@article {3059, title = {Electromicrobiology: the ecophysiology of phylogenetically diverse electroactive microorganisms.}, journal = {Nat Rev Microbiol}, volume = {20}, year = {2022}, month = {2022 Jan}, pages = {5-19}, abstract = {

Electroactive microorganisms markedly affect many environments in which they establish outer-surface electrical contacts with other cells and minerals or reduce soluble extracellular redox-active molecules such as flavins and humic substances. A growing body of research emphasizes their broad phylogenetic diversity and shows that these microorganisms have key roles in multiple biogeochemical cycles, as well as the microbiome of the gut, anaerobic waste digesters and metal corrosion. Diverse bacteria and archaea have independently evolved cytochrome-based strategies for electron exchange between the outer cell surface and the cell interior, but cytochrome-free mechanisms are also prevalent. Electrically conductive protein filaments, soluble electron shuttles and non-biological conductive materials can substantially extend the electronic reach of microorganisms beyond the surface of the cell. The growing appreciation of the diversity of electroactive microorganisms and their unique electronic capabilities is leading to a broad range of applications.

}, keywords = {Archaea, Bacteria, Bacterial Physiological Phenomena, Cytochromes, Electron Transport, Oxidation-Reduction, Phylogeny}, issn = {1740-1534}, doi = {10.1038/s41579-021-00597-6}, author = {Lovley, Derek R and Holmes, Dawn E} } @article {3063, title = {Correlation of Key Physiological Properties of Isolates with Environment of Origin.}, journal = {Appl Environ Microbiol}, volume = {87}, year = {2021}, month = {2021 Jun 11}, pages = {e0073121}, abstract = {

It is known that the physiology of species can differ significantly, but the ecological impact of these differences is unclear. We recovered two strains of from two different ecosystems with a similar enrichment and isolation method. Both strains had the same ability to metabolize organic substrates and participate in direct interspecies electron transfer but also had major physiological differences. Strain DH-1, which was isolated from an anaerobic digester, used H as an electron donor. Genome analysis indicated that it lacks an Rnf complex and conserves energy from acetate metabolism via intracellular H cycling. In contrast, strain DH-2, a subsurface isolate, lacks hydrogenases required for H uptake and cycling and has an Rnf complex for energy conservation when growing on acetate. Further analysis of the genomes of previously described isolates, as well as phylogenetic and metagenomic data on uncultured in anaerobic digesters and diverse soils and sediments, revealed a physiological dichotomy that corresponded with environment of origin. The physiology of type I revolves around H production and consumption. In contrast, type II species eschew H and have genes for an Rnf complex and the multiheme, membrane-bound -type cytochrome MmcA, shown to be essential for extracellular electron transfer. The distribution of species in diverse environments suggests that the type I H-based physiology is well suited for high-energy environments, like anaerobic digesters, whereas type II Rnf/cytochrome-based physiology is an adaptation to the slower, steady-state carbon and electron fluxes common in organic-poor anaerobic soils and sediments. Biogenic methane is a significant greenhouse gas, and the conversion of organic wastes to methane is an important bioenergy process. species play an important role in methane production in many methanogenic soils and sediments as well as anaerobic waste digesters. The studies reported here emphasize that the genus is composed of two physiologically distinct groups. This is important to recognize when interpreting the role of in methanogenic environments, especially regarding H metabolism. Furthermore, the finding that type I species predominate in environments with high rates of carbon and electron flux and that type II species predominate in lower-energy environments suggests that evaluating the relative abundance of type I and type II may provide further insