@article {3131, title = {A Geobacter sulfurreducens strain expressing pseudomonas aeruginosa type IV pili localizes OmcS on pili but is deficient in Fe(III) oxide reduction and current production.}, journal = {Appl Environ Microbiol}, volume = {80}, year = {2014}, month = {2014 Feb}, pages = {1219-24}, abstract = {

The conductive pili of Geobacter species play an important role in electron transfer to Fe(III) oxides, in long-range electron transport through current-producing biofilms, and in direct interspecies electron transfer. Although multiple lines of evidence have indicated that the pili of Geobacter sulfurreducens have a metal-like conductivity, independent of the presence of c-type cytochromes, this claim is still controversial. In order to further investigate this phenomenon, a strain of G. sulfurreducens, designated strain PA, was constructed in which the gene for the native PilA, the structural pilin protein, was replaced with the PilA gene of Pseudomonas aeruginosa PAO1. Strain PA expressed and properly assembled P. aeruginosa PilA subunits into pili and exhibited a profile of outer surface c-type cytochromes similar to that of a control strain expressing the G. sulfurreducens PilA. Surprisingly, the strain PA pili were decorated with the c-type cytochrome OmcS in a manner similar to the control strain. However, the strain PA pili were 14-fold less conductive than the pili of the control strain, and strain PA was severely impaired in Fe(III) oxide reduction and current production. These results demonstrate that the presence of OmcS on pili is not sufficient to confer conductivity to pili and suggest that there are unique structural features of the G. sulfurreducens PilA that are necessary for conductivity.

}, keywords = {Amino Acid Sequence, Cytochromes c, Electricity, Ferric Compounds, Fimbriae Proteins, Fimbriae, Bacterial, Geobacter, Methanosarcinaceae, Molecular Sequence Data, Oxidation-Reduction, Pseudomonas aeruginosa, Sequence Alignment}, issn = {1098-5336}, doi = {10.1128/AEM.02938-13}, author = {Liu, Xing and Tremblay, Pier-Luc and Malvankar, Nikhil S and Nevin, Kelly P and Lovley, Derek R and Vargas, Madeline} } @article {3135, title = {Sulfur oxidation to sulfate coupled with electron transfer to electrodes by Desulfuromonas strain TZ1.}, journal = {Microbiology (Reading)}, volume = {160}, year = {2014}, month = {2014 Jan}, pages = {123-129}, abstract = {

Microbial oxidation of elemental sulfur with an electrode serving as the electron acceptor is of interest because this may play an important role in the recovery of electrons from sulfidic wastes and for current production in marine benthic microbial fuel cells. Enrichments initiated with a marine sediment inoculum, with elemental sulfur as the electron donor and a positively poised (+300 mV versus Ag/AgCl) anode as the electron acceptor, yielded an anode biofilm with a diversity of micro-organisms, including Thiobacillus, Sulfurimonas, Pseudomonas, Clostridium and Desulfuromonas species. Further enrichment of the anode biofilm inoculum in medium with elemental sulfur as the electron donor and Fe(III) oxide as the electron acceptor, followed by isolation in solidified sulfur/Fe(III) medium yielded a strain of Desulfuromonas, designated strain TZ1. Strain TZ1 effectively oxidized elemental sulfur to sulfate with an anode serving as the sole electron acceptor, at rates faster than Desulfobulbus propionicus, the only other organism in pure culture previously shown to oxidize S{\textdegree} with current production. The abundance of Desulfuromonas species enriched on the anodes of marine benthic fuel cells has previously been interpreted as acetate oxidation driving current production, but the results presented here suggest that sulfur-driven current production is a likely alternative.

