylselenide is degraded to CH4 and CO2 by a methylotrophic methanogen grown with dimethylsulide (Oremland and Zehr 1986), and serves as a source of selenium for Methanocccus voltae during selenium limitation (Niess and Klein 2004).

REFERENCES Choi S-C, TT Chase, R Bartha (1994) Metabolic pathways leading to mercury methylation in Desulfovibrio desulfuricans LS. Appl Environ Microbiol 60: 4072–4077. Ekstrom EB, FM Morel, JM Benoit (2003) Mercury methylation independent of the acetyl-coenzyme A pathway in sulfate-reducing bacteria. Appl Environ Microbiol 69: 5414–5422. Errécalde O, M Astruc, G Maury, R Pinel (1995) Biotransformation of butyltin compounds using pure strains of microorganisms. Appl Organomet Chem 9: 23–28. Feldmann J, WR Cullen (1997) Occurrence of volatile transition metal compounds in landill has: synthesis of molybdenum and tungsten carbonyls in the environment. Environ Sci Technol 31: 2125–2129. Inoue H, O Takimura, H Fuse, K Murakami, K Kamimura, Y Yamaoka (2000) Degradation of triphenyltin by a luorescent pseudomonad Appl Environ Microbiol 66: 3492–3498. Inoue H, O Takimura, K Kawaguchi, T Nitoda, H Fuse, K Murakami, Y Yamaoka (2003) Tin-carbon cleavage of organotin compounds by pyoverdine from Pseudomonas chlororaphis. Appl Environ Microbiol 69: 878–883. Kawai S, Y Kurokawa, H Harino, M Fukushima (1998) Degradation of tributyltin by a bacterial strain isolated from polluted river water. Environ Pollut 102: 259–263. Kümmerer K, E Helmers (2000) Hospital efluents as a source of gadolinium in the aquatic environment. Environ Sci Technol 34: 573–577. Lacoste A-M, C Dumora, BRS Ali, E Neuzil, HBF Dixon (1992) Utilization of 2-aminoethylarsonic acid in Pseudomonas aeruginosa. J Gen Microbiol 138: 1283–1287. Mendz GL, F Mégraud, V Korolik (2005) Phosphonate catabolism by Campylobacter spp. Arch Microbiol 183: 113–120. Mulroy, PT, L-T Ou (1998) Degradation of tetraethyllead during the degradation of leaded gasoline hydrocarbons in soil. Environ Toxicol Chem 17: 777–782. Niess UM, A Klein (2004) Dimethylselenide demethylation is an adaptaive response to selenium deprivation in the archaeon Methanococcus voltae. J Bacteriol 186: 3640–3648. Oremland RS, JP Zehr (1986) Formation of methane and carbon dioxide from dimethylselenide in anoxic sediments and by a methanogenic bacterium. Appl Environ Microbiol 52: 1031–1036. Pak K-R, R Bartha (1998) Mercury methylation and demethylation in anoxic lake sediments by strictly anaerobic bacteria. Appl Environ Microbiol 64: 1013–1017.

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Quinn JP, G McMullan (1995) Carbon–arsenic bond cleavage by a newly isolated Gram-negative bacterium strain ASV2. Microbiology (UK) 141: 721–727. Schottel JL (1978) The mercuric and organomercurial detoxifying enzymes from a plasmid-bearing strain of Escherichia coli. J Biol Chem 253: 4341–4349. Silver S, LT Phung (2005) Genes and enzymes in bacterial oxidation and reduction of inorganic arsenic. Appl Environ Microbiol 71: 599–608. Sun G-X, J-J Zhong (2006) Mechanism of augmentation of organotin decomposition by ferripyochelin: formation of hydroxyl radical and organotin-iron ternary complex. Appl Environ Microbiol 72: 7264–7269. Sun G-X, W-Q Zhou, J-J Zhong (2006) Organotin decomposition by pyochelin secreted by Pseudomonas aeruginosa even in an iron-suficient environment. Appl Environ Microbiol 72: 6411–6413. Tamaki S, WT Frankenberger (1992) Environmental biochemistry of arsenic. Rev Environ Contam Toxicol 124: 79–110. Thayer JS (2002) Biological methylation of less-studied elements. Appl Organometal Chem 16: 677–691. Thompson KH, C Orvig (2003) Boon and bane of metal ions in medicine. Science 300: 936–939.

Section IV Bioremediation

12 Bioremediation: Overview INTRODUCTION Few of the compounds that are the object of bioremediation programs are readily degraded, and although many have been shown to be degradable in controlled laboratory experiments, the cardinal question is whether they are degraded in the speciic environment. Biodegradation implies a signiicant degree of mineralization, and not merely biotransformation (Chapter 2). The general aspects of bioremediation have been discussed by Thomas and Ward (1989), Morgan and Watkinson (1989a,b), Edgehill (1992), and Alexander (1995a). Discussion of the pathways followed during the biodegradation and biotransformation of a wide range of xenobiotics by both bacteria and fungi has already been given in Chapters 7 through 11. This attempts to provide a general background to details, which are discussed in Chapters 13 and 14.

STRATEGIES Three rather different strategies for bioremediation have been employed: these involve treatment in situ, on-site, or off-site, and each has both advantages and disadvantages. The last two offer a more controlled approach that may be based on scale-up of procedures developed in simulation experiments in microcosms. All of them, however, necessitate a full appreciation of the underlying microbiological issues. It should be emphasized that all procedures will of necessity be site-speciic since they must take into account both the physical environment and basic microbiological issues. An illustrative example of a problem that may arise in pump-and-treat systems for treating contaminated aquifers is the reduced permeability at the delivery site, which was due to deposition of colloidal material that was mobilized during the treatment (Wiesner et al. 1996). This was apparently enhanced by gas formation from the hydrogen peroxide used to increase the oxygen concentration in the aquifer. Strategies will also be contaminant-speciic, and take into account both the pathways and the regulation mechanisms for degradation of the generally complex range of contaminants. For a given substrate, the induction an d maintenance of the degradative enzymes will depend on the environmental conditions (Guerin and Boyd 1992). The presence or addition of readily degradable substrates may enhance the bacterial population, though not necessarily those required for the degradation of recalcitrant compounds. For example, addition of toluene to an aquifer to facilitate the degradation of trichloroethene by indigenous bacteria could result in the dominance of populations that degrade trichloroethene only poorly. In general, the principles that have emerged from the study of aquatic systems, which have been outlined in previous chapters, can be adapted to the terrestrial environment merely with change of emphasis. For example, the cardinal role of association of xenobiotics with organic components of the soil (Bollag and Loll 1983), the concentration of water (water potential), and the potential role of fungi must be taken into consideration. Two main strategies have been used for bioremediation or bioattenuation (although this may fail to take into account stable metabolites): (a) stimulation of the activity of endogenous organisms by the addition of a substrate (bioaugmentation) or (b) inoculation with the active organisms—often isolated from the same site. This chapter attempts to provide an overview of the application of principles, outlined in previous chapters, to the bioremediation of contaminated terrestrial sites and the associated groundwater. Cardinal microbiological processes will be addressed only briely, and references should be made to previous chapters for metabolic details. There are several reasons for the heightened concern over the increasing volume of solid waste—both industrial and domestic. On the positive side, however, 599

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although the volume of domestic waste is huge, households will diminish its heterogeneity with the adoption of at-source separation and recycling: 1. Some sites occupy valuable land in urban areas, and it is therefore imperative that its reuse for commercial or domestic building be ensured against current or future health hazards. 2. Although the use of landills is being phased out, they have been extensively used in the past. a. For several reasons, there is widespread environmental concern over the adverse longterm effects of landills, which have been used for on-site disposal of industrial waste or sludge after biological treatment. Leachate may be discharged into watercourses, while transformation of the original components in the landill into others may have taken place, which are equally or even more undesirable. b. The sludge from municipal water treatment facilities may have been sent to landills, which may therefore contain both nondegraded—and presumably more recalcitrant—substrates including terminal metabolites, which may have been produced after deposition.

CONTAMINANTS The range of compounds in nondomestic landills is extremely wide, and includes not only industrial waste from the manufacture of chemicals but also in some circumstances substantial volumes of military waste containing explosives and chemical warfare agents. It should also be appreciated that continuous atmospheric precipitation will have occurred, and therefore virtually any established atmospheric contaminant may also be present. Indeed, the atmospheric input into Lake Michigan has been found to exceed that from landills (Hornbuckle et al. 1995); so important interphase partitions should be taken into account. The range of relevant compounds to which attention should be directed is dependent on the availability and sophistication of analytical procedures both for the original compounds and for their transformation products. An illustrative example is provided by the development of chromatographic procedures that have been applied to carbon black and coal tar, which have revealed the presence of polycyclic aromatic hydrocarbons (PAHs) with up to nine rings (Bemgård et al. 1993). Because many of the compounds discussed here are toxic, there is increasing demand for the remediation of contaminated sites and removal of the offending compounds. In this overview, the concept will be enlarged to include remediation of riverine sediments in the vicinity of industrial production and contamination of groundwater by low-molecular-mass compounds that have penetrated the overlying cover. Emphasis is placed on microbiological aspects, whereas engineering considerations that are of cardinal importance lie beyond the expertise of the authors. An attempt is made in Chapter 14 to bring together and summarize (1) a range of sites that have attracted attention; (2) the contaminants involved; (3) the results of laboratory-model and full-scale experiments; (4) the relevant microbiological aspects including the organisms, the pathways of biodegradation and biotransformation; and (5) determinants of biodegradability, particularly bioavailability and oxygen concentration. A review by Bollag (1992) addresses the important issue of fungus-mediated polymerization reactions of phenols and anilines, which are relevant to their bioavailability and therefore their biodegradability. Biological treatment of wastewater and industrial exhaust gases is excluded. In addition, there is an increasing interest in recovery rather than destruction of valuable components in these discharges. Although this chapter is self-contained, reference should be made to sections of preceding chapters for additional details. Undue prominence may have been given to PAHs and related compounds. There are a number of reasons for this that illustrate clearly the interaction of different—yet collectively important—issues.

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1. History. Interest in sites containing PAHs that antedate the introduction of modern synthetic chemicals. Gas works and the production of tar residues are common in countries that used coal as a source of coal gas for lighting and heating. Many of these sites have now been abandoned since the industry has been replaced by the dominance of electricity and oil. 2. Urban planning. For convenience in the distribution of coal gas, the production sites were often placed close to areas of urban populations. As cities expand, these sites are of increasing interest for new building, and the existence of gasworks residues presents a potentially serious problem. 3. Recalcitrance. It has been demonstrated that although some of the low-molecular-mass PAHs such as naphthalene and phenanthrene (and their alkylated homologs) are biodegradable, those with more than four rings generally present an increasing degree of recalcitrance. 4. Health hazard. It was established in the 1920s and 1930s that many components of coal tar were carcinogenic and that this was due to the presence of PAHs containing four to six aromatic rings. Their existence therefore presents a potential threat to residents, and to ofice and factory users. Previous chapters have been directed primarily to the aquatic environment. The principles may, with appropriate modiication, be extended to terrestrial systems. In practice, there is no distinct boundary between terrestrial and aquatic systems. Both are inluenced by the level of the water table and the possibility of leaching from the soil phase. Substantial effort has been directed to a wide range of agrochemicals, and a few of these have already been used as illustration in earlier chapters. Some important general conclusions from these studies have a direct bearing on the subject of this chapter: 1. After successive applications of an agrochemical, a population that has enhanced capability for their degradation may develop. This is negative for the functioning of the chemicals, but would be positive from the view of bioremediation (Racke and Coats 1990). 2. Many organic compounds partition into the organic matrix of soils and sediments as a result of both chemical and microbial reactions, which have been discussed in Chapter 4, and these associated residues may be both less toxic and less amenable to biodegradation than the free compounds. This presents an adverse prognosis for bioremediation. 3. The composition of the original contaminants in sediments may have been altered during deposition on land sites, either by biotic or abiotic transformation. Loss may also have occurred through volatilization of the more volatile components, for example, alkylnaphthalenes in PAHs, or partially dechlorinated PCBs (polychlorinated biphenyls) that have been subjected to drying (Bushart et al. 1998). In addition, bioavailability may be altered by cycles of wetting and drying (White et al. 1998), so that the bioremediation of dredged material may be adversely affected. 4. Mere alteration of the structure of the contaminant by biotransformation may not necessarily be acceptable. For example, although anaerobic dechlorination of PCBs is desirable, microbial reduction of 3,3′-dichlorobenzidine, which is an intermediate in the manufacture of dyes, produced benzidine that is both more toxic and more susceptible to dissemination in the aquatic phase (Nyman et al. 1997). Procedures for the improvement of microorganisms for their applicability to treatment programs have been presented by Timmis et al. (1994); but in this overview, only a parenthetical note is made of procedures for the genetic manipulation to improve the effectiveness of bacteria. The account is devoted to organisms indigenous at contaminated sites, or to inoculation with naturally occurring organisms of established metabolic relevance. In many situations, the waste will have lain for

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considerable lengths of time with the result that a natural lora of degradative microorganisms will have developed through enrichment under natural conditions. This is well established for agrochemicals (Racke and Coats 1990), and it is, therefore, highly desirable to optimize the activity of such organisms in bioremediation programs. There is an enormous literature in this area and only a small fraction of this is cited. Only primary publications have been cited although, as far as possible, references to review articles have been given where extensive literature citations may be found. Attention is drawn to overviews that offer valuable and stimulating general perspectives (Errampalli et al. 1997; Strauss 1997).

SITES A number of contaminated sites have been used for illustration, though the extent to which bioremediation has received practical application is variable. For a number of reasons, emphasis is placed on basic microbiological issues that have emerged from controlled laboratory experiments: a. These illustrate many cardinal issues that should be taken into consideration in scale-up to ield exploitation. b. They reveal fundamental issues such as the reasons for using biphenyl to facilitate degradation of PCBs, or of phenol or toluene to induce enzymes for the degradation of trichloroethene. c. Mixtures of a number of compounds are often involved, and among groups such as PAHs, PCBs, and polybrominated diphenyl ethers (PBDEs), there are wide variations in the biodegradability of individual components.

CHEMICAL PROCEDURES For the sake of completeness, attention is drawn to physical procedures for removal of contaminants and for their chemical destruction. A valuable review by Hamby (1996) summarizes chemical and physical treatments of soils and contaminated ground and surface waters. Examples include the following: • Supercritical carbon dioxide extraction of hydrocarbon contaminants (Schleussinger et al. 1996) • Extraction by vapor stripping (Siegrist et al. 1995) • Thermal blanket in situ removal and destruction of PCBs (Iben et al. 1996) • The application of sorbents (Verstraete and Devlieger 1996) • An electrokinetic process combined with in situ chemical degradation (Ho et al. 1999) • The use of subcritical water at 275°C (Lagadec et al. 2000) The application of enzymes has been discussed by Bollag (1992), and is not covered here.

PHYTOREMEDIATION There has been considerable interest in the use of plants for bioremediation and this merits a rather extensive discussion. Plants can play an important role in bioremediation for several reasons: (1) they can transport contaminants from the soil, (2) they can metabolize the contaminants after uptake, or (3) they can produce exudes that support microbial activity for degradation of the contaminants. In addition, bacteria can produce metabolites that counter the effect of toxins produced by fungi, and serve as biocontrol agents that diminish the need for the application of agrochemicals. Plant exudates play an important role in supporting the growth and activity of bacteria that carry out the degradation of contaminants in the rhizosphere and rhizoplane (the external surface of roots

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including adhering particles of soil). Bacteria are also of increasing importance as biocontrol agents against plant pathogens in the roots of plants. The use of higher plants in bioremediation has been discussed (Schnoor et al. 1995; McIntyre and Lewis 1997; Salt et al. 1998). There are, however, important limitations to the use of plants, which must be considered. These include a. The extent and rate at which the contaminants are accumulated, taking into account the loss of volatile components b. The means for disposal of the contaminated plants, for example, by incineration with its accompanying problems c. Metabolism of the contaminants including not only transformation but also the cardinal issue of the extent of degradation In summary, the secondary role of plants in supporting degradative bacteria will probably be the most important factor. Although this account does not attempt to cover municipal or industrial waste-treatment systems, a brief note is included on the use of wetland, in which plants can play a signiicant role. Wetlands are generally constructed from low-through or static ponds into which aquatic plants have been introduced. They have mostly been examined for the treatment of wastewater from small communities and their success has often been quantiied using traditional parameters. There has, however, been interest in using these for the elimination of contaminants including nonpoint sources of agrochemicals. Aquatic plants have included species of Phragmites and Typha, and the range of contaminants included alkylbenzenesulfonates (Huang et al. 2004), pharmaceuticals such as iboprofen, carbamazapine, and cloibric acid (Matamoros et al. 2005), and the insecticide azinphos-methyl (Schulz et al. 2003). The results should be evaluated carefully since a range of factors can contribute to lowering the concentrations of contaminants including sorption to plants and sediment, photolysis, temperature, and water depth in determining the role of aerobic or anaerobic microbial reactions. The accumulation of p,p′-DDT and trans-nonachlor in ish that were present in a wetland, and the potential for accumulation of other chlorinated contaminants illustrated the adverse potential for further dissemination of the contaminants (Barber et al. 2006). Primary Role of Plants In addition to their direct role in the bioremediation of contaminants, plants can play an important role in their dissemination through consumption by ruminants. The detoxiication and metabolism of higher plants has been reviewed by Sandermann (1994), and some illustrative examples include the following: 1. Hybrid poplars (Populus deltoides x nigra) have attracted considerable interest since they are able to transport and metabolize—even though they do not generally degrade—diverse xenobiotics: a. Trichloroethene was metabolized to trichloroethanol and trichloroacetate (Newman et al. 1997, 1999). b. Atrazine was metabolized by reactions involving dealkylation and hydrolytic dechlorination to yield 2-hydroxy-4,6-diamino-1,3,5-triazine (Burken and Schnoor 1997). c. Tissue cultures of poplar metabolized the explosive hexahydro-1,3,5-trinitro-1,3, 5-triazine (RDX) by partial reduction to the 1-nitroso- and 1,3-dintroso derivatives, and in the presence of light these were further metabolized to CH2O, CH3OH, and CO2 (Van Aken et al. 2004). d. The fate of [U-14C]TNT was examined both in soil and hydroponic systems (Thompson et al. 1998). Most of substrate that was taken up was not extractable, and the main

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reaction was association with the roots, while uptake in aged soil was signiicantly lower than in spiked soils. Partial reduction to 2-amino-4,6-dinitrotoluene, 4-amino-2, 6-dinitrotoluene, and 2,4-diamino-6-nitrotoluene took place as a minor reaction. e. In a long-term study at a site contaminated with creosote, there was a reduction in the area of the plume that coincided with root development into the water table. Although loss of naphthalene, acenaphthylene, and acenaphthene were observed, levels of PAHs with four or more rings persisted. It was concluded that water solubility was the limiting factor (Widdowson et al. 2005). 2. The metabolism of xenobiotics by other plants including aquatic plants has been examined: a. Pentachlorophenol is metabolized by the aquatic plant Eichhornia crassipes to a number of metabolites including di-, tri-, and tetrachlorocatechol; 2,3,5-tri- and tetrachlorohydroquinone; pentachloroanisole; and tetrachloroveratrole (Roy and Hänninen 1994). The phenolic products can be compared with those produced during the photochemical and initial stages in the microbiological metabolism of pentachlorophenol, followed by O-methylation. b. Quite complex transformations can be mediated, and the metabolism of phoxim by plant organs and cell suspension of soybean (Glycine max) are given as examples (Höhl and Barz 1995). c. The uptake and biotransformation of benzene from soil and from the atmosphere have been studied in a number of plants. For example, it was shown that in leaves of spinach (Spinacia oleracea), the label from 14C-benzene was found in muconic, fumaric, succinic, malic, and oxalic acids as well as in speciic amino acids. In addition, an enzyme preparation in the presence of NADH or NADPH produced phenol (Ugrekhelidze et al. 1997). d. 2,4,6-Trinitrotoluene was reduced by the aquatic plant Myriophyllum spicatum to aminodinitrotoluenes (Pavlostathis et al. 1998), and in axenic root cultures of Catharanthus roseus the initial metabolites 2-amino-4,6-dinitrotoluene and 4-amino-2,6-dinitro toluene were conjugated—probably with C6 units (Bhadra et al. 1999). There are therefore several important unresolved issues before the phytoremediation of TNT can be exploited. These include accumulation in plant tissues (Hughes et al. 1997) and the phytotoxicity of amino metabolites if they are excreted. e. Reed canary grass (Phalaris arundinacea) was grown in liquid culture and exposed to RDX that was metabolized to the potentially toxic 4-nitro-2,4-diazabutanal (Just and Schnoor 2004). This metabolite is also produced from RDX by strains of Rhodococcus sp., and from the homologous octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) by Phanerochaete chrysosporium. 3. Plant cultures have been examined for their ability to transform contaminants. Generally, only limited changes take place, such as hydroxylation and the formation of conjugates with phenolic groups: a. The transformation of pentachlorophenol by cultures of wheat (Triticum aestivum) produced tetrachlorocatechol as its glucuronide (Schäfer and Sandermann 1988). b. Cultures of wheat (Triticum aestivum), tomato (Lycopersicon asculentum), lettuce (Lactuca sativa), and a rose variety carried out rather limited transformations of luoranthene with plant-speciic formation of 1-, 3-, and 8-hydroxy compounds that were conjugated (Kolb and Harms 2000). c. Transformation of PCBs was examined in plant cultures (Wilken et al. 1995). The rates of transformation were generally greater for congeners with lower degrees of substitution, although neither pentachlorobiphenyl (PCB 101) nor hexachlorobiphenyl (PCB 153) was metabolized. The cultures of soybean (Glycine max), white clover (Trifolium repens), and some of the grasses were most effective. A range of conjugated hydroxylated

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products was formed from 2-chlorobiphenyl including 3-chloro-2-hydroxybiphenyl, which involved an NIH shift, while 2,5,2′,5′-tetrachlorobiphenyl (PCB 52) produced four monohydroxylated metabolites (Wilken et al. 1995). d. The transformation of 4-n-nonyl[U-14C]phenol was examined in a range of plant cultures. Metabolism took place in the alkyl side chain with the formation of monoand dihydroxylated products, with a substantial fraction of the label occurring in bound residues including starch, protein, lignin, and hemicellulose (Bokern and Harms 1997). 4. The role of plants has emerged from studies with soil slurries at a site with a cover of Paspalum notatum, Lespedeza cuneata, Solidago sp., and Pinus taeda in which increased degradation of trichloroethene to CO2 took place (Walton and Anderson 1990). In addition, prairie grasses can stimulate the effective remediation of PAH-contaminated soil (Aprill and Sims 1990). 5. Endophytic bacteria can colonize plant tissues without bringing about adverse effects on the plant, in contrast to epiphytes that remain in the external environment. Bacteria with the established potential for degradation have been used to improve the tolerance and degradation of contaminants: a. Cuttings of hybrid poplar (Populus trichocarpa x deltoides) were inoculated with a strain of Burkholderia cepacia VM 1468 carrying genes for the constitutive expression of toluene degradation. Compared with the uninoculated control, plant growth increased both in the absence and in the presence of toluene. Although the introduced strains did not establish themselves in the endophytic bacterial community, gene transfer to other bacteria with the Tol+ phenotype took place in the roots and stems (Taghavi et al. 2005). b. The plasmid pTOM of Burkholderia cepacia G4 was introduced into B. cepacia strain L.S.2.4, which is a natural endophyte of yellow lupin (Lupinus luteus), and the resulting strain VM 1330 was used to inoculate plants of yellow lupin. These plants were tolerant of toluene up to a concentration of 1 g/L in hydroponic cultivation and up to 500 mg/L in nonsterile soil (Barac et al. 2004). Secondary Role of Plants As introduction, general comments address the role of low-molecular-mass products exuded by plants and their role in biodegradation. Bacteria growing at the expense of these compounds can be advantageous both to the plants in their neighborhood (rhizosphere and rhizoplane) and for their possible role in the biodegradation of contaminants in the rhizosphere and neighboring areas. Organic compounds that are exuded from plant roots mediate the colonization of the rhizosphere of many crop plants by luorescent pseudomonads. Although the structures of these compounds have not always been identiied, it has been demonstrated that higher plants excrete a range of phenolic compounds (Fletcher and Hegde 1995; Hegde and Fletcher 1996). These metabolites include naringin, catechin, and myricitin (Donnelly et al. 1994), and although carbohydrates may predominate, malate and succinate are of primary importance. In contrast, amino acids are generally of lesser signiicance except for chemotaxis that is a requisite for virulence of the wild pathogen Ralstonia solanacearum (Yao and Allen 2006). It has been shown that organic sulfur compounds—putatively sulfonates and sulfate esters—are important for the survival of bacteria in the rhizosphere (Mirleau et al. 2005). In addition, mesophilic archaea belonging to the Crenarchaeota have been characterized in extracts of tomato plants by a combination of enrichment and molecular methods (Simon et al. 2005). There may also be an indirect effect of plants. For example, mineralization of PAHs was examined in microcosms prepared with freshwater sediments and planted with the reed Phragmites australis (Jouanneau et al. 2005). Inoculation with the pyrene-degrading Mycobacterium sp. strain 6PY1 resulted in a greater degree of mineralization than in the absence of plants, and this was

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accompanied by the release of phenanthrene-4,5-dicarboxylic acid, which is an established metabolite from the degradation of pyrene. The positive effect of the plants could be attributed to the increased access of oxygen to the sediment and therefore direct stimulation of bacterial growth. Degradative Enzymes 1. The degradation of 2-chlorobenzoate was supported—presumptively involving enzymatic reaction—by exudates from Dahurian wild rye (Elymus dauricus) (Siciliano et al. 1998). It was also shown that concentrations of 2-chlorobenzoate that had aged in soil for 2 years could be reduced by the indigenous microlora (Siciliano and Germida 1999). Experiments have been carried out on the growth of Dahurian wild rye in the presence of bacterial inoculants that did not adversely affect the mineralization of atrazine under various conditions (Burken and Schnoor 1996). But in the absence of plants of poplar hybrids (Populus deltoides nigra DN34), root exudate resulted in only a slight stimulation of the mineralization of 14 C-labeled atrazine; addition of crushed roots provided a more substantial positive effect. 2. The extradiol catechol ission enzyme from Terrabacter sp. strain DBf63 was introduced into Arabidopsis thaliana using Agrobacterium tumefaciens-mediated transformation, and the haloalkane dehalogenase from Rhodococcus sp. strain m15-3 into Nicotiana tabacum. Seedlings were introduced into hydroponic media and incubated either in darkness or under illumination. It was shown that enzymatic activities from plants expressing the apoplasm-targeted enzymes exceeded those for the cytoplasm-targeted enzymes. This is consistent with transport between the apoplast and the roots, and it was suggested on the basis of these rather preliminary experiments that this methodology could be effective for degrading contaminants in the aquatic environment (Uchida et al. 2005). 3. Mammalian cytochrome P450 2E1 was introduced into tobacco plants that were exposed to trichloroethene in hydroponic medium for 5 d. Trichloroethene epoxide was produced initially, and was rearranged to trichloroacetaldehyde, which was then reduced to trichloroethanol. This was found in samples of leaves, stems, and roots, but was absent in the control plants. Trichloroethanol was subsequently transported to the leaves where it was apparently metabolized (Doty et al. 2000). 4. Pseudomonas luorescens strain F113 is an important biocontrol strain for sugar beet, and a transposon that contained the genes from Burkholderia sp. strain LB400 for the degradation of biphenyl was inserted into the chromosome (Brazil et al. 1995). The resulting hybrid F113pcb was stable under nonselective conditions, and presented a possible candidate for bioremediation, although the level of expression of the bph genes was low. Improvement was accomplished by cloning the bhp operon under control of the nod system in Sinorhizobium meliloti to produce P. luorescens strain F113L::1180, which grew faster with biphenyl and was able to transform effectively a range of PCB congeners as great as, or greater than, the original Burkholderia sp. strain LB400 (Villacieros et al. 2005). 5. It is well established that one of the pathways for the aerobic degradation of trichloroethene is monooxygenation by the toluene ortho monooxygenase (Nelson et al. 1987). Transposon integration was used to insert the gene from Burkholderia cepacia strain G4 into the chromosome of Pseudomonas luorescens strain 2-79. The strain was added to the germinated wheat seedling before planting in soil microcosms (Yee et al. 1998). The average degradation using this strain was 63%, and root colonization was comparable to that of the parent strain lacking the monooxygenase genes. 6. Ralstonia eutropha (Alcaligenes eutrophus) strain NH9 is able to degrade 3-chlorobenzene by the “modiied ortho” pathway. The cbnA gene that encodes 3-chlorocatechol-1, 2-dioxygenase was introduced into rice plants (Oryza sativa ssp. japonica) under the control of a virus 35S promoter. 3-Chlorocatechol induced dioxygenase activity in the callus of the plants, and leaf tissues oxidized 3-chlorocatechol with the production of 2-chloromuconate

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(Shimizu et al. 2002). It was therefore shown that it is possible to produce transgenic plants with the capability of degrading chlorinated aromatic compounds, which are degraded with the formation of 3-chlorocatechol. The Role of Plant Exudates in Degradation The interaction of plants and bacteria in the root system plays an important role in the remediation of contaminants, and may involve the use of plant exudates to stimulate the growth of degradative bacteria as well as the penetration of the soil by plant roots (Kuiper et al. 2004): 1. Metabolites that include naringin, catechin, and myricitin (Donnelly et al. 1994) were able to induce the growth and metabolism of bacteria that degrade a range of PCB congeners (Donnelly et al. 1994). It has also been shown that enzymes for the biodegradation of some PCB congeners could be induced by a number of terpenoids (Gilbert and Crowley 1997), which may originate from higher plants. There is therefore a plausible relation between metabolites excreted by higher plants and utilization of them to support bacterial degradation of xenobiotics in the rhizosphere. In addition, some coumarin, lavone, lavanol, and lavanone plant metabolites were able to support the growth of anaerobic bacteria during dechlorination of chlorocatechols (Allard et al. 1992). 2. It has been shown that the ine roots of mulberry (Morus sp.) die at the end of the growing season, and that this coincides with the accumulation of lavones (morusin, morusinol, and kuwanon) that have C5 substituents at C-3 and C-8. These lavones were able to support the growth of Burkholderia sp. strain LB400, which is effective in the degradation of a range of PCB congeners. It was therefore suggested that the growth of ine roots and the production of phenolic metabolites should be taken into account in evaluating remediation in the rhizosphere (Leigh et al. 2002). 3. Pseudomonas putida strain PCL 1444 is an eficient colonizer of the roots of Lolium multilorum, which produces a highly branched root system, and it was evaluated for its ability to utilize root exudates and the ability to degrade naphthalene (Kuiper et al. 2001). The exudate from seeds, seedlings, and roots contained a range of low-molecular-weight fatty acids including citrate, malate, and succinate and carbohydrates, particularly fructose, glucose, and arabinose, which could support growth of the strain. Although concentrations of propionate were low in the exudate, propionate allowed a high rate of expression of the genes for naphthalene degradation. These results illustrated the importance of root colonization by bacteria that used plant exudates for growth (Kuiper et al. 2002). 4. Bacteria associated with the roots of plants have an important potential for the biodegradation of biogenic methane and carbon monoxide. Examples include methanotrophs associated with aquatic vegetation (King 1994) and the oxidation of CO by bacteria associated with freshwater macrophytes (Rich and King 1998). An important example of considerable environmental signiicance is the generation of methane in rice paddies where the plant roots provide the carbon source for methanogenesis (Lu et al. 2005). Other Functions of Bacteria in the Rhizosphere Considerable effort has been devoted to the application of bacteria as agents for the biocontrol of plant pathogens. This is motivated by the desire to diminish the application of agrochemicals and, in addition, improve soil quality. Bacteria in the rhizosphere are able to fulill a number of quite different functions: direct stimulation of plant growth and the production of secondary metabolites by strains of Pseudomonas, including 2,4-diacetylphloroglucinol, phenazine-1-carboxylate, and pyrrolnitrin, which are toxic to seed- and root-rotting plant pathogenic fungi. Valuable overviews discuss in detail the roles of luorescent pseudomonads (Haas and Défago 2005) and fungi,

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principally species of Trichoderma (Harman et al. 2004), in the control of soil pathogens. Bacteria may have a positive inluence on plants by a number of different mechanisms: 1. Association with nonsymbiotic diazotrophs that can contribute to the nitrogen nutrition of the plants: a. Species of Azospirillum can penetrate the roots of cereal crops, and species of Burkholderia, which are established human and plant pathogens, have now been shown to be able to ix nitrogen. Such strains have been isolated from the rhizosphere, rhizoplane, and the roots of ield crops of maize and sugar in Mexico and Brazil (Perin et al. 2006). b. Stimulating the growth of plants by the production, for example, of auxins by Pseudomonas putida (Patten and Glick 2002) or of quinolinate phosphoribosyl transferase by Burkholderia sp. strain PsJN (Wang et al. 2006). 2. For effective function as biological control agents, there are a number of determinants that must be fulilled: a. Bacteria must be present on the roots of the plants, be able to produce microcolonies, and synthesize inhibitory compounds. Examples include the production against root infection by fungal pathogens of (i) the antimicrobial 2,4-diacetylphloroglucinol by Pseudomonas luorescens CHA0 (Bottiglieri and Keel 2006), (ii) pyoluteorin by Pseudomonas luorescens Pf-5 (Brodhagen et al. 2004), and (iii) phenazine-1-carboxamide by Pseudomonas chlororaphis PCL 1391 (Chin-A-Woeng et al. 2000). The combination of Pseudomonas luorescens CHA0 and P. luorescens Q2-87, each of which produces 2,4-diacetylphloroglucinol, resulted in reciprocal stimulation of the expression of 2,4-diacetylphloroglucinol (Maurhofer et al. 2004). Conversely, Fusarium oxysporum can induce resistance to 2,4-diacetylphloroglucinol by deacylation to the less-toxic 2-acetylphloroglucinol and phloroglucinol (Schouten et al. 2004). b. The production of phenazine-1-carboxamide by Pseudomonas chlororaphis PCL 1391 is a requirement for its function in controlling tomato rot caused by Fusarium oxysporum, and quorum sensing mediated by N-hexanoyl-l-homoserine lactone in the medium (Chin-A-Woeng et al. 2001) regulates its synthesis. Its production in this strain is promoted by a number of conditions including the presence of amino acids, especially phenylalanine and tryptophan (Tjeerd van Rij et al. 2004). This is consistent with the biosynthesis of aromatic amino acids and phenazines in branches of the chorismate pathway, whereas both the N-9 and the N-10 heteroatoms of phenazine originate from glutamine (Mavrodi et al. 1998, 2001). c. Degradation of fungal toxins may contribute to the protection of the plants. For example, fusaric acid produced by Fusarium oxysporum can be degraded by Burkholderia spp. (Utsumi et al. 1991). In addition, fusaric acid produced by the fungus may have other adverse effects: i. In the production of phenazine-1-carboxamide, which is required for the suppression of tomato rot by Pseudomonas chlororaphis PCL1391 (Tjeerd van Rij et al. 2005) ii. In the biosynthesis of 2,4-diacetylphloroglucinol in Pseudomonas luorescens CHA0, which is important for biocontrol in the wheat rhizosphere (Notz et al. 2002) d. It has been shown in Pseudomonas luorescens CHA0, which is an antagonist of the plant pathogenic nematode Meloidogyne incognita, that the extracellular protease encoded by the gene aprA was involved either directly or indirectly (Siddiqui et al. 2005). e. Phase variation regulates the production of lagellae, surface lipoproteins, secondary metabolites, and hydrolytic enzymes including proteases, and is important in the colonization of the rhizosphere by biocontrol agents as a result of increased motility. This has been examined in Pseudomonas luorescens strain F113 during the colonization of alfalfa (Medicago sativa). Colony variation was implicated in its effectiveness

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(Sánchez-Contreras et al. 2002), and is mediated by the site-speciic recombinases Sss and XerD (Martínez-Granero et al. 2005, 2006). An analogous phenomenon occurred in Pseudomonas sp. strain PCL1171 in which mutations in the genes gacA and gacS were shown to be responsible (van den Broek et al. 2005). 3. Several studies have been directed to Pseudomonas putida strain KT2440, which has attracted interest both as a biocontrol agent and for the degradation of contaminants. It was able to maintain high cell densities when it was introduced as a coating of seeds during growth of agricultural crops (Molina et al. 2000). This organism is able to utilize a number of amino acids including proline, lysine, and glutamate for growth, and attention has been directed to their metabolism. The enzymes in the davDt operon for proline degradation are induced by corn-root exudates (Vílchez et al. 2000). There are several pathways for the degradation of lysine (Revelles et al. 2005), and the operon that is involved in its metabolism is induced by δ-aminovalerate, which is one of the early degradation products (Revelles et al. 2004). Particular attention has been directed to 1-aminocyclopropane-1carboxylate (ACC), which is a key intermediate in the biosynthesis of ethene by plants, and to its role in promoting the growth of agricultural plants: a. It has been shown that Pseudomonas putida strain GR12-2 exhibits ACC deaminase activity, and that this organism promoted the root development of canola (Brassica campestris) (Glick et al. 1997). The speciic role of ACC was inferred from the fact that mutants unable to utilize ACC and lacking the deaminase did not exhibit this stimulation (Glick et al. 1994). b. ACC deaminase has been demonstrated in a range of bacteria isolated from the rhizosphere of Pisum sativum and Brassica juncea (Belimov et al. 2001). It has been proposed on the basis of several lines of evidence that the stimulation by ACC deaminase is accomplished in several steps initiated by extrusion of ACC from the plant, which is then removed through bacterial degradation mediated by ACC deaminase. This results in decreased ethene production by the plant and thereby, limitation of growth inhibition. Bacteria in the rhizosphere are therefore able to play an important role in seed and plant development. The Role of Mycorrhizal Fungi Mycorrhizal fungi play an important role in the nutrition and survival of higher plants, and the importance of their associated bacteria has been recognized. In a study of the bacterial communities in the mycorrhizospheres of Pinus sylvestris—Suillus bovinus and P. sylvestris— and Paxillus involutis, the occurrence of both Gram-negative and Gram-positive bacteria was recognized (Timonen et al. 1998). A wide range of taxa were found, including Burkholderia cepacia and Paenibacillus sp., in which strains with established biodegradative capability have been recognized. The relevance of rhizosphere bacteria was illustrated by the demonstration of a bioilm community at the interface of the petroleum-contaminated soil/mycorrhizosphere. Strains of Pseudomonas luorescens biovars were isolated and these were able to grow at the expense of 1,3-dimethyl benzene and 3-methylbenzoate, brought about ission of catechol, and harbored the plasmid-borne genes xylE and xylM (Sarand et al. 1998). Important conclusions can be drawn collectively from the results of these studies: • Microbial degradation in the root system of higher plants can be signiicant. • Higher plants play a cardinal role in the provision of organic carbon and of exudates. • The effectiveness of bacteria depends on the nature of the soil and, in particular, its organic content. As a dividend, bacteria are important as biocontrol agents against a number of plant pathogens.

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MICROBIOLOGICAL ASPECTS Essential aspects of the metabolism of xenobiotics are given in earlier chapters. Therefore, only a cursory discussion is given for classes of compounds that have already been reviewed; for others, a few additional comments have been given. Although a valuable review on microbiological aspects of bioremediation of sites contaminated with organochlorine compounds has been given (Morgan and Watkinson 1989b), it is convenient to provide a short summary of some cardinal issues that are equally signiicant for all xenobiotics. A number of issues that have already been noted in Chapter 4 are discussed here in the context of bioremediation. In natural systems, many different microorganisms will invariably be present, and the degradation of a xenobiotic is frequently dependent upon the activity of several microorganisms. The increased appreciation of the role of populations is considered in Chapter 13.

