@article {591,
	title = {Bioremediation. Anaerobes to the rescue.},
	journal = {Science},
	volume = {293},
	year = {2001},
	month = {2001 Aug 24},
	pages = {1444-6},
	keywords = {Bacteria, Aerobic, Bacteria, Anaerobic, Biodegradation, Environmental, Euryarchaeota, Ferric Compounds, Genome, Archaeal, Genome, Bacterial, Hydrocarbons, Aromatic, Hydrocarbons, Chlorinated, Metals, Methane, Nitrates, Oxidation-Reduction, Oxygen, Soil Microbiology, Sulfates, Sulfur-Reducing Bacteria, Water Pollutants, Chemical},
	issn = {0036-8075},
	doi = {10.1126/science.1063294},
	author = {Lovley, D R}
}
@article {593,
	title = {Anaerobic benzene degradation.},
	journal = {Biodegradation},
	volume = {11},
	year = {2000},
	month = {2000},
	pages = {107-16},
	abstract = {Although many studies have indicated that benzene persists under anaerobic conditions in petroleum-contaminated environments, it has recently been documented that benzene can be anaerobically oxidized with most commonly considered electron acceptors for anaerobic respiration. These include: Fe(III), sulfate, nitrate, and possibly humic substances. Benzene can also be converted to methane and carbon dioxide under methanogenic conditions. There is evidence that benzene can be degraded under in situ conditions in petroleum-contaminated aquifers in which either Fe(III) reduction or methane production is the predominant terminal electron-accepting process. Furthermore, evidence from laboratory studies suggests that benzene may be anaerobically degraded in petroleum-contaminated marine sediments under sulfate-reducing conditions. Laboratory studies have suggested that within the Fe(III) reduction zone of petroleum-contaminated aquifers, benzene degradation can be stimulated with the addition of synthetic chelators which make Fe(III) more available for microbial reduction. The addition of humic substances and other compounds that contain quinone moieties can also stimulate anaerobic benzene degradation in laboratory incubations of Fe(III)-reducing aquifer sediments by providing an electron shuttle between Fe(III)-reducing microorganisms and insoluble Fe(III) oxides. Anaerobic benzene degradation in aquifer sediments can be stimulated with the addition of sulfate, but in some instances an inoculum of benzene-oxidizing, sulfate-reducing microorganisms must also be added. In a field trial, sulfate addition to the methanogenic zone of a petroleum-contaminated aquifer stimulated the growth and activity of sulfate-reducing microorganisms and enhanced benzene removal. Molecular phylogenetic studies have provided indications of what microorganisms might be involved in anaerobic benzene degradation in aquifers. The major factor limiting further understanding of anaerobic benzene degradation is the lack of a pure culture of an organism capable of anaerobic benzene degradation.},
	keywords = {Bacteria, Anaerobic, Benzene, Biodegradation, Environmental, Oxidation-Reduction},
	issn = {0923-9820},
	author = {Lovley, D R}
}
@article {608,
	title = {Novel forms of anaerobic respiration of environmental relevance.},
	journal = {Curr Opin Microbiol},
	volume = {3},
	year = {2000},
	month = {2000 Jun},
	pages = {252-6},
	abstract = {Novel forms of anaerobic respiration continue to be discovered. Many of these are environmentally significant as they have important impacts on the fate of organic carbon and the cycling of many inorganic compounds. Furthermore, anaerobic respiration is becoming increasing recognized as a strategy for the remediation of organic and metal contaminants in the subsurface.},
	keywords = {Anaerobiosis, Bacteria, Anaerobic, Environment, Industrial Microbiology, Industrial Waste},
	issn = {1369-5274},
	author = {Lovley, D R and Coates, J D}
}
@article {627,
	title = {Dissimilatory arsenate and sulfate reduction in Desulfotomaculum auripigmentum sp. nov.},
	journal = {Arch Microbiol},
	volume = {168},
	year = {1997},
	month = {1997 Nov},
	pages = {380-8},
	abstract = {A newly discovered arsenate-reducing bacterium, strain OREX-4, differed significantly from strains MIT-13 and SES-3, the previously described arsenate-reducing isolates, which grew on nitrate but not on sulfate. In contrast, strain OREX-4 did not respire nitrate but grew on lactate, with either arsenate or sulfate serving as the electron acceptor, and even preferred arsenate. Both arsenate and sulfate reduction were inhibited by molybdate. Strain OREX-4, a gram-positive bacterium with a hexagonal S-layer on its cell wall, metabolized compounds commonly used by sulfate reducers. Scorodite (FeAsO42. H2O) an arsenate-containing mineral, provided micromolar concentrations of arsenate that supported cell growth. Physiologically and phylogenetically, strain OREX-4 was far-removed from strains MIT-13 and SES-3: strain OREX-4 grew on different electron donors and electron acceptors, and fell within the gram-positive group of the Bacteria, whereas MIT-13 and SES-3 fell together in the epsilon-subdivision of the Proteobacteria. Together, these results suggest that organisms spread among diverse bacterial phyla can use arsenate as a terminal electron acceptor, and that dissimilatory arsenate reduction might occur in the sulfidogenic zone at arsenate concentrations of environmental interest. 16S rRNA sequence analysis indicated that strain OREX-4 is a new species of the genus Desulfotomaculum, and accordingly, the name Desulfotomaculum auripigmentum is proposed.},
