@article {420,
	title = {Molecular analysis of the metabolic rates of discrete subsurface populations of sulfate reducers.},
	journal = {Appl Environ Microbiol},
	volume = {77},
	year = {2011},
	month = {2011 Sep},
	pages = {6502-9},
	abstract = {Elucidating the in situ metabolic activity of phylogenetically diverse populations of sulfate-reducing microorganisms that populate anoxic sedimentary environments is key to understanding subsurface ecology. Previous pure culture studies have demonstrated that the transcript abundance of dissimilatory (bi)sulfite reductase genes is correlated with the sulfate-reducing activity of individual cells. To evaluate whether expression of these genes was diagnostic for subsurface communities, dissimilatory (bi)sulfite reductase gene transcript abundance in phylogenetically distinct sulfate-reducing populations was quantified during a field experiment in which acetate was added to uranium-contaminated groundwater. Analysis of dsrAB sequences prior to the addition of acetate indicated that Desulfobacteraceae, Desulfobulbaceae, and Syntrophaceae-related sulfate reducers were the most abundant. Quantifying dsrB transcripts of the individual populations suggested that Desulfobacteraceae initially had higher dsrB transcripts per cell than Desulfobulbaceae or Syntrophaceae populations and that the activity of Desulfobacteraceae increased further when the metabolism of dissimilatory metal reducers competing for the added acetate declined. In contrast, dsrB transcript abundance in Desulfobulbaceae and Syntrophaceae remained relatively constant, suggesting a lack of stimulation by added acetate. The indication of higher sulfate-reducing activity in the Desulfobacteraceae was consistent with the finding that Desulfobacteraceae became the predominant component of the sulfate-reducing community. Discontinuing acetate additions resulted in a decline in dsrB transcript abundance in the Desulfobacteraceae. These results suggest that monitoring transcripts of dissimilatory (bi)sulfite reductase genes in distinct populations of sulfate reducers can provide insight into the relative rates of metabolism of different components of the sulfate-reducing community and their ability to respond to environmental perturbations.},
	keywords = {Biodiversity, Deltaproteobacteria, DNA, Bacterial, Gene Expression Profiling, Hydrogensulfite Reductase, Molecular Sequence Data, Oxidation-Reduction, Sequence Analysis, DNA, Soil Microbiology, Sulfates, Water Microbiology},
	issn = {1098-5336},
	doi = {10.1128/AEM.00576-11},
	author = {Miletto, M and Williams, K H and N{\textquoteright}Guessan, A L and Lovley, D R}
}
@article {486,
	title = {Characterization of extracellular minerals produced during dissimilatory Fe(III) and U(VI) reduction at 100 degrees C by Pyrobaculum islandicum.},
	journal = {Geobiology},
	volume = {6},
	year = {2008},
	month = {2008 Mar},
	pages = {147-54},
	abstract = {In order to gain insight into the significance of biotic metal reduction and mineral formation in hyperthermophilic environments, metal mineralization as a result of the dissimilatory reduction of poorly crystalline Fe(III) oxide, and U(VI) reduction at 100 degrees C by Pyrobaculum islandicum was investigated. When P. islandicum was grown in a medium with poorly crystalline Fe(III) oxide as an electron acceptor and hydrogen as an electron donor, the Fe(III) oxide was reduced to an extracellular, ultrafine-grained magnetite with characteristics similar to that found in some hot environments and that was previously thought to be of abiotic origin. Furthermore, cell suspensions of P. islandicum rapidly reduced the soluble and oxidized form of uranium, U(VI), to extracellular precipitates of the highly insoluble U(IV) mineral, uraninite (UO(2)). The reduction of U(VI) was dependent on the presence of hydrogen as the electron donor. These findings suggest that microbes may play a key role in metal deposition in hyperthermophilic environments and provide a plausible explanation for such phenomena as magnetite accumulation and formation of uranium deposits at ca. 100 degrees C.},
	keywords = {Ferric Compounds, Ferumoxytol, Hot Temperature, Hydrogen, Minerals, Oxidation-Reduction, Pyrobaculum, Uranium, X-Ray Diffraction},
	issn = {1472-4669},
	doi = {10.1111/j.1472-4669.2007.00142.x},
	author = {Kashefi, K and Moskowitz, B M and Lovley, D R}
}
@article {479,
	title = {Power output and columbic efficiencies from biofilms of Geobacter sulfurreducens comparable to mixed community microbial fuel cells.},
	journal = {Environ Microbiol},
	volume = {10},
	year = {2008},
	month = {2008 Oct},
	pages = {2505-14},
	abstract = {It has been previously noted that mixed communities typically produce more power in microbial fuel cells than pure cultures. If true, this has important implications for the design of microbial fuel cells and for studying the process of electron transfer on anode biofilms. To further evaluate this, Geobacter sulfurreducens was grown with acetate as fuel in a continuous flow {\textquoteright}ministack{\textquoteright} system in which the carbon cloth anode and cathode were positioned in close proximity, and the cation-selective membrane surface area was maximized in order to overcome some of the electrochemical limitations that were inherent in fuel cells previously employed for the study of pure cultures. Reducing the size of the anode in order to eliminate cathode limitation resulted in maximum current and power densities per m(2) of anode surface of 4.56 A m(-2) and 1.88 W m(-2) respectively. Electron recovery as current from acetate oxidation was c. 100\% when oxygen diffusion into the system was minimized. This performance is comparable to the highest levels previously reported for mixed communities in similar microbial fuel cells and slightly higher than the power output of an anaerobic sludge inoculum in the same ministack system. Minimizing the volume of the anode chamber yielded a volumetric power density of 2.15 kW m(-3), which is the highest power density per volume yet reported for a microbial fuel cell. Geobacter sulfurreducens formed relatively uniform biofilms 3-18 mum thick on the carbon cloth anodes. When graphite sticks served as the anode, the current density (3.10 A m(-2)) was somewhat less than with the carbon cloth anodes, but the biofilms were thicker (c. 50 mum) with a more complex pillar and channel structure. These results suggest that the previously observed disparity in power production in pure and mixed culture microbial fuel cell systems can be attributed more to differences in the fuel cell designs than to any inherent superior capability of mixed cultures to produce more power than pure cultures.},
	keywords = {Acetic Acid, Biofilms, Carbon, Electricity, Electrodes, Geobacter, Oxidation-Reduction},
	issn = {1462-2920},
	doi = {10.1111/j.1462-2920.2008.01675.x},
	author = {Nevin, K P and Richter, H and Covalla, S F and Johnson, J P and Woodard, T L and Orloff, A L and Jia, H and Zhang, M and Lovley, D R}
}
@article {524,
	title = {Characterization of metabolism in the Fe(III)-reducing organism Geobacter sulfurreducens by constraint-based modeling.},
	journal = {Appl Environ Microbiol},
	volume = {72},
	year = {2006},
	month = {2006 Feb},
	pages = {1558-68},
	abstract = {Geobacter sulfurreducens is a well-studied representative of the Geobacteraceae, which play a critical role in organic matter oxidation coupled to Fe(III) reduction, bioremediation of groundwater contaminated with organics or metals, and electricity production from waste organic matter. In order to investigate G. sulfurreducens central metabolism and electron transport, a metabolic model which integrated genome-based predictions with available genetic and physiological data was developed via the constraint-based modeling approach. Evaluation of the rates of proton production and consumption in the extracellular and cytoplasmic compartments revealed that energy conservation with extracellular electron acceptors, such as Fe(III), was limited relative to that associated with intracellular acceptors. This limitation was attributed to lack of cytoplasmic proton consumption during reduction of extracellular electron acceptors. Model-based analysis of the metabolic cost of producing an extracellular electron shuttle to promote electron transfer to insoluble Fe(III) oxides demonstrated why Geobacter species, which do not produce shuttles, have an energetic advantage over shuttle-producing Fe(III) reducers in subsurface environments. In silico analysis also revealed that the metabolic network of G. sulfurreducens could synthesize amino acids more efficiently than that of Escherichia coli due to the presence of a pyruvate-ferredoxin oxidoreductase, which catalyzes synthesis of pyruvate from acetate and carbon dioxide in a single step. In silico phenotypic analysis of deletion mutants demonstrated the capability of the model to explore the flexibility of G. sulfurreducens central metabolism and correctly predict mutant phenotypes. These results demonstrate that iterative modeling coupled with experimentation can accelerate the understanding of the physiology of poorly studied but environmentally relevant organisms and may help optimize their practical applications.},