REGULATION OF PATHWAYS It is very seldom that only a single substrate is present. It is therefore important to examine how the regulation of degradative pathways may be affected and, in particular, whether the simultaneous presence of other contaminants has an adverse effect. In addition, some of the components of a contaminant may directly inhibit degradation by toxiication of the relevant organism. The example of azaarenes in groundwater at a wood preservation site that inhibit PAH degradation (Lantz et al. 1997) is noted in Chapter 14. The regulatory pathways for monocyclic aromatic compounds such as phenol, benzoate, and hydroxybenzoates have been reviewed in detail (Ornston and Yeh 1982). Whereas biodegradation of a substrate is frequently induced by growth with an early metabolite, for example, of biphenyl (Furukawa et al. 1983) and naphthalene (Barnsley 1976) by salicylate, the metabolites in the lower pathway may suppress induction of essential degradative enzymes. For example, although the enzymes for the degradation of toluene in Pseudomonas putida strain pWWO are induced during succinate-limited growth, they are suppressed when succinate is in excess (Austen and Dunn 1980; Duetz et al. 1994). Where plausibly comparable degradation pathways exist, however, for example, in the biodegradation of PAHs, a single organism may display wide versatility. For example, Sphingomonas (Pseudomonas) paucimobilis strain EPA505 is capable of degrading luoranthene, pyrene, benz[a]anthracene, chrysene, benzo[a]pyrene, and benzo[b]luoranthene (Ye et al. 1996). Degradation of all of them involves the sequential operation of a dioxygenase, a dehydrogenase, and ring-ission enzymes. For halogenated substrates, the situation is more complex. Whereas aerobic degradation of PCBs is often carried out by organisms enriched by growth with biphenyl itself (Hernandez et al. 1995), naphthalene is a much less effective inducer (Pellizari et al. 1996). The degradation of toluene and chlorobenzene generally proceeds by respective extradiol (2:3) and intradiol (1:2) ission of the initially formed catechols. However, since 3-chlorocatechol inhibits the activity of the 2,3-dioxygenase, the degradation of toluene and chlorobenzene are generally incompatible except in strains, such as Pseudomonas sp. strain JS150, which have developed a strategy for overcoming this limitation (Haigler et al. 1992). Further discussion of this issue has been given in Chapter 9, Part 1. A strain of Comamonas testosteroni was, however, able to degrade both 4-chlorophenol and 4-methylphenol (Hollender et al. 1994), and Phanerochaete chrysosporium to degrade simultaneously chlorobenzene and toluene (Yadav et al. 1995). Comparable incompatibility due to the synthesis of toxic metabolites may also be displayed in the degradation of chlorobenzoates (Reineke et al. 1982). An additional example is the synthesis of protoanemonin by organisms that degrade 4-chlorobiphenyl by intradiol ission of 4-chloroatechol (Blasco et al. 1995); protoanemonin may then inhibit the growth of other PCB-degrading organisms in terrestrial systems (Blasco et al. 1997).

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ALTERNATIVE ELECTRON ACCEPTORS In the absence of molecular oxygen, a number of alternative electron acceptors may be used; these include nitrate, sulfate, selenate, carbonate, chlorate, Fe(III), Cr(VI), and U(VI), and have already been discussed in Chapter 3, Part 2. In Chapter 14, which deals with applications, attention is directed primarily to the role of nitrate, sulfate, and Fe(III)—with only parenthetical remarks on Cr(VI) and U(VI). The role of nitrate and sulfate as electron acceptors for the degradation of monocyclic aromatic compounds is discussed, and the particularly broad metabolic versatility of sulfate-reducing bacteria is worthy of notice.

AGING This is a cardinal issue (Hatzinger and Alexander 1995), and the term is applied to processes—whose mechanisms are only incompletely established—whereby organic compounds become associated with polymeric components of the soil matrix with the result that these initially monomeric compounds are no longer accessible to the relevant degradative microorganisms. This implies that evaluations of biodegradability that do not take this into account may seriously underestimate the persistence of the compound. A critical issue is the degree of reversibility of these complexes, since slow release by leaching could introduce the xenobiotic into the aqueous phase and thereby contaminate groundwater and present an additional problem. Although this process has been suggested as a mechanism whereby in the short term the adverse effect of contaminants may be diminished, it seems unwise to conclude that this is an acceptable long-term solution to diminishing their environmental impact (Alexander 1995b).

BIOFILMS These are ubiquitous and only a few brief comments are given here in the context of biodegradation. Both in aquatic and terrestrial systems, bacteria may be present in the form of bioilms that are formed from polymers produced by the organisms themselves. These may both increase their penetration of the matrix and localize the organisms, thereby preventing their loss from the system (Wolfaardt et al. 1995). Their role in wastewater trickling ilter treatment systems is, for example, well established, and examples of their possible signiicance in the biorestoration of contaminated groundwater and a contaminated stream are given in Chapter 14.

METABOLITES AND ENZYMES Metabolite-related parameters have also been used directly to establish biodegradation and biotransformation, and include the following examples: 1. The presence of metabolites determined from laboratory experiments of degradation pathways. Examples include (a) cis-dihydrodiols of PAHs in a marine sediment (Li et al. 1996) and naphthalene in leachate from a contaminated site (Wilson and Madsen 1996), (b) chlorobenzoates from the degradation of PCBs (Flanagan and May 1993), and (c) benzylsuccinates from the anaerobic degradation of benzene, toluene, ethylbenzene, and xylenes (BTEX) (Beller et al. 1995; Beller 2002). 2. Some enzymes have a low substrate speciicity, and are able to accept analog substrates with the formation of colored metabolites. This may be used to detect enzymatic activity toward the desired substrates when a large number of colonies have to be examined. Examples include the following: a. For PAHs, toluene 2,3-dioxygenase (Eaton and Chapman 1995) and naphthalene dioxygenase (Ensley et al. 1983) have been used, for which indigo is produced from indole carboxylates.

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b. Toluene-2-monooxygenase for trichloroethene cometabolism by formation of the epoxide (Fries et al. 1998a,b). c. For the degradation of 2,4-dichlorophenoxyacetate, 2,4-dichlorophenoxyacetate/ 2-ketoglutarate dioxygenase, which can accept 4-nitrophenoxyacetate as a substrate with the formation of colored 4-nitrophenol, has been used (Sassenella et al. 1997). Care ought to be exercised, however, since it was also shown that not all strains with established degradative capability for 2,4-dichlorophenoxyacetate were able to form 4-nitrophenol from the surrogate substrate (Sassenella et al. 1997). 3. Examination of a collection of strains of Sphingomonas sp. from a range of localities has suggested that the glutathione S-transferase-encoding gene might be used as a marker for PAH-degrading bacteria (Lloyd-Jones and Lau 1997). In addition, the formation of terminal metabolites may be adverse either for the organism itself, or for other organisms in the ecosystem. Microbial metabolites may also undergo purely chemical reactions to compounds that are terminal products. Examples include the formation of 5-hydroxyquinoline-2-carboxylate from 5-aminonaphthalene-2-sulfonate (Nörtemann et al. 1993) or benzo[b]naphtho[1,2-d]thiophene from benzothiophene (Kropp et al. 1994). Microbial metabolites may be toxic to both the bacteria producing them and to higher organisms. Illustrative examples of toxicity include the following: a. Protoanemonin synthesized during the biodegradation of 4-chlorobiphenyl (Blasco et al. 1997) to PCB-degrading bacteria b. 3,4,3′,4′-Tetrachloroazobenzene produced from 3,4-dichloroaniline (Lee and Kyung 1995) c. The greater carcinogenicity of benzidine produced by anaerobic dechlorination of 3,3′-dichlorobenzidine (Nyman et al. 1997), which is a reduction product of azo dyes and pigments formerly used Metabolites may also play a role in the association of the substrate with humic and fulvic acid components. Two illustrations are given: (a) naphth-1-ol, an established fungal metabolite of naphthalene, may play a role in the association of naphthalene with humic material (Burgos et al. 1996) and (b) it has been shown that 13C-labeled metabolites of [9-13C]-anthracene including 2-hydroxyanthracene-3-carboxylate and phthalate were not extractable from soil with acetone or dichloromethane, and required alkaline hydrolysis for their recovery (Richnow et al. 1998). The identiication of volatile compounds of both Mo and W in gases from a municipal landill (Feldmann and Cullen 1997) illustrated unusual transformation products. Although these compounds were tentatively identiied as Mn2(CO)10 and W(CO)6, neither the mechanism of their formation nor their potential health hazards has been resolved.

UTILIZATION OF NITROGEN, SULFUR, AND PHOSPHORUS Many contaminants contain nitrogen, phosphorus, or sulfur, and degradative organisms may utilize one or more of these leaving the major part of the substrate intact. This is particularly important for munitions-related compounds with a high N/C ratio, when the addition of carbon sources may lead to the favorable development of anaerobic or facultatively anaerobic microorganisms.

SUBSTRATE CONCENTRATION There is substantial evidence from the aquatic environment for the existence of threshold concentrations below which rates of degradation of xenobiotics are slow or even negligible (Alexander 1985). A number of hypotheses have been put forward including the critical concentrations required for

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induction and maintenance of the degradative enzymes (Janke 1987). Whether this occurs in the terrestrial environment as well has been explored only supericially, but may be important when only low concentrations of the substrate are available, for example, by desorption. However, organisms that are adapted to such concentrations may be present, and examples have been provided in Chapter 4. Studies with Burkholderia sp. strain PS14 are instructive: 1,2,4,5-tetra- and 1,2,4-trichlorobenzenes at concentrations of 500 nM were mineralized to the extent of 70% in mineral liquid medium within 1 h, and in spiked sterilized soil to ca. 80% after 100 min (Rapp and Timmis 1999). Although in this experiment there was no evidence for a threshold concentration >0.5 nM, the situation in aged soils in which mass transfer is limiting may be signiicantly less encouraging.

TEMPERATURE Many contaminated sites are located in areas with temperatures considerably less than 15°C, and investigations into the role of temperature have therefore been carried out. Some of the cardinal results have been discussed in Chapter 4, and it may be concluded that although the rates at 4–5°C may be low, selection of organisms for adaptation to the ambient temperature will generally ensure that degradative activity is retained. There may, however, be selective degradation of speciic groups of components in mixtures such as PCBs.

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Schleussinger A, B Ohlmeier, I Reiss, S Schulz (1996) Moisture effects on the cleanup of PAH-contaminated soil with dense carbon dioxide. Environ Sci Technol 30: 3199–3204. Schnoor JL, LA Licht, SV McCutcheon, NL Wolfe, LH Carreiora (1995) Phytoremediation of organic and nutrient contaminants. Environ Sci Technol 29: 318A–323A. Schouten A, G van den Berg, C Edel-Hermann, C Steinberg, N Gautheron, C Alabouvette, CH de Vos, P Lemanceau, JM Raaijmakers (2004) Defense responses of Fusarium oxysporum to 2,4-diacetylphloroglucinol, a broad-spectrum antibiotic produced by Pseudomonas luorescens. Mol Plant–Microbe Interact 17: 1201–1211. Schulz R, C Hahn, ER Bennett, JD Dabrowski, G Thiere, SKC Peall (2003) Fate and effects of azinophosmethyl in a low-through wetlands in South Africa. Environ Sci Technol 37: 2139–2144. Shimizu M, T Kimura, T Koyama, K Suzuki, N Ogawa, K Miyashita, K Dakka, K Ohmiya (2002) Molecular breeding of transgenic rice plants expressing a bacterial chlorocatechol dioxygenase gene. Appl Environ Microbiol 68: 4061–4066. Siciliano SD, H Holdie, JJ Germida (1998) Enzymatic activity in root exudates of Dahurian wild rye (Elymus daurica) that degrades 2-chlorobenzoic acid. J Agric Food Chem 46: 5–7. Siciliano SD, JJ Germida (1999) Enhanced phytoremediation of chlorobenzoates in rhizosphere soil. Soil Biol Biochem 31: 299–305. Siddiqui IA, D Haas, S Heb (2005) Extracellular protease of Pseudomonas luorescens CHA0, a biocontrol factor with activity against the root-knot nematode Meloidogyne incognita. Appl Environ Microbiol 71: 5646–5649. Siegrist RL, OR West, MI Morris, DA Pickering, DW Greene, CA Muhr, DD Davenport, JS Gierke (1995) In situ mixed region vapor stripping in low-permeability media. 2. Full-scale ield experiments. Environ Sci Technol 29: 2198–2207. Simon HM, CE Jahn, LT Bergerud, MK Sliwinski, PJ Weimer, DK Willis, RM Goodman (2005) Cultivation of mesophilic soil crenarchaeotes in enrichment cultures from plant roots. Appl Environ Microbiol 71: 4751–4760. Strauss HS (1997) Is bioremediation a green technology? J Soil Contam 6: 219–225. Sturchio NC, JL Clausen, IJ Heraty, L Huang, BD Holt, TA Abrajano (1998) Chlorine isotope investigation of natural attenuation of trichloroethene in an aerobic aquifer. Environ Sci Technol 32: 3037–3042. Taghavi S, T Barac, B Greenberg, B Borremans, J Vangronsveld, D van der Lelie (2005) Horizontal gene transfer to endogenous endophytic bacteria from poplar trees improves phytoremediation of toluene. Appl Environ Microbiol 71: 8500–8505. Thomas JM, CH Ward (1989) In situ biorestoration of organic contaminants in the subsurface. Environ Sci Technol 23: 760–766. Thompson PL, LA Ramer, JL Schnoor (1998) Uptake and transformation of TNT by hybrid poplar trees. Environ Sci Technol 32: 975–980. Timmis KN, RJ Steffan, R Unterman (1994) Designing microorganisms for the treatment of toxic wastes. Annu Rev Microbiol 48: 525–557. Timonen S, KS Jörgensen, K Haahtela, R Sen (1998) Bacterial community structure at deined locations of Pinus sylvestris–Suillus bovinus and Pinus sylvestris–Paxillus involutus mycorrhizospheres in dry pine forest humus and nursery peat. Can J Microbiol 44: 499–513. Tjeerd van Rij E, G Girard, BJJ Lugtenberg, GV Bloemberg (2005) Inluence of fusaric acid on phenazine-1carboxamide synthesis and gene expression of Pseudomonas chlororaphis strain PCL1391. Microbiology (UK) 151: 2805–2814. Tjeerd van Rij E, M Wesselink, TFC Chin-A-Woeng, GV Bloemberg, BJJ Lugtenberg (2004) Inluence of environmental conditions on the production of phenazine-1-carboxamide by Pseudomonas chlororaphis PCL 1391. Mol Plant-Microbe Interact 17: 557–566. Uchida E, T Ouchi, Y Suzuki, T Yoshida, H Habe, I Yamaguchi, T Omori, H Nojiri (2005) Secretion of bacterial xenobiotic-degrading enzymes from transgenic plants by an apoplastic expression system: applicability for phytoremediation. Environ Sci Technol 39: 7671–7677. Ugrekhelidze D, F Korte, G Kvesitadze (1997) Uptake and transformation of benzene and toluene by plant leaves. Ecotoxicol Environ Saf 37: 24–29. Utsumi R et al. (1991) Molecular cloning and characterization of the fusaric acid-resistance gene from Pseudomonas cepacia. Agric Biol Chem 55: 1913–1918. Van Aken B, JM Yoon, CL Just, JL Schnoor (2004) Metabolism and mineralization of hexahydro-1,3, 5-trinitro-1,3,5-triazine inside poplar tissues (Populus deltoides x nigra DN-34). Environ Sci Technol 38: 4572–4579.

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van den Broek D, TFC Chin-A-Wong, GV Bloemberg, BJJ Lugtenberg (2005) Molecular nature of spontaneous modiications in gacS which cause colony phase variation in Pseudomonas sp. strain PCL1171. J Bacteriol 187: 593–600. Verstraete W, W Devlieger (1996) Formation of non-bioavailable organic residues in soil: perspectives for site remediation. Biodegradation 7: 471–485. Vílchez S, L Moloina, C Ramos, JL Ramos (2000) Proline catabolism by Pseudomonas putida: cloning, characterization, and expression of the put genes in the presence of root exudates. J Bacteriol 182: 91–99. Villacieros M et al. (2005) Polychlorinated biphenyl rhizoremediation by Pseudomonas luorescens F113 derivatives, using a Sinorhizobium meliloti nod system to drive bph gene expresssion. Appl Environ Microbiol 71: 2687–2694. Walton BT, TA Anderson (1990) Microbial degradation of trichloroethylene in the rhizosphere: potential application to biological remediation of waste sites. Appl Environ Microbiol 56: 1012–1016. Wang K, K Conn, G Lazarovits (2006) Involvement of quinolinate phosphoribosyl transferase in promotion of potato growth by a Burkholderia strain. Appl Environ Microbiol 72: 760–768. White C, A Quiñones-Rivera, M Alexander (1998) Effect of wetting and drying on the bioavailability of organic compounds sequestered in soil. Environ Toxicol Chem 17: 2378–2382. Widdowson MA, S Shearer, RK Andersen, JT Novak (2005) Remediation of polycyclic aromatic hydrocarbon compounds in groundwater using poplar trees. Environ Sci Technol 39: 1598–1605. Wiesner MR, MC Grant, SR Hutchins (1996) Reduced permeability in groundwater remediation systems: role of mobilized colloids and injected chemicals. Environ Sci Technol 30: 3184–3191. Wilken A, C Bock, M Bokern, H Harms (1995) Metabolism of PCB congeners in plant cell cultures. Environ Toxicol Chem 14: 2017–2022. Wilson MS, EL Madsen (1996) Field extraction of a transient intermediary metabolite indicative of real time in situ naphthalene biodegradation Environ Sci Technol 30: 2099–2103. Wolfaardt GM, JR Lawrence, RD Robarts, DE Caldwell (1995) Bioaccumulation of the herbicide diclofop in extracellular polymers and its utilization by a bioilm community during starvation. Appl Environ Microbiol 61: 152–158. Yadav JS, RE Wallace, CA Reddy (1995) Mineralization of mono- and dichlorobenzenes and simultaneous degradation of chloro- and methyl-substituted benzenes by the white-rot fungus Phanerochaete chrysosporium. Appl Environ Microbiol 61: 677–690. Yao J, C Allen (2006) Chemotaxis is required for virulence and competitive itness of the bacterial wilt pathogen Ralstonia solanacearum. J Bacteriol 188: 3697–3708. Ye D, MA Siddiq, A Maccubbin, S Kumar, HC Sikka (1996) Degradation of polynuclear aromatic hydrocarbons by Sphingomonas paucimobilis. Environ Sci Technol 30: 136–142. Yee DC, JA Maynard, TK Wood (1998) Rhizoremediation of trichloroethyelene by a recombinant, rootcolonizing Pseudomonas luorescens strain expressing ortho-monooxygenase constitutively. Appl Environ Microbiol 64: 112–118.

13 Evaluation of Bioremediation INTRODUCTION An essential component of any bioremediation program is the evaluation of its success. Evaluation is not as readily accomplished as might be assumed for a number of reasons (Madsen 1991; Heitzer and Sayler 1993; Macdonald and Rittman 1993; Shannon and Unterman 1993). A valuable and critical review (Dott et al. 1995) discussed the need for an assessment that takes into account all the phases involved, and suggested that the dificulty of demonstrating in situ bioremediation may require long-term studies. An illustrative example is provided by bioremediation of an aquifer in Switzerland, which was contaminated with diesel fuel. Oxidants were provided in the form of O2 and NO3–, but measurements of carbon and nitrogen balance were not suficiently precise to assess the spatial effectiveness of the treatment. A laboratory microcosm using material from the aquifer was constructed: the use of gene probes revealed that bacteria belonging to different phylogenetic groups were present, and bacteria able to degrade toluene and 1,3-dimethylbenzene were isolated (Hess et al. 1997). It was, however, pointed out that, because of the greater diversity of organisms in the aquifer, there were limitations in the extent to which the results of the laboratory experiments could be extrapolated to the ield situation. Cardinal issues for assessing the effectiveness of bioremediation include the following: 1. Diminution in the concentration of the substrate(s) is not alone an acceptable measure of degradation, since loss may occur by volatilization or by transformation with the formation of transient or terminal metabolites. In addition there may be a continuous input, for example, by leaching. 2. The terrestrial environment is highly heterogeneous, so that representative sampling generally presents a serious problem, and the evaluation of spatial effectiveness is dificult (Hess et al. 1997). 3. The extent of leaching into groundwater may be dificult to evaluate, because few of the systems are suficiently enclosed to make a convincing balance of the concentrations of the substrates and their metabolites—including CO2 or CH4 —that are lost to the atmosphere. 4. Most ield environments are dynamic. There are therefore continuous changes in the input and in the metabolites that are being produced. Interpretation of chemical analyses may therefore be equivocal, and metabolites may be removed at different rates. One approach has been to use surrogate contaminants, for example, (E/Z)-chloroluoroethene for chloroethene, in which only the E isomer is dechlorinated (Ennis et al. 2005). 5. Chemical analysis alone is insuficient in view of analytical uncertainties in the optimal methods for extraction. These must take into account both the free and associated analytes (Cajthaml and Sasek 2005), as well as metabolic products. A number of strategies have been proposed as potentially attractive solutions to evaluate the number of speciic degradative organisms, or of the appropriate degradative enzymes. These procedures include chemical analysis of contaminants and degradation products, the analysis of populations, and the use of stable isotope enrichment, which are discussed below. All of them require knowledge of the degradation pathways under the relevant conditions, and this is generally based on laboratory studies with pure or mixed cultures achieved by enrichment at the expense of the contaminant. Although many of the examples that are given refer to laboratory experiments, the principles that

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emerge are relevant to ield application with appropriate changes in the methodology. The questions all of them attempt to address are (a) is degradation taking place? and (b) at what rate?

ANALYSIS OF POPULATIONS Whereas in aquatic systems, bacteria are generally considered to be the major agents of biodegradation, the role of fungi in terrestrial systems may be equal or greater. Among fungi, considerable attention has been devoted to the metabolically versatile white-rot fungi (Shah et al. 1992; Barr and Aust 1994), and several examples are cited later. It is important to appreciate the wide range of organisms belonging to this group, even though greatest attention has hitherto been devoted to Phanerochaete chrysosporium. Further comments are given in Chapter 9, Parts 1 and 2, and the following discussion is restricted to bacteria. Pathways for the degradation of synthetic substrates have been elucidated in laboratory experiments using cultures of bacteria that have been obtained by elective enrichment with the given or a related substrate. This may, however, introduce a bias, not only in the organisms but also in the degradative genes that they contain (Marchesi and Weightman 2003). In addition, there are many organisms in natural habitats that have not hitherto been cultivated (Stevenson et al. 2004), and these will almost certainly play an important role in degradation. Natural enrichment certainly takes place in environments that have been chronically exposed to contaminants, and this is an important mechanism for the loss of agrochemicals. At the same time, bacteria that have been isolated from pristine environments with no established exposure to the contaminants may be able to degrade contaminants (e.g., Kitagawa et al. 2002; Sánchez et al. 2004). A number of procedures have been used for the analysis of natural populations including some, which are directed to speciic metabolic activity, and use a variety of methods that have been developed in molecular biology. In general, these presuppose knowledge of the mechanisms for degradation of the contaminants, and this is equally true for methods using stable isotope analysis. In spite of the caution that has been directed to the limitations of pure culture methods, it is the use of these that has built up the background for these studies, which are not dependent on isolation of speciic organisms. Application of polymerase chain reaction (PCR) to speciic degradative organisms has been reviewed (Steffan and Atlas 1991).

ANALYSIS OF DEGRADATIVE POPULATIONS There has been substantial interest in identifying bacteria in environmental samples with a view to determining the components of bacterial communities and understanding their role in biodegradation and biotransformation. This has been possible by using molecular procedures including appropriate genetic probes to determine the existence of speciic metabolic activity, and analysis of 16S rRNA and 16S rDNA to assess the similarity of isolates to other taxa. A valuable overview of the principles and application of a range of molecular procedures has been given (Power et al. 1998). Potential applications include: a. Analysis of natural degradation in the context of bioremediation that may usefully be combined with the use of stable isotope enrichment factors. b. Comparison of the degradation potential of natural populations with that of organisms isolated by enrichment. c. Prospecting for novel enzyme activity by analysis of soil metagenomes. These studies have revealed a number of cardinal aspects of microbial ecology: (a) the complexity of bacterial ecosystems, (b) the number of organisms of hitherto undetermined taxonomy, (c) the existence of organisms that have not been cultivated, and (d) the dificulty of assigning metabolic roles to many of the genomic sequences that have been revealed. Some examples are given to

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illustrate the range and application of these procedures. These include dioxygenation of aromatic compounds, alkane degradation, anaerobic dechlorination, and the discovery of hydrolytic enzymes for natural polymers.

APPLICATION TO THE DEGRADATION OF SPECIFIC CONTAMINANTS Hydrocarbons 1. Analysis of the occurrence and frequency of genes encoding the dioxygenases for aromatic hydrocarbons have been used to evaluate the potential of a site for bioremediation: a. An evaluation of the effect of plants on the remediation of a PAH-contaminated combined mineralization of 13C-labeled naphthalene in the bulk soil and in the rhizosphere, with the occurrence of genes speciic for dioxygenation of naphthalene (ndoB), alkane monooxygenation (alkB), and catechol 2,3-dioxygenase (xylE) (Siciliano et al. 2003). The results showed that even aged contaminants were susceptible to plant-mediated degradation in the rhizosphere. b. A study directed to the analysis of aromatic hydrocarbon degradation used real-time PCR ampliication of oxygenase genes. The primer sets were identiied for the large subunits (α) of genes for dioxygenases including those for naphthalene, biphenyl, and toluene, and monooxygenases for xylene, phenol, and ring monooxygenases for toluene (Baldwin et al. 2003). c. The abundance of genes similar to the α-subunit of the nagAc naphthalene dioxygenase gene in Ralstonia sp. strain U2, which encodes the degradation of naphthalene to salicylate, was analyzed by real-time PCR in samples from a coal tar–contaminated site (Dionisi et al. 2004). There was a strong positive correlation between the number of gene copies and the concentration of naphthalene at the site, and a lower correlation with concentrations of phenanthrene, and it was concluded that active biodegradation was occurring. d. Isolates from a site contaminated with benzene, toluene, ethylbenzene, and xylenes (BTEX) were analyzed to assess the diversity of dioxygenases in the α-subunit of the toluene/biphenyl subfamily and the ability to grow with benzene, toluene, and ethylbenzene. All strains could degrade benzene, but only a few of them could degrade toluene and ethylbenzene. There was strong correlation between sequence type and substrate utilization, and sequence analysis showed that dioxygenases belonging to the isopropylbenzene is branch-dominated (Witzig et al. 2006). 2. A reverse sample genome probe procedure has been used to monitor sulfate-reducing bacteria in oil-ield samples (Voordouw et al. 1991). It was extended to include 16 heterotrophic bacteria (Telang et al. 1997), and applied to evaluating the effect of nitrate on an oil-ield bacterial community. Denatured genomic DNAs were used in a reverse sample genomic probe procedure to examine the effect of toluene and dicyclopentadiene on the community structure of bacteria in a contaminated soil. Hybridization of total community DNA isolated from soil exposed to toluene showed enrichment of strains that were able to metabolize toluene. At the same time, DNA from the soil contaminated with dicyclopentadiene indicated the enrichment of organisms that were able to form products by oxygenation with masses of 146 and 148, which corresponded to derivatives with epoxide or ketone groups. In contrast, no mineralization of dicyclopentadiene was observed (Shen et al. 1998). 3. The archaeal population in anaerobic oil-contaminated water at a crude oil storage site was examined using PCR ampliication of fragments of 16S rDNA using a range of primers. Although two of the sequences were closely related to Methanosaeta concilii and Methanomethylovorans hollandica, other sequences could not be identiied, including the most abundant (KuA12) that accounted for ≈50% of the total archaeal rDNA copies that

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were detected. Species of novel archaea were enriched at the site, and were putatively active methanogens (Watanabe et al. 2002). 4. A stable mixed culture that could degrade benzene was established, and the speciic role of sulfate-reducing bacteria was inferred from the inhibition of degradation in the presence of molybdate. The consortium was characterized from the sequence of small subunit rRNA genes, some of which could be assigned to the family Desulfobacteriaceae (Phelps et al. 1998). Trichloroethene 1. Populations of bacteria had been enriched by adding lactate to enrich the indigenous organisms for in situ dechlorination of trichloroethene (TCE) to ethene. The consortia in the groundwater source were assessed using PCR ampliication of 16S rRNA genes. In a clone library, a homoacetogen dominated the archaea, with a clone afiliated to the acetoclastic methanogen Methanosaeta concilii, while proteobacteria similar to Geobacter (Trichlorobacter) thiogenes and Sulfurospirillum multivorans were also found. A mixed culture that dechlorinated TCE to ethene was enriched from the groundwater and this was compared with that in the groundwater by terminal restriction fragment length polymorphism (RFLP). Although the enrichment community was less diverse than that from the groundwater, its archaeal structure was similar. It was concluded that acetate produced from the fermentation of lactate was the source of methane by the acetoclastic pathway (Macbeth et al. 2004). 2. The use of toluene to induce oxygenation of haloalkanes has been discussed in Chapter 7, Part 3, and probes for toluene-2-monooxygenase have been used to evaluate the potential number of TCE-degrading organisms in an aquifer (Fries et al. 1997b). In this study, repetitive extragenic palindromic PCR (REP-PCR) (de Bruijn 1992) of isolates was used to classify their metabolic capability. 3. To assess the population of organisms capable of degrading TCE at a contaminated site, samples were examined from a contiguous, but pristine site. Attention was directed to methane- and ammonia-oxidizing bacteria, and included both free-living and attached communities. Primer sets included genes for particulate methane monooxygenase and ammonia monooxygenase. Whole-genome ampliication was used for metagenomic DNA from each of the communities at the sampling sites. Bacteria related to Methylocystis dominated both the free-living and attached communities, and gene sequences associated with TCE metabolism were observed for both of them (Erwin et al. 2005). Phenol 1. Analysis of the populations of two phenol-degrading bacteria Pseudomonas putida BH and Comamonas sp. strain E6 introduced into an activated sludge system was carried out by extraction of DNA, PCR ampliication of the gyrB gene fragments using strain-speciic primers, and quantiication after electrophoresis by densitometry. Appropriate dilutions of the extracted DNA were used to maintain linearity between the measured intensity and population density. The initial inocula of ca. 108 cells/mL fell to ca. 104 cell/mL after 10 d and thereafter remained steady for a further 18 d (Watanabe et al. 1998a). 2. A study of the community in a phenol-degrading population used ampliication of the gene encoding the largest subunit of phenol hydroxylase, followed by analysis using temperature gradient gel electrophoresis. Bacteria were also isolated by three procedures: (i) direct plating on a complex medium or a mineral medium supplemented with phenol, (ii) by enrichment in batch culture, and (iii) by chemostat enrichment. The dominant population could be isolated only by direct plating or by chemostat enrichment. One of the dominant organisms that contained a novel large phenol hydroxylase subunit was closely related to

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Variovorax paradoxus, and it was proposed that this was the principal organism for degradation of phenol in the community (Watanabe et al. 1998b). 3. A site at the Agricultural Experimental Station (Ithaca, NY) was treated in microcosms with 13C-labeled glucose, phenol, caffeine, and naphthalene. Levels of 13CO2 were measured to assess utilization of the substrates, and the populations analyzed by separating the 13 C-labeled DNA by density centrifugation, followed by PCR ampliication and sequencing of 16S rRNA (Padmanabhan et al. 2003). Populations contained relatives to a range of bacteria that varied with the substrate. Only relatives of Acinetobacter were found in all samples, and for caffeine only Pantoea. 4. In a further study (DeRito et al. 2005) at the same site, attention was concentrated on phenol using respiration of 13C-labeled phenol and stable isotope probes of soil DNA. It was shown that the whole community could utilize products from the degradation of phenol. The distribution of labeled carbon was determined by using different regimes for the addition of substrate, and populations could be distinguished on the basis of their diversity. The greatest diversity was found in organisms from soil that had not been enriched with phenol, while members of the Gram-positive genera Kocuria and Staphylococcus dominated the phenol-degrading population. Members of the genus Pseudomonas dominated those that were metabolically versatile and were able to utilize the carbon from other organisms. Chlorophenol Soil samples were enriched in medium containing 2,4,6-trichlorophenol and subjected to a procedure to reduce the complexity of the mixed lora. This involved cyclic serial dilution, plating, and growth in liquid medium. REP-PCR and ampliied ribosomal DNA restriction analysis (ARDRA) were used to monitor the lora during the cycles. From the fourth cycle, four organisms were isolated. Although three of them were unable to utilize 2,4,6-trichlorophenol, an additional slow-growing organism that was able to do so was isolated, and tentatively assigned to the genus Nocardioides (Maltseva and Oriel 1997). Chlorobenzoate The occurrence of bacteria that can mineralize 3-chlorobenzoate has been examined in soil samples from widely separated regions in ive continents (Fulthorpe et al. 1998). The genotypes of the isolates were examined by two procedures: (i) REP-PCR genomic ingerprints (de Bruijn 1992) and (ii) analysis of restriction digests of the 16S rRNA (ARDRA) (Weisberg et al. 1991). The results showed that each genotype was generally (91%) restricted to the site from which the samples were collected, and that therefore the genotypes were not derived by global dispersion. Phenylurea Herbicides 1. DNA was extracted from soil samples that had been treated with three phenylurea herbicides during 10 years and from an untreated control. The PCR products using two primers were analyzed by denaturing gradient gel electrophoresis (DGGE), and the patterns used to assess the quantitative similarities of the bands. PCR using two different primers followed by DGGE was used to obtain 16S rDNA for sequencing (El Fantroussi et al. 1999). The microbial diversity determined from the gel proiles had decreased in the treated soils, and the sequencing revealed that the organisms that were most affected belonged to hitherto uncultivated taxa. Enrichment cultures showed that dichlorinated linuron was more readily degraded in cultures using the treated soils than from those using the untreated soils. DGGE analysis and sequencing showed that one of the components, which was found only in these enrichments, showed a 95% similarity to Variovorax sp. that was also found in enrichments using 2,4-dichlorophenoxyacetate (Kamagata et al. 1997). The

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effect of the herbicide applications had therefore affected both the composition of the bacteria lora and the metabolic capabilities of its components. 2. Analysis of a bacterial population that could degrade the chlorinated phenylurea herbicide linuron revealed the presence of several strains of bacteria, which were identiied on the basis of 16S rRNA gene sequences, isolation of the strains, and determination of their metabolic role (Dejonghe et al. 2003). Five strains were identiied of which Variovorax strain WDL1 was able to use linuron as a source of carbon, nitrogen, and energy. Among the other strains, Hyphomicrobium sulfonivorans was able to degrade N,O-dimethylhydroxylamine, while degradation of linuron was stimulated by the presence of these other strains. Dehalogenation of Chloroalkanoates Dehalogenases from bacteria enriched from activated sludge for the degradation of 2,2-dichloropropionate were compared with those from the environmental metagene pool. Although the dehalogenases found in pure cultures dominated the enrichment culture, they were only a minor part of the community used for enrichment. Analysis of dehalogenase genes found in pure cultures with those from the metagenome pool from which they were isolated revealed the substantial bias introduced by culturing both in the bacteria and in their degradative genes (Marchesi and Weightman 2003). Dechlorination of PCBs Metabolic inhibitors were used in an elegant set of experiments designed to enrich for the anaerobic organisms that carried out the ortho dechlorination of 2,3,5,6-tetrachlorobiphenyl (Holoman et al. 1998), and the community structure was followed by analysis of total community genes for 16S rRNA. It was shown that the diversity of the community could be reduced in mineral medium by the addition of inhibitors for methanogens (2-bromoethanesulfonic acid) and Clostridium spp. (vancomycin), without eliminating dechlorination that was inhibited by the addition of molybdate, which inhibited sulfate reduction. The bacteria that actively carried out ortho dechlorination belonged to three groups: the δ group, the low G + C Gram-positive group, and the Thermotogales subgroup that had not hitherto been implicated in anaerobic dechlorination.

APPLICATION TO SPECIFIC GROUPS OF ORGANISMS There has been considerable interest in the anaerobic metabolism of methane in the large reservoirs that lie beneath the sealoor, since little of this reaches the oxic conditions in the water column. Consortia of archaea that have so far resisted isolation and sulfate-reducing bacteria have been implicated (Orphan et al. 2002): 1. A hydrothermal vent in the Gulf of California produces hydrocarbons that support the growth of sulfate-reducing bacteria. PCR-ampliied genes for sulite reductase (dsrAB) and 16S rRNA were analyzed in sediment cores. Groups related to Desulfobacter that could utilize acetate represented a major group, while organisms afiliated with members of the genus Desulfotomaculum and organisms in the δ proteobacteria were also found (Dhillon et al. 2003). 2. Cores from the same vent were examined by 16S rRNA sequencing complemented with isotopic analysis of lipids. Uncultured groups associated with anaerobic methane oxidation ANME-1 and ANME-2 were identiied, while δ13C values for archaeal lipids (archaeol, sn-2-hydroxyarcheol, and diphytanediol) indicated their origin in methanotrophic archaea (Teske et al. 2002). Analysis of the sequences for methyl coenzyme M reductase A (mcrA) in ANME-1 and ANME-2 suggested its potential catalytic activity (Hallam et al. 2003). It was proposed that anaerobic methane oxidation could occur by the reversal of methanogenesis, since many, though not all, of the genes could be identiied in both pathways (Hallam et al. 2004).

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NONDIRECTED EXAMINATION OF NATURAL POPULATIONS 1. Core samples from three redox zones at depths of 6.1, 7.3, and 9.2 m in an aquifer contaminated with hydrocarbons and chlorinated solvents were examined (Dojka et al. 1998). Small subunit rRNA genes from core DNA were ampliied directly by PCR with Bacteriaor Archaea-speciic primers and cloned, and the clones screened by RFLP. Analysis of the sequences showed the existence of the following types: (a) 10 with no known taxonomic divisions, (b) 21 with no cultured representatives, and (c) 63 with recognized divisions. The sequences were classiied into seven major groups, and it was shown that the two most abundant sequence types could be correlated with sequences of Methanosaeta sp. and Syntrophus sp. It was proposed that hydrocarbon degradation proceeded by oxidation of the hydrocarbons, fermentation of the resulting carboxylic acids by organisms with sequences related to Syntrophus sp., followed by acetoclastic methanogenesis by organisms related in sequence to Methanosaeta sp. 2. Small subunit rRNA genes were ampliied directly by PCR in DNA from a sediment sample in Yellowstone National Park and cloned: universally conserved or Bacteriaspeciic rDNA primers were used (Hugenholtz et al. 1998). RFLP was used to classify rDNA fragments. Most of the sequences were representatives of established bacterial division, although 30% were unrelated. Database matches suggested the presence of organisms closely related to (a) Thermodesulfovibrio yellowstonii that could carry out anaerobic sulfate reduction, (b) the organotrophs Thermus sp. and Dictyoglomus thermophilum, and (c) the hydrogen-oxidizing Calderobacterium hydrogenophilum. In contrast to previous perceptions, however, members of Bacteria dominated over Archaea in this sediment, so that the ecological boundaries between Bacteria and Archaea were less clearly deined. 3. The organisms in a high-salinity evaporation pond were examined by plating on solid media with prolonged incubation, and by analysis of a library of PCR-ampliied 16S rRNA genes (Burns et al. 2004). The isolates were related to species of several genera including Haloferax, Halorubrum, and Natromonas. The irst of these was not, however, represented in the gene library, and it was suggested that this could be the result of the ability to form colonies, even when it was not a dominant group. A major group identiied in the library was the SHOW square organisms that have so far deied cultivation.

APPLICATION OF STABLE ISOTOPES The application of stable isotopes has been introduced in Chapter 6, and the following is devoted to illustrating speciic applications.