}, keywords = {Bioelectric Energy Sources, Desulfuromonas, DNA, Bacterial, Electricity, Electrodes, Geologic Sediments, Molecular Sequence Data, Oxidation-Reduction, Sequence Analysis, DNA, Sulfates, Sulfur}, issn = {1465-2080}, doi = {10.1099/mic.0.069930-0}, author = {Zhang, Tian and Bain, Timothy S and Barlett, Melissa A and Dar, Shabir A and Snoeyenbos-West, Oona L and Nevin, Kelly P and Lovley, Derek R} } @article {3155, title = {Anaerobic benzene oxidation by Geobacter species.}, journal = {Appl Environ Microbiol}, volume = {78}, year = {2012}, month = {2012 Dec}, pages = {8304-10}, abstract = {

The abundance of Geobacter species in contaminated aquifers in which benzene is anaerobically degraded has led to the suggestion that some Geobacter species might be capable of anaerobic benzene degradation, but this has never been documented. A strain of Geobacter, designated strain Ben, was isolated from sediments from the Fe(III)-reducing zone of a petroleum-contaminated aquifer in which there was significant capacity for anaerobic benzene oxidation. Strain Ben grew in a medium with benzene as the sole electron donor and Fe(III) oxide as the sole electron acceptor. Furthermore, additional evaluation of Geobacter metallireducens demonstrated that it could also grow in benzene-Fe(III) medium. In both strain Ben and G. metallireducens the stoichiometry of benzene metabolism and Fe(III) reduction was consistent with the oxidation of benzene to carbon dioxide with Fe(III) serving as the sole electron acceptor. With benzene as the electron donor, and Fe(III) oxide (strain Ben) or Fe(III) citrate (G. metallireducens) as the electron acceptor, the cell yields of strain Ben and G. metallireducens were 3.2 {\texttimes} 10(9) and 8.4 {\texttimes} 10(9) cells/mmol of Fe(III) reduced, respectively. Strain Ben also oxidized benzene with anthraquinone-2,6-disulfonate (AQDS) as the sole electron acceptor with cell yields of 5.9 {\texttimes} 10(9) cells/mmol of AQDS reduced. Strain Ben serves as model organism for the study of anaerobic benzene metabolism in petroleum-contaminated aquifers, and G. metallireducens is the first anaerobic benzene-degrading organism that can be genetically manipulated.

}, keywords = {Anaerobiosis, Benzene, Carbon Dioxide, Cluster Analysis, Culture Media, DNA, Bacterial, DNA, Ribosomal, Ferric Compounds, Geobacter, Groundwater, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Sequence Analysis, DNA}, issn = {1098-5336}, doi = {10.1128/AEM.02469-12}, author = {Zhang, Tian and Bain, Timothy S and Nevin, Kelly P and Barlett, Melissa A and Lovley, Derek R} } @article {462, title = {Anode biofilm transcriptomics reveals outer surface components essential for high density current production in Geobacter sulfurreducens fuel cells.}, journal = {PLoS One}, volume = {4}, year = {2009}, month = {2009}, pages = {e5628}, abstract = {The mechanisms by which Geobacter sulfurreducens transfers electrons through relatively thick (>50 microm) biofilms to electrodes acting as a sole electron acceptor were investigated. Biofilms of Geobacter sulfurreducens were grown either in flow-through systems with graphite anodes as the electron acceptor or on the same graphite surface, but with fumarate as the sole electron acceptor. Fumarate-grown biofilms were not immediately capable of significant current production, suggesting substantial physiological differences from current-producing biofilms. Microarray analysis revealed 13 genes in current-harvesting biofilms that had significantly higher transcript levels. The greatest increases were for pilA, the gene immediately downstream of pilA, and the genes for two outer c-type membrane cytochromes, OmcB and OmcZ. Down-regulated genes included the genes for the outer-membrane c-type cytochromes, OmcS and OmcT. Results of quantitative RT-PCR of gene transcript levels during biofilm growth were consistent with microarray results. OmcZ and the outer-surface c-type cytochrome, OmcE, were more abundant and OmcS was less abundant in current-harvesting cells. Strains in which pilA, the gene immediately downstream from pilA, omcB, omcS, omcE, or omcZ was deleted demonstrated that only deletion of pilA or omcZ severely inhibited current production and biofilm formation in current-harvesting mode. In contrast, these gene deletions had no impact on biofilm formation on graphite surfaces when fumarate served as the electron acceptor. These results suggest that biofilms grown harvesting current are specifically poised for electron transfer to electrodes and that, in addition to pili, OmcZ is a key component in electron transfer through differentiated G. sulfurreducens biofilms to electrodes.