THE APPLICATION OF MOLECULAR METHODS INCLUDING STABLE ISOTOPE PROBING TO IDENTIFY THE MICROORGANISMS INVOLVED IN TOLUENE AND MTBE DEGRADATION IN MIXED MICROBIAL SYSTEMS By Weimin Sun A DISSERTATION Submitted to Michigan State University In partial fulfillment of the requirements for the degree of DOCTORAL OF PHILOSOPHY Environmental Engineering 2012 ABSTRACT THE APPLICATION OF MOLECULAR METHODS INCLUDING STABLE ISOTOPE PROBING TO IDENTIFY THE MICROORGANISMS INVOLVED IN TOLUENE AND MTBE DEGRADATION IN MIXED MICROBIAL SYSTEMS BY Weimin Sun Sites containing leaking underground storage tanks (LUST sites) are a national problem, with over 443 568 releases confirmed as of 2003, resulting in BTEX (benzene, toluene, ethylbenzene, xylenes) or oxygenate (e.g. MTBE or TBA) contamination. These chemicals are a threat to drinking water supplies because of their human health effects and relatively high aqueous solubilities. Bioremediation can be a cost-effective method to remove such groundwater contaminants either through natural attenuation or by advanced engineering methods. Understanding the microbial processes involved in the biodegradation of BTEX and MTBE has the potential to improve the efficiency of LUST site remediation. The overall aims of this project were to: 1) characterize the microorganisms able to degrade toluene under a range of redox conditions from a variety of soil and sediment sources using stable isotope probing (SIP); 2) investigate the diversity of the bssA and bamA genes in a wide range of anaerobic toluene-degrading consortia; and 3) identify the microorganisms able to transform MTBE anaerobically using SIP. The first study in this research involved using SIP to identify the active members in an aerobic toluene degrading consortium. Specifically, SIP was used with terminal restriction fragment length polymorphism (TRFLP) and the results indicated that a 313 bp terminal restriction fragment (T-RF) incorporated the majority of the 13 C from 13 C labeled toluene. Sequencing of 16S rRNA genes from these communities indicated the organism represented by this T-RF was a Polaromonas spp. Real-time PCR was also utilized to provide quantitative patterns in gradient fractions and document increases in Polaromonas populations as toluene was degraded. In the second study, SIP was applied to five toluene-degrading consortia under sulfate and nitrate amended conditions. In all, five different phylotypes were found to be responsible for toluene degradation and these included previously identified toluene degraders as well as novel toluene degrading microorganisms. In nitrate amended microcosms, inoculated from granular sludge, microorganisms classifying within the genus Thauera were the primary toluene degraders. Whereas in nitrate amended microcosms, inoculated from a different source (agricultural soil), microorganisms in the family Comamonadaceae (genus unclassified) were the key degraders. In one set of sulfate amended microcosms (agricultural soil), the primary degrader affiliated within the class Clostridia (genus Desulfosporosinus), while in other sulfate amended microcosms, the primary degraders affiliated with the class Deltaproteobacteria, classifying within the families Syntrophobacteraceae (digester sludge) or Desulfobulbaceae (contaminated soil) (genus unclassified for both). The third study involved an investigation into the diversity of anaerobic toluene-degrading functional genes (bssA and bamA genes) in a number of inocula sources. The results suggest that targeting the bamA and bssA genes in a quantitative or non-quantitative manner could be a productive approach for investigating toluene biodegradation potential over a range of samples and redox conditions. The final study involved using SIP to investigate the dominant degraders in an anaerobic MTBE degrading microcosms. These experiments indicated bacteria in the phyla Firmicutes (family Ruminococcaceae) and Alphaproteobacteria (genus Sphingopyxis) were the dominant MTBE degraders in a methanogenic MTBE-degrading consortium seeded from activated sludge. ACKNOWLEDGEMENTS There are many people who have made my research possible, by giving me guidance and lending me their time and moral support. I would like to thank and acknowledge these people who have made my research experience an opportunity for personal growth, while allowing me to contribute to the field. First and foremost, I would like to extend my appreciation to my advisor, Dr. Alison Cupples for her encouragement, patience, research ideas, manuscript revisions, personal guidance and giving me the opportunity to explore different areas of interest in these five years of my PhD study. I would also like to thank my other committee members, Dr. Thomas Voice, Dr. Syed Hashsham and Dr. Terence Marsh, for taking the time to review my work and suggest areas of improvement. Also, I would like to express my appreciation to Dr. Marsh for the use of his laboratory and software. I am very thankful for the help from the members in Dr. Cupples' lab, Shuguang Xie, Chunlin Luo, Indumathy Jayamani, Fernanda Paes and Xiaoxu Sun. This work would not have been possible without such support. I would also like to express my appreciation to Alla Alpatova and Kelvin Wong for their help in my dissertation completion. I owe debt and gratitude to all of the group members of Dr. Hashsham and Dr. Xagoraraki, for the use of their equipment and for sharing great research ideas. I would like to give special thanks to Xiaoxu Sun, who has helped me tremendously and was willing to stay with me doing bench work late at night. I want to thank my good friends Jie Niu, Pin Gao, Biao Chang, Tan Zhao, Liyan Song, Fulin Wang and Xufeng Xu for their kind help and valuable research ideas. Finally, I would like to thank my parents and my girlfriend for their support and encouragement during the past years. iv TABLE OF CONTENTS LIST OF TABLES........................................................................................................................ vii LIST OF FIGURES ....................................................................................................................... ix ABBREVIATIONS ..................................................................................................................... xiii CHAPTER 1 ................................................................................................................................... 1 INTRODUCTION .......................................................................................................................... 1 MTBE and BTEX contamination ............................................................................................ 1 Stable isotope probing (SIP) .................................................................................................... 1 The functional gene responsible for anaerobic toluene biodegradation .................................. 2 Objectives ................................................................................................................................ 3 References:............................................................................................................................... 7 CHAPTER 2 ................................................................................................................................. 11 TOLUENE DEGRADATION IN CONTAMINATED SITE MICROCOSMS IS DIRECTLY LINKED TO A POLAROMONAS STRAIN............................................................................... 11 Introduction............................................................................................................................ 11 MATERIALS AND METHODS........................................................................................... 13 Experimental design, microcosm setup and chemical analyses...................................... 13 DNA extraction ............................................................................................................... 14 DNA ultracentrifugation ................................................................................................. 15 PCR and TRFLP ............................................................................................................. 15 16S rRNA gene sequencing ............................................................................................ 16 Real-time PCR ................................................................................................................ 17 RESULTS AND DISCUSSION ............................................................................................ 18 References.............................................................................................................................. 31 CHAPTER 3 ................................................................................................................................. 33 DIVERSITY OF TOLUENE DEGRADING MICROORGANIMS AND THE BSSA GENE IN FIVE NITRATE OR SULFATE AMENDED MICROBIAL COMMUNITIES INVESTIGATED USING STABLE ISOTOPE PROBING (SIP)............................................................................. 33 Introduction............................................................................................................................ 33 Materials and Methods........................................................................................................... 35 Development of Toluene Degrading Microcosms .......................................................... 35 Analytical Techniques..................................................................................................... 37 DNA Extraction and Ultracentrifugation ........................................................................ 37 PCR and TRFLP ............................................................................................................. 38 Presence of bssA in Microcosms and Enumeration in SIP Fractions ............................. 38 Sequencing of Partial bssA and 16S rRNA Genes.......................................................... 39 Results.................................................................................................................................... 40 Frequency of Toluene Degradation................................................................................. 40 v SIP on Agricultural Soil Nitrate Amended Microcosms (AgN) ..................................... 41 SIP on the Granular Sludge Nitrate Amended Microcosms (GNS)................................ 42 SIP on the Agricultural Soil Sulfate Amended Microcosms (AgS) ................................ 43 SIP on the Digester Sludge Sulfate Amended Microcosms (DSS)................................. 43 SIP on Gas Compressor Site Soil Sulfate Amended Microcosms (CSS) ....................... 44 Partial Sequencing of the bssA Gene .............................................................................. 45 Quantification of bssA Genes in SIP Fractions............................................................... 46 Discussion .............................................................................................................................. 46 Acknowledgements................................................................................................................ 52 References.............................................................................................................................. 79 CHAPTER 4 ................................................................................................................................. 85 PRESENCE,DIVERSITY AND THE ENUMERATION OF TOLUENE DEGRADING FUNCTIONAL GENES (BSSA AND BAMA) ACROSS A RANGE OF REDOX CONDITIONS AND INOCULUM SOURCES .................................................................................................... 85 Introduction............................................................................................................................ 85 Materials and Methods........................................................................................................... 87 Screening of Toluene Degrading Microcosms................................................................ 87 DNA Extraction and PCR ............................................................................................... 88 Quantitative PCR ............................................................................................................ 89 Sequencing of Partial bssA and bamA Genes ................................................................. 90 Results.................................................................................................................................... 90 bssA and bamA Gene Amplification ............................................................................... 91 bssA and bamA Gene Quantification .............................................................................. 92 Discussion .............................................................................................................................. 94 References............................................................................................................................ 109 CHPATER 5 ................................................................................................................................111 ANAEROBIC MTBE DEGRADING MICROORGANISMS IDENTIFIED IN WASTEWATER TREATMENT PLANT SAMPLES USING STABLE ISOTOPE PROBING ...........................111 Introduction...........................................................................................................................111 Methods................................................................................................................................ 113 Microcosm Construction and Analytical Techniques ................................................... 113 DNA Extraction and Ultracentrifugation ...................................................................... 114 PCR, TRFLP and Sequencing of 16S rRNA Genes...................................................... 115 Results and Discussion ........................................................................................................ 116 References............................................................................................................................ 130 vi LIST OF TABLES Table 2.1. Average percent toluene remaining in control and sample microcosms (error bars represent standard deviations represent from triplicates). ..................................................... 24 Table 2.2. Comparison of dominant fragments in heavy fraction TRFLP to clone restriction enzyme cut sites predicted from sequence analyses. .............................................................. 25 Table 3.1. Primers used in this study to investigate the presence of the bssA gene ...................... 53 Table 3.2. Phylogenetic affiliation of each 16S rRNA clone in nitrate amended toluene degrading microcosms as determined with the RDP analysis tool “classifier” ....................................... 54 Table 3.3. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment length from in silico sequence analyses (nitrate amended agricultural soil microcosms)............................................................................................................................ 56 Table 3.4. Comparison of fragment length of dominant T-RFs in heavy fractions to predicted fragment lengths from in silico sequence analyses (nitrate amended granular sludge microcosms)............................................................................................................................ 57 Table 3.5. Phylogenetic affiliation of each 16S rRNA clone in sulfate amended toluene degrading microcosms as determined with the RDP analysis tool “classifier” ....................................... 58 Table 3.6. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment lengths from in silico sequence analyses (sulfate amended agricultural soil microcosms)............................................................................................................................ 60 Table 3.7. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment lengths from in silico sequence analyses (digester sludge sulfate amended microcosms)............................................................................................................................ 61 Table 3.8. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment lengths from in silico sequence analyses (sulfate amended contaminated site soil microcosms)............................................................................................................................ 62 Table 3.9. Success (+) or failure (-) of primers sets for bssA gene amplification. ........................ 63 Table 4.1. Success of bssA and bamA primers, amplicons cloned and the consortia targeted for qPCR. .................................................................................................................................... 101 Table 5.1. Summary of the investigations conducted on the anaerobic degradation of MTBE in different inoculum types ....................................................................................................... 122 Table 5.2. Phylogenetic affiliation of bacterial 16S rRNA clone in methanogenic MTBE vii degrading microcosms as determined with the RDP analysis tool “classifier” .................... 123 Table 5.3. Phylogenetic affiliation of Archaeal 16S rRNA clone in methanogenic MTBE degrading microcosms as determined with the RDP analysis tool “classifier” .................... 124 Table 5.4. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment length from in silico sequence analyses ................................................................ 125 viii LIST OF FIGURES -1 Figure 2.1. Comparison of TRFLP electropherograms of heavier fractions (>1.736 g mL ) between DNA obtained from labeled and unlabeled toluene amended microcosms, illustrating the dominance of TFRLP fragment 313 bp in fractions from the labeled toluene amended microcosms. A similar pattern was observed in the soil 1 replicate and in replicates of soil 2...................................................................................................... 26 Figure 2.2. Difference between abundance of Polaromonas sp. rRNA gene copies in 13 ultracentrifugation fractions from labeled ( C toluene) and unlabeled toluene amended microcosms from soil 2 as determined via qPCR. Fractions obtained from soil 1 illustrated a similar trend. ............................................................................................... 27 Figure 2.3. Correlation between Polaromonas sp. 16S rRNA gene copies (determined by qPCR) and toluene removal over time in live samples and no-toluene controls (microcosms constructed ...................................................................................................................... 28 Figure 2.4. Benzene, m-xylene and cis-dichloroethene (cDCE) concentrations over time in supernatant of microcosms samples and in autoclaved controls (error bars represent standard deviations). ....................................................................................................... 29 Figure 3.1. Percent relative abundance of fragments (digested by Hae III) assigned to Comamonadaceae within buoyant density gradients of DNA extracted from the nitrate 13 amended agricultural soil microcosms. Figure symbols: ▲ C-toluene (~33% toluene 13 13 degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene 12 degraded); □ C-toluene (~100% toluene degraded). ................................................... 64 Figure 3.2. Percent relative abundance of fragments (digested by Hae III) assigned to Azoarcus within buoyant density gradients of DNA extracted from the nitrate amended agricultural 13 soil microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); 13 13 ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); 12 □ C-toluene (~100% toluene degraded). ....................................................................... 65 Figure 3.3. Percent relative abundance of fragments (digested by Hae III) assigned to Thauera, within buoyant density gradients of DNA extracted from the nitrate amended granular 13 sludge microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); 13 13 ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); 12 □ C-toluene (~100% toluene degraded). ....................................................................... 66 Figure 3.4. Percent relative abundance of fragments (digested by Hae III) assigned to Desulfosporosinus with T-RF 77 bp within buoyant density gradients of DNA extracted 13 from the agricultural soil sulfate amended microcosms. Figure symbols: ▲ C-toluene 13 13 (~33% toluene degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene ix 12 (~100% toluene degraded); □ C-toluene (~100% toluene degraded). .......................... 67 Figure 3.5. Percent relative abundance of fragments (digested by Hae III) assigned to Desulfosporosinus with T-RF 213 bp within buoyant density gradients of DNA extracted 13 from the agricultural soil sulfate amended microcosms. Figure symbols: ▲ C-toluene 13 13 (~33% toluene degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene 12 (~100% toluene degraded); □ C-toluene (~100% toluene degraded). ........................... 68 Figure 3.6. Percent relative abundance of fragments (digested by Hae III) assigned to Syntrophobacteraceae within buoyant density gradients of DNA extracted from the 13 digester sludge sulfate amended microcosms. Figure symbols: ▲ C-toluene (~33% 13 13 toluene degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% 12 toluene degraded); □ C-toluene (~100% toluene degraded). ........................................ 69 Figure 3.7. Percent relative abundance of fragments (digested by Hae III) assigned to Desulfobulbaceae within buoyant density gradients of DNA extracted from the 13 contaminated site, sulfate amended microcosms. Figure symbols: ▲ C-toluene (~33% 13 13 toluene degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% 12 toluene degraded); □ C-toluene (~100% toluene degraded). ........................................ 70 Figure 3.8. Phylogenetic tree of bssA partial sequences (722 bp) from nitrate amended agricultural soil microcosms (using the primer set 7772f/8546r) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. ............................................................................................................................ 71 Figure 3.9. Phylogenetic tree of bssA partial sequences (722 bp) from nitrate amended granular sludge microcosms (using the primer set 7772f/8546r) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. ... 72 Figure 3. 10. Phylogenetic trees of bssA partial sequences (97 bp) from sulfate amended digester sludge microcosms (using the primer set SRBf/SRBr) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. ... 73 Figure 3.11. Phylogenetic trees of bssA partial sequences (637 bp) from sulfate amended contaminated soil microcosms (using the primer set 7772f/8828r) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. ............................................................................................................................ 74 Figure 3.12. Difference between abundance of bssA gene copies in ultracentrifugation fractions 13 from labeled ( C toluene) and unlabeled toluene amended microcosms from the granular sludge nitrate amended microcosms as determined via qPCR. Figure symbols: 13 12 ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded)..... 75 Figure 3.13. Difference between abundance of bssA gene copies in ultracentrifugation fractions x 13 from labeled ( C toluene) and unlabeled toluene amended microcosms from the agricultural soil nitrate amended microcosms as determined via qPCR. Figure symbols: 13 12 ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded)..... 76 Figure 3.14. Difference between abundance of bssA gene copies in ultracentrifugation fractions 13 from labeled ( C toluene) and unlabeled toluene amended microcosms from the digester sludge sulfate amended microcosms as determined via qPCR. Figure symbols: 13 12 ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded)..... 77 Figure 4. 1. Gene numbers of bssA and bamA during toluene degradation in nitrate amended microcosms AgN. The error bars represent standard deviations form triplicate qPCR samples......................................................................................................................... 102 Figure 4.2. Gene numbers of bssA and bamA during toluene degradation in nitrate amended microcosms BoN1. The error bars represent standard deviations form triplicate qPCR samples. ......................................................................................................................... 103 Figure 4.3. Gene numbers of bssA and bamA during toluene degradation in nitrate amended microcosms GSN. The error bars represent standard deviations form triplicate qPCR samples. ......................................................................................................................... 104 Figure 4.4. Gene numbers of bssA and bamA during toluene degradation in a sulfate amended microcosm, DUKE.The error bars represent standard deviations form triplicate qPCR samples. ......................................................................................................................... 105 Figure 4.5. Gene numbers of bssA and bamA during toluene degradation in a methaongeic microcosm, ASM. The error bars represent standard deviations form triplicate qPCR samples. ......................................................................................................................... 106 Figure 4.6. Gene numbers of bssA and bamA during toluene degradation in a methaongeic microcosm, HM. The error bars represent standard deviations form triplicate qPCR samples. ......................................................................................................................... 107 12 Figure 5.1. MTBE concentration over time in C-MTBE amended abiotic controls (♦), 13 12 C-MTBE (■) and C-MTBE (□) amended samples. The arrows indicate when DNA was extracted. The error bars represent standard deviations from triplicate microcosms. ..................................................................................................................................... 