	keywords = {Amino Acids, Electron Transport, Escherichia coli, Fumarates, Geobacter, Iron, Models, Biological, Mutation, Oxidation-Reduction, Phenotype, Protons, Quinones, Species Specificity},
	issn = {0099-2240},
	doi = {10.1128/AEM.72.2.1558-1568.2006},
	author = {Mahadevan, R and Bond, D R and Butler, J E and Esteve-Nu{\~n}ez, A and Coppi, M V and Palsson, B O and Schilling, C H and Lovley, D R}
}
@article {531,
	title = {Adaptation to disruption of the electron transfer pathway for Fe(III) reduction in Geobacter sulfurreducens.},
	journal = {J Bacteriol},
	volume = {187},
	year = {2005},
	month = {2005 Sep},
	pages = {5918-26},
	abstract = {Previous studies demonstrated that an outer membrane c-type cytochrome, OmcB, was involved in Fe(III) reduction in Geobacter sulfurreducens. An OmcB-deficient mutant was greatly impaired in its ability to reduce both soluble and insoluble Fe(III). Reintroducing omcB restored the capacity for Fe(III) reduction at a level proportional to the level of OmcB production. Here, we report that the OmcB-deficient mutant gradually adapted to grow on soluble Fe(III) but not insoluble Fe(III). The adapted OmcB-deficient mutant reduced soluble Fe(III) at a rate comparable to that of the wild type, but the cell yield of the mutant was only ca. 60\% of that of the wild type under steady-state culturing conditions. Analysis of proteins and transcript levels demonstrated that expression of several membrane-associated cytochromes was higher in the adapted mutant than in the wild type. Further comparison of transcript levels during steady-state growth on Fe(III) citrate with a whole-genome DNA microarray revealed a significant shift in gene expression in an apparent attempt to adapt metabolism to the impaired electron transport to Fe(III). These results demonstrate that, although there are many other membrane-bound c-type cytochromes in G. sulfurreducens, increased expression of these cytochromes cannot completely compensate for the loss of OmcB. The concept that outer membrane cytochromes are promiscuous reductases that are interchangeable in function appears to be incorrect. Furthermore, the results indicate that there may be different mechanisms for electron transfer to soluble Fe(III) and insoluble Fe(III) oxides in G. sulfurreducens, which emphasizes the importance of studying electron transport to the environmentally relevant Fe(III) oxides.},
	keywords = {Adaptation, Physiological, Bacterial Outer Membrane Proteins, Base Sequence, Cytochromes c, DNA Primers, Electron Transport, Ferric Compounds, Gene Expression Regulation, Bacterial, Geobacter, Kinetics, Oxidation-Reduction, Reverse Transcriptase Polymerase Chain Reaction},
	issn = {0021-9193},
	doi = {10.1128/JB.187.17.5918-5926.2005},
	author = {Leang, Ching and Adams, L A and Chin, K-J and Nevin, K P and Meth{\'e}, B A and Webster, J and Sharma, M L and Lovley, D R}
}
@article {527,
	title = {Outer membrane c-type cytochromes required for Fe(III) and Mn(IV) oxide reduction in Geobacter sulfurreducens.},
	journal = {Appl Environ Microbiol},
	volume = {71},
	year = {2005},
	month = {2005 Dec},
	pages = {8634-41},
	abstract = {The potential role of outer membrane proteins in electron transfer to insoluble Fe(III) oxides by Geobacter sulfurreducens was investigated because this organism is closely related to the Fe(III) oxide-reducing organisms that are predominant in many Fe(III)-reducing environments. Two of the most abundant proteins that were easily sheared from the outer surfaces of intact cells were c-type cytochromes. One, designated OmcS, has a molecular mass of ca. 50 kDa and is predicted to be an outer membrane hexaheme c-type cytochrome. Transcripts for omcS could be detected during growth on Fe(III) oxide, but not on soluble Fe(III) citrate. The omcS mRNA consisted primarily of a monocistronic transcript, and to a lesser extent, a longer transcript that also contained the downstream gene omcT, which is predicted to encode a second hexaheme outer membrane cytochrome with 62.6\% amino acid sequence identity to OmcS. The other abundant c-type cytochrome sheared from the outer surface of G. sulfurreducens, designated OmcE, has a molecular mass of ca. 30 kDa and is predicted to be an outer membrane tetraheme c-type cytochrome. When either omcS or omcE was deleted, G. sulfurreducens could no longer reduce Fe(III) oxide but could still reduce soluble electron acceptors, including Fe(III) citrate. The mutants could reduce Fe(III) in Fe(III) oxide medium only if the Fe(III) chelator, nitrilotriacetic acid, or the electron shuttle, anthraquinone 2,6-disulfonate, was added. Expressing omcS or omcE in trans restored the capacity for Fe(III) oxide reduction. OmcT was not detected among the sheared proteins, and genetic studies indicated that G. sulfurreducens could not reduce Fe(III) oxide when omcT was expressed but OmcS was absent. In contrast, Fe(III) oxide was reduced when omcS was expressed in the absence of OmcT. These results suggest that OmcS and OmcE are involved in electron transfer to Fe(III) oxides in G. sulfurreducens. They also emphasize the importance of evaluating mechanisms for Fe(III) reduction with environmentally relevant Fe(III) oxide, rather than the more commonly utilized Fe(III) citrate, because additional electron transfer components are required for Fe(III) oxide reduction that are not required for Fe(III) citrate reduction.},
	keywords = {Amino Acid Sequence, Bacterial Outer Membrane Proteins, Bacterial Proteins, Base Sequence, Cytochromes c, DNA Primers, Ferric Compounds, Geobacter, Kinetics, Manganese Compounds, Molecular Sequence Data, Oxidation-Reduction, Oxides, Peptide Fragments},
	issn = {0099-2240},
	doi = {10.1128/AEM.71.12.8634-8641.2005},
	author = {Mehta, T and Coppi, M V and Childers, S E and Lovley, D R}
}
@article {562,
	title = {Genome of Geobacter sulfurreducens: metal reduction in subsurface environments.},
	journal = {Science},
	volume = {302},
	year = {2003},
	month = {2003 Dec 12},
	pages = {1967-9},
	abstract = {The complete genome sequence of Geobacter sulfurreducens, a delta-proteobacterium, reveals unsuspected capabilities, including evidence of aerobic metabolism, one-carbon and complex carbon metabolism, motility, and chemotactic behavior. These characteristics, coupled with the possession of many two-component sensors and many c-type cytochromes, reveal an ability to create alternative, redundant, electron transport networks and offer insights into the process of metal ion reduction in subsurface environments. As well as playing roles in the global cycling of metals and carbon, this organism clearly has the potential for use in bioremediation of radioactive metals and in the generation of electricity.},
	keywords = {Acetates, Acetyl Coenzyme A, Aerobiosis, Anaerobiosis, Bacterial Proteins, Carbon, Chemotaxis, Chromosomes, Bacterial, Cytochromes c, Electron Transport, Energy Metabolism, Genes, Bacterial, Genes, Regulator, Genome, Bacterial, Geobacter, Hydrogen, Metals, Movement, Open Reading Frames, Oxidation-Reduction, Phylogeny},
	issn = {1095-9203},
	doi = {10.1126/science.1088727},
	author = {Meth{\'e}, B A and Nelson, K E and Eisen, J A and Paulsen, I T and Nelson, W and Heidelberg, J F and Wu, D and Wu, M and Ward, N and Beanan, M J and Dodson, R J and Madupu, R and Brinkac, L M and Daugherty, S C and DeBoy, R T and Durkin, A S and Gwinn, M and Kolonay, J F and Sullivan, S A and Haft, D H and Selengut, J and Davidsen, T M and Zafar, N and White, O and Tran, B and Romero, C and Forberger, H A and Weidman, J and Khouri, H and Feldblyum, T V and Utterback, T R and Van Aken, S E and Lovley, D R and Fraser, C M}
}
@article {571,
	title = {OmcB, a c-type polyheme cytochrome, involved in Fe(III) reduction in Geobacter sulfurreducens.},
	journal = {J Bacteriol},
	volume = {185},
	year = {2003},
	month = {2003 Apr},
	pages = {2096-103},
	abstract = {Microorganisms in the family Geobacteraceae are the predominant Fe(III)-reducing microorganisms in a variety of subsurface environments in which Fe(III) reduction is an important process, but little is known about the mechanisms for electron transport to Fe(III) in these organisms. The Geobacter sulfurreducens genome was found to contain a 10-kb chromosomal duplication consisting of two tandem three-gene clusters. The last genes of the two clusters, designated omcB and omcC, encode putative outer membrane polyheme c-type cytochromes which are 79\% identical. The role of the omcB and omcC genes in Fe(III) reduction in G. sulfurreducens was investigated. OmcB and OmcC were both expressed during growth with acetate as the electron donor and either fumarate or Fe(III) as the electron acceptor. OmcB was ca. twofold more abundant under both conditions. Disrupting omcB or omcC by gene replacement had no impact on growth with fumarate. However, the OmcB-deficient mutant was greatly impaired in its ability to reduce Fe(III) both in cell suspensions and under growth conditions. In contrast, the ability of the OmcC-deficient mutant to reduce Fe(III) was similar to that of the wild type. When omcB was reintroduced into the OmcB-deficient mutant, the capacity for Fe(III) reduction was restored in proportion to the level of OmcB production. These results indicate that OmcB, but not OmcC, has a major role in electron transport to Fe(III) and suggest that electron transport to the outer membrane is an important feature in Fe(III) reduction in this organism.},
	keywords = {Amino Acid Sequence, Bacterial Outer Membrane Proteins, Bacterial Proteins, Cytochrome c Group, Deltaproteobacteria, Gene Expression Regulation, Bacterial, Iron, Molecular Sequence Data, Multigene Family, Mutation, Oxidation-Reduction, Sequence Homology, Amino Acid},
	issn = {0021-9193},
	author = {Leang, Ching and Coppi, M V and Lovley, D R}
}
@article {603,
	title = {Acetate oxidation coupled to Fe(iii) reduction in hyperthermophilic microorganisms.},
	journal = {Appl Environ Microbiol},
	volume = {67},
	year = {2001},
	month = {2001 Mar},
	pages = {1363-5},
	abstract = {No hyperthermophilic microorganisms have previously been shown to anaerobically oxidize acetate, the key extracellular intermediate in the anaerobic oxidation of organic matter. Here we report that two hyperthermophiles, Ferroglobus placidus and "Geoglobus ahangari," grow at 85 degrees C by oxidizing acetate to carbon dioxide, with Fe(III) serving as the electron acceptor. These results demonstrate that acetate could potentially be metabolized within the hot microbial ecosystems in which hyperthermophiles predominate, rather than diffusing to cooler environments prior to degradation as has been previously proposed.},
	keywords = {Acetates, Anaerobiosis, Archaea, Ferric Compounds, Hot Temperature, Oxidation-Reduction},
	issn = {0099-2240},
	doi = {10.1128/AEM.67.3.1363-1365.2001},
	author = {Tor, J M and Kashefi, K and Lovley, D R}
}
@article {598,
	title = {Anaerobic degradation of aromatic compounds coupled to Fe(III) reduction by Ferroglobus placidus.},
	journal = {Environ Microbiol},
	volume = {3},
	year = {2001},
	month = {2001 Apr},
	pages = {281-7},
	abstract = {Aromatic compounds are an important component of the organic matter in some of the anaerobic environments that hyperthermophilic microorganisms inhabit, but the potential for hyperthermophilic microorganisms to metabolize aromatic compounds has not been described previously. In this study, aromatic metabolism was investigated in the hyperthermophile Ferroglobus placidus. F. placidus grew at 85 degrees C in anaerobic medium with a variety of aromatic compounds as the sole electron donor and poorly crystalline Fe(III) oxide as the electron acceptor. Growth coincided with Fe(III) reduction. Aromatic compounds supporting growth included benzoate, phenol, 4-hydroxybenzoate, benzaldehyde, p-hydroxybenzaldehyde and t-cinnamic acid (3-phenyl-2-propenoic acid). These aromatic compounds did not support growth when nitrate was provided as the electron acceptor, even though nitrate supports the growth of this organism with Fe(II) or H2 as the electron donor. The stoichiometry of benzoate and phenol uptake and Fe(III) reduction indicated that F. placidus completely oxidized these aromatic compounds to carbon dioxide, with Fe(III) serving as the sole electron acceptor. This is the first example of an Archaea that can anaerobically oxidize an aromatic compound. These results also demonstrate for the first time that hyperthermophilic microorganisms can anaerobically oxidize aromatic compounds and suggest that hyperthermophiles may metabolize aromatic compounds in hot environments such as the deep hot subsurface and in marine and terrestrial hydrothermal zones in which Fe(III) is available as an electron acceptor.},
	keywords = {Anaerobiosis, Archaea, Electron Transport, Ferric Compounds, Hot Temperature, Hydrocarbons, Aromatic, Oxidation-Reduction},
	issn = {1462-2912},
	author = {Tor, J M and Lovley, D R}
}
@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 {600,
	title = {Comment on "Abiotic controls on H2 production from basalt-water reactions and implications for aquifer biogeochemistry".},
	journal = {Environ Sci Technol},
	volume = {35},
	year = {2001},
	month = {2001 Apr 1},
	pages = {1556-9},
	keywords = {Hydrogen, Minerals, Organic Chemicals, Oxidation-Reduction, Silicates, Water, Water Microbiology},
	issn = {0013-936X},
	author = {Anderson, R T and Chapelle, F H and Lovley, D R}
}
@article {606,
	title = {Differences in Fe(III) reduction in the hyperthermophilic archaeon, Pyrobaculum islandicum, versus mesophilic Fe(III)-reducing bacteria.},
	journal = {FEMS Microbiol Lett},
	volume = {195},
	year = {2001},
	month = {2001 Feb 20},
	pages = {253-8},
	abstract = {The discovery that all hyperthermophiles that have been evaluated have the capacity to reduce Fe(III) has raised the question of whether mechanisms for dissimilatory Fe(III) reduction have been conserved throughout microbial evolution. Many studies have suggested that c-type cytochromes are integral components in electron transport to Fe(III) in mesophilic dissimilatory Fe(III)-reducing microorganisms. However, Pyrobaculum islandicum, the hyperthermophile in which Fe(III) reduction has been most intensively studied, did not contain c-type cytochromes. NADPH was a better electron donor for the Fe(III) reductase activity in P. islandicum than NADH. This is the opposite of what has been observed with mesophiles. Thus, if previous models for dissimilatory Fe(III) reduction by mesophilic bacteria are correct, then it is unlikely that a single strategy for electron transport to Fe(III) is present in all dissimilatory Fe(III)-reducing microorganisms.},
	keywords = {Cytochrome c Group, Electron Transport, Ferric Compounds, FMN Reductase, NADH, NADPH Oxidoreductases, NADP, Oxidation-Reduction, Temperature, Thermoproteaceae},
	issn = {0378-1097},
	author = {Childers, S E and Lovley, D R}
}
@article {601,
	title = {Geobacter hydrogenophilus, Geobacter chapellei and Geobacter grbiciae, three new, strictly anaerobic, dissimilatory Fe(III)-reducers.},
	journal = {Int J Syst Evol Microbiol},
	volume = {51},
	year = {2001},
	month = {2001 Mar},
	pages = {581-8},
	abstract = {Recent studies on the diversity and ubiquity of Fe(III)-reducing organisms in different environments led to the isolation and identification of four new dissimilatory Fe(III)-reducers (strains H-2T, 172T, TACP-2T and TACP-5). All four isolates are non-motile, Gram-negative, freshwater, mesophilic, strict anaerobes with morphology identical to that of Geobacter metallireducens strain GS-15T. Analysis of the 16S rRNA sequences indicated that the new isolates belong to the genus Geobacter, in the delta-Proteobacteria. Significant differences in phenotypic characteristics, DNA-DNA homology and G+C content indicated that the four isolates represent three new species of the genus. The names Geobacter hydrogenophilus sp. nov. (strain H-2T), Geobacter chapellei sp. nov. (strain 172T) and Geobacter grbiciae sp. nov. (strains TACP-2T and TACP-5) are proposed. Geobacter hydrogenophilus and Geobacter chapellei were isolated from a petroleum-contaminated aquifer and a pristine, deep, subsurface aquifer, respectively. Geobacter grbiciae was isolated from aquatic sediments. All of the isolates can obtain energy for growth by coupling the oxidation of acetate to the reduction of Fe(III). The four isolates also coupled Fe(III) reduction to the oxidation of other simple, volatile fatty acids. In addition, Geobacter hydrogenophilus and Geobacter grbiciae were able to oxidize aromatic compounds such as benzoate, whilst Geobacter grbiciae was also able to use the monoaromatic hydrocarbon toluene.},
	keywords = {Base Composition, Deltaproteobacteria, Ferric Compounds, Gram-Negative Anaerobic Straight, Curved, and Helical Rods, Hydrocarbons, Iron, Molecular Sequence Data, Nucleic Acid Hybridization, Oxidation-Reduction, RNA, Ribosomal, 16S},
	issn = {1466-5026},
	author = {Coates, J D and Bhupathiraju, V K and Achenbach, L A and Mclnerney, M J and Lovley, D R}
}
@article {590,
	title = {Isolation, characterization and gene sequence analysis of a membrane-associated 89 kDa Fe(III) reducing cytochrome c from Geobacter sulfurreducens.},
	journal = {Biochem J},
	volume = {359},
	year = {2001},
	month = {2001 Oct 1},
	pages = {147-52},
	abstract = {Geobacter sulfurreducens is capable of anaerobic respiration with Fe(III) as a terminal electron acceptor via a membrane-bound Fe(III) reductase activity associated with a large molecular mass cytochrome c. This cytochrome was purified by detergent extraction of the membrane fraction, Q-Sepharose ion-exchange chromatography, preparative electrophoresis, and MonoQ ion-exchange chromatography. Spectrophotometric analysis of the purified cytochrome reveals a c-type haem, with no evidence of haem a, haem b or sirohaem. The cytochrome has an M(r) of 89000 as determined by denaturing PAGE, and has an isoelectric point of 5.2 as determined by analytical isoelectric focusing. Dithionite-reduced cytochrome can donate electrons to Fe(III)-nitrilotriacetic acid and synthetic ferrihydrite, thus demonstrating that the cytochrome has redox and thermodynamic properties required for reduction of Fe(III). Analysis using cyclic voltammetry confirmed that the reduced cytochrome can catalytically transfer electrons to ferrihydrite, further demonstrating its ability to be an electron transport mediator in anaerobic Fe(III) respiration. Sequence analysis of a cloned chromosomal DNA fragment revealed a 2307 bp open reading frame (ferA) encoding a 768 amino acid protein corresponding to the 89 kDa cytochrome. The deduced amino acid sequence (FerA) translated from the open reading frame contained 12 putative haem-binding motifs, as well as a hydrophobic N-terminal membrane anchor sequence, a lipid-attachment site and an ATP/GTP-binding site. FerA displayed 20\% or less identity with amino acid sequences of other known cytochromes, although it does share some features with characterized polyhaem cytochromes c.},
	keywords = {Amino Acid Sequence, Bacterial Proteins, Chromatography, Ion Exchange, Cloning, Molecular, Cytochrome c Group, Deltaproteobacteria, DNA Primers, Electron Transport, Electrophoresis, Polyacrylamide Gel, Ferric Compounds, Gene Expression Regulation, Bacterial, Molecular Sequence Data, Molecular Weight, Nitrilotriacetic Acid, Oxidation-Reduction, Polymerase Chain Reaction, Sequence Homology, Amino Acid},
	issn = {0264-6021},
	author = {Magnuson, T S and Isoyama, N and Hodges-Myerson, A L and Davidson, G and Maroney, M J and Geesey, G G and Lovley, D R}
}
@article {594,
	title = {Reductive precipitation of gold by dissimilatory Fe(III)-reducing bacteria and archaea.},
	journal = {Appl Environ Microbiol},
	volume = {67},
	year = {2001},
	month = {2001 Jul},
	pages = {3275-9},
	abstract = {Studies with a diversity of hyperthermophilic and mesophilic dissimilatory Fe(III)-reducing Bacteria and Archaea demonstrated that some of these organisms are capable of precipitating gold by reducing Au(III) to Au(0) with hydrogen as the electron donor. These studies suggest that models for the formation of gold deposits in both hydrothermal and cooler environments should consider the possibility that dissimilatory metal-reducing microorganisms can reductively precipitate gold from solution.},
	keywords = {Archaea, Bacteria, Chemical Precipitation, Ferric Compounds, Gold, Oxidation-Reduction},
	issn = {0099-2240},
	doi = {10.1128/AEM.67.7.3275-3279.2001},
	author = {Kashefi, K and Tor, J M and Nevin, K P and 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 {613,
	title = {Characterization of a membrane-bound NADH-dependent Fe(3+) reductase from the dissimilatory Fe(3+)-reducing bacterium Geobacter sulfurreducens.},
	journal = {FEMS Microbiol Lett},
	volume = {185},
	year = {2000},
	month = {2000 Apr 15},
	pages = {205-11},
	abstract = {Geobacter sulfurreducens produces a single, membrane-associated Fe(3+) reductase activity when grown on fumarate or Fe(3+). The activity was initially isolated by solubilization of membranes with the non-ionic detergent dodecyl-beta-D-maltoside, and partially purified by a combination of ion exchange chromatography and preparative non-denaturing gel electrophoresis. Molecular mass of the reductase, as determined by gel filtration chromatography, was approximately 300 kDa. Cofactor analysis of the purified reductase demonstrates that it contains a hemoprotein and flavin adenine dinucleotide. Kinetic and inhibitor studies show that the reductase is specific for NADH as electron donor, and confirm that the reductase enzymatically reduces Fe(3+). The cytochrome associated with the complex undergoes a reoxidation upon addition of Fe(3+) compounds, indicating an ability to pass reducing equivalents to Fe(3+). This is the first description of a purified NADH-dependent Fe(3+) reductase from a microorganism capable of coupling Fe(3+) reduction to growth.},
	keywords = {Cell Membrane, Deltaproteobacteria, Ferric Compounds, FMN Reductase, NADH, NADPH Oxidoreductases, Oxidation-Reduction},
	issn = {0378-1097},
	author = {Magnuson, T S and Hodges-Myerson, A L and Lovley, D R}
}
@article {607,
	title = {Direct and Fe(II)-mediated reduction of technetium by Fe(III)-reducing bacteria.},
	journal = {Appl Environ Microbiol},
	volume = {66},
	year = {2000},
	month = {2000 Sep},
	pages = {3743-9},
	abstract = {The dissimilatory Fe(III)-reducing bacterium Geobacter sulfurreducens reduced and precipitated Tc(VII) by two mechanisms. Washed cell suspensions coupled the oxidation of hydrogen to enzymatic reduction of Tc(VII) to Tc(IV), leading to the precipitation of TcO(2) at the periphery of the cell. An indirect, Fe(II)-mediated mechanism was also identified. Acetate, although not utilized efficiently as an electron donor for direct cell-mediated reduction of technetium, supported the reduction of Fe(III), and the Fe(II) formed was able to transfer electrons abiotically to Tc(VII). Tc(VII) reduction was comparatively inefficient via this indirect mechanism when soluble Fe(III) citrate was supplied to the cultures but was enhanced in the presence of solid Fe(III) oxide. The rate of Tc(VII) reduction was optimal, however, when Fe(III) oxide reduction was stimulated by the addition of the humic analog and electron shuttle anthaquinone-2,6-disulfonate, leading to the rapid formation of the Fe(II)-bearing mineral magnetite. Under these conditions, Tc(VII) was reduced and precipitated abiotically on the nanocrystals of biogenic magnetite as TcO(2) and was removed from solution to concentrations below the limit of detection by scintillation counting. Cultures of Fe(III)-reducing bacteria enriched from radionuclide-contaminated sediment using Fe(III) oxide as an electron acceptor in the presence of 25 microM Tc(VII) contained a single Geobacter sp. detected by 16S ribosomal DNA analysis and were also able to reduce and precipitate the radionuclide via biogenic magnetite. Fe(III) reduction was stimulated in aquifer material, resulting in the formation of Fe(II)-containing minerals that were able to reduce and precipitate Tc(VII). These results suggest that Fe(III)-reducing bacteria may play an important role in immobilizing technetium in sediments via direct and indirect mechanisms.},
	keywords = {Culture Media, Deltaproteobacteria, Ferric Compounds, Ferrous Compounds, Fresh Water, Oxidation-Reduction, Technetium},
	issn = {0099-2240},
	author = {Lloyd, J R and Sole, V A and Van Praagh, C V and Lovley, D R}
}
@article {611,
	title = {Lack of production of electron-shuttling compounds or solubilization of Fe(III) during reduction of insoluble Fe(III) oxide by Geobacter metallireducens.},
	journal = {Appl Environ Microbiol},
	volume = {66},
	year = {2000},
	month = {2000 May},
	pages = {2248-51},
	abstract = {Studies with the dissimilatory Fe(III)-reducing microorganism Geobacter metallireducens demonstrated that the common technique of separating Fe(III)-reducing microorganisms and Fe(III) oxides with semipermeable membranes in order to determine whether the Fe(III) reducers release electron-shuttling compounds and/or Fe(III) chelators is invalid. This raised doubts about the mechanisms for Fe(III) oxide reduction by this organism. However, several experimental approaches indicated that G. metallireducens does not release electron-shuttling compounds and does not significantly solubilize Fe(III) during Fe(III) oxide reduction. These results suggest that G. metallireducens directly reduces insoluble Fe(III) oxide.},
	keywords = {Deltaproteobacteria, Electron Transport, Ferric Compounds, Iron, Kinetics, Oxidation-Reduction, Solubility},
	issn = {0099-2240},
	author = {Nevin, K P and Lovley, D R}
}
@article {604,
	title = {N2-dependent growth and nitrogenase activity in the metal-metabolizing bacteria, Geobacter and Magnetospirillum species.},
	journal = {Environ Microbiol},
	volume = {2},
	year = {2000},
	month = {2000 Jun},
	pages = {266-73},
	abstract = {Cells of Geobacter metallireducens, Magnetospirillum strain AMB-1, Magnetospirillum magnetotacticum and Magnetospirillum gryphiswaldense showed N2-dependent growth, the first anaerobically with Fe(III) as the electron acceptor, and the latter three species microaerobically in semi-solid oxygen gradient cultures. Cells of the Magnetospirillum species grown with N2 under microaerobic conditions were magnetotactic and therefore produced magnetosomes. Cells of Geobacter metallireducens reduced acetylene to ethylene (11.5+/-5.9 nmol C2H4 produced min(-1) mg(-1) cell protein) while growing with Fe(III) as the electron acceptor in anaerobic growth medium lacking a fixed nitrogen source. Cells of the Magnetospirillum species, grown in a semi-solid oxygen gradient medium, also reduced acetylene at comparable rates. Uncut chromosomal and fragments from endonuclease-digested chromosomal DNA from these species, as well as Geobacter sulphurreducens organisms, hybridized with a nifHDK probe from Rhodospirillum rubrum, indicating the presence of these nitrogenase structural genes in these organisms. The evidence presented here shows that members of the metal-metabolizing genera, Geobacter and Magnetospirillum, fix atmospheric dinitrogen.},
	keywords = {Acetylene, DNA, Bacterial, Ethylenes, Genes, Bacterial, Iron, Nitrogen Fixation, Nitrogenase, Oxidation-Reduction, Oxidoreductases, Proteobacteria, Rhodospirillaceae},
	issn = {1462-2912},
	author = {Bazylinski, D A and Dean, A J and Sch{\"u}ler, D and Phillips, E J and Lovley, D R}
}
@article {614,
	title = {Reduction of Fe(III), Mn(IV), and toxic metals at 100 degrees C by Pyrobaculum islandicum.},
	journal = {Appl Environ Microbiol},
	volume = {66},
	year = {2000},
	month = {2000 Mar},
	pages = {1050-6},
	abstract = {It has recently been noted that a diversity of hyperthermophilic microorganisms have the ability to reduce Fe(III) with hydrogen as the electron donor, but the reduction of Fe(III) or other metals by these organisms has not been previously examined in detail. When Pyrobaculum islandicum was grown at 100 degrees C in a medium with hydrogen as the electron donor and Fe(III)-citrate as the electron acceptor, the increase in cell numbers of P. islandicum per mole of Fe(III) reduced was found to be ca. 10-fold higher than previously reported. Poorly crystalline Fe(III) oxide could also serve as the electron acceptor for growth on hydrogen. The stoichiometry of hydrogen uptake and Fe(III) oxide reduction was consistent with the oxidation of 1 mol of hydrogen resulting in the reduction of 2 mol of Fe(III). The poorly crystalline Fe(III) oxide was reduced to extracellular magnetite. P. islandicum could not effectively reduce the crystalline Fe(III) oxide minerals goethite and hematite. In addition to using hydrogen as an electron donor for Fe(III) reduction, P. islandicum grew via Fe(III) reduction in media in which peptone and yeast extract served as potential electron donors. The closely related species P. aerophilum grew via Fe(III) reduction in a similar complex medium. Cell suspensions of P. islandicum reduced the following metals with hydrogen as the electron donor: U(VI), Tc(VII), Cr(VI), Co(III), and Mn(IV). The reduction of these metals was dependent upon the presence of cells and hydrogen. The metalloids arsenate and selenate were not reduced. U(VI) was reduced to the insoluble U(IV) mineral uraninite, which was extracellular. Tc(VII) was reduced to insoluble Tc(IV) or Tc(V). Cr(VI) was reduced to the less toxic, less soluble Cr(III). Co(III) was reduced to Co(II). Mn(IV) was reduced to Mn(II) with the formation of manganese carbonate. These results demonstrate that biological reduction may contribute to the speciation of metals in hydrothermal environments and could account for such phenomena as magnetite accumulation and the formation of uranium deposits at ca. 100 degrees C. Reduction of toxic metals with hyperthermophilic microorganisms or their enzymes might be applied to the remediation of metal-contaminated waters or waste streams.},
	keywords = {Chromium, Cobalt, Energy Metabolism, Ferric Compounds, Geological Phenomena, Geology, Iron, Manganese, Metals, Heavy, Oxidation-Reduction, Technetium, Thermoproteaceae, Uranium, Water Pollutants, Chemical},
	issn = {0099-2240},
	author = {Kashefi, K and Lovley, D R}
}
@article {616,
	title = {Geothrix fermentans gen. nov., sp. nov., a novel Fe(III)-reducing bacterium from a hydrocarbon-contaminated aquifer.},
	journal = {Int J Syst Bacteriol},
	volume = {49 Pt 4},
	year = {1999},
	month = {1999 Oct},
	pages = {1615-22},
	abstract = {In an attempt to understand better the micro-organisms involved in anaerobic degradation of aromatic hydrocarbons in the Fe(III)-reducing zone of petroleum-contaminated aquifers, Fe(III)-reducing micro-organisms were isolated from contaminated aquifer material that had been adapted for rapid oxidation of toluene coupled to Fe(III) reduction. One of these organisms, strain H-5T, was enriched and isolated on acetate/Fe(III) medium. Strain H-5T is a Gram-negative strict anaerobe that grows with various simple organic acids such as acetate, propionate, lactate and fumarate as alternative electron donors with Fe(III) as the electron acceptor. In addition, strain H-5T also oxidizes long-chain fatty acids such as palmitate with Fe(III) as the sole electron acceptor. Strain H-5T can also grow by fermentation of citrate or fumarate in the absence of an alternative electron acceptor. The primary end-products of citrate fermentation are acetate and succinate. In addition to various forms of soluble and insoluble Fe(III), strain H-5T grows with nitrate, Mn(IV), fumarate and the humic acid analogue 2,6-anthraquinone disulfonate as alternative electron acceptors. As with other organisms that can oxidize organic compounds completely with the reduction of Fe(III), cell suspensions of strain H-5T have absorbance maxima indicative of a c-type cytochrome(s). It is proposed that strain H-5T represents a novel genus in the Holophaga-Acidobacterium phylum and that it should be named Geothrix fermentans sp. nov., gen. nov.},
	keywords = {Biodegradation, Environmental, DNA, Bacterial, DNA, Ribosomal, Ferric Compounds, Geologic Sediments, Gram-Negative Anaerobic Bacteria, Molecular Sequence Data, Oxidation-Reduction, Petroleum, Phylogeny, RNA, Ribosomal, 16S, Water Microbiology, Water Pollutants, Chemical, Water Supply},
	issn = {0020-7713},
	author = {Coates, J D and Ellis, D J and Gaw, C V and Lovley, D R}
}
@article {619,
	title = {Microbial communities associated with anaerobic benzene degradation in a petroleum-contaminated aquifer.},
	journal = {Appl Environ Microbiol},
	volume = {65},
	year = {1999},
	month = {1999 Jul},
	pages = {3056-63},
	abstract = {Microbial community composition associated with benzene oxidation under in situ Fe(III)-reducing conditions in a petroleum-contaminated aquifer located in Bemidji, Minn., was investigated. Community structure associated with benzene degradation was compared to sediment communities that did not anaerobically oxidize benzene which were obtained from two adjacent Fe(III)-reducing sites and from methanogenic and uncontaminated zones. Denaturing gradient gel electrophoresis of 16S rDNA sequences amplified with bacterial or Geobacteraceae-specific primers indicated significant differences in the composition of the microbial communities at the different sites. Most notable was a selective enrichment of microorganisms in the Geobacter cluster seen in the benzene-degrading sediments. This finding was in accordance with phospholipid fatty acid analysis and most-probable-number-PCR enumeration, which indicated that members of the family Geobacteraceae were more numerous in these sediments. A benzene-oxidizing Fe(III)-reducing enrichment culture was established from benzene-degrading sediments and contained an organism closely related to the uncultivated Geobacter spp. This genus contains the only known organisms that can oxidize aromatic compounds with the reduction of Fe(III). Sequences closely related to the Fe(III) reducer Geothrix fermentans and the aerobe Variovorax paradoxus were also amplified from the benzene-degrading enrichment and were present in the benzene-degrading sediments. However, neither G. fermentans nor V. paradoxus is known to oxidize aromatic compounds with the reduction of Fe(III), and there was no apparent enrichment of these organisms in the benzene-degrading sediments. These results suggest that Geobacter spp. play an important role in the anaerobic oxidation of benzene in the Bemidji aquifer and that molecular community analysis may be a powerful tool for predicting a site{\textquoteright}s capacity for anaerobic benzene degradation.},