}, keywords = {Amino Acid Sequence, Bacterial Outer Membrane Proteins, Bioelectric Energy Sources, Biofilms, Cytochromes, Electrodes, Electron Transport, Fumarates, Gene Deletion, Gene Expression Profiling, Gene Expression Regulation, Bacterial, Genetic Complementation Test, Geobacter, Microscopy, Confocal, Molecular Sequence Data, Oligonucleotide Array Sequence Analysis, Oxidation-Reduction, RNA, Messenger, Up-Regulation}, issn = {1932-6203}, doi = {10.1371/journal.pone.0005628}, author = {Nevin, Kelly P and Kim, Byoung-Chan and Glaven, Richard H and Johnson, Jessica P and Woodard, Trevor L and Meth{\'e}, Barbara A and Didonato, Raymond J and Covalla, Sean F and Franks, Ashley E and Liu, Anna and Lovley, Derek R} } @article {483, title = {Genes for two multicopper proteins required for Fe(III) oxide reduction in Geobacter sulfurreducens have different expression patterns both in the subsurface and on energy-harvesting electrodes.}, journal = {Microbiology}, volume = {154}, year = {2008}, month = {2008 May}, pages = {1422-35}, abstract = {Previous studies have shown that Geobacter sulfurreducens requires the outer-membrane, multicopper protein OmpB for Fe(III) oxide reduction. A homologue of OmpB, designated OmpC, which is 36 \% similar to OmpB, has been discovered in the G. sulfurreducens genome. Deletion of ompC inhibited reduction of insoluble, but not soluble Fe(III). Analysis of multiple Geobacter and Pelobacter genomes, as well as in situ Geobacter, indicated that genes encoding multicopper proteins are conserved in Geobacter species but are not found in Pelobacter species. Levels of ompB transcripts were similar in G. sulfurreducens at different growth rates in chemostats and during growth on a microbial fuel cell anode. In contrast, ompC transcript levels increased at higher growth rates in chemostats and with increasing current production in fuel cells. Constant levels of Geobacter ompB transcripts were detected in groundwater during a field experiment in which acetate was added to the subsurface to promote in situ uranium bioremediation. In contrast, ompC transcript levels increased during the rapid phase of growth of Geobacter species following addition of acetate to the groundwater and then rapidly declined. These results demonstrate that more than one multicopper protein is required for optimal Fe(III) oxide reduction in G. sulfurreducens and suggest that, in environmental studies, quantifying OmpB/OmpC-related genes could help alleviate the problem that Pelobacter genes may be inadvertently quantified via quantitative analysis of 16S rRNA genes. Furthermore, comparison of differential expression of ompB and ompC may provide insight into the in situ metabolic state of Geobacter species in environments of interest.}, keywords = {Acetates, Amino Acid Sequence, Bacterial Outer Membrane Proteins, Electrodes, Ferric Compounds, Gene Deletion, Gene Expression Profiling, Geobacter, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, Sequence Alignment, Sequence Homology, Nucleic Acid, Soil Microbiology, Uranium}, issn = {1350-0872}, doi = {10.1099/mic.0.2007/014365-0}, author = {Holmes, Dawn E and Mester, T{\"u}nde and O{\textquoteright}Neil, Regina A and Perpetua, Lorrie A and Larrahondo, M Juliana and Glaven, Richard and Sharma, Manju L and Ward, Joy E and Nevin, Kelly P and Lovley, Derek R} } @article {508, title = {Geobacter pickeringii sp. nov., Geobacter argillaceus sp. nov. and Pelosinus fermentans gen. nov., sp. nov., isolated from subsurface kaolin lenses.}, journal = {Int J Syst Evol Microbiol}, volume = {57}, year = {2007}, month = {2007 Jan}, pages = {126-35}, abstract = {The goal of this project was to isolate representative Fe(III)-reducing bacteria from kaolin clays that may influence iron mineralogy in kaolin. Two novel dissimilatory Fe(III)-reducing bacteria, strains G12(T) and G13(T), were isolated from sedimentary kaolin strata in Georgia (USA). Cells of strains G12(T) and G13(T) were motile, non-spore-forming regular rods, 1-2 mum long and 0.6 mum in diameter. Cells had one lateral flagellum. Phylogenetic analyses using the 16S rRNA gene sequence of the novel strains demonstrated their affiliation to the genus Geobacter. Strain G12(T) was most closely