126 Figure 5.2. Percent relative abundance of fragments (digested by Hae III) assigned to Clostridiales within buoyant density gradients of Bacterial DNA extracted from the 13 methanogenic activated sludge microcosms. Figure symbols: ♦ C-MTBE (~30% 13 12 toluene degraded); ■ C-MTBE (~70% toluene degraded); □ C-MTBE (~70% toluene degraded). ...................................................................................................................... 127 Figure 5.3. Percent relative abundance of fragments (digested by Hae III) assigned to xi Sphingomonadales within buoyant density gradients of Bacterial DNA extracted from 13 the methanogenic activated sludge microcosms. Figure symbols: ♦ C-MTBE (~30% 13 12 toluene degraded); ■ C-MTBE (~70% toluene degraded); □ C-MTBE (~70% toluene degraded). ...................................................................................................................... 128 Figure 5.4. Percent relative abundance of fragments (digested by Hae III) assigned to Methanosarcina within buoyant density gradients of Archaeal DNA extracted from the 13 methanogenic activated sludge microcosms. Figure symbols:■ C-MTBE (~70% 12 toluene degraded); □ C-MTBE (~70% toluene degraded). ......................................... 129 Figure 5.5. Percent relative abundance of fragments (digested by Hae III) assigned to Methanocorpusculum within buoyant density gradients of Archaeal DNA extracted from 13 the methanogenic activated sludge microcosms. Figure symbols:■ C-MTBE (~70% 12 toluene degraded); □ C-MTBE (~70% toluene degraded). ......................................... 130 xii ABBREVIATIONS bamA- the gene encoding 6-oxocyclohex-1-ene-1-carBoN1yl-CoA hydrolase BSS - benzylsuccinate synthase, a glycyl radical enzyme catalyzing the first step in anaerobic toluene degradation BssA- α-subunit of benzyl succinate synthase bssA - the gene encoding BssA BTEX - benzene, toluene, ethylbenzene and o-, p-, and m-xylenes DNA - deoxyribonucleic acid MTBE - methyl tertiary butyl ether OTU - operational taxonomic unit PCR - polymerase chain reaction qPCR- quantitative PCR rDNA - ribosomal DNA TBA - tertiary butyl alcohol TRFLP - terminal restriction fragment length polymorphism xiii CHAPTER 1 INTRODUCTION MTBE and BTEX Contamination The chemicals benzene, toluene, ethylbenzene and xylene (BTEX) and MTBE (a fuel oxygenate) are frequently the major pollutants at gasoline contaminated sites (leaking underground storage tank sites or LUST sites) (24). In the United states, 50 states have reported MTBE in groundwater, surface water and drinking water (29). Bioremediation can be a cost-effective method to remove groundwater contaminants either through natural attenuation or by advanced engineering methods. Understanding the microbial processes involved in the biodegradation of BTEX and MTBE has the potential to improve the efficiency of LUST site remediation. Stable Isotope Probing (SIP) Although many BTEX degraders have been identified through enrichment and isolation procedures, a question arises that culturing microorganisms may not fully reflect the microbial diversity (2, 3, 30). Stable isotope probing (SIP) is a novel molecular method which can link the function to active microbial members in environmental samples or directly in field studies. The application of SIP has the potential to increase our understanding of function in mixed microbial systems and its use has increased remarkably in recent years (9, 11, 20, 22, 23). The method consists of sample exposure to labeled substrates (e.g. 1 13 15 18 C, N, O), separation of labeled and unlabeled nucleic acids (DNA or RNA) and analysis of separated heavy (labeled) or unlabeled (background) nucleic acids. Nucleic acids can be separated by needle extraction (25, 26) or by fractionation (9, 16, 21). Functional Genes for Anaerobic Toluene Degradation The gene encoding for the enzyme benzylsuccinate synthase has been linked to anaerobic toluene degradation under nitrate reducing (1, 15), sulfate reducing (32-34), ferric iron reducing (7, 10), and methanogenic enrichment cultures or environmental samples (31, 32). The enzyme benzylsuccinate synthase catalyzes the first step of anaerobic toluene degradation and involves the addition of toluene across the double bond of fumarate to produce (R)-benzylsuccinate. Benzylsuccinate is then oxidized to benzoyl-CoA and succinate via β-oxidation pathway. The final step is the recycling of the fumarate cosubstrate of benzylsuccinate synthase from succinate by succinate dehydrogenase. The overall result is an oxygen-independent reaction (6). Benzylsuccinate synthase, which has been identified in denitrifying bacteria, was characterized as a novel glycyl radical enzyme (19). The enzyme contains a big subunit, α-subunit (98 kDA) and two small subunits β (8.6 kDa) and γ (6.6 kDa); bssA encodes the large α subunits while bssB and bssC encode the other two small subunits, β and γ (13). A limited number of bssA sequences from pure cultures are available to date (1, 8, 10, 14, 19, 27, 28). Previous studies have developed PCR methodologies to target the bssA gene (5, 12) and the current work involved using these methods to amplify the functional gene. The other functional gene investigated in this research was previously reported to be important for the degradation of aromatics. Anaerobic aromatic biodegradation typically involves the 2 channeling of aromatic growth substrates to the central intermediate benzoyl-coenzyme A (CoA) prior to dearomatization and ring cleavage (17). In Thauera aromatica, the metabolism of benzoyl-CoA comprises of several steps with ring cleavage action by 6-oxocylcohex-1-ene-1-carbonyl-CoA (6-OCH-CoA) hydrolase, which likely catalyzes the transformation of 6-OCH-CoA to 6-hydroxypimelyl-CoA (17, 18). The ring-cleaving hydrolase of the benzoyl-CoA pathway is encoded by the bamA gene. Recently, this pathway was studied in obligate anaerobes that use aromatic growth substrates (17). Objectives The overall objectives of this project were: 1) To characterize the microorganisms able to degrade toluene under a range of redox conditions (aerobic, nitrate and sulfate reducing and methanogenic) from a variety of soil and sediment sources using stable isotope probing (SIP) (Chapters 2 and 3). 2) To investigate the diversity of the bssA gene (encodes for benzylsuccinate synthase α unit) and bamA genes (encodes for the ring-cleaving hydrolase of the benzoyl-CoA pathway) in a wide range of anaerobic toluene-degrading consortia (Chapter 4); 3) To identify the organisms able to transform MTBE anaerobically using SIP (Chapter 5). Chapter 2 describes the work targeting aerobic toluene degradation and also describes the SIP methodology used throughout the thesis. In summary, the work identified members of 3 Polaromonas as the key aerobic toluene-degrading bacteria. This conclusion was also supported by quantitative PCR (qPCR) results. A modified version of Chapter 2 was published in Applied and Environmental Microbiology. The same SIP methodology was used in Chapter 3 to investigate diversity of microorganisms able to uptake carbon from toluene in a diverse number of samples under sulfate and nitrate amended conditions. In these studies, different microorganisms were identified as toluene degraders. Microorganisms classifying within the family Comamonadaeae and the genus Thauera were pinpointed in nitrate amended microcosms seeded from agricultural soil and granular sludge, respectively. Members of Desulfosporosinus, Syntrophaceae, Desulfobulbaceae were identified from agricultural soil, digester sludge and contaminated aquifer sediment as toluene degraders under sulfate amended conditions. A modified version of Chapter 3 was published in Applied and Environmental Microbiology. The work described in Chapter 4 focuses on previously designed primer pairs to amplify the bssA and bamA genes. The bssA phylogenetic information was also related to the toluene degraders identified via SIP in Chapter 3. In Chapter 4, I tested a range of bssA- and bamAprimers on 16 toluene-degrading consortia. Two primer pairs, 7772f/8546r and SRBr/SRBf, exhibited good coverage for nitrate amended samples and sulfate amended samples, respectively. The bamA primer set (bam-sp9 and bam-asp1) produced a strong amplicon in DNA extracted from all except one microcosm. Partial bssA and bamA sequences were obtained for a number of samples (four bssA and six bamA sequences) and compared to those available in GenBank. The partial bssA sequences (from nitrate amended and methanogenic microcosms) were most similar 4 to Thauera sp. DNT-1, Thauera aromatica, Aromatoleum aromaticum EbN1 and bssA clones from a study involving sulfate reducing toluene degradation. The bamA sequences obtained could be placed into five clades. In Chapter 5, SIP was utilized on a methanogenic MTBE-degrading consortium. The SIP experiments indicated bacteria in the phyla Firmicutes (family Ruminococcaceae) and Alphaproteobacteria (genus Sphingopyxis) were the dominant MTBE degraders. Previous studies on have suggested a role for Firmicutes in anaerobic MTBE degradation, however the Alphaproteobacteria phylotype represents a novel MTBE degrader. Two archaeal phylotypes (genera Methanosarcina and Methanocorpusculum) were also enriched in the heavy fractions and these organisms may be responsible for minor amounts of MTBE degradation or for the uptake of metabolites released from the primary MTBE degraders. The work described in Chapters 5 was published in Applied and Environmental Microbiology. 5 REFERENCES 6 References 1. Achong, G. R., A. M. Rodriguez, and A. M. Spormann. 2001. Benzylsuccinate synthase of Azoarcus sp strain T: Cloning, sequencing, transcriptional organization, and its role in anaerobic toluene and m-xylene mineralization. J Bacteriol 183:6763-6770. 2. Akkermans, A. D. L., M. S. Mirza, H. J. M. Harmsen, H. J. Blok, P. R. Herron, A. Sessitsch, and W. M. Akkermans. 1994. Molecular Ecology of Microbes - a Review of Promises, Pitfalls and True Progress. Fems Microbiol Rev 15:185-194. 3. Ampe, F., N. Ben Omar, C. Moizan, C. Wacher, and J. P. Guyot. 1999. Polyphasic study of the spatial distribution of microorganisms in Mexican pozol, a fermented maize dough, demonstrates the need for cultivation-independent methods to investigate traditional fermentations. Applied and Environmental Microbiology 65:5464-5473. 4. Baehr, A. L., P. E. Stackelberg, and R. J. Baker. 1999. Evaluation of the atmosphere as a source of volatile organic compounds in shallow groundwater. Water Resources Research 35:127-136. 5. Beller, H. R., S. R. Kane, T. C. Legler, J. R. McKelvie, B. S. Lollar, F. Pearson, L. Balser, and D. M. MacKay. 2008. Comparative assessments of benzene, toluene, and xylene natural attenuation by quantitative polymerase chain reaction analysis of a catabolic gene, signature metabolites, and compound-specific isotope analysis. Environ Sci Technol 42:6065-6072. 6. Boll, M., G. Fuchs, and J. Heider. 2002. Anaerobic oxidation of aromatic compounds and hydrocarbons. Curr Opin Chem Biol 6:604-611. 7. Botton, S., M. van Harmelen, M. Braster, J. R. Parsons, and W. F. M. Roling. 2007. Dominance of Geobacteraceae in BTX-degrading enrichments from an iron-reducing aquifer. Fems Microbiol Ecol 62:118-130. 8. Coschigano, P. W., T. S. Wehrman, and L. Y. Young. 1998. Identification and analysis of genes involved in anaerobic toluene metabolism by strain T1: Putative role of a glycine free radical. Applied and Environmental Microbiology 64:1650-1656. 9. Cupples, A. M., and G. K. Sims. 2007. Identification of in situ 2,4-dichlorophenoxyacetic acid-degrading soil microorganisms using DNA-stable isotope probing. Soil Biology & Biochemistry 39:232-238. 10. Kane, S. R., H. R. Beller, T. C. Legler, and R. T. Anderson. 2002. Biochemical and genetic evidence of benzylsuccinate synthase in toluene-degrading, ferric iron-reducing Geobacter metallireducens. Biodegradation 13:149-154. 7 11. Kasai, Y., Y. Takahata, M. Manefield, and K. Watanabe. 2006. RNA-based stable isotope probing and isolation of anaerobic benzene-degrading bacteria from gasoline-contaminated groundwater. Applied and Environmental Microbiology 72:3586-3592. 12. Kazy, S. K., A. L. Monier, and P. J. J. Alvarez. 2010. Assessing the correlation between anaerobic toluene degradation activity and bssA concentrations in hydrocarbon-contaminated aquifer material. Biodegradation 21:793-800. 13. Krieger, C. J., W. Roseboom, S. P. J. Albracht, and A. M. Spormann. 2001. A stable organic free radical in anaerobic benzylsuccinate synthase of Azoarcus sp strain T. J Biol Chem 276:12924-12927. 14. Kube, M., J. Heider, J. Amann, P. Hufnagel, S. Kuhner, A. Beck, R. Reinhardt, and R. Rabus. 2004. Genes involved in the anaerobic degradation of toluene in a denitrifying bacterium, strain EbN1. Arch Microbiol 181:182-194. 15. Kuhner, S., L. Wohlbrand, I. Fritz, W. Wruck, C. Hultschig, P. Hufnagel, M. Kube, R. Reinhardt, and 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. 16. Kunapuli, U., T. Lueders, and R. U. Meckenstock. 2007. The use of stable isotope probing to identify key iron-reducing microorganisms involved in anaerobic benzene degradation. Isme Journal 1:643-653. 17. Kuntze, K., Y. Shinoda, H. Moutakki, M. J. McInerney, C. Vogt, H. H. Richnow, and M. Boll. 2008. 6-Oxocyclohex-1-ene-1-carbonyl-coenzyme A hydrolases from obligately anaerobic bacteria: characterization and identification of its gene as a functional marker for aromatic compounds degrading anaerobes. Environmental Microbiology 10:1547-1556. 18. Laempe, D., M. Jahn, and G. Fuchs. 1999. 6-hydroxycyclohex-1-ene-1-carbonyl-CoA dehydrogenase and 6-oxocycsohex-1-ene-1-carbonyl-CoA hydrolase, enzymes of the benzoyl-CoA pathway of anaerobic aromatic metabolism in the denitrifying bacterium Thauera aromatica. European Journal of Biochemistry 263:420-429. 19. Leuthner, B., C. Leutwein, H. Schulz, P. Horth, W. Haehnel, E. Schiltz, H. Schagger, and J. Heider. 1998. Biochemical and genetic characterization of benzylsuccinate synthase from Thauera aromatica: a new glycyl radical enzyme catalysing the first step in anaerobic toluene metabolism. Molecular Microbiology 28:615-628. 20. Lin, J. L., S. Radajewski, B. T. Eshinimaev, Y. A. Trotsenko, I. R. McDonald, and J. C. Murrell. 2004. Molecular diversity of methanotrophs in Transbaikal soda lake sediments and identification of potentially active populations by stable isotope probing. 8 Environmental Microbiology 6:1049-1060. 21. Lu, Y. H., and R. Conrad. 2005. In situ stable isotope probing of methanogenic archaea in the rice rhizosphere. Science 309:1088-1090. 22. Lueders, T., M. Manefield, and M. W. Friedrich. 2004. Enhanced sensitivity of DNAand rRNA-based stable isotope probing by fractionation and quantitative analysis of isopycnic centrifugation gradients. Environmental Microbiology 6:73-78. 23. Lueders, T., B. Wagner, P. Claus, and M. W. Friedrich. 2004. Stable isotope probing of rRNA and DNA reveals a dynamic methylotroph community and trophic interactions with fungi and protozoa in oxic rice field soil. Environmental Microbiology 6:60-72. 24. Mcallister, P. M., and C. Y. Chiang. 1994. A Practical Approach to Evaluating Natural Attenuation of Contaminants in-Ground Water. Ground Water Monit R 14:161-173. 25. Morris, S. A., S. Radajewski, T. W. Willison, and J. C. Murrell. 2002. Identification of the functionally active methanotroph population in a peat soil microcosm by stable-isotope probing. Applied and Environmental Microbiology 68:1446-1453. 26. Radajewski, S., G. Webster, D. S. Reay, S. A. Morris, P. Ineson, D. B. Nedwell, J. I. Prosser, and J. C. Murrell. 2002. Identification of active methylotroph populations in an acidic forest soil by stableisotope probing. Microbiol-Sgm 148:2331-2342. 27. Shinoda, Y., J. Akagi, Y. Uchihashi, A. Hiraishi, H. Yukawa, H. Yurimoto, Y. Sakai, and N. Kato. 2005. Anaerobic degradation of aromatic compounds by Magnetospirillum strains: Isolation and degradation genes. Bioscience Biotechnology and Biochemistry 69:1483-1491. 28. Shinoda, Y., Y. Sakai, H. Uenishi, Y. Uchihashi, A. Hiraishi, H. Yukawa, H. Yurimoto, and N. Kato. 2004. Aerobic and anaerobic toluene degradation by a newly isolated denitrifying bacterium, Thauera sp. strain DNT-1. Applied and Environmental Microbiology 70:1385-1392. 29. Stephenson, J. 2002. MTBE Contamination From Underground Storage Tanks. 30. Temmerman, R., I. Scheirlinck, G. Huys, and J. Swings. 2003. Culture-independent analysis of probiotic products by denaturing gradient gel electrophoresis. Applied and Environmental Microbiology 69:220-226. 31. Washer, C. E., and E. A. Edwards. 2007. Identification and expression of benzylsuccinate synthase genes in a toluene-degrading methanogenic consortium. Appl Environ Microb 73:1367-1369. 32. Winderl, C., B. Anneser, C. Griebler, R. U. Meckenstock, and T. Lueders. 2008. Depth-resolved quantification of anaerobic toluene degraders and aquifer microbial 9 community patterns in distinct redox zones of a tar oil contaminant plume. Appl Environ Microb 74:792-801. 33. Winderl, C., H. Penning, F. von Netzer, R. U. Meckenstock, and T. Lueders. 2010. DNA-SIP identifies sulfate-reducing Clostridia as important toluene degraders in tar-oil-contaminated aquifer sediment. Isme J 4:1314-1325. 34. Winderl, C., S. Schaefer, and T. Lueders. 2007. Detection of anaerobic toluene and hydrocarbon degraders in contaminated aquifers using benzylsuccinate synthase (bssA) genes as a functional marker. Environ Microbiol 9:1035-1046. 10 CHAPTER 2 TOLUENE DEGRADATION IN CONTAMINATED SITE MICROCOSMS IS DIRECTLY LINKED TO A POLAROMONAS STRAIN Introduction Sites containing leaking underground storage tanks (LUST sites) are a national problem, resulting in BTEX (benzene, toluene, ethylbenzene, xylenes) or oxygenate (e.g. MTBE or TBA) contamination and risk to sensitive receptors such as drinking water supplies. A common remediation method for such sites involves in situ biological degradation of these contaminants. Aerobic bioremediation has been favored over other electron acceptors, such as nitrate, sulfate and ferric iron, because BTEX degradation is typically faster when oxygen is available. Although many aerobic BTEX isolates have been obtained in pure culture, less is known about the organisms responsible for in situ contaminant transformation. For example, toluene transformation has been particularly well studied in a number of isolates (e.g. Pseudomonas putida F1, P. putida mt-2, P. mendocina KR1, P. stutzeri OX1, Burkholderia vietnamiensis G4, Burkholderia sp. strain JS150 and Ralstonia pickettii PK01, for review see (14)), however, information on the organisms responsible for toluene degradation in a mixed community sample is lacking. In this study, we attempt to address this knowledge gap, focusing on toluene as a model BTEX contaminant. Identification of microorganisms responsible for BTEX degradation in mixed community environmental samples should result in a better understanding of microorganisms responsible for degradation in situ. It is hoped that such information can aid in the design of remediation approaches as well as in the prediction of contaminant removal rates. 11 To identify the dominant organism responsible for toluene transformation within a mixed community sample, an approach was adopted to result in less culture bias than would be produced using repeated enrichments or isolation. Therefore, the data produced should more accurately reflect the organisms responsible for in situ toluene transformation. To do this, stable isotope probing (SIP), a method that links in situ function with identity for mixed microbial systems (15), was adopted. The method involves sample exposure to labeled compounds, separation of heavy (label incorporated) and light (background) nucleic acids using ultracentrifugation, then gene sequencing (16S rRNA) to identify the label-consuming microorganisms. For this purpose, SIP has two key advantages over traditional microbiological methods for investigating contaminant removal, as follows, (1) identification of organisms able to assimilate carbon from the contaminant, therefore selectively pinpoints efficient degraders and (2) studies can be conducted on environmental samples, thus results are much more applicable to the field environment than traditional approaches. The objective here was to identify the organisms responsible for aerobic carbon uptake from the environmental contaminant toluene in two soils obtained from a BTEX contaminated site. DNA based SIP was utilized to identify the active toluene degrader and following this, a real time PCR assay was designed to confirm these results. The results were also compared with those from previous m-xylene and benzene SIP studies on this soil (5). The research offers new insight into contaminant transformation in mixed communities. 12 MATERIALS AND METHODS Experimental design, microcosm setup and chemical analyses The gasoline-contaminated soil used in this study was collected from a gasoline-contaminated site located in Michigan. Two soil samples, obtained at different depths (3 - 4 ft and 5 - 6 ft deep) at the same site were used and are further referred to as soil 1 and soil 2. Microcosms were constructed with 6 g soil along with 20 mL phosphate-buffered mineral media (12) in a 150 mL serum bottle sealed with rubber stoppers and aluminum seals. Three sets of experiments were conducted, experiment 1 involved SIP to identify the dominant toluene degraders in both soils, experiment 2 focused on real-time PCR to confirm SIP results and investigate microorganism growth on toluene and experiment 3 involved simple biodegradation studies with other environmental contaminants (benzene, m-xylene and cis-dichloroethene). The SIP study (experiment 1) was conducted on both soils 1 and 2 and involved triplicate abiotic controls, triplicate unlabeled toluene (1 μL, 99 %, Chem Service, West Chester, PA) and 13 triplicate labeled toluene (1 μL ring- C6 toluene, 99%, Cambridge Isotope Laboratories, Inc. Andover, MA) amended samples. Experiment 2 involved sixteen sample microcosms, each with 6 g soil 2 and 20 mL media (as above). Toluene (1 μL, 99 %, Chem Service, West Chester, PA) was added to eight of these and the other eight served as no-toluene controls (to determine if toluene was needed to cause an increase in Polaromonas sp. cell numbers). At each sampling time, two samples and two controls were sacrificed for DNA extraction and qPCR. In experiment 3, for each contaminant investigated (benzene, m-xylene and cis-dichloroethene), 13 three sample microcosms and two autoclaved control microcosms were constructed using the supernatant of toluene degrading soil microcosms from soil 2. Specifically, following the depletion of toluene, 5 mL supernatant was transferred to a 150 mL serum bottle with 20 mL media (as above). Following this, either benzene (99.8%, Sigma Aldrich), cis-dichloroethene (purity not provided, Supelco) or m-xylene (99%, Sigma Aldrich) were added to a final solution -1 concentration of approximately 45 mg L . All microcosms were incubated at room temperature (~20 °C) with reciprocal shaking. Contaminant (toluene, benzene, m-xylene and cis-dichloroethene) concentrations in headspace gas samples (200 μL) were typically determined daily with a gas chromatograph (Perkin Elmer) equipped with flame ionization detector and a capillary column (J&W Scientific, DB-624, diameter 0.53mm). Injector and detector temperature were set at 200 oC and the column temperature was 120oC. DNA extraction The powersoil DNA extraction kit (MO BIO Laboratories, Inc. Carlsbad, CA) was used for soil DNA extraction in experiments 1 and 2 according to the manufacturer’s recommended procedure. Extraction times, number of samples and mass of soil extracted varied depending on the experiment. In experiment 1, DNA was extracted from the entire microcosm, whereas in experiment 2, DNA was extracted from 0.3 g soil. In experiment 1 (SIP study), for both soil 1 and soil 2, two labeled and two unlabeled microcosms were sacrificed for DNA extraction at day 7 (at this time, all toluene had been depleted). In experiment 2 (qPCR study), DNA was extracted from samples sacrificed at successive time points for the unlabeled toluene sample microcosms and no-toluene-amended control microcosms. Specifically, two sample and two control 14 microcosms were scarified at day 3, 4, 5, 6 when approximately 20 %, 50 %, 80 % and 100 % of the added toluene was transformed. DNA ultracentrifugation Approximately 10 μg DNA (quantified with Nanodrop, ND-1000) was added to Quick-Seal polyallomer tubes (13×51 mm, 5.1 ml, Beckman Coulter) along with a Tris-EDTA (TE, pH 8.0) /CsCl solution. Prior to sealing (cordless quick-seal tube topper, Beckman), the buoyant density (BD) was determined with a model AR200 digital refractometer (Leica Microsystems Inc.) and adjusted by adding small volumes of CsCl solution or Tris-EDTA buffer. The tubes were centrifuged at 178,000 g (20 ºC) for 48 h in a Stepsaver 70 V6 Vertical Titanium Rotor (8 x 5.1 ml capacity) within a Sorvall WX 80 Ultra Series Centrifuge (Thermo Scientific). Following centrifugation, the tubes was placed onto a fraction recovery system (Beckman) and fractions (150 l) were collected. The BD of each fraction was measured, and CsCl was removed by glycogen-assisted ethanol precipitation. PCR and TRFLP The ultracentrifugation fractions from replicates of labeled and unlabeled microcosms for both soils were PCR-amplified using 27F-FAM (5’-AGAGTTTGATCMTGGCTCAG, 5’ end-labeled with carboxyfluorescine) and 1492R (5’-GGTTACCTTGTTACGACTT) (Operon Biotechnologies) as previously described (4). The presence of PCR products was confirmed by 1.5% agarose gel electrophoresis and the subsequent staining of the gels with ethidium bromide. PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.), following the manufacturer’s instructions and approximately 150 ng purified PCR products were digested with 15 Hae III (New England Biolabs) with a 6-hour incubation period. Additional digests (Hha I, Mse I, Bsp1286I, BsrB I) for TRFLP analyses in a number of heavy labeled fractions were included to correlate the TRFLP fragment lengths to the in silico cut sites of the cloned 16S rRNA gene sequences. DNA fragments were separated by capillary electrophoresis (ABI Prism 3100 Genetic Analyzer, Applied Biosystems) at the Research Technology Support Facility (RTSF) at Michigan State University. Data were analyzed with GeneScan software (Applied Biosystems) and the percent abundance of each fragment was determined. 16S rRNA gene sequencing Heavy fraction 13 -1 C-DNA (BD value of 1.744 g mL ) was amplified as above except the forward primer was unlabeled and the final extension time was extended to 15 minutes. The PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.) and cloned into Escherichia coli TOP10 vector supplied with a TOPO TA cloning kit (Invitrogen Corporation). E. -1 coli clones were grown on Luria-Bertani (LB) medium solidified with 15 g agar L with 50 g ampicillin L-1 for 16 h at 37 ºC. Colonies with inserts were verified by PCR with primers M13 F (5’-TGTAAAACGACGGCCAGT-3’) and M13 R (5’-AACAGCTATGACCATG-3’), plasmids were extracted from the positive clones with a QIAprep miniprep system (Qiagen, Inc.) and the insertions were sequenced at RTSF. The Ribosomal Database Project (RDP) (Center for Microbial Ecology, Michigan State University) analysis tool “classifier” was utilized to assign taxonomic identity. 16 Real-time PCR A quantitative real-time PCR assay (qPCR) was developed targeting the 16S rRNA gene of the dominant toluene degrader identified above. The assay was developed to quantify the increase in the DNA BD resulting from label incorporation. In addition, the assay provided a rapid method to investigate cell numbers under mixed culture conditions as toluene was depleted. The assay was conducted in a Chromo 4 real-time PCR cycler (Bio-Rad) using the primer set PO313F (5’AATGGATGGTACAGAGGGTC-3’) and PO313R (5’-ATTACTAGCGATTCCGACTT-3’) (Operon Biotechnologies), and produced a 114 bp PCR product. Primers were designed with NCBI primer-BLAST (National Center for Biotechnology Information, Bethesda, MD) and checked for specificity using the Ribosomal Database Project (RDP) probe match tool. The forward primer matched 64 16S rRNA gene sequences (out of a total of 856,341) and of this, 32 belonged to the genus Polaromonas. The reverse primer matched 105,600 16S rRNA gene sequences and from this, 252 belonged to the genus Polaromonas. For the purposes of this study, this level of specificity was considered adequate. Both nucleic acid samples from density gradient fractions (experiment 1, SIP fractions) and total DNA extractions at successive time points (experiment 2, real-time PCR) were quantified with primers PO313F and PO313R using a SYBR green real-time PCR kit (Applied Biosystems) following the manufacturer’s recommended recipe. Each 20 μL PCR reaction mixture containing 10 μL ABI real-time PCR kit , 0.25 μM of each primer, and 1 μL DNA template. The thermal protocol consisted of an initial denaturation (95 ºC, 15 s), 40 cycles of amplification (95 ºC, 15 s; 60 ºC, 20 s; 72 ºC 20 s) and a terminal extension step (72 ºC, 2 min). Melting curves were constructed from 55.0ºC to 95.0ºC, read every 0.6ºC for 2 s. For each gradient fraction, 1 μL was diluted with 3 μL water as template (to conserve the sample). For experiment 2, 1 μL total DNA was used directly as the template. 17 For both, samples were measured in triplicate. Cloned plasmid DNA was utilized as a standard for quantification and gene copies were determined as shown in the equation below, as previously described (16) (plasmid size was 5441 bp, including 1485 bp of insert).   1 mol bp DNA   6.023  10 23 bp   ng   1g     gene copies   DNA concentration,     3 ng   660g DNA   mol bp L  1000          1 copy   plasmid size [bp]   volume, L     RESULTS AND DISCUSSION Toluene removal (both labeled and unlabeled) occurred rapidly (~100 % removal in seven days) in triplicates of soil 1 and soil 2 microcosms, but was limited in the autoclaved controls (~20% decrease, likely due to sorption), confirming a biological removal mechanism (Table 2.1). Several molecular methods (SIP and qPCR) were employed to identify the dominant microorganism responsible for aerobic toluene removal in these microcosms. Following toluene depletion, DNA was extracted from replicate soil 1 and soil 2 microcosms (labeled and unlabeled toluene amended) and subjected to ultracentrifugation, followed by fractionation of the ultracentrifugation samples. TRFLP was then conducted on all fractions so that heavy fractions from the labeled and unlabeled samples could be compared and thus account for false positives (from contamination or high GC content microorganisms) in the sample heavy fractions. TRFLP profiles indicated one fragment (313 bp) was more dominant in the heavy fractions (> ~ 1.74 g -1 mL ) of labeled toluene amended microcosms compared to the controls (unlabeled toluene) (Figure 2.1). This trend was observed in the replicates of both soils. Other TRFLP fragments were found in the heavy fractions from the labeled toluene amended samples, however, as these 18 were also found at similar levels in the heavy fractions of the controls, they were excluded from further analyses. The identity of the organism producing the TRFLP 313 bp fragment was determined using two -1 methods. Firstly, the fraction (BD value of 1.744 g mL ) with highest relative abundance of the 313 bp fragment was subject to cloning and sequencing. Sequences with a Hae III cut site of 313 bp were identified from this. Additionally, fractions with dominant 313 bp fragments were chosen for additional TRFLP analyses with four other enzyme (Hha I, Mse I, Bsp1286I, BsrB I). The dominant fragments obtained from these additional TRFLP digests were then compared to the clone library sequences to correlate actual cut sites with predicted cuts sites, thus determine the identity of the organism producing the Hae III 313 bp peak (Table 2.2). Only slight differences (1 to 2) between the predicted and actual lengths were seen, such differences have been noted by others (1, 13) and may be a result of variability within the TRFLP method. The clone sequence obtaining the five appropriate cut sites classified as a Polaromonas strain within the class β Proteobacteria. To our knowledge, this is the first report directly linking toluene degradation to the Polaromonas genus. Two additional lines of inquiry provided further evidence that the Polaromonas strain was indeed responsible for toluene transformation within the mixed community sample. Firstly, the relative distribution of Polaromonas 16S rRNA genes, as determined via the developed qPCR assay, indicated an increase in DNA BD between the labeled and unlabeled toluene amended microcosms (Figure 2.2, soil 1). Maximum 16S rRNA gene abundance levels from labeled -1 -1 toluene amended microcosms were found at 1.742 g mL (soil 1) and1.744 g mL (soil 2), a 19 clear increase over the maximum abundance values in the unlabeled toluene amended samples -1 -1 (1.719 g mL for soil 1 and 1.726 g mL for soil 2). Thus, the BD differences between the peak -1 abundance in unlabeled compared to the labeled were 0.023 g mL (soil 1) and 0.018 g mL -1 (soil 2), respectively. The slight difference between the two soils is likely a result of analytical variability. As expected, the increase is less than has been seen with pure cultures exposed to -1 higher concentrations of labeled substrates (e.g. an increase of 0.038 g mL was noted in E. coli -1 13 following exposure to 1.3 g L C lactate (3)), yet it is a large enough signal to indicate label uptake from toluene by the Polaromonas population. The second line of evidence indicating the Polaromonas sp. was responsible for toluene degradation is provided by Polaromonas specific qPCR analyses of toluene degrading microcosms. Specifically, qPCR was utilized to monitor the total number of Polaromonas species at successive time points of toluene removal. The data collected indicated a clear increase in Polaromonas sp. cell numbers as toluene was depleted in the replicate live samples but not in the replicate no-toluene controls, indicating toluene was required for growth of these organisms (Figure 2.3). The qPCR assay provided a rapid investigative tool enabling cell populations to be determined and correlated with toluene removal in mixed culture, without the need for isolation. Again, to our knowledge, these data represent the first report of growth on toluene of by an organism in the Polaromonas genus. Supernatant samples transferred from toluene degrading microcosms (following complete removal of toluene) were tested for their ability to transform other contaminants. Previous SIP 20 research indicated the same (based on 16S rRNA gene sequences) Polaromonas sp. was responsible for benzene transformation within a mixed community microcosm sample constructed from the same soil (5), therefore benzene degradation was tested to confirm this result. Another SIP study on m-xylene degradation with the same soil found that a microorganism other than the Polaromonas sp., was responsible for m-xylene degradation (5), therefore m-xylene was also added to the supernatant to further investigate this finding. Finally, given the importance of cis-dichloroethene (cDCE) as an environmental contaminant, and previous reports of Polaromonas sp. strain JS666 using cDCE as a sole energy and carbon source (2, 11), the supernatant was also tested for cDCE removal. As expected, benzene transformation occurred rapidly in the samples but not in the autoclaved controls, whereas neither m-xylene nor cDCE concentrations declined in either the samples or controls (Figure 2.4). This research provides evidence that that a Polaromonas species survives and grows in the presence of toluene while in a mixed community sample. Research to date on both aerobic and anaerobic toluene degradation has typically focused on pure cultures, due to the technical difficulties associated with examining particular species while existing in mixed culture. The primary method of inquiry used here, SIP, allows function to be linked with identity in a mixed community sample, more realistically reflecting a real-world scenario. The method has been utilized once before to investigate toluene degradation in mixed community samples. In that study, another novel organism, belonging to the “candidate” phylum TM7 was responsible for toluene transformation in mixed community samples (10). Clearly, SIP provides a unique ability to open up the “black box” of the microbial world providing interesting contrasts to previous reports based on isolations. Stable isotope probing, in theory, avoids the biases involved in 21 conventional isolation procedures. In other words, microorganisms that do not grow well under typical isolation conditions can still be studied and identified if SIP is used. The results presented here confirm this, as others have indicated Polaromonas species have traits (e.g. oligotrophic and slow growing) that are likely to impede their isolation and characterization by standard methods (11). Since the genus was first reported in 1996 (6), only a small number of other Polaromonas strains have been obtained. The type stain, P. vacuolata, was isolated in 1996 from Antarctic marine waters (6). Others, also obtained from interesting sources, were isolated more recently, including P. aquatica obtained from tap water in 2006 (9) and P. hydrogenivorans, a psychrotolerant hydrogen oxidizing bacterium isolated from soil over permafrost in Alaska in 2007 (17). More relevant to the research presented here are the remaining two Polaromonas strains previously reported, as both have been linked to the degradation of important environmental contaminants. The first, isolated in 2002 from granular activated carbon from a chlorinated solvent pump-and-treat plant in Germany, Polaromonas sp. strain JS666, is the only known microorganism able to grow using the environmental contaminant cDCE as a sole carbon and energy source (2, 11). The other, isolated in 2003 from coal-tar contaminated sediment, P. naphthalenivorans strain CJ2 uses naphthalene as a sole carbon and energy source (7). Interestingly, P. naphthalenivorans strain CJ2 was also first identified with the SIP method (8). The 16S rRNA gene of the toluene degrading Polaromonas strain described here was 96.6 % (1447/1498) and 97.6 % (1459/1495) similar to P. naphthalenivorans strain CJ2 and Polaromonas sp. strain JS666, respectively. 22 In conclusion, several lines of evidence indicated a Polaromonas species was responsible for toluene removal in mixed culture samples. Firstly, SIP illustrated that a 313 bp TRFLP fragment was more dominant in heavy fractions obtained from labeled microcosms compared to the heavy fractions of the unlabeled controls. This pattern suggests the microorganism represented by fragment 313 bp was responsible for 13 C uptake from toluene. The identity of this organism was determined by 16S rRNA gene sequencing as well as TRFLP with additional enzymes on heavy fractions. Additionally, qPCR targeted to the identified Polaromonas species indicated an increase in DNA BD over the gradient fractions between the labeled and unlabeled samples, further confirming label uptake occurred. A second line of evidence indicating the Polaromonas strain was responsible for growth on toluene in mixed culture was provided by qPCR, which illustrated an increase in cell numbers only when toluene was present. In addition, samples highly enriched with Polaromonas cells rapidly depleted benzene. These results contribute to the growing body of knowledge on the abilities of Polaromonas species to degrade and grow on key environmental organic pollutants and thus indicate these may be key species for use in situ contaminant removal. Further, we provided evidence that this particulate Polaromonas strain can thrive in mixed culture suggesting they will likely compete well at a contaminated site. 23 Tables and figures Table 2.1. Average percent toluene remaining in control and sample microcosms (error bars represent standard deviations represent from triplicates). -1 Soil 1 Soil 2 Time (days) 0 4 5 7 0 4 5 7 Toluene concentration (mg L ) Unlabeled toluene Labeled toluene (13C) 12 ( C) samples samples Sterile controls 37.2 ± 1.9 38.0 ± 0.5 34.7 ± 4.8 33.5 ± 2.4 23.8 ± 7.7 25.6 ± 7.6 29.4 ± 3.3 9.0 ± 4.6 6.5 ± 7.1 29.3 ± 0.5 0.1 ± 0.2 0.3 ± 0.2 31.3 ± 1.9 28.3 ± 0.8 28.3 ± 0.8 25.6 ± 1.6 34.2 ±2.7 22.6 ± 4.3 10.8 ± 3.4 0.1 ± 0.1 24 30.2 ± 4.1 17.2 ± 4.8 9.0 ± 3.6 0.1 ± 0.1 Table 2.2. Comparison of dominant fragments in heavy fraction TRFLP to clone restriction enzyme cut sites predicted from sequence analyses. Restriction enzyme Hha I Bsp 1286 I BsrB I Mse II TRFLP 204 119 214 535 25 Clones 203 117 212 534 From 13 C From toluene amended 313 bp 50 100 150 200 250 300 350 400 450 12 50 100 150 200 250 300 350 400 450 500 1.751 g/mL 1.753 g/mL 1.749 g/mL 1.748 g/mL 1.747 g/mL 1.745 g/mL 1.744 g/mL 1.740 g/mL 1.739 g/mL Fluorescence intensity C toluene amended 313 bp 1.736 g/mL Fragment length (bp) -1 Figure 2.1. Comparison of TRFLP electropherograms of heavier fractions (>1.736 g mL ) between DNA obtained from labeled and unlabeled toluene amended microcosms, illustrating the dominance of TFRLP fragment 313 bp in fractions from the labeled toluene amended microcosms. A similar pattern was observed in the soil 1 replicate and in replicates of soil 2. 26 Polaromonas rRNA gene abundance (normalized) 1.2 1 0.8 0.6 0.4 0.2 0 1.7 1.72 1.74 1.76 1.78 DNA Buoyant Density (g/mL) Figure 2.2. Difference between abundance of Polaromonas sp. rRNA gene copies in 13 ultracentrifugation fractions from labeled ( C toluene) and unlabeled toluene amended microcosms from soil 2 as determined via qPCR. Fractions obtained from soil 1 illustrated a similar trend. 27 3 2.5 2 120 100 80 60 1.5 40 1 Toluene removal rate (%) 16S rRNA gene copies per ul template per gram soil Gene copies (rep.1) Gene copies (rep.2) Control (rep.1) Control (rep.2) Toluene removed (rep.1) Toluene removed (rep.2) 3.5 20 0.5 0 0 0 2 4 6 8 Time (days) Figure 2.3. Correlation between Polaromonas sp. 16S rRNA gene copies (determined by qPCR) and toluene removal over time in live samples and no-toluene controls (microcosms constructed from soil 2). 28 Benzene, m-xulene or cDCE concentration (mg/L) 60 40 Benzene (sample) cDCE (sample) m-xylene (sample) m-xylene (sample) 20 Benzene (control) cDCE (control) m-xylene (control) m-xylene (control) 0 0 10 20 30 Time (days) 40 50 60 Figure 2.4. Benzene, m-xylene and cis-dichloroethene (cDCE) concentrations over time in supernatant of microcosms samples and in autoclaved controls (error bars represent standard deviations). 29 REFERENCES 30 References 1. Clement, B. G., L. E. Kehl, K. L. DeBord, and C. L. Kitts. 1998. Terminal restriction fragment patterns (TRFPs), a rapid, PCR-based method for the comparison of complex bacterial communities. Journal of Microbiological Methods 31:135-142. 2. Coleman, N. V., T. E. Mattes, J. M. Gossett, and J. C. Spain. 2002. Biodegradation of cis-dichloroethene as the sole carbon source by a beta-proteobacterium. Applied and Environmental Microbiology 68:2726-2730. 3. Cupples, A. M., E. A. Shaffer, J. C. Chee-Sanford, and G. K. Sims. 2007. DNA buoyant density shifts during N-15-DNA stable isotope probing. Microbiological Research 162:328-334. 4. Cupples, A. M., and G. K. Sims. 2007. Identification of in situ 2,4-dichlorophenoxyacetic acid-degrading soil microorganisms using DNA-stable isotope probing. Soil Biology & Biochemistry 39:232-238. 5. Cupples, A. M., S. Xie, C. Luo, and W. Sun. 2009. Novel toluene, m-xylene and benzene degraders at contaminated and uncontaminated sites identified by SIP. 109th General Meeting, American Society for Microbiology, Philadelphia, PA. 6. Irgens, R. L., J. J. Gosink, and J. T. Staley. 1996. Polaromonas vacuolata gen nov, sp nov, a psychrophilic, marine, gas vacuolate bacterium from Antarctica. International Journal of Systematic Bacteriology 46:822-826. 7. Jeon, C. O., W. Park, W. C. Ghiorse, and E. L. Madsen. 2004. Polaromonas naphthalenivorans sp nov., a naphthalene-degrading bacterium from naphthalene-contaminated sediment. International Journal of Systematic and Evolutionary Microbiology 54:93-97. 8. Jeon, C. O., W. Park, P. Padmanabhan, C. DeRito, J. R. Snape, and E. L. Madsen. 2003. Discovery of a bacterium, with distinctive dioxygenase, that is responsible for in situ biodegradation in contaminated sediment. Proceedings of the National Academy of Sciences of the United States of America 100:13591-13596. 9. Kampfer, P., H. J. Busse, and E. Falsen. 2006. Polaromonas aquatica sp nov., isolated from tap water. International Journal of Systematic and Evolutionary Microbiology 56:605-608. 10. Luo, C., S. Xie, W. Sun, X. Li, and A. M. Cupples. 2009. Identification of a novel toluene-degrading bacterium from the candidate phylum TM7 determined by DNA stable isotope probing. Applied and Environmental Microbiology In press. 11. Mattes, T. E., A. K. Alexander, P. M. Richardson, A. C. Munk, C. S. Han, P. Stothard, and N. V. Coleman. 2008. The genome of Polaromonas sp. strain JS666: Insights into 31 the evolution of a hydrocarbon- and xenobiotic-degrading bacterium, and features of relevance to biotechnology. Applied and Environmental Microbiology 74:6405-6416. 12. Mu, D. Y., and K. M. Scow. 1994. Effect of trichloroethylene (TCE) and toluene concentrations on TCE and toluene biodegradation and the population density of TCE and toluene degraders in soil. Applied and Environmental Microbiology 60:2661-2665. 13. Osborn, A. M., E. R. B. Moore, and K. N. Timmis. 2000. An evaluation of terminal-restriction fragment length polymorphism (T-RFLP) analysis for the study of microbial community structure and dynamics. Environmental Microbiology 2:39-50. 14. Parales, R. E., J. V. Parales, D. A. Pelletier, and J. L. Ditty. 2008. Diversity of microbial toluene degradation pathways. Advances in Applied Microbiology, Vol 64 64:1-+. 15. Radajewski, S., P. Ineson, N. R. Parekh, and J. C. Murrell. 2000. Stable-isotope probing as a tool in microbial ecology. Nature 403:646-649. 16. Ritalahti, K. M., B. K. Amos, Y. Sung, Q. Z. Wu, S. S. Koenigsberg, and F. E. Loffler. 2006. Quantitative PCR targeting 16S rRNA and reductive dehalogenase genes simultaneously monitors multiple Dehalococcoides strains. Applied and Environmental Microbiology 72:2765-2774. 17. Sizova, M., and N. Panikov. 2007. Polaromonas hydrogenivorans sp nov., a psychrotolerant hydrogen-oxidizing bacterium from Alaskan soil. International Journal of Systematic and Evolutionary Microbiology 57:616-619. 32 CHAPTER 3 DIVERSITY OF TOLUENE DEGRADING MICROORGANIMS AND THE BSSA GENE IN FIVE NITRATE OR SULFATE AMENDED MICROBIAL COMMUNITIES INVESTIGATED USING STABLE ISOTOPE PROBING (SIP) Introduction Among the petroleum-related environmental contaminants, benzene, toluene, ethylbenzene and xylene (BTEX) are of particular concern because of their toxicity and easy migration in groundwater. Aerobic degradation of these chemicals is generally rapid (37, 53, 59, 60), however, because anaerobic conditions typically exist at contaminated sites, understanding anaerobic biodegradation is more relevant to site cleanup. Unfortunately, the fate of BTEX under anaerobic conditions is still difficult to predict because removal is slow (or non-existent), and therefore difficult to study, and the microorganisms responsible are still being identified. In addition, many factors, such as electron acceptor availability, substrate competition between potential indigenous biodegraders and co-contamination (e.g. ethanol), can affect anaerobic BTEX degradation. More knowledge on the diversity of degrading species in complex samples and the effect of electron acceptor availability on these species has the potential to enhance our understanding of the variability associated with anaerobic degradation. From the BTEX contaminants, toluene degradation has been of great interest to many, with information available on pure and mixed cultures (based on the 16S rRNA gene) as well as the functional genes and enzymes involved. Toluene degradation has been observed over a range of electron accepting conditions with nitrate and sulfate being two important electron acceptors for 33 toluene degradation. Nitrate reduction may be an important mechanism for aromatic biodegradation because agricultural activity may result in high groundwater nitrate concentrations. In addition, relatively high levels of sulfate may occur naturally in some groundwater systems or may be added to enhance anaerobic degradation. A number of key toluene denitrifiers have been identified, affiliating within the genera of Azoarcus, Aromatoleum, Magnetospirillum Pseudomonas, Dechloromonas and Thaurea (5, 15, 23, 45, 48, 49, 54, 62). Similarly, microorganisms have also been linked to toluene degradation under sulfate reducing conditions, including, for example, microorganisms in the genera Desulfobacula (10), Desulfocapsa (39, 58), Desulfotomaculum (40), Desulfotignum (42), Desulfovibrio (3) and Desulfosporosinus (31, 57) (34). Although numerous organisms have been linked to anaerobic toluene degradation in pure or mixed cultures, it is challenging to determine if these organisms are actually responsible for toluene degradation in complex samples. To address this, molecular methods have been developed to link function with identity in complex samples enabling a greater understanding of microbial communities involved in contaminant removal or other biological processes. A key molecular method for this has been stable isotope probing (SIP). This method has been used only recently to study anaerobic toluene degradation. To date, SIP has been applied in three different studies under sulfate reducing conditions. In 2010, SIP was used to identify the active toluene degraders in aquifer sediment from a former gasworks site in Germany (12, 41, 57), and also in a sulfate reducing consortium developed from a BTEX contaminated aquifer also in Germany (12, 41, 57). In 2011, SIP was also applied to contaminated sediment samples from Germany to identify active toluene degrading species (44). 34 In the current study, we expand on this knowledge by applying SIP to samples from a wider range of sources, including uncontaminated sites. SIP was applied over two electron accepting conditions (nitrate or sulfate amended) and time-series SIP (DNA extraction over time) was used to enable label cross-feeding between species to be investigated. SIP was applied to the ribosomal gene as well as the functional gene (bssA encoding for benzylsuccinate synthase) previously correlated to anaerobic toluene degradation. Benzylsuccinate synthase has been recognized as a key enzyme for anaerobic toluene biodegradation under nitrate reducing (2, 29), sulfate reducing (56-58), ferric iron reducing (13, 25), and methanogenic enrichment cultures or environmental samples (55, 56). Here, the overall aim was to determine the diversity of active anaerobic toluene degraders and bssA genes across different habitats, both contaminated and uncontaminated samples, and compare these results to the current knowledge on pure cultures as well as previous SIP studies involving only contaminated site samples. This work represents the first study to use SIP to examine the diversity of active anaerobic toluene degraders across diverse sample sources. Materials and Methods Development of Toluene Degrading Microcosms A wide range of inocula sources were investigated for toluene degrading potential. These sources included agricultural soils (MI), subsurface soil from BTEX-contaminated sites (MI), sediments from a former gas-compressor site (24) (OK), digester sludges from wastewater treatment plants 35 (MI) and anaerobic granular sludge (WA). Triplicates of ~10g (wet weight) were incubated in sterile 160 mL serum bottles containing 50 mL anaerobic basal media (61), sealed with rubber stoppers and aluminum seals. Microcosms were prepared under strictly anaerobic conditions in an anaerobic chamber (Coy Laboratory Products INC, Grass Lake, MI). Potassium nitrate and magnesium sulfate were amended as electron acceptors. From approximately 38 incubations, only two nitrate-amended and three sulfate-amended microcosms exhibited toluene degradation and these were selected for the SIP experiments. The two active nitrate-amended microcosms were seeded from an agricultural soil (hereafter AgN) and anaerobic granular sludge from an UASB reactor in Washington (hereafter GSN). The three sulfate-amended toluene-degrading microcosms were inoculated from the same agricultural soil (hereafter AgS), contaminated sediments from a previous BTEX contaminated aquifer (hereafter CSS) (24) and digester sludge from a wastewater treatment plant in St. Clair, Michigan (hereafter DSS). For each microcosm, 3 g biomass (wet weight: enrichment cultures obtained in screening stage were inoculated for AgN, AgS and CSS; freshly sampled sludges were seeded for GSN and DSS) were anoxically incubated in 60 mL serum bottles containing 25 mL of anaerobic basal media as described above. -1 - Potassium nitrate and magnesium sulfate were added to a final concentration of 1 g L NO3 and 2- SO4 . Each treatment involved triplicate abiotic controls, triplicate unlabeled toluene (1 μL, 99 %, Chem Service, West Chester, PA) and three triplicate labeled toluene (1 μL ring -13 C6 toluene, 99%, Cambridge Isotope Laboratories, Inc. Andover, MA) amended samples. These microcosms were incubated at room temperature (~20 °C) with reciprocal shaking. 