	keywords = {Arsenates, Bacteria, Anaerobic, Biotransformation, Geologic Sediments, Gram-Positive Endospore-Forming Rods, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Substrate Specificity, Sulfates, Sulfides, Sulfur-Reducing Bacteria, Water Microbiology},
	issn = {0302-8933},
	author = {Newman, D K and Kennedy, E K and Coates, J D and Ahmann, D and Ellis, D J and Lovley, D R and Morel, F M}
}
@article {634,
	title = {Phylogenetic analysis of dissimilatory Fe(III)-reducing bacteria.},
	journal = {J Bacteriol},
	volume = {178},
	year = {1996},
	month = {1996 Apr},
	pages = {2402-8},
	abstract = {Evolutionary relationships among strictly anaerobic dissimilatory Fe(III)-reducing bacteria obtained from a diversity of sedimentary environments were examined by phylogenetic analysis of 16S rRNA gene sequences. Members of the genera Geobacter, Desulfuromonas, Pelobacter, and Desulfuromusa formed a monophyletic group within the delta subdivision of the class Proteobacteria. On the basis of their common ancestry and the shared ability to reduce Fe(III) and/or S0, we propose that this group be considered a single family, Geobacteraceae. Bootstrap analysis, characteristic nucleotides, and higher-order secondary structures support the division of Geobacteraceae into two subgroups, designated the Geobacter and Desulfuromonas clusters. The genus Desulfuromusa and Pelobacter acidigallici make up a distinct branch within the Desulfuromonas cluster. Several members of the family Geobacteraceae, none of which reduce sulfate, were found to contain the target sequences of probes that have been previously used to define the distribution of sulfate-reducing bacteria and sulfate-reducing bacterium-like microorganisms. The recent isolations of Fe(III)-reducing microorganisms distributed throughout the domain Bacteria suggest that development of 16S rRNA probes that would specifically target all Fe(III) reducers may not be feasible. However, all of the evidence suggests that if a 16S rRNA sequence falls within the family Geobacteraceae, then the organism has the capacity for Fe(III) reduction. The suggestion, based on geological evidence, that Fe(III) reduction was the first globally significant process for oxidizing organic matter back to carbon dioxide is consistent with the finding that acetate-oxidizing Fe(III) reducers are phylogenetically diverse.},
	keywords = {Bacteria, Anaerobic, Base Sequence, DNA, Ribosomal, Ferric Compounds, Iron, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Sequence Homology, Nucleic Acid},
	issn = {0021-9193},
	author = {Lonergan, D J and Jenter, H L and Coates, J D and Phillips, E J and Schmidt, T M and Lovley, D R}
}
@article {639,
	title = {Fe(III) and S0 reduction by Pelobacter carbinolicus.},
	journal = {Appl Environ Microbiol},
	volume = {61},
	year = {1995},
	month = {1995 Jun},
	pages = {2132-8},
	abstract = {There is a close phylogenetic relationship between Pelobacter species and members of the genera Desulfuromonas and Geobacter, and yet there has been a perplexing lack of physiological similarities. Pelobacter species have been considered to have a fermentative metabolism. In contrast, Desulfuromonas and Geobacter species have a respiratory metabolism with Fe(III) serving as the common terminal electron acceptor in all species. However, the ability of Pelobacter species to reduce Fe(III) had not been previously evaluated. When a culture of Pelobacter carbinolicus that had grown by fermentation of 2,3-butanediol was inoculated into the same medium supplemented with Fe(III), the Fe(III) was reduced. There was less accumulation of ethanol and more production of acetate in the presence of Fe(III). P. carbinolicus grew with ethanol as the sole electron donor and Fe(III) as the sole electron acceptor. Ethanol was metabolized to acetate. Growth was also possible on Fe(III) with the oxidation of propanol to propionate or butanol to butyrate if acetate was provided as a carbon source. P. carbinolicus appears capable of conserving energy to support growth from Fe(III) respiration as it also grew with H2 or formate as the electron donor and Fe(III) as the electron acceptor. Once adapted to Fe(III) reduction, P. carbinolicus could also grow on ethanol or H2 with S0 as the electron acceptor. P. carbinolicus did not contain detectable concentrations of the c-type cytochromes that previous studies have suggested are involved in electron transport to Fe(III) in other organisms that conserve energy to support growth from Fe(III) reduction.(ABSTRACT TRUNCATED AT 250 WORDS)},
	keywords = {Bacteria, Anaerobic, Base Sequence, Butylene Glycols, Culture Media, Ethanol, Ferrous Compounds, Hydrogen, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Sulfur},
	issn = {0099-2240},
	author = {Lovley, D R and Phillips, E J and Lonergan, D J and Widman, P K}
}