	keywords = {Anaerobiosis, Benzene, Biodegradation, Environmental, Culture Media, DNA, Bacterial, DNA, Ribosomal, Fresh Water, Geologic Sediments, Gram-Negative Anaerobic Bacteria, Molecular Sequence Data, Oxidation-Reduction, Petroleum, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Water Pollutants},
	issn = {0099-2240},
	author = {Rooney-Varga, J N and Anderson, R T and Fraga, J L and Ringelberg, D and Lovley, D R}
}
@article {617,
	title = {Role of humic-bound iron as an electron transfer agent in dissimilatory Fe(III) reduction.},
	journal = {Appl Environ Microbiol},
	volume = {65},
	year = {1999},
	month = {1999 Sep},
	pages = {4252-4},
	abstract = {The dissimilatory Fe(III) reducer Geobacter metallireducens reduced Fe(III) bound in humic substances, but the concentrations of Fe(III) in a wide range of highly purified humic substances were too low to account for a significant portion of the electron-accepting capacities of the humic substances. Furthermore, once reduced, the iron in humic substances could not transfer electrons to Fe(III) oxide. These results suggest that other electron-accepting moieties in humic substances, such as quinones, are the important electron-accepting and shuttling agents under Fe(III)-reducing conditions.},
	keywords = {Deltaproteobacteria, Electron Transport, Ferric Compounds, Humic Substances, Iron, Oxidation-Reduction},
	issn = {0099-2240},
	author = {Lovley, D R and Blunt-Harris, E L}
}
@article {618,
	title = {Sulfurospirillum barnesii sp. nov. and Sulfurospirillum arsenophilum sp. nov., new members of the Sulfurospirillum clade of the epsilon Proteobacteria.},
	journal = {Int J Syst Bacteriol},
	volume = {49 Pt 3},
	year = {1999},
	month = {1999 Jul},
	pages = {1177-80},
	abstract = {Two strains of dissimilatory arsenate-reducing vibrio-shaped bacteria are assigned to the genus Sulfurospirillum. These two new species, Sulfurospirillum barnesii strain SES-3T and Sulfurospirillum arsenophilum strain MIT-13T, in addition to Sulfurospirillum sp. SM-5, two strains of Sulfurospirillum deleyianum, and Sulfurospirillum arcachonense, form a distinct clade within the epsilon subclass of the Proteobacteria based on 16S rRNA analysis.},
	keywords = {Arsenates, Bacterial Typing Techniques, DNA, Ribosomal, Genes, rRNA, Gram-Negative Bacteria, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Selenium Compounds, Sequence Analysis, DNA},
	issn = {0020-7713},
	author = {Stolz, J F and Ellis, D J and Blum, J S and Ahmann, D and Lovley, D R and Oremland, R S}
}
@article {626,
	title = {Anaerobic benzene degradation in petroleum-contaminated aquifer sediments after inoculation with a benzene-oxidizing enrichment.},
	journal = {Appl Environ Microbiol},
	volume = {64},
	year = {1998},
	month = {1998 Feb},
	pages = {775-8},
	abstract = {Sediments from the sulfate-reduction zone of a petroleum-contaminated aquifer, in which benzene persisted, were inoculated with a benzene-oxidizing, sulfate-reducing enrichment from aquatic sediments. Benzene was degraded, with apparent growth of the benzene-degrading population over time. These results suggest that the lack of benzene degradation in the sulfate-reduction zones of some aquifers may result from the failure of the appropriate benzene-degrading sulfate reducers to colonize the aquifers rather than from environmental conditions that are adverse for anaerobic benzene degradation.},
	keywords = {Anaerobiosis, Benzene, Biodegradation, Environmental, Fresh Water, Geologic Sediments, Iron, Oxidation-Reduction, Petroleum, Sulfates},
	issn = {0099-2240},
	author = {Weiner, JM and Lovley, D R}
}
@article {622,
	title = {Humic acids as electron acceptors for anaerobic microbial oxidation of vinyl chloride and dichloroethene.},
	journal = {Appl Environ Microbiol},
	volume = {64},
	year = {1998},
	month = {1998 Aug},
	pages = {3102-5},
	abstract = {Anaerobic oxidation of [1,2-14C]vinyl chloride and [1, 2-14C]dichloroethene to 14CO2 under humic acid-reducing conditions was demonstrated. The results indicate that waterborne contaminants can be oxidized by using humic acid compounds as electron acceptors and suggest that natural aquatic systems have a much larger capacity for contaminant oxidation than previously thought.},
	keywords = {Aerobiosis, Anaerobiosis, Bacteria, Biodegradation, Environmental, Geologic Sediments, Humic Substances, Oxidation-Reduction, Vinyl Chloride, Water Microbiology, Water Pollutants},
	issn = {0099-2240},
	author = {Bradley, P M and Chapelle, F H and Lovley, D R}
}
@article {620,
	title = {Microbiological evidence for Fe(III) reduction on early Earth.},
	journal = {Nature},
	volume = {395},
	year = {1998},
	month = {1998 Sep 3},
	pages = {65-7},
	abstract = {It is generally considered that sulphur reduction was one of the earliest forms of microbial respiration, because the known microorganisms that are most closely related to the last common ancestor of modern life are primarily anaerobic, sulphur-reducing hyperthermophiles. However, geochemical evidence indicates that Fe(III) is more likely than sulphur to have been the first external electron acceptor of global significance in microbial metabolism. Here we show that Archaea and Bacteria that are most closely related to the last common ancestor can reduce Fe(III) to Fe(II) and conserve energy to support growth from this respiration. Surprisingly, even Thermotoga maritima, previously considered to have only a fermentative metabolism, could grow as a respiratory organism when Fe(III) was provided as an electron acceptor. These results provide microbiological evidence that Fe(III) reduction could have been an important process on early Earth and suggest that microorganisms might contribute to Fe(III) reduction in modern hot biospheres. Furthermore, our discovery that hyperthermophiles that had previously been thought to require sulphur for cultivation can instead be grown without the production of toxic and corrosive sulphide, should aid biochemical investigations of these poorly understood organisms.},
	keywords = {Earth (Planet), Electron Transport, Environmental Microbiology, Ferric Compounds, Gram-Negative Anaerobic Bacteria, Oxidation-Reduction, Thermoproteaceae},
	issn = {0028-0836},
	doi = {10.1038/25720},
	author = {Vargas, M and Kashefi, K and Blunt-Harris, E L and Lovley, D R}
}
@article {628,
	title = {Anaerobic degradation of polycyclic aromatic hydrocarbons and alkanes in petroleum-contaminated marine harbor sediments.},
	journal = {Appl Environ Microbiol},
	volume = {63},
	year = {1997},
	month = {1997 Sep},
	pages = {3589-93},
	abstract = {Although polycyclic aromatic hydrocarbons (PAHs) have usually been found to persist under strict anaerobic conditions, in a previous study an unusual site was found in San Diego Bay in which two PAHs, naphthalene and phenanthrene, were oxidized to carbon dioxide under sulfate-reducing conditions. Further investigations with these sediments revealed that methylnaphthalene, fluorene, and fluoranthene were also anaerobically oxidized to carbon dioxide in these sediments, while pyrene and benzo[a]pyrene were not. Studies with naphthalene indicated that PAH oxidation was sulfate dependent. Incubating the sediments with additional naphthalene for 1 month resulted in a significant increase in the oxidation of [14C]naphthalene. In sediments from a less heavily contaminated site in San diego Bay where PAHs were not readily degraded, naphthalene degradation could be stimulated through inoculation with active PAH-degrading sediments from the most heavily contaminated site. Sediments from the less heavily contaminated site that had been adapted for rapid anaerobic degradation of high concentrations of benzene did not oxidize naphthalene, suggesting that the benzene- and naphthalene-degrading populations were different. When fuels containing complex mixtures of alkanes were added to sediments from the two sites, there was significant degradation in the alkanes. [14C]hexadecane was also anaerobically oxidized to 14CO2 in these sediments. Molybdate, a specific inhibitor of sulfate reduction, inhibited hexadecane oxidation. These results demonstrate that a wide variety of hydrocarbon contaminants can be degraded under sulfate-reducing conditions in hydrocarbon-contaminated sediments, and they suggest that it may be possible to use sulfate reduction rather than aerobic respiration as a treatment strategy for hydrocarbon-contaminated dredged sediments.},
	keywords = {Alkanes, Anaerobiosis, Biodegradation, Environmental, California, Naphthalenes, Oxidation-Reduction, Petroleum, Polycyclic Hydrocarbons, Aromatic, Sulfates, Water Microbiology, Water Pollutants, Chemical},
	issn = {0099-2240},
	author = {Coates, J D and Woodward, J and Allen, J and Philp, P and Lovley, D R}