36 Analytical Techniques Toluene concentrations in headspace gas samples (200 μL) were typically determined weekly with a gas chromatograph (Perkin Elmer) equipped with flame ionization detector and a capillary column (J&W Scientific, DB-624, diameter 0.53mm). Injector and detector temperature were set at 200 oC and the column temperature was 120oC. DNA Extraction and Ultracentrifugation Microcosms were sacrificed for DNA extraction at various time points during toluene depletion for AgN, GSN, AgS and DSS to further understand the flow of carbon through these microbial communities. For CSS, an early time stage (50% toluene removal) was investigated due to limited availability of active microcosms. The powersoil DNA extraction kit (MO BIO Laboratories, Inc. Carlsbad, CA) was used for total nucleic acids extraction from entire microcosms in each treatment according to the manufacturer’s recommended procedure. Quantified DNA extracts (~10 μg) were loaded into Quick-Seal polyallomer tubes (13×51 mm, 5.1 ml, Beckman Coulter) along with a Tris-EDTA (TE, pH 8.0) /CsCl solution. Prior to sealing (cordless quick-seal tube topper, Beckman), the buoyant density (BD) was determined with a model AR200 digital refractometer (Leica Microsystems Inc) and adjusted by adding small volumes of CsCl solution or -1 Tris-EDTA buffer with a final BD of 1.7300 mgL . The tubes were centrifuged at 178,000 g (20 ºC) for 48 h in a Stepsaver 70 V6 Vertical Titanium Rotor (8 x 5.1 ml capacity) within a Sorvall WX 80 Ultra Series Centrifuge (Thermo Scientific). Following centrifugation, the tubes was placed onto a fraction recovery system (Beckman) and fractions (150 l) were collected. The BD of each fraction was measured, and CsCl was removed by glycogen-assisted ethanol precipitation. 37 PCR and TRFLP The density-resolved fractions from 12 C and 13 C microcosms for each treatment were PCR-amplified using 27F-FAM (5’-AGAGTTTGATCMTGGCTCAG, 5’ end-labeled with carboxyfluorescine) and 1492R (5’-GGTTACCTTGTTACGACTT) (Operon Biotechnologies) as previously described (16). The presence of PCR products was confirmed by 1.5% agarose gel electrophoresis and the subsequent staining of the gels with ethidium bromide. PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.), following the manufacturer’s instructions and approximately 150 ng was digested with HaeIII (New England Biolabs) with a 6-hour incubation period. Additional digests (HhaI, MseI, Bsp1286I, BsrBI etc.) for TRFLP analyses in a number of heavy labeled fractions were included to correlate the TRFLP fragment lengths to the in silico cut sites of the cloned 16S rRNA gene sequences. DNA fragments were separated by capillary electrophoresis (ABI Prism 3100 Genetic Analyzer, Applied Biosystems) at the Research Technology Support Facility (RTSF) at Michigan State University. Data were analyzed with GeneScan software (Applied Biosystems) and the percent abundance of each fragment was determined. Presence of bssA in Microcosms and Enumeration in SIP Fractions The presence of the benzylsuccinate synthase alpha-subunit gene (bssA) was investigated using different primers pairs (Table 3.1) on DNA extracted from each of the five treatments. A gradient PCR was performed with annealing temperature ranging from 45ºC to 58 ºC. Positive bssA amplicons were selected for cloning and sequencing (see below). Four treatments illustrated the 38 presence of partial bssA genes (AgN, GSN, DSS and CSS). For three of these (except CSS due to lack of sample), quantitative PCR (qPCR) was used to enumerate bssA gene copy numbers in gradient fractions. The assay was conducted in a Chromo 4 real-time PCR cycler (Bio-Rad) using the primer set 7772f/8546r for AgN and GSN, and SRBf/SRBr for DSS. Both 12C and 13C nucleic acid samples from density gradient fractions were subject to quantification. Each 20 μL PCR reaction mixture containing 10 μL SYBR green real-time PCR solution (Applied Biosystems), 0.25 μM of each primer, and 1 μL DNA template. The thermal protocol consisted of an initial denaturation (95 ºC, 15 min), 40 cycles of amplification (95 ºC, 15 s; 55 ºC, 20 s; 72 ºC 20 s) and a terminal extension step (72 ºC, 2 min). Melting curves were constructed from 55 ºC to 95 ºC, read every 0.6ºC for 2 s. For each gradient fraction, 1 μL solution was diluted with 3 μL water as template (to conserve the sample). Cloned plasmid DNA was utilized as a standard for quantification and gene copies were determined as shown below (plasmid size was 4730 bp, including 774 bp(7772f/8546r amplicons) and 97 bp(SRBf/SRBr amplicons) of insert).   1 mol bp DNA   6.023  10 23 bp   ng   1g     gene copies   DNA concentration,     3 ng   660g DNA   L  1,000 mol bp          1 copy   plasmid size [bp]   volume, L     Sequencing of Partial bssA and 16S rRNA Genes Clone libraries of the 16S rRNA genes were constructed for each treatment using DNA extracted following toluene depletion. The DNA was amplified with 27F/1492R as above except the forward primer was unlabeled and the final extension time was extended to 15 minutes. To reduce sequencing redundancy, restriction fragment length polymorphism (RFLP) analyses was performed and specific operational taxonomic units (OTU) were selected for sequencing. In 39 addition to 16S rRNA sequencing, amplicons generated with bssA primer pairs were also prepared for cloning and sequencing. The PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.) and cloned into Escherichia coli TOP10 vector supplied with a TOPO TA cloning kit (Invitrogen Corporation). E. coli clones were grown on Luria-Bertani (LB) -1 medium solidified with 15 g agar L -1 with 50 g ampicillin L for 16 h at 37 ºC. Colonies with inserts were verified by PCR with primers M13 F (5’-TGTAAAACGACGGCCAGT-3’) and M13 R (5’-AACAGCTATGACCATG-3’), plasmids were extracted from the positive clones with a QIAprep miniprep system (Qiagen, Inc.) and the insertions were sequenced at RTSF. The Ribosomal Database Project (RDP) (Center for Microbial Ecology, Michigan State University) analysis tool “classifier” was utilized to assign taxonomic identity. Phylogenetic trees for the partial bssA sequences along with the closest matches in Genbank were obtained by the neighbor-joining method using MEGA 4.1 software. Results Frequency of Toluene Degradation Toluene degradation using various inocula sources, including agricultural soil, digester sludge, anaerobic granular sludge and contaminated soils and sediments, was examined under nitrate and sulfate amended conditions. Toluene biodegradation was observed in 2 from 18 and in 3 from 20 experiments set-ups, involving nitrate amendment and sulfate amendments, respectively. Active toluene microcosms were also tested for their benzene biodegradation, however, no biodegradation was found in any consortia. SIP was performed on the two nitrate amended (an agricultural soil and granular sludge) and on the three sulfate amended microcosms (an 40 agricultural soil, digester sludge and contaminated site soil). At various time points, DNA was extracted from the labeled and unlabeled toluene-amended microcosms, and was subject to ultracentrifugation, fractionation and TRFLP (on each fraction). The organisms responsible for 13 C assimilation were identified by the comparison of relative abundances of specific T-RFs between the control (unlabeled toluene amended) and the sample (labeled toluene amended) at selective time points for each fraction. The identities of each enriched T-RFs for each microcosm type were then determined using additional restriction enzyme digests and by comparison to predicted cut sites in each 16S rRNA gene clone library, as described below. SIP on Agricultural Soil Nitrate Amended Microcosms (AgN) In AgN, a 214 bp HaeIII T-RF fragment became the only dominant T-RF fragment (>80%) among -1 labeled ‘heavy’ fractions (banding between 1.7523 to 1.7448 g ml ) in all three sampling points (33%, 75% and 100% toluene removal) (Figure 3.1 a). To identify the toluene-degrading bacteria based on the TRFLP results and to assign phylogenetic affiliation to distinct T-RFs, the16S rRNA clone library (Table 3.2) derived from total DNA was inspected. Three different Burkholderiales-related microorganisms classifying within the families Alcaligenaceae, Comamonadaceae and Oxalobacteraceae all exhibited a predicted HaeIII T-RF close to 214 bp. Specifically, from the analysis of the clone sequences, each had a predicted Hae III cut site of 219 bp (Table 3.2). Multiple digestions were then applied to determine which of these three sequences were actually responsible for the 214 bp HaeIII T-RF in the heavy fractions. From these digests (Table 3.3), the phylotype within the family Comamonadaceae were found to be directly correlated with carbon uptake from toluene and hence toluene degradation. Interestingly, the AgN 41 clone library (Table 3.2) contained a partial sequence related to the genus Azoarcus, which has previously been linked to toluene degradation under nitrate amended conditions (2, 8, 23, 63). However, no enrichment of the appropriate Azoarcus T-RF (77 bp) was noted in the heavy labeled fractions (Figure 3.1 b), indicated these organisms were likely not the major toluene degraders. SIP on the Granular Sludge Nitrate Amended Microcosms (GSN) Compared to AgN, the nitrate amended microcosms inoculated from anaerobic granular sludge exhibited a more diverse microbial community (Table 3.2). TRFLP revealed significant 13 C uptake for three T-RF (Figure 3.2), a fragment sized 72 bp dominated in labeled heavy fractions -1 (BD> 1.7448 g ml ). Additional enzyme digestions (Table 3.4) in combination with the 16S rRNA clone library (Table 3.2) were utilized to further distinguish this Hae III T-RF. The putative toluene degrader classified within the genus Thauera (72 bp). Thauera-related phylotypes were strongly enriched in the heavy fractions in all three time points with relative abundances > 70% at first two sampling points and >34% at the last time point. The peak of relative abundance decreased over time, suggesting the 13 C-label assimilation by other microorganisms may have diluted the fraction of Thauera-related phylotypes in heavy fractions. Thauera-related bssA genes and the enrichment of these genes in The presence of 13 C heavy fractions (see below) as quantified by qPCR strengthens the hypothesis that the Thauera phylotype was responsible for toluene degradation in this complex microbial community. 42 SIP on the Agricultural Soil Sulfate Amended Microcosms (AgS) In the sulfate amended agricultural soil microcosms (AgS), the majority (22 from 29 clones) of the microbial community classified within the class Clostridia (Table 3.5). Slight label assimilation was noted in two T-RFs in the DNA extracted from microcosms which consumed ~33% toluene, however, in the later two DNA extraction points, (~75% and ~100% toluene removal) label assimilation was more pronounced (Figure 3.3 a & b). Two TRFLP fragments, 77 bp and 213 bp, were enriched in the heavy 13 C-fractions during the course of biodegradation and no PCR products were found in the corresponding heavy 12 C-fractions. It is likely that both phylotypes were responsible for carbon uptake from toluene over the course of the incubations. The 16S rRNA clone library data (Table 3.5) in combination with additional restriction digests (Table 3.6) indicated that the two TRFLP fragments both affiliated with genus Desulfosporosinus (>98% sequence identity). SIP on the Digester Sludge Sulfate Amended Microcosms (DSS) In DSS, a significant proportion (20 from 59 clones) of the microbial community classified within the class Deltaproteobacteria (Table 3.5). The most abundant TRFLP fragment in C-heavy fractions was a 204 bp T-RF. This fragment was highly enriched in heavy fractions at 13 the three extraction times and the effect was most obvious for the last two time points (~75 % and ~100 % toluene depleted) (Figure 3.4). The maximum relative abundances of the 204 bp -1 -1 fragment was 27 % (at BD of 1.7360 g ml ), 43 % (at BD of 1.7480 g ml ) and 50 % (at BD of -1 1.7502 g ml ) for the three extraction points, indicating an increase in label uptake with time. In 43 contrast, the relative abundance of this fragment was less than 5 % in each unlabeled control gradient fraction (Figure 3.4). The BD values of these “heavy” peaks are very close to that of fully 13 -1 C labeled M. extorquens (1.757 g ml )(36), indicating a high degree of label assimilation. The bacterial clone library generated (Table 3.5) indicated the 204 bp T-RF was assigned with family Syntrophobacteraceae. As described above, additional digestion on the heavy fractions were performed to confirm this correlation between 204 bp T-RF and the associated 16S rRNA sequence (Table 3.7). SIP on Gas Compressor Site Soil Sulfate Amended Microcosms (CSS) The third sulfate amended sample involved microcosms inoculated with sediment from a former gas compressor site (24). Previous research indicated sulfate was the major terminal electron acceptor at this site. The clone library for this treatment indicated the dominance (91 from 106 clones) of microorganisms classifying within the Deltaproteobacteria (orders Desulfobacterales and Desulfuromonadales). Unfortunately, because of sample limitations, SIP was performed only on an early toluene-degrading stage (~50% toluene removal). A 202 bp T-RF was enriched in the -1 heavy 13C- fractions (relative abundance as ~70% with a BD of 1.7469 g ml ). The clone library for this microbial community (Table 3.5) illustrated a dominance of Desulfobulbaceae-affiliated organisms (80 from 106 clones) which correlated with the 203 bp T-RF. Multiple enzyme digestions (Table 3.8) confirmed that the Desulfobulbaceae-affiliated 16S rRNA gene sequence was responsible for the enriched Hae III 203 bp T-RF. These data indicate the Desulfobulbaceae affiliated microorganisms were responsible for toluene degradation. 44 Partial Sequencing of the bssA Gene A number of primers successfully amplified partial bssA genes from four of the five treatments (Table 3.9). Amplicons from AgN, GSN, DSS and CSS were selected for sequencing and phylogenetic trees were generated for each enrichment culture along with their closest matches in Genbank (Figure 3.6-3.9). Primer set 7772f/8546r, produced expected-size PCR products (~774 bp) within the two nitrate amended consortia (Figures 3.6 & 3.7). A total of 32 clones from agricultural soil and granular sludge nitrate amended enrichment cultures were digested and representative clones (as indicated by restriction digests) were selected for sequencing. All 64 clones showed the same OTU indicating sequence similarity, belonging to Thauera-related bssA genes (Figures 3.6 & 3.7). Primer pairs SRBf/SRBr displayed good coverage for the sulfate amended enrichment cultures (Table 3.9). Representative OTUs from the DSS and CSS were sequenced and three amplicons of each sample showed ~92% (90 bp out of 97 bp) similarity to partial sulfate-reducing bacterium PRTOL1 bssA gene (EU780921.1), which was congruent with the template sequences of the primer set. In addition, for CSS, longer partial bssA genes were obtained using primer pair 7772f/8828r and the sequences obtained were found to branch into two distinct lineages (Figure 3.9). Of these, 19 were closely related to bssA gene of strain TRM1 (99% sequence similarity)(58). Two clones were affiliated with uncultured bacterium clone Zz-ox_12 bssA gene, showing only 73% sequence similarity with the sulfate-reducing bacterium TRM1 bssA gene (22). Three clones could not be classified with any known bssA sequences. Unfortunately, unspecific PCR products or no PCR products were produced from the sulfate amended agricultural soil (AgS) from the primers tested (Table 3.1). 45 Quantification of bssA Genes in SIP Fractions To further confirm anaerobic toluene degradation in the nitrate and sulfate amended samples, the bssA genes were quantified from 12 C and 13 C gradient fractions at the last time point using primer sets 7772f/8546r and SRBf/SRBr. Quantitative PCR analysis of gradient fractions detected separation of bssA genes in labeled and unlabeled samples (Figure 3.10, a-c). In GSN, 13 quantitative label assimilation was very evident in the C-fractions where bulk bssA gene -1, moved to a heavier fraction with a BD of 1.7513 g mL -1 compared to that of the 12 C-fractions 13 (1.7208 g mL ) (Figure 3.10 a). In AgN, highly C-labeled bssA genes was present at a BD of -1 1.7415 g mL , while such ‘heavy’ bssA genes were not found in the 12 C-fractions but the peak -1 occurred at a lighter fraction with a BD of 1.7099 g mL . Also a tail of bssA gene formed in 13 -1 C-lighter fractions with a BD of 1.7046 g mL and (Figure 3.10 b). In DSS, a separation of 12 C 13 C peak was also seen (Figure 3.10 c). Quantitative PCR was not performed on the AgS fractions (no bssA primers were suitable for these microcosms) or the CSS fractions (limitation on sample available). Discussion Previous SIP studies on BTEX biodegradation have focused primarily on samples or biomass from former contaminated sites (20, 30, 57). To expand on this work and to discover novel toluene-degrading bacteria, the current study applied SIP to a wide range of inocula sources including agricultural soil, contaminated aquifer sediment and anaerobic granular and digester sludge. Noteably, the selection of inocula sources covers both uncontaminated and contaminated 46 sources, as well as natural and engineered microbial communities. These experiments involved the characterization of five toluene-degrading microbial consortia (through 16S rRNA clone libraries) and the identification of the active toluene degraders in each sample using time series DNA based SIP. For some of these samples, bssA gene sequences were also obtained and label uptake into the bssA gene was also documented. Toluene biodegradation under nitrate reducing conditions has been studied extensively (4, 11, 14, 46). To the authors’ knowledge, no detailed SIP study has not been conducted on nitrate-reducing, toluene-degrading mixed consortia. For the current study, a natural microbiota (agricultural soil) and an engineered microbial community (granular sludge) were investigated. These communities were targeted, in part, because it was likely that both had high levels of denitrifying microorganisms. In the nitrate amended agricultural soil (AgN), microorganisms classifying within family Comamonadaceae were found to be responsible for toluene biodegradation. Although Comamonadaceae-related bacteria are often characterized as aerobic bacteria, others have reported members of the Comamonadaceae as denitrifying bacteria (17, 26). Comamonadaceae-related microorganisms have been correlated with cyclohexanol (38) and poly(3-hydroxybutyrate-co-3-hydroxyvalerate) (PHBV) (26) biodegradation under nitrate reducing conditions. Depletion of nitrate was not measured in the current study, however, the following lines of evidence suggest the Comamonadaceae-related bacteria were degradating toluene under nitrate reducing conditions: 1) strict anaerobic methods were followed, 2) partial bssA genes were obtained from the micrososms and 3) the bssA genes were enriched in the heavy 47 fractions (qPCR data, Figure 10) indicating the Comamonadaceae-related bacteria (also enriched in the heavy fractions) were anaerobic (benzylsuccinate synthase is irreversibly inactivated in the presence of molecular oxygen (28)). These results are novel because the most commonly reported nitrate-reducing, toluene-degrading species (genera Azoarcus, Thauera and Dechloromonas) classify within another Betaproteobacteria family, the Rhodocyclaceae. The AgN clone library (Table 3.2) also contained a 77 bp fragment belonging to genus Azoarcus, a common toluene degrader under nitrate reducing conditions (2, 8, 23, 63), however, no enrichment of this T-RF was noted in the heavy fractions, indicating these organisms were not responsible for 13 C-substrate assimilation. The enrichment of bssA and Comamonadaceae 16S rRNA genes in the heavy 13 C–fractions along with the presence of Azoarcus sp. in the clone library could indicate the Comamonadaceae-related biodegraders may have obtained the Azoarcus bssA gene by horizontal gene transfer. Horizontal gene transfer of such catabolic genes has been suggested or found previously (13, 48, 56, 58). These finding illustrates the importance of culture independent approaches, compared to culture dependent approaches, for understanding functions in mixed cultures. In the nitrate amended, granular sludge treatments (GSN), a 72 bp T-RF associated with genus Thauera was enriched in all three time points. This is a reasonable conclusion because Thauera spp. have been reported by others to be an important toluene-degrading species under nitrate reducing conditions (6, 11, 32, 50). The toluene metabolic pathway in Thauera is known to be initiated by the formation of benzylsuccinate from toluene and fumarate(10). Sequencing of the 48 partial bssA genes revealed that all 32 clones were closely related with Thauera spp. bssA gene. The presence of Thauera-related bssA genes and the enrichment of these genes in 13 C heavy fractions as quantified by qPCR strengthen the hypothesis that the Thauera phylotype was responsible for toluene degradation in this complex microbial community. In the sulfate amended agricultural soil (AgS), two T-RFs (77 bp and 213 bp), both belonging to the genus Desulfosporosinus exhibited strong label assimilation at the last two sampling points (Figures 3.3 a & b). The genus Desulfosporosinus has previously been linked to toluene degradation (31, 47). It was also identified as being able to assimilate 13 C-toluene in a recent SIP project (57). Since no other T-RFs are significantly enriched in the labeled heavy fractions over the three time points, it is likely that the Desulfosporosinus spp. were responsible for toluene degradation in the AgS microcosms. In the sulfate-amended, digester sludge treatment (DSS), a 204 bp T-RF, representing a phylotype within the family Syntrophobacteraceae, was the only T-RF dominated in the 13 C-heavy fractions. The label assimilation of this T-RF intensified over time (Figure 3.4). This effect was most prominent at the last sampling point with more than 50 % relative abundance in the 13 C-heavy fractions. Notably, a 77-bp T-RF affiliated within the genus Desulfovibrio, was slightly enriched in the 13 C-heavy fractions (abundance around or less than 10%). The Desulfovibrio spp. may have been able to scavenge labelled metabolic by-products from the Syntrophobacteraceae related microorganisms. Members of Syntrophobacteraceae have previously been identified as sulfate reducing bacteria (18, 35) and can degrade long chain fatty 49 acids (51, 52) and propionate (7) under sulfate-reducing conditions. The closest relatives of the 204 bp T-RF with a validly published name is Syntrophobacter wolinii (19), sharing 91% sequence similarity. S. wolinii has been reported as a sulfate-reducing bacterium and its closest relatives are Desulfomonile tiedjei and Desulfoarculus baarsii. The 204 bp T-RF also shared a more distant similarity (88% 16S rRNA similarity) with sulfate reducing strain PRTOL1, a toluene sulfate reducer isolated from fuel-contaminated subsurface soil (9, 10). Syntrophobacteraceae were identified in a toluene-degrading sulfate-reducing bacterial consortium, but in that study, the Desulfobulbaceae were identified as key organisms of toluene degradation within the consortium (41). In another study, carbon stable isotope analysis in combination with whole-cell hybridization linked toluene degradation to the Desulfobacter-like populations, while Synthrophobacter was present in the microbiota but not responsible for toluene biodegradation (43). The Syntrophobacteraceae was also observed in a benzene-degrading in situ microcosm but was not linked with benzene biodegradation (21). To date, to the authors’ knowledge, there has been no direct evidence to correlate members of the family of Syntrophobacteraceae with anaerobic toluene biodegradation. The presence of bssA genes similar to sulfate reducing strain PRTOL1-related bssA genes (Figure 3.8) in DNA extracted from the digester sludge treatment also confirmed the hypothesis that the novel Syntrophobacteraceae clade played an active role in toluene biodegradation in these sulfate amended samples. The third sulfate amended sample involved microcosms inoculated with material originating from a former gas compressor site (CSS). SIP was only performed at one time point (~50% toluene removal), however, the 16S rRNA gene and bssA gene clone libraries support the SIP 50 results. Microorganisms classifying within the Desulfobulbaceae family appeared to be dominant in the 13 C-heavy fractions and in the clone library. Desulfobulbaceae have previously been classified as BTEX sulfate reducers (1, 27, 30, 33, 41). They were also reported in the DNA-SIP project described above (57) but were not identified as the primary toluene degrader. Interestingly, Desulfosporosinus-related microorganisms (identified as primary toluene degraders in AgS) were present in the CSS clone library (Table 5) but were not enriched in the 13 C-heavy fractions. In summary, five distinct phylotypes were identified as the active toluene-degrading bacteria under either nitrate or sulfate amended conditions for five different microbial communities. For one microcosm type, syntrophic partners were also identified. For three treatments, the phylotypes were similar to previously identified toluene degraders (Thauera, Desulfosporosinus and Desulfobulbaceae related phylotypes), whereas two treatments produced novel toluene degraders (Comamonadaceae and Syntrophobacteraceae related phylotypes). The discovery of two novel toluene degraders indicates the importance of culture independent approaches for identifying the active microorganisms in complex samples. In addition, this study provided information on the diversity of bssA sequences and the utility of a number of primer pairs for detecting the bssA gene. Further, the work highlights the value of combining ribosomal and functional gene based SIP to link function with identity for complex microbial samples and adds to our understanding of the microbial ecology of toluene degrading communities from various environments. 51 Acknowledgements Funding for this work was provided by a grant awarded to A. Cupples from the National Science Foundation (Grant 0853249). The authors thank Paul Fallgren (Western Research Institute) and Zhenbo Yue (Michigan State University) for supplying the contaminated soil sample (CSS) and anaerobic granular sludge (GSN) respectively. 52 Tables and figures Table 3.1. Primers used in this study to investigate the presence of the bssA gene Primer Sequence(5'-3') Reference 6888f AATTCATCGTCGGCTACCACG (Winderl et al. 2007) 7772f GACATGACCGACGCSATYCT (Winderl et al. 2007) 8546r TCGTCGTCRTTGCCCCAYTT (Winderl et al. 2007) 8828r AGCAGRTTGSCCTTCTGGTT (Winderl et al. 2007) SRBf (Beller et al. 2008) SRBr GTSCCCATGATGCGCAGC CGACATTGAACTGCACGTGRT CG bssApd2f CCTATGCGACGAGTAAGGTT (Winderl et al. 2008) bssApd2r TGATAGCAACCATGGAATTG (Winderl et al. 2008) bssN2f GGCTATCCGTCGATCAAGAA (Winderl et al. 2008) bssN2r GTTGCTGAGCGTGATTTCAA (Winderl et al. 2008) bssAf ACGACGGYGGCATTTCTC (Beller et al. 2002) bssAr GCATGATSGGYACCGACA (Beller et al. 2002) 53 (Beller et al. 2008) Table 3.2. Phylogenetic affiliation of each 16S rRNA clone in nitrate amended toluene degrading microcosms as determined with the RDP analysis tool “classifier” Enriched in Soil/Fragment (Hae III # of 13 Class Order Genus C heavy digestion) clones fractions - Agricultural Soil, NO3 Amended 39 bp 219 bp 77 bp 219 bp 41 bp 219 bp 39 bp 250 bp 250 bp 269 bp 315 bp No Yes No No No No No No No No No 20 7 8 5 4 3 1 1 1 1 1 Gammaproteobacteria Pseudomonadales Betaproteobacteria Burkholderiales Betaproteobacteria Rhodocyclales Betaproteobacteria Burkholderiales Gammaproteobacteria Xanthomonadales Betaproteobacteria Burkholderiales Gammaproteobacteria Xanthomonadales Sphingobacteria Sphingobacteriales Clostridia Clostridiales Acidobacteria_Gp3 Betaproteobacteria Burkholderiales Pseudomonas Unclassified Azoarcus Unclassified Dokdonella Unclassified Luteimonas Ferruginibacter Sedimentibacter Gp3 Polaromonas Yes Yes Yes No No No No No No No No No 25 14 12 8 8 7 7 5 5 4 4 4 Betaproteobacteria Rhodocyclales Deltaproteobacteria Syntrophobacterales Betaproteobacteria Burkholderiales Deltaproteobacteria Syntrophobacterales Bacteroidia Bacteroidales Flavobacteria Flavobacteriales Epsilonproteobacteria Campylobacterales Nitrospira Nitrospirales Planctomycetia Planctomycetales Bacteroidia Flavobacteria Bacteroidia Bacteroidales Clostridia Clostridiales Thauera Smithella Simplicispira Unclassified - Granular Sludge, NO3 Amended 77 bp 77 bp 217 bp 82 bp, 205 bp, 271 bp 260 bp 39 bp 226 bp 180 bp 180 bp, 245 bp 39 bp 260 bp 318 bp 54 Arcobacter Magnetobacterium Planctomyces Unclassified Unclassified Fusibacter Table 3.2 (cont’d) 951 bp 189 bp 191 bp 37 bp 202 bp 318 bp 951bp No No No No No No No 4 2 2 1 1 1 1 Epsilonproteobacteria Campylobacterales Synergistia Synergistales Flavobacteria Flavobacteriales Thermotogae Thermotogales Clostridia Clostridiales Epsilonproteobacteria Campylobacterales 55 Sulfurospirillum Unclassified OP3 Unclassified Kosmotoga Fusibacter Sulfurospirillum Table 3.3. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment length from in silico sequence analyses (nitrate amended agricultural soil microcosms) TRFLP (bp) Sequence Data (bp) Restriction Enzyme Comamonadaceae affiliated sequence Hae III 214 219 Msp I 485 490 Hha I 205 207 RSA I 424 429 Mse I 534 538 BsrBi 211 216 56 Table 3.4. Comparison of fragment length of dominant T-RFs in heavy fractions to predicted fragment lengths from in silico sequence analyses (nitrate amended granular sludge microcosms). TRFLP (bp) Sequence Data (bp) Restriction Enzyme Simplicispira affiliated sequence 204 210 470 476 537 541 119 123 Hae III 73 77 Msp I 508 507 89 95 240 244 BSP 1286 I Enriched fragment 3 82 RSA I affiliated 77 Hha I Smithella sequence Msp I BSP 1286 I Enriched fragment 2 77 Mse I affiliated 72 RSA I Thauera sequence Hae III Hha I Enriched fragment 1 625 623 Hae III 213 217 Msp I 489 488 Hha I 205 205 RSA I 472 471 Mse I 537 536 57 Table 3.5. Phylogenetic affiliation of each 16S rRNA clone in sulfate amended toluene degrading microcosms as determined with the RDP analysis tool “classifier” Enriched in #of 13 Soil/Fragment Class Order Genus heavy C clones fractions Agricultural Soil, 2SO4 Amended 2 82bp,214 bp Yes 5 Clostridia Clostridiales Desulfosporosinus 252 bp No 4 Gammaproteobacteria Pseudomonadales Acinetobacter 39 bp No 1 Gammaproteobacteria Pseudomonadales Pseudomonas 223 bp No 1 Bacilli Bacillales Paenibacillus 228 bp No 1 Clostridia Clostridiales Gracilibacter 228 bp No 1 Clostridia Clostridiales Gracilibacter 249 bp No 1 Clostridia Clostridiales Sedimentibacter 262 bp No 1 Sphingobacteria Sphingobacteriales Toxothrix 299 bp No 1 Clostridia Clostridiales Proteiniborus 316 bp No 1 Clostridia Clostridiales Centipeda Digester Sludge, 2SO4 Amended 1 77bp, 209bp Yes 0 Unclassified Deltaproteobacteria Syntrophobacterales 1 Unclassified 77bp, 214bp No 0 Deltaproteobacteria Deltaproteobacteria 258bp, 298 bp No 9 Bacteroidia Bacteroidales 203bp No 8 Thermotogae Thermotogales Kosmotoga 238bp, 299bp No 6 Caldisericia Caldisericales Caldisericum 220 bp No 4 Unclassified Anaerolineae Anaerolineales Bacterium Eub 3 914 bp No 4 OP9 324 bp No 3 214 bp No 2 Unclassified Spirochaetes Spirochaetales Unclassified 267 bp No 2 Clostridia Clostridiales 58 Table 3.5 (cont’d) 251 bp Contaminated 2Soil, SO4 Amended No 1 Planctomycetia Planctomycetales Planctomyces 205 bp 209 bp, 275 bp Yes No 8 0 6 Deltaproteobacteria Deltaproteobacteria Unclassified Unclassified 206 bp 220 bp 206 bp 318 bp 171 bp 214 bp 220 bp No No No No No No No 5 5 4 3 1 1 1 Deltaproteobacteria Actinobacteria Clostridia Clostridia Nitrospira Clostridia Clostridia Desulfobacterales Desulfobacterales Desulfuromonadale s Unclassified Clostridiales Clostridiales Nitrospirales Clostridiales Clostridiales 59 Geobacter Fusibacter Magnetobacterium Desulfosporosinus Acetivibrio Table 3.6. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment lengths from in silico sequence analyses (sulfate amended agricultural soil microcosms). Restriction Enzyme Desulfosporosinus affiliated sequence Desulfosporosinus affiliated sequence HaeIII MspI BsrBI MseII Restriction Enzyme HaeIII MspI BsrBI MseII 60 TRFLP (bp) 213 136 52 178 TRFLP (bp) 77 53 N/A 223 Sequence Data (bp) 216 140 56 180 Sequence Data (bp) 82 62 N/A 227 Table 3.7. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment lengths from in silico sequence analyses (digester sludge sulfate amended microcosms). Restriction TRFLP Sequence Data (bp) Enzyme (bp) Syntrophobacteraceae affiliated sequence 204 209 HaeIII 160 168 MspI 626 628 MseII 238 230 RsaI 91 99 HhaI 61 Table 3.8. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment lengths from in silico sequence analyses (sulfate amended contaminated site soil microcosms). Restriction Enzyme Desulfobulbaceae affiliated sequence HaeIII MspI RsaI HhaI 62 TRFLP (bp) Sequence Data (bp) 202 158 222 92 205 162 226 93 Table 3.9. Success (+) or failure (-) of primers sets for bssA gene amplification. Inocula sources Granular sludge (nitrate amended) Agricultural soil (nitrate amended) Agricultural soil (sulfate amended) Digester sludge (sulfate amended) Contaminated soil (sulfate amended) Forward bssAf Reverse bssAr SRBf SRBr BssN2f BssN2r 7772f 8546r 6888f 8546r 7772f 8828r - - - +(cloned) + + - - - +(cloned) + + - - - - - - - +(cloned) - - - - - +(cloned) - - - +(clone d) 63 TRFLP Relative Abundance (% 100 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3. 1. Percent relative abundance of fragments (digested by Hae III) assigned to Comamonadaceae within buoyant density gradients of DNA extracted from the nitrate amended 13 agricultural soil microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); 13 13 12 ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded). 64 TRFLP Relative Abundance (% 100 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3.2. Percent relative abundance of fragments (digested by Hae III) assigned to Azoarcus within buoyant density gradients of DNA extracted from the nitrate amended agricultural soil 13 13 microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); ♦ C-toluene (~75% 13 12 toluene degraded); ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded). 65 TRFLP Relative Abundance (% 100 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 1.79 DNA Buoyant Density (g/mL) Figure 3.3. Percent relative abundance of fragments (digested by Hae III) assigned to Thauera, within buoyant density gradients of DNA extracted from the nitrate amended granular sludge 13 13 microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); ♦ C-toluene (~75% 13 12 toluene degraded); ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded). 66 TRFLP Relative Abundance (% 100 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density Figure 3.4. Percent relative abundance of fragments (digested by Hae III) assigned to Desulfosporosinus with T-RF 77 bp within buoyant density gradients of DNA extracted from the 13 agricultural soil sulfate amended microcosms. Figure symbols: ▲ C-toluene (~33% toluene 13 13 degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); 12 □ C-toluene (~100% toluene degraded). 67 TRFLP Relative Abundance (% 100 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3.5. Percent relative abundance of fragments (digested by Hae III) assigned to Desulfosporosinus with T-RF 213 bp within buoyant density gradients of DNA extracted from 13 the agricultural soil sulfate amended microcosms. Figure symbols: ▲ C-toluene (~33% toluene 13 13 degraded); ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); 12 □ C-toluene (~100% toluene degraded). 68 TEFLP Relative Abundance (% 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 1.79 DNA Buoyant Density (g/mL) Figure 3.6. Percent relative abundance of fragments (digested by Hae III) assigned to Syntrophobacteraceae within buoyant density gradients of DNA extracted from the digester 13 sludge sulfate amended microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); 13 13 12 ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded). 69 TRFLP Relative Abundance (% 80 60 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3.7. Percent relative abundance of fragments (digested by Hae III) assigned to Desulfobulbaceae within buoyant density gradients of DNA extracted from the contaminated site, 13 sulfate amended microcosms. Figure symbols: ▲ C-toluene (~33% toluene degraded); 13 13 12 ♦ C-toluene (~75% toluene degraded); ■ C-toluene (~100% toluene degraded); □ C-toluene (~100% toluene degraded). 70 Ag Soil Nitrate Amended Clone 12 Ag Soil Nitrate Reducing Clone 10 Ag Soil Nitrate Amended Clone 11 Ag Soil Nitrate Amended Clone 5 Ag Soil Nitrate Amended Clone 4 Thauera sp. DNT-1 Uncultured Clone LA07bs04 (GU133294.1) Uncultured Clone LA07bs07 (GU133296.1) Azoarcus sp. DN11 (AB285034.1) Azoarcus sp. T (AY032676.1) Uncultured Clone bssAC12 (FJ810633.1) Uncultured Clone bssAC18 (FJ810639.1) Uncultured Clone bssAC06 (FJ810627.1) Uncultured Clone bssAC08 (FJ810629.1) Uncultured Clone bssAC11 (FJ810632.1) Uncultured Clone bssAD01 (FJ810643.1) Uncultured Clone bssAD03 (FJ810645.1) Uncultured Clone bssAC09 (FJ810630.1) Uncultured Clone bssAC07 (FJ810628.1) Uncultured Clone bssAC15 (FJ810636.1) Uncultured Clone bssAD07 (FJ810647.1) Magnetospirillum sp. TS-6 (AB167725.1) Azoarcus aromaticum EbN1 (CR555306.1) Thauera aromatica (AJ001848.3) Uncultured Clone LA07bs16 (GU133304.1) Uncultured Clone bssAC17 (FJ810638.1) Uncultured Clone bssAC19 (FJ810640.1) Uncultured Clone bssAD02 (FJ810644.1) Desulfobacterium cetonicum (EF123662.1) Bacterium Clone B1C1 (GU123599.1) Sulfate Reduc. Bact. TRM1 (EF123667.1) Bacterium Clone B1B6 (GU123598.1) Uncultured Clone Zz-ox 76 (FJ889137.1) Geobacter sp. TMJ1 (EF123666.1) Bacterium bssA-1 (EF134966.1) Uncultured Clone bssAC03 (FJ810624.1) Uncultured Clone bssAC01 (FJ810622.1) 0.05 Figure 3.8. Phylogenetic tree of bssA partial sequences (722 bp) from nitrate amended agricultural soil microcosms (using the primer set 7772f/8546r) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. 71 Granular Sludge Nitrate Amended Clone 1 Granular Sludge Nitrate Amended Clone 3 Granular Sludge Nitrate Amended Clone 5 Granular Sludge Nitrate Amended Clone 6 Granular Sludge Nitrate Amended Clone 2 Granular Sludge Nitrate Amended Clone 4 Thauera sp. DNT-1 (AB066263.1) Uncultured Clone LA07bs07 (GU133296.1) Uncultured Clone LA07bs04 (GU133294.1) Thauera aromatica (AF113168.1) Azoarcus sp. DN11 (AB285034.1) Azoarcus sp. T (AY032676.1) Uncultured Clone bssAC12 (FJ810633.1) Uncultured Clone bssAC18 (FJ810639.1) Uncultured Clone bssAC11 (FJ810632.1) Uncultured Clone bssAC06 (FJ810627.1) Uncultured Clone bssAC08 (FJ810629.1) Uncultured Clone bssAD03 (FJ810645.1) Azoarcus aromaticum EbN1 (CR555306.1) Magnetospirillum sp. TS-6 (AB167725.1) Uncultured Clone bssAC17 (FJ810638.1) Uncultured Clone bssAC19 (FJ810640.1) Uncultured Clone bssAD02 (FJ810644.1) Uncultured Clone LA07bs01 (GU133291.1) 0.05 Figure 3.9. Phylogenetic tree of bssA partial sequences (722 bp) from nitrate amended granular sludge microcosms (using the primer set 7772f/8546r) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. 72 Digester Sulfate Amended Clone 2 Digester Sulfate Amended Clone 1 Digester Sulfate Amended Clone 3 Sulf. reduc. bact. PRTOL1 (EU780921.1) Bacterium bssA (EF134966.1) Magnetospirillum sp. TS-6 (AB167725.1) Aromatoleum aromaticum EbN1 (CR555306.1) Uncultured Thauera sp. (AM887515.1) Uncultured Thauera sp. (AM887514.1) Uncultured Thauera sp. (AM887512.1) Uncultured Thauera sp. (AM887517.1) Uncultured Thauera sp. (AM887513.1) Thauera aromatica (AJ001848.3) Uncultured Thauera sp. (AM887516.1) Thauera aromatica strain T1 (AF113168.1) Thauera sp. DNT-1 (AB066263.1) Desulfobacula toluolica (CU466268.1) Geobacter metallireducens (AF441130.1) 0.5 Figure 3. 10. Phylogenetic trees of bssA partial sequences (97 bp) from sulfate amended digester sludge microcosms (using the primer set SRBf/SRBr) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. 73 Contam. Soil Sulfate Amended Clone 1 Contam. Soil Sulfate Amended Clone 5 Contam. Soil Sulfate Amended Clone 3 Enrichment Clone B1C1 (GU123599.1) Sulfate Reduc. Bact. TRM1 (EF123667.1) Contam. Soil Sulfate Amended Clone 7 Contam. Soil Sulfate Amended Clone 4 Enrichment Clone B2B2 (GU123600.1) Contam. Soil Sulfate Amended Clone 2 Contam. Soil Sulfate Reducing Clone 6 Enrichment Clone B1B6 (GU123598.1) Sulfate Reduc. Bact. PRTOL1 (EU780921.1) Desulfobacula toluolica (CU466268.1) Uncultured Clone LA07bs01 (GU133291.1) Uncultured Clone bssAC14 (FJ810635.1) Contam. Soil Sulfate Reducing Clone 8 Uncultured Clone Zz-ox 76 (FJ889137.1) Geobacter sp. TMJ1 (EF123666.1) Geobacter grbiciae DSM (EF123664.1) Geobacter metallireducens (AF441130.1) Bacterium bssA-1 (EF134966.1) Azoarcus aromaticum EbN1 (CR555306.1) Thauera aromatica (AJ001848.3) Magnetospirillum sp. TS-6 (AB167725.1) Thauera sp. DNT-1 (AB066263.1) Uncultured Clone Zz-ox 12 (FJ889136.1) Azoarcus sp. DN11 (AB285034.1) Azoarcus sp. T (AY032676.1) 0.05 Figure 3.11. Phylogenetic trees of bssA partial sequences (637 bp) from sulfate amended contaminated soil microcosms (using the primer set 7772f/8828r) along with the closest matches in GenBank, constructed with MEGA 4.1 software using the neighbor-joining method. 74 bssA Gene Abundance 1 0.8 0.6 0.4 0.2 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3.12. Difference between abundance of bssA gene copies in ultracentrifugation fractions 13 from labeled ( C toluene) and unlabeled toluene amended microcosms from the granular sludge 13 nitrate amended microcosms as determined via qPCR. Figure symbols: ■ C-toluene (~100% 12 toluene degraded); □ C-toluene (~100% toluene degraded). 75 bssA Gene Abundance 1 0.8 0.6 0.4 0.2 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3.13. Difference between abundance of bssA gene copies in ultracentrifugation fractions 13 from labeled ( C toluene) and unlabeled toluene amended microcosms from the agricultural soil 13 nitrate amended microcosms as determined via qPCR. Figure symbols: ■ C-toluene (~100% 12 toluene degraded); □ C-toluene (~100% toluene degraded). 76 bssA Gene Abundance 1 0.8 0.6 0.4 0.2 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 3.14. Difference between abundance of bssA gene copies in ultracentrifugation fractions 13 from labeled ( C toluene) and unlabeled toluene amended microcosms from the digester sludge 13 sulfate amended microcosms as determined via qPCR. Figure symbols: ■ C-toluene (~100% 12 toluene degraded); □ C-toluene (~100% toluene degraded). 77 REFERENCES 78 References 1. Abu Laban, N., D. Selesi, T. Rattei, P. Tischler, and R. U. Meckenstock. 2010. Identification of enzymes involved in anaerobic benzene degradation by a strictly anaerobic iron-reducing enrichment culture. Environ Microbiol 12:2783-2796. 2. Achong, G. R., A. M. Rodriguez, and A. M. Spormann. 2001. Benzylsuccinate synthase of Azoarcus sp strain T: Cloning, sequencing, transcriptional organization, and its role in anaerobic toluene and m-xylene mineralization. J Bacteriol 183:6763-6770. 3. Allen, T. D., P. F. Kraus, P. A. Lawson, G. R. Drake, D. L. Balkwill, and R. S. Tanner. 2008. Desulfovibrio carbinoliphilus sp nov., a benzyl alcohol-oxidizing, sulfate-reducing bacterium isolated from a gas condensate-contaminated aquifer. Int J Syst Evol Micr 58:1313-1317. 4. Altenschmidt, U., and G. Fuchs. 1991. Anaerobic degradation of toluene in denitrifying Pseudomonas sp.: indication for toluene methylhydroxylation and benzoyl-CoA as central aromatic intermediate. Arch Microbiol 156:152-158. 5. Altenschmidt, U., and G. Fuchs. 1992. Anaerobic Toluene Oxidation to Benzyl Alcohol and Benzaldehyde in a Denitrifying Pseudomonas Strain. J Bacteriol 174:4860-4862. 6. Anders, H. J., A. Kaetzke, P. Kampfer, W. Ludwig, and G. Fuchs. 1995. Taxonomic Position of Aromatic-Degrading Denitrifying Pseudomonad Strains K-172 and Kb-740 and Their Description as New Members of the Genera Thauera, as Thauera-Aromatica Sp-Nov, and Azoarcus, as Azoarcus-Evansii Sp-Nov, Respectively, Members of the Beta-Subclass of the Proteobacteria. Int J Syst Bacteriol 45:327-333. 7. Ariesyady, H. D., T. Ito, K. Yoshiguchi, and S. Okabe. 2007. Phylogenetic and functional diversity of propionate-oxidizing bacteria in an anaerobic digester sludge. Appl Microbiol Biot 75:673-683. 8. Beller, H. R., S. R. Kane, T. C. Legler, J. R. McKelvie, B. S. Lollar, F. Pearson, L. Balser, and D. M. MacKay. 2008. Comparative assessments of benzene, toluene, and xylene natural attenuation by quantitative polymerase chain reaction analysis of a catabolic gene, signature metabolites, and compound-specific isotope analysis. Environ Sci Technol 42:6065-6072. 9. Beller, H. R., and A. M. Spormann. 1997. Benzylsuccinate formation as a means of anaerobic toluene activation by sulfate-reducing strain PRTOL1. Appl Environ Microb 63:3729-3731. 10. Beller, H. R., A. M. Spormann, P. K. Sharma, J. R. Cole, and M. Reinhard. 1996. Isolation and characterization of a novel toluene-degrading, sulfate-reducing bacterium. Appl Environ Microb 62:1188-1196. 79 11. Biegert, T., G. Fuchs, and F. 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. 12. Bombach, P., A. Chatzinotas, T. R. Neu, M. Kastner, T. Lueders, and C. Vogt. 2010. Enrichment and characterization of a sulfate-reducing toluene-degrading microbial consortium by combining in situ microcosms and stable isotope probing techniques. Fems Microbiol Ecol 71:237-246. 13. Botton, S., M. van Harmelen, M. Braster, J. R. Parsons, and W. F. M. Roling. 2007. Dominance of Geobacteraceae in BTX-degrading enrichments from an iron-reducing aquifer. Fems Microbiol Ecol 62:118-130. 14. Chakraborty, R., S. M. O'Connor, E. Chan, and J. D. Coates. 2005. Anaerobic degradation of benzene, toluene, ethylbenzene, and xylene compounds by Dechloromonas strain RCB. Appl Environ Microbiol 71:8649-8655. 15. Coates, J. D., R. Chakraborty, J. G. Lack, S. M. O'Connor, K. A. Cole, K. S. Bender, and L. A. Achenbach. 2001. Anaerobic benzene oxidation coupled to nitrate reduction in pure culture by two strains of Dechloromonas. Nature 411:1039-1043. 16. Cupples, A. M., and G. K. Sims. 2007. Identification of in situ 2,4-dichlorophenoxyacetic acid-degrading soil microorganisms using DNA-stable isotope probing. Soil Biol Biochem 39:232-238. 17. Etchebehere, C., M. I. Errazquin, P. Dabert, R. Moletta, and L. Muxi. 2001. Comamonas nitrativorans sp nov., a novel denitrifier isolated from a denitrifying reactor treating landfill leachate. Int J Syst Evol Micr 51:977-983. 18. Gittel, A., K. B. Sorensen, T. L. Skovhus, K. Ingvorsen, and A. Schramm. 2009. Prokaryotic Community Structure and Sulfate Reducer Activity in Water from High-Temperature Oil Reservoirs with and without Nitrate Treatment. Appl Environ Microb 75:7086-7096. 19. Harmsen, H. J. M., B. Wullings, A. D. L. Akkermans, W. Ludwig, and A. J. M. Stams. 1993. Phylogenetic Analysis of Syntrophobacter-Wolinii Reveals a Relationship with Sulfate-Reducing Bacteria. Arch Microbiol 160:238-240. 20. Herrmann, S., S. Kleinsteuber, A. Chatzinotas, S. Kuppardt, T. Lueders, H. H. Richnow, and C. Vogt. 2010. Functional characterization of an anaerobic benzene-degrading enrichment culture by DNA stable isotope probing. Environ Microbiol 12:401-411. 21. Herrmann, S., S. Kleinsteuber, T. R. Neu, H. H. Richnow, and C. Vogt. 2008. Enrichment of anaerobic benzene-degrading microorganisms by in situ microcosms. Fems Microbiol Ecol 63:94-106. 80 22. Herrmann, S., C. Vogt, A. Fischer, A. Kuppardt, and H. H. Richnow. 2009. Characterization of anaerobic xylene biodegradation by two-dimensional isotope fractionation analysis. Env Microbiol Rep 1:535-544. 23. Hurek, T., and B. Reinholdhurek. 1995. Identification of Grass-Associated and Toluene-Degrading Diazotrophs, Azoarcus Spp, by Analyses of Partial 16s Ribosomal DNA-Sequences. Appl Environ Microb 61:2257-2261. 24. Jin, S., P. H. Fallgren, A. A. Bilgin, J. M. Morris, and P. W. Barnes. 2007. Bioremediation of benzene, ethylbenzene, and xylenes in groundwater under iron-amended, sulfate-reducing conditions. Environ Toxicol Chem 26:249-253. 25. Kane, S. R., H. R. Beller, T. C. Legler, and R. T. Anderson. 2002. Biochemical and genetic evidence of benzylsuccinate synthase in toluene-degrading, ferric iron-reducing Geobacter metallireducens. Biodegradation 13:149-154. 26. Khan, S. T., Y. Horiba, M. Yamamoto, and A. Hiraishi. 2002. Members of the family Comamonadaceae as primary poly(3-hydroxybutyrate-co-3-hydroxyvalerate)-degrading denitrifiers in activated sludge as revealed by a polyphasic approach. Appl Environ Microb 68:3206-3214. 27. Kleinsteuber, S., K. M. Schleinitz, J. Breitfeld, H. Harms, H. H. Richnow, and C. Vogt. 2008. Molecular characterization of bacterial communities mineralizing benzene under sulfate-reducing conditions. Fems Microbiol Ecol 66:143-157. 28. Krieger, C., W. Roseboom, S. P. J. Albracht, and A. M. Spormann. 2001. A Stable Organic Free Radical in Anaerobic Benzylsuccinate Synthase of Azoarcus sp. Strain T. The Journal of Biological Chemistry 286:4. 29. Kuhner, S., L. Wohlbrand, I. Fritz, W. Wruck, C. Hultschig, P. Hufnagel, M. Kube, R. Reinhardt, and 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. 30. Kunapuli, U., T. Lueders, and R. U. Meckenstock. 2007. The use of stable isotope probing to identify key iron-reducing microorganisms involved in anaerobic benzene degradation. Isme J 1:643-653. 31. Lee, Y. J., C. S. Romanek, and J. Wiegel. 2009. Desulfosporosinus youngiae sp nov., a spore-forming, sulfate-reducing bacterium isolated from a constructed wetland treating acid mine drainage. Int J Syst Evol Micr 59:2743-2746. 32. Leuthner, B., C. Leutwein, H. Schulz, P. Horth, W. Haehnel, E. Schiltz, H. Schagger, and J. Heider. 1998. Biochemical and genetic characterization of benzylsuccinate synthase from Thauera aromatica: a new glycyl radical enzyme catalysing the first step in 81 anaerobic toluene metabolism. Mol Microbiol 28:615-628. 33. Liou, J. S. C., C. M. DeRito, and E. L. Madsen. 2008. Field-based and laboratory stable isotope probing surveys of the identities of both aerobic and anaerobic benzene-metabolizing microorganisms in freshwater sediment. Environ Microbiol 10:1964-1977. 34. Liu, A., E. Garcia-Dominguez, E. D. Rhine, and L. Y. Young. 2004. A novel arsenate respiring isolate that can utilize aromatic substrates. Fems Microbiol Ecol 48:323-332. 35. Loy, A., K. Kusel, A. Lehner, H. L. Drake, and M. Wagner. 2004. Microarray and functional gene analyses of sulfate-reducing prokaryotes in low-sulfate, acidic fens reveal cooccurrence of recognized genera and novel lineages. Appl Environ Microb 70:6998-7009. 36. Lueders, T., M. Manefield, and M. W. Friedrich. 2004. Enhanced sensitivity of DNAand rRNA-based stable isotope probing by fractionation and quantitative analysis of isopycnic centrifugation gradients. Environ Microbiol 6:73-78. 37. Luo, C. L., S. G. Xie, W. M. Sun, X. D. Li, and A. M. Cupples. 2009. Identification of a Novel Toluene-Degrading Bacterium from the Candidate Phylum TM7, as Determined by DNA Stable Isotope Probing. Appl Environ Microb 75:4644-4647. 38. Mechichi, T., E. Stackebrandt, and G. Fuchs. 2003. Alicycliphilus denitrificans gen. nov., sp nov., a cyclohexanol-degrading, nitrate-reducing beta-proteobacterium. Int J Syst Evol Micr 53:147-152. 39. Meckenstock, R. U. 1999. Fermentative toluene degradation in anaerobic defined syntrophic cocultures. Fems Microbiol Lett 177:67-73. 40. Morasch, B., B. Schink, C. C. Tebbe, and R. U. Meckenstock. 2004. Degradation of o-xylene and m-xylene by a novel sulfate-reducer belonging to the genus Desulfotomaculum. Archives of Microbiology 181:407-417. 41. Muller, S., C. Vogt, M. Laube, H. Harms, and S. Kleinsteuber. 2009. Community dynamics within a bacterial consortium during growth on toluene under sulfate-reducing conditions. Fems Microbiol Ecol 70:586-596. 42. Ommedal, H., and T. Torsvik. 2007. Desulfotignum toluenicum sp nov., a novel toluene-degrading, sulphate-reducing bacterium isolated from an oil-reservoir model column. Int J Syst Evol Micr 57:2865-2869. 