STABLE ISOTOPE PROBES This procedure makes it possible to relate function in the environment to speciic organisms or enzymes that carry out degradation. 1. Application to a site contaminated with coal tar waste and containing aromatic hydrocarbons was examined using a number of procedures. These included the use of 13C-labeled naphthalene followed by fractionation of labeled DNA, and construction of a library of cloned bacterial 16S rRNA. These were complemented with conventional assays for respiration, and isolation of bacteria by serial dilution and plating on a mineral medium during exposure to naphthalene. A strain CJ2 that closely resembled Polaromonas vacuolata was isolated from the contaminated sediment and was active in situ, even though the naphthalene dioxygenase gene was not related to that of existing strains of the genus (Jeon et al. 2003). 2. A phenol-degrading community was examined using 13C phenol followed by analysis of the stable-isotope-labeled RNA by equilibrium density centrifugation, and complemented

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with reverse-transcription-PCR and DGGE. The results suggested the dominance of a species of Thauera in addition to organisms conventionally associated with phenol degradation (Maneield et al. 2002). a. The population of putative methanotrophs in a peat soil microcosm was examined by long-term incubation with 13CH4 followed by separation of DNA by gradient centrifugation. This was used as a template for PCR. The ampliied products of 16S rRNA genes and those for genes that encode enzymes established for methane oxidation were analyzed (Morris et al. 2002). Although sequences related to type I and type II methanotrophs were identiied, the existence of clones related to the β-subclass of Proteobacteria indicated the presence of other groups. b. In an analogous study, the assimilation of 13CH3OH or 13CH4 was examined (Radajewski et al. 2002). Analysis showed the presence of bacteria belonging to the genera Methylocella, Methylocystis, and Methylocapsa, while DNA from the microcosms that was used as a template for PCR with ammonia oxygenase-speciic primers showed sequences belonging to Nitrosomomas and Nitrosospira. A number of other sequences were observed, although their function was not resolved. c. The methylotrophic community in soil from rice paddies was examined by a number of methods including 13C labeling with methanol followed by incubation under aerobic conditions and analysis of 13C-labeled rRNA by density measurement in a Cs triluoroacetate gradient. Sequence analysis of labeled rRNA revealed the presence of bacteria belonging to the Methylobacteriaceae, although with increasing length of incubation the Methylophilaceae dominated. In addition, labeled nucleic acids were observed in fungi and protozoans, and it was concluded that the 13C accumulated in the methylotrophs had been transferred during incubation to these organisms (Lueders et al. 2004a). Gasoline-contaminated groundwater containing BTEX from an aquifer was supplemented with [13C]benzene and an electron acceptor. Analysis of the 13C-RNA fraction revealed the presence of a phylotype related to the genus Azoarcus only when nitrate was used as supplement. This was conirmed by DGGE of 16S rRNA gene fragments. Isolation on a nonselective medium and screening of the colonies by DGG resulted in the isolation of two strains that were able to degrade benzene, toluene, and m-xylene though—not o- or p-xylene. It was suggested that the success of this procedure lay in combining stable isotope probing with DGGE screening of strains isolated on nonselective medium (Kasai et al. 2006). It has been established that methane is produced on rice roots by reduction of CO2. This was examined in rice roots using a combination of 16S rRNA sequencing and density gradient fractionation of 13C-labeled DNA after incubation with 13CO2. The major groups of archaea detected were Methanosarcinaceae that decreased with time to be replaced by the hitherto uncultured Rice Cluster I, although the former subsequently dominated (Lu et al. 2005). The syntrophic population of anaerobic organisms that carry out the oxidation of propionate was examined using [13C]propionate. Analysis of the “heavy” 13C-labeled rRNA by terminal restriction length polymorphism ingerprinting and sequence analysis of the resolved populations showed the presence of the genera Syntrophobacter, Smithella, and Pelotomaculum whose degradation of propionate had already been conirmed in other laboratory studies. Among the archaea, species of Methanobacterium, Methanosarcina, and members of the Rice Cluster I were found (Lueders et al. 2004b).

APPLICATION OF STABLE ISOTOPE ENRICHMENT This has attracted considerable attention in evaluating the effectiveness of remediation either by natural populations or those enriched by speciic additions. Isotopic analysis of the contaminant supplemented with that of established metabolites makes it possible to determine whether degradation

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and transformation has taken place within the impacted area. It may also be possible to determine the rates at which this has taken place, and sometimes degradation pathways. Results from these experiments have been reported in a number of ways depending on the objective, and these have been summarized in Chapter 6. Illustrative examples include the following. Application of δ13C Chlorinated Aromatic Hydrocarbons 1. Values of δ13C have been measured for a number of polychlorinated biphenyl (PCB) congeners and applied to a number of commercial PCB mixtures. Both the number and the position of the chlorine substituents affected the depletion of 13C, and this relected the manufacturing procedures that involved kinetic isotope effects as well as the source of the biphenyl starting material (Jarman et al. 1998). It was suggested that this could be applied to determine the source of PCBs in the environment. 2. An anaerobic bacterial enrichment culture was used to examine the dechlorination of 2,3,4,5-tetrachlorobiphenyl that produced 2,3,5-trichlorobiphenyl exclusively. Although there was no alteration in the values of δ13C, compound-speciic analysis of Arochlor 1268 showed that there was a trend for decreasing 13C abundance with increasing content of chlorine. This is consistent with dechlorination of the congeners with more chlorine substituents. It was suggested that reductive dechlorination of PCBs would produce congeners with more depleted values of δ13C compared with unweathered Arochlors (Drenzer et al. 2001). 3. Values of δ13C were measured for the degradation of trichlorobenzenes (Griebler et al. 2004). For aerobic degradation by Pseudomonas sp. strain P51, which carried out degradation by dioxygenation, the values were not signiicant. In contrast, the isotope enrichment factor (ε) for anaerobic dechlorination by Dehalococcoides sp. strain CDB1, which produced 1,3-dichlorobenzene from 1,2,3-trichlorobenzene, was –3.4 ppm, and for 1,2,4trichlorobenzaene, which produced 1,4-dichlorobenzene, was –3.2 ppm. Methyl tert-Butyl Ether Enrichment factors have been used in studies with methyl tert-butyl ether (MTBE) that is a fuel additive and is a widespread contaminant in subsurface aquatic systems. 1. In laboratory enrichments with MTBE under both methanogenic and sulfate-reducing conditions, carbon enrichment of –14.4 ± 0.7 ppm was found (Somsamak et al. 2006), and in a methanogenic enrichment –14 ± 4.5 ppm for tert-amyl methyl ether (Somsamak et al. 2005). 2. Both δ13C and δ2H were used in an examination of several contaminated groundwater sites (Kuder et al. 2005). The isotopes were extensively fractionated during anaerobic degradation with stable enrichment factors of –13 ppm for carbon and –16 ppm for hydrogen. These values were used to predict the extent of biodegradation at the sites using the Raleigh model for degradation. 3. In a ield investigation of groundwater where there were several sources of MTBE, values of δ13C ranged from –26 to +40 ppm, and δ2H from –73.1 to +60.3 ppm that were consistent with degradation along the plume (Zwank et al. 2005). At the same time, the carbon composition of tert-butanol that is produced by demethylation was constant, which showed that this was not further degraded. Comparison with previous measurements and important aspects of the methodology were discussed. Aromatic Hydrocarbons Investigations have examined applications to monocyclic aromatic hydrocarbons and phenols, under both aerobic and anaerobic conditions.

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Aerobic Conditions

1. Two strains for which the mechanism of biodegradation of benzene had not been established were examined for carbon and hydrogen isotope fractionation (Hunkeler et al. 2001). Values for Acinetobacter sp. and Burkholderia sp. were, respectively, –1.46 and –3.53 ppm for carbon and –12.8 and –11.2 ppm for hydrogen. Values of δ13C and δ2H for benzene differed from various sources, and it was pointed out that these differences should be taken into consideration. 2. Fractionation factors (ε) were measured for the aerobic degradation of aromatic hydrocarbons using several strains of bacteria that used different mechanisms for its initiation (Morasch et al. 2002). For strains of Pseudomonas putida strain F1 and naphthalene (strain BCIB 9816) that degrade toluene by dioxygenation, values for toluene were not signiicant. In contrast, for strains that initiated the degradation of alkylbenzenes by monooxygenation, values for Pseudomonas putida strain mt-2 were –3.3 ppm for toluene, –1.7 ppm for m-xylene, and –2.3 ppm for p-xylene, and for Ralstonia pickettii strain PJO1 –1.1 ppm for toluene. Anaerobic Conditions

1. Under laboratory methanogenic and sulidogenic conditions, only low values of enrichment factors were observed, although 13C enrichment of toluene was found at late stages of transformation (Ahad et al. 2000). 2. In a continuous low headspace system, δ2H analysis was used during methanogenic degradation of toluene (Ward et al. 2000). Enrichment values exceeding –60 ppm were found, and these are about 10 times greater than the values reported for δ13C. It was suggested that combined use of both δ13C and δ2H would be attractive for assessing bioremediation at contaminated sites. 3. Four different conditions for the degradation of toluene were examined in cultures that used different electron acceptors (oxygen, nitrate, ferric iron, or sulfate), and different pathways for degradation (Meckenstock et al. 1999). The fractionation factors for Pseudomonas putida (1.0026), Thauera aromatica (1.0017), Geobacter metallireducens (1.0018), and a sulfate-reducing organism (1.0017) were in the same range for all the organisms. 4. Enrichment factors for both carbon and hydrogen were measured during anaerobic degradation of benzene using different electron acceptors (Mancini et al. 2003). There were no signiicant differences in the enrichment factors among the cultures, with values for δ13C from –1.9 to –3.6 ppm, and much larger values for δ2H (–29 to –79 ppm). This would be consistent with different mechanisms for degradation involving C–H bond ission. 5. Enrichment factors during the anaerobic degradation of o-xylene, m-xylene, m-cresol, and p-cresol by pure cultures of sulfate-reducing bacteria that use the fumarate pathway ranged from –1.5 to –3.9 ppm (Morasch et al. 2004). It was therefore proposed that this could be applied to evaluating in situ bioremediation of contaminants that use this pathway for biodegradation. 6. A sulfate enrichment culture prepared from a contaminated site gave enrichment factors (ε) of –1.1 for naphthalene and –0.9 for 2-methylnaphthalene (Griebler et al. 2004). These values combined with literature values from analogous laboratory experiments were used to quantify degradation of toluene, xylenes, and naphthalene at the site. Additional evidence for degradation of BTEX was derived from analyses of established metabolites produced by anaerobic degradation. 7. Direct evidence for the biodegradation of benzene and toluene in a contaminated aquifer was lacking, and an alternative strategy was examined. Bio-Sep beads were maintained in tubes and [13C] benzene or [13C]toluene were sorbed on to the surface. Analysis of δ13C in fatty acids extracted from lipids showed enrichments up to 13,500 ppm for benzene and

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toluene, and signiicant differences between values of individual fatty acids for the benzene and toluene amendments. It was therefore concluded that both benzene and toluene in the aquifer were being degraded, and in addition that different groups of organisms were responsible (Geyer et al. 2005). Chloroalkanes and Chloroalkenes Aerobic Conditions

1. For C1 and C2 chloroalkanes and chloroalkenes, δ13C values ranged from –25.58 (trichloroethane) to –58.77 (CH3Cl), and δ37Cl values from –2.86 (trichloroethane) to +1.56 (CH2Cl2). Although for analysis of environmental samples the method has the disadvantage that water must irst be removed from the samples, it has been used to determine the distribution of TCE in a contaminated aquifer (Sturchio et al. 1998). 2. During the aerobic degradation of chloroethene (vinyl chloride [VC]) by strains of Mycobacteria and Nocardioides, enrichment factors (ε) lay within the range –8.2 ± 0.1 to –7.0 ± 0.3 ppm (Chartrand et al. 2005). These values were lower than those for the anaerobic degradation of chloroethene, and values of the kinetic isotope effect were 1.10 ± 0.001 for aerobic degradation, compared with the value of 1.03 ± 0.007 for anaerobic degradation. These are consistent with the pathways in which the aerobic reaction involves the C=C bond compared with the higher mass of the C–Cl bond in the anaerobic reaction. 3. Experiments have been carried out with 1,2-dichloroethane for which the pathways of degradation have been established. For degradation by Pseudomonas sp. strain DCA1 in which degradation is initiated by monooxygenation, the enrichment factor was –3.0 ppm, whereas for organisms including Xanthobacter autotrophicus in which a dehalogenase initiates degradation values of –32.3 ppm were found (Hirschorn et al. 2004). This procedure therefore differentiated the mechanisms by which degradation took place, and would be applicable to ield studies. 4. Carbon isotope fractionation was examined during the aerobic degradation of TCE by Burkholderia cepacia strain G4 that possesses toluene monooxygenase activity (Barth et al. 2002). There were substantial differences in values of isotope shifts during degradation, from –57 to –17 ppm, and when the data were corrected to correspond to the same amount of substrate reduction the Releigh enrichment factor was –18.2. Anaerobic Conditions

1. A methanogenic enrichment culture was used to determine δ13C enrichment factors during the dechlorination of TCE, cis-1,2-dichloroethene (cis-DCE), and chloroethene (VC) (Bloom et al. 2000). Using the Raleigh model, enrichment factors (ε) were –6.6 and –2.5 ppm for TCE, –14.1 and –16.1 ppm for cis-DCE, and –26.6 and –21.5 ppm for VC. The large isotope effects that were observed suggested the value of this procedure for evaluating anaerobic dechlorination of chlorinated ethenes. 2. Anaerobic microbial consortia from different sources were used to determine enrichment factors for TCE, cis-dichloroethene, and chloroethene (VC) during dechlorination (Slater et al. 2001). For one of them (KB-1) that was able to bring about reductive dechlorination using methanol as electron donor, Raleigh enrichment factors values were –13.8, –20.4, and –22.4 ppm, whereas for tetrachloroethene for which the Raleigh model could not be applied, values varied among the consortia. It was suggested that this procedure could provide a valuable indication of dechlorination in spite of the rather wide spread of the enrichment factors that were observed. 3. A site at which earlier attempts at remediation of TCE did not proceed beyond production of cis-dichloroethene was augmented with the KB-1 culture, which had already been

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examined in microcosms. The isotope levels of cis-dichloroethene and chloroethene were increased at the inal sampling, although that of the continuous input of TCE remained essentially constant (Chartrand et al. 2005). 4. A comparison had been made of 13C fractionation during the dechlorination of tetrachloroethene by Sulfurospirillum multivorans and Desulitobacterium sp. strain PCE-S in laboratory experiments (Nijenhuis et al. 2005). Isotope fractionation in growing cultures was 1.0052 for Desulitobacterium sp. and only 1.00042 for Sulfurospirillum multivorans, whereas fractionation was greater in crude cell extracts from both strains. It was concluded that caution should therefore be exercised in applying fractionation factors to the evaluation of in situ bioremediation. Isotopes of oxygen, sulfur, and chlorine have been much less extensively used. Illustrations include the following. Application of δ18O

The values for δ13C and δ18O were examined during degradation of diesel oil by a mixed culture under aerobic conditions. Oxygen in the gas phase of closed samples was analyzed by conversion into CO2 after cryogenic separation. The values for oxygen were particularly valuable in correlating the production of carbon dioxide with the loss in substrate concentration (Aggarwal et al. 1997), and it was therefore suggested that this methodology could be used to provide rates of in situ biodegradation. Application of δ34S

1. Determinations of δ34S have been extensively used in studies on the sulfur cycle, including reactions involving microbial anaerobic reduction of sulfate and thiosulfate (Smock et al. 1998). 2. Isotope fractionation during sulfate reduction by the hyperthermophilic Archaeoglobus fulgidus varied with the concentration of sulfate, and it was suggested that different pathways were operative at concentrations >0.6 or 300. Those with more than seven rings are probably ubiquitous, although their determination is made dificult by the inaccessibility of reference compounds and by their long retention times on GC columns (Biggs and Fetzer 1996). PAHs with molecular mass >300 that occur in both carbon black and the NIST SRM 1597 coal tar extract include dibenzo[a,j]coronene (Mr 400) with nine rings, dinaphtho[2,1-a: 2,1-h]anthracene (Mr 378), and benzo[a]coronene (Mr 350) with eight rings (Bemgård et al. 1993). The degradability of such compounds is unknown, and they may possibly contain carcinogenic representatives. Attention should be directed to those PAHs that have been accepted as human carcinogens after metabolic activation: these include benzo[a]pyrene and dibenz[a,h]anthracene. In general, degradation of three- and four-ring PAHs is readily accomplished, whereas those with ive or more rings may be recalcitrant. However, a study using endogenous

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bacteria in a creosote-contaminated soil showed that benz[a]anthracene and chrysene were substantially degraded, although the degradation of chrysene was less when nutrients or a biosurfactant were added (Vinas et al. 2005). It is important to emphasize that not only PAHs may be present, but also the corresponding analogs containing nitrogen (azaarenes) and sulfur (thiaarenes) in the rings. This important group of contaminants has been reviewed in detail by Herod (1998), and some azaarenes such as dibenz[a,h]acridine and 7H-dibenzo[c,g]carbazole are carcinogenic. Although the biodegradation of these has been presented in Chapter 10 and in a review (Schwarz and Lingens 1994), the possibility of remediating sites contaminated with heteroarenes presents a number of unresolved issues. The fate of azaarenes seems not to have been examined directly in this context, while that of thiaarenes has attracted attention mainly in connection with the desulfurization of coal and coal oil (Wang et al. 1996; Macpherson et al. 1998). Azaarenes do, however, have an inhibitory effect on the biodegradation of PAHs even by a versatile strain such as Sphingomonas paucimobilis strain EPA505 (Lantz et al. 1997). By comparison with their carbocyclic analogs, rather less is known about the biodegradation of azaarenes, although the biochemistry of the aerobic degradation of quinolines (including methyl- and carboxyquinolines) has been extensively investigated by Lingens and his colleagues (Schwartz and Lingens 1994). As a broad generalization, it may be stated that the initial reaction frequently involves formal hydroxylation (addition of the elements of H2O followed by dehydrogenation) in the hetero ring, whereas ission of the carbocyclic ring is accomplished by dioxygenation. It is worth noting that these organisms may be quite restricted in their ability to use other azaarenes. For example, a strain of Rhodococcus sp. that was isolated by enrichment of pristine samples with quinoline was unable to use isoquinoline or acridine, and supported only poor growth with a series of pyridines (O’Loughlin et al. 1996). Although the degradation of acridine and phenanthridine seems to have been examined only parenthetically, the degradation of carbazole has been examined more extensively. An exhaustive study has revealed the production of several terminal metabolites formed by cyclization of the ission products from the carbocyclic ring (Gieg et al. 1996). However, benzocarbazoles seem not to have been examined. The mechanism of the degradation of dibenzofurans has been established in detail and is accomplished by angular dioxygenation with ission of the furan ring, while the biodegradation of benzothiophenes is complicated by oxidation at the sulfur atom. The biotransformation of dimethylbenzothiophenes was studied in three strains of Pseudomonas sp. growing with 1-methylnaphthalene or glucose (Kropp et al. 1997). A number of oxidations of different isomers was observed: (a) methyl groups to groups and carboxylic acids, (b) at the sulfur atom to produce sulfoxides and sulfones, and (c) the thiophene ring to form the 2- and 3-hydroxy compounds [2(3H) ones, 3(2H) ones], and 2,3-diones. The same pseudomonads were able to degrade 3,4-dimethyl- and 2,7-dimethyldibenzothiophenes by oxidative ission of one of the benzene rings, followed by oxidation of the thiophene ring. The Range of Degradative Bacteria Bacteria vary considerably in their capacity to degrade a range of PAHs, and extrapolation of results from the more-readily degraded naphthalene and phenanthrene should be carried out with caution. Some bacteria degrade only the more readily degradable naphthalene and phenanthrene, although pyrene and luoranthene seem to be more generally degradable. For example, Pseudomonas paucimobilis strain EPA 505 can degrade luoranthene, pyrene, benz[a]anthracene, chrysene, benzo[a]pyrene, and benzo[b]luoranthene, (Ye et al. 1996), and Gram-positive mycobacteria have attracted increasing attention: for example, a strain of Mycobacterium sp. degraded pyrene, benz[a]anthracene, and benzo[a]pyrene (Schneider et al. 1996). Details of these are given in Chapter 8, Part 2. In practice, contaminated sites will maintain a wide range of bacteria, and it has been shown that the lora will alter during degradation and will be inluenced by the addition of nitrogen and phosphorus nutrients (Vinas et al. 2005). In that study, denaturing gradient gel electrophoresis (DGGE) revealed a range of taxa. These included organisms belonging to the α-Proteobacteria

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(Sphingomonas) at the early stages of biodegradation, whereas at later stages in the absence of nitrogen and phosphorus supplementation these were supplemented by members of the γ-Proteobacteria (Xanthomonas) and the Cytophaga–Flexibacter–Bacteroides group (Bacteroides). Bioavailability and the Use of Surfactants This is a cardinal issue with many, sometimes contradictory facets, that merits more detailed consideration than can be given here. Strategies that have been used by cells for substrates with low or negligible water solubility are relevant to strategies for bioremediation. The accessibility of substrates at sites with a long history of contamination is a serious limitation to bioremediation, and attempts have been made to increase this by the addition of surfactants (Grimberg et al. 1996). A review (Volkering et al. 1998) has summarized data from experiments with alkanes and PAHs that used a range of surfactants. A few of the sometimes-contradictory aspects of the role of surfactants are briely summarized: 1. Signiicant differences have been found among different organisms (Guerin and Boyd 1992b; Crocker et al. 1995), and indeed incorporation of PAHs into micelles may make them less accessible as substrates (Volkering et al. 1995). 2. It has been shown in biodegradation experiments using a mixed bacterial culture, that components in a mixture of naphthalene, phenanthrene, and pyrene were bioavailable from the micellar phase of Triton X-100, although the degree of bioavailability decreased with increasing surfactant concentration (Guha et al. 1998). A model was constructed that could be used to determine optimal surfactant concentration for criteria including maximum rates of biodegradation. 3. There is evidence that, as for alkanes, biosurfactants may be produced during growth with PAHs (Déziel et al. 1996), although the practical implementation of this may be limited by the requirement of a suitable monomer such as glucose or mannitol for their synthesis. Pseudomomas aeruginosa GL1 that was part of a community that degraded PAHs, produced a rhamnolipid in the late stage of growth with glycerol or n-hexadecane and inhibited the growth of Bacillus cereus and Rhodococcus erythropolis (Arino et al. 1998). 4. The biodegradation of pyrene, chrysene, luoranthene, benz[a]anthracene, dibenz[a,h] anthracene, benzo[a]pyrene, and coronene by Stenotrophomonas maltophilia has been studied in the presence of a range of synthetic surfactants (Boonchan et al. 1998). Nonneutral surfactants were toxic, biodegradation was also inhibited by the neutral Igepal CA-630, and the positive enhancement of removal of substrates was generally low—in the range of 10%. 5. A comparison was made of the mineralization of 14C-luoranthene by two strains each of Mycobacterium sp. and Sphingomonas sp. (Willumsen et al. 1998). Triton X-100 decreased the rate of mineralization by the Mycobacterium strains, inhibited mineralization by Sphingomonas sp. strain EPA505, and diminished the survival of both Gram-negative strains during 50 h incubation. It is worth noting that the Sphingomonas strain EPA 505 is able to degrade a wide range of PAHs (Ye et al. 1996), and would therefore otherwise be a potential candidate for the bioremediation of PAH-contaminated sites. The differential effects of the neutral surfactants 2,2,4,4,6,8,8-heptamethylnonane and Triton X-100 on the formation of cis-dihydrodiols of naphthalene and phenanthrene by Pseudomonas sp. strain 9816/11 and Sphingomonas yanoikuyae strain B8/36 further illustrated the signiicance of both the organism and the structure of the surfactants (Allen et al. 1999). 6. During degradation of artiicial surfactants, the consumption of oxygen may, however, result in diminished PAH degradation (Tiehm et al. 1997), so that surfactants with lower biodegradability would be advantageous from this point of view.

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7. A lipoprotein surfactant is produced during growth of Pseudomonas marginalis strain PD-14B with succinate, and prevented locculation of cells in media containing anthracene, acenaphthylene, naphthalene, and chrysene (Burd and Ward 1996). 8. Increased removal of phenanthrene from soil columns spiked with the rhamnolipid mixture synthesized by Pseudomonas aeruginosa UG2 has been demonstrated, and shown to depend both on the increased desorption of the substrate and on partitioning into micelles (Noordman et al. 1998). However, the addition of the biosurfactant from the same strain of Pseudomonas aeruginosa UG2 or of sodium dodecyl sulfate had no effect on the rate of biodegradation of anthracene and phenanthrene from a chronically contaminated soil. At concentrations of sodium dodecyl sulfate >100 mg/kg, there was a marked inhibition of the degradation of luoranthene, pyrene, benz[a]anthracene, and chrysene (Deschênes et al. 1996). It was suggested that this was due to competition with the increasingly dominant surfactant-degrading microorganisms. This conclusion is supported by evidence that the addition of nonionic surfactants (alcohol ethoxylates) was more effective in enhancing biodegradation of PAHs in coal tar–contaminated soil than the more readily degradable glycoside surfactants (Madsen and Kristensen 1997). 9. The addition of a rhamnolipid biosurfactant produced by Pseudomonas aeruginosa stain AT10 apparently reduced the extent of degradation by endogenous bacteria of benz[a]anthracene and chrysene in a creosote-contaminated soil (Vinas et al. 2005). The relation between the type and concentration of surfactant and the stimulation of biodegradation is therefore complex, and has not so far been fully resolved (Burd and Ward 1996). There seems to be a consensus, however, that supplementation with surfactants is one of the factors that might enhance bioremediation of some contaminated sites (Walter et al. 1997). Some cardinal issues that are potentially negative include the following (Willumsen et al. 1998): • Diminished bioavailability of substrates from micelles • Toxicity or inhibition of biodegradation by some nonneutral synthetic surfactants as a result of surfactant-induced permeabilization of the cells • Toxicity as a result of the surfactant-enhanced PAH concentration in the aqueous phase • Adverse effect of surfactants on bacterial adhesion to surfaces in the matrix • Adverse effect of readily degraded surfactants that diminish the oxygen concentration available to the substrate-degrading organisms • The need to maintain a high density of the substrate-degrading organisms

SUPPLEMENTATION WITH FUNGI Some preliminary comments are given to provide perspective: a. It is important to emphasize that, in contrast to bacterial degradation of PAHs, many fungi carry out only transformation without ring ission. An important consequence is that demonstration of loss during bioremediation experiments is equivocal. A monooxygenase produces an epoxide that is either hydrolyzed to a trans-dihydrodiol or rearranged to a phenol that is often conjugated. It has been suggested that naphth-1-ol, which is one of the expected transformation products of naphthalene is the form in which at least part of naphthalene is associated with soil matrices (Burgos et al. 1996). b. The hydrogen peroxide that is required by white-rot fungi is produced by a range of reactions that include the activity of several oxidases and, in Ceriporiopsis subvermispora by manganese peroxide–dependent oxidation of glycolate and oxalate that are synthesized by the organism (Urzúa et al. 1998).

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c. Although considerable attention has been directed to the application of white-rot fungi, several important issues should be noted. Most attention has hitherto been given to species of Phanerochaete especially Ph. chrysosporium and Ph. sordida, although other species and other taxa (Field et al. 1992) may be of greater interest in view of their greater biodegradative capability. d. Whereas transformation has been demonstrated—often to quinones—only relatively low levels of mineralization to CO2 have frequently been observed, for example, in Pleurotus ostreatus (Bezalel et al. 1996a,b; Hofrichter et al. 1998). Illustrative examples of the application of fungi include the following: 1. The use of fungi has already been noted (Potin et al. 2004), although no analysis of putative metabolites was carried out. This is important since there has been considerable interest in the use of fungi in bioremediation programs, in which quinones may be produced as transient or terminal metabolites. For example, although anthracene-9,10-quinone is produced by Pleurotus ostreatus strain MUCL 29257 as a terminal metabolite from anthracene, it is only transiently formed by Phanerochaete chrysosporium strain DSM 1556 (Andersson and Henrysson 1996). In a study with spiked soil, transformation by Pleurotus ostreatus produced luorenone, benz[a]anthracene-7,12-quinone, and 4-hydroxyperinaphthenone (Andersson et al. 2003). White-rot fungi belonging to other taxa may, however, be more effective in mineralization. For example, Nematoloma frowardii mineralized 8.6% of the 14C-labeled phenanthrene supplied, although a substantial portion (46%) was associated with the mycelia (Sack et al. 1997; Hofrichter et al. 1998). A few examples of bioremediation using fungi are given as illustration. The supplementation of indigenous bacteria with Phanerochaete chrysosporium increased the loss of phenanthrene at a former oil gasiication site, although there was apparently a signiicant contribution to “polar metabolites” (Brodkorb and Legge 1992). Phenanthrene is not, however, representative of the toxicological proile of PAHs, although the presence of unidentiied metabolites may plausibly be interpreted as evidence of transformation. Application of the white-rot fungus Phanerochaete sordida to treat creosote-contaminated soil has been described, but again had limited success with PAHs having more than four rings (Davis et al. 1993). 2. Not only white-rot fungi have been examined, but comprehensive studies also have been made using Cunninghamella sp. (references in Sutherland et al. 1995). Experiments in microcosms supplemented with sources of inorganic nitrogen and phosphorus using the nonlignolytic fungus Cunninghamella echinulata var. elegans showed not only the expected loss of three- and four-ring PAHs but also partial loss of benzo[b]luoranthene and benzo[g,h,i]perylene (Cutright 1995). In this study, hydrogen peroxide was used as source of oxygen, although in natural systems the presence of bacteria with catalase activity would probably effectively destroy the hydrogen peroxide. 3. An important series of observations with a PAH-contaminated soil (May et al. 1997) showed that, although the fraction that was mineralized was low (ca. 2.5%), the PAHs were lost by polymerization processes mediated by the fungus. It was suggested that this was consistent with (a) the formation of pyrene-1,6-quinone and pyrene-1,8-quinone from pyrene (Hammel et al. 1986) and the 1,6-, 3,6-, and 6,12-quinones from benzo[a]pyrene by this organism (Haemmerli et al. 1986); (b) the tendency of quinones to polymerize and associate with soil humic material. The loss of the higher PAHs was highly variable, ranging from ca. 70% for benzo[b]luoranthene to ca. 5.5% for benzo[a]pyrene. 4. It is worth drawing attention to the signiicance of other issues. In natural ecosystems, other microorganisms including bacteria are almost always present and it has been shown that, in experiments using [7,10-14C]benzo[a]pyrene, incubation for 215 d with Bjerkandera sp. strain BOS55 alone resulted in the formation of 13.5% 14CO2 and 61% of labeled metabolites in the

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water phase. Addition of microbial cultures from forest soil at day 15 increased the 14CO2 evolution to 32% and reduced the water-soluble metabolites to 18% (Kotterman et al. 1998).

APPLICATION OF HIGHER PLANTS 1. The use of hybrid poplar (Populus deltoides × P. nigra) has been examined in a few investigations at sites contaminated with creosote. There are several issues that complicate the interpretation of these results, including the physical state of the contaminants, the mechanism of uptake from the soil, and translocation and metabolism in the plants. These have seldom been addressed in studies of PAHs. a. A push–pull study illustrated differences in respiration between sites that had been planted and those that had not, although data were not presented in terms of speciic PAH components (Pitterle et al. 2005). b. A 7-year study established a diminution in the PAH plume, although the major decline in speciic PAHs was limited primarily to naphthalene, and the occurrence of a dense liquid phase of creosote (Widdowson et al. 2005). 2. A site polluted for over 20 years with hydrocarbons was assessed for improvement using a range of plants, including grasses and legumes, some of them native species. The analysis combined mineralization of 13C-labeled naphthalene in the bulk soil and in the rhizosphere with the occurrence of genes speciic for dioxygenation of naphthalene (ndoB), alkane monooxygenation (alkB), and catechol 2,3-dioxygenase (xylE). Festuca arundinacea (Tall fescue) brought about an increase in the prevalence of the genes and mineralization of naphthalene in soil from the rhizosphere, whereas Trifolium hirtum (Rose clover) diminished both (Siciliano et al. 2003). There were several important conclusions: (a) aged contaminants were susceptible to plant-mediated degradation, (b) the results were plantspeciic, and (c) they revealed the signiicance of the rhizosphere.

ANOXIC OR ANAEROBIC ENVIRONMENTS At many sites, the subsurface environment will be anoxic or even anaerobic due to the activity of aerobic and facultatively anaerobic bacteria in the surface layers of the soil. It is therefore essential to take into consideration the extent to which anaerobic degradation may be expected to be signiicant. Reactions may take place under sulidogenic or methanogenic conditions, and the occurrence of sulfate at sites containing building material waste and the metabolic versatility of sulfate-reducing bacteria makes them particularly attractive. Hydrocarbons Hitherto, studies on the anaerobic degradation of aromatic hydrocarbons have been limited to monocyclic representatives—particularly toluene and xylenes. This issue has been discussed more fully in the context of benzene/toluene/ethylbenzene/xylene (BTEX) remediation in groundwater and the anaerobic degradation of monocyclic aromatic hydrocarbons. There is, however, evidence for the degradation of naphthalene and phenanthrene coupled to sulfate reduction under anaerobic conditions (Coates et al. 1996), and of naphthalene, phenanthrene, and pyrene under denitrifying conditions (McNally et al. 1998). It has been shown that the transformation of 2-methylnaphthalene and the cometabolism of benzothiophene and benzofuran are carried out under sulfate-reducing conditions with the formation of the polar carboxylates (Sainowski et al. 2006). These could therefore be used as markers for the occurrence of partial degradation in groundwater under anaerobic conditions in the presence of sulfate. Phenols The anaerobic degradation of phenol proceeds by carboxylation of phenyl phosphate, followed by dehydroxylation, and ission of the ring after partial reduction (Brackmann and Fuchs 1993).

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Degradation of o- (Bisaillon et al. 1991) and m-cresol (Roberts et al. 1990) has been observed under methanogenic conditions, and a summary of the possibilities under denitrifying conditions has been given (Rudolphi et al. 1991). An alternative pathway involving oxidation of the methyl groups under denitrifying conditions has also emerged (Bonting et al. 1995). Heteroarenes Although the anaerobic degradation of azaarenes containing several nitrogen atoms—particularly pyrimidines and purines—has been extensively studied, less is known about those with only a single heteroatom. Evidence for the loss of pyridine in sulfate-reducing and methanogenic aquifer slurries and of 2-methylpyridine in the former has been presented (Kuhn and Sulita 1989), although no details of the degradative pathways are available. Whereas indole and quinoline were degraded anaerobically under nitrate-reducing, sulfate-reducing, and methanogenic conditions, neither benzofuran nor benzothiophene were degraded (Licht et al. 1996).

ABIOTIC TRANSFORMATIONS Although this issue has not been frequently addressed, it is relevant to evaluating bioremediation. Several important issues emerged from a study using a range of three- and four-ring PAHs. 1. In contrast to the three-ring compounds, residues of benz[a]anthracene, chrysene, and benzo[a]pyrene were found after 15 weeks incubation in compost-amended soil. 2. Neither dihydrodiols formed by bacterial dioxygenation, nor phenols from fungal monooxygenation followed by rearrangement or hydrolysis and elimination, were found. 3. Whereas plausible fungal metabolites from anthracene, acenaphthylene, luorene, and benz[a]anthracene—anthracene-9,10-quinone, acenaphthene-9,10-dione, luorene-9-one, and benz[a]anthracene-7,12-quinone—were found transiently in compost-amended soil, these were formed even in sterile controls by abiotic reactions (Wischmann and Steinhart 1997). These results clearly illustrate the care that must be exercised in interpreting the occurrence of PAH oxidation products in bioremediation experiments as evidence of biological activity. All these factors should be carefully considered in the design and implementation of any bioremediation program. The rather pessimistic views presented above are supported by quoting the succinct conclusions of a study on PAH loss in laboratory microcosms using soil from a site contaminated with PAHs from a previous gas manufacturing facility (Erickson et al. 1993). a. PAHs were unavailable for microbial degradation and resistant to mineralization. b. The soils contained signiicant populations of bacteria that were not adversely affected by the toxicity of the contaminants. c. Addition of readily degradable naphthalene or phenanthrene did not improve degradation of the indigenous PAHs. d. PAHs were not leached into aqueous extracts from the soil. Since the indigenous microlora will have been exposed to the substrates, the relevant degradative pathways will often be present in populations of these microorganisms and induction of the appropriate degradative enzymes will have taken place. Indeed, many of the most versatile organisms have been isolated from heavily contaminated sites. If therefore, organisms with the relevant degradative capacity have been demonstrated, the prognosis for remediation is good. In contrast, although a mixed lora obtained by enrichment with creosote was able to degrade two- and three-ring PAHs, those with four or ive more rings including luoranthene that is a dominant component of creosote were unaltered (Selifonov et al. 1998). In addition, readily degradable carbon sources are probably

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counterproductive to maintaining the required degradative capacity, although addition of inorganic nutrients and provision of suitable oxygen concentrations and of water may be necessary. There are therefore several potentially serious problems that merit further critical investigation.

CONCLUSIONS There are several important conclusions that may be drawn from the results of these studies: 1. Determination of degradation by measurement of loss may be ambiguous since this fails to take into account transformation to metabolites. At ield sites, loss by other processes such as volatilization is dificult to assess, but may be inferred, for example, from low concentrations of the more volatile alkylnaphthalenes. The use of stable isotopes is discussed in Chapter 13. 2. The collective evidence suggests that although PAH components with less than four rings are probably lost, those with ive or more rings may be recalcitrant. 3. The presence of azaarenes—primarily quinolines, acridine, and carbazole—in creosote may inhibit or be incompatible with the degradation of PAHs. 4. The presence of high concentrations of phenols may have an adverse effect of the microlora as a result of their toxicity. 5. The extent to which bioavailability is a limiting factor and may be circumvented by addition of surfactants remains incompletely resolved. 6. The most serious limitation is probably the degree to which the substrates are accessible to the relevant microorganisms, while the advantage of adding surfactants is equivocal. 7. Oxygen limitation may be a seriously limiting factor especially in deep subsurface sites, and there is evidence that degradation in the solid phase is less effective than in slurries. 8. Supplementation with nitrogen and phosphorus may increase the total numbers of heterotropic organisms without necessarily improving degradation of PAHs. On the basis of these limitations, a cautious view of the effectiveness of bioremediation of PAHs seems justiied, and they should be taken into account in the design and strategy of bioremediation.

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May R, P Schröder, H Sandermann (1997) Ex-situ process for treating PAH-contaminated soil with Phanerochaete chrysosporium. Environ Sci Technol 31: 2626–2633. McNally DL, JR Mihelcic, DR Lueking (1998) Biodegradation of three- and four-ring polycyclic aromatic hydrocarbons under aerobic and denitrifying conditions. Environ Sci Technol 32: 2633–2639. Mueller JG, PJ Chapman, PH Pritchard (1989) Creosote-contaminated sites. Their potential for bioremediation. Environ Sci Technol 23: 1197–1201. Mueller JG, SE Lantz, BO Blattmann, PJ Chapman (1991a) Bench-scale evaluation of alternative biological treatment processes for the remediation of pentachlorophenol- and creosote-contaminated materials: solid-phase bioremediation. Environ Sci Technol 25: 1045–1055. Mueller JG, SE Lantz, BO Blattmann, PJ Chapman (1991b) Bench-scale evaluation of alternative biological treatment processes for the remediation of pentachlorophenol- and creosote-contaminated materials: slurry-phase bioremediation. Environ Sci Technol 25: 1055–1061. Noordman WH, W Ji, ML Briusseau, DB Janssen (1998) Effects of rhamnolipid biosurfactants on removal of phenanthrene from soil. Environ Sci Technol 32: 1806–1812. O’Loughlin EJ, SR Kehrmeyer, GK Sims (1996) Isolation, characterization, and substrate utilization of a quinoline-degrading bacterium. Int Biodet Biodeg 38: 107–118. Ogunseitan OA, BH Olson (1993) Effect of 2-hydroxybenzoate on the rate of naphthalene mineralization in soil. Appl Microbiol Biotechnol 38: 799–807. Pitterle MT, RG Andersen, MA Widdowson (2005) Push-pull tests to quantify in situ degradation rates at a phytoremediation site. Environ Sci Technol 39: 9317–9323. Potin O, C Rain, E Veignie (2004) Bioremediation of an aged polycyclic aromatic hydrocarbons (PAHs)contaminated soil by ilamentous fungi isolated from the soil. Int Biodet Biodeg 54: 45–52. Pradhan SP, JR Paterek, BY Liu, JR Conrad, VJ Srivastava (1997) Pilot-scale bioremediation of PAHcontaminated soils. Appl Biochem Biotechnol 63/65: 759–773. Ram NM, DH Bass, R Falotico, M Leahy (1993) A decision framework for selecting remediation technologies at hydocarbon-contaminated sites. J Soil Contam 2: 167–189. Roberts DJ, PM Fedorak, SE Hrudey (1990) CO2 incorporation and 4-hydroxy-2-methylbenzoic acid formation during anaerobic metabolism of m-cresol by a methanogenic consortium. Appl Environ Microbiol 56: 472–478. Rudolphi A, A Tschech, G Fuchs (1991) Anaerobic degradation of cresols by denitrifying bacteria. Arch Microbiol 155: 238–248. Sack M Hofrichter, W Fritsche (1997) Degradation of phenanthrene and pyrene by Nematoloma frowardii. J Basic Microbiol 4: 287–293. Sainowski M, C Griebler, RU Meckenstock (2006) Anaerobic cometabolic transformation of polycyclic and heterocyclic aromatic hydrocarbons: evidence from laboratory and ield studies. Environ Sci Technol 40: 4165–4173. Sandoli RL, WC Ghiorse, EL Madsen (1996) Regulation of microbial phenanthrene mineralization in sediment samples by sorbent-sorbate contact time, inocula and gamma irradiation-induced sterilization artifacts. Environ Toxicol Chem 15: 1901–1907. Schneider J, R Grosser, K Jayasimhulu, W Xue, D Warshawsky (1996) Degradation of pyrene, benz[a]anthracene, and benzo[a]pyrene by Mycobacterium sp strain RGHII-135, isolated from a former coal gasiication site. Appl Environ Microbiol 62: 13–19. Schwartz G, F Lingens (1994) Bacterial degradation of N-heterocyclic compounds. In Biochemistry of Microbial Degradation (Ed C Ratledge), pp. 459–486. Kluwer Academic Publishers, Dordrecht, The Netherlands. Selifonov SA, PJ Chapman, SB Akkerman, JE Gurst, JM Bortiatynski, MA Nanny, PG Hatcher (1998) Use of 13C nuclear magnetic resonance to assess fossil fuel biodegradation: fate of [1-13C]acenaphthene in creosote polycyclic aromatic compound mixtures degraded by bacteria. Appl Environ Microbiol 64: 1447–1453. Siciliano SD, JJ Germida, K Banks, CW Greer (2003) Changes in microbial community composition and function during a polyaromatic hydrocarbon phytoremediation ield trial. Appl Environ Microbiol 69: 483–489. Sutherland JB, F Raii, AA Kahn, CE Cerniglia (1995) Mechanisms of polycyclic aromatic hydrocarbon degradation. In Microbial transformation and degradation of toxic organic chemicals (Eds LY Young and CE Cerniglia), pp. 269–306. Wiley-Liss, New York. Thomas AO, JM Lester (1993) The microbial remediation of former gasworks sites, a review. Environ Technol 14: 1–24.