related to Geobacter pelophilus (94.7 \%) and Geobacter chapellei (94.1 \%). Strain G13(T) was most closely related to Geobacter grbiciae (95.3 \%) and Geobacter metallireducens (95.1 \%). Based on phylogenetic analyses and phenotypic differences between the novel isolates and other closely related species of the genus Geobacter, the isolates are proposed as representing two novel species, Geobacter argillaceus sp. nov. (type strain G12(T)=ATCC BAA-1139(T)=JCM 12999(T)) and Geobacter pickeringii sp. nov. (type strain G13(T)=ATCC BAA-1140(T)=DSM 17153(T)=JCM 13000(T)). Another isolate, strain R7(T), was derived from a primary kaolin deposit in Russia. The cells of strain R7(T) were motile, spore-forming, slightly curved rods, 0.6 x 2.0-6.0 microm in size and with up to six peritrichous flagella. Strain R7(T) was capable of reducing Fe(III) only in the presence of a fermentable substrate. 16S rRNA gene sequence analysis demonstrated that this isolate is unique, showing less than 92 \% similarity to bacteria of the Sporomusa-Pectinatus-Selenomomas phyletic group, including {\textquoteright}Anaerospora hongkongensis{\textquoteright} (90.2 \%), Acetonema longum (90.6 \%), Dendrosporobacter quercicolus (90.9 \%) and Anaerosinus glycerini (91.5 \%). On the basis of phylogenetic analysis and physiological tests, strain R7(T) is proposed to represent a novel genus and species, Pelosinus fermentans gen. nov., sp. nov. (type strain R7(T)=DSM 17108(T)=ATCC BAA-1133(T)), in the Sporomusa-Pectinatus-Selenomonas group.}, keywords = {Bacterial Typing Techniques, Base Composition, DNA, Bacterial, DNA, Ribosomal, Ferric Compounds, Genes, rRNA, Geobacter, Geologic Sediments, Georgia, Kaolin, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Russia, Sequence Analysis, DNA, Species Specificity}, issn = {1466-5026}, doi = {10.1099/ijs.0.64221-0}, author = {Shelobolina, Evgenya S and Nevin, Kelly P and Blakeney-Hayward, Jessie D and Johnsen, Claudia V and Plaia, Todd W and Krader, Paul and Woodard, Trevor and Holmes, Dawn E and Vanpraagh, Catherine Gaw and Lovley, Derek R} } @article {504, title = {Prolixibacter bellariivorans gen. nov., sp. nov., a sugar-fermenting, psychrotolerant anaerobe of the phylum Bacteroidetes, isolated from a marine-sediment fuel cell.}, journal = {Int J Syst Evol Microbiol}, volume = {57}, year = {2007}, month = {2007 Apr}, pages = {701-7}, abstract = {A Gram-negative, non-motile, filamentous, rod-shaped, non-spore-forming bacterium (strain F2(T)) was isolated from the surface of an electricity-harvesting electrode incubated in marine sediments. Strain F2(T) does not contain c-type cytochromes, flexirubin or carotenoids. It is a facultative anaerobe that can ferment sugars by using a mixed acid fermentation pathway and it can grow over a wide range of temperatures (4-42 degrees C). The DNA G+C (44.9 mol\%) content and chemotaxonomic characteristics (major fatty acids, a-15 : 0 and 15 : 0) were consistent with those of species within the phylum Bacteroidetes. Phylogenetic analysis of the 16S rRNA nucleotide and elongation factor G amino acid sequences indicated that strain F2(T) represents a unique phylogenetic cluster within the phylum Bacteroidetes. On the basis of 16S rRNA gene sequence phylogeny, the closest relative available in pure culture, Alkaliflexus imshenetskii, is only 87.5 \% similar to strain F2(T). Results from physiological, biochemical and phylogenetic analyses showed that strain F2(T) should be classified as a novel genus and species within the phylum Bacteroidetes, for which the name Prolixibacter bellariivorans gen. nov., sp. nov. is proposed. The type strain is F2(T) (=ATCC BAA-1284(T)=JCM 13498(T)).}, keywords = {Bacteroidetes, Carbohydrate Metabolism, Cold Temperature, DNA, Bacterial, DNA, Ribosomal, Energy-Generating Resources, Geologic Sediments, Molecular Sequence Data, Phylogeny, RNA, Ribosomal, 16S, Seawater}, issn = {1466-5026}, doi = {10.1099/ijs.0.64296-0}, author = {Holmes, Dawn E and Nevin, Kelly P and Woodard, Trevor L and Peacock, Aaron D and Lovley, Derek R} } @article {493, title = {Subsurface clade of Geobacteraceae that predominates in a diversity of Fe(III)-reducing subsurface environments.}, journal = {ISME J}, volume = {1}, year = {2007}, month = {2007 Dec}, pages = {663-77}, abstract = {There are distinct differences in the physiology of Geobacter species available in pure culture. Therefore, to understand the ecology of Geobacter species in subsurface environments, it is important to know which species predominate. Clone libraries were assembled with 16S rRNA genes and transcripts amplified from three subsurface environments in which Geobacter species are known to be important members of the microbial community: (1) a uranium-contaminated aquifer located in Rifle, CO, USA undergoing in situ bioremediation; (2) an acetate-impacted aquifer that serves as an analog for the long-term acetate amendments proposed for in situ uranium bioremediation and (3) a petroleum-contaminated aquifer in which Geobacter species play a role in the oxidation of aromatic hydrocarbons coupled with the reduction of Fe(III). The majority of Geobacteraceae 16S rRNA sequences found in these environments clustered in a phylogenetically coherent subsurface clade, which also contains a number of Geobacter species isolated from subsurface environments. Concatamers constructed with 43 Geobacter genes amplified from these sites also clustered within this subsurface clade. 16S rRNA transcript and gene sequences in the sediments and groundwater at the Rifle site were highly similar, suggesting that sampling groundwater via monitoring wells can recover the most active Geobacter species. These results suggest that further study of Geobacter species in the subsurface clade is necessary to accurately model the behavior of Geobacter species during subsurface bioremediation of metal and organic contaminants.}, keywords = {Biodegradation, Environmental, Ecosystem, Ferric Compounds, Geobacter, Hydrocarbons, Aromatic, Molecular Sequence Data, Oxidation-Reduction, Petroleum, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Uranium}, issn = {1751-7362}, doi = {10.1038/ismej.2007.85}, author = {Holmes, Dawn E and O{\textquoteright}Neil, Regina A and Vrionis, Helen A and N{\textquoteright}guessan, Lucie A and Ortiz-Bernad, Irene and Larrahondo, Maria J and Adams, Lorrie A and Ward, Joy A and Nicoll, Julie S and Nevin, Kelly P and Chavan, Milind A and Johnson, Jessica P and Long, Philip E and Lovley, Derek R} } @article {532, title = {Geobacter bemidjiensis sp. nov. and Geobacter psychrophilus sp. nov., two novel Fe(III)-reducing subsurface isolates.}, journal = {Int J Syst Evol Microbiol}, volume = {55}, year = {2005}, month = {2005 Jul}, pages = {1667-74}, abstract = {Fe(III)-reducing isolates were recovered from two aquifers in which Fe(III) reduction is known to be important. Strain Bem(T) was enriched from subsurface sediments collected in Bemidji, MN, USA, near a site where Fe(III) reduction is important in aromatic hydrocarbon degradation. Strains P11, P35(T) and P39 were isolated from the groundwater of an aquifer in Plymouth, MA, USA, in which Fe(III) reduction is important because of long-term inputs of acetate as a highway de-icing agent to the subsurface. All four isolates were Gram-negative, slightly curved rods that grew best in freshwater media. Strains P11, P35(T) and P39 exhibited motility via means of monotrichous flagella. Analysis of the 16S rRNA and nifD genes indicated that all four strains are delta-proteobacteria and members of the Geobacter cluster of the Geobacteraceae. Differences in phenotypic and phylogenetic characteristics indicated that the four isolates represent two novel species within the genus Geobacter. All of the isolates coupled the oxidation of acetate to the reduction of Fe(III) [iron(III) citrate, amorphous iron(III) oxide, iron(III) pyrophosphate and iron(III) nitrilotriacetate]. All four strains utilized ethanol, lactate, malate, pyruvate and succinate as electron donors and malate and fumarate as electron acceptors. Strain Bem(T) grew fastest at 30 degrees C, whereas strains P11, P35(T) and P39 grew equally well at 17, 22 and 30 degrees C. In addition, strains P11, P35(T) and P39 were capable of growth at 4 degrees C. The names Geobacter bemidjiensis sp. nov. (type strain Bem(T)=ATCC BAA-1014(T)=DSM 16622(T)=JCM 12645(T)) and Geobacter psychrophilus sp. nov. (strains P11, P35(T) and P39; type strain P35(T)=ATCC BAA-1013(T)=DSM 16674(T)=JCM 12644(T)) are proposed.}, keywords = {Bacterial Proteins, Bacterial Typing Techniques, Cold Temperature, DNA, Bacterial, DNA, Ribosomal, Ferric Compounds, Fresh Water, Genes, rRNA, Geobacter, Geologic Sediments, Massachusetts, Minnesota, Molecular Sequence Data, Oxidation-Reduction, RNA, Ribosomal, 16S, Species Specificity, Water Supply}, issn = {1466-5026}, doi = {10.1099/ijs.0.63417-0}, author = {Nevin, Kelly P and Holmes, Dawn E and Woodard, Trevor L and Hinlein, Erich S and Ostendorf, David W and Lovley, Derek R} } @article {547, title = {Comparison of 16S rRNA, nifD, recA, gyrB, rpoB and fusA genes within the family Geobacteraceae fam. nov.