43. Pelz, O., A. Chatzinotas, A. Zarda-Hess, W. R. Abraham, and J. Zeyer. 2001. Tracing toluene-assimilating sulfate-reducing bacteria using C-13-incorporation in fatty acids and whole-cell hybridization. Fems Microbiol Ecol 38:123-131. 82 44. Pilloni, G., F. von Netzer, M. Engel, and T. Lueders. 2011. Electron acceptor-dependent identification of key anaerobic toluene degraders at a tar-oil-contaminated aquifer by Pyro-SIP. Fems Microbiol Ecol. 45. Rabus, R., and F. Widdel. 1995. Anaerobic degradation of ethylbenzene and other aromatic hydrocarbons by new denitrifying bacteria. Archives of Microbiology 163:96-103. 46. Reinhard, M., S. Shang, P. K. Kitanidis, E. Orwin, G. D. Hopkins, and C. A. Lebron. 1997. In situ BTEX biotransformation under enhanced nitrate- and sulfate-reducing conditions (vol 31, pg 28, 1997). Environ Sci Technol 31:1580-1580. 47. Robertson, W. J., P. D. Franzmann, and B. J. Mee. 2000. Spore-forming, Desulfosporosinus-like sulphate-reducing bacteria from a shallow aquifer contaminated with gasolene. J Appl Microbiol 88:248-259. 48. Shinoda, Y., J. Akagi, Y. Uchihashi, A. Hiraishi, H. Yukawa, H. Yurimoto, Y. Sakai, and N. Kato. 2005. Anaerobic degradation of aromatic compounds by Magnetospirillum strains: Isolation and degradation genes. Biosci Biotech Bioch 69:1483-1491. 49. Shinoda, Y., Y. Sakai, H. Uenishi, Y. Uchihashi, A. Hiraishi, H. Yukawa, H. Yurimoto, and N. Kato. 2004. Aerobic and anaerobic toluene degradation by a newly isolated denitrifying bacterium, Thauera sp strain DNT-1. Appl Environ Microb 70:1385-1392. 50. Song, B., L. Y. Young, and N. J. Palleroni. 1998. Identification of denitrifier strain T1 as Thauera aromatica and proposal for emendation of the genus Thauera definition. Int J Syst Bacteriol 48:889-894. 51. Sousa, D. Z., J. I. Alves, M. M. Alves, H. Smidt, and A. J. M. Stams. 2009. Effect of sulfate on methanogenic communities that degrade unsaturated and saturated long-chain fatty acids (LCFA). Environ Microbiol 11:68-80. 52. Sousa, D. Z., M. A. Pereira, A. J. M. Stams, M. M. Alves, and H. Smidt. 2007. Microbial communities involved in anaerobic degradation of unsaturated or saturated long-chain fatty acids. Appl Environ Microb 73:1054-1064. 53. Sun, W. M., S. G. Xie, C. L. Luo, and A. M. Cupples. 2010. Direct Link between Toluene Degradation in Contaminated-Site Microcosms and a Polaromonas Strain. Appl Environ Microb 76:956-959. 54. Trautwein, K., S. Kuhner, L. Wohlbrand, T. Halder, K. Kuchta, A. Steinbuchel, and R. Rabus. 2008. Solvent stress response of the denitrifying bacterium "Aromatoleum aromaticum" strain EbN1. Applied and Environmental Microbiology 74:2267-2274. 55. Washer, C. E., and E. A. Edwards. 2007. Identification and expression of benzylsuccinate synthase genes in a toluene-degrading methanogenic consortium. Appl 83 Environ Microb 73:1367-1369. 56. Winderl, C., B. Anneser, C. Griebler, R. U. Meckenstock, and T. Lueders. 2008. Depth-resolved quantification of anaerobic toluene degraders and aquifer microbial community patterns in distinct redox zones of a tar oil contaminant plume. Appl Environ Microb 74:792-801. 57. Winderl, C., H. Penning, F. von Netzer, R. U. Meckenstock, and T. Lueders. 2010. DNA-SIP identifies sulfate-reducing Clostridia as important toluene degraders in tar-oil-contaminated aquifer sediment. Isme J 4:1314-1325. 58. Winderl, C., S. Schaefer, and T. Lueders. 2007. Detection of anaerobic toluene and hydrocarbon degraders in contaminated aquifers using benzylsuccinate synthase (bssA) genes as a functional marker. Environ Microbiol 9:1035-1046. 59. Xie, S. G., W. M. Sun, C. L. Luo, and A. M. Cupples. 2011. Novel aerobic benzene degrading microorganisms identified in three soils by stable isotope probing. Biodegradation 22:71-81. 60. Xie, S. G., W. M. Sun, C. L. Luo, and A. M. Cupples. 2010. Stable Isotope Probing Identifies Novel m-Xylene Degraders in Soil Microcosms from Contaminated and Uncontaminated Sites. Water Air Soil Poll 212:113-122. 61. Yang, Y. R., and J. Zeyer. 2003. Specific detection of Dehalococcoides species by fluorescence in situ hybridization with 16S rRNA-targeted oligonucleotide probes. Appl Environ Microb 69:2879-2883. 62. Zhou, J. Z., M. R. Fries, J. C. Cheesanford, and J. M. Tiedje. 1995. Phylogenetic Analyses of a New Group of Denitrifiers Capable of Anaerobic Growth on Toluene and Description of Azoarcus-Tolulyticus Sp-Nov. Int J Syst Bacteriol 45:500-506. 63. Zhou, J. Z., A. V. Palumbo, and J. M. Tiedje. 1997. Sensitive detection of a novel class of toluene-degrading denitrifiers, Azoarcus tolulyticus, with small-subunit rRNA primers and probes. Appl Environ Microb 63:2384-2390. 84 CHAPTER 4 PRESENCE,DIVERSITY AND THE ENUMERATION OF TOLUENE DEGRADING FUNCTIONAL GENES (BSSA AND BAMA) ACROSS A RANGE OF REDOX CONDITIONS AND INOCULUM SOURCES Introduction An understanding of the biodegradation pathways for aromatic compounds is important for the remediation of many contaminated environments. Biodegradation under anaerobic conditions is especially critical to comprehend because under these conditions, which are typical at many contaminated aquifers, removal rates are slow and therefore time for site closure may be prolonged. A common approach for understanding biodegradation pathways involves an analysis of the microbial community at the molecular level. Although an investigation into 16S rRNA genes can provide useful indicator data, it is now well recognized that more information can be gained by studying key functional genes. Recent research in this area involves the design and application of molecular assays targeted to the benzoyl-CoA degradation pathway to investigate the diversity of microorganisms involved in anaerobic aromatic biodegradation (9, 10, 14). Anaerobic aromatic biodegradation typically involves the channeling of aromatic growth substrates to the central intermediate benzoyl-coenzyme A (CoA) prior to dearomatization and ring cleavage(9). In Thauera aromatica, the metabolism of benzoyl-CoA comprises of several steps with ring cleavage action by 6-oxocylcohex-1-ene-1-carbonyl-CoA (6-OCH-CoA) hydrolase, which likely catalyzes the transformation of 6-OCH-CoA to 6-hydroxypimelyl-CoA (9, 11). Enzymes similar to those in the benzoyl-CoA pathway in T. aromatica are reported to be present in most other aromatic degrading facultative anaerobes(5, 12). The ring-cleaving 85 hydrolase of the benzoyl-CoA pathway is encoded by the bamA gene. Recently, this pathway was studied in obligate anaerobes that use aromatic growth substrates (9). The researchers expressed genes putatively encoding for 6-OCH-CoA hydrolases from the obligately anaerobic Geobacter metallireducens and Syntrophus aciditrophicus in Escherichia coli and identified the products as 6-OCH-CoA hydrolases and found these genes to be highly conserved in all anaerobic bacteria using aromatic growth substrates (9). The researchers also designed primers to amplify the gene of 6-OCH-CoA in a number or obligate and facultative anaerobes (G. metallireducens GS-15, T. aromatic K172, Azoarcus EbN1, A. evansii KB740, Desulfococcus multivorans, S. aciditrophicus SB, Magnetospirillum species TS-6 and CC-26) as well as from two sediment-free sulfate reducing mixed cultures degrading toluene or m-xylene. To date, there have only been two applications of the primers developed from this first study, the bamA assay was modified and used to investigate bamA gene sequences in two recent field studies(10, 14). One study investigated the diversity of bamA sequences in microcosms incubated at benzene contaminated aquifers (10). In the other study, the authors investigated the diversity of mono-aromate-degrading microorganisms by targeting the functional genes encoding benzylsuccinate synthase α-subunit (bssA) as well as bamA (14). Benzylsuccinate synthase is a key enzyme for anaerobic toluene biodegradation under nitrate reducing (1, 8), sulfate reducing (18-20), ferric iron reducing (4, 7), and methanogenic enrichment cultures or environmental samples (17, 18). In this second field study, the site was a leachate contaminated aquifer near the Banisveld landfill (the Netherlands) under iron reducing conditions. The work involved analysis of groundwater samples along a pollution plume in 1999 and 2004, which enabled the researchers to correlate site conditions (e.g. ferrous iron concentrations and dissolved organic 86 matter) with sequence diversity. The overall objective of the current study was to expand on the three bamA studies to further investigate the diversity of bamA sequences across different redox conditions and inoculum sources. For this, we studied a number of toluene-degrading mixed microbial communities seeded from a wide range of sources, including contaminated soil from different sites, uncontaminated soil, anaerobic granular and digester sludge and aerobic activated sludge. The work is novel because it is the first to provide an in depth investigation of bamA diversity in microcosms over a range of redox conditions and inoculum sources. In addition, quantitative PCR (qPCR) assays to both bamA and bssA were developed and applied to a sub-set of these samples. In summary, this research involved the following specific objectives 1) to determine the diversity of bamA sequences in toluene degrading microcosms over a range of redox conditions, 2) to investigate the diversity of bamA sequences in microcosms from different sources including contaminated and non-contaminated sites and 3) to determine if qPCR targeted to the bamA and bssA genes could provide a reliable indicator for growth related toluene degradation. Materials and Methods Screening of Toluene Degrading Microcosms A wide range of inoculum sources were examined for toluene biodegradation. The inocula were taken from pristine agricultural soils (MI), previous gasoline contaminated soils (MI), sediments from a former gas-compressor site (6) (OK), digester sludges from two wastewater treatment plants (MI), activated sludge (MI) and anaerobic granular sludge (WA). Triplicates of ~10g (wet 87 weight) biomass were incubated in sterile 160 mL serum bottles containing 50 mL anaerobic basal media (21), sealed with rubber stoppers and aluminum seals. Microcosms were prepared under strictly anaerobic conditions in an anaerobic chamber (Coy Laboratory Products INC, Grass Lake, MI). Potassium nitrate and magnesium sulfate were added to a final concentration of 1gL -1 - 2- NO3 and SO4 .From approximately fifty three incubations, six nitrate-amended, five sulfate-amended and five methane generating (methanogenic) microcosms exhibited toluene degradation and these were selected for DNA extraction. In addition, three nitrate amended, one sulfate amended and two methanogenic microcosms were selected for qPCR. In this experimental set, triplicate microcosms were set up for each treatment. For each microcosm, 3 g biomass was anoxically incubated in 60 mL serum bottles containing 25 mL of anaerobic basal media as described above. The microcosm inoculum sources and the experiments conducted on each microcosm type are summarized in table 3.1. Toluene concentrations in headspace gas samples (200 μL) were typically determined weekly with a gas chromatograph (Perkin Elmer) equipped with flame ionization detector and a capillary column (J&W Scientific, DB-624, diameter 0.53mm). Injector and detector temperature were set at 200 oC and the column temperature was 120oC. DNA Extraction and PCR For the functional gene diversity studies (see below), microcosms exhibiting toluene biodegradation were sacrificed for DNA extraction when toluene was depleted in each microcosm. For the qPCR studies, DNA was extracted from samples (0.3g soil, wet weight) sacrificed at successive time points (typically 0, 50, and 100%) to enumerate the bamA genes and 88 bssA genes during the course of toluene depletion. The powersoil DNA extraction kit (MO BIO Laboratories, Inc. Carlsbad, CA) was used for total nucleic acids extraction according to the manufacturer’s recommended procedure. The presence of the benzylsuccinate synthase alpha-subunit gene (bssA) and 6-oxocyclohex-1-ene-1-carBoN1yl-CoA hydrolase (bamA) was investigated with a number of previously reported primers pairs (Table 4.1). A gradient PCR was performed with annealing temperature ranging from 45ºC to 58 ºC. The presence of PCR amplicons were determined using gel electrophoresis. A number of positive amplicons were selected for cloning and sequencing (see below). Quantitative PCR Three nitrate amended consortia, one sulfate amended consortium and two methanogenic consortia were selected for enumerating bssA and bamA genes during toluene biodegradation (Table 4.1). The quantification assays were conducted in a Chromo 4 real-time PCR cycler (Bio-Rad) using the primer sets 7772f/8546r (AgN, GSN, BoN11, HaM, ASM), 7772f/8828r (DUKE), (bssA) or Bam-sp9 and Bam-asp1 (bamA) (Table 4.1). Each 20 μL PCR reaction mixture containing 10 μL SYBR green real-time PCR solution (Applied Biosystems), 0.25 μM of each primer, and 1 μL DNA template. The thermal protocol consisted of an initial denaturation (95 ºC, 15 min), 40 cycles of amplification (95 ºC, 15 s; 55 ºC, 20 s; 72 ºC 20 s) and a terminal extension step (72 ºC, 2 min). Melting curves were constructed from 55 ºC to 95 ºC, read every 0.6ºC for 2 s. For each gradient fraction, 1 μL solution was diluted with 3 μL water as template (to conserve the sample). Cloned plasmid DNA was utilized as a standard for quantification. 89 Sequencing of Partial bssA and bamA Genes Representative bssA and bamA amplicons were prepared for cloning and sequencing. The PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.) and cloned into Escherichia coli TOP10 vector supplied with a TOPO TA cloning kit (Invitrogen Corporation). E. -1 coli clones were grown on Luria-Bertani (LB) medium solidified with 15 g agar L with 50 g -1 ampicillin L for 16 h at 37 ºC. Colonies with inserts were verified by PCR with primers M13 F (5’-TGTAAAACGACGGCCAGT-3’) and M13 R (5’-AACAGCTATGACCATG-3’), plasmids were extracted from the positive clones with a QIAprep miniprep system (Qiagen, Inc.) and the insertions were sequenced at RTSF. Phylogenetic trees for the partial bamA and bssA sequences along with the closest matches in Genbank were obtained by the neighbor-joining method using MEGA 4.1 software. Results This research builds on a previous study that involved a community analysis of five anaerobic toluene degrading consortia. In that research, the active toluene degraders were identified using stable isotope probing. The putative toluene degraders were classified within the genus Thauera (nitrate amended, GSN), the family Comamonadaceae (nitrate amended, AgN), the genus Desulfosporosinus (sulfate amended AgS), the family Syntrophobacteraceae (sulfate amended, DSS) and the family Desulfobulbaceae (sulfate amended, DUKE). In addition, partial bssA sequences were obtained from four of the five consortia. The current study expands on this research to investigate a larger number of toluene degrading samples (sixteen), includes methanogenic microcosms, targets the presence and diversity of the bamA gene and 90 quantitatively investigates the presence of the bamA and bssA genes in six of these samples. bssA and bamA Gene Amplification Primer sets 7772f/8546r(20) and bssAf/bssAr(2) produced strong specific amplicons for all six and for five of the six (except DSN) of the nitrate amended microcosms, respectively. The three other bssA primer pairs produced strong amplicons in only a small number of these microcosms (Table 4.1). In the sulfate amended microcosms, SRBf/SRBr(3) produced strong specific amplicons in four of the five (except BoS1) tested microcosms. Again, other primer pairs produced specific amplicons in only a small number of the microcosms. The primer set 7772f/8828r(20) produced a strong specific amplicon for DUKE and was therefore used for the qPCR assay on this sample. In the methanogenic microcosms, 7772f/8546f(20) performed well in two (HaM and ASM) of the five microcosms tested and was used for the qPCR assays. Only one other primer pair (bss1500f/bss2100r(13)) produced a strong amplicon in the methanogenic microcosms, and this was true for only one of the five methanogenic microcosms (SM). Overall, the success of bssA gene amplification was greatest in the nitrate amended microcosms and least in the methanogenic microcosms. This reflects the limited bssA sequence information (and therefore primers) on toluene degradation under methanogenic conditions compared to under nitrate reducing conditions. A number of the partial bssA sequences amplified were cloned and sequenced. This work is an extension of a previous study on these samples. Previously, we obtained partial bssA sequences from four of these samples (AgN, GSN, DSS and DUKE). The partial bssA sequences from the nitrate amended microcosms (AgN and GSN) were found to be most similar to the bssA gene 91 from Thauera sp. DNT-1. In contrast, the majority (except one) of the previously obtained bssA sequences from the sulfate amended samples (DSS and DUKE) were most similar to the bssA sequence from sulfate reducing bacterium PRTOL1. One sequence from the contaminated site soil (DUKE) classified closest to an uncultured clone (Zz-ox 76) submitted to GenBank from an unpublished study entitled characterization of anaerobic xylene biodegradation by two dimensional isotope fractionation analysis. The current study adds to this growing database on bssA gene diversity. Specifically, bssA sequences were determined from two additional nitrate amended microcosms constructed from another agricultural soil (BoN11) and from digester sludge (DSN). Also, partial bssA sequences were obtained from methanogenic microcosms constructed from agricultural soil (HaM) or contaminated soil (SM). The results regarding the amplification of bamA displayed a higher level of success. The primer pair (bam-sp9 and Bam-asp1(9)) targeting the bamA gene produced strong specific amplicons in all toluene-degrading microcosms tested except for one (contaminated soil, SM, methanogenic microcosm). To examine the diversity of the bamA gene, amplicons were sequenced from six of these samples (GSN, BoN1, DSS, DUKE, HaM and ASM). These samples were selected to represent two of each redox condition. The sequences obtained were compared to the GenBank database. bssA and bamA Gene Quantification Quantitative PCR was used to examine the applicability of targeting both functional genes as a potential rapid screening method for toluene degradation potential. Microcosms from each redox condition were selected for qPCR, three for nitrate amended samples (AgN, GSN, BoN1), one 92 for sulfate amended samples (DUKE) and two for the methanogenic samples (HaM and ASM). In each case, the number of both genes increased over time as toluene was degraded (Figure 4.1-4.6). In the nitrate amended samples (Figure 4.1-4.3), DNA was extracted three or three times during the toluene degradation period. For each experiment, a clear increase in bssA and bamA gene numbers was seen and the raise occurred simultaneously with the course of toluene degradation. The gene numbers of the bssA in GSN, AgN and BoN1 were approximately 145, 10200 and 400 times higher than those in the original sampling point. Similarly, the gene numbers of bamA were 3.62, 394 and 236 higher at the end compared to the beginning of the study for GSN, AgN and BoN1, respectively. In the one sulfate amended (DUKE) and two methanogenic (ASM and HaM) microcosms (Figure 4.4-4.6), DNA was extracted two times during the toluene degradation period. In all three, gene numbers of bssA and bamA increased with time as toluene was degraded. Interestingly, the final gene number for both genes differed considerably between the range of redox conditions. In the nitrate amended samples, the final bssA gene numbers were 8 between 10 and 10 10 per gram of soil. Whereas in the sulfate amended and methanogenic 7 8 microcosms, bssA gene numbers were between 10 and 10 per gram of soil. A similar trend was noted for the bamA gene. In the nitrate amended microcosms, final bamA gene numbers were in 8 9 the range of 10 and 10 per gram of soil. In the sulfate amended and methanogenic microcosms, 7 9 bamA gene numbers were between 10 and 10 per gram of soil. These patterns suggest the toluene degrading population is higher under nitrate amended conditions. 93 Discussion The partial bssA and bamA sequences obtained in the current study provide an interesting picture of the diversity of these sequences across redox conditions and different environments. Although a significant number of partial bssA sequences are available in the literature, only three studies have investigated the bamA gene (9, 10, 14). Here, we combine an investigation into both genes, investigating their diversity across samples types. In addition, we provide data to indicate qPCR targeted to these genes correlated well with toluene biodegradation. These results indicate the qPCR assay has the potential for providing evidence of toluene degradation potential at contaminated sites. The study illustrated the difficulty associated with amplifying the bssA gene in sulfate amended and methanogenic toluene degrading microcosms. As stated above, we previously obtained four partial bssA sequences from nitrate and sulfate amended samples. In the current study, we expand on this and identified four additional bssA gene sequences. These sequences were obtained from two nitrate amended microcosms, one constructed from agricultural soil (BoN1) and the other from digester sludge (DSN). In addition, two partial sequences were obtained from methanogenic microcosms, one concentrated from agricultural soil (HaM) and the other from a contaminated site (SM). The agricultural soil (BoN1) under nitrate amended conditions contained two different partial bssA sequences with one being similar to Thauera sp. DNT-1 (87%). Interestingly, the other illustrated a high degree of similarity (83% identity) to bssA clones obtained from a study involving sulfate reducing toluene degradation from a tar-oil-contaminated aquifer at a former coal gasification plant (19). In the other nitrate amended samples (DSN), only one clone was found and this had the highest similarity to Thauera 94 aromatica (82%), a clone (clone LA07bs16) from the sulfate reducing study (81%) and Aromatoleum aromaticum EbN1 (80%). For the methanogenic microcosms, only one dominant sequence was obtained and these illustrated the greatest similarity to the clones described above from the study on toluene degradation from a tar-oil-contaminated aquifer (85% and 83% for HaM and SM, respectively). Several of these sequences were previously referred to as the “F2”-cluster bssA (19). In contrast to the difficultly in amplifying bssA, amplifying bamA was highly successful in all except one toluene degrading microcosm (methanogenic SM). These results were unexpected, because previous studies (10, 14) modified the primer pair originally proposed in 2008 (9) and used in the current study. As discussed above, only three studies have investigated the bamA gene in relation to aromatic degradation. The first manuscript developed the primer pair bam-sp9 and bam-asp (9) and these primers were modified for use in the two field studies (10, 14). One study investigated the diversity of bamA sequences in microcosms incubated at benzene contaminated aquifers (10). The other involved a landfill leachate contaminated aquifer under iron reducing conditions (14). These two field studies are discussed below, followed by a comparison between the bamA sequences obtained in the current study and those found in the three previous studies. The bamA assays used on DNA from the benzene contaminated sites involve the primers designed previously (9) as well as the development of two additional reverse primers (to produce ~700 and ~800-bp amplicons) to amplify the GMT (Geobacter, Magnetospirillum and Thauera) cluster and the SA (Gram-negative/Gram positive sulfate reducing bacteria and Syntrophus, 95 Azoarcus and Aromatoleum) cluster. The PCR assays were performed on in situ microcosms incubated at two different tar oil and BTEX contaminated anoxic aquifers (called Gneisenau and benzene production plant or BPP). The Gneisenau site had low concentrations of organics and previous work had demonstrated the potential for benzene and toluene degradation (15). The site had elevated concentration of total dissolved iron, indicating Fe (III) to Fe (II) reduction (10). At this site, one bamA clone showed the highest sequence identity to Geobacter metallireducens (88%). Five other clones had the highest similarity to bamA from Geobacter daltonii (85-88%). Interestingly, the authors did not obtain any appropriate amplicons using the SA cluster targeting bamA assay. The BPP site had a high concentration of benzene and the total dissolved iron concentrations indicated Fe (III) reduction. Again the authors used both bamA assays. Using the SA cluster targeting bamA assay, they found 8 clones with highest similarities to bamA genes from species of the genera Azoarcus and Aromatoleum (75-78% identity). Using the GMT cluster targeting bamA assay, they found two sequences similar to bamA sequences from species of the genera Magnetospirillum and Thauera (80% identity). The other field study involved a leachate contaminated aquifer near the Banisveld landfill (the Netherlands) under iron reducing conditions (14). In this case, both the bamA and bssA genes were investigated. This field study produced the most extensive collection of bamA sequences to date. The sequences obtained were placed into seven clades: bamA-clade 1, bamA-clade 2, bamA-clade 3, Thauera/Magnetospirillum-clade, Geobacter-clade, Syntrophus-clade and a Georgfuchsia/Azoarcus clade (9). The work involved analysis of groundwater samples along the pollution plume in 1999 and 2004, which enabled the researchers to correlate site conditions e.g. ferrous iron concentrations and dissolved organic matter, with sequence diversity. The 96 researchers used qPCR to obtain a ratio of functional genes to bacterial 16S rRNA genes. On average, 1.8 bssA copies and 33.7 bamA copies were present per 10,000 16S rRNA copies in polluted samples in 2004. They found that species containing bssA sequences closely affiliated with Georgfuchsia toluolica. In contrast, bamA genes closely related to Geobacteraceae were dominant and only <2% of bamA genes were related to Georgfuchsia. From 64 partial bssA sequence variants, 57 bssA sequences clustered to the bssA gene of Georgfuchsia toluolica G5G6. A minor number of other bssA sequences affiliated with Geobacter spp., Magnetospirillum sp. TS-6 and Aromatoleum aromaticum sp. EbN1. In contrast, samples from 1999 illustrated a high occurrence of Aromatoleum related bssA sequences which coincided with denitrification being a dominant redox process. The 188 partial bamA sequence variants showed a high gene diversity and these sequences were placed into seven clades. A small fraction (1.5%) strongly grouped with sequences from Georgfuchsia toluolica sp. G5G6, Azoarcus sp. and Aromatoleum aromaticum sp. EbN1. A larger percentage (43.2%) contained sequences highly related to Geobacter spp., and these were referred to as the ‘Geobacter-clade’. A number of sequences (13.4%) showed similarity to Syntrophus aciditrophicus sp. SB and were called the ‘Syntrophus-clade’. A small number of sequences (5 of 188) were placed with the ‘Thauera/Magnetospirillum-clade’. Two clades (bamA-clade 1 and 2) did not contained reference genes from isolates and one clade (bamA-clade 3) had low similarity to Azoarcus and Syntrophus aciditrophicus sp. SB. The bamA sequences obtained in the current study affiliated with five of these seven clades described above. The bamA sequences from the nitrate amended samples were placed within three clades (bamA-clade 1, Georgfuchsia/Azoarcus and Magnetospirillum/Thauera clades). In 97 contrast, the bamA sequences obtained from the sulfate amended microcosms were placed within two different clades (Syntrophus and Geobacter clades). The bamA sequences from the methanogenic microcosms were all placed within the Syntrophus clade. The details for each are described below. In the nitrate amended agricultural soil microcosms, two different bamA sequences were obtained. Three sequences has the greatest similarity to bamA clone 0c_1999(1C) from the landfill study (97% identity) and the bamA sequence from Azoarcus toluvorans strain Td21 (97% identity). These three sequences could be placed in the Georgfuchsia/Azoarcus clade. The other sequence type had the greatest similarity to landfill clone -200b_2004(1B) (92% identity) and could be placed inside the bamA-clade 1. This was the only sequence obtained in the current study to be placed in this clade. This clade does not contain reference genes from isolates (9). The other nitrate amended microcosms (inoculated with digester sludge) contained a different set of bamA genes. This time, the sequences were most similar to Magnetospirillum magneticum (92% identity) and could be placed with the Magnetospirillum/Thauera clade. The placement of the bamA sequences from nitrate amended samples within clades containing known nitrate reducing toluene degrading species (Azoarcus, Georgfuchsia, Magnetospirillum and Thauera) suggests the bamA gene is highly conserved. Interestingly, one sequence was placed in a clade with no reference genes from isolates, indicating gene diversity under nitrate reducing conditions cannot be not completely accounted for by known isolates. The bamA sequences obtained from the sulfate amended samples were placed into two clades. All clones from the digester sludge inoculated microcosms were placed into the Syntrophus clade 98 and had the greatest similarity to the landfill leachate plume clones (89% identity). In contrast, the bamA clone from microcosm inoculated with the contaminated site sediment was placed with the Geobacter clade and had the greatest similarity (84% identity) to bamA clones from the Gneisenau site (10). This site is located near a former coking plant and contained iron and sulfate as potential electron acceptors. All of the sequences obtained from the methanogenic samples could be placed within the Syntrophus clade. The bamA clones from the methanogenic activated sludge samples had to highest similarity to the bamA sequence from the obligately anaerobic bacteria Syntrophus aciditrophicus (87% identity) and to bamA sequences from the landfill leachate plume (9). The bamA sequences from the agricultural soil under methanogenic conditions were also most similar to Syntrophus aciditrophicus (84% identity) and the landfill leachate plumes. Again, these data indicate bamA sequence diversity to be strongly correlated with electron accepting conditions. In the current study, bssA and bamA gene numbers were obtained for a select number of microcosms during toluene degradation. The only other published data quantifying these genes together exists in the landfill leachate study (14). In that case, the authors reported on average 1.8 bssA copies and 33.7 bamA copies were present per 10,000 16S rRNA copies in polluted samples in 2004. Although the current study did not quantify 16S rRNA gene numbers, a ratio of bamA/bssA can be calculated to compare the new data to the field data described above. In the nitrate amended microcosms, the bamA/bssA ratios are ~0.06, 1 and 0.25 for AgN, BoN1 and GSN, respectively. These ratios are much lower than those described above. In the sulfate amended sample (DUKE), the rate is ~11 and in the methanogenic microcosms the ratios are ~2.7 (HaM) and ~1.6. It is not clear why the ratios are lower in the laboratory studies. It is 99 possible that the presence of a diverse range of contaminants at the field site favors bamA, whereas microcosms exposed to toluene only favors bssA. In summary, this work provides the first in-depth study of the diversity of bamA gene sequences across redox conditions and in microcosms constructed from different inoculum sources. Since 2008, to our knowledge, only three studies have investigated the bamA gene in anaerobic aromatic degrading cultures (9, 10, 14). The research also examined the presence and diversity of the bssA gene and documented the utility of a range of primers for bssA detection. Further, qPCR was targeted to these two functional genes and the results provided evidence that toluene degradation can be correlated with bamA and bssA gene numbers. Therefore, the qPCR assays have the potential for use at field sites to document toluene degradation. 100 Tables and figures Table 4.1. Success of bssA and bamA primers, amplicons cloned and the consortia targeted for qPCR. Consorti Inoculum Likely 7772f/ SRBf/ bss1500f/ Bamr/ qPCR a Source TEA 8546r(20) SRBr(3) bss2100r(13) Bamf(9) ++ AgN Ag soil Nitrate yes +* ++* X ++ X GSN Granular Nitrate yes -* ++* X sludge ASN Activated Nitrate ++ ++ no sludge BoN1 Ag soil Nitrate ++ X ++ ++ X yes BoN2 Ag soil Nitrate ++ ++ ++ no DSN Digester Nitrate ++ X ++ ++ no sludge DSS Digester Sulfate ++ ++ X no +* ++* X sludge # ++ X DUKE Contamin Sulfate ++* X yes +* ated soil ++ no AgS Ag soil Sulfate ++* +* BoS1 Ag soil Sulfate ++ no StS Digester Sulfate + ++ ++ ++ no sludge + + ++ X SM Contamin + no CO2 ated soil ++ X HaM Ag soil + ++ X yes CO2 ++ + ++ X ASM Activated yes CO2 sludge ++ no DSM Digester CO2 sludge KRM Ag soil + + ++ no CO 2 ++ strong specific amplicon + unspecific amplicon(s) - no amplicon X – amplicons sequenced # - the primer set 7772f/8828r (20) was used to target bssA for qPCR * Previous study in our group(16) 101 10 bssA bamA Log numbers of gene copies 9 8 7 6 5 4 3 2 1 0 33% 75% 100% Toluene removed (%) Figure 4. 1. Gene numbers of bssA and bamA during toluene degradation in nitrate amended microcosms AgN. The error bars represent standard deviations form triplicate qPCR samples. 102 9 bssA bamA Log numbers of gene copies 8 7 6 5 4 3 2 1 0 33% 75% 100% Toluene removed (%) Figure 4.2. Gene numbers of bssA and bamA during toluene degradation in nitrate amended microcosms BoN1. The error bars represent standard deviations form triplicate qPCR samples. 103 9 bssA bamA Log numbers of gene copies 8 7 6 5 4 3 2 1 0 50% 100% Toluene removed (%) Figure 4.3. Gene numbers of bssA and bamA during toluene degradation in nitrate amended microcosms GSN. The error bars represent standard deviations form triplicate qPCR samples. 104 9 bssA bamA Log numbers of gene copies 8 7 6 5 4 3 2 1 0 50% 100% Toluene removed (%) Figure 4.4. Gene numbers of bssA and bamA during toluene degradation in a sulfate amended microcosm, DUKE.The error bars represent standard deviations form triplicate qPCR samples. 105 Log numbers of gene copies 8 bssA 7 bamA 6 5 4 3 2 1 0 50% 100% Toluene removed (%) Figure 4.5. Gene numbers of bssA and bamA during toluene degradation in a methaongeic microcosm, ASM. The error bars represent standard deviations form triplicate qPCR samples. 106 8 bssA bamA Log numbers of gene copies 7 6 5 4 3 2 1 0 50% 100% Toluene removed (%) Figure 4.6. Gene numbers of bssA and bamA during toluene degradation in a methaongeic microcosm, HM. The error bars represent standard deviations form triplicate qPCR samples. 107 REFERENCES 108 References 1. Achong, G. R., A. M. Rodriguez, and A. M. Spormann. 2001. Benzylsuccinate synthase of Azoarcus sp strain T: Cloning, sequencing, transcriptional organization, and its role in anaerobic toluene and m-xylene mineralization. Journal of Bacteriology 183:6763-6770. 2. Beller, H. R., S. R. Kane, T. C. Legler, and P. J. J. Alvarez. 2002. A real-time polymerase chain reaction method for monitoring anaerobic, hydrotarbon-degrading bacteria based on a catabolic gene. Environmental Science & Technology 36:3977-3984. 3. Beller, H. R., S. R. Kane, T. C. Legler, J. R. McKelvie, B. S. Lollar, F. Pearson, L. Balser, and D. M. MacKay. 2008. Comparative assessments of benzene, toluene, and xylene natural attenuation by quantitative polymerase chain reaction analysis of a catabolic gene, signature metabolites, and compound-specific isotope analysis. Environmental Science & Technology 42:6065-6072. 4. Botton, S., M. van Harmelen, M. Braster, J. R. Parsons, and W. F. M. Roling. 2007. Dominance of Geobacteraceae in BTX-degrading enrichments from an iron-reducing aquifer. Fems Microbiology Ecology 62:118-130. 5. Gibson, J., and C. S. Harwood. 2002. Metabolic diversity in aromatic compound utilization by anaerobic microbes. Annual Review of Microbiology 56:345-369. 6. Jin, S., P. H. Fallgren, A. A. Bilgin, J. M. Morris, and P. W. Barnes. 2007. Bioremediation of benzene, ethylbenzene, and xylenes in groundwater under iron-amended, sulfate-reducing conditions. Environmental Toxicology and Chemistry 26:249-253. 7. Kane, S. R., H. R. Beller, T. C. Legler, and R. T. Anderson. 2002. Biochemical and genetic evidence of benzylsuccinate synthase in toluene-degrading, ferric iron-reducing Geobacter metallireducens. Biodegradation 13:149-154. 8. Kuhner, S., L. Wohlbrand, I. Fritz, W. Wruck, C. Hultschig, P. Hufnagel, M. Kube, R. Reinhardt, and R. Rabus. 2005. Substrate-dependent regulation of anaerobic degradation pathways for toluene and ethylbenzene in a denitrifying bacterium, strain EbN1. Journal of Bacteriology 187:1493-1503. 9. Kuntze, K., Y. Shinoda, H. Moutakki, M. J. McInerney, C. Vogt, H. H. Richnow, and M. Boll. 2008. 6-Oxocyclohex-1-ene-1-carbonyl-coenzyme A hydrolases from obligately anaerobic bacteria: characterization and identification of its gene as a functional marker for aromatic compounds degrading anaerobes. Environmental Microbiology 10:1547-1556. 10. Kuntze, K., C. Vogt, H. H. Richnow, and M. Boll. 2011. Combined application of PCR-based functional assays for the detection of aromatic-compound-degrading anaerobes. Applied and Environmental Microbiology 77:5056-5061. 11. Laempe, D., M. Jahn, and G. Fuchs. 1999. 6-hydroxycyclohex-1-ene-1-carbonyl-CoA dehydrogenase and 6-oxocycsohex-1-ene-1-carbonyl-CoA hydrolase, enzymes of the 109 benzoyl-CoA pathway of anaerobic aromatic metabolism in the denitrifying bacterium Thauera aromatica. European Journal of Biochemistry 263:420-429. 12. Lopez Barragan, M. J., E. Diaz, J. L. Garcia, and M. Carmona. 2004. Genetic clues on the evolution of anaerobic catabolism of aromatic compounds. Microbiology-Sgm 150:2018-2021. 13. Moore, E. 2009. Developing protocols to facilitate the enrichment and characterization of hydrocarbon-degrading anaerobic microbial communities. Department of Chemical Engineering and Applied Chemistry, MS Thesis, University of Toronto. 14. Staats, M., M. Braster, and W. F. M. Roling. 2011. Molecular diversity and distribution of aromatic hydrocarbon-degrading anaerobes across a landfill leachate plume. Environmental Microbiology 13:1216-1227. 15. Stelzer, N., C. Buning, F. Pfeifer, A. B. Dohrmann, C. C. Tebbe, I. Nijenhuis, M. Kastner, and H. H. Richnow. 2006. In situ microcosms to evaluate natural attenuation potentials in contaminated aquifers. Organic Geochemistry 37:1394-1410. 16. Sun, W., and A. M. Cupples. Diversity of five anaerobic toluene degrading microbial communities investigated using stable isotope probing (SIP). Submitted. 17. Washer, C. E., and E. A. Edwards. 2007. Identification and expression of benzylsuccinate synthase genes in a toluene-degrading methanogenic consortium. Applied and Environmental Microbiology 73:1367-1369. 18. Winderl, C., B. Anneser, C. Griebler, R. U. Meckenstock, and T. Lueders. 2008. Depth-resolved quantification of anaerobic toluene degraders and aquifer microbial community patterns in distinct redox zones of a tar oil contaminant plume. Applied and Environmental Microbiology 74:792-801. 19. Winderl, C., H. Penning, F. von Netzer, R. U. Meckenstock, and T. Lueders. 2010. DNA-SIP identifies sulfate-reducing Clostridia as important toluene degraders in tar-oil-contaminated aquifer sediment. Isme Journal 4:1314-1325. 20. Winderl, C., S. Schaefer, and T. Lueders. 2007. Detection of anaerobic toluene and hydrocarbon degraders in contaminated aquifers using benzylsuccinate synthase (bssA) genes as a functional marker. Environmental Microbiology 9:1035-1046. 21. Yang, Y. R., and J. Zeyer. 2003. Specific detection of Dehalococcoides species by fluorescence in situ hybridization with 16S rRNA-targeted oligonucleotide probes. Applied and Environmental Microbiology 69:2879-2883. 110 CHPATER 5 ANAEROBIC MTBE DEGRADING MICROORGANISMS IDENTIFIED IN WASTEWATER TREATMENT PLANT SAMPLES USING STABLE ISOTOPE PROBING Introduction Methyl tert-butyl ether (MTBE) is a synthetic organic compound that was added to gasoline in the late 1970s, following the phase out of tetraethyl lead. Later, the implementation of the Clean Air Act Amendments (1990) caused a significant increase in MTBE use. In 1970, MTBE was the 39th highest produced US organic chemical whereas by 1998 it ranked 4th. During this time the aggregate production of MTBE was 60 million metric tons (11). The large scale use, combined with MTBE’s physiochemical properties, has resulted in severe contamination. MTBE has a high -1 water solubility (51 g L ), strongly partitions to water from air (dimensionless Henry’s Law constant 0.02) (14), has a low sorption partition coefficient (Koc is 1.035-1.091(15)) and, thus, is highly mobile in water (51). MTBE contamination has been reported in surface waters (3, 4, 9, 11, 15, 26, 46), groundwater (11, 15, 28, 29, 34, 38, 40, 53, 59, 64), and drinking water sources (1, 6, 11, 20, 35, 42, 48, 52, 56). MTBE contamination in drinking water has been reported in 36 states, with removal estimates being $25-33.2 billion (5). Biological degradation is becoming increasing common as a remediation method for groundwater contaminants, either through natural attenuation or enhanced bioremediation. There have been numerous studies on aerobic MTBE biodegradation (32, 45, 57, 58) and microorganisms capable of degrading MTBE under aerobic conditions have been isolated (16, 39, 111 47, 49). Anaerobic MTBE biodegradation has also been documented (10, 21-23, 36, 41, 43, 54), however, much less is known about the microorganisms involved and, to date, no MTBE degrading isolates have been obtained. This knowledge gap is a significant limitation to in situ MTBE bioremediation because many contaminated sites are anaerobic. More information on the microorganisms capable of anaerobic MTBE degradation could result in the application of molecular methods to investigate their presence and abundance, and therefore the potential for MTBE degradation at different sites. The microbial composition of anaerobic MTBE degrading enrichment cultures has only recently been investigated. In 2009, the microbial communities of three anaerobic MTBE degrading cultures derived from MTBE-contaminated aquifer material were examined using 16S rDNA based amplified ribosomal DNA restriction analysis (ARDRA) and 16S rRNA gene sequencing (17). The cultures were maintained with anthroquinone-2,6-disufonate (AQDS), sulfate or fumarate as electron acceptors and the authors found that the microbial diversity varied under these different conditions. In another recent study, other researchers characterized the community composition of anaerobic enrichment cultures originating from three different contaminated sediments (63). Interestingly, terminal restriction fragment length polymorphism (TRFLP) profiles indicated substantially different community profiles from MTBE degrading microcosms established from different sediment sources. A third group investigated the microbial community present (16S rRNA gene sequencing) when MTBE degradation occurred under sulfate or iron reducing conditions or when both electron acceptors were present together and identified five to eight microorganisms in the three consortia (43). 112 The current study expands on these investigations by applying DNA based stable isotope probing (SIP) to determine which organisms are responsible for 13 C label uptake from MTBE in anaerobic MTBE degrading microcosms under methanogenic conditions. The SIP method is unique in that it can directly identify the microorganisms responsible for contaminant degradation and therefore offers more targeted information than community analysis alone (e.g. TRFLP, ADARA, 16S rRNA clone libraries). To date, SIP has yet to be used to investigate MTBE degradation in anaerobic MTBE degrading microcosms. The SIP method involves exposure of mixed cultures to the labeled compounds of interest (e.g., 13 C MTBE) and DNA extraction over time. The DNA is then subject to ultracentrifugation, fractionation (to separate label incorporated DNA from the unlabeled DNA) and TRFLP on each fraction. Any TRFLP fragment illustrating an increase in relative abundance in the heavy fraction of the samples (exposed to labeled substrate) compared to the controls (exposed to unlabeled substrate) is identified as the putative degrader. The method has been used to identify the microorganisms involved in the degradation of numerous contaminants (2, 13, 27, 30, 31, 37, 55, 60, 61). In the current study, a range of sources (contaminated site sediment, agricultural soils and wastewater treatment samples) were examined for anaerobic MTBE degradation potential. In the active anaerobic MTBE degrading microcosms, SIP targeted to both bacteria and archaea was applied to identify the putative MTBE degrading microorganisms. Methods Microcosm Construction and Analytical Techniques A range of sources were tested for their potential to degrade MTBE (Table 5.1), including 113 agricultural soil, contaminated site soil and wastewater treatment samples. From all samples tested only one source (WWTP sample) demonstrated MTBE degradation and was further investigated. Microcosms were prepared under strictly anaerobic conditions in an anaerobic chamber (Coy Laboratory Products INC, Grass Lake, MI). For each microcosm, ~6g sample (wet weight) was anoxically incubated in 60 mL serum bottles containing 25 mL of anaerobic basal media (62). Each treatment involved triplicate abiotic controls, triplicate unlabeled MTBE 13 (1 μL, 99 %, Sigma Aldrich, St. Louis, MO) and three triplicate labeled MTBE ( C5-MTBE 1 μL Sigma Aldrich, St. Louis, MO) amended samples. These microcosms were incubated at room temperature (~20 °C) with reciprocal shaking. MTBE concentrations in headspace gas samples (200 μL) were determined with a gas chromatograph (Perkin Elmer) equipped with flame ionization detector and a capillary column (J&W Scientific, DB-624, diameter 0.53mm). Injector and detector temperature were set at 200 oC and the column temperature was 120oC. DNA Extraction and Ultracentrifugation Microcosms were sacrificed for DNA extraction at two time points (~30% and ~70% MTBE removal) during MTBE depletion to understand the flow of carbon through these microbial communities. The powersoil DNA extraction kit (MO BIO Laboratories, Inc. Carlsbad, CA) was used for total nucleic acids extraction according to the manufacturer’s recommended procedure. Quantified DNA extracts (~10 μg) were loaded into Quick-Seal polyallomer tubes (13×51 mm, 5.1 ml, Beckman Coulter) along with a Tris-EDTA (TE, pH 8.0) /CsCl solution. Prior to sealing (cordless quick-seal tube topper, Beckman), the buoyant density (BD) was determined with a model AR200 digital refractometer (Leica Microsystems Inc) and adjusted by adding small 114 -1 volumes of CsCl solution or Tris-EDTA buffer with a final BD of 1.7300 mgL . The tubes were centrifuged at 178,000 g (20 ºC) for 48 h in a Stepsaver 70 V6 Vertical Titanium Rotor (8 x 5.1 ml capacity) within a Sorvall WX 80 Ultra Series Centrifuge (Thermo Scientific). Following centrifugation, the tubes was placed onto a fraction recovery system (Beckman) and fractions (150 l) were collected. The BD of each fraction was measured, and CsCl was removed by glycogen-assisted ethanol precipitation. PCR, TRFLP and Sequencing of 16S rRNA Genes The density-resolved fractions from 12 C and 13 C microcosms for each treatment were PCR-amplified using 27F-FAM (5’-AGAGTTTGATCMTGGCTCAG, 5’ end-labeled with carboxyfluorescine) and 1492R (5’-GGTTACCTTGTTACGACTT) for generating bacterial amplicons and A109F—FAM (5’- ACKGCTCAGTAACACGT) and A934R (5’- GTGCTCCCCCGCCAATTCCT ) for archaeal amplicons (Operon Biotechnologies). The presence of PCR products was confirmed by 1.5% agarose gel electrophoresis and the subsequent staining of the gels with ethidium bromide. PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.), following the manufacturer’s instructions and approximately 150 ng was digested with HaeIII (New England Biolabs) with a 6-hour incubation period. Additional digests (HhaI, MseI, Bsp1286I, BsrBI etc.) for TRFLP analyses in a number of heavy labeled fractions were included to correlate the TRFLP fragment lengths to the in silico cut sites of the cloned 16S rRNA gene sequences. DNA fragments were separated by capillary electrophoresis (ABI Prism 3100 Genetic Analyzer, Applied Biosystems) at the Research Technology Support Facility (RTSF) at Michigan State University. Data were analyzed with 115 GeneScan software (Applied Biosystems) and the percent abundance of each fragment was determined. Clone libraries of the 16S rRNA genes were constructed using DNA amplified with 27F/1492R , A109F/A934R as above except the forward primer was unlabeled and the final extension time was extended to 15 minutes. To reduce sequencing redundancy, restriction fragment length polymorphism (RFLP) analyses was performed and specific operational taxonomic units (OTU) were selected for sequencing. The PCR products were purified with QIAquick PCR purification kit (Qiagen Inc.) and cloned into Escherichia coli TOP10 vector supplied with a TOPO TA cloning kit (Invitrogen Corporation). E. coli clones were grown on -1 -1 Luria-Bertani (LB) medium solidified with 15 g agar L with 50 g ampicillin L for 16 h at 37 ºC. Colonies with inserts were verified by PCR with primers M13 F (5’-TGTAAAACGACGGCCAGT-3’) and M13 R (5’-AACAGCTATGACCATG-3’), plasmids were extracted from the positive clones with a QIAprep miniprep system (Qiagen, Inc.) and the insertions were sequenced at RTSF. The Ribosomal Database Project (RDP) (Center for Microbial Ecology, Michigan State University) analysis tool “classifier” was utilized to assign taxonomic identity. Results and Discussion From twenty-two experimental set-ups, anaerobic MTBE biodegradation was noted in microcosms constructed from only one source and only under methanogenic conditions (Table 5.1). Microcosms for the SIP experiment were constructed using freshly sampled material from the wastewater treatment plant (WWTP). MTBE degradation occurred in both labeled MTBE amended and unlabeled MTBE amended samples, but not in the abiotic controls (Figure 5.1). At 116 two time points during the time period for MTBE biodegradation (~30% and 70% removal), DNA was extracted from the labeled and unlabeled MTBE-amended microcosms, and was subject to ultracentrifugation, fractionation and TRFLP. Bacterial microbial communities were profiled by TRFLP when 30% and 70% MTBE was degraded, whereas archaeal communities were only profiled when 70% was degraded. Assimilation of 13C labeled MTBE was detected by comparing TRFLP profiles of DNA derived from labeled treatments with DNA from unlabeled treatments. Specifically, the organisms responsible for 13 C assimilation were identified by the comparison of relative abundances of specific terminal restriction fragments (T-RFs) between the labeled and unlabeled gradient-fractions. Labeled bacterial DNA was successfully amplified in the fractions with buoyant density (BD) values of 1.7154 to 1.7719 g ml -1 (~70% degraded) and 1.7306 to 1.7653 g ml -1 (~30% -1 degraded). PCR products were seen in the fractions with BDs of 1.7024 to 1.7589 g ml in the unlabeled treatment (~70% degraded). Two bacterial T-RFs (67 bp and 215 bp) were highly enriched in the heavy 13 C fractions while such enrichment was not seen in the corresponding fractions with similar buoyant density (Figure 5.2A and B). A high (>30%) relative abundance (RA) of both T-RFs was noted in the heavier fractions and their RA increased over time, as MTBE was degraded (30% and 70% MTBE degraded). The RA of 215 bp T-RF was > 20% -1 among the heavy fractions (banding between 1.7545 to 1.7719 g ml ) with the maximum RA (46.6%) in the fraction with BD of 1.7676 g ml -1 (~70 % degraded) (Figure 5.2A). The RA of the 67 bp T-RF was generally > 30% in labeled heavy fractions (banding between 1.7480 to 117 -1 1.7719 g ml ) under both time points with the maximum RA (48.4%) in the fraction with BD of 1.7643 g ml -1 (~70% degraded) (Figure 5.2B). An analysis of the archaeal SIP TRFLP profiles (from ~70% MTBE degraded) indicated two T-RFs (132 bp and 162 bp) were relatively more dominant in the labeled fractions compared to the controls (Figure 5.3 A and B). Clone libraries for both bacteria (Table 5.2) and archaea (Table 5.3) were generated to investigate the diversity of the MTBE degrading microcosms and to identity the putative MTBE degraders represented by the T-RFs discussed above. The most