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Tiehm A, M Stieber, P Werner, FM Frimmel (1997) Surfactant-enhanced mobilization and biodegradation of polycyclic aromatic hydrocarbons in manufactured gas plant soil. Environ Sci Technol 31: 2570–2576. Urzúa U, PJ Kersten, R Vicuna (1998) Manganese peroxidase-dependent oxidation of glycolic and oxalic acids synthesized by Ceriporiopsis subvermispora produces extracellular hydrogen peroxide. Appl Environ Microbiol 64: 68–73. Vinas M, J Sabaté, MJ Espuny, AM Solanas (2005) Bacterial community dynamics and polycyclic aromatic hdrocarbon degradation during bioremediation of heavily creosote-contaminated soil. Appl Environ Microbiol 71: 7008–7018. Volkering F, AM Breure, JG van Andel, WH Rulkens (1995) Inluence of nonionic surfactants on bioavailability and biodegradation of polycyclic hydrocarbons. Appl Environ Microbiol 61: 1699–1705. Volkering F, AM Breure, WH Rulkens (1998) Microbiological aspects of surfactant use for biological soil remediation. Biodegradation 8: 401–417. Walter MV, EC Neilson, G Firmstone, DG Martin, MJ Clayton, S Simpson, S Spaulding (1997) Surfactant enhances biodegradation of hydrocarbons: microcosm and ield study. J Soil Contam 6: 61–77. Wang P, AE Humphrey, S Krawiec (1996) Kinetic analysis of desulfurization of dibenzothiophene by Rhodococcus erythropolis in continuous cultures. Appl Environ Microbiol 62: 3066–3068. Widdowson MA, S Shearer, RG Andersen, JT Novak (2005) Remediation of polycyclic aromatic hydrocarbon compounds in groundwater using poplar trees. Environ Sci Technol 39: 1598–1605. Widdowson MA, S Shearer, RK Andersen, JT Novak (2005) Remediation of polycyclic aromatic hydrocarbon compounds in groundwater using poplar trees. Environ Sci Technol 39: 1598–1605, Environ Sci Technol 39: 9317–9323. Willumsen PA, U Karlson, PH Pritchard (1998) Response of luoranthene-degrading bacteria to surfactants. Appl Microbiol Biotechnol 50: 475–483. Wilson SS, KC Jones (1993) Bioremediation of soil contaminated with polynuclear aromatic hydrocarbons PAHs, a review. Environ Pollut 81: 229–249. Wischmann H, H Steinhart (1997) The formation of PAH oxidation products in soils and soil/compost mixtures. Chemosphere 35: 1681–1698. Ye D, MA Siddiq, A Maccubbin, S Kumar, HC Sikka (1996) Degradation of polynuclear aromatic hydrocarbons by Sphingomonas paucimobilis. Environ Sci Technol 30: 136–142.

PART 3 WOOD PRESERVATION SITES: CHLOROPHENOLIC COMPOUNDS Creosote contamination has already been noted, and in this section only contamination with polychlorinated phenols—particularly pentachlorophenol—will be discussed. It should, however, be noted that commercial samples of pentachlorophenol also contain lower chlorinated congeners, and possibly chlorinated dibenzodioxins dibenzofurans. Concern with the production, use, and disposal of chlorophenols is motivated by their widely occurring toxic effects (Ahlborg and Thunberg 1980) and their possible persistence. The degradation of chlorophenols has been extensively investigated by a number of workers, and the pathways have been reviewed (Häggblom 1990). The application of speciic strains to remediation of a wood preservation site in Finland and elsewhere has been presented in detail (Häggblom and Valo 1995). Contamination of surrounding groundwater may also have occurred, and luidized-bed reactors inoculated with activated sludge from pulp mill producing chemothermomechanical pulp have been used to treat groundwater highly contaminated with chlorophenols. An important aspect of this study was that the organisms were fully functional at the relatively low temperature of 5–7°C (Järvinen et al. 1994). Evaluation of white-rot fungi for treatment of pentachlorophenol-contaminated soil has been made (Lamar and Dietrich 1990; Lamar et al. 1993), and two negative aspects have emerged: the production of the highly lipophilic pentachloroanisole and the association of the substrate with the soil matrix that presents a potentially serious problem. A pilot-scale study examined the possibility of injecting low-pressure steam beneath the surface, and it was suggested that desorption of pentachlorophenol resulted in its accessibility to treatment (Tse et al. 2001). Some general microbiological issues are briely summarized in addition to details that are given in Chapter 9, Part 2.

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AEROBIC BACTERIA The aerobic bacterial degradation of phenols with less than three chlorine atoms occurs by initial hydroxylation, followed by ring ission and elimination of chloride from the acyclic intermediates. For compounds with more than three chlorine atoms, a different mechanism has been elucidated for the degradation of pentachlorophenol by (a) Mycobacterium chlorophenolicum strain PCP1 (Apajalahti and Salkinoja-Salonen 1987a,b), (b) a strain of Flavobacterium sp. (Steiert and Crawford 1986; Xun et al. 1992), and (c) Sphingomonas chlorophenolica (Miethling and Karlson 1996). Details of the pathway can be found in a review (Häggblom 1990). In the application of such strains to bioremediation of contaminated sites, a number of important considerations should be considered. 1. The tolerance of the strains to high concentrations of pentachlorophenol—S. chlorophenolica appears to be less sensitive than M. chlorophenolicus (Miethling and Karlson 1996). This may be attributed to the ability of the cells to adapt their metabolism to avoid synthesis of toxic concentrations of chlorinated hydroquinones, and is consistent with the low levels of these metabolites measured in the cytoplasm of cells metabolizing pentachlorophenol (McCarthy et al. 1997). Inocula have also been immobilized on polyurethane that, in addition, ameliorates the toxicity of chlorophenols (Valo et al. 1990). 2. The longevity of the strains in the environment. This is dramatically illustrated from the observations that an initial inoculum of 108 cells/g of S. chlorophenolica fell to zero within 7 months, whereas 106 –107 cells/g of M. chlorophenolicum could be recovered from a similar inoculum after 7 months (Miethling and Karlson 1996). 3. There are important requirements that may be necessary, and an additional substrate may be required either to promote cell growth or to serve as a reductant. Degradation may be functional under low oxygen concentrations and be facilitated by the presence of straw compost (Laine and Jörgensen 1996). 4. Microbial O-methylation to chloroanisoles may occur, and under aerobic conditions these may be terminal metabolites. As a result of their lipophilic character they may be transported into higher biota and hence into the food chain via earthworms (Palm et al. 1991). The detection and persistence of Mycobacterium chlorophenolicum in soil that is a prerequisite for demonstrating its positive effect on biodegradation has been examined. This used 16S rRNA combined with polymerase chain reaction (PCR) (Briglia et al. 1996) that had a detection limit of ca. 3 × 102 cells/g. It should be noted that extensive investigations by Laine have shown the effectiveness of additives in facilitating the biodegradation of chlorophenols. For contaminated soils that already contain degradative microorganisms, however, the addition of an inoculum provided little or no additional advantage (Laine and Jörgensen 1997).

DEGRADATION BY FUNGI Both 2,4-dichlorophenol and 2,4,5-trichlorophenol can be degraded by the white-rot fungus Phanerochaete chrysosporium by a complex pathway that involves oxidative displacements of chloride and O-methylation with the formation of 1,2,4,5-tetrahydroxybenzene before ring ission (Valli and Gold 1991). Although pentachloroanisole is formed from pentachlorophenol by a number of species of Phanerochaete, it can subsequently be mineralized. The formation of products by oxidative coupling with loss of chloride mediated by laccase or peroxidase should also be noted (Dec and Bollag 1994). Fungal activity may also result in the formation of stable associations by reaction of xenobiotics and their metabolites with humic acids.

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ANAEROBIC DECHLORINATION Anaerobic dechlorination of halogenated phenols has been discussed in detail in Chapter 9, Part 2. It remains only to be noted that although dechlorination is a widespread reaction, it may represent merely a biotransformation and not ultimate degradation. Indeed partial dechlorination is extremely common. A review of anaerobic dechlorination has been given (Mohn and Tiedje 1992). Under these conditions—and in contrast to aerobic conditions—the more highly substituted compounds are more readily transformed. Partial anaerobic dechlorination of pentachlorophenol has been observed and, since the resulting chlorophenols are degradable under aerobic conditions complete mineralization may be accomplished under alternating anaerobic–aerobic conditions. Pure cultures of Desulfomonile tiedjei are able to carry out dechlorination, strain DCB-1 of polychlorinated phenols (Mohn and Kennedy 1992), and strain DCB-2 of 2,4,6-trichlorophenol and dichlorophenols (Madsen and Licht 1992). Desulitobacterium hafniense (frappieri) strain PCP-1 that was isolated from a methanogenic consortium can dechlorinate pentachlorophenol to 3-chlorophenol via 2,3,4,5-tetra-, 3,4,5-tri-, and 3,5-dichlorophenol (Bouchard et al. 1996). Reinoculation was, however necessary to achieve >95% removal with high concentrations of pentachlorophenol (Beaudet et al. 1998). In addition, this strain is able to dechlorinate a wide range of polychlorinated aromatic substrates including phenols, catechols, anilines, pentachloronitrobenzene (PCNB), and pentachloropyridine (Dennie et al. 1998).

CONCLUSION There is evidence for the success of bioremediation of chlorophenol-contaminated sites by on-site processes using a number of aerobic microorganisms as inocula, although their activity depended on a number of factors that should be investigated for each site (Miethling and Karlson 1996). However, advantage should be taken of indigenous microlora together with the addition of suitable sorbents. A relatively high degree of mineralization may be attained, although the possibly undesired formation of chloroanisoles could present a potential hazard, together with the fungal-catalyzed polymerization of chlorophenols. The extent to which this is applicable to chlorophenols containing methyl or nitro substituents is apparently unresolved.

REFERENCES Ahlborg UG, TM Thunberg (1980) Chlorinated phenols: occurrence, toxicity, metabolism, and environmental impact. CRC Crit Rev Toxicol 7: 1–35. Apajalahti JHA, MS Salkinoja-Salonen (1987a) Dechlorination and para-hydroxylation of polychlorinated phenols by Rhodococcus chlorophenolicus. J Bacteriol 169: 675–681. Apajalahti JHA, MS Salkinoja-Salonen (1987b) Complete dechlorination of tetrachlorohydroquinone by cell extracts of pentachlorophenol induced Rhodococcus chlorophenolicus. J Bacteriol 169: 5125–5130. Beaudet R, M-J Lévesque, R Villemur, M Lanthier, M Chénier, F Lépine, J-G Bisaillon (1998) Anaerobic biodegradation of pentachlorophenol in a contaminated soil inoculated with a methanogenic consortium, or with Desulitobacterium frappieri PCP-1. Appl Microbiol Biotechnol 50: 135–141. Bouchard B, R Beaudet, R Villemur, G MscSween, F Lépine, J-G Bisaillon (1996) Isolation and characterization of Desulitobacterium frappieri sp. nov., an anaerobic bacterium which reductively dechlorinates pentachlorophenol to 3-chlorophenol. Int J Syst Bacteriol 46: 1010–1015. Briglia M, RIL Eggen, WM de Vos et al. (1996) Rapid and sensitive method for the detection of Mycobacterium chlorophenolicum PCP-1 in soil based on 16S rRNA gene-targeted PCR. Appl Environ Microbiol 62: 1478–1480. Dec J, J-M Bollag, (1994) Dehalogenation of chlorinated phenols during oxidative coupling. Environ Sci Technol 28: 484–490. Dennie D, I Gladu, F Lépine, R Villemur, J-G Bisaillon, R Beaudet (1998) Spectrum of the reductive dehalogenation activity of Desulitobacterium frappieri PCP-1. Appl Environ Microbiol 64: 4603–4606. Häggblom M (1990) Mechanisms of bacterial degradation and transformation of chlorinated monoaromatic compounds. J Basic Microbiol 30: 115–141.

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Häggblom MM, RJ Valo (1995) Bioremedation of chlorophenol wastes. In Microbial transformation and Degradation of Toxic Organic Chemicals (Eds LY Young and CE Cerniglia), pp. 389–434. Wiley-Liss, New York. Järvinen KT, ES Melin, JA Puhakka (1994) High-rate bioremediation of chlorophenol-contaminated groundwater at low temperatures. Environ Sci Technol 28: 2387–2392. Laine MM, KS Jörgensen (1996) Straw compost and bioremediated soil as inocula for the bioremediation of chlorophenol contaminated soil. Appl Environ Microbiol 62: 1507–1513. Laine MM, KS Jörgensen (1997) Effective and safe composting of chlorophenol contaminated soil in pilot scale. Environ Sci Technol 30: 371–378. Lamar RT, DM Dietrich (1990) In situ depletion of pentachlorophenol from contaminated soil by Phanerochaete spp. Appl Environ Microbiol 56: 3093–3100. Lamar RT, JW Evans, J Glaser (1993) Solid-phase treatment of a pentachlorophenol-contaminated soil using lignin-degrading fungi. Environ Sci Technol 27: 2566–2571. Madsen T, D Licht (1992) Isolation and characterization of an anaerobic chlorophenol-transforming bacterium. Appl Environ Microbiol 58: 2874–2878. McCarthy DL, AA Claude, SD Copley (1997) In vivo levels of chlorinated hydroquinones in a pentachlorophenoldegrading bacterium. Appl Environ Microbiol 63: 1883–1888. Miethling R, U Karlson (1996) Accelerated mineralization of pentachlorophenol in soil upon inoculation with Mycobacterium chlorophenolicum PCP1 and Sphingomonas chlorophenolica RA2. Appl Environ Microbiol 62: 4361–4366. Mohn WW, JM Tiedje (1992) Microbial reductive dehalogenation. Microbiol Rev 56: 482–507. Mohn WW, KJ Kennedy, (1992) Reductive dehalogenation of chlorophenols by Desulfomonile tiedjei DCB-1. Appl Environ Microbiol 58: 1367–1370. Palm H, J Knuutinen, J Haimi, J Salminen, V Huhta (1991) Methylation products of chorophenols, catechols and hydroquinones in soil and earthworm of sawmill environments. Chemosphere 23: 263–267. Steiert JG, RL Crawford (1986) Catabolism of pentachlorophenol by a Flavobacterium sp. Biochem Biophys Res Commun 141: 1421–1427. Tse KKC, S-L Lo, JWH Wang (2001) Pilot study of in-situ thermal treatment for the remediation of pentachlorophenol-contaminated aquifers. Environ Sci Technol 35: 4910–4915. Valli K, MH Gold (1991) Degradation of 2,4-dichlorophenol by the lignin-degrading fungus Phanerochaete chrysosporium. J Bacteriol 173: 345–352. Valo RJ, MM Häggblom, MS Salkinoja-Salonen (1990) Bioremediation of chlorophenol containing simulated ground water by immobilized bacteria. Water Res 24: 253–258. Xun L, E Topp, CS Orser (1992) Conirmation of oxidative dehalogenation of pentachlorophenol by a Flavobacterium pentachlorophenol hydroxylase. J Bacteriol 174: 5745–5747.

PART 4 CHEMICAL WASTE The range of compounds in waste or in by-products from the production of chemical is enormous. It includes aliphatic and aromatic and heterocyclic compounds, some of which contain luorine, chlorine, bromine, nitro, sulfonate, or thiophosphate substituents. A useful structural listing of a wide range of chemicals has been compiled (Hartter 1985; Swoboda-Colberg 1995), and attention is drawn to two less-prominent groups containing the CF3 group, and organic iodine compounds such as the herbicide ioxynil and x-ray contrast agents. Chlorophenols have already been discussed and commercial chlorophenols may contain impurities including chlorinated dioxins and furans. Phenoxyalkanoic acid herbicides are discussed in the section on agrochemicals, and nitro compounds and phosphorothioate esters in later sections. The present discussion concentrates on halogenated aromatic and alicyclic hydrocarbons, although attention is directed also to other structural groups such as benzothiazoles (Reemtsma et al. 1995; Kumata et al. 1996) that have wide industrial application, although less is known of their biodegradability (De Vos et al. 1993). It should be emphasized that accumulation of by-products may present problems so that attention should not be conined to the manufactured product. Illustrative examples include (a) diphenyl sulfone as a by-product from the production of phenol by sulfonation of benzene followed by hydrolysis (Wick and Gschwend 1998), and (b) the diverse compounds containing chlorine and triluoromethyl substituents resulting from the production of 4-chloro-(triluoromethyl) (Jaffe and Hites 1985), which is noted later.

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CHLORINATED ALICYCLIC HYDROCARBONS Hexachlorocyclohexane (HCH) isomers were among the organochlorine contaminants at sites contaminated with previous pesticide production (Lang et al. 1992). Although evidence has been presented for the existence of a rich soil microlora at such sites, it appears that many of the substrates may remain even after 30 years (Feidieker et al. 1994). This suggests the existence of one or more limiting factors, of which the degree of bioavailability is probably of major signiicance, and is consistent with the established dificulty of chemical recovery of HCH from aged contaminated soil (Westcott and Worobey 1985). The situation is additionally complicated by the existence of various isomers of HCH (α,β,γ,δ) each of which behaves differently, and the existence of enantiomers of the α-isomer. The aerobic degradation of HCH isomers has been discussed in Chapter 9, Part 1. The degradation of γ-hexachloro[aaaeee]cyclohexane has been accomplished by several bacteria including Pseudomonas paucimobilis strain UT26 (Nagasawa et al. 1993), and involves a complex sequence of elimination, hydrolytic displacement of chlorine, and ring-ission reactions. It should be noted that the biotransformation to chlorobenzenes as terminal metabolites presents an undesirable alternative. The aerobic degradation of α-hexachloro[aaaaee]cyclohexane by indigenous bacteria in soil slurries has been demonstrated (Bachmann et al. 1988) and, was apparently limited by the rates of soil desorption and intraparticle mass transfer (Rijnaarts et al. 1990). Although the β-isomer (eeeeee) is highly persistent, its susceptibility to transformation under methanogenic conditions in a laboratory column reactor has been studied (Middeldorp et al. 1996). Chlorobenzene and benzene were terminal metabolites, plausibly produced from an intermediate δ-2,3,4,5-tetrachlorocyclohex1-ene. The anaerobic transformation of the structurally related γ-hexachlorocyclohexene and γ-1,3,4,5,6-pentachlorocyclohexene by Clostridium rectum produced 1,2,4-trichlorobenzene and 1,4-dichlorobenzene, respectively (Ohisa et al. 1980). Considerable attention has been directed to the highly toxic polychlorinated bornanes (toxaphene), and derivatives of hexachlorocyclopentadiene (chlordane) that were used as pesticides. Chlordane has been recovered from biota (Buser et al. 1992) and toxaphene components from sediments (Stern et al. 1996), so that these are highly persistent contaminants. For both, the commercial products contain a large number of congeners, and the analysis of chlordane is complicated additionally by the occurrence of enantiomers, some of which have undergone degradation and transformation after discharge. Toxaphene is a complex mixture of compounds prepared by chlorinating camphene, and contains several hundred polychlorinated bornanes. Although experiments with Sulfurospirillum (Dehalospirillum) multivorans have demonstrated partial dechlorination (Ruppe et al. 2003, 2004), only limited attention appears to have been directed to waste from locations at which these products were manufactured.

CHLORINATED AND BROMINATED AROMATIC HYDROCARBONS The structural range of industrially important representatives of these groups is enormous, and includes chlorobenzenes (solvents), polychlorinated biphenyls (PCBs) (hydraulic and insulating luids), and polybrominated biphenyls and diphenyl ethers (lame retardants). There is widespread concern over both the persistence and the potential toxicity of all these compounds, and sites that have become contaminated during their production represent a threat both to the environment and to human health. Pathways for the aerobic bacterial degradation of chlorobenzenes and chlorobiphenyls, and their brominated analogs have been discussed in Chapter 9, Part 1.

CHLOROBENZENES Although the possibly incompatible pathways for the degradation of chlorobenzene and toluene has been noted, a strain of Ralstonia sp. from a site contaminated with chlorobenzene contained the genes for both chlorocatechol degradation and the dioxygenase system for the degradation of benzene/toluene (van der Meer et al. 1998). The evolution of this strain resulted in a natural lowering

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in the groundwater concentration. Aerobic organisms capable of degrading chlorobenzenes with less than ive chlorine atoms have been described and the pathways elucidated: the metabolism can be initiated by dioxygenation without elimination of a chlorine atom from 1,2,4-trichlorobenzene or with elimination of a single chlorine atom from 1,2,4,5-tetrachlorobenzene (Sander et al. 1991). The possible application of the soluble methane monooxygenase of Methylosinus trichosporium to the bioremediation of 1,2,3-trichlorobenzene is attended by three negative factors: (a) the formation of the toxic 2,3,4- and 3,4,5-trichlorophenol, (b) the requirement of a substrate such as formate, and (c) the permanent inactivation of the cells by the substrate (Sullivan and Chase 1996). The anaerobic dechlorination of hexachlorobenzene has been described in anaerobic mixed cultures supplemented with electron donors including lactate, ethanol, or glucose (Holliger et al. 1992): successive and partial dechlorination produced 1,2,4- and 1,3,5-trichlorobenzenes, while the 1,2,3-trichlorobenzene was further dechlorinated. The partial dechlorination of 1,2,3,4-tetra-, 1,2,3,5-tetra-, and pentachlorobenzene has been examined in a methanogenic mixed culture using lactate as electron donor (Middeldorp et al. 1997), and sterile Rhine River sand was needed to maintain dechlorination activity for unresolved reasons.

DDT There has been renewed interest in DDT in spite of the fact that its use has been banned in many countries for several years. The degradation of DDT has been discussed in Chapter 7, Part 3, and attention has been directed to the apparently recalcitrant DDE (Quensen et al. 1998) and DDA (Heberer and Dünnbier 1999). Uptake and metabolism of p,p′-DDT and the isomeric o,p′-DDT have been examined in a range of plants, and the results illustrate a number of important issues. 1. One study used weathered contaminated soil that had been exposed to DDT for 3 years and had lain undisturbed since 1950 (Lunney et al. 2004). Three groups of plants were used, zucchini and pumpkin (Cucurbita pepo hybrids), alfalfa (Medicago sativa), and the grasses, tall fescue (Festuca arundinacea) and rye grass (Lolium multilorum), at two levels of exposure. Accumulation was greatest in the roots and shoots for both strains of Cucurbita pepo, whereas for the others accumulation was essentially restricted to the roots. The grasses are distinguished by the development of extensive root systems, whereas the Curcubita pepo have an extensive above-ground biomass and leaf surfaces that could have a positive effect in translocating the contaminant from the roots to the shoots. It was suggested that in addition, plant exudates might contribute to uptake. 2. The metabolism of DDT in aqueous solution was examined in the aquatic plant Elodea canadensis, and in stems and leaves of the perennial vine Pueraria thunbergiana (Garrison et al. 2000). Use of [14C]-labeled DDT conirmed the uptake of DDT that was strongly bound to the plant material. It was shown that DDT was transformed to DDD by reductive dechlorination, and signiicant aspects emerged: (a) the reaction took place with irradiated samples that contained no viable microorganisms, which were not therefore directly involved, and (b) dead plants of Elodea maintained reductive capability. It was concluded that the observed reduction was therefore abiotic, although it was dependent on some unknown factor that was present in the plants. This pathway of transformation to DDD in Elodea canadensis was conirmed in a study using the additional aquatic plants, duckweed (Spirodela oligorrhiza) and parrot feather (Mariophyllum aquaticum) (Gao et al. 2000).

POLYCHLORINATED BIPHENYLS There is an enormous literature on the degradation of PCBs, and it is not intended to attempt to cover this. The degradation of PCBs is exacerbated not only by the number of congeners, but by the fact that heavily ortho-substituted congeners occur in enantiomeric forms as a result of restricted

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rotation between the rings. Attention is directed to reviews on anaerobic dechlorination (Bedard and Quensen 1995), and to others that include a summary of aerobic degradation (Bedard 1990; Sylvestre 1995). The last also includes valuable comments on the regulation of PCB degradation and the signiicance of chlorobenzoate degradation. As a background to a discussion of bioremediation technologies, a few simplistic remarks are given here on the metabolic pathways used for the degradation of PCBs that has been discussed in detail in Chapter 9, Part 1. It should be emphasized that there are very considerable differences among the congeners in their susceptibility to degradation, in details of the mechanisms whereby this is accomplished, and among the various organisms. No attempt is, however, made to discuss here the details of these important differences. One important parameter is temperature, that is of particular signiicance for naturally occurring mixed cultures of organisms in the natural environment, since temperature may result in important changes in the composition of the microbial lora as well as on the rates. Some illustrative examples of the importance of temperature under both aerobic and anaerobic situations include the following: 1. An anaerobic sediment sample was incubated with 2,3,4,6-tetrachlorobiphenyl at various temperatures between 4 and 66°C (Wu et al. 1997). The main products were 2,4,6- and 2,3,6-trichlorobiphenyl and 2,6-dichlorobiphenyl: the irst of these was produced maximally and discontinuously at 12 and 34°C, the second maximally at 18°C, and the third was dominant from 25 to 30°C. Dechlorination was not observed above 37°C. 2. Sediment samples from a contaminated site were spiked with Arochlor 1242 and incubated at 4°C for several months (Williams and May 1997). Degradation by aerobic organisms in the upper layers of the sediment occurred with the selective production of di- and trichlorobiphenyls—although not in those at more than 15 mm below the surface. Some congeners were not found including the 2,6- and 4,4′-dichlorobiphenyls and a wider range of trichlorobiphenyls which were presumably further degraded. A number of aerobic organisms are able to degrade various congeners of PCB and has been discussed in Chapter 9, Part 1. Most have been isolated by enrichment with biphenyl as sole carbon and energy source. These include both Gram-negative strains belonging to the genera Alcaligenes and Pseudomonas, and Gram-positive strains of the genus Rhodococcus. Growth and the ability to carry out dechlorination may be accomplished by bacteria growing not only at the expense of biphenyl that was used for enrichment of the organisms, but also at the expense of typical plant metabolites that are noted in Chapter 12. In an ingenious application, the recovery of chlorobenzoates has been used to demonstrate aerobic degradation under natural conditions (Flanagan and May 1993). Protoanemonin can be formed from 4-chlorocatechol that is an intermediate in the degradation if 4-chlorobiphenyl (Blasco et al. 1995). This has an adverse effect on PCB-degrading bacteria in soil (Blasco et al. 1997), and may therefore present a signiicant problem in the bioremediation of PCB-contaminated sites. Conversely, naturally occurring compounds may be able to induce the enzymes for PCB metabolism. For example, effective degradation by cometabolism of a number of congeners in Arochlor 1242 was induced in Arthrobacter sp. strain B1B by the monoterpenoid carvone that was not used as a growth substrate, although it was toxic at high concentrations (>500 mg/L) (Gilbert and Crowley 1997). Other structurally related compounds of terpenes including limonene, p-cymene, and isoprene were also effective. Aerobic Conditions A valuable overview (Adriaens and Vogel 1995) includes a range of chlorinated aromatic compounds and provides illustrative engineering designs. In the light of the microbiological background that has already been presented, a number of different strategies can be distinguished. All of these have been applied to, and evaluated in contaminated soils or sediments.

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1. Contaminated soil has been inoculated with bacteria of established capacity for degradation of chlorobenzoates (Hickey et al. 1993). In the presence of added biphenyl, mineralization of PCBs was shown, although it was pointed out that there may exist incompatibility between the production of chlorocatechols from chlorobenzoates and their inhibition of dihydroxybiphenyl-2,3-dioxygenase that catalyzes the ring ission of many PCBs. 2. Experiments using Pseudomonas testosteroni strain B-356 in microcosm systems revealed the necessity of adding biphenyl to promote degradation of the tetrachlorinated congeners of Arochlor 1242, and the effectiveness of repeated inoculation (Barriault and Sylvestre 1993). 3. In situ stimulation of aerobic PCB degradation has been shown in Hudson River sediments (Harkness et al. 1993). Biodegradative capacity of the indigenous organisms was enhanced by the addition of biphenyl and inorganic nutrients, although repeated inoculation with an organism having established capability to degrade PCBs did not apparently improve the degree of biodegradation. 4. As for PAHs, attempts have been made to increase bioavailability by use of surfactants, and a complex picture has again developed (Fava and Di Gioia 1998). Triton-100 exerted both positive and negative effects: in soil slurries even though it was not metabolized by the soil microlora, it adversely affected the degradation of chlorobenzoate intermediates, whereas in ixed-bed reactors, depletion of PCBs was enhanced. 5. It is well established that the enzymes for the aerobic degradation of PCBs can be induced by biphenyl. Efforts have therefore been made to ind naturally occurring metabolites that would function as inducers, and whether plants are able to exert a beneicial effect. The putative role of terpenoids in inducing the degradation of PCBs has been noted in Chapter 9, Part 2 and Chapter 12. 6. An important study examined soil in the neighborhood of trees at a site historically contaminated with Arochlor 1260 (Leigh et al. 2006). Organisms able to degrade PCBs were isolated by sequential screening using biphenyl and 4-bromobiphenyl, followed by analysis for their ability to degrade PCBs. Highest numbers of PCB-degrading bacteria were found near mature stands of Pinus nigra (Austrian pine) and Salix caprea (willow). Strains with degradative activity comparable to that of Burkholderia xenovorans LB400 and Rhodococcus sp. strain RHA1 were found in soil from the willow. The most active strains displayed high similarities to Rhodococcus ruber, Rh. erythreus, and Pseudomonas frederiksbergensis, but activity was also found in strains of Williamsia and Luteibacter that have not hitherto been reported to degrade PCBs. These results clearly underscore the importance of plant metabolites in supporting the growth of bacteria with important degradative potential. Anaerobic Conditions Anaerobic dechlorination has been demonstrated under a number of conditions, and a complex pattern of dechlorination among the congeners has been observed (Bedard and Quensen 1995). There are also varying, and sometimes conlicting, views on the role of sulfate. 1. The anaerobic dechlorination of PCBs has been extensively studied both in microcosms and in ield samples from heavily contaminated sites in the United States. Three main patterns have been found—N that removed lanked meta-chlorines, P that removed para-chlorines, and LP that removed unlanked para-chlorines (Bedard et al. 1998). By contrast, ortho-chlorines were more recalcitrant. These experiments, which have been discussed in Chapter 9, Part 2, laid the foundation for analysis of a ield situation and an appreciation of the effect of long-term exposure of contaminated lake sediment (Magar et al. 2005a,b). Substantial dechlorination took place in buried sediment cores (35–40 cm) compared with the surface sediment cores (0–5 cm). Although there were some variations among the cores, the di- and trichlorinated biphenyls were produced at the expense of the

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more highly chlorinated congeners. There was preferential removal of meta- and parachlorine substituents, whereas the ortho-substituted congeners were essentially recalcitrant even after burial for 50 years, which was consistent with previous observations in laboratory experiments. Important conclusions were that (a) rates of dechlorination were substantially less than those expected on the basis of some laboratory experiments, and (b) sediments exposed near the surface were dechlorinated only to a very limited extent. 2. Anaerobic strategies are complicated by the different susceptibility of the various congeners to dechlorination and by the effect of electron acceptors especially sulfate. Ingenious alternatives have used addition of speciic PCB congeners that are more readily dechlorinated to “prime” dechlorination at speciic positions (Bedard and Quensen 1995), and the use of dibromo biphenyls in the presence of malate to stimulate dechlorination of the hexachloroto nanochlorobiphenyls (Bedard and Quensen 1995). The use of brominated biphenyls to induce dechlorination of highly chlorinated biphenyls has been systematically examined. Di- and tribromobiphenyls were the most effective in priming dechlorination including the hepta-, hexa-, and pentachloro congeners, and they were subsequently reduced to biphenyl (Bedard et al. 1998). 2,6-Dibromobiphenyl stimulated the growth of anaerobes that effectively dechlorinated hexa-, hepta-, octa-, and nanochlorobiphenyls over the temperature range from 8 to 30°C (Wu et al. 1999). Other compounds have been examined as “primers” for dechlorination of hexa- to nonachloro congeners (Deweerd and Bedard 1999). For example, 4-bromobenzoate was effective—though less so that 2,6-dibromobiphenyl—whereas the chlorobenzoates that are metabolites of aerobic degradation of PCBs were ineffective. The positive effect of brominated biphenyls in “priming” the anaerobic dechlorination of PCBs has also been encountered in the dechlorination of octachlorodibenzo[1,4]dioxin to the 2,3,7,8 congener that was induced by 2-bromodibenzo[1,4]dioxin (Albrecht et. al 1999).

POLYBROMINATED BIPHENYLS AND DIPHENYL ETHERS Highly brominated biphenyls and diphenyl ethers have been manufactured as lame retardants, and the diphenyl ethers have apparently become widespread environmental contaminants (references in Sellström et al. 1998). One reason for concern is the formation of polybrominated dibenzofurans and dibenzo[1,4]dioxins (though not 2,3,7,8-tetrabromodibenzo[1,4]dioxin) during subsequent incineration (Buser 1986). Mixed cultures of organisms isolated from sediments contaminated with PCBs and PBBs were shown to debrominate PBBs under anaerobic conditions (Morris et al. 1992), and the dominant congener—2,4,5,2′,4′,5′-hexabromobiphenyl—could be successively debrominated to 2,2′-dibromobiphenyl. In contrast, in sediments from the most heavily contaminated site containing contaminants in addition to PBBs, very little debromination occurred, and the recalcitrance was attributed to the toxicity of the other contaminants (Morris et al. 1993). Debromination of decabromodiphenyl ether has been described and, as for PCB, the rate was increased by the addition of primers (Gerecke et al. 2005). Octa- and nanobrominated congeners were produced, predominantly by loss of bromine at the meta and para positions, and not appreciably at the ortho position. An alternative procedure used two anaerobes that were able to dechlorinate chlorinated ethenes, and the results showed signiicant differences between them. One of them debrominated decabromodiphenyl ether to octa and hepta congeners, whereas the other that was unable to debrominate decabromodiphenyl ether, carried out debromination of the octa congeners to the hexa (154) and subsequently to the penta (99) and tetra (49) + tetra (47) congeners (He et al. 2006).

CHLORINATED DIBENZODIOXINS These are probably ubiquitous in the environment, and their biodegradability has been extensively examined. This will not be discussed in detail here, and attention will be drawn merely to a few investigations that illustrate important aspects.

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Chlorinated dioxins have been recovered from sediments contaminated with industrial discharge and from atmospheric deposition (Götz et al. 1993; Macdonald et al. 1992; Evers et al. 1993). Attention has been directed to anaerobic dechlorination processes (Beurskens et al. 1995; Adriaens et al. 1995). It has been suggested that microbial dechlorination of cell-partitioned 2,3,7,8tetrachlorodibenzo[1,4]dioxin in aged sediments was as effective as that in freshly spiked sediment (Barkovskii and Adriaens 1996). This suggests that the kinetics of transport into the cells is a cardinal determinant, although the extent to which hydrophobic xenobiotics in sediments are partitioned into the indigenous microlora has not been generally established. Chlorinated dioxins occur in atmospheric deposition (Koester and Hites 1992), and will thereby enter the terrestrial environment and watercourses. The degradation of tetrachloro- through octachlorodibenzo[1,4]dioxins has been examined in low-nitrogen medium by Phanerochaete sordida YK-624 (Takada et al. 1996). All the compounds were extensively degraded, and the ring ission of 2,3,7,8-tetra- and octachlorodibenzo[1,4]dioxin produced 4,5-di- and tetrachlorocatechol. These results established important evidence for the biodegradability of even highly chlorinated dibenzodioxins.

ORGANOFLUORO COMPOUNDS These have found a wide range of application including use as, for example, agrochemicals (Cartwright 1994), liquid crystals (Inoi 1994), luorine-containing dyes (Herd 1994; Engel 1994), plastics (Feiring 1994), elastomers (Logothetis 1994), and chemotherapeutic agents (Edwards 1994). The plethora of structures is a tribute to the ingenuity of the synthetic chemist, and both aliphatic and aromatic structures are widely represented. Examples include diphenyl ether herbicides containing the CF3 group (Lee et al. 1995), and luoroaromatic compounds used as pharmaceuticals such as the luoroquinolone carboxylic acids that are used in substantial amounts in large-scale animal husbandry (Nowara et al. 1997). A few examples of the existence of luorinated organic compounds are used as illustration of a problem area. 1. Sediments containing waste from the production of 4-chloro-(triluoromethyl)benzene contained a number of compounds containing both chlorine and triluoromethyl substituents. These included a benzophenone, a diluorodiphenylmethane, and several biphenyls (Jaffe and Hites 1985), although the more widespread occurrence of these compounds is unknown. This is important since, whereas pathways for the degradation of luorophenols and luorobenzoates are well established, the CF3 group appears to be resistant to both chemical and microbiological degradation. Microbial reactions brought about the degradation of 3- and 4-triluoromethylbenzoate to 7,7,7-triluoro-hepta-2,4-diene-6-one carboxylate that could, however, be degraded photochemically with the loss of luoride (Taylor et al. 1993). 2. A series of dibenzo[1,4]dioxins bearing nitro and triluoromethyl substituents in one ring and chlorine in the other was synthesized for comparison with impurities in commercial samples of the lampricide 3-triluoromethyl-4-nitrophenol, and to assess their ability to induce MFO activity (Hewitt et al. 1998). Although they appeared to be relatively weak inducers, there were other unidentiied components that were highly active. 3. Polyluorinated carboxylic acids and sulfonic acids have been used extensively, for example, in ire-retardant foams, as surfactants under extreme conditions, and as additives to fabrics and domestic products. What is more disturbing is their ubiquity in a wide range of environmental samples including humans. There is no evidence for their biodegradation, although photochemical procedures have been successful in bringing about their partial degradation (Hori et al. 2004a,b; 2005a,b).