}, journal = {Int J Syst Evol Microbiol}, volume = {54}, year = {2004}, month = {2004 Sep}, pages = {1591-9}, abstract = {The sequences of five conserved genes, in addition to the 16S rRNA gene, were investigated in 30 members of the Geobacteraceae fam. nov. All members of the Geobacteraceae examined contained nifD, suggesting that they are capable of nitrogen fixation, which may explain their ability to compete effectively in nitrogen-poor subsurface environments undergoing remediation for petroleum or metal contamination. The phylogenies predicted from rpoB, gyrB, fusA, recA and nifD were generally in agreement with the phylogeny predicted from 16S rRNA gene sequences. Furthermore, phylogenetic analysis of concatemers constructed from all five protein-coding genes corresponded closely with the 16S rRNA gene-based phylogeny. This study demonstrated that the Geobacteraceae is a phylogenetically coherent family within the delta-subclass of the Proteobacteria that is composed of three distinct phylogenetic clusters: Geobacter, Desulfuromonas and Desulfuromusa. The sequence data provided here will make it possible to discriminate better between physiologically distinct members of the Geobacteraceae, such as Pelobacter propionicus and Geobacter species, in geobacteraceae-dominated microbial communities and greatly expands the potential to identify geobacteraceae sequences in libraries of environmental genomic DNA.}, keywords = {Bacterial Proteins, Deltaproteobacteria, Desulfuromonas, DNA Gyrase, DNA, Bacterial, DNA, Ribosomal, DNA-Directed RNA Polymerases, Genes, Bacterial, Genes, rRNA, Geobacter, Molecular Sequence Data, Nitrogen Fixation, Peptide Elongation Factor G, Phylogeny, Rec A Recombinases, RNA, Bacterial, RNA, Ribosomal, 16S, Sequence Analysis, DNA}, issn = {1466-5026}, doi = {10.1099/ijs.0.02958-0}, author = {Holmes, Dawn E and Nevin, Kelly P and Lovley, Derek R} } @article {554, title = {Isolation, characterization, and U(VI)-reducing potential of a facultatively anaerobic, acid-resistant Bacterium from Low-pH, nitrate- and U(VI)-contaminated subsurface sediment and description of Salmonella subterranea sp. nov.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 May}, pages = {2959-65}, abstract = {A facultatively anaerobic, acid-resistant bacterium, designated strain FRCl, was isolated from a low-pH, nitrate- and U(VI)-contaminated subsurface sediment at site FW-024 at the Natural and Accelerated Bioremediation Research Field Research Center in Oak Ridge, Tenn. Strain FRCl was enriched at pH 4.5 in minimal medium with nitrate as the electron acceptor, hydrogen as the electron donor, and acetate as the carbon source. Clones with 16S ribosomal DNA (rDNA) sequences identical to the sequence of strain FRCl were also detected in a U(VI)-reducing enrichment culture derived from the same sediment. Cells of strain FRCl were gram-negative motile regular rods 2.0 to 3.4 micro m long and 0.7 to 0.9 microm in diameter. Strain FRCl was positive for indole production, by the methyl red test, and for ornithine decarboxylase; it was negative by the Voges-Proskauer test (for acetylmethylcarbinol production), for urea hydrolysis, for arginine dihydrolase, for lysine decarboxylase, for phenylalanine deaminase, for H(2)S production, and for gelatin hydrolysis. Strain FRCl was capable of using O(2), NO(3)(-), S(2)O(3)(2-), fumarate, and malate as terminal electron acceptors and of reducing U(VI) in the cell suspension. Analysis of the 16S rDNA sequence of the isolate indicated that this strain was 96.4\% similar to Salmonella bongori and 96.3\% similar to Enterobacter cloacae. Physiological and phylogenetic analyses suggested that strain FRCl belongs to the genus Salmonella and represents a new species, Salmonella subterranea sp. nov.}, keywords = {Anaerobiosis, Culture Media, DNA, Ribosomal, Fresh Water, Geologic Sediments, Hydrogen-Ion Concentration, Molecular Sequence Data, Nitrates, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Salmonella, Sequence Analysis, DNA, Uranium, Water Pollution, Chemical}, issn = {0099-2240}, author = {Shelobolina, Evgenya S and Sullivan, Sara A and O{\textquoteright}Neill, Kathleen R and Nevin, Kelly P and Lovley, Derek R} }