dominant bacterial phylum was the Proteobacteria (59 from 122 clones or 48.4%), which contained Alphaproteobacteria (22/59), Betaproteobacteria (21/59), Gammaproteobacteria (10/59) and Deltaproteobacteria (6/59). The second most dominant phylum was the Firmicutes (29/122 or 23.8%), which primarily consisted of Clostridia (26/29). Other minor phyla included Verrucomicrobia (9/122), Nitrospira (6/122), Bacteroidetes (5/122), OP10 (5/122), Lentisphaerae (4/122), Tenericutes (3/122) and Acidobacteria (1/122). The genera of each clone determined from the RDP are also shown, with a significant number (13/26) from being unclassified to the genus level (Table 5.2). The archaeal community was less diverse with only 7 different phylotypes (Table 5.3), all within the class Methanomicrobia (phylum Euryarchaeota). Two phylotypes could not be classified at the genus level. The bacterial and archaeal sequences were digested in silico to identify the T-RFs enriched in the heavy fractions as discussed above. The two bacterial T-RFs dominant in the heavy fractions were identified as Clostridia (215 bp) and Alphaproteobacteria (67 bp). The Clostridia-related phylotype could be classified to the family level (Ruminococcaceae) and was most similar to an 118 uncultured Acetivibrio spp. (95% 16S rRNA gene sequence similarity: GenBank accession number EF613411.1). The Alphaproteobacteria-related clone classified to the genus Sphingopyxix and was most similar to an uncultured bacterium clone reservoir-30 (99% of 16S rRNA gene sequence similarity: GenBank accession number JF697411.1). The archaeal 132 bp and 162 bp T-RFs belonged to the genera Methanosarcina and Methanocorpusculum, respectively. The putative identifies of the bacterial T-RFs were confirmed with additional digests on the heavy fractions (Table 5.4). The SIP data indicate the primary MTBE degraders in the methanogenic enrichment are bacteria and belong to the phyla Clostridia (family Ruminococcaceae) and Alphaproteobacteria (genus Sphingopyxis). As the label enrichment level was low in the archaeal phylotypes in the heavy fractions, it is unlikely that these organisms (genera Methanosarcina and Methanocorpusculum) are the dominant degraders. It is possible that the identified archaeal phylotypes are responsible for minor amounts of MTBE degradation or they are consuming metabolites produced by the primary bacterial degraders. Interestingly, other researchers have identified Clostrida as dominant organisms in their anaerobic MTBE degrading enrichments. Specifically, from the three enrichments (AQDS, sulfate or fumarate reducing) developed from MTBE contaminated aquifer material, the sulfate reducing enrichment contained 19.3% assigned to the order Clostridiales and the fumarate reducing enrichment contained a dominant clone (related to Clostridium sp. Kw12) (22.8%) also belonging to the phylum Firmicutes (17). Similarly, following continual enrichment of an anaerobic MTBE degrading consortium, researchers reduced the community to three dominant phylotypes belonging to Deltaproteobacteria, Chloroflexi and Firmicutes (63). In addition, Clostridia were found in anaerobic MTBE 119 degrading consortia under sulfate and iron reducing conditions (44). These previous studies, combined with the data in the current study indicate organisms in the phylum Firmicutes are important for the anaerobic degradation of MTBE. Microorganisms associated with the family of Ruminococcaceae within the phylum Firmicutes are predominant members of mammalian gut microbial flora. The presence of these organisms in the enrichments is therefore not surprising given the source of the inocula (WWTP sample). Members of Ruminococcaceae isolated from human gut were correlated with biodegradation of complex polysaccharides such as starch or xylan (19). Ruminococcaceae isolated from rumen or human guts were proven to be able to degrade cellulose (7, 8, 18). Chassard et al. reported Ruminococcaceae were responsible for cellulose biodegradation in the fecal samples of methane-excreting subjects while the main cellulose-degrading bacteria belong essentially to Bacteroidetes in non-methane-excreting subjects (7), indicating a possible link between methane production and Ruminococcaceae-associated cellulose biodegradation. This observation is consistent with the current study in that no MTBE biodegradation under the sulfate- and nitrateamended conditions (no methane was produced) although they were seeded from the same inocula. Ruminococcaceae were also linked with 2,4,6-trinitrotoluene (TNT) degradation in a recent study (12). The most similar isolate to the putative MTBE degrader (family Ruminococcaceae) identified in the current study is uncultured Acetivibrio sp. clone ZZ-S2G3 (95% 16S rRNA similarity; Genbank accession number EF613411.1) which was found in a sulfate reducing benzene-degrading microbial community but was not correlated with benzene biodegradation (33). 120 In contrast to the putative MTBE degrader (Firmicutes phylotype, TR-F 215 bp) discussed above, the other putative MTBE degrader (phylum Alphaproteobacteria, genus Sphingopyxis TR-F 67 bp), has no obvious previous links to anaerobic MTBE biodegradation. The 67-bp T-RF showed a high level of 16S rRNA similarity (98%) to an uncultured Alphaproteobacteria bacterium (GeneBank CU926829.1) detected in anaerobic digestion of sludge (50). The data obtained from the current study indicate this phylotype may be a novel anaerobic MTBE degrader and should be further investigated. The presence of two enriched T-RFs suggests more than one microorganism may be responsible for MTBE biodegradation. Youngster et al. (24) suggested that anaerobic MTBE biodegradation required the interaction of a consortium. The exact mechanism of MTBE anaerobic biodegradation in the current study has yet to be elucidated. Others have reported tert-butyl alcohol (TBA) as a MTBE degradation metabolite (22, 25, 49), indicating the cleavage of ether bond is the initial step of MTBE biodegradation. Interestingly, the –C–O–C– bond found in MTBE also occurs in cellulose, therefore one might hypothesize that Ruminococcaceae which can degrade cellulose may be responsible for the initial step of MTBE biodegradation. 121 Tables and figures Table 5. 1. The sources and conditions investigated for anaerobic MTBE degradation potential. Inoculum type Electron acceptor sulfate Degr Comment Contaminated soil 1 Incubation time 1 year No Contaminated soil 1 Contaminated soil 2 1 year 1 year nitrate sulfate No No Contaminated soil 2 Agricultural soil 1 Agricultural soil 1 Agricultural soil 1 Agricultural soil 2 1 year 1 year 1 year 1 year 1 year nitrate sulfate nitrate carbon dioxide sulfate No No No No No Agricultural soil 2 Agricultural soil 2 Agricultural soil 2 Agricultural soil 3 Agricultural soil 3 Agricultural soil 3 Granular sludge Granular sludge Granular sludge Activated sludge 1 year 1 year 1 year 1 year 1 year 1 year 1 year 1 year 1 year 1 year nitrate carbon dioxide sulfate sulfate nitrate carbon dioxide sulfate nitrate carbon dioxide sulfate No No No No No No No No No No Activated sludge Activated sludge 1 year 2 months nitrate carbon dioxide No Yes Digester sludge Digester sludge Digester sludge 1 year 1 year 1 year sulfate nitrate carbon dioxide No No No Samples obtained from a previously MTBE contaminated LUST site Same soil as above Samples obtained from a previously MTBE contaminated LUST site Same soil as above Samples obtained from a farm located at Michigan, Same soil as above Same soil as above Samples obtained from a farm located at Michigan, the crop is soybean Same soil as above Same soil as above Same soil as above Samples obtained from a farm located at Michigan, the crop is corn Same soil as above Same soil as above Samples obtained from a UASB reactor in Washington Same sludge as above Same sludge as above Samples obtained from East Lansing WWTP. The sludge was taken from the aeration tank of the WWTP. Same sludge as above Same sludge as above,~90% MTBE removal, Significant methane production Samples obtained from St.Clair WWTP. Same sludge as above Same sludge as above 122 Table 5.2. Phylogenetic affiliation of bacterial 16S rRNA clone in methanogenic MTBE degrading microcosms as determined with the RDP analysis tool “classifier” Number Soil/Fragment Enriched in of Phylum Class Order Genus (Hae III heavy digestion) fractions clones 39 bp N 2 Bacteroidetes Bacteroidia Bacteroidales unclassified 39 bp N 6 Proteobacteria Gammaproteobacteria Xanthomonadales Dokdonella 39 bp N 3 Proteobacteria Alphaproteobacteria unclassified 39bp,76 bp N 3 Proteobacteria Deltaproteobacteria Myxococcales Kofleria 75,251 3 N Bacteroidetes Sphingobacteria Sphingobacteriales Haliscomenobacter 71bp,227 bp Y 18 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingopyxis 190 bp N 1 Proteobacteria Alphaproteobacteria unclassified 198 bp 3 N Proteobacteria Betaproteobacteria unclassified 200 bp N 4 Proteobacteria Gammaproteobacteria Xanthomonadales Aquimonas 212bp 3 N Firmicutes Clostridia Clostridiales 217 bp 16 N Proteobacteria Betaproteobacteria Burkholderiales Simplicispira 217 bp,224 bp,266 bp,349bp Y 12 Firmicutes Clostridia Clostridiales unclassified 219 bp 2 N Proteobacteria Betaproteobacteria Burkholderiales Methylibium 221 bp N 3 Tenericutes Mollicutes Acholeplasmatales Acholeplasma 224 bp 4 N Verrucomicrobia Subdivision5 unclassified Subdivision5 231 bp 5 N OP10 unclassified OP10 240 bp,318 bp N 2 Firmicutes Clostridia Clostridiales 248 bp N 4 Lentisphaerae Lentisphaeria Victivallales Victivallis 255 bp N 3 Firmicutes Erysipelotrichi Erysipelotrichales unclassified 264 bp N 6 Nitrospira Nitrospira Nitrospirales Nitrospira 265 bp N 3 Proteobacteria Deltaproteobacteria Myxococcales unclassified 268 bp N 1 Acidobacteria Acidobacteria_Gp3 unclassified Gp3 290 bp N 5 Firmicutes Clostridia Clostridiales Sporacetigenium 293bp 1 N Proteobacteria unclassified 123 Table 5.3. Phylogenetic affiliation of Archaeal 16S rRNA clone in methanogenic MTBE degrading microcosms as determined with the RDP analysis tool “classifier” Soil/Fragment(Hae III digestion) 135 bp 138 bp 135 bp 400 bp 162 bp 28 bp,135 bp 150 bp Enriched in 13 C heavy fractions N Y Y N Y N N Number of Phylum Class clones 4 12 15 3 18 11 9 Euryarchaeota Euryarchaeota Euryarchaeota Euryarchaeota Euryarchaeota Euryarchaeota Euryarchaeota Methanomicrobia Methanomicrobia Methanomicrobia Methanomicrobia Methanomicrobia Methanomicrobia Methanomicrobia 124 Order Methanomicrobiales Methanosarcinales Methanomicrobiales Genus Methanosarcina Methanoculleus Methanomicrobiales Methanocorpusculum Methanomicrobiales Methanospirillum Methanosarcinales Methanosaeta Table 5.4. Comparison of fragment length of dominant T-RF in heavy fractions to predicted fragment length from in silico sequence analyses Microorganism Restriction enzyme TRFLP Sequence data Ruminococcaceae HaeIII 215 217 MspI 199 204 MSEI 588 583 RsaI 453 450 Microorganism Restriction enzyme TRFLP Sequence data Sphingomonadaceae HaeIII 67 71 MspI 147 150 MSEI 418 422 RsaI 507 506 125 MTBE concentration (mg/L) 30 20 10 0 -5.00 5.00 15.00 Time (days) 25.00 35.00 12 Figure 5.1. MTBE concentration over time in C-MTBE amended abiotic controls (♦), 13 12 C-MTBE (■) and C-MTBE (□) amended samples. The arrows indicate when DNA was extracted. The error bars represent standard deviations from triplicate microcosms. 126 TRFLP Relative Abundance (% 60 40 20 0 1.69 1.71 1.73 1.75 1.77 1.79 DNA Buoyant Density (g/mL) Figure 5.2. Percent relative abundance of fragments (digested by Hae III) assigned to Clostridiales within buoyant density gradients of Bacterial DNA extracted from the 13 methanogenic activated sludge microcosms. Figure symbols: ♦ C-MTBE (~30% toluene 13 12 degraded); ■ C-MTBE (~70% toluene degraded); □ C-MTBE (~70% toluene degraded). 127 TRFLP Relative Abundance (% 60 40 20 0 1.69 1.71 1.73 1.75 1.77 1.79 DNA Buoyant Density (g/mL) Figure 5.3. Percent relative abundance of fragments (digested by Hae III) assigned to Sphingomonadales within buoyant density gradients of Bacterial DNA extracted from the 13 methanogenic activated sludge microcosms. Figure symbols: ♦ C-MTBE (~30% toluene 13 12 degraded); ■ C-MTBE (~70% toluene degraded); □ C-MTBE (~70% toluene degraded). 128 TRFLP Relative Abundance (% 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 5.4. Percent relative abundance of fragments (digested by Hae III) assigned to Methanosarcina within buoyant density gradients of Archaeal DNA extracted from the 13 methanogenic activated sludge microcosms. Figure symbols:■ C-MTBE (~70% toluene 12 degraded); □ C-MTBE (~70% toluene degraded). 129 TRFLP Relative Abundance (% 40 20 0 1.69 1.71 1.73 1.75 1.77 DNA Buoyant Density (g/mL) Figure 5.5. Percent relative abundance of fragments (digested by Hae III) assigned to Methanocorpusculum within buoyant density gradients of Archaeal DNA extracted from the 13 methanogenic activated sludge microcosms. Figure symbols:■ C-MTBE (~70% toluene 12 degraded); □ C-MTBE (~70% toluene degraded). 130 REFERENCES 131 References 1. Achten, C., A. Kolb, and W. Puttmann. 2002. Occurrence of methyl tert-butyl ether (MTBE) in riverbank filtered water and drinking water produced by riverbank filtration 2. Environmental Science & Technology 36:3662-3670. 2. Aitken, M. D., D. R. Singleton, R. Sangaiah, A. Gold, and L. M. Ball. 2006. Identification and quantification of uncultivated Proteobacteria associated with pyrene degradation in a bioreactor treating PAH-contaminated soil. Environmental Microbiology 8:1736-1745. 3. An, Y. J., D. H. Kampbell, and M. L. Cook. 2002. Co-occurrence of MTBE and benzene, toluene, ethylbenzene, and xylene compounds at marinas in large reservoir. Journal of Environmental Engineering-Asce 128:902-906. 4. An, Y. J., D. H. Kampbell, and G. W. Sewell. 2002. Water quality at five marinas in Lake Texoma as related to methyl tert-butyl ether (MTBE). Environmental Pollution 118:331-336. 5. AWWA. 2005. American Water Works Association. Two updated MTBE contamination cost analyses pin MTBE clean up costs between $25-$85 billion. http://www.awwa.org/Communications/news/index.cfm?ArticleID=459 (accessed June 2006). 6. Ayotte, J. D., D. M. Argue, and F. J. McGarry. 2005. Methyl tert-butyl ether occurrence and related factors in public and private wells in southeast New Hampshire. Environmental Science & Technology 39:9-16. 7. Bernalier-Donadille, A., C. Chassard, E. Delmas, and C. Robert. 2010. The cellulose-degrading microbial community of the human gut varies according to the presence or absence of methanogens. Fems Microbiology Ecology 74:205-213 . 8. Bernalier-Donadille, A., and C. Robert. 2003. The cellulolytic microflora of the human colon: evidence of microcrystalline cellulose-degrading bacteria in methane-excreting subjects. Fems Microbiology Ecology 46:81-89. 9. Borden, R. C., D. C. Black, and K. V. McBlief. 2002. MTBE and aromatic hydrocarbons in North Carolina stormwater runoff. Environmental Pollution 118:141-152. 10. Bradley, P. M., F. H. Chapelle, and J. E. Landmeyer. 2001. Effect of redox conditions on MTBE biodegradation in surface water sediments. Environmental Science & Technology 35:4643-4647. 11. Carter, J. M., S. J. Grady, G. C. Delzer, B. Koch, and J. S. Zogorski. 2006. 132 Occurrence of MTBE and other gasoline oxygenates in CWS source waters. Journal American Water Works Association 98:91-+. 12. Craig, A. M., S. Perumbakkam, and E. A. Mitchell. 2011. Changes to the rumen bacterial population of sheep with the addition of 2,4,6-trinitrotoluene to their diet. Antonie Van Leeuwenhoek International Journal of General and Molecular Microbiology 99:231-240. 13. Cupples, A. M., and G. K. Sims. 2007. Identification of in situ 2,4-dichlorophenoxyacetic acid-degrading soil microorganisms using DNA-stable isotope probing. Soil Biology & Biochemistry 39:232-238. 14. Davis, L. C., and L. E. Erickson. 2004. A review of bioremediation and natural attenuation of MTBE. Environmental Progress 23:243-252. 15. Deeb, R. A., K. H. Chu, T. Shih, S. Linder, I. Suffet, M. C. Kavanaugh, and L. Alvarez-Cohen. 2003. MTBE and other oxygenates: Environmental sources, analysis, occurrence, and treatment. Environmental Engineering Science 20:433-447. 16. Deeb, R. A., K. M. Scow, and L. Alvarez-Cohen. 2000. Aerobic MTBE biodegradation: an examination of past studies, current challenges and future research directions. Biodegradation 11:171-186. 17. Finneran, K. T., and N. Wei. 2009. Microbial community analyses of three distinct, liquid cultures that degrade methyl tert-butyl ether using anaerobic metabolism. Biodegradation 20:695-707. 18. Flint, H. J., E. A. Bayer, M. T. Rincon, R. Lamed, and B. A. White. 2008. Polysaccharide utilization by gut bacteria: potential for new insights from genomic analysis. Nature Reviews Microbiology 6:121-131. 19. Flint, H. J., E. C. M. Leitch, A. W. Walker, S. H. Duncan, and G. Holtrop. 2007. Selective colonization of insoluble substrates by human faecal bacteria. Environmental Microbiology 9:667-679. 20. Gullick, R. W., and M. W. LeChevallier. 2000. Occurrence of MTBE in drinking water sources. Journal American Water Works Association 92:100. 21. Haggblom, M. M., P. Somsamak, and R. M. Cowan. 2001. Anaerobic biotransformation of fuel oxygenates under sulfate-reducing conditions. Fems Microbiology Ecology 37:259-264. 22. Haggblom, M. M., P. Somsamak, and H. H. Richnow. 2006. Carbon isotope fractionation during anaerobic degradation of methyl tert-butyl ether under sulfate-reducing and methanogenic conditions. Applied and Environmental Microbiology 72:1157-1163. 133 23. Haggblom, M. M., P. Somsamak, and H. H. Richnow. 2005. Carbon isotopic fractionation during anaerobic biotransformation of methyl tert-butyl ether and tert-amyl methyl ether. Environmental Science & Technology 39:103-109. 24. Haggblom, M. M., L. K. G. Youngster, and P. Somsamak. 2008. Effects of co-substrates and inhibitors on the anaerobic O-demethylation of methyl tert-butyl ether (MTBE). Applied Microbiology and Biotechnology 80:1113-1120. 25. Hardison, L. K., S. S. Curry, L. M. Ciuffetti, and M. R. Hyman. 1997. Metabolism of diethyl ether and cometabolism of methyl tert-butyl ether by a filamentous fungus, a Graphium sp. Applied and Environmental Microbiology 63:3059-3067. 26. Heald, P. C., S. G. Schladow, J. E. Reuter, and B. C. Allen. 2005. Modeling MTBE and BTEX in lakes and reservoirs used for recreational boating. Environmental Science & Technology 39:1111-1118. 27. Hyman, M., D. Aslett, and J. Haas. 2011. Identification of tertiary butyl alcohol (TBA)-utilizing organisms in BioGAC reactors using (13)C-DNA stable isotope probing. Biodegradation 22:961-972. 28. Juhler, R. K., and G. Felding. 2003. Monitoring methyl tertiary butyl ether (MTBE) and other organic micropollutants in groundwater: Results from the Danish National Monitoring Program. Water Air and Soil Pollution 149:145-161. 29. Kelley, C. A., B. T. Hammer, and R. B. Coffin. 1997. Concentrations and stable isotope values of BTEX in gasoline-contaminated groundwater. Environmental Science & Technology 31:2469-2472. 30. Kerkhof, L. J., E. M. Gallagher, L. Y. Young, and L. M. McGuinness. 2010. Detection of 2,4,6-trinitrotoluene-utilizing anaerobic bacteria by (15)N and (13)C incorporation. Applied and Environmental Microbiology 76:1695-1698. 31. Kerkhof, L. J., A. R. Oka, C. D. Phelps, L. M. McGuinness, A. Mumford, and L. Y. Young. 2008. Identification of critical members in a sulfidogenic benzene-degrading consortium by DNA stable isotope probing. Applied and Environmental Microbiology 74:6476-6480. 32. Kharoune, M., A. Pauss, and J. M. Lebeault. 2001. Aerobic biodegradation of an oxygenates mixture: ETBE, MTBE and TAME in an upflow fixed-bed reactor. Water Research 35:1665-1674. 33. Kleinsteuber, S., K. M. Schleinitz, J. Breitfeld, H. Harms, H. H. Richnow, and C. Vogt. 2008. Molecular characterization of bacterial communities mineralizing benzene under sulfate-reducing conditions. Fems Microbiology Ecology 66:143-157. 134 34. Klinger, J., C. Stieler, F. Sacher, and H. J. Branch. 2002. MTBE (methyl tertiary-butyl ether) in groundwaters: Monitoring results from Germany. Journal of Environmental Monitoring 4:276-279. 35. Lince, D. P., L. R. Wilson, G. A. Carlson, and A. Bucciferro. 2001. Effects of gasoline formulation on methyl tert-butyl ether (MTBL) contamination in private wells near gasoline stations. Environmental Science & Technology 35:1050-1053. 36. Lovley, D. R., and K. T. Finneran. 2001. Anaerobic degradation of methyl tert-butyl ether (MTBE) and tert-butyl alcohol (TBA). Environmental Science & Technology 35:1785-1790. 37. Luo, C. L., S. G. Xie, W. M. Sun, X. D. Li, and A. M. Cupples. 2009. Identification of a novel toluene-degrading bacterium from the candidate phylum TM7, as determined by DNA stable isotope probing. Applied and Environmental Microbiology 75:4644-4647. 38. Magar, V. S., K. Hartzell, C. Burton, J. T. Gibbs, and T. L. Macchiarella. 2002. Aerobic and cometabolic MTBE biodegradation at Novato and Port Hueneme. Journal of Environmental Engineering-Asce 128:883-890. 39. Mo, K., C. O. Lora, A. E. Wanken, M. Javanmardian, X. Yang, and C. F. Kulpa. 1997. Biodegradation of methyl t-butyl ether by pure bacterial cultures. Applied Microbiology and Biotechnology 47:69-72. 40. Moran, M. J., J. S. Zogorski, and P. J. Squillace. 2005. MTBE and gasoline hydrocarbons in ground water of the United States. Ground Water 43:615-627. 41. Mormile, M. R., S. Liu, and J. M. Suflita. 1994. Anaerobic biodegradation of gasoline oxygenate - extrapolation of information to multiple sites and redox conditions. Environmental Science & Technology 28:1727-1732. 42. NEIWPCC. 2003. A Survey of State Experiences with MTBE Contamination at LUST Sites. A Project of the New England Interstate Water Pollution Control Commission, http://www.neiwpcc.org/PDF_Docs/2003mtbecom.pdf (accessed June 2006). 43. Pruden, A., M. Raynal, and B. Crimi. 2010. Enrichment and characterization of MTBE-degrading cultures under iron and sulfate reducing conditions. Canadian Journal of Civil Engineering 37:522-534. 44. Raynal, M., B. Crimi, and A. Pruden. 2010. Enrichment and characterization of MTBE-degrading cultures under iron and sulfate reducing conditions. Canadian Journal of Civil Engineering 37:522-534. 45. Raynal, M., and A. Pruden. 2008. Aerobic MTBE biodegradation in the presence of BTEX by two consortia under batch and semi-batch conditions. Biodegradation 19:269-282. 135 46. Reuter, J. E., B. C. Allen, R. C. Richards, J. F. Pankow, C. R. Goldman, R. L. Scholl, and J. S. Seyfried. 1998. Concentrations, sources, and fate of the gasoline oxygenate methyl tert-butyl ether (MTBE) in a multiple use lake. Environmental Science & Technology 32:3666-3672. 47. Salanitro, J. P., L. A. Diaz, M. P. Williams, and H. L. Wisniewski. 1994. Isolation of a bacterial culture that degrades methyl t-butyl ether. Applied and Environmental Microbiology 60:2593-2596. 48. Schmidt, T. C., S. B. Haderlein, R. Pfister, and R. Forster. 2004. Occurrence and fate modeling of MTBE and BTEX compounds in a Swiss Lake used as drinking water supply. Water Research 38:1520-1529. 49. Scow, K. M., J. R. Hanson, and C. E. Ackerman. 1999. Biodegradation of methyl tert-butyl ether by a bacterial pure culture. Applied and Environmental Microbiology 65:4788-4792. 50. Sghir, A., D. Riviere, V. Desvignes, E. Pelletier, S. Chaussonnerie, S. Guermazi, J. Weissenbach, T. Li, and P. Camacho. 2009. Towards the definition of a core of microorganisms involved in anaerobic digestion of sludge. Isme Journal 3:700-714. 51. Smith, A. E., K. Hristova, I. Wood, D. M. Mackay, E. Lory, D. Lorenzana, and K. M. Scow. 2005. Comparison of biostimulation versus bioaugmentation with bacterial strain PM1 for treatment of groundwater contaminated with methyl tertiary butyl ether (MTBE). Environmental Health Perspectives 113:317-322. 52. Squillace, P. J., M. J. Moran, W. W. Lapham, C. V. Price, R. M. Clawges, and J. S. Zogorski. 1999. Volatile organic compounds in untreated ambient groundwater of the United States, 1985-1995. Environmental Science & Technology 33:4176-4187. 53. Squillace, P. J., M. J. Moran, and C. V. Price. 2004. VOCs in shallow groundwater in new residential/commercial areas of the United States. Environmental Science & Technology 38:5327-5338. 54. Suidan, M. T., A. Pruden, M. A. Sedran, and A. D. Venosa. 2005. Anaerobic biodegradation of methyl tert-butyl ether under iron-reducing conditions in batch and continuous-flow cultures. Water Environment Research 77:297-303. 55. Sun, W. M., S. G. Xie, C. L. Luo, and A. M. Cupples. 2010. Direct link between toluene degradation in contaminated-site microcosms and a Polaromonas strain. Applied and Environmental Microbiology 76:956-959. 56. USEPA. September 15, 1999. Blue Ribbon Panel. Achieving clean air and clean water: The report of the Blue Ribbon Panel on oxygenates in gasoline. EPA420-R-99-021. . 136 57. Wilson, G. J., A. Pruden, M. T. Suidan, and A. D. Venosa. 2002. Biodegradation kinetics of MTBE in laboratory batch and continuous flow reactors. Journal of Environmental Engineering-Asce 128:824-829. 58. Wilson, G. J., A. P. Richter, M. T. Suidan, and A. D. Venosa. 2001. Aerobic biodegradation of gasoline oxygenates MTBE and TBA. Water Science and Technology 43:277-284. 59. Wilson, J. T., R. Kolhatkar, T. Kuder, P. Philp, and S. J. Daugherty. 2005. Stable isotope analysis of MTBE to evaluate the source of TBA in ground water. Ground Water Monitoring and Remediation 25:108-116. 60. Xie, S. G., W. M. Sun, C. L. Luo, and A. M. Cupples. 2011. Novel aerobic benzene degrading microorganisms identified in three soils by stable isotope probing. Biodegradation 22:71-81. 61. Xie, S. G., W. M. Sun, C. L. Luo, and A. M. Cupples. 2010. Stable isotope probing identifies novel m-xylene degraders in soil microcosms from contaminated and uncontaminated sites. Water Air and Soil Pollution 212:113-122. 62. Yang, Y. R., and J. Zeyer. 2003. Specific detection of Dehalococcoides species by fluorescence in situ hybridization with 16S rRNA-targeted oligonucleotide probes. Applied and Environmental Microbiology 69:2879-2883. 63. Youngster, L. K. G., L. J. Kerkhof, and M. M. Haggblom. 2010. Community characterization of anaerobic methyl tert-butyl ether (MTBE)-degrading enrichment cultures. FEMS Microbiology Ecology 72:279-288. 64. Zein, M. M., M. T. Suidan, and A. D. Venosa. 2006. Bioremediation of groundwater contaminated with gasoline hydrocarbons and oxygenates using a membrane-based reactor. Environmental Science & Technology 40:1997-2003. 137