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CONCLUSION There are a number of factors that contribute to the dificulty in the bioremediation of waste from chemical production. These include the enormous range of chemical structures and this is exacerbated by the frequent occurrence of structurally related compounds that have different susceptibilities to degradation. A major problem is exempliied by the complex mixture in commercial preparations of PCBs that includes not only a range of congeners but also polychlorinated terphenyls (Wester et al. 1996). In addition, most sites have been subjected to historical contamination so that aging that results in reduced bioavailability may present a serious problem. Although several strategies have been used, most often with bacteria, increasing interest has been directed to the use of plants. This is illustrated by PCBs where there is unequivocal evidence for successful bioremediation of PCBs. Current research is directed to understanding the basis of the biodegradability of speciic congeners, and to the possibility of developing strategies to overcome this. All these considerations apply to contaminants including PBBs, PCDDs, and aromatic compounds containing CF3 groups for which cardinal aspects of the basic microbiology remain to be developed.

REFERENCES Adriaens P, Q Fu, D Grbic-Galic (1995) Bioavailability and transformation of highly chlorinated dibenzo-pdioxins and dibenzofurans in anaerobic soils and sediments. Environ Sci Technol 29: 2252–2260. Adriaens P, TM Vogel (1995) Biological treatment of chlorinated organics. In Microbial transformation and Degradation of Toxic Organic Chemicals. (Eds LY Young and CE Cerniglia), pp. 435–486. Wiley-Liss, New York, USA. Albrecht ID, AL Barkovskii, P Adriaens (1999) Production and dechlorination of 2,3,7,8-tetrachlorodibenzop-dioxin in historically-contaminated estuarine sediments. Environ Sci Technol 33: 737–744. Bachmann A, P Walet, P, Wijnen, W de Bruin, JLM Huntjens, W Roelofsen, AJB Zehnder (1988) Biodegradation of alpha- and beta-hexachlorocyclohexane in a soil slurry under different redox conditions. Appl Environ Microbiol 54: 143–149. Barkovskii AI, P Adriaens (1996) Microbial dechlorination of historically present and freshly spiked chlorinated dioxins and diversity of dioxin-dechlorinating populations. Appl Environ Microbiol 62: 4556–4562. Barriault D, M Sylvestre (1993) Factors affecting PCB degradation by an implanted bacterial strain in soil microcosms. Can J Microbiol 39: 594–602. Bedard DL, (1990) Bacterial transformation of polychlorinated biphenyls. In Biotechnology and Biodegradation (Eds D Kamely, A Chakrabarty, GS Omenn), Vol. 4, pp. 369–388. Gulf Publishing Company, Houston. Bedard DL, H van Dort, KA Deweerd (1998) Brominated biphenyls prime extensive microbial reductive dehalogenation of Arochlor 1260 in Housatonic River sediment. Appl Environ Microbiol 64: 1786–1795. Bedard DL, JF Quensen (1995) Microbial reductive dechlorination of polychlorinated biphenyls. In Microbial Transformation and Degradation of Toxic Organic Chemicals (Eds LY Young, CE Cerniglia), pp. 127–216. Wiley-Liss, New York. Beurskens JEM, M Toussaint, J de Wolf, JMD van der Steen, PC Slot, LCM Commandeur, JR Parsons (1995) Dehalogenation of chlorinated dioxins by an anaerobic consortium from sediment. Environ Toxicol Chem 14: 939–943. Blasco R, M Mallavarapu, R-M Wittich, KN Timmis, DH Pieper (1997) Evidence that formation of protoanemonin from metabolites of 4-chlorobiphenyl degradation negatively affects the survival of 4-chlorobiphenyl-cometabolizing microorganisms. Appl Environ Microbiol 63: 427–434. Blasco R, R-M Wittich, M Mallavarapu, KN Timmis, DH Pieper (1995) From xenobiotic to antibiotic, formation of protoanemonin from 4-chlorocatechol by enzymes of the 3-oxoadipate pathway. J Biol Chem 270: 29229–29235. Buser H-R (1986) Polybrominated dibenofurans and dibenzo-p-dioxins: thermal reaction products of polybrominated diphenyl ether lame retardants. Environ Sci Technol 20: 404–408. Buser H-R, MD Müller, C Rappe (1992) Enantioselective determination of chlordane components using chiral high-resolution gas chromatography-mass spectrometry with application to environmental samples Environ Sci Technol 26: 1533–1540.

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Cartwright D (1994) Recent developments in luorine-containing agrochemicals. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 237–262. Plenum Press, London. De Vos DE, H De Wever, G Bryon, H Verachtert (1993) Isolation and characteristics of 2-hydroxybenzothiazole-degrading bacteria. Appl Microbiol Biotechnol 39: 377–381. Deweerd KA, DL Bedard (1999) Use of halogenated benzoates and other halogenated aromatic compounds to stimulate the microbial dechlorination of PCBs. Environ Sci Technol 33: 2057–2063. Edwards PN (1994) Uses of luorine in chemotherapy. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 501–541. Plenum Press, New York. Engel A (1994) Fluorine-Containing Dyes. B. Other luorinated dyestuffs. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 321–338. Plenum Press, New York. Evers EHG, HJC Klamer, RWPM Laane, HAJ Govers (1993) Polychlorinated dibenzo-p-dioxin and dibenzofuran residues in estuarine and coastal North Sea sediments Sources and distribution. Environ Toxicol Chem 12: 1583–1598. Fava F, D Di Gioia (1998) Effects of Triton X-100 and quillaya saponin on the ex situ bioremediation of a chronically polychlorobiphenyl-contaminated soil. Appl Microbiol Biotechnol 50: 623–630. Feidieker D, P Kämpfer, W Dott (1994) Microbiological and chemical evaluation of a site contaminated with chlorinated aromatic compounds and hexachlorocyclohexanes. FEMS Microbiol Ecol 15: 265–278. Feiring AE (1994) Fluoroplastics. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 339–372. Plenum Press, London. Flanagan WP, RJ May (1993) Metabolite detection as evidence for naturally occurring aerobic PCB degradation in Hudson River sediments. Environ Sci Technol 27: 2207–2212. Gao J, AW Garrison, C Hoehamer, CS Mazur, NL Wolfe (2000) Uptake and phytotransformation of o,p′-DDT and p,p′-DDT by axenically cultivated aquatic plants. J Agric Food Chem 48: 6121–6127. Garrison AW, VA Nzengung, JK Avanta, JJ Ellington, WJ Jones, D Rennels, NL Wolfe (2000) Phytodegradation of p,p′-DDT and the enantiomers of o,p′-DDT. Environ Sci Technol 34: 1663–1670. Gerecke AC, PC Hartmann, NV Heeb, H-PE Kohler, W Giger, P Schmid, M Zennegg, M Kohler (2005) Anaerobic degradation of decabromodiphenyl ether. Environ Sci Technol 39: 1078–1083. Gilbert ES, DE Crowley (1997) Plant compounds that induce polychlorinated biphenyl degradation by Arthrobacter sp strain B1B. Appl Environ Microbiol 63: 1933–1938. Götz R, P Friesel, K Roch, O Päpke, M Ball, M, A Lis (1993) Polychlorinated-p-dioxins PCDDs, dibenzofurans PCDFs, and other chlorinated compounds in the River Elbe: results on bottom sediments and fresh sediments collected in sedimentation chambers. Chemosphere 27: 105–111. Harkness MR, JB McDermott, DA Abramowicz, JJ Salvo, WP Flanagan, ML Stephens, FJ Mondello, RJ May, JH Lobos, KM Carroll, MJ Brennan, AA Bracco, KM Fish, GL Warner, PR Wilson, DK Dietrich, DT Lin, CB Morgan, WL Gately (1993) In situ stimulation of aerobic PCB biodegradation in Hudson River sediments. Science 259: 503–507. Hartter DR (1985) The use and importance of nitroaromatic compounds in the chemical industry. In Toxicity of Nitroaromatic Compounds (Ed DE Rickert), pp. 1–13. Hemisphere Publishing Corporation, Washington, DC. He J, KR Robrock, L Alvarez-Cohen (2006) Microbial reductive debromination of polybrominated diphenyl ethers (PBDEs). Environ Sci Technol 40: 4429–4434. Heberer T, U Dünnbier (1999) DDT metabolite bis(chlorophenyl)acetic acid; the neglected environmental contaminant. Environ Sci Technol 33: 2346–2351. Herd KJ (1994) Fluorine-containing dyes A Reactive dyes. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 287–314. Plenum Press, London. Hewitt LM, JH Carey, KR Munkittrick, JL Parrott, KR Solomon, MR Servos (1998) Identiication of chloronitro-triluoromethyl-substituted dibenzo-p-dioxins in lampricide formulations of 3-triluoromethyl4-nitrophenol: assessment to induce mixed function oxidase activity. Environ Toxicol Chem 17: 941–950. Hickey WJ, DB Searles, DD Focht (1993) Enhanced mineralization of polychlorinated biphenyls in soil inoculated with chlorobenzoate-degrading bacteria. Appl Environ Microbiol 59: 1194–1200. Holliger C, G Schraa, AJM Stams, AJB Zehnder (1992) Enrichment and properties of an anaerobic mixed culture reductively dechlorinating 1,2,3-trichlorobenzene to 1,3-dichlorobenzene. Appl Environ Microbiol 58: 1636–1644.

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Hori H, A Yamamoto, E Hayakawa, S Taniyasu, S Kutsuna, H Kiatagawa, R Arakawa (2005a) Eficient decomposition of environmentally persistent perluorocarboxylic acids by use of persulfate as a photochemical oxidant. Environ Sci Technol 39: 2383–2388. Hori H, A Yamamoto, S Kutsuna (2005b) Eficient photochemical decomposition of long-chain perluorocarboxylic acids by means of an aqueous/liquid CO2 biphasic system. Environ Sci Technol 39: 7692–7697. Hori H, E Hayakawa, H Einaga, S Kutsuna, K Koike, T Ibusuki, H Koatagawa, R Arakawa (2004a) Decomposition of environmentally persistent perluorooctanoic acid in water by photochemical approaches. Environ Sci Technol 38: 6118–6124. Hori H, E Hayakawa, K Koike, H Einaga, T Ibusuki (2004b) Decomposition of nonaluoropentanoic acid by heteropolyacid photocatalyst H3PW12O40 in aqueous solution. J Mol Cat A 211: 35–41. Inoi T (1994) Fluorinated liquid crystals. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 263–286. Plenum Press, New York. Jaffe R, RA Hites (1985) Identiication of new, luorinated biphenyls in the Niagara River Lake Ontario area. Environ Sci Technol 19: 736–740. Koester CJ, RA Hites (1992) Wet and dry deposition of chlorinated dioxins and furans. Environ Sci Technol 26: 1375–1382. Kumata H, H Takada, N Ogura (1996) Determination of 2-4-morpholinyl benzothiazole in environmental samples by a gas chromatograph equipped with a lame photometric detector. Anal Chem 68: 1976–1981. Lang E, H Viedt, J Egestorff, HH Hanert (1992) Reaction of the soil microlora after contamination with chlorinated aromatic compounds and HCH. FEMS Microbiol Ecol 86: 275–282. Lee HJ, MV Duke, JH Nirk, M Yamamoto, SO Duke (1995) Biochemical and physiological effects of benzheterocycles and related compounds. J Agric Food Chem 43: 2722–2727. Leigh MB, P Prouzová, M Macková, T Macek, DP Nagle, JS Fletcher (2006) Polychlorinated biphenyl (PCB)-degrading bacteria associated with trees in a PCB-contaminated site. Appl Environ Microbiol 72: 2331–2342. Logothetis AL (1994) Fluoroelastomers. In Organoluorine Chemistry Principles and Commercial Applications (Eds RE Banks, BE Smart, JC Tatlow), pp. 373–396. Plenum Press, London. Lunney AA, BA Zeeb, KJ Reimer (2004) Uptake of weathered DDT in vascular plants: potential for phytoremediation. Environ Sci Technol 38: 6147–6154. Macdonald RW, WJ Cretney, N Crewe, D Paton (1992) A history of octachlorodibenzo-p-dioxin, 2,3,7,8tetrachlorodibenzofuran, and 3,3′,4,4′-tetrachlorobiphenyl contamination in Howe Sound, British Columbia. Environ Sci Technol 26: 1544–1550. Magar VS, GW Johnson, RFC Brenner, JF Quensen, EA Foote, G Durell, JA Ickes, C Peven-Mccarthy (2005a) Long-term recovery of PCB-contaminated sediments at the Lake Hartwell superfund site: PCB dechlorination. 1. End-member characterization. Environ Sci Technol 39: 3538–3547. Magar VS, RFC Brenner, GW Johnson, JF Quensen (2005b) Long-term recovery of PCB-contaminated sediments at the Lake Hartwell superfund site: PCB dechlorination. 2. Rates and extent. Environ Sci Technol 39: 3548–3554. Middeldorp PJ, M Jaspers, AJB Zehnder, G Schraa (1996) Biotransformation of α−, β−, γ−, and δ-hexachlorocyclohexane under methanogenic conditions. Environ Sci Technol 30: 2345–2349. Middeldorp PJM, J de Wolf, AJB Zehnder, G Schraa (1997) Enrichment and properties of a 1,2,4-trichlorobenzene-dechlorinating microbial consortium. Appl Environ Microbiol 63: 1225–1229. Morris PJ, JF Quensen, JM Tiedje, SA Boyd (1992) Reductive debromination of the commercial polybrominated biphenyl mixture Firemaster BP6 by anaerobic microorganisms from sediments. Appl Environ Microbiol 58: 3249–3256. Morris PJ, JF Quensen, JM Tiedje, SA Boyd (1993) An assessment of the reductive debromination of polybrominated biphenyls in the Pine River reservoir. Environ Sci Technol 27: 1580–1586. Nagasawa S, R Kikuchi, Y Nagata, M Takagi, M Matsuo (1993) Aerobic mineralization of γ-HCH by Pseudomonas paucimobilis UT26. Chemosphere 26: 1719–1728. Nowara A, J Burhenne, M Spiteller (1997) Binding of luoroquinolone carboxylic acid derivatives to clay minerals. J Agric Food Chem 45: 1459–1463. Ohisa N, M Yamaguchi, N Kurihara (1980) Lindane degradation by cell-free extracts of Clostridium rectum. Arch Microbiol 125: 221–225. Quensen JF, SA Mueller, MK Jain, JM Tiedje (1998) Reductive dechlorination of DDE to DDMU in marine sediment microcosms. Science 280: 722–724. Reemtsma T, O Fiehn, G Kalnowski, M Jekel (1995) Microbial transformations and biological effects of fungicide-derived benzothiazoles determined in industrial wastewater. Environ Sci Technol 29: 478–485.

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Rijnaarts HHM, A Bachmann, JC Jumelet, AJB Zehnder (1990) Effect of desorption and intraparticle mass transfer on the aerobic biomineralization of alpha-hexachlorocyclohexane in a contaminated calcareous soil. Environ Sci Technol 24: 1349–1354. Ruppe S, A Neumann, E Braekevalt, GT Tomy, GA Stern, KA Maruya, W Vetter (2004) Anaerobic transformation of compounds of technical toxaphene. 2. Fate of compounds lacking geminal chlorine aroms. Environ Toxicol Chem 23: 591–598. Ruppe S, A Neumann, W Vetter (2003) Anaerobic transformation of compounds of technical toxaphene. I. Regiospeciic reaction of chlorobornanes with geminal chlorine aroms. Environ Toxicol Chem 22: 2614–2621. Sander P, R-M Wittich, P Fortnagel, H Wilkes, W Francke (1991) Degradation of 1,2,4-trichloro- and 1,2,4,5tetrachlorobenzene by Pseudomonas strains Appl Environ Microbiol 57: 1430–1440. Sellström U, A Kierkegaard, C de Witt, B Jansson (1998) Polybrominated diphenyl ethers and hexabromocyclododecane in sediment and ish from a Swedish river. Environ Toxicol Chem 17: 1065–1072. Stern GA, MD Loewen, BM Miskimmin, DCG Muir, JB Westmore (1996) Characterization of two major toxaphene components in treated lake sediment. Environ Sci Technol 30: 2251–2258. Sullivan JP, HA Chase (1996) 1,2,3-Trichlorobenzene transformation by Methylosinus trichosporium OB3b expressing soluble methane monooxygenase. Appl Microbiol Biotechnol 45: 427–433. Swoboda-Colberg NG (1995) Chemical contamination of the environment: sources, types, and fate of synthetic organic chemicals. In Microbial transformation and degradation of toxic organic chemicals (Eds LYYoung and CE Cerniglia), pp. 27–74. Wiley-Liss, New York. Sylvestre M (1995) Biphenyl/chlorobiphenyls catabolic pathway of Comamonas testosteroni B-356: prospect for use in bioremediation. Int Biodet Biodeg 35: 189–211. Takada S, M Nakamura, T Matsueda, R Kondo, K Sakai (1996) Degradation of polychlorinated dibenzo-pdioxins and polychlorinated dibenzofurans by the white rot fungus Phanerochaete sordida YK-624. Appl Environ Microbiol 62: 4323–4328. Taylor BF, JA Amador, HS Levinson (1993) Degradation of meta-triluoromethylbenzoate by sequential microbial and photochemical treatments. FEMS Microbiol Lett 110: 213–216. Van der Meer JR, C Werlen, SF Nishino, JC Spain (1998) Evolution of a pathway for chlorobenzene metabolism leads to natural attenuation in contaminated groundwater. Appl Environ Microbiol 64: 4185–4193. Westcott ND, BL Worobey (1985) Novel solvent extraction of lindane from soil. J Agric Food Chem 33: 58–60. Wester PG, J de Boer, UAT Brinkman (1996) Determination of polychlorinated terphenyls in aquatic biota and sediment with gas chromatography/mass spectrometry using negative chemical ionization. Environ Sci Technol 30: 473–480. Wick LY, PM Gschwend (1998) Source and chemodynamic behaviour of diphenyl sulfone and ortho- and para-hydroxybiphenyl in a small lake receiving discharges from an adjacent superfund site. Environ Sci Technol 32: 1319–1328. Williams WA, RJ May (1997) Low-temperature microbial aerobic degradation of polychlorinated biphenyls in sediment. Environ Sci Technol 31: 3491–3496. Wu Q, DL Bedard, J Wiegel (1997) Effect of incubation temperature on the route of microbial reductive dechlorination of 2,3,4,6-tetrachlorobiphenyl in polychlorinated biphenyl (PCB)-contaminated and PCB-free freshwater sediments. Appl Environ Microbiol 63: 2836–2843. Wu Q, DL Bedard, J Wiegel (1999) 2,6-Dibromobiphenyl primes extensive dechlorination of Arochlor 1260 in contaminated sediment at 8–30°C by stimulating growth of PCB-dehalogenating microorganisms. Environ Sci Technol 33: 595–602.

PART 5 AGROCHEMICALS As for waste from the production of chemicals, the array of structures represented by agrochemicals is truly enormous. Only some illustrative examples are provided, and it is important to emphasize that not only the original compound, but also potential metabolites should be considered. The pathways for biodegradation of many of the structures have been presented in Chapter 9 and reference should be made to these for details. There is increased interest in the degradation of agrochemicals after application, and abiotic reactions including photochemical degradation that are important on the soil surface are discussed in Chapter 1.

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PHENOXYALKANOIC ACIDS The pathway for their degradation that involves the intermediate formation of chlorophenols is well established, and several groups of organisms able to do so have been isolated. Kinetic parameters for the rate of degradation and for sorption of 2,4-dichlorophenoxyacetic acid (2,4-D) (Estrella et al. 1993) have been carried out, and showed higher values for the maximum growth rate constants in column experiments than in batch experiments. Experiments on the bioremediation of 2,4-Dcontaminated soil using Pseudomonas cepacia strain BRI 6001 were promising, and indicated the critical role of the cell density of the inoculum added to nonsterile soil (Comeau et al. 1993). However, the bacterial degradation of 2,4-D sorbed to sterile soil has been shown to be extremely slow (Ogram et al. 1985), and the rates in soil with a low organic content were greater than in an organic-rich soil (Greer and Shelton 1992). The biodegradation of phenoxypropion-2-oic acids is less widely established, and mecoprop [2-(2-methyl-4-chlorophenoxy)propionic acid] has consistently been found in municipal landill leachates (Gintautas et al. 1992). Whereas in pure cultures of bacteria, only one enantiomer of 2-(2-methyl-4-chlorophenoxy)propionic acid—the (S)-(–)enantiomer—may be degraded (Tett et al. 1994), in agricultural soil treated with a herbicide mixture containing 2-(2,4-dichlorophenoxy)propionic acid, both enantiomers were degraded with the opposite preference (Garrison et al. 1996). The same preference for degradation of racemic 2-(2-methyl4-chlorophenoxy)propionic acid was observed in Sphingomonas herbicidovorans by Zipper et al. (1996) who made the important observation that cells grown with either of the pure enantiomers preferentially degraded the corresponding enantiomer. Current formulations contain, however, only the biologically active and more readily biodegradable enantiomer. Additional comments on the enantiomerization of 2-phenoxypropionic acids (Buser and Müller 1997) have been given.

CHLORINATED ANILINES These are the starting compounds for production of a range of agrochemicals (insecticides, herbicides, and fungicides) including anilides, carbamates, and ureas. In addition, the chloroanilines produced by their hydrolysis are widely distributed, and are notorious for their association with and incorporation into humic substances (Bollag and Loll 1983). The mechanism of this interaction has been examined in model enzyme-mediated reactions with ferulic acid (Tatsumi et al. 1994), and it has been shown that oligomerization of 4-chloroaniline mediated by oxidoreductases may produce 4,4′-dichloroazobenzene and 4-chloro-4′-aminodiphenyl as well as trimers and tetramers (Simmons et al. 1987). These associations are also expected for the chlorinated anilines produced from the fungicide PCNB. From a purely microbiological view, there are some important additional issues. 1. Although aerobic bacteria that degrade monochloroanilines have been isolated, the biodegradation of dichloroanilines appears to be more exceptional (Brunsbach and Reineke 1993). In particular, the regulation of chloroaniline degradation should be taken into account, including the possible requirement for additional carbon sources. The anaerobic dechlorination of chloroanilines has been discussed in Chapter 9, Part 2, and the pathway for the anaerobic degradation of aniline itself is carried out by carboxylation followed by deamination. 2. Biotransformation to acetanilides has been demonstrated, although a strain of Pseudomonas putida stimulated by aniline was able to degrade 3,4-dichloroaniline (You and Bartha 1982). The formation of 3,3′,4,4′-tetrachloroazobenzene, 1,3-bis(3,4-dichlorophenyl)triazine, and 3,3′,4,4′-tetrachlorobiphenyl from 3,4-dichloroaniline by Escherichia coli in the presence of nitrate plausibly involves intermediate formation of the diazonium compound by reaction of the amine with nitrite (Corke et al. 1979). The chloroaniline component of lignin complexes is slowly mineralized by Phanerochaete chrysosporium, though as effectively as the free compound (Arjmand and Sandermann 1985). The mineralization of 3,4-dichloroaniline by P. chrysosporium proceeds sequentially by conjugation with 2-ketoglutaryl CoA to produce the amide and N-(3,4-dichloro)succinamide before

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mineralization (Sandermann et al. 1998). Negative aspects of fungal metabolism include (a) the transformation of 3,4-dichloroaniline by white-rot fungi (Pieper et al. 1992), which may produce the toxic 3,3′,4,4′-tetrachloroazobenzene that is absorbed from plant roots (Lee and Kyung 1995) and (b) facilitated association with humic and fulvic acids. 3. Chlorinated anilines are produced by the reduction of PCNB that is used as a fungicide against a variety of commercial crops. The transformation of PCNB has been examined with a methanogenic enrichment culture from contaminated sediment, although this contained neither PCNB nor its reduction product pentachloroaniline (PCNA). The culture not only reduced the initial PCNB, but also carried out sequential dechlorination to tetra-, tri-, dichloroanilines, and ultimately to 3- and 4-chloroaniline (Tas and Pavlostathis 2005). 4. The removal of 2,4-, 2,6-dichloroaniline, and 2,6-dichloro-4-methylaniline at an aged contaminated site was accomplished by the fungi Allescheriella sp., Stachybotrys, and Phlebia, although their ultimate fate was not determined (D’Annibale et al. 2006). PCNA was removed only by the second of these. 5. A strain that is able to degrade 2-chloro-N-isopropylacetanilide was successful in removing this from soil (Martin et al. 1995). It is notable that this strain was unable to grow with either aniline or phenol. The prognosis for bioremediation of residues containing polychlorinated anilines and their impurities is rather discouraging. Important factors include (a) limited biodegradability, (b) restricted bioavailability, and (c) the possible formation of oligomeric coupling products.

TRIAZINES 1,3,5-Triazines A number of substituted triazines are used as herbicides, and their biodegradation has been discussed in Chapter 10, Part 1. Treatment of soil contaminated with atrazine (2-chloro-4-(ethylamino)-6isopropylamino-1,3,5-triazine) illustrated a number of signiicant features. Although the soil that was used had the potential for degradation, a laboratory experiment with Pseudomonas sp. strain ADP that had an established potential for atrazine degradation revealed important limitations. There was a substantial decline in the numbers of Pseudomonas sp. strain ADP and only limited mineralization. Supplementation with citrate or succinate increased the survival of the strain, and successful mineralization was dependent on the preservation of a carbon/nitrogen ratio >10 (Silva et al. 2004). The last would apply generally to substrates with a low C/N ratio such as triazines. 1,2,4-Triazines The pathway for the degradation of metribuzin that has been used as a herbicide has been established, and attention has been directed to the occurrence of the metabolites in leachate from agricultural soil in Denmark. Although the parent metribuzin was not found, the metabolites produced by loss of the N-amino group and the thiomethyl groups were produced and contributed to groundwater contamination (Kjaer et al. 2005). 2,4-Dintro-6-sec-Butylphenol (Dinoseb) This was previously used as a herbicide, and attention has been directed to its degradation in storage areas or where it has been spilled. A strain of Clostridium bifermentans KMR-1 (that is protected by a U.S. patent) was unable to use dinoseb as carbon or energy source. In the presence of a starch extract, however, a low level of transformation was observed, and the products could subsequently be mineralized by aerobic bacteria (Hammill and Crawford 1996). These observations have been extended to the remediation of soil slurries from a contaminated site by adding phosphate and starch waste that achieved anaerobic conditions, and inoculation with a culture from a pilot-scale

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experiment. This treatment avoided the formation of undesirable polymeric compounds produced by partial reduction (Kaake et al. 1992; Roberts et al. 1993).

REFERENCES Arjmand M, H Sandermann (1985) Mineralization of chloroaniline/lignin conjugates and of free chloroanilines by the white-rot fungus Phanerochaete chrysosporium. J Agric Food Chem 33: 1055–1060. Bollag J-M, MJ Loll (1983) Incorporation of xenobiotics into soil humus. Experientia 39: 1221–1231. Brunsbach FR, W Reineke (1993) Degradation of chloroanilines in soil slurry by specialized organisms. Appl Microbiol Biotechnol 40: 402–407. Buser H-R, MD Müller (1997) Conversion reactions of various phenoxyalkanoic acid herbicides in soil. 2. Elucidation of the enantiomerization process of chiral phenoxy acids from incubation in a D2O/soil system. Environ Sci Technol 31: 1960–1967. Comeau Y, CW Greer, R Samson (1993) Role of inoculum preparation and density on the bioremediation of 2,4-d-contaminated soil by bioaugmentation. Appl Microbiol Biotechnol 38: 681–687. Corke CT, NJ Bunce, A-L Beaumont, RL Merrick (1979) Diazonium cations as intermediates in the microbial transformations of chloroanilines to chlorinated biphenyls, azo compounds and triazenes. J Agric Food Chem 27: 644–646. D’Annibale A, F Rosetto, F Federici, M Petruccioli (2006) Role of autochthonous ilamentous fungi in bioremediation of a soil historically contaminated with aromatic hydrocarbons. Appl Environ Microbiol 72: 28–36. Estrella MR, ML Brusseau, RS Maier, IL Pepper, PJ Wierenga, RM Miller (1993) Biodegradation, sorption, and transport of 2,4-dichlorophenoxyacetic acid in saturated and unsaturated soils. Appl Environ Microbiol 59: 4266–4273. Garrison AW, P Schmitt, O Martens, A Kettrup (1996) Enantiomeric selectivity in the environmental degradation of dichloroprop as determined by high-performance capillary electrophoresis. Environ Sci Technol 30: 2449–2455. Gintautas PA, SR Daniel, DL Macalady (1992) Phenoxyalkanoic acid herbicides in municipal landill leachates. Environ Sci Technol 26: 517–521. Greer LE, DR Shelton (1992) Effect of inoculant strain and organic matter content on kinetics of 2,4-dichlorophenoxyacetic acid degradation in soil. Appl Environ Microbiol 58: 1459–1465. Hammill TB, RL Crawford (1996) Degradation of 2-sec-butyl-4,6-dinitrophenol (Dinoseb) by Clostridium bifermentans KMR-1. Appl Environ Microbiol 62: 1842–1846. Kaake RH, DJ Roberts, TO Stevens, RL Crawford, DL Crawford (1992) Bioremediation of soils contaminated with the herbicide 2-sec-butyl-4,6-dinitrophenol (Dinoseb). Appl Environ Microbiol 58: 1683–1689. Kjaer J, P Olsen, T Henriksen, M Ullum (2005) Leaching of metribuzin metabolites and the associated contamination of a sandy Danish aquifer. Environ Sci Technol 39: 8374–8381. Lee JK, KS Kyung (1995) Uptake of 3,3′,4,4′-tetrachloroazobenzene soil residues by rice (Oryza sativa L.). J Agric Food Chem 43: 519–523. Martin M, E Ferrer, R Alonso, J Fernández (1995) Bioremediation of soil contaminated by propachlor using native bacteria. Int Biodet Biodeg 213–225. Ogram AV, RE Jessup, LT Ou, PSC Rao (1985) Effects of sorption on biological degradation rates of 2,4dichlorophenoxyacetic acid in soils. Appl Environ Microbiol 49: 582–587. Pieper DH, R Winkler, H Sandermann (1992) Formation of a toxic dimerization product of 3,4-dichloroaniline by lignin peroxidase from Phanerochaete chrysosporium. Angewandte Chemie 104: 60–61. Roberts DJ, RH Kaake, SB Funk, DL Crawford, RL Crawford (1993) Anaerobic remediation of dinoseb from contaminated soil. An on-site demonstration. Applied Biochemistry and Biotechnology – Part A Enzyme Engineering and Biotechnology 39–40: 781–789. Sandermann H Jr., W Heller, N Hertkorn, E Hoque, D Pieper, R Winkler (1998) A new intermediate in the mineralization of 3,4-dichloroaniline by the white rot fungus Phanerochaete chrysosporium. Appl Environ Microbiol 64: 3305–3312. Silva E, AM Fialho, I Sa-Correia, RG Burns, LJ Shaw (2004) Combined bioaugmentation and biostimulation to cleanup soil contaminated with high concentrations of atrazine Environ Sci Technol 38: 632–637. Simmons KE, RD Minard, J-M Bollag (1987) Oligomerization of 4-chloroaniline by oxidoreductases. Environ Sci Technol 21: 999–1003. Tas DO, SG Pavlostathis (2005) Microbial reductive transformation of pentachloronitrobenzene under methanogenic conditions. Environ Sci Technol 39: 8264–8272.

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Tatsumi K, A Freyer, RD Minard, J-M Bollag (1994) Enzyme-mediated coupling of 3,4-dichloroaniline and ferulic acid: a model for pollutant binding to humic materials. Environ Sci Technol 28: 210–215. Tett VA, AJ Willetts, HM Lappin-Scott (1994) Enantioselective degradation of the herbicide mecoprop [2-2methyl-4-chlorophenoxypropionic acid] by mixed and pure bacterial cultures. FEMS Microbiol Ecol 14: 191–200. You IS, R Bartha (1982) Stimulation of 3,4-dichloroaniline mineralization by aniline. Appl Environ Microbiol 44: 678–681. Zipper C, K Nickel, W Angst, H-PE Kohler (1996) Complete microbial degradation of both enantiomers of the chiral herbicide mecoprop [2-4-chloro-2-methylphenoxypropionic acid] in an enantioselective manner by Sphingomonas herbicidovorans sp. nov. Appl Environ Microbiol 62: 4318–4322.

PART 6 MILITARY WASTE EXPLOSIVES A wide range of nitro compounds has been used as military explosives, including nitrotoluenes, nitrate esters, and nitramines. There is concern over the destruction of these toxic and potentially explosive products, and considerable effort has been devoted to the development of microbiological processes of destruction (Kaplan 1990; Crawford 1995). Details of the degradation pathways of the relevant compounds have been given (Walker and Kaplan 1992), and general comments on the degradation of aromatic nitro compounds may be found in a review (Spain 1995a) and in a book (Spain 1995b). A review speciically devoted to 2,4,6-trinitrotolune is also available (Esteve-Núnez et al. 2001). Although the biodegradation of aromatic nitro compounds has been discussed in Chapter 9, Part 5, attention is drawn to the role of fungi (Bayman and Radkar 1997) including Phanerochaete chrysosporium (Bumpus and Tatarko 1994), and the signiicance of association between reduced metabolites and soil organic matter (Achnich et al. 1999; Thorn and Kennedy 2002). Compared with the wastes that have already been considered, these compounds like triazines are distinguished by a higher N/C ratio, so that although they may serve as sources of both carbon and nitrogen, when only the nitrogen is used by some organisms an additional carbon source must be added. The biodegradation of aromatic nitro compounds has already been discussed in Chapter 9, Part 5.

NITROARENES Only limited data are available on full- or pilot-scale operations, and the results from these may present an oversimpliied view. In general reduction to amines is the initial—and sometimes the only—transformation. 1. Indigenous microorganisms from a munitions-contaminated site reduced only a single nitro group of 2,4- and 2,6-dinitrotoluene (DNT), and 2,4,6-trinitrotoluene (TNT) to amines, while TNT was mineralized to ca. 10% (Bradley et al. 1994). A preliminary experiment using soil contaminated with both TNT and nitramines was carried out by adding phosphate and starch to the surface. The anaerobic lora that developed reduced the nitro groups of TNT, and subsequently the reduced compounds were removed though their fate was not established (Funk et al. 1993). One important additional observation was that under aerobic conditions or under anaerobic conditions at alkaline pH, polymerization of the intermediate amines took place. This experiment has since been extended to the evaluation of an in situ bioreactor (Funk et al. 1995). 2. Bioreactors containing an undeined anaerobic consortium reduced TNT to 2,4,6triaminotoluene (TAT) in the presence of glucose (Daun et al. 1998). The sorption of TAT to montmorillonite clay was irreversible, and the substrate could not be released by solvent extraction or by acid or alkaline treatment. Similar results were obtained with humic acids in which covalent reactions with carbonyl or activated C=C bonding presumably occurred. Results from laboratory experiments using 14C-labeled TNT in reactors to which

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molasses was added as carbon source, showed that after 9 weeks 83% of the radioactivity was recovered in soil components (humin, humic acids, and fulvic acids) (Drzyzga et al. 1998). In a full-scale application where sucrose was added to obtain anaerobic conditions, reduction of the nitro groups to amines was observed, followed by irreversible binding to the soil. Subsequent aerobic treatment was used to remove the sucrose and its fermentation products (Lenke et al. 1998). These results illustrate the cardinal issue of the association of metabolic products from TNT with soil components, and this in turn may substantially reduce the effectiveness of remediation. 3. Simultaneous degradation of 2,4- and 2,6-DNT has been achieved in a luidized-bed bioilm reactor (Lendemann et al. 1998) that was successfully operated with contaminated groundwater containing 2- and 4-nitrotoluenes and 2,4- and 2,6-DNTs. The nitrite that was produced during degradation was recovered as nitrate. 4. Partial reduction by clostridia has been demonstrated and has already been discussed in Chapter 9, Part 5. The effectiveness of clostridia in the anaerobic digestion of a number of nitroaromatics has prompted development of a procedure for the production of spores of Clostridium bifermentans, and a medium for their effective production has been developed (Sembries and Crawford 1997).

NITRODIPHENYLAMINES Although these are no longer used as explosives, they are formed from diphenylamine that is used as a stabilizer for nitrocellulose explosives. The metabolism of nitrodiphenylamines has been examined under anaerobic conditions, and phenazine and 4-aminoacridine that are cyclization products of the initially formed 2-aminodiphenylamine have been identiied (Drzyzga et al. 1996).

NITRATE ESTERS A review (White and Snape 1993) has been devoted to this topic, and only very brief comments need be added. The reductive biotransformation of glycerol trinitrate by strains of Bacillus thuringiensis/ cereus or Enterobacter agglomerans involves the expected successive loss of nitrite with formation of glycerol (Meng et al. 1995). The transformation of pentaerythritol tetranitrate by Enterobacter cloacae that used this as a source of nitrogen proceeded analogously, with further metabolism of the two hydroxymethyl groups to the dialdehyde (Binks et al. 1996). The enzymes that produce nitrite from the nitrate esters are reductases rather than hydrolases, and the enzyme from E. cloacae is strongly inhibited by steroids, and is capable of the reduction of cyclohex-2-ene-1-one (French et al. 1996). In a medium containing glucose and ammonium nitrate, glyceryl trinitrate is transformed by Penicillium corylophilum to the dinitrate and the mononitrate before complete degradation (Zhang et al. 1997.). In contrast, the metabolism of glyceryl trinitrate by Phanerochaete chrysosporium involves the production of the physiologically important nitric oxide (Servent et al. 1991).

NITRAMINES Of the nitramines used as explosives, greatest attention has been directed to the degradation of 1,3,5-trinitro-hexahydro-1,3,5-triazine (RDX) and octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX). RDX is degraded by several species of Enterobacteriaceae (Kitts et al. 1994), and is used by Stenotrophomonas sp. strain PB1 as a source of nitrogen with the production of metabolites formed by loss of two nitro groups and a single nitrogen atom from the triazine. Their structures were tentatively put forward (Binks et al. 1995), although an alternative anaerobic pathway involving reduction of the nitro groups to nitroso and a series of transformations yielding hydrazine, dimethylamine, and 1,2-dimethylhydrazine has been presented (McCormick et al. 1981). In addition to military uses, it should be noted that aromatic nitro compounds such as triluralin (2,6-dinitro-N,N-dipropyl-4-(triluoromethyl)aniline and dinoseb (2,4-dinitro-6-sec-butylphenol)

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have been used as herbicides, and parathion (O,O-diethyl-O-(4-nitrophenyl)phosphorothioate) as an insecticide. In addition, aromatic nitro compounds are of considerable industrial value for the production of the anilines (Hartter 1985) that are components of several agrochemicals.

CONCLUSIONS Although the possibility of bioremediation of sites contaminated with nitrotoluene waste is clearly possible, important issues should be clearly appreciated. These include (a) additional carbon sources may be necessary to accomplish partial or complete reduction of nitro groups, (b) under aerobic conditions, dimeric azo compounds may be formed as terminal metabolites, and (c) aromatic amines may be incorporated into humic material by covalent bonding and thereby resist further degradation.

CHEMICAL WARFARE AGENTS Brief notes are added on phosphoroluoridates even though their destruction by microbial activity— though clearly possible—is limited by their toxicity to the requisite microorganisms. One of the motivations for their inclusion is the fact that the hydrolytic enzyme(s) responsible for deluorination—organophosphorus acid anhydrase (OPA)—is widespread, and is found in a number of bacteria (Landis and DeFrank 1990). The microbial hydrolysis of organophosphorus pesticides and cholinesterase inhibitors is accomplished by several distinct enzymes, which are collectively termed organophosphorus acid anhydrases (OPAs). These have been reviewed (DeFrank 1991), so that only a few additional comments are necessary. The enzymes from Pseudomonas putida strain MG and Flavobacterium sp. (ATCC 27551) are carried on plasmids (Mulbry et al. 1986) and are membrane-bound. Although they hydrolyze a range of phosphorothioate esters at rates greatly exceeding those for chemical hydrolysis and have been proposed for application to destruction of these (Munnecke 1976), they hydrolyze phosphoroluoridates much more slowly (Dumas et al. 1989). This, together with the fact that they are membranebound makes them of somewhat limited attraction for the destruction of phosphoroluoridates. Two other enzymes have attracted attention for the hydrolysis of phosphoroluoridates: one from Bacillus stearothermophilus is also membrane-bound, whereas the other from Alteromonas sp. strain JD 6.5 is a soluble enzyme. OPA activity has also been observed in a number of other organisms (DeFrank et al. 1993). The enzyme designated OPA-2 has been puriied from Alteromonas strain JD 6.5, and has a molecular mass of 60 kDa (DeFrank and Cheng 1991). There has been considerable speculation on the natural substrate for OPA activity, and a surprising fact emerged from a detailed comparison of the amino acid sequence. This revealed a high degree of homology with an aminopeptidase from Escherichia coli and that the OPA anhydrase had high prolidase activity (Cheng et al. 1996). All these observations underscore the potential for application of appropriate OPAs to the destruction of organophosphorus compounds with anticholinesterase activity (Cheng and Calomiris 1996). However, since, hydrolysis results in release of luoride, the possibility of its subsequent incorporation into organic substrates to produce luoroacetate and 4-luorothreonine (Reid et al. 1995) may be worth consideration.

REFERENCES Achnich A, E Fernandes, J-M Bollag, H-J Knackmuss, H Lenke (1999) Covalent binding of reduced metabolites of [15N3]TNT to soil organic matter during a bioremediation process analyzed by 15N NMR spectroscopy. Environ Sci Technol 33: 4448–4456. Bayman P, GV Radkar (1997) Transformation and tolerance of TNT (2,4,6-trinitrotoluene) by fungi. Int Biodet Biorem 39: 45–53. Binks PR, CE French, S Nicklin, NC Bruce (1996) Degradation of pentaerythritol tetranitrate by Enterobacter cloacae PB2. Appl Environ Microbiol 62: 1214–1219.

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Binks PR, S Nicklin, NC Bruce (1995) Degradation of hexahydro-1,3,5-trinitro-1,3,5-triazine RDX by Stenotrophomonas maltophilia. PB1 Appl Environ Microbiol 61: 1318–1322. Bradley PM, FH Chapelle, JE Landmeyer, JG Schumacher (1994) Microbial transformation of nitroaromatics in surface soils and aquifer materials. Appl Environ Microbiol 60: 2170–2175. Bumpus JA, M Tatarko (1994) Biodegradation of 2,4,6-trinitrotoluene by Phanerochaete chrysosporium: identiication of initial degradation products and the discovery of a metabolite that inhibits lignin peroxidases. Curr Microbiol 28: 185–190. Cheng T-C, JJ Calomiris (1996) A cloned bacterial enzyme for nerve agent decontamination. Enz Microbiol Technol 18: 597–601. Cheng T-C, SP Harvey, GL Chen (1996) Cloning and expression of a gene encoding a bacterial enzyme for decontamination of organophosphorus nerve agents and nucleotide sequence of the enzyme. Appl Environ Microbiol 62: 1636–1641. Crawford RL (1995) The microbiology and treatment of nitroaromatic compounds. Curr Opinion Biotechnol 6: 329–336. Daun G, H Lenke, M Reuss, H-J Knackmuss (1998) Biological trearment of TNT-contaminated soil. 1. Anaerobic cometabolic reduction and interaction of TNT and metabolites with soil components. Environ Sci Technol 32: 1956–1963. DeFrank JJ (1991) Organophosphorus cholinesterase inhibitors: detoxiication by microbial enzymes. In Applications of Enzyme Biotechnology (Ed JW Kelly and TO Baldwin), pp. 165–180. Plenum Press, New York. DeFrank JJ, T-C Cheng (1991) Puriication and properties of an organophosphorus acid anhydrase from a halophilic bacterial isolate. J Bacteriol 173: 1938–1943. DeFrank JJ, WT Beaudry, T-C Cheng, SP Harvey, AN Stroup, LL Szafraniec (1993) Screening of halophiliuc bacteria and Alteromonas species for organophosphorus hydrolyzing enzyme activity. Chem-Biol Interact 87: 141–148. Drzyzga O, A Schmidt, K-H Blotevogel (1996) Cometabolic transformation and cleavage of nitrodiphenylamines by three newly isolated sulfate-reducing bacterial strains. Appl Environ Microbiol 62: 1710–1716. Drzyzga O, D Bruns-Nagel, T Gorontzy, K-H Blotevogel, E von Löw (1998) Incorporation of 14C-labeled 2,4,6-trinitrotoluene metabolites into different soil fractions after anaerobic and anaerobic-aerobic treatment of soil/molasses mixtures. Environ Sci Technol 32: 3529–3535. Dumas DP, JR Wild, FM Raushel (1989) Diisopropylluorophosphate hydrolysis by an organophosphate anhydrase from Pseudomonas diminuta. Biotechnol Appl Biochem 11: 235–243. Esteve-Núnez A, A Caballero, JL Ramos (2001) Biological degradation of 2,4,6-trinitrotoluene. Microbiol Mol Biol Rev 65: 335–352. French CE, S Nicklin, NC Bruce (1996) Sequence and properties of pentaerythritol tetranitrate reductase from Enterobacter cloacae PB2. J Bacteriol 178: 6623–6627. Funk SB, DJ Roberts, DL Crawford, RL Crawford (1993) Initial-phase optimization for bioremediation of munition compound-contaminated soils. Appl Environ Microbiol 59: 2171–2177. Funk SB, DL Crawford, RL Crawford, G Mead, W Davis-Hoover (1995) Full-scale anaearobic bioremediation of trinitrotoluene TNT contaminated soil. Appl Biochem Biotechnol 51/52: 625–633. Hartter DR (1985) The use and importance of nitroaromatic compounds in the chemical industry. In Toxicity of Nitroaromatic Compounds (Ed D Rickert), pp. 1–13. Hemisphere Publishing Corporation, Washington, DC. Kaplan DL (1990) Biotransformation pathways of hazardous energetic organo-nitro compounds. In Biotechnology and Biodegradation (Eds D Kamely, A Chakrabarty and GS Omenn), Vol. 4, pp. 155–181. Gulf Publishing Company, Houston. Kitts CL, DP Cunningham, PJ Unkefer (1994) Isolation of three hexahydro-1,3,5-trinitro-1,3,5-triazinedegrading species of the family Enterobacteriaceae from nitramine explosive-contaminated soil. Appl Environ Microbiol 60: 4608–4711. Landis WG, JJ DeFrank (1990) Enzymatic hydrolysis of toxic organoluorophosphate compounds. In Biotechnology and Biodegradation (Eds D Kamely, A Chakrabarty, GS Omenn), Vol. 4, pp. 183–201. Gulf Publishing Company, Houston, USA. Lendemann U, JC Spain, BF Smets (1998) Simultaneous biodegradation of 2,4-dinitrotoluene and 2,6-dinitrotoluene in an anerobic luidized-bed bioilm reactor. Environ Sci Technol 32: 82–87. Lenke H, J Warrelmann, G Daun, K Hund, U Sieglen, U Walter, H-J Knackmuss (1998) Biological treatment of TNT-contaminated soil. 2. Biologically induced immobilization of the contaminants and full-scale application. Environ Sci Technol 32: 1964–1971.

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McCormick NG, JH Cornell, AM Kaplan (1981) Biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine. Appl Environ Microbiol 42: 817–823. Meng M, W-Q Sun, LA Geelhaar, G Kumar, AR Patel, GF Payne, MK Speedie, JR Stacy (1995) Denitration of glycerol trinitrate by resting cells and cell extracts of Bacillus thuringiensis/cereus and Enterobacter agglomerans. Appl Environ Microbiol 61: 2548–2553. Microbiol Rev 45: 180–209. Mulbry WW, JS Karns, PC Kearney, JO Nelson, CS McDaniel, JR Wild (1986) Identiication of a plasmidborne parathion hydrolase gene from Flavobacterium sp. by Southern hybridization with opd from Pseudomonas diminuta. Appl Environ Microbiol 51: 926–930. Munnecke DM (1976) Enzymatic hydrolysis of organophosphate insecticides, a possible pesticide disposal method. Appl Environ Microbiol 32: 7–13. Preuss A, J Fimpel, G Diekert (1993) Anaerobic transformation of 2,4,6-trinitrotoluene (TNT). Arch Microbiol 159: 345–353. Reid KA, JTG Hamilton, RD Bowden, D O’Hagan, L Dasaradhi, MR Amin, DB Harper (1995) Biosynthesis of luorinated secondary metabolites by Streptomyces cattleya. Microbiology (UK) 141: 1385–1393. Sembries S, RL Crawford (1997) Production of Clostridium bifermentans spores as inoculum for bioremediation of nitroaromatic contaminants. Appl Environ Microbiol 63: 2100–2104. Servent D, C Ducrorq, Y Henry, A Guissani, M Lenfant (1991) Nitroglycerin metabolism by Phanerochaete chrysosporium: evidence for nitric oxide and nitrite formation. Biochim biophys Acta 1074: 320–325. Spain JC (1995a) Biodegradation of nitroaromatic compounds. Annu Rev Microbiol 49: 523–555. Spain JC (Ed) (1995b) Biodegradation of Nitroaromatic Compounds. Plenum Press, New York. Thorn KA, KR Kennedy (2002) 15N NMR investigation of the covalent binding of reduced TNT amines to soil humic acid, model compounds, and lignocellulose. Environ Sci Technol 36: 3787–3796. Walker JE, DL Kaplan (1992) Biological degradation of explosives and chemical agents. Biodegradation 3: 369–385. White GF, JR Snape (1993) Microbial cleavage of nitrate esters, defusing the environment. J Gen Microbiol 139: 1947–1957. Zhang YZ, ST Sundaram, A Sharma, BW Brodman (1997) Biodegradation of glyceryl trinitrate by Penicillium corylophilum Dierckx. Appl Environ Microbiol 63: 1712–1714.

PART 7 GROUNDWATER CONTAMINATION BENZENE/TOLUENE/ETHYLBENZENE/XYLENES These compounds along with trimethylbenzenes are components of automobile gasoline, and may enter aquatic systems and eventually groundwater through spillage at illing stations, leakage from underground storage tanks, or during transport. Aerobic Conditions All these substrates can be degraded under aerobic conditions and, although there appear to be important differences among the xylene isomers and mutant strains have been isolated that can degrade all three isomers (Di Lecce et al. 1997). Reviews have covered various aspects of this problem: 1. Biodegradation in gas-condensate-contaminated groundwater with emphasis of the role of inorganic nutrients and oxygen (Morgan et al. 1993) 2. Determinative factors for treating aquifer plumes after accidental spillage of automobile fuel with discussions on the design of systems, and the role of the indigenous microlora (Salanitro 1993) 3. General procedures including the provision of oxygen and comments on anaerobic treatment (Bowlen and Kosson 1995) The pathways for the aerobic biodegradation of alkylated benzenes have been elucidated in extensive investigations and have been discussed in Chapter 8, Part 1, so that only salient features are briely summarized here. The genes for the degradation of toluene may be either chromosomal or

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plasmid-borne. The latter may, therefore be lost in the absence of selection pressure. The degradation of toluene may occur by different pathways: 1. Dioxygenation or successive monooxygenation of the substrate, with subsequent ring ission leaving the alkyl group intact 2. Oxidation of the alkyl group to a carboxylic acid before ring ission. For xylenes, it appears that there are signiicant differences in the degradability of the isomers, o-xylene being apparently more recalcitrant The results of laboratory experiments with luidized-bed reactors treating toluene-contaminated inluent (Massol-Deyá et al. 1997) came to important conclusions: 1. Toluene-degrading strains in the bioilm were displaced by groundwater organisms from a putatively pristine source. 2. These organisms were able to establish a stable microbial community and were able to bring about a decrease in toluene concentration in the efluent from 0.140 to 0.063 mg/L. These results clearly show the advantage and desirability of using indigenous organisms under appropriate conditions, and that they may effectively degrade relatively low substrate concentrations. The latter is consistent with the ability of bacteria in natural aquatic systems to utilize low substrate concentrations, which has been noted in Chapter 4. An experiment on toluene biodegradation under ield and laboratory conditions provided results of value in the design of laboratory simulation experiments, and illustrated the caution required in assessing the fate of contaminants. Experiments were carried out under three conditions: (i) in low-through horizontal columns containing sediment and rocks, (ii) in shaking cultures containing sediments, rocks, or plant material, and (iii) in situ in a contaminated stream (Cohen et al. 1995). There were a number of important conclusions: a. The rates of biodegradation observed in the shake-lask experiment more closely paralleled those from the in situ experiment than those using the low-through column system b. Biodegradation took place on streambed surfaces particularly on rocks, so that the formation of bioilms was essential c. Conversion into CO2 was incomplete, and 15% of the substrate was converted into soluble metabolites, and 62% to biomass or insoluble material Consistent with this, it was observed that, during the metabolism of 14C-labeled BTEX although the substrates were mineralized to ca. 70%, ca. 20% of the label in toluene and ca. 30% in o-xylene were found in humus. It was suggested that the alkylated catechol metabolites might plausibly be responsible for this association (Tsao et al. 1998). The effect of increased oxygen was examined in contaminated groundwater (Gibson et al. 1998). Oxygen was supplied by diffusion from silicone tubing to areas within the plume that were oxygen-deicient due to the activity of indigenous bacteria. The rate of aerobic BTEX degradation increased at the expense of anaerobic degradation, and resulted in the degradation of both benzene and ethylbenzene that are generally less readily degraded under anaerobic conditions. Anoxic or Anaerobic Conditions In many situations, such as in deep groundwater, oxygen concentration may be severely limiting due to its consumption by suricial aerobic organisms, or its low rate of transport into the system. Therefore, there has been great interest in the anaerobic degradation of BTEX. Although this has been

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demonstrated for benzene under anaerobic conditions by methanogenic consortia, sulfate-reducing bacteria, and Fe(III)-reducing bacteria, greatest attention has been directed in laboratory studies to the anaerobic degradation of toluene in the presence of nitrate. This is supported by the fact that the appropriate organisms are widely distributed (Fries et al. 1994). Some of the important principles may be illustrated from two groups of experiments. The irst used a laboratory microcosm and a ield experiment with a contaminated aquifer (Barbaro et al. 1992). Although the results clearly showed the effectiveness of adding nitrate, there were signiicant differences in the extent to which the substrates were degraded: for example, benzene appeared recalcitrant, and the xylenes and ethyl benzene were less degradable than toluene. Nitrate was apparently consumed by indigenous organisms at the expense of other carbon substrates, so that this was effectively removed from the system. In this experiment—and possibly in general—sorption of these substrates to organic carbon was not a limiting factor. In the second example, the effect of nitrate or sulfate additions was examined by adding either of these, together with samples of BTEX to a contaminated aquifer in the form of “slugs” of puriied groundwater (Reinhard et al. 1998). For nitrate additions, the rates of removal of the substrates were in the order benzene < o-xylene < ethylbenzene < toluene = m-xylene, the last three being removed within 6 d. For sulfate additions, removal of toluene and all the xylenes occurred within 50 d. Metabolites characteristic of degradation (Beller et al. 1995) were isolated as conirmation of biotransformation. In the interpretation of such results, several important considerations should be taken into account in the application of this procedure. a. Although the results (Beller et al. 1995) were broadly in agreement with those from laboratory microcosm experiments, the rates of degradation of toluene and m- and p-xylenes seemed to be lower. Benzene and o-xylene seem to be considerable more recalcitrant than other components of BTEX. b. In an aquifer that was contaminated with BTEX, it has been shown that the methylbenzylsuccinates arising from xylenes were present, although benzylsuccinate, which would be expected from the toluene that was present was not observed. This was presumed to have undergone further degradation in the aquifer (Beller 2002). The application of deuterated toluene in assessing anaerobic biodegradation (Fischer et al. 2006) has already been noted in Chapter 6, Part 1. A review (Lovley 1997) has summarized the various strategies and suggests that uncertainties, particularly in the bioremediation of benzene, can only be resolved by greater emphasis on ield-oriented studies, and a better understanding of the reactions involved and the factors that limit the rates of degradation. These experiments should be viewed against the results of extensive laboratory investigations of the anaerobic degradation and transformation of the individual components of BTEX. The degradation of ethylbenzene and n-propylbenzene—though not xylenes—has been shown in pure cultures of denitrifying bacteria (Rabus and Widdel 1995). In crude oil, toluene, ethylbenzene, and m-xylene were degraded, though neither o-xylene nor p-xylene (Rabus and Widdel 1996). Degradation of toluene by the sulfate-reducing anaerobe Desulfobacula toluolica has been shown (Rabus et al. 1993), and by another sulfate-reducing bacterium with a novel 16S rRNA gene sequence (Beller et al. 1996). The mechanism of these anaerobic degradations is complex and reviews have been given by some of the pioneers in this area (Evans and Fuchs 1988; Fuchs et al. 1994). It is important to note that benzylsuccinates and benzylfumarates have been proved to be intermediates during the oxidation of alkylbenzenes to carboxylates (Biegert et al. 1997; Beller and Spormann 1997). As noted above, these compounds together with the analogous compounds that would be produced from xylenes have been used in support of the active in situ anaerobic degradation of toluene and xylenes (Beller et al. 1995, Beller 2002). In addition, the potential for application of the analogous carboxylates of naphthalene, benzothiophene, and benzofuran has been suggested (Sainowski et al. 2006).

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HALOGENATED ALKANES AND ALKENES Tetrachloromethane The degradation of tetrachloromethane by Pseudomonas stutzeri strain KC involves hydrolysis to CO2 by a mechanism involving the naturally produced pyridine-2,6-dithiocarboxylic acid (Lewis et al. 2001): details have already been discussed in Chapter 7, Part 3. This organism was used in ield evaluation at a site at which the indigenous lora was ineffective, and acetate was used as electron donor (Dybas et al. 2002). One novel feature was inoculation at a series of wells perpendicular to the established low of the groundwater plume. Effective removal of tetrachloromethane was sustained over a period of 4 years, and transient levels of chloroform and H2S disappeared after reducing the concentration of acetate. Chloroethenes Tetrachloroethene (TeCE; perchloroethene [PCE]) and trichloroethene (TCE) have been used extensively as solvents and degreasing agents, and substantial effect has been devoted to the bioremediation of contaminated groundwater. Determinative issues are the relatively low substrate concentrations combined with the large volumes of groundwater that are involved. Remediation is made more dificult by the high density and poor water solubility of chlorinated ethenes, and the possibility of improvement by using cyclodextrin to enhance solubility has been examined for a TeCE-contaminated aquifer (Tick et al. 2003). There has therefore been greater interest in the application of in situ procedures than in more conventional “pump and treat” on-site methods. To appreciate the microbiology of the procedures, a brief summary of the relevant aspects is given. Reviews provide additional details (Ensley 1991; Arp 1995), and relevant details of the reactions have already been given. A valuable review (Lee et al. 1998) includes a discussion of microbial processes, and provides illustrative examples of both in situ and natural attenuation. An overview of possible procedures has been given (Stroo et al. 2003). Aerobic Conditions TCE is not able to support the growth of a single organism, but it is susceptible to cooxidation by oxygenases elaborated by organisms during growth with structurally unrelated substrates. A review of methanotrophic bacteria (Hanson and Hanson 1996) contains a useful account of their application to bioremediation of TCE-contaminated sites. There are several bacterial oxygenases that can bring about cooxidation of TCE after induction with the relevant substrates: methane monooxygenase in Methylosinus trichosporium strain OB3b (Jahng and Wood 1994), propane monooxygenase in Mycobacterium vaccae (Vanderberg et al. 1995), and ammonia monooxygenase (Arciero et al. 1989; Vannelli et al. 1990). Although the methane monooxygenase system involves an epoxide intermediate that may form CO and toxiies the organism, this may be overcome by addition of a suitable reductant such as formate (Henry and Grbic-Galic 1991). An alternative strategy is the intermittent provision of substrate TCE (Walter et al. 1997). Pseudomonas putida strain F1 elaborates a dioxygenase for the degradation of toluene, and this is able to cooxidize TCE that may also be carried out by growth with phenol (Nelson et al. 1988). A similar situation prevails for the isopropylbenzene-degrading Rhodococcus erythropolis strain BD-2 (Dabrock et al. 1994). Increased biodegradation of TCE has also been observed in a constructed strain of Escherichia coli carrying the genes for the large subunit of toluene terminal oxygenase (from Pseudomonas putida F1), the small subunit of biphenyl terminal oxygenase, and the ferredoxin and ferredoxin reductase (from P. pseudoalcaligenes KF707) (Furukawa et al. 1994). Monooxygenase systems may also be involved in the degradation of toluene and bring about the cooxidation of TCE under suitable growth conditions. P. cepacia strain G4 carries out ortho hydroxylation,

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P. mendocina KR-1 carries out para hydroxylation, and Ralstonia (Pseudomonas) pickettii carries out para hydroxylation, although it was originally reported to carry out meta hydroxylation. The complexity introduced by exposure of an established mixed culture growing with a single substrate to an alternative cosubstrate is illustrated by the following. A stable mixed culture of Pseudomonas putida mt-2, P. putida F1, P. putida GJ31, and Burkholderia cepacia G4 growing with limited concentrations of toluene was established. Exposure to TCE for a month resulted in the loss of viability of the last three organisms, and resulted in a culture dominated by P. putida mt-2 from which mutants had fortuitously arisen (Mars et al. 1998). Two different types of experiments on bioremediation of sites contaminated with TCE have been carried out, and have been preceded by, and taken advantage of the valuable results obtained in microcosm experiments. Application of Indigenous Bacteria One procedure used an indigenous microlora enriched by the addition of substrates that induced the appropriate oxygenases. Microcosm experiments (Hopkins et al. 1993b) demonstrated the differential effects of phenol, toluene, methane, and ammonia. Whereas the irst two substrates were equally effective in removing both TCE and trans-1,2-dichloroethene (DCE), methane was only marginally effective in removing TCE though more effective in removing trans-1,2-DCE, while ammonia was less effective in removing all the substrates. It was shown that in bioreactors fed with phenol under various conditions, maximum removal of TCE occurred when phenol was supplied as a pulse every 24 h. In this reactor there was a greater diversity of microorganisms and higher numbers that degraded phenol and TCE (Shih et al. 1996). Field evaluation of this procedure has been carried out, using phenol or toluene or methane as oxygenase inducers (Hopkins et al. 1993a; Hopkins and Mccarty 1995). The effectiveness of the various substrates for removal of a number of chloroethenes is given in Table 14.3. Using phenol or toluene, therefore there remains no serious concern over the recalcitrance of chloroethenes—and particularly of vinyl chloride produced by partial anaerobic dechlorination of TCE. In this experiment, the concentrations of residual phenol and toluene were below the standards set for drinking water. A full-scale treatment of TCE-contaminated groundwater used pulsed addition of toluene and supplied oxygen both as O2 and H2O2: a high level of TCE removal was achieved over a 410-d period (McCarty et al. 1998). In a further development, in situ stripping of TCE was used to release the TCE from the dense water phase, and this was then mixed with toluene, hydrogen peroxide, oxygen, and a tracer and was pumped down-low into the aquifer where degradation occurred. A high level of removal was accomplished with the stripping, and a further amount by biodegradation that resulted in an efluent with the concentration of TCE reduced to 250 µg/L (Goltz et al. 2005).

TABLE 14.3 Influence of Growth Substrates on the Removal of Chloroethenes % Removal of Substrate Growth Substrate

Concentration (mg/L)

TCE

1,1-DCE

cis-DCE

trans-DCE

MCE

Methane 6.6 19 — 43 90 95 Phenol 12.5 94 54 92 73 >98 Toluene 9 93 — >98 75 — Note: TCE = trichloroethene; 1,1-DCE = 1,1-dichloroethene; cis-DCE = cis-1,2-dichloroethene; trans-DCE = trans-1,2dichloroethene; MCE = chloroethene (vinyl chloride)

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Microbiological investigations after treatment have revealed several important additional facts: a. The adverse effect of 1,1-DCE on the populations was restored after its removal, and the original population diversity was recovered only after treatment with toluene and TCE. The dominant Gram-negative taxa belonged to the genera Comamonas-Variovorax, Azoarcus, and Burkholderia (Fries et al. 1997a); b. Although many Gram-negative strains hybridized to a toluene 2-monooxygenase probe, not all positive strains effectively degraded TCE, and none were as effective as Burkholderia cepacia strain G4. Since many indigenous strains were able to degrade toluene—though not all of them were able to metabolize TCE—such strains would dominate populations in the absence of TCE (Fries et al. 1997b). This is consistent with the results of a laboratory study using B. cepacia strain G4 (Mars et al. 1996). Application of Exogenous Bacteria In the second procedure, organisms with an established degradation potential for TCE were injected at the site. 1. Cells of Methylosinus trichosporium strain OB3b were added and became attached to the sediments to form an “in situ bioreactor.” The concentration of TCE in samples withdrawn through the bioilter region fell rapidly, although after 40 d the concentrations had reverted to background levels (Duba et al. 1996). The major remaining unresolved issue was therefore how the degradative activity could be maintained during the length of time required for effective bioremediation. 2. In the light of possible concern over the introduction of phenol into aquifers, mutant strains of Burkholderia (Pseudomonas) cepacia strain G4 in which toluene 2-monooxygenase is constitutive have been examined in microcosm experiments. Effective removal of TCE could be demonstrated (Krumme et al. 1993; Munakata-Marr et al. 1996), although in the irst experiment serious loss in the viability of the cells occurred during the 10-week incubation. This aspect therefore presents a remaining challenge. Experiments have been conducted in a contaminated aquifer to examine the effect of Triton X-100 on increasing the release of TCE from sediments (Sahoo et al. 1998). The increase was rather modest (ca. 30%), and is consistent with the limited effect of surfactants in increasing the availability of PAHs, which has been discussed in Part 2 of this chapter. Anoxic and Anaerobic Conditions The anaerobic dechlorination of chloroethenes has received considerable attention, and has been encouraged by concern that partial dechlorination could result in the production of vinyl chloride as a terminal metabolite. After induction by growth of Desulfomonile tiedjei DCB-1 with 3-chlorobenzoate, partial dechlorination of TeCE to TCE and cis-1,1-DCE has been observed (Cole et al. 1995; Townsend and Sulita 1996). Dehalogenases for both TCE and TeCE have been examined in a strain of Sulfurospirillum (Dehalospirillum) multivorans (Neumann et al. 1994), and it has been shown that the dechlorination of TeCE in anaerobic aquifer slurries was stimulated by C-3 carboxylic acids or ethanol (Gibson and Sewell 1992). Particular attention has centered on the application of organisms such as Dehalococcoides ethenogenes that can carry out complete dechlorination to ethene. Details of the anaerobic degradation of chloroalkanes and chloroalkenes have been discussed in detail in Chapter 7, Part 3, and the application of reductive processes to bioremediation has been examined under denitrifying, sulidogenic, and methanogenic conditions. An important observation

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was the dechlorination of TeCE to ethene in an enrichment culture when it was linked to the anaerobic degradation of toluene (Shen and Sewell 2005). Practical implementations have been discussed, and many references to conference proceedings and reports have been given (Lee et al. 1998). The following provide illustrations of effective procedures: 1. An enrichment culture KB-1 that contained organisms related to Dehalococcoides ethenogenes was used to treat groundwater contaminated with TeCE and lower concentrations of TCE (Major et al. 2002). The groundwater was irst inoculated with methanol and acetate to produce anaerobic conditions before introduction of the culture. Within 200 d, the concentrations of all the chlorooethenes were low, and their loss was equivalent to the ethene that was produced. It was shown using a Dehalococcoides ethenogenes—speciic PCR that the population increased during treatment and that this populated the contaminated aquifer. 2. A valuable comparison was made of the relative effectiveness of (a) augmentation with a culture containing Dehalococcoides ethenogenes, (b) stimulation of the natural dechlorinated population by addition of lactate and mineral nutrients, and (c) a recirculation control without amendment (Lendvay et al. 2003). The irst procedure rapidly affected complete dechlorination, whereas the second was effective only after a lag period, and in both the irst and second treatments the population of Dehalococcoides increased. 3. A comparison of electron donors was made to establish the effectiveness of the dechlorination of TCE to ethene. The results of analysis of 16S rDNA and terminal restriction fragment length polymorphism showed that ive groups of organisms were found in all the enrichments including Dehalococcoides sp. whose presence was proved by the quantitative PCR. Although dechlorination of TCE to ethene has been demonstrated in species of this genus, other organisms including species of Citrobacter, Bacteroides, and Desulfovibrio probably played a role in establishing syntrophic associations (Freeborn et al. 2005). 4. The organisms in a reactor fed with TeCE and methanol were analyzed using a 16S rDNA clone library and luorescence in situ hybridization (Rossetti et al. 2003). Dechlorination to chloroethene was the major reaction and, in contrast to the enrichments already noted and those that are discussed in Chapter 7, Part 3, sequences similar to those of the well-established dechlorinating organisms Dehalococcoides ethenogenes, Dehalobacter restrictus, Desulfuromonas chloroethenica, or Sulfurospirillum multivorans were absent. The majority of clones belonged to the phyla Spirochaetes (56%), Firmicutes (18%), Chlorolexi (16%), and Bacteroidetes (6%). No microbial type could therefore be correlated with the observed dechlorination, and it was concluded that dechlorination was carried out by hitherto undescribed organisms. Application of Higher Plants Use of higher plants has attracted attention for the remediation of TCE-contaminated aquatic systems, and in particular the use of hybrid poplar (Newman et al. 1999). Although this was encouraged by the removal of labeled TCE to >90% using hybrid poplar under hydroponic conditions (Orchard et al. 2000), and the ability of hybrid poplar to metabolize TCE (Newman et al. 1997; Shang et al. 2001), there are additional considerations that must be evaluated to determine its general applicability. a. The concentration of the established metabolites is generally low, and was apparently greatest in the roots (Orchard et al. 2000). This suggests the possible involvement of microbial activity. b. Loss by volatilization can occur from the stems by transport along the transpiration pathway (Ma and Burken 2003), and may present a problem through its introduction into the atmosphere.

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CONCLUSION In situ procedures using indigenous organisms induced for the aerobic degradation of chloroethenes have been successful, particularly in broadening the range of substrates to include those that might be produced by partial anaerobic dechlorination. Limited use has been made of anaerobic processes, though these may effectively be combined with aerobic reactions. The application of introduced organisms is currently limited by the relatively short time during which their activity can be maintained, but this could possibly be achieved by designing more effective “in situ bioreactors.”

METHYL TERT-BUTYL ETHER Methyl tert-butyl ether (MTBE) has replaced tetraethyl lead as an octane booster in gasoline and to minimize automobile discharge of carbon monoxide in cold weather. It is produced on a large scale, and there has been concern over its possible adverse effects. Its occurrence in groundwater can be associated with gasoline spillage or leakage from underground tanks that are used to store oxygenated fuel. This has already been discussed as a source for BTEX. A survey has revealed the widespread distribution of MTBE in water in the United States, although in no case did concentrations exceed those set for drinking water standards (Squillace et al. 1996). Contrary to initial fears, this compound was not associated with the simultaneous presence of BTEX so that its source remained unestablished. Attention has been directed to its toxicity, and a somewhat complex picture has emerged (references in Kado et al. 1998; Nihlén et al. 1998). Attention is drawn here only to some aspects of its biodegradability and the possibility of bioremediation of adversely affected groundwater. Experiments have been carried out under different conditions and reached apparently conlicting conclusions. 1. Under aerobic conditions, a mixed bacterial culture was able to degrade the substrate with intermediate formation of tert-butanol (Salanitro et al. 1994). 2. Evidence from ield measurements indicated slow decay near the source of contamination but persistence further downstream. This was consistent with the results of laboratory experiments that showed only slow biodegradation of MTBE under aerobic condition (Borden et al. 1997). 3. In a simulated spill, groundwater was spiked with BTEX, MTBE, and chloride as marker, and injected into a sandy aquifer (Schirmer and Barker 1998). Whereas the level of BTEX fell, loss of MTBE was much slower, and only ca. 3% remained after 8 years, although the mechanism of its loss was not resolved. 4. Degradation of [U-14C]-MTBE and [U-14C]-tert-butanol was demonstrated within 105 d in laboratory micrososms containing stream sediments from a contaminated area (Bradley et al. 1994). 5. Under prolonged incubation under a variety of anaerobic conditions, the substrate was recalcitrant under sulfate-reducing conditions, and very poorly degraded under nitratereducing conditions (Mormille et al 1994). However, ission of the ether group to tertbutanol has been observed in laboratory sulfate-reducing cultures (Somsamak et al. 2001), and in methanogenic enrichment cultures (Somsamak et al. 2005), while extensive degradation in groundwater has been reported (Kuder et al. 2005). 6. As a result of the slow growth rates of organisms that can degrade MTBE, a membrane reactor was designed to retain the organisms while allowing free access of water within the system. In one application the inoculum was grown separately with MTBE and BTEX, and added as a concentrate to the reactor that was fed with a nutrient solution of ammonium sulfate and potassium phosphate. The inluent contained MTBE, its degradation products (tert-butyl formate and tert-butanol), and BTEX. Over a period of 6 months the removal eficiency for the contaminants exceeded 99% (Zein et al. 2006).

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The collective evidence suggests the variable recalcitrance of MTBE under aerobic conditions, a degree of recalcitrance anaerobic conditions, and that the presence of the putative degradation product tert-butanol cannot necessarily be construed as evidence for biodegradation (Landmeyer et al. 1998). Bioremediation of groundwater contaminated with MTBE is clearly beset with problems for its practical implementation.

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Mars AE, GT Prins, P Wietzes, W de Konig, DB Janssen (1998) Effect of trichloroethylene on the competitive behaviour of toluene-degrading bacteria. Appl Environ Microbiol 64: 208–215. Mars AE, J Houwing, J Dfoling, DB Janssen (1996) Degradation of toluene and trichloroethylene by Burkholderia cepacia G4 in growth-limited fed-batch culture. Appl Environ Microbiol 62: 886–891. Massol-Deyá A, R Weller, L Ríos-Hernández, J-Z Zhou, RF Hickey, JM Tiedje (1997) Succession and convergence of bioilm communities in ixed-ilm reactors treating aromatic hydrocarbons in groundwater. Appl Environ Microbiol 63: 270–276. McCarty PL, MN Goltz, GD Hopkins, ME Dolan, JP Allan, BT Kawakami, TJ Carrothers (1998) Full-scale evaluation of in situ cometabolic degradation of trichloroethylene in groundwater through toluene injection. Environ Sci Technol 32: 88–100. Morgan P, ST Lewis, RJ Watkinson (1993) Biodegradation of benzene, toluene, ethylbenzene and xylenes in gas-condensate-contaminated water. Environ Pollut 82: 181–190. Mormille MR, S Liu, JM Sulita (1994) Anaerobic biodegradation of gasoline oxygenates: extrapolation of information to multiple sites and redox conditions. Environ Sci Technol 28: 1727–1732. Munakata-Marr J, PL McCarty, MS Shields, M Reagin, CS Francesconi (1996) Enhancement of trichloroethylene degradation in aquifer microcosms bioaugmented with wild-type and genetically altered Burkholderia Pseudomonas cepacia G4 and PR1. Environ Sci Technol 30: 2045–2052. Nelson MJK, SO Montgomery, PH Pritchard (1988) Trichloroethylene metabolism by microorganisms that degrade aromatic compounds. Appl Environ Microbiol 54: 604–606. Neumann A, H Scholz-Muramatsu, G Diekert (1994) Tetrachloroethene metabolism of Dehalospirillum multivorans. Arch Microbiol 162: 295–301. Newman LA, SE Strand, N Choe, J Duffy, G Ekuan, M Ruiszai, BB Shurtleff, J Wilmoth, MP Gordon (1997) Uptake and biotransformation of trichloroethylene by hybrid poplars. Environ Sci Technol 31: 1062–1067. Newman LA, X Wang, IA Muizniekls, G Ekuan, M Ruszaj, R Cortelucci, D Domroes, G Karscig, T Newman, RS Crampton, MG Yost, PE Heilman, J Duffy, MP Gordon, SE Strand (1999) Remediation of trichloroethylene in an artiicial aquifer with trees: a controlled ield study. Environ Sci Technol 33: 2257–2265. Nihlén A, R Wålindrer, A Löf, G Johanson (1998) Experimental exposure to methyl tertiary-butyl ether. II. Acute effects in humans. Toxicol Appl Pharmacol 148: 281–287. Orchard BJ, WJ Doucette, JK Chard, B Bugbee (2000) Uptake of trichloroethylene by hybrid poplar trees grown hydroponically in low-through plant growth chambers. Environ Toxicol Chem 19: 895–903. Rabus R, F Widdel (1995) Anaerobic degradation of ethylbenzene and other aromatic hydrocarbons by new denitrifying bacteria. Arch Microbiol 163: 96–103. Rabus R, F Widdel (1996) Utilization of alkylbenzenes during anaerobic growth of pure cultures of denitrifying bacteria on crude oil. Appl Environ Microbiol 62: 1238–1241. Rabus R, R Nordhaus, W Ludwig, F Widdel (1993) Complete oxidation of toluene under strictly anoxic conditions by a new sulfate-reducing bacterium. Appl Environ Microbiol 59: 1444–1451. Reinhard M, S Shang, PK Kitanidis, E Orwin, GD Hopkins, CA Lebron (1998) In situ BTEX biotransformation under enhanced nitrate- and sulfate-reducing conditions. Environ Sci Technol 31: 28–36. Rossetti S, LL Blackall, M Majone, P Hugenholtz, JJ Plumb, V Tandoi (2003) Kinetic and phylogenetic characterization of an anaerobic dechlorinating microbial community. Microbiology (UK) 149: 459–469. Sainowski M, C Griebler, RU Meckenstock (2006) Anaerobic cometabolic transformation of polycyclic and heterocyclic aromatic hydrocarbons: evidence from laboratory and ield studies. Environ Sci Technol 40: 4165–4173. Sahoo D, JA Smith, TE Imbrigiotta, HM Mclallan (1998) Surfactant-enhanced remediation of a trichloroethene-contaminated aquifer. 2. Transport of TCE. Environ Sci Technol 32: 1686–1693. Salanitro JP (1993) The role of bioatttenuation in the management of aromatic hydrocarbon plumes in aquifers. Ground Water Monit Remed 13: 150–161. Salanitro JP, LA Diaz, MP Williams, HL Wisniewski (1994) Isolation of a bacterial culture that degrades methyl t-butyl ether. Appl Environ Microbiol 60: 2593–2596. Schirmer M, JF Barker (1998) A study of long-term MTBE attenuation in the Borden aquifer, Ontario, Canada. Ground Water Monitoring and Remediation: 113–122. Shang TO, SL Doty, AM Wilson, WNJ Howard, MP Gordon (2001) Trichloroethylene oxidative metabolism in plants: the trichloroethanol pathway. Phytochemistry 58: 1055–1065. Shen H, GW Sewell (2005) Reductive biotransformation of tetrachloroethene to ethene during anaerobic degradation of toluene: experimental evidence and kinetics. Environ Sci Technol 39: 9286–9294.

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Shih C-C, ME Davey, J Zhou, JM Tiedje, CS Criddle (1996) Effects of phenol feeding pattern on microbial community structure and cometabolism of trichloroethylene. Appl Environ Microbiol 62: 2953–2960. Somsamak P, HH Richnow, MM Häggblom (2005) Carbon isotope fractionation during anaerobic biotransformation of methyl tert-butyl ether and tert-amyl methyl ether. Environ Sci Technol 39: 103–109. Somsamak P, RM Cowan, MM Häggblom (2001) Anaerobic biotransformation of fuel oxygenates under sulfate-reducing conditions. FEMS Microbiol Ecol 37: 259–264. Squillace PI, JS Zogorski, WG Wilber, CV Price (1996) Preliminary assessment of the occurrence and possible sources of MTBE in groundwater in the United States, 1993–1994. Environ Sci Technol 30: 1721–1730. Stroo HF et al. (2003) Remediating chlorinated solvent source zones Environ Sci Technol 37: 225A–230A. Tick GR, F Lourenso, AL Wood, ML Brusseau (2003) Pilot-scale demonstration of cyclodextrin as a solubilityenhancement agent for remediation of a tetrachloroethene-contaminated aquifer Environ Sci Technol 37: 5829–5834. Townsend GT, JM Sulita (1996) Characterization of chloroethylene dehalogenation by cell extracts of Desulfomonile tiedjei and its relationship to chlorobenzoate dehalogenation. Appl Environ Microbiol 62: 2850–2853. Tsao C-W, H-G Song, R Bartha (1998) Metabolism of benzene, toluene, and xylene hydrocarbons in soil. Appl Environ Microbiol 64: 4924–4929. Vanderberg LA, BL Burback, JJ Perry (1995) Biodegradation of trichloroethylene by Mycobacterium vaccae. Can J Microbiol 41: 298–301. Vannelli T, M Logan, DM Arciero, AN Hooper (1990) Degradation of halogenated aliphatic compounds by the ammonia-oxidizing bacterium Nitrosomonas europaea. Appl Environ Microbiol 56: 1169–1171. Walter GA, SE Strand, RP Herwig, TP Treat, HD Stensel (1997) Trichloroethylene and methane feeding strategies to sustain degradation by methanotrophic enrichments. Water Environ Res 69: 1066–1074. Zein MM, MT Suidan, AD Venosa (2006) Bioremediation of groundwater contaminated with gasoline hydrocarbons and oxygenates using a membrane-based reactor. Environ Sci Technol 40: 1997–2003.

FINALE: A HIERARCHICAL STRATEGY It is obvious that there are several basic questions that must be answered before considering bioremediation: • • • • •

What compounds are present and which have to be removed? What quantities are involved? By what means is success to be evaluated? Are indigenous or exogenous organisms to be used? What additional carbon additives are appropriate?

In virtually all the examples that have been used as illustration, three stages may be discerned, and it is convenient to assemble these into a hierarchical system: (I) basic laboratory studies, (II) microcosm studies using site material, and (III) evaluation in large-scale systems, on-site pilot plants, or in situ installations. For all of them, the use of speciic isotope enrichment (Chapter 13) can provide invaluable evidence of degradation or transformation. It is essential in addition that geological, engineering, microbiological, and chemical interactions be setup before initiating the project and maintained throughout. The design of laboratory experiments on degradation has been discussed in Chapter 5 and includes illustrative examples of both micro- and mesocosm systems. Several examples of the use of microcosms have been given in this chapter.

I. LABORATORY EXPERIMENTS For both exogenous and indigenous organisms, the following merit attention: • Examination of pathways including transformation with the formation of intermediate and terminal metabolites

Applications of Bioremediation

691

Use of the substrates as sources of carbon, nitrogen, sulfur, or phosphorus Physiological optima of temperature, pH, and oxygen concentration Toxicity of the substrates Induction of catabolic enzymes by growth with structurally unrelated substrates Degradation of a compound during growth with a metabolically compatible substrate (cometabolism or concurrent metabolism) • The existence of mixtures of substrates when their biodegradation can be metabolically incompatible • Evaluation of relevant probes for the presence of the relevant microorganisms and their activity • • • • •

For many exogenous organisms, many of these issues will already have been established, so that only complementation will be required for indigenous organisms: determination of their presence, number, and metabolic activity by conventional laboratory procedures. It may be valuable to set up enrichment cultures using site material to provide suitable material for laboratory and microcosm studies.

II. MICROCOSM EXPERIMENTS These should be constructed from material collected from the relevant site and simulate aerobic, microaerophilic, or anaerobic conditions. They should provide the kinetic data necessary for largescale operation, and speciically address the following—although some of them will already have been examined: • Rates of substrate loss • Data on the existence and stability of metabolites and their toxicity to other biota • Existence of threshold substrate concentration below which rates of degradation are low or negligible • Effectiveness of analog substrates and metabolites in promoting degradation • Stability of the system under prolonged operation It is appropriate at this stage to evaluate procedures that will be used to assess the effectiveness of bioremediation, which have been discussed in Chapter 13. These may include (a) use of radiolabeled substrates (although these will not generally be permitted in ield operations) and the application of 13 C-labeled substrates, (b) evaluation of the occurrence of metabolites, and (c) evaluation of markers such as speciic enzymes.

III. LARGE-SCALE OPERATIONS Apart from the preceding issues, it is specially important at this stage that very close collaboration with geologists and engineers is necessary. Putatively optimal solutions may not be realistic for the site, and alternatives may have to be adopted. The choice may then depend on returning to Stage II—or even Stage I—to evaluate these new constraints. A good example is provided by the reduced permeability of substrata encountered during application of a pump-and-treat system: this was due to several causes including mobilization of colloidal material in the system and subsequent deposition and fouling at injection sites and iniltration zones (Wiener et al. 1996). It is probably inadvisable to initiate the evaluation of alternative strategies in large-scale systems. All the intrinsic problems of scale-up will clearly have to be addressed and solved. These include: (a) the mobility of microorganisms, substrates, nutrients, and metabolites, (b) oxygen transport or the maintenance of other electron acceptors generally nitrate, and (c) the long-term stability of the system.

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CONCLUDING COMMENTS Whereas the potential of bioremediation is substantial, its application may encounter important limitations that are apparent from many of the examples that have been used as illustration. The authors feel that these limitations can be overcome only when adequate attention is directed to fundamental microbiological, chemical, and engineering issues. Only then can the barriers to achieving success in full-scale operation be surmounted, since there are signiicant problems with in situ or on-site programs that have not taken advantage of experiments under the controlled conditions in microcosms or small-scale bioreactors. Of the several unresolved microbiological issues, it is suggested that the following deserve particular consideration: • The degree to which the compounds are accessible to the appropriate microorganisms. • The extent to which the population of degradative organisms can be maintained and increased. • The relative biodegradability of components in complex mixtures such as PAHs and PCBs, since some of the less readily degraded components may be the least desirable from an environmental and toxicological viewpoint. • Even when removal of, say 90% of the contaminant has been achieved, it may not be possible to attain 99% removal due to the possible existence of threshold concentrations below which rates of degradation are slow or even negligible. • Evaluation of success is of primary importance. Loss of substrates is a necessary but not suficient condition, in the light of the frequency of biotransformation reactions and the formation of terminal and possibly toxic metabolites.

Index A Acenaphthene-[13C] aerobic degradation, NMR application, 286 Acetaminophen, chlorination (Cl2), 33 Acetate anaerobic metabolism/dismutation, 319 methanogenesis, 319 Acetone, aerobic metabolism, 306 Acetophenone, degradation, 434 Acetylene hydratase, 187, 309 Acid tolerance, amino acid decarboxylation, 176 Actinomycetes, 65 cytochrome P450 monooxygenation, 65 dioxygenation, 66 Acyl chloride intermediates, 122, 126, 455–456 chlorobenzene degradation, 122 hexachlorocyclohexane degradation, 122 pentachlorophenol degradation, 122 Adamantane, cytochrome P450 hydroxylation, 115 Adaptive degradation, 216−217 Adenine, aerobic degradation, 542 Aging determinant biodegradation, 208–210 bioremediation, 611 Agrochemicals, adaptive degradation, 217 Alachlor, chironomid larvae transformation, 96 Aldehyde oxidoreductase, 164 Aldicarb, chemical hydrolysis, 23 Aliphatic ethers, aerobic degradation, 573 Alkaliphiles, 75 Alkanes aerobic degradation, 298−303, 299 chain-branched, 300, 301 cytochrome P450 bacteria, 303 Prototheca zopii, 99 yeast, 132, 303 anaerobic degradation, 304, 305 atmospheric transformation, 17, 18 bioremediation, 639−642 bioavailability, 640 surfactant production, 640 terrestrial habitat requirements, 640 oxygen provision, 640 inorganic nitrogen source, 640 growth, emulsiier, Candida, 213 oxidation, Nitrosomonas europaea, 71 Alkane degradation, marine systems, 641 nutrient addition, 642 oil dispersant, 642 Alkane hydroxylase, 103, 301, 303 ω-alkane hydroxylase, 300 Alkane hydroxylation, 298−299, 299 yeast, 116 Alkane monooxygenase gene, rhizosphere, 652 Alkane sulfonates, electron acceptor, 156 Alkanones, degradation, 310

Alkenes double bond ission, 305 epoxidation, 104, 305−308 Alkylethoxy sulfates degradation, ether bond ission, 570 Alkyl arenes, atmospheric transformation, 17 Alkyl carboxylates aerobic reduction, 164 Alkyl phosphonates, reduction alkanes, 589 Alkyl sulfatases, 569 Alkyl sulfates, hydrolysis/inversion alkyl−oxygen ission, 570 Alkyl sulides, atmospheric transformation, 21 Alkyl sulfonate, anaerobic degradation, Bilophilia, 590 Alkylsulfonate-[35S], metabolism, 279 Alkylamines deaminase, 313 degradation, oxidase, 132 dehydrogenase, 311 oxidase, 311 Alkylbenzenes, degradation, 149 Alkylnaphthalenes, aerobic bacterial oxidation, 400 Alkylphenol polyethoxylates, partial degradation, 575 Alkynes, triple bond hydration, 308 Alternative substrates, growth, 258 Amidase, 322 Amino acid metabolism anaerobic rearrangement, 316 dismutation (Stickland reaction), 316 decarboxylation, 315 fermentation, clostridia, 73 pyridoxal 5′-phosphate enzymes, 312 pyruvoyl enzymes, 315 2-aminobenzenesulfonate, degradation, 507 4-aminobenzenesulfonate degradation, 507 excretion, 521 Aminobenzoate monooxygenation, 109 2-aminobenzoate, anaerobic degradation, 436 2-aminobenzoate CoA ester, aerobic degradation Azoarcus, 432, 433 3-aminobenzoate-6-hydroxylase, 109 1-aminocyclopropane-1-carboxylate (ACC) deaminase, 609 degradation, 313, 314 Aminodinitrotoluene, ozone degradation, 30 2-aminodiphenylamine, transformation phenazine, 4-aminoacridine, 510 2-aminoethylarsonic acid, degradation, 594 2-aminoethylphosphonate, degradation, 588 2-aminoethylsulfonate, dioxygenation, 126 5-aminonaphthalene-2-sulfonate, sequential microbial/ chemical reactions, 55 6-aminonaphthalene-2-sulfonate, degradation, 507 2-aminophenol distal 1,6-dioxygenase, 124, 511 2-aminophenoxazine-3-one, terminal metabolite, 510 2-aminopropane, transformation to alaninol, 311 5-aminosalicylate degradation, 426

693

694 Amitrole (3-amino-1H-1,2,4-triazole), TiO2 photochemical degradation, 10 Anaerobic bacteria carboxylation, 449−452 experimental procedures, 258 nitrate tolerance, 72 oxygen tolerance, 72, 202 Anaerobic xylene degradation, methylbenzylsuccinate markers, 681 Anaeromyxobacter, 2-chlorophenol anaerobic dechlorination, 488 Anammox, 148 Androgens, cytochrome P450 demethylation, 117 Aniline aerobic degradation, 452 dioxygenase, 452 ozone transformation, 31 Aniline-[15N] reaction humic/fulvic acid, NMR application, 287 ANME-1/ANME-2, methane anaerobic oxidation, 626 Anodic oxidation, 37 Anthracene degradation bacteria 403, 404 white-rot fungi, 414 Anthracene-9[13C] degradation, 278 Anthranilate 1,2-dioxygenase, 425 Anthranilate-5-hydroxylase, 108 Anthraquinone-2,6-disulfonate (AQDS) as electron acceptor, 153−155 Antibiotic resistance, 170−172 covalent modiication, 170 eflux pump, 171 plasmids, 224 Aquatic plant metabolism pentachlorophenol, 604 phoxim, 604 2,4,6-trinitrotoluene (TNT), 604 Archaea, 58 Archaeal population, oil contamination, 623 Arene aldehyde oxidoreductase, Clostridium, 439 Arene aldehyde, anaerobic reactions oxidation/sulfate reduction 439 reduction to benzyl alcohols, 439 Arene carboxylate degradation, low oxygen concentration, 204 Arene carboxylates. See also speciic compounds aerobic reduction to aldehyde, 433 decarboxylation, 430 low oxygen concentration, degradation, 203 Arene cis-dihydrodiols, synthetic applications, 392−394, 393 Arene dihydroxylation, 18O application, 279 Arene hydrocarbon contamination, 13C-naphthalene analysis, 627 Arene hydrocarbons. See also PAH degradation, Novosphingobium, 67 δ13C fractionation, 630 pyrolysis, 35 Arene hydroxylation fungi, 389 Streptomyces, 115 cytochrome P450, 65, 388 Arene monooxygenation, 106

Index Arene oxide, NIH shift, 107, 410, 411 Arenesulfonates anaerobic desulfonation, 508 dioxygenase, 506 Arginine, anaerobic growth Pseudomonas, 201 Aromatic amino acids, sequential microbial/chemical reactions, 55 Aromatic carboxylic acids, decarboxylation, 68 Arsenate, electron acceptor, 151 Arsenoacetate, growth substrate, 594 Artiicial streams, pentachlorophenol degradation, 266 Aryl carboxylates, aerobic reduction, 164 Aryl sulfatase, mycobacteria, 570 Aryl sulfates, hydrolysis with O−S ission, 570 Aryl-alcohol oxidase, fungi, 133 Arylamine reactions N-acetylation, 509 association with organic matter, 509 dimerization, 509 Association organic compounds humic matter, 15 N − NMR application, 287 Association, substrates − soil organics, 206 Atmospheric reactants − hydroxyl radicals, nitrate radicals, ozone, 14 Atmospheric reactions relative rates, 15 survey, 15 ATP synthesis anaerobic bacteria, 52 purine degradation, 544 coupled to transformation 3-chlorobenzoate, 475 hexachlorocyclohexane, 355, 369 tri-/tetrachloroethene, 367 Atrazine bioremediation, carbon/nitrogen ratio, 673 degradation, 545, 546 metabolism, hybrid poplar, 98, 603 ozone/H2O2 transformation, 31 photochemical transformation, 5, 9 sulfate radical degradation, 32 Atropine, degradation, 345, 346 Azaarene. See also speciic compounds inhibition PAH degradation, 647 Azoarene reductase, 163−164 aerobic bacteria, 521 Clostridium perfringens, 521 reduction/N−N scission, 520 Azo group decolorization fungal peroxidase, 521 yeast, 521 Azo pigments/dyes, reduction/N−N scission, 507 Azotobacter sp., 2,4,6-trichlorophenol degradation, 66 Azotobacter, degradation potential, 66

B Bacterial dioxygenases, 105 Baeyer-Villiger monooxygenation acetophenone, 434 alkanone, 310 cycloalkanone, 337

695

Index Bentazone, association soil organic matter, 207 Benz[a]anthracene, bacterial metabolism, 406 Benzene aerobic degradation, 386 anaerobic degradation, δ13C/δ2H, 630 anaerobic hydroxylation, 18O application, 280 cytochrome P450 hydroxylation, 115 dioxygenase, 387 metabolism, spinach, 604 oxidation, Nitrosomonas europaea, 71 monooxygenation, 387 Benzene-[13C] degradation, 278 Benzene-[13C]/toluene-[13C], δ13C lipid analysis, 630−631 Benzoate/acetate, diauxic growth, 221 Benzoate. See also speciic compounds anaerobic degradation, 436−438, 437 dioxygenase, 424 metabolism, Trichosporon, 427 transport, 214 Benzofuran dioxygenation, 555 hydroxylation/ring ission, Paecilomyces, 558 Benzo[a]pyrene metabolism bacteria, 408 Cunninghamella transformation, 412 cytochrome P450 Saccharomyces hydroxylase, 413 Paralichthys, 93, 94 photooxidation, 11 quinones, white-rot fungal metabolites, 416 Saccharomyces hydroxylation, 116 Selenastrum, 413 transformation, white-rot fungi, 416 Benzo[a]pyrene quinones, white-rot fungal metabolites, 416 Benzo[b]thiophene, sequential microbial/chemical reactions, 55 Benzothiazole degradation, 567, 568 [15N] degradation, NMR application, 287 Benzothiophene sulfoxide, abiotic reaction, 566, 567 Benzothiophene dioxygenation, 565 oxidation sulfoxide, 566 Benzoyl CoA ester aerobic degradation, Azoarcus, 432 pathway inducer, 436 reductase, Thauera aromatica, 290 Benzylsuccinate synthase, 450 toluene, anaerobic metabolism, 390−391 Bias in elective enrichment, 622 Bile acids, anaerobic transformation, 343 Biocontrol agents, bacteria, 607 Biodegradability, ready/inherent, 247 Biodegradation/biotransformation, deinitions, 51 Bioilms bioremediation, 611 BTEX degradation, 680 Biogenic terpenes, atmospheric transformation, 17 Bioremediation, pathway regulation, 610 Biosurfactant production alkane growth, 640 PAH growth, 649

Biphenyl aerobic degradation, 401 Porphyrobacter, 59 dioxygenase, 401 hydroxylation/ring ission, Paecilomyces liliacus, 77, 402, 558 inducer, PCB degradation, 196, 210 regulation degradation pathway, 464 transformation, Cunninghamella, 411 Bis-(1-chloro-2-propyl)ether, enantiomeric biodegradation, 54, 575 Bis-(pentaluorophenylpropyl)sulide, sulfur source, 578 Bisphenol-A aerobic degradation, 301, 302, 447 cytochrome P450 hydroxylation, 116 Boronate, monooxygenation, 591 Box proteins, aerobic benzoyl-CoA degradation, 432 Bradyrhizobium, constitutive 3-ketoadipate enzymes, 221 Brominated biphenyls, primers anaerobic PCB dechlorination, 196, 666 2-bromobenzoate, aerobic degradation, 469−470, 470 4-bromobenzoate, primer anaerobic PCB dechlorination, 467, 666 5-bromo-5,6-dihydrouracil, debromination, 541 2-bromodibenzo[1,4]dioxin, primer octachlorodibenzo [1,4]dioxin anaerobic dechlorination, 467, 666 5-bromouridylate, debromination, 541 Bromoacetaldehyde toxicity, 360 Bromophenol, reductive debromination, Desulfovibrio, 488 BTEX aerobic degradation, 679−680 aerobic metabolites, humic associated, 680 13 C-benzene analysis, 628 luidized-bed reactor, 680 white-rot fungus, 389 BTEX, groundwater contamination, 679−681 anaerobic conditions, 680−681 relative component degradation, 681 methylbenzylsuccinate markers, xylenes, 681 in situ stream treatment, 680 remediation advantage, indigenous organisms, 679 toluene/biphenyl dioxygenase family, 623 tert-Butyl diphenyl phosphate, degradation, 265

C 13

C Metabolic application, 277−278 NMR, 285−286 C14 Methyl steroid oxidation, 18O application, 280 Camphor catabolic plasmid, 225 cytochrome P450 (P450 cam) hydroxylation, 115, 458 degradation, 340 Carbamazepine, ozone degradation, 30 Carbaryl, abiotic transformation, 3 Carbazole 1,9a dioxygenase, 555 three component, 527 relaxed speciicity, 527 Carbazole, aerobic degradation, 527, 528 Carbocyclic ring reductase, 164 Carbon disulide, growth substrate, 580 Carbon monoxide dehydrogenase, 183, 185 structure, 291

696 Carbon monoxide metabolite, 128, 539, 559 Carbon monoxide metabolism, 323 Carboxylation alkane degradation aerobic, 300 anaerobic, 304 phenol/aniline anaerobic, 449−452 Carboxylic acid reductase, 188 Carotenoids, sulide reduction, 28 Caryophyllene oxide, transformation, Botrytis, 345 Catabolic plasmids, 225−226, 225 Catechol alternative ring ission, 123 degradation, 472−474 incompatibilities, 3-substituted, 474 ring ission dioxygenation, 428. See also Extradiol ring ission, Intradiol ring ission Catechol 2,3-dioxygenase gene, rhizosphere, 652 Cation electron aceptor, 152−154 reduction, 172 toxicity eflux system, 175 polyphosphate, 175 Chemical industry contaminants, conclusion for bioremediation, 668 Chlorate electron acceptor, 150 reductase, 150−151, 187 Chlorinated alkane degradation, Rhodococcus, 64 Chlorinated arene hydrocarbons. See also speciic compounds atmospheric transformation, 17 remediation, δ13C application, 631 Chlorinated biphenyl, catabolic plasmid, 225 Chlorinated dibenzo[1,4]dioxin partial anaerobic dechlorination, 558 photoproduction, pentachlorophenol, 7 thermal production, 35 Chlorinated ethanes, zero-valent iron transformation, 26 Chlorinated phenoxyalkanoates, remediation, 672. See also speciic compounds Chlorination (Cl2 ), 32 Chlorite dismutase, 151 Chloroacetophenone, PCB metabolite, 463 2-chloroacetophenone degradation, 18O application, 280 2-chloroacrylate degradation, 362 reductase, 163 3-chloroacrylate, degradation, 363 Chloroalkane/chloroalkene, δ13C, δ37Cl, 632 Chloroalkanes oxidation, Nitrosomonas europaea, 71, 364 Chloroalkene, aerobic degradation, δ13C application, 631 Chloroaniline, regulation of bacterial degradation, 672 4-chloroaniline aerobic degradation, 490 association with soil organic matter, 207 Chloroanisole metabolite, 659 Chlorobenzene/toluene degradation Phanerochaete, 610 Ralstonia, 662−663 Chlorobenzene degradation. See also speciic compounds

Index acyl chloride intermediate, 122 Fenton’s reagent transformation, 9 terminal metabolite hexachlorocyclohexane, 662 threshold concentration, 212 Chlorobenzoates marker, PCB metabolism, 664 PCB metabolites, 463 3-chlorobenzoate aerobic degradation, 469, 470−472 low oxygen concentration, 203 pristine environment, 216 anaerobic dechlorination, Desulfomonile, 475 catabolic plasmid, persistence, 227 3-chlorobenzoate-degrading genotypes, 625 4-chlorobenzoate aerobic degradation, 469, 470−472 transport, 214 2-chlorobiphenyl metabolism, NIH shift, 464 4-chlorobiphenyl, nitrated metabolites, 57 3-chlorocatechol aerobic metabolism ring ission, 469, 471 alternatives, 123, 456 Candida, 487 toxic metabolite, 222 3-chlorocatechol 1,6-dioxygenation 470, 471 Chlorocatechol-sediment, resistance to anaerobic dechlorination, 209 3-chloro-/3-methylcatechol, degradation incompatibility, 223 4-chlorocatechol, aerobic metabolism, 469, 471 3-chloro-1,2-epoxyethane (epichlorohydrin), degradation, 362 Chloroethene anaerobic dechlorination, 684−685 cooxidation, 682 reductase, 368−369 Chloroethene (vinyl chloride) aerobic degradation, enrichment factors, 631 Chloroethene bioremediation in situ procedure preference, 682 application of exogenous bacteria, 684 application of indigenous bacteria, 683−684 toluene/phenol oxygenase induction, 682, 683 Chloroethene oxidation methane/propane/ammonia monooxygenase, 682 pseudomonad monooxygenase/dioxygenase, 682–683 Chloroluoroalkanes, porphyrin dehalogenation, 27 Chloroform degradation, 364 methane/butane induction, 197 2-chlorohydroquinone dioxygenation, 126 5-chloro-2-hydroxypyridine-3-carboxylate, aerobic degradation, 534, 535 Chloromuconate metabolism, 470, 471 Chlorophenols. See also 2,4-Dichlorophenol, Pentachlorophenol aerobic bacteria, degradation, 482−483 anaerobic dechlorination, 488, 660 aerobic degradation mycobacteria, 63 Phanerochaete, 486−487 Sphingobium, 67 white-rot fungi, 659 metabolism, Candida, 487

697

Index monooxygation, 111 reductive dechlorination, 488−489 remediation, 659 tolerance, 176 2-chlorophenol, electron acceptor, Anaeromyxobacter dehalogenans, 74 4-chlorophenol/4-methylphenol degradation, Comamonas, 610 Chlorophenoxyacetate, catabolic plasmid, 225 4-chlorophenylacetate, two-component dioxygenase, 475 2-chloropropionate dehalogenase, 362 5-chloropyrogallol, ring ission Candida, 487 3-chloroquinoline-8-carboxylate, dioxygenation, 537 Chlorotoluenes, transformation, 457 2-chlorotoluene, degradation, 456 Chlorpyrifos chlorination (Cl2 ), 33 transformation, Enterobacter, 69 2-chloro-6-(trichloromethyl)-pyridine metabolism, Nitrosomonas europaea, 71 oxygen dependent metabolism, 202, 205 transformations, 534, 535 Cholesterol degradation, 149 oxidase oxidation, 132 Cholic acid biotransformation / biodegradation, oxygen dependence, 205 Chromium (VI) reduction, Deinococcus, 154 Chromous chloride dehalogenation, 26 Ciproloxacin, fungal transformation, 539 Cis-stilbene, photocyclization, 11 Clinical bacteria, degradative capability, 58. See also Mycobacteria Clostridia, 73 CO2 alkanone degradation, 310 epoxide metabolism, 306 growth requirement, 53 Coal-tar globules, 646 Coenzyme M, vinyl chloride degradation, 307 Combined biological/chemical treatment, PAHs, 645 Cometabolism, 195 Complexing agents, degradation, 312 Continuous culture, application, 262 Cooxidation, chloroethene remediation, 682 Copper dioxygenase, 124 structure, Aspergillus, 290 Copper enzymes, 184−185 Copper methane monooxygenase, 184, 298 Copper−quinoprotein amine oxidase, structure, 291 C-P lyase, 588 Cresol degradation aerobic, 446 anaerobic, 451 fumarate pathway, 450 Cyanide, metabolism, 323 Cyanobacteria hexachlorocyclohexane dechlorination, 61 PAH metabolism, 413 Cycloalkanes, monooxygenation, 327 Cycloalkanone monooxygenase, 105, 106, 337

Cycloclasticus, arene degradation, 58−59 Cyclodextrin, chloroethene solubility enhancement, 682 Cyclohexane aerobic degradation, 337 monooxygenase, 69, 70 Cyclohexenone, dismutation, 163 Cyclohexylacetate, degradation, 337, 338 Cycloisomerase limitation, degradation of 2-chlorotoluene, 456 Cyclopropane carboxylate, degradation, 337, 338 Rhodococcus, 65 Cytidine, aerobic degradation, 540 Cytochrome oxidase, anaerobic bacteria, 202 Cytochrome P450 monooxygenase ish, 92 oxaarene transformation, 553, 554 systems, 114 yeast, 116 oxygen level dependence, 204 Cytochrome P450cam, 115, 340, 458 l-cysteate, transformation, 590 l-cysteine, desulfhydrase, 579

D Daidzein, anaerobic degradation, 560, 562 DDE dioxygenation, 458 recalcitrance, 198 DDT CaO degradation, 29 degradation, Phanerochaete chrysosporium, 76 reduction, zero-valent iron, 25 resistance, lies, 96 ring hydroxylation, 458 transformation, 67, 350, 351 aquatic plants, 663 photochemical, 8 uptake/metabolism, plants, 663 Decabromodiphenyl ether metabolism anaerobic debromination, 468, 666 ish, 95 n-decane, anaerobic degradation, 304 Decarboxylation non-oxidative, 430−431 phthalate degradation, 431 reversible anaerobic, 431−432 Degradative population, molecular procedures, 622 Dehalogenases halogenated alkanes, 359−361 halogenated alkanoates, 362 reductive 3-chlorobenzoate, 475 tetrachloro-/trichloroethene, 367, 368, 684 Dehalorespiration, 156, 367 Dehydroabietic acid cytochrome P450 hydroxylation, 115 degradation, 344 Dehydroxylation, phenol anaerobic degradation, 165, 187, 449 Denitriication, 148 Dense cell-suspensions, 261 O-demethylase, three-component anaerobic, 577

698 O-demethylation methoxybenzoates, 577 sulide-dependent, 578 Desulitobacterium spp., chlorophenol anaerobic dechlorination, 488 Desulfomonile, anaerobic dechlorination 3-chlorobenzoate, 475 chlorophenols, 488 Desulfovibrio vulgaris, oxygen tolerance, 202 Desulfurization, dibenzothiophene, 565 3,5-diacetamino-2,4,6-triiodobenzoate, partial deiodination, Trametes, 476 2,4-diacetylphloroglucinol hydrolase, 449 2,4-diacetylphloroglucinol, bacterial metabolite, 607, 608 α,ω-diamines, degradation, 311 2,3-diaminonaphthalene, reaction with nitrite, Escherichia coli, 55 Dibenzo[1,4]dioxan, degradation, 556, 557 Dibenzofuran degradation, 556, 557 Porphyrobacter, 59 dioxygenation, 556 hydroxylation/ring ission, Paecilomyces, 558 Dibenzothiophene anaerobic transformation, 567 dioxygenation, 565 monooxygenation, 113 nitrated metabolites from nitrite, 57 sulfur elimination, 565, 566 2,6-dibromobiphenyl, primer anaerobic PCB dechlorination, 465 Dibromoethane, methanogen anaerobic elimination, 355 Dibromoethene, methanogen anaerobic elimination, 355 4,4′-dicarboxyazobenzene, long-term adaptive degradation, 217 α,ω-Dicarboxylic acids, 300 3,4-Dichloroaniline association with soil organic matter, 207, 208 degradation bacteria, 490, 672 fungi, 673 nitrite reactions, Escherichia coli, 55 1,4-dichlorobenzene, degradation, 457 2,4-dichlorobenzoate, degradation, 472 reductive/hydrolytic steps, 475 2,7-dichlorodibenzo[1,4]dioxin degradation peroxidase, 559 Phanerochaete chrysosporium, 76 2,3-dichlorodibenzofuran, dioxygenation, 558 2,8-dichlorodibenzofuran, dioxygenation, 558 Dichlorodiluoromethane, CaO decomposition, 30 1,2-dichloroethane, aerobic dechlorination, 37Cl kinetic isotope effect, 633 1,1-sichloroethene, adverse effect on trichloroethene remediation, 684 2,6-dichlorohydroquinone degradation, 484 dioxygenation, 483 Dichloromethane aerobic degradation, fractionation factors 13 C / 37Cl, 632 degradation, 358, 363

Index 2,4-dichlorophenol association with soil organic matter, 207, 208 degradation, 112, 483 Phanerochaete, 487 hydroxylase, 111 sulfate radical, degradation, 32 2,4-dichlorophenoxyacetate degradation plasmid/chromosomal genes, 226 pristine environment, 215 protection by sorption, 208, 210 threshold concentration, 212 dioxygenation, 127 Fenton’s reagent transformation, 9 metabolism, Aspergillus, NIH shift, 486, 487 transport, 214, 215 Dichlorophenoxypropionate degradation, Sphingobium, 67 1,3-dichloropropene, degradation, 362 2,2-dichloropropionate degradation, 362 dehalogenase bias, 626 Diclofenac, photochemical degradation, 8 Diethyl ether fungal degradation, Graphium, 575 monooxygenation, 574 Diluorobenzoate dioxygenation, 498−499, 499 19 F − NMR application, 288 2,2′-diluorobiphenyl, dioxygenation, 495 4,4′-diluorobiphenyl ether, dioxygenase transformation, 495 2,3-diluorophenol, transformation, Rhodococcus, 500, 501 Dihydropyrimidine dehydrogenase, dehalogenation, 541 Dihydroxybenzoates, anaerobic degradation, 438 3,4-dihydroxybenzoate aerobic degradation, regulation, 220 2,3-dihydroxybiphenyl 1,2-dioxygenase, 461 1,2-dihydroxynaphthalene dioxygenase, 507 2,5-dihydroxypyridine, degradation, 530, 531 7,12-dimethylbenz[a]anthracene, photooxidation, 11 2,2-dimethylpropionate, aerobic degradation, 301 Dimethyldisulide, degradation, 580 Dimethylsulide, anaerobic growth, 578 Dimethylsulfoniopropionate anaerobic degradation, 579−580 degradation, roseobacters, 59 degradation/elimination, 579 de-S-methylation, 580 Dinitramine dealkylation by carp, 93 fungal metabolism, 509 4,6-dinitrohexanoate, 2,4-dinitrophenol metabolite, 516 2,4-dinitrophenol aerobic degradation, 164 transformation, 516−517, 517 2,4-dinitrotoluene degradation 18 O application, 279 Phanerochaete chrysosporium, 513, 514 2,6-dinitrotoluene, nitro group reduction by Salmonella, 68, 509

699

Index 2,4-/2,6-dinitrotoluene degradation, 676 dioxygenation, 512 Dinoseb, soil slurry remediation, starch waste/ pilot-scale inoculum, 673−674 1,4-dioxane, aerobic degradation, 576 Dioxygenases,104, 105 arene dihydroxylation, 118−122 concomitant elimination, 119–120, 120 2-halobenzoate 1,2-dioxygenases, 425, 496 two component, 469 three component, 470 2-ketoglutarate, 125−126 nitroarene three component, 512 PCB degradation, three component, 459 region III and IV in large α-subunit, 460 increased speciicity, 460 Phanerochaete, 1,2,4-trihydroxybenzene, 129 phenol formation, 119 phenoxyalkanoate degradation, 577 ring ission, 123−125, 455−456 Dioxygenation pathways, PAH degradation, 399, 402, 404 Diphenyl ether degradation, 555−556, 555 Trichosporium, 78 Dismutations acetate, anaerobic metabolism, 319 amino acids (Stickland reaction), 317 cyclohexenone, 163 2-hydroxypurine, 544 trichloroacetaldehyde, 364 Dissolved organic carbon, chemical hydrolysis rate, 25 DMSO reductase family, 148, 187

E EDTA anodic oxidation, 30 degradation, 312 photochemical transformation, 7 transport, 215 Eflux systems antibiotic resistance, 171 hydrocarbon tolerance, 169 metal/metalloid resistance, 175 Elective enrichment, 249−252 Electrohydrolic discharge plasmas, 37 Electron acceptors alkane sulfonate, 156 arsenate, 151 chlorate, 150 2-chlorophenol, 74 humic acid, 155 metal cations, 152−154 nitrate, 148 nitroalkane, 156 selenate, 151 tetrachloroethene, 74 Electron acceptors, fractionation factor in toluene anaerobic degradation, 630 Electron donors, anaerobic trichloroethene dechlorination, 685 Elimination reactions, 350

Elongation of carbon chain during alkethoxy sulfate degradation, 570 Emulsiier/biosurfactant, 213 Enantiomeric biodegradations bis-(1-chloro-2-propyl)ether, 54, 575 α-hexachlorocyclohexane, 54, 353 mandelate, 54, 435 phenoxyalkanoate, 577 3-phenylbutyrate, 54 2-(2-methyl-4-chlorophenoxy)propionate (Mecoprop), 54 β-endosulfan, transformation, 570 Enediol dioxygenase, 128, 182, 183 dual Fe and Ni enzymatic activity, 182 Enoate, anaerobic reduction, 163 α,β-Enone dismutation, 339 reduction clostridia, 73 lavanoid degradation, 560 reductase, clostridia, 163 Mössbauer spectrum, 280 Enrichments, elective bias, 622 Enroloxacin, fungal transformation, 539 Enterobacteriaceae metabolism, 67 Enzyme-mediated substrate association, 206−208, 207 Enzymes, plant introduction 3-chlorocatechol 1,2-dioxygenase, 606 cytochrome P450 2E1, 606 extradiol catechol dioxygenase, 606 haloalkane dehalogenase, 606 Epichlorohydrin (3-chloro-1,2-epoxyethane), degradation, 362 Epoxidation, alkene, 305 Epoxides metabolism, 306 resolution, 307−308 EPR applications, 289 Estrogens, ozone degradation, 31 Estrone, chlorination (Cl 2), 34 Ethionamide (pyridine-2-ethyl-4-carbothiomaide), metabolic activation, 170 Ethylbenzene aerobic hydroxylation, 388 anaerobic degradation, 391 4-ethylcatechol, toxic metabolite, 222, 224 4-ethylphenol dehydrogenation, 447 hydroxylation, Nitrosomonas, 388 EUROPHORE reactor, 21, 246 Extracellular enzymes, 213 peroxidase, white-rot fungi, 133 Extradiol ring ission, 105, 110, 123 dioxygenases, 123 Fe3+ enzyme, 428 Mn enzyme, 428

F F420 dependent reductase, 164 hydride transfer, ring reduction, 516 Fe(III) reductase, Geobacter sulfurreducens, 153, 155

700 Fe, regulation toxicant concentration, 203 Fenton’s reagent, oxidant, 9 Fenvalerate, chemical hydrolysis, 23 Five-membered heteroarene oxidoreductase, 129 Flavanoids aerobic degradation, 560, 563 anaerobic degradation, 560, 562 anaerobic ring B reduction, 163 inducer PCB degradation, 210, 211, 464, 607 plant metabolite, PCB degradation, 607 Flavanone, Aspergillus transformation, 559 Fluoroacetate degradation, 381 metabolite, 381 Fluoranthene alternative bacterial dioxygenations, 405 quinones as bacterial metabolites, 406 transformation, Cunninghamella, 410 Fluorinated hydroxybenzoate decarboxylation, Candida, 19 F − NMR application, 287 Fluorobenzenes, toluene 2,3-dioxygenase transformation, 494 Fluorobenzoate, dioxygenation, 496 2-luorobenzoate metabolism aerobic, 496 denitrifying, 499 3-luorobenzoate, distal dioxygenation, 497, 498 4-luorobenzoate 1,2-dioxygenation, 498, 499 hydrolytic luoride loss, 498, 499 4-luorobiphenyl, transformation, Tylospora, 495 Fluoromethane, oxidation, Nitrosomonas, 378 6-luoro-3-methylphenol, methanogenic transformation, 502 1-luoronaphthalene, metabolism, Cunninghamella, 495 5-luoronicotinate, degradation, 534 Fluorophenol hydroxylation, 19 F − NMR application, 288 Fluoroquinolone cipraloxacin, MnO2 transformation, 32 enroloxacin, photolysis, 7 photolability, 539 Fluorotelomer alcohol, degradation, 382 Fluorotoluene, dehydrogenation to luorobenzoate, 496 5-luorouracil fungal transformation, 540 metabolism, 19F − NMR application, 287 Fluoxetine, (Prozac), abiotic degradation, 8 Formate dehydrogenase, 188 Formate interspecies transfer, 320 Free radical, toluene anaerobic activation, EPR application, 289 Fumarate anaerobic metabolic pathways alkane, 304, 305 cresol, 4502-methylnaphthalene, 409 toluene 390−391, 448 xylene, 681 Fungal reactions hydroxylation/ring ission, Paecilomyces, 77, 558 analogous to mammalian systems, 76 Furan-2-carboxaldehyde, anaerobic degradation, 553, 554 Furan-2-carboxylate, aerobic degradation, 523, 524 Furan-3-carboxylate, anaerobic degradation, 553, 554 Fusaric acid, bacterial degradation, 608

Index

G Gallate (3,4,5-trihydroxybenzoate), anaerobic degradation, 450 Gentisate (2,5-dihydroxybenzoate) dioxygenase, 110, 125, 428, 430 pathway, 111, 425−426, 426 Geobacter Fe(III) electron acceptor, 153 reduction, 74 metallireducens, humic acid free radical production, EPR application, 289 sulfurreducens, oxygen as electron acceptor, 202 Glucose, enhancement/suppression of biodegradation, 198 Glutathione-mediated transformation, 307, 363, 369 Glutathione S-transferase, reactant, 307 Glycerol, anaerobic degradation, 310 Glycerol trinitrate reductase, 571 Glyoxal oxidase, 185 Phanerochaete, 133 Glyoxalase I, 182 Glyoxylate, aerobic metabolism, 317, 318 Glyphosate, degradation, 589 Gordonia, 65 Grass, naphthalene-[13C] mineralization analysis, 652

H Haloalkane degradation, 358−360 mycobacteria, 63 dehalogenase, structure, 290, 361 Haloalkanol dehalogenase, 361−362 2-Halobenzoate 1,2-dioxygenases, 425, 496 two component, 469 three component, 470 4-Halobenzoate, hydrolytic reactions, 472 Halogenated arene hydrocarbons, aerobic degradation, 455−458. See also PCB Halogenated benzoates. See also speciic compounds degradation, Rhodococcus, 64 dioxygenation, 469−472 Halogenated phenols. See also speciic compounds degradation, 482−486 hydroxylation, 483 Halogenated substrates, inhibition of degradation acyl chloride intermediate, 455 protoanemonin, 456 Halogenation, biotic, 134, 135 Haloperoxidase activities degradation of thiocarbamates, 116, 134 dihydrocoumarin hydrolase, 134−135 halogenation, 134, 135 Halophiles, 75 Heavy metal resistance plasmids, 224 Heme oxygenase, 114 Heptachlor transformations Daphnia magna, 99 photochemical, 6 Heteroarenes. See also speciic compounds anaerobic degradation, 653 partial removal, microcosm, 647