}
@article {629,
	title = {Bioremediation of metal contamination.},
	journal = {Curr Opin Biotechnol},
	volume = {8},
	year = {1997},
	month = {1997 Jun},
	pages = {285-9},
	abstract = {Recent studies have demonstrated that microbes might be used to remediate metal contamination by removing metals from contaminated water or waste streams, sequestering metals in soils and sediments or solubilizing metals to aid in their extraction. This is primarily accomplished either by biosorption of metals or enzymatically catalyzed changes in the metal redox state. Bioremediation of metals is still primarily a research problem with little large-scale application of this technology.},
	keywords = {Adsorption, Bacteria, Biomass, Biotechnology, Environmental Pollutants, Metals, Oxidation-Reduction},
	issn = {0958-1669},
	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 {641,
	title = {Bioremediation of organic and metal contaminants with dissimilatory metal reduction.},
	journal = {J Ind Microbiol},
	volume = {14},
	year = {1995},
	month = {1995 Feb},
	pages = {85-93},
	abstract = {Dissimilatory metal reduction has the potential to be a helpful mechanism for both intrinsic and engineered bioremediation of contaminated environments. Dissimilatory Fe(III) reduction is an important intrinsic process for removing organic contaminants from aquifers contaminated with petroleum or landfill leachate. Stimulation of microbial Fe(III) reduction can enhance the degradation of organic contaminants in ground water. Dissimilatory reduction of uranium, selenium, chromium, technetium, and possibly other metals, can convert soluble metal species to insoluble forms that can readily be removed from contaminated waters or waste streams. Reduction of mercury can volatilize mercury from waters and soils. Despite its potential, there has as yet been limited applied research into the use of dissimilatory metal reduction as a bioremediation tool.},
	keywords = {Bacteria, Biodegradation, Environmental, Chromium, Hydrocarbons, Iron, Mercury, Metals, Oxidation-Reduction, Selenium, Uranium},
	issn = {0169-4146},
	author = {Lovley, D R}
}
@article {637,
	title = {Desulfuromonas palmitatis sp. nov., a marine dissimilatory Fe(III) reducer that can oxidize long-chain fatty acids.},
	journal = {Arch Microbiol},
	volume = {164},
	year = {1995},
	month = {1995 Dec},
	pages = {406-13},
	abstract = {Studies on the microorganisms living in hydrocarbon-contaminated sediments in San Diego Bay, California led to the isolation of a novel Fe(III)-reducing microorganism. This organism, designated strain SDBY1, was an obligately anaerobic, non-motile, non-flagellated, gram-negative rod. Strain SDBY1 conserves energy to support growth from the oxidation of acetate, lactate, succinate, fumarate, laurate, palmitate, or stearate. H2 was also oxidized with the reduction of Fe(III), but growth with H2 as the sole electron donor was not observed. In addition to various forms of soluble and insoluble Fe(III), strain SDBY1 also coupled growth to the reduction of fumarate, Mn(IV), or S0. Air-oxidized minus dithionite-reduced difference spectra exhibited peaks at 552.8, 523.6, and 422.8 nm, indicative of c-type cytochrome(s). Strain SDBY1 shares physiological characteristics with organisms in the genera Geobacter, Pelobacter, and Desulfuromonas. Detailed analysis of the 16S rRNA sequence indicated that strain SDBY1 should be placed in the genus Desulfuromonas. The new species name Desulfuromonas palmitatis is proposed. D. palmitatis is only the second marine organism found (after D. acetoxidans) to oxidize multicarbon organic compounds completely to carbon dioxide with Fe(III) as an electron acceptor and provides the first pure culture model for the oxidation of long-chain fatty acids coupled to Fe(III) reduction.},
	keywords = {Electron Transport, Fatty Acids, Gram-Negative Anaerobic Bacteria, Iron, Microscopy, Electron, Scanning, Oxidation-Reduction, Phylogeny, RNA, Bacterial, RNA, Ribosomal, 16S, Water Microbiology},
	issn = {0302-8933},
	author = {Coates, J D and Lonergan, D J and Philips, E J and Jenter, H 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}
}
@article {642,
	title = {Geobacter sulfurreducens sp. nov., a hydrogen- and acetate-oxidizing dissimilatory metal-reducing microorganism.},
	journal = {Appl Environ Microbiol},
	volume = {60},
	year = {1994},
	month = {1994 Oct},
	pages = {3752-9},
	abstract = {A dissimilatory metal- and sulfur-reducing microorganism was isolated from surface sediments of a hydrocarbon-contaminated ditch in Norman, Okla. The isolate, which was designated strain PCA, was an obligately anaerobic, nonfermentative nonmotile, gram-negative rod. PCA grew in a defined medium with acetate as an electron donor and ferric PPi, ferric oxyhydroxide, ferric citrate, elemental sulfur, Co(III)-EDTA, fumarate, or malate as the sole electron acceptor. PCA also coupled the oxidation of hydrogen to the reduction of Fe(III) but did not reduce Fe(III) with sulfur, glucose, lactate, fumarate, propionate, butyrate, isobutyrate, isovalerate, succinate, yeast extract, phenol, benzoate, ethanol, propanol, or butanol as an electron donor. PCA did not reduce oxygen, Mn(IV), U(VI), nitrate, sulfate, sulfite, or thiosulfate with acetate as the electron donor. Cell suspensions of PCA exhibited dithionite-reduced minus air-oxidized difference spectra which were characteristic of c-type cytochromes. Phylogenetic analysis of the 16S rRNA sequence placed PCA in the delta subgroup of the proteobacteria. Its closest known relative is Geobacter metallireducens. The ability to utilize either hydrogen or acetate as the sole electron donor for Fe(III) reduction makes strain PCA a unique addition to the relatively small group of respiratory metal-reducing microorganisms available in pure culture. A new species name, Geobacter sulfurreducens, is proposed.},
	keywords = {Acetic Acid, Acetic Acids, Base Sequence, DNA Primers, DNA, Bacterial, DNA, Ribosomal, Electron Transport, Gram-Negative Anaerobic Bacteria, Hydrogen, Metals, Microscopy, Electron, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Bacterial, RNA, Ribosomal, 16S, Soil Microbiology},
	issn = {0099-2240},
	author = {Caccavo, F and Lonergan, D J and Lovley, D R and Davis, M and Stolz, J F and McInerney, M J}
}
@article {643,
	title = {Stimulated anoxic biodegradation of aromatic hydrocarbons using Fe(III) ligands.},
	journal = {Nature},
	volume = {370},
	year = {1994},
	month = {1994 Jul 14},
	pages = {128-31},
	abstract = {Contamination of ground waters with water-soluble aromatic hydrocarbons, common components of petroleum pollution, often produces anoxic conditions under which microbial degradation of the aromatics is slow. Oxygen is often added to contaminated ground water to stimulate biodegradation, but this can be technically difficult and expensive. Insoluble Fe(III) oxides, which are generally abundant in shallow aquifers, are alternative potential oxidants, but are difficult for microorganisms to access. Here we report that adding organic ligands that bind to Fe(III) dramatically increases its bioavailability, and that in the presence of these ligands, rates of degradation of aromatic hydrocarbons in anoxic aquifer sediments are comparable to those in oxic sediments. We find that even benzene, which is notoriously refractory in the absence of oxygen, can be rapidly degraded. Our results suggest that increasing the bioavailability of Fe(III) by adding suitable ligands provides a potential alternative to oxygen addition for the bioremediation of petroleum-contaminated aquifers.},
	keywords = {Benzene, Biodegradation, Environmental, Ferric Compounds, Hydrocarbons, Ligands, Methane, Nitrilotriacetic Acid, Oxidation-Reduction, Toluene, Water Pollutants, Chemical},
	issn = {0028-0836},
	doi = {10.1038/370128a0},
	author = {Lovley, D R and Woodward, J C and Chapelle, F H}
}
@article {652,
	title = {Dissimilatory metal reduction.},
	journal = {Annu Rev Microbiol},
	volume = {47},
	year = {1993},
	month = {1993},
	pages = {263-90},
	abstract = {Microorganisms can enzymatically reduce a variety of metals in metabolic processes that are not related to metal assimilation. Some microorganisms can conserve energy to support growth by coupling the oxidation of simple organic acids and alcohols, H2, or aromatic compounds to the reduction of Fe(III) or Mn(IV). This dissimilatory Fe(III) and Mn(IV) reduction influences the organic as well as the inorganic geochemistry of anaerobic aquatic sediments and ground water. Microorganisms that use U(VI) as a terminal electron acceptor play an important role in uranium geochemistry and may be a useful tool for removing uranium from contaminated environments. Se(VI) serves as a terminal electron acceptor to support anaerobic growth of some microorganisms. Reduction of Se(VI) to Se(O) is an important mechanism for the precipitation of selenium from contaminated waters. Enzymatic reduction of Cr(VI) to the less mobile and less toxic Cr(III), and reduction of soluble Hg(II) to volatile Hg(O) may affect the fate of these compounds in the environment and might be used as a remediation strategy. Microorganisms can also enzymatically reduce other metals such as technetium, vanadium, molybdenum, gold, silver, and copper, but reduction of these metals has not been studied extensively.},
	keywords = {Bacteria, Metals, Oxidation-Reduction},
	issn = {0066-4227},
	doi = {10.1146/annurev.mi.47.100193.001403},
	author = {Lovley, D R}
}
@article {651,
	title = {Geobacter metallireducens gen. nov. sp. nov., a microorganism capable of coupling the complete oxidation of organic compounds to the reduction of iron and other metals.},
	journal = {Arch Microbiol},
	volume = {159},
	year = {1993},
	month = {1993},
	pages = {336-44},
	abstract = {The gram-negative metal-reducing microorganism, previously known as strain GS-15, was further characterized. This strict anaerobe oxidizes several short-chain fatty acids, alcohols, and monoaromatic compounds with Fe(III) as the sole electron acceptor. Furthermore, acetate is also oxidized with the reduction of Mn(IV), U(VI), and nitrate. In whole cell suspensions, the c-type cytochrome(s) of this organism was oxidized by physiological electron acceptors and also by gold, silver, mercury, and chromate. Menaquinone was recovered in concentrations comparable to those previously found in gram-negative sulfate reducers. Profiles of the phospholipid ester-linked fatty acids indicated that both the anaerobic desaturase and the branched pathways for fatty acid biosynthesis were operative. The organism contained three lipopolysaccharide hydroxy fatty acids which have not been previously reported in microorganisms, but have been observed in anaerobic freshwater sediments. The 16S rRNA sequence indicated that this organism belongs in the delta proteobacteria. Its closest known relative is Desulfuromonas acetoxidans. The name Geobacter metallireducens is proposed.},
	keywords = {Cytochrome c Group, Fatty Acids, Gram-Negative Anaerobic Bacteria, Iron, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S},
	issn = {0302-8933},
	author = {Lovley, D R and Giovannoni, S J and White, D C and Champine, J E and Phillips, E J and Gorby, Y A and Goodwin, S}
}
@article {647,
	title = {Reduction of uranium by cytochrome c3 of Desulfovibrio vulgaris.},
	journal = {Appl Environ Microbiol},
	volume = {59},
	year = {1993},
	month = {1993 Nov},
	pages = {3572-6},
	abstract = {The mechanism for U(VI) reduction by Desulfovibrio vulgaris (Hildenborough) was investigated. The H2-dependent U(VI) reductase activity in the soluble fraction of the cells was lost when the soluble fraction was passed over a cationic exchange column which extracted cytochrome c3. Addition of cytochrome c3 back to the soluble fraction that had been passed over the cationic exchange column restored the U(VI)-reducing capacity. Reduced cytochrome c3 was oxidized by U(VI), as was a c-type cytochrome(s) in whole-cell suspensions. When cytochrome c3 was combined with hydrogenase, its physiological electron donor, U(VI) was reduced in the presence of H2. Hydrogenase alone could not reduce U(VI). Rapid U(VI) reduction was followed by a subsequent slow precipitation of the U(IV) mineral uraninite. Cytochrome c3 reduced U(VI) in a uranium-contaminated surface water and groundwater. Cytochrome c3 provides the first enzyme model for the reduction and biomineralization of uranium in sedimentary environments. Furthermore, the finding that cytochrome c3 can catalyze the reductive precipitation of uranium may aid in the development of fixed-enzyme reactors and/or organisms with enhanced U(VI)-reducing capacity for the bioremediation of uranium-contaminated waters and waste streams.},
	keywords = {Biotransformation, Chemical Precipitation, Cytochrome c Group, Desulfovibrio vulgaris, Oxidation-Reduction, Uranium, Water Pollutants, Radioactive},
	issn = {0099-2240},
	author = {Lovley, D R and Widman, P K and Woodward, J C and Phillips, E J}
}
@article {654,
	title = {Acetate oxidation by dissimilatory Fe(III) reducers.},
	journal = {Appl Environ Microbiol},
	volume = {58},
	year = {1992},
	month = {1992 Sep},
	pages = {3205-8},
	keywords = {Acetates, Ferric Compounds, Gram-Negative Bacteria, Oxidation-Reduction},
	issn = {0099-2240},
	author = {Lovley, D R and Phillips, E J and Caccavo, F}
}
@article {655,
	title = {Reduction of uranium by Desulfovibrio desulfuricans.},
	journal = {Appl Environ Microbiol},
	volume = {58},
	year = {1992},
	month = {1992 Mar},
	pages = {850-6},
	abstract = {The possibility that sulfate-reducing microorganisms contribute to U(VI) reduction in sedimentary environments was investigated. U(VI) was reduced to U(IV) when washed cells of sulfate-grown Desulfovibrio desulfuricans were suspended in a bicarbonate buffer with lactate or H2 as the electron donor. There was no U(VI) reduction in the absence of an electron donor or when the cells were killed by heat prior to the incubation. The rates of U(VI) reduction were comparable to those in respiratory Fe(III)-reducing microorganisms. Azide or prior exposure of the cells to air did not affect the ability of D. desulfuricans to reduce U(VI). Attempts to grow D. desulfuricans with U(VI) as the electron acceptor were unsuccessful. U(VI) reduction resulted in the extracellular precipitation of the U(IV) mineral uraninite. The presence of sulfate had no effect on the rate of U(VI) reduction. Sulfate and U(VI) were reduced simultaneously. Enzymatic reduction of U(VI) by D. desulfuricans was much faster than nonenzymatic reduction of U(VI) by sulfide, even when cells of D. desulfuricans were added to provide a potential catalytic surface for the nonenzymatic reaction. The results indicate that enzymatic U(VI) reduction by sulfate-reducing microorganisms may be responsible for the accumulation of U(IV) in sulfidogenic environments. Furthermore, since the reduction of U(VI) to U(IV) precipitates uranium from solution, D. desulfuricans might be a useful organism for recovering uranium from contaminated waters and waste streams.},
	keywords = {Biodegradation, Environmental, Desulfovibrio, Kinetics, Oxidation-Reduction, Sulfates, Uranium, X-Ray Diffraction},
	issn = {0099-2240},
	author = {Lovley, D R and Phillips, E J}
}
@article {656,
	title = {Dissimilatory Fe(III) and Mn(IV) reduction.},
	journal = {Microbiol Rev},
	volume = {55},
	year = {1991},
	month = {1991 Jun},
	pages = {259-87},
	abstract = {The oxidation of organic matter coupled to the reduction of Fe(III) or Mn(IV) is one of the most important biogeochemical reactions in aquatic sediments, soils, and groundwater. This process, which may have been the first globally significant mechanism for the oxidation of organic matter to carbon dioxide, plays an important role in the oxidation of natural and contaminant organic compounds in a variety of environments and contributes to other phenomena of widespread significance such as the release of metals and nutrients into water supplies, the magnetization of sediments, and the corrosion of metal. Until recently, much of the Fe(III) and Mn(IV) reduction in sedimentary environments was considered to be the result of nonenzymatic processes. However, microorganisms which can effectively couple the oxidation of organic compounds to the reduction of Fe(III) or Mn(IV) have recently been discovered. With Fe(III) or Mn(IV) as the sole electron acceptor, these organisms can completely oxidize fatty acids, hydrogen, or a variety of monoaromatic compounds. This metabolism provides energy to support growth. Sugars and amino acids can be completely oxidized by the cooperative activity of fermentative microorganisms and hydrogen- and fatty-acid-oxidizing Fe(III) and Mn(IV) reducers. This provides a microbial mechanism for the oxidation of the complex assemblage of sedimentary organic matter in Fe(III)- or Mn(IV)-reducing environments. The available evidence indicates that this enzymatic reduction of Fe(III) or Mn(IV) accounts for most of the oxidation of organic matter coupled to reduction of Fe(III) and Mn(IV) in sedimentary environments. Little is known about the diversity and ecology of the microorganisms responsible for Fe(III) and Mn(IV) reduction, and only preliminary studies have been conducted on the physiology and biochemistry of this process.},
	keywords = {Bacteria, Electron Transport, Ferric Compounds, Fungi, Geological Phenomena, Geology, Manganese, Oxidation-Reduction, Soil Microbiology, Water Microbiology},
	issn = {0146-0749},
	author = {Lovley, D R}
}