701

Index Hexachlorobenzene (HCB) anaerobic dechlorination/electron donor supplement, 663 partial anaerobic dechlorination, 489 reductive dechlorination, 458 Hexachlorobuta-1,3-diene, hydroxocobalamin dehalogenation, 27 Hexachlorocyclohexane (HCH) aerobic metabolism, 350−353, 354 isomers, 352 terminal metabolites, 352, 353 anaerobic transformation, 353−355 coupling to ATP synthesis, 355, 369 catabolic plasmid, 225 [36Cl] metabolism, 278 dechlorination, cyanobacteria, 61 degradation, acyl chloride intermediate, 122 enantiomeric biodegradation, α-isomer, 54, 353 extreme persistence, 662 hydroxocobalamin dehalogenation, 27 reductive dechlorination, Clostridium, 369 subcritical water degradation, 37 transformation, Citrobacter, 68 α-Hexachlorocyclohexane (HCH) aerobic mineralization, limitation by desorption, 209 Hexachloroethane anaerobic dehalogenation, 355 thiol reduction, 28 Hexadecane aerobic degradation at low oxygen concentration, 203 Hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX), degradation, 585, 676 Histidine aerobic degradation, 523, 524 ammonia lyase, 434 decarboxylation, 68 HMX degradation, 585 Humic acids bacterial reduction, 154 degradation role, 208 electron acceptor, 155 free radical production, EPR application, 289 photolytic role, aqueous media, 3 singlet oxygen (1O2) production, 12 Hybrid poplars, metabolism atrazine, 98, 603 creosote contamination, 652 hexahydro-1,3,5-trinitro-1,3,5-trizine (RDX), 603 trichloroethene, 98, 603, 685 Hydratase C=C,130 C≡C,131 R-C≡N,131 Hydrocarbons bacterial tolerance, 169 emulsiier synthesis/growth, 213 low temperature degradation, 200−201 Hydroluorocarbon, monooxygenation, 379 Hydrogenases, 184, 188 nitroarene reduction, Clostridium, 509 Hydroperoxide, alkane aerobic degradation, 303 3-Hydroxyanthranilate, metabolite, 514 4-Hydroxybenzaldehyde rearrangement, 427

Hydroxybenzoate, hydroxylation, 108 3-Hydroxybenzoate aerobic degradation, 428 fermentation, Sporotomaculum, 439 3-Hydroxybenzoate-6-hydroxylase, 108 4-Hydroxybenzoate anaerobic degradation, Thauera, 439 monooxygenation/NIH rearrangement, 426 oxidative decarboxylation, yeast, 427 reversible anaerobic decarboxylation, 431 4-Hydroxybenzoate-3-hydroxylase, 108 2-Hydroxybiphenyl metabolite dibenzothiophene, nitration, 57, 566−567 monooxygenase, 425 2-Hydroxyethylsulfonate, terminal electron acceptor, 590 Hydroxyl radicals, 4 Fenton´s reagent, 9 generation mechanisms, 4 toxicity to bacteria, 289 tropospheric formation, 14 3-Hydroxykynurenine pathway, tryptophan degradation, 526 4-Hydroxyphenylacetate hydroxylase, 111 monooxygenation/NIH rearrangement, 426 3-Hydroxyphenylpropionate, growth substrate, 69 4-Hydroxyphenylpyruvate dioxygenation, 126, 127, 426 Hydroxypurines, anaerobic hydroxylation, Peptococcus, 544 2-Hydroxypurine, dismutation Peptococcus, 544 4-Hydroxypyridine (pyridin-4-one), degradation, 530, 531 3-Hydroxyquinol-4-one dioxygenation, 539 2-Hydroxyquinoline-8-hydroxylase, 109 5-Hydroxysalicylate, ring ission, 425 Hydroxylamine-[15N reaction with humic/fulvic acid, NMR application, 287 Hydroxylase, 104. See also speciic substrate luoroacetate, 381 Hydroxylation/ring ission, Paecilomyces, 558 benzofuran, Paecilomyces, 558 biphenyl, hydroxylation/ring ission, 77, 558

I Iboprofen, degradation, 435 Immobilization, chlorophenol-degrading organisms, 659 Immobilized cells application to degradation, 261 chlorophenol-degrading organisms, 659 Indol-3-acetate, degradation, 526 Induction, catabolic enzymes, 195−198 analogue substrate, 195 induction by cosubstrates, 365 unrelated substrate, 197 Intradiol ring ission, 105, 110, 123 Fe2+ enzymes, 428 Intramolecular hydroxyl transfer, 1,2,3-trihydroxybenzene degradation, 450 isomerase, 450 Iodoacetate, product of chlorination (Cl2)/iodide, 32 Iodobenzoate. See 3,5-Diacetamino-2,4,6-triiodobenzoate Iron siderophore, 182

702 Isolavanoids, aerobic degradation, 560, 561 Isolavanone, Aspergillus, transformation, 559 Isonicotinic acid hydrazide (INH), metabolic activation, 170 Isonitrile metabolism, 322 Isoprene, metabolism, 65, 307 Isoquinoline degradation, 539 oxidoreductase, 130, 164, 187, 539 Isotope fractionation factor, 281 ratio, 281 experimental determination, 282 Isotope δ13C fractionation, bioremediation, 629−632 Isoxalutole, chemical hydrolysis, 24

K Karakin aglycone, electron acceptor, 586 Kinetic isotope effect, 281 3-Ketoadipate pathway, 110, 220−221, 428 2-Ketoglutarate anaerobic oxidoreductase, 164 dioxygenase, 125−126, 577 2,4-dichlorophenoxyacetate, 127 marker, 4-nitrophenoxyacetate substrate, 612 taurine, 590 Rhodotorula glutinis reactions, 129

L Lanosteroid, cytochrome P450 demethylation, 117 Limonene degradation, 339−340 transformation, by cutworm larvae of Spodoptera litura, 97 Linuron herbicide, adaptive degradation, 217 Lithotrophic bacteria, 60 Long-chain alkane degradation, yeast, 78 alkanoate, syntrophic degradation, 194 alkyl sulfonates, monooxygenation, 590 dialkyl ethers, degradation, 574 Low oxygen-concentration, degradation, 203−204

M Magnesium dioxygenase, 124 Malonate, anaerobic metabolism, 73, 318 Mandelate degradation, 433, 434 regulation, 221 Manganese dioxygenase, 124 Bacillus, Mössbauer spectroscopy, 290 enzymes, 181 Marine bacteria, degradation potential, 58 Marine ecosystems, biodegradation, 249 Marinobacter, alkane degradation, 58 Mecoprop [2-(4-chloro-2-methylphenoxy)propionate)], degradation, 54, 577 Media dilute complex, 58, 258 mineral basal, 252 solid, 257 Meisenheimer-type hydride complex, 164, 512, 516−517

Index 2-mercaptobenzothiazole, degradation, 567 Mesocosms, 266 Metabolic markers dioxygenase enzymes 2-ketoglutarate, 612 naphthalene, 611 toluene, 611 metabolites arene dihydrodiols/PAH degradation, 611 benzylsuccinate/toluene, anaerobic degradation, 267 chlorobenzoates/PCB degradation, 664 methylbenzylsuccinates/xylene, anaerobic degradation, 681 7-Methylbenz[a]anthracene, transformation, Cunninghamella, 410 3-O-Methylgallate central metabolite, 429, 577 degradation, 429, 430 2-Methylnaphthalene, anaerobic metabolism, 408, 409 Metabolic association, 194 Metabolite conjugation in ish, 95 Metabolites/bioremediation, association with humic acid, 612 Metal/metalloid microbial resistance, 172−175 Metal cation/oxyanion reductase, 165 Metal cations, electron acceptor, 152−154 Metal concentration, metabolism, 253, 254−256 Metallothionein, 175 Metamitron degradation, 546 Methane aerobic degradation, 297 anaerobic oxidation, 304, 626 plant-root, bacterial degradation, 607 Methanearsonic acid, degradation, 594 Methane/propane/ammonia monooxygenase, chloroethene oxidation, 682 Methane monooxygenase, 103, 298 copper enzyme, 184, 298 versatility, 69, 70, 297−298 Methane sulfonate, monooxygenation, 590 Methanogenesis, 182, 183 Methanol, anaerobic oxidation, 310 Methanotrophs, 13C-methane analysis, 628 Methionine degradation/elimination, 579 salvage, enediol dioxygenation, 126, 128, 182 Methoxybenzoates aerobic degradation, 429 aerobic O demethylation, 577 anaerobic growth, 577 anaerobic O-demethylation, 577 sulide-dependent, 578 Methylamine, degradation, 311 Methylamine-[15N] degradation, NMR application, 287 Methylation, metal/metalloid resistance mechanism, 173 Methylbenzylsuccinate markers, anaerobic xylene degradation, 681 Methyl chloride aerobic/anaerobic degradation, corrinoid pathway, 357 2-(2-methyl-4-chlorophenoxy)propionate (Mecoprop) enantiomeric preference biodegradation, 54, 577 removal, 672

Index Methyl coenzyme M reductase, 182 sequence application, 626 structure, 291 Methyl luoride, oxidation Nitrosomonas, 364 Methylglyoxal, degradation, 183, 310 N-methylisonicotinate, degradation, 532, 533 Methylmercury chloride, transformation to methane, 594 2-methylnaphthalene, anaerobic degradation, 409, 608−609 Methylotrophs, rice paddy, 13C-methanol analysis, 628 Methylparathion transformation, multiphase kinetics, 219 Methylphenylphosphonate, reduction to benzene, 67, 589 Methylquinolones, degradation, 538 Methyl tert-butyl ether (MTBE) bacterial metabolism, 686 degradation, 574 remediation, δ13C application, 629 TiO2 photochemical degradation, 10 transformation, 574 Metribuzin metabolites in leachate, 673 transformation, 546 Microcosm application, 264−265 13 C-substrate, DNA probe, 625 Mimosine, aerobic degradation, 532, 535 Mineralization, 247 Miserotoxin aglycone, electron acceptor, 586 Models of natural systems, 266 Molybdenum, oxidoreductase, 185−187 Molybdenum-dependent dehydrogenase, 185 W application, 280 Molybdopterin, 130, 185−187 Monochloroanilines, aerobic degradation, 490 Monoluorophenol, metabolism Rhodococcus, 500, 501 Monomethylsulfate, oxidative degradation, 570 Monooxygenase/dioxygenase, dual activity Mycobacterium, 406 Pseudomonas, 107, 400, 682–683 Monooxygenations, 106−113 alkene, 305 halogenated alkenes, 364 Monoterpenoid aerobic degradation, 300, 339−341 Morpholine degradation, 312 [13C] degradation, NMR, 286 cytochrome P450, 116 mycobacteria, 63 Mössbauer spectra, 57Fe application, 280 Mössbauer spectroscopy, application, 280, 290 Mutase, phenylhydroxylamine, 510 Mycobacteria degradation potential, 63 dehalogenase, 360 haloalkane degradation, 63 Mycobacterium chlorophenolicum detection by 16S rRNA / PCR, 659 Mycobacterium, dual monooxygenase/dioxygenase activity, 406 Mycorrhizosphere, Pinus sp., 609

N 15

N, NMR applications, 287 Naphthalene aerobic degradation, 399−400

703 catabolic plasmid, 225 dioxygenation pathway, 399 pathway induction, 399 plasmid-borne 399 anaerobic mineralization, 408 fungal transformation, 411 metabolism, oxygenic phototrophs, 413 toxicity, low oxygen concentration, 204, 647 transformation to naphth-1-ol by Bacillus, 400 Naphthalene/2-methylnaphthalene, sulfate-reduction, enrichment factor, 630 Naphthalene carboxylates, aerobic degradation, 401 Naphthalene dioxygenase, 400 marker, indigo production, 611 rhizosphere gene, 652 Naphthalene monooxygense/dioxygenase, dual activity, 400 Naphthalene-2-sulfonate metabolites as redox mediators, 155 Naphthalene soil-sorbed, degradation, 210 Naphthalenesulfonates, degradation, 506−507 Naphthenates, degradation, 641 Naphth-1-oate, surfactant during growth, 213 Naphth-1-ol, degradation, 401 Natural consortia, 264 Natural substrates, induction of PCB metabolism, 664 Neptumonas, naphthalene dioxygenase, 59 Nickel enzymes, 182−184 Nicotinate anaerobic metabolism, 534−536, 536 hydroxylase Mo(V) EPR spectrum 280 77 Selenium, application, 280 Nicotine aerobic degradation, 132, 532, 533 diazodiphenoquinone, chemical artefact, 532 catabolic plasmid, 225 oxidase, 132 18 O application, 279 NIH shift − metabolism, 426 arene oxide bacteria, 107 fungal transformation, 410 2-chlorobiphenyl hydroxylation, 464 1,3-dichlorobenzene monooxygenation, 458 2,4-dichlorophenoxyacetate fungus, 486 4-hydroxybenzoate degradation, 109 4-hydroxyphenyolacetate degradation, 426 Nitrate anaerobic electron acceptor, 148 PAH degradation, 647 assimilation, 148 Nitrate ester reductase, 162 reductive degradation, 571 Nitrate radicals, 14 Nitrated metabolites from nitrite, 57 Nitrilase, selectivity, 322 Nitrite, metabolite incorporation, 57 Nitroalkane degradation, Fusarium oxidase, 133, 586 electron acceptor, 156 oxidation, 129

704 Nitroarenes. See also speciic compounds bioremediation, problem areas, 675, 677 degradation, mycobacteria, 63 partial reduction to hydroxylamine, 510 reductase, 162 three component dioxygenase, 512 Nitrobenzene degradation dioxygenation, 512 reduction/rearrangement, 511 2-nitrobenzoate, reductive metabolism, 515 anthranilate pathway, 514 hydroxylamine/rearrangement, 514 3-nitrobenzoate, dioxygenation with nitrite loss, 514, 515 4-nitrobenzoate, reduction to hydroxylamine/ rearrangement, 514, 515 Nitrodiphenylamine, nitro group reduction, 510 Nitroluoranthenes, atmospheric production, 21 2-nitronaphthalene, atmospheric production, 20 Nitrophenols, secondary atmospheric oxidation products from monocyclic arenes, 21 2-nitrophenol, degradation by monooxygenation, 515 3-nitrophenol degradation by reduction/rearrangement, 516 4-nitrophenol adaptive degradation, 217 degradation, 515−516, 516 monooxygenation, 112 2-nitropropane dioxygenation, yeast, 586 oxidation, 128 3-nitropropanol, electron acceptor, Denitrobacterium, 586 Nitropyrenes, atmospheric production, 21 1-nitropyrene, phototransformation, 11 N-nitrosodimethylamine monooxygenation, 586 Nitrosomonas europaea oxidation, 70−71 haloalkane oxidation, 364 2-nitrotoluene dioxygenase, three component, 512 4-nitrotoluene oxidation to nitrobenzoate, 513 3-nitrotyrosine, degradation, 515 NMR technical developments, 284 NMR, application 13 C, 285 19 F, 287 15 N, 287 17 O, 287 31 P, 288 Nonaluoropentanoic acid, polyoxometalate degradation, 10 Non-oxidative decarboxylation, 430−431 Nonsymbiotic diazotroph, 608 4n-nonylphenol metabolism, plant cultures, 605 Nonylphenol, degradation, 301, 302, 448 side-chain rearrangement, 301−302, 427, 448 Nonylphenol, polyethoxylate partial degradation, 575 NTA degradation, 312 Nutrient media, metabolic effects, 219−220

O Octachlorodibenzo[1,4]dioxin anaerobic partial dechlorination, 467, 666 degradation, Phanerochaete, 667 photochemical product from pentachlorophenol, 7

Index Octachlorostyrene, blue mussel transformation, 96 Octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX), degradation, 585, 676 Octane, cytochrome P450 hydroxylation, 114 Octyl-2-sulfate, hydrolysis, 570 O-demethylation aerobic, 577 anaerobic, 577 sulide-dependent, 578 Old yellow enzyme reaction α,β-unsaturated ketone, 339 reductase, 163 reduction α,β-unsaturated nitro compounds, 586 Oligotrophs, 211 Oligotrophic bacteria, 59 On-site vs off-site PAH remediation, 645 Organophorphorus pesticide hydrolysis, 677 Organophosphate as source of phosphorus, 571 Organophosphorous acid anhydrase (OPA), 571 Orotic acid, anaerobic degradation, 541 o-phthalate. See also Phthalate dioxygenation, 532 metabolite from degradation anthracene, phenanthrene, 404 isoquinoline, 539 Oxaarenes cytochrome P450 transformation, 553, 554 three component 4,4a-dioxygenase, 555, 556 Oxalate anaerobic metabolism, 73, 318 decarboxylase, 185 Oxidoreductases, 129−130. See also Pyridine, Isoquinoline, Quinoline Oxygen concentration as determinant, 201 synthesis of toxicant, 203 tolerance Clostridium during microaerophilic growth, 202 Desulfovibrio vulgaris, 202 Oxygenases, 104, 105 Oxygenic phototrophs, metabolism, 413

P PAH degradation. See also speciic compounds adaptive, 216 aerobic bacteria, 403 aging, 208 cis dihydrodiol markers, 611 combined biological/chemical treatment, 645 fractionation factor, 630 growth with phenanthrene as substrate, 196 induction, 221 Leclercia, 69 mycobacteria, 63 PAH degradation (contd.) range of bacteria, 647 subcritical water, 37, 645 stereospeciicity, 403 white-rot fungi, 77 PAH metabolism anaerobic, 652 cytochrome P450 hydroxylations, Streptomyces, 115

Index ish, 92−93 fungal transformations 76, 409−413, 646 H2O2 requirement, 650 mammalian metabolism model, 409 phenolic metabolites, 410 quinone production, 651 stereospeciicity compared, 409 fungus-mediated polymerization, 651 ozone oxidation, 31 polychaetes, 97 sorption/desorption, 208, 646 surfactants, 649−650 transformation, phototrophic bacteria, 61 PAH quinones, abiotic formation, 653 PAH remediation combined biological/chemical treatment, 645 conclusions, 654 gas works site, application of fungi, 646 naphthalene dioxygenase genes, 623 oxygenase genes, PCR ampliication, 623 plant role, 623 prairie grass stimulation, 605 primary targets, 644 white-rot fungi, 651 Paraquat photolysis, 8, 532 Partition/organic matrix, contaminants, 601 PCB/PBB, adaptive degradation, 217 PCB atmospheric hydroxylation, 16 bioavailability, surfactants, 665 chlorobenzenes as degradation markers, 267, 611 remediation, 665−666 ring ission, 461 sediment association, 209 sub-critical water dechlorinations, 25, 37 PCB aerobic degradation, 459−464, 462, 664 chloroacetophenone metabolites, 463 lavanoids as inducers, 210, 464, 607 hydrolytic reactions after ring ission, 461−462 long-term exposure, 665 organisms, 459 rhizobia, 67 tree proximity, 665 PCB anaerobic dechlorination, 465−467 Chlorolexi group, 466 Dehalococcoides group, 466 metabolic inhibitors, 626 non-methanogenic mixed culture, 466 patterns, N-, P -, LP -, 465, 665−666 preferential congener removal, 666 temperature signiicance, 664 δ13C fractionation, 629 PCB metabolism ish hydroxylation, 95 Nereis virens, 97 Phanerochaete chrysosporium, 77, 465 plant cultures, 604 Pentachloroaniline, partial anaerobic dechlorination, 490 Pentachloroanisole, Phanerochaete formation/ mineralization, 659

705 Pentachlorobenzene hydroxylation, P450 cam mutants, 458 partial anaerobic dechlorination/electron donor, 663 Pentachloronitrobenzene transformation methanogenic, 673 Tetrahymena thermophila, 99 Pentachlorophenol abiotic degradation, glow discharge plasma, 38 association with soil organic matter, 206 biodegradation, 485, 486 acyl chloride intermediate, 122 additional substrate requirement, 659 Fenton´s reagent transformation, 9 monooxygenation, 112 dehalogenation, 486 photochemical transformation, 5 octachlorodibenzo[1,4]dioxin, formation, 7 stream degradation, 266 tolerance to aerobic bacteria, 659 Pentachlorophenol metabolism Phanerochaete chrysosporium, 76 Eichornia crassipes, 97 plant, 604 Pentachloropyridine, partial anaerobic dechlorination, 534 Pentaerythritol tetranitrate degradation, 69, 571 reductase, 571 Pentaluorophenol, monooxygenation, 500 Perluoroalkanecarboxylates degradation partial photochemical, 667 sulfate radical, 12 Perluorooctanoate, photochemical degradation, 12 Peroxyalkanoyl nitrates, photochemical formation, 13 pH buffer control, 254 Phenanthrene anaerobic mineralization, 408 bacterial aerobic degradation, 403, 404 degradation, humic matter-associated, 209 dioxygenase, 403 growth substrate for PAH degradation, 196 metabolism by oxygenic phototrophs, 413 transformation Phanerochaete, 415 Streptomyces to trans dihydrodiol, 405 Phenazine, 2-aminodiphenylamine metabolite, 510 Phenazine-1-carboxamide, bacterial metabolite, 607 tomato rot control, 608 Phenazine-1-carboxylate, bacterial metabolite, 607 Phenmedipham, chemical hydrolysis, 23 Phenol degradation anaerobic, 449−452 dehydroxylation, 165, 187 Aspergilllus fumigatus, 77 community, 13C-phenol analysis, 627−628 strain introduction, 624 Variovorax sp., 625 Phenol metabolism conjugation by fungi, 410 hydroxylase, 446 gene, 624 monooxygenation, 110, 446 yeast, 77−78

706 Phenol-degrading community, 13C-phenol analysis, 627−628 Phenoxyalkanoate degradation, 576 dioxygenase dealkylation, 577 enantiomeric speciicity, 577 Phenylacetate degradation, Escherichia coli, 435 Phenylacetate-[13C] aerobic degradation, NMR application, 286 l-phenylalanine aerobic transformation, 113 ammonia lyase, 434 anaerobic degradation, Thauera, 436 hydroxylation, 113, 426 3-phenylbutyrate, degradation, 435 enantiomeric speciicity, 54, 435 4-phenylcatechol, toxic metabolite, 222 Phenylhydroxylamine, rearrangement, 510 Phenylmercuric acetate, transformation to benzene, 594 Phenylphosphate synthesis, anaerobic degradation of phenol, 449 Phenylurea herbicide-degrading population diversity, 625−626 Variovorax sp., 616, 625 Phloroglucinol (1,3,5-trihydroxybenzene) degradation, Fusarium, 449 metabolite from 3,4,5-trihydroxybenzoate, 450 Phosphatase, 571 Phosphonatase, 588 Phosphonates degradation pathway, 588−589 phosphorus source, 588 Phosphonomycin, degradation, 67 Phosphoroluoridates, degradation, 677 Photochemical experimental generation of reactants, 245−246 Phototrophic bacteria, transformation, 61 Phoxin transformation by Glycine max, 97 Phthalate. See also o-phthalate aerobic degradation, 431 dioxygenase, 431 esters, hydrolysis, 569 Phthalazine, hydroxylation, 539 Phytoremediation, 602−603 α-pinene, degradation, 341 Plant cultures, metabolism 4n-nonylphenol, 605 pentachlorophenol, 604 PCB, 604 Plant cuticles, roles in photochemical transformations, 11−12 Plant exudates, 605 metabolism, 97−98 metabolites, PCB degradation, 665 remediation primary role, 603 secondary role, 605 Plasmids catabolic, 224−227, 225 transmission, 226 Poly(cis-1,4,isoprene), aerobic degradation, 66, 305 Polybrominated biphenyls (PBB)

Index anaerobic debromination, 467, 468, 666 primers, dechlorination PCBs, 467 Polychlorinated dibenzo[1,4]dioxin, atmospheric hydroxylation, 16 Polyethylene glycol degradation aerobic, 67, 575 anaerobic, 575 Polyluorinated phenol, hydroxylation, Trichosporon, 500 Polyluorinated substrates, metabolism, 382 Polyhalogenated alkanes, cytochrome P450 reductive dehalogenation, 366 Polyisoprenoid oxygenase, 128 Polyoxometalates (heteropolyacids) degradation 2,4,6-Trichlorophenol, 10 oxidants, 10 Porphyrin-mediated dehalogenation, 26−27 Porphyrobacter, biphenyl and dibenzofuran degradation, 59 Prairie grass-stimulated PAH remediation, 605 Prednisone reduction, “old yellow enzyme”, 163 Pre-exposure enhanced degradation, 601 naphthalene degradation, 216 Pregnenolone, C17 side-chain removal by cytochrome P450, 117 Primers for anaerobic dehalogenation PCB, 465, 467 octachlorodibenzo[1,4]dioxin, 467 Pristane, aerobic degradation, 300 Pristine environments degradation, 215−216 degradative bacteria, 622 Prodrug metabolism, 170 Progesterone, cytochrome P450 15β-hydroxylation, 115 Propane exceptional oxidation by Rhodococcus, 126, 303 Propan-2-yl sulfate, oxidative degradation, 570 Propham, abiotic degradation, 3 Propionate aerobic degradation, 299 anaerobic metabolism, 319 [13C], NMR application, 286 analysis, [13C] syntrophic oxidation, 628 syntrophic, 194, 320 Protoanemonin 4-chlorobenzoate synthesis, inhibition of PCB degradation, 223 metabolic inhibition, 463 Pseudomonad monooxygenase/dioxygenase, chloroethene oxidation, 682−683 Psychrophiles, 74 Purine aerobic degradation, 542 anaerobic degradation, 544−545, 545 fermentation, clostridia, 73 hydroxylase, 130, 545 Pyrene aerobic degradation, 406−407,407 chlorination (Cl2), 33 degradation at low oxygen concentration, 203 dihydrodiol marker for aerobic degradation, 267 hydroxylation by Porcellio scaber, 97 mineralization, [13C] pristine forest soil, 646 oxidation by Nematoloma frowardii, 77

707

Index transformation Cunninghamella, 412 white-rot fungi, 415−416 Pyrene quinone bacterial metabolite, 407 white-rot fungus metabolites, 416 Pyridine aerobic degradation, 529 dioxygenation, 532, 534 oxidoreductase, 129 ring reductive pathway, 529 Pyridine carboxylates degradation, 531 interacting pathways, 530 Pyridine-4-carboxylate, degradation, 530 Pyridine dicarboxylates coupled photolytic/microbial degradation, 13 oxidation, 532 Pyridine-2,6-dithiocarboxylate, function in tetrachloromethane degradation, 363 Pyridoxal, degradation, 529 Pyrimidines. See also speciic compounds aerobic/anaerobic ring reduction, 540, 541 degradation, clostridia, 73 Pyrrole-2-carboxylate, aerobic degradation, 523, 524 Pyruvate, anaerobic metabolism Pseudomonas, 201 Pyruvate formate lyase mechanism, EPR application, 289 Pyruvoyl enzyme, amino acid metabolism, 315

Q Quercitin anaerobic degradation, 560, 562 dioxygenase, 126, 185 Quinazoline, hydroxylation, 539 Quinoid mediators, azoreductase, 521 Quinoline aerobic degradation, 536−539, 538 dioxygenation, 537 hydroxylation, 536 oxidoreductase, 130, 537 Quinolone. See also Methylquinolone degradation, 536 pathway, tryptophan degradation, 526 Quinol-2-one 5,6-dioxygenase, single component enzyme, 537 Quinol-4-one-2-carboxylate, dioxygenation, 537 Quinone-mediated redox reductions azo dyes, 155, 521 nitroarenes, 28−29 Quinones bacterial metabolites luoranthene, 406 pyrene, 407 pyrene and benzo[a]pyrene, Cunninghamella, 412

R Raleigh model, 281 RDX/HMX, subcritical water degradation, 36 RDX degradation, 585 partial metabolism

hybrid poplar, 98 Reed Canary grass, 99 partial reduction, Klebsiella, 69 subcritical water degradation, 37 Reaction rates, kinetic aspects, 218−219 Recalcitrance, biodegradation, 247 Redox potential determinant, 205 growth media, 256 Redox mediators cinnaquinone, secondary metabolite from Streptomyces, 28 naphthalene-2-sulfonate metabolites from Sphingomonas, 155, 521 Regulation, degradative pathways, 220−222, 413 Remediation, chemical procedures, 602 Resorcinol, aerobic degradation, 448 Reverse methanogenesis, anaerobic methane oxidation, 304, 626 Rhizobia degradation potential, 66 PCB degradation, 67 Rhizosphere alkane monooxygenase gene, 652 catechol 2,3-dioxygenase gene, 652 colonization, phase variation in bacteria, 608 Rhodamine B, polyoxometalate degradation, 10 Rhodococcus metabolic versatility, 64−65 Ribolavin, degradation, 542, 543 Rimsulfuron, chemical hydrolysis, 23 Ring ission dioxygenases, 123, 428–429, 428, 430 Roseovarius, dimethylsulfoniopropionate degradation, 59 Rutin dioxygenation Aspergillus, 559 carbon monoxide metabolite, 128, 129

S Salicylate degradation, 425−426 5-hydroxylase, 108, 109 Salinity evaporation pond, population, 627 Secondary metabolites produced by bacteria, 607 Selenate electron acceptor, 151 reductase, 151 Sequential microbial/chemical reactions, 55 Selenium requirement purine hydroxylase, 545 xanthine dehydrogenase, 544 Silicibacter, dimethylsulfoniopropionate degradation, 59, 580 Simulated tropospheric reactions, 16, 245 Singlet oxygen (1O2), reactant, 12 Soil slurries vs solid phase microcosm system, 647 Solid media, preparation, 257 Sphingomonad classiication, 67 Squalene, aerobic degradation, 305 Stable enrichment cultures, 260 Steroid 3-keto-4,6-diene, anaerobic reduction, 163 Steroids cytochrome P450 demethylation, 117

708 Steroids (contd.) degradation, 342, 343 fungal hydroxylation, 116, 341 Stilbene, oxidative ission, 392 Storage of samples, 247 Streptomyces, metabolic potential, 65−66 PAH hydroxylation, 115 phenanthrene trans-9,10-dihydrodiol, 405 Structure-activity relationship, reaction rates, 219 Styrene metabolism ring dioxygenation, 392 side-chain monooxygenation, 392 Subcritical water, 25, 36−37 degradation hexachlorocyclohexane, 37 PAH, 644 PCB, 37 RDX/HMX, 36 Substrate concentration degradation, 248 desorption as limiting factor, 208, 209, 210 inluence on degradation, 211−212 particulate matter attachment, 265 remediation signiicance, 612−613 Succinyloxyacetate degradation, lyase, 574 Sulcotrione, photochemical transformation, 12 Sulfamethoxazone, chlorination (Cl2), 33 Sulfate radical, oxidant, 32 Sulfate-reducing anaerobic bacteria, 73 Sulides, organic enantiomeric oxidation, 580−581 oxidation, Nitrosomonas europaea, 71 Sulfoacetaldehyde central metabolite from C2 sulfonates, 590 degradation, 590 Sulfometron, chemical hydrolysis, 23 Sulfonates bacterial rhizosphere survival, 605 electron acceptor, 590 Sulfone metabolites, aquatic mammals, 96 Sulfonylurea, cytochrome P450 hydroxylation, 65, 116 Sulfosuccinate, degradation, 590 sulfur sources, phototrophic bacteria, 61 Superoxide dismutases, 182, 303 Surfactant, naphtho-1-ate growth, 213 Syntrophic degradation, 194

T Taurine degradation, 590 electron source, Rhodopseudomonas, 590 TCA cycle modiied, acetate anaerobic metabolism, 319 Temperature anaerobic dehalogenation, 466−467 bioremediation, 613 degradation determinant, 200 Terminal metabolites 2-aminophenol, 2-aminophenoxazine-3-one, 510 bioremediation, adverse prognosis, 612 hexachlorocyclohexane, 352, 353 nitrated metabolites from nitrite, 57 triluorobenzoates, 503

Index Terpenoid, PCB degradation, 210, 464, 607 Tetrabromobisphenol-A, anaerobic debromination, 489 Tetrachloroaniline, partial anaerobic dechlorination, 489 1,2,3,4-tetrachlorobenzene, degradation, 456 1,2,4,5-tetrachlorobenzene, degradation, 456,503 Tetrachlorobiphenyl congeners, TiO2 photochemical degradation, 10 2,3,4,6-tetrachlorobiphenyl dechlorination, temperature effect, 200 1,2,3,4-tetrachlorodibenzo[1,4]dioxin, CaO transformation, 29 2,3,7,8-tetrachlorodibenzo[1,4]dioxin degradation, Phanerochaete, 667 anaerobic dechlorination in aged sediment, 667 Tetrachloroethene anaerobic dechlorination, 366−369, 367 Clostridium bifermentans, 368 Desulfurospirillum, 367 Methanosarcina, 368 strain KB-1, 685 Sulfurospirillum multivorans, 74, 684 37 Cl fractionation factor, 632 dehalogenase, 684 electron acceptor, Desulitobacterium metallireducens, 74 partial reduction, Enterobacter, 69 reactor dechlorination, 685 reentry of tropospheric transformation products, 19 Tetrachloromethane bacterial supplementation/electron donor, 682 degradation, 149 EPR application, 289 pyridine-2,6-dithiocarboxylate, 289, 363 [13C] degradation, 277, 289 partial anaerobic dechlorination, 370 thiol reduction, 28 Tetraethyl lead, degradation, 593 1,1,1,2-tetraluoroethane, reentry of tropospheric transformation products, 19 Tetrahydrofuran, growth substrate, 576 Tetrahydronaphthalene (tetralin), degradation, 337, 338 Thermophiles, 75 Thiocarbamate, metabolism, 322−323 Thiocyanate, metabolism, 324 Thiol reduction, 27 Thiophene-2-carboxylate, aerobic degradation, 523, 524 Threshold concentration, degradation, 212 Thymidylate synthetase, gratuitous dehalogenation, 541 Thymine, aerobic degradation, 540 TiO2 surface, photochemical degradation, 10 α-tocopherol, nitrated metabolite from nitrite, 57 Toluene as metabolite phenylalanine, anaerobic, 317 TNT − nitrogen source, 511 Toluene/phenol enzyme induction for trichloroethene degradation, 197 Toluene/phenol oxygenase induction for chloroethene remediation, 682−683, 683 Toluene 2,3-dioxygenase marker, indigo production, 611 Toluene activation to benzyl radical, 390−391 EPR application, 289 aerobic degradation, 387−388

Index chromosomal, 387 methyl oxidation, 387 ring dioxygenation, 387 amino acid anaerobic metabolite, 317 anaerobic degradation, 389−391 [13C], 630 benzylsuccinate marker, 267 condensation reactions, 390 methyl group dehydrogenation, 389 degradation desorption as limiting factor, 209 low oxygen concentration, 203 2,3-dioxygenase, 387 monooxygenation, 107−108, 387−388 plasmid-borne degradation, 387 plasmid/chromosomal genes, 226 Toluene-4-sulfonate degradation, 506 transport, 214 Toxaphene, partial anaerobic dechlorination, 370, 662 Toxic metabolites, 222−224 Toxic substrates, experimental procedures, 256 Transhalogenation, haloalkanol dehalogenase, 362 Transport mechanisms, 214−215 systems benzoate, 214 EDTA, 215 4-chlorobenzoate, 214 2,4-dichlorophenoxyacetate, 214, 215 toluene-4-sulfonate, 214 1,2,4-triazine degradation, 546 1,3,5-triazine, nitrogen/sulfur source, 545 2,4,6-tribromophenol, anaerobic debromination, Desulfovibrio, 488 2,3,5-tribromopyrrole, product from chlorination with (Cl2)/bromide, 331 Tributyl tin aerobic transformation, 593 degradation, 3 2,2,2-trichloroacetaldehyde, dismutation, 364 Trichloroacetate aerobic degradation, 362 anaerobic transformation, Geobacter, 362 1,1,2-trichloro-1,2,2-triluoroethane, reductive dechlorination, 379−380 1,2,3-trichlorobenzene bioremediation, methane monooxygenase, 663 1,2,4-trichlorobenzene, degradation, 456, 457 concentration dependence, 219 2,3,5-trichlorobenzoate, anaerobic dechlorination, 475 1,2,3-trichlorodibenzo[1,4]dioxin, dioxygenation, 558 1,1,1-trichloroethane photochemical transformation, 6 reentry of tropospheric products, 19 Trichloroethene metabolism aerobic degradation isotope fractionation, 631 toluene/phenol induction, 197 anaerobic dechlorination, δ13C, 631 electron donors, 685 ethene production, 685

709 dehalogenase, 684 non-established dechlorinating taxa, 685 metabolism, hybrid poplar, 98, 603 methane/ammonia-oxidizing bacteria, 624 monooxygenation, 364, 365 population analysis, 624 removal hybrid poplar, 685 stimulated degradation, grass, 605 TiO2 photochemical degradation, 10 toluene-2-monoxygenase probe, 624 zero-valent iron transformation, 26 Trichloroluoromethane cytochrome P450 degradation, 379 reductive dechlorination, Methanosarcina, 379 2,4,5-trichlorophenol degradation, 484, 485monooxygenation, 112 2,4,6-trichlorophenol degradation, 484, 485 polyoxometalate, 10 population, analysis, 625 pristine environment, 216 monooxygenation, 112 1,2,3-trichloropropane, aerobic degradation, 365 3,5,6-trichloropyridine-2-ol, aerobic degradation, 534 Triclopyr, aqueous photolysis, 3 Triclosan, MnO2 transformation, 32 Triluoroacetate, potential atmospheric photochemical product, 19 Triluoroethene, methane monooxygenase oxidation, 378, 381 Triluoromethylarenes, resistance to biodegradation, 667 Triluoromethyl benzoates cometabolism, 503 dioxygenation, 502−503 terminal metabolites, 503 3-triluoromethylbenzoate, coupled photolytic/microbial degradation, 13 3-triluoromethyl-4-nitrophenol, photochemical transformation, 5 2-triluoromethylphenol transformation, Bacillus, 503 Triluralin, photochemical degradation, 6 Trihalopropanes, degradation, 362, 365 1,2,3-trihydroxybenzene (pyrogallol), anaerobic degradation, 450 1,2,4-trihydroxybenzene dioxygenase, Phanerochaete, 129 metabolite from 2,4-dichloro- and 2,4-dinitrophenol, Phanerochaete, 129 1,3,5-trihydroxybenzene (phloroglucinol) degradation, Fusarium solani, 77 2,4,6-/3,4,5-trihydroxybenzoate, anaerobic degradation, 439 2,4,6-trihydroxypurine (uric acid) aerobic degradation, 542, 543 anaerobic degradation, 542 2,4,6-trinitrocyclohexanone, 516 2,4,6-trinitrophenol aerobic degradation, 65, 164 transformation, 516 2,4,6-trinitrotoluene (TNT) aquatic plant metabolism, 604 nitrogen source, formation of toluene, 511 reduction

710 2,4,6-trinitrotoluene (TNT) (contd.) additional fermentable substrates, 675 amine polymerization, 675 Clostridium, 509 Myriophyllum spicatum, 98 Triphenyltin, pyoverdine transformation to benzene, 593 Tropic acid, degradation, 434 Tropospheric reactions, 14−15 Tryptophan degradation, 524−526 3-hydroxykynurenine pathway, 526 quinolone pathway, 526 Tryptophan dioxygenase, 124 Tryptophanase, 525 Tungsten enzymes, 187−188 Tyrosine, degradation, 426

U Uracil, degradation aerobic, 540 anaerobic, 541 α,β-unsaturated nitro compound, reduction, 586 Urease, 182 Urocanase, 523

Index Volatile substrates, experimental procedures, 257 Volatilization, contaminants, 601

W Water solubility, determinant, 213 White-rot fungi bioremediation, 622 degradation, 76−77 oxidation systems hydroxylase, 414 monooxygenase, 414 peroxidase, 414

X Xanthine dehydrogenase, 130, 544 Xanthine, central anaerobic metabolite, 544 Xanthone, aerobic degradation, 555, 556 Xylene/cresol, anaerobic degradation, enrichment factors, 630 Xylene aerobic degradation, 388−389 anaerobic degradation methylbenzylsuccinate markers, 681 sulfate-reduction, 391 Xylenols, aerobic degradation, 446

V Vanadium enzymes, 188 Vanillate, aerobic degradation, 433 Vanillyl alcohol degradation, oxidase, 133 Verrumicrobia, 58 Vibrionaceae, degradation, 69 Vinyl chloride aerobic degradation, 307 epoxidation, 364−365 metabolite, anaerobic dechlorination, 366, 367 microbial hydrolysis, 364 recalcitrance, 684 Vitamin additives, 254

Y Yeasts alkane, degradation, 78, 303 aromatic substrate degradation, 77−78 biphenyl, hydroxylation/ring ission, Paecilomyces, 77, 558 ring ission, 5-chloropyrogallol, Candida, 487

Z Zero-valent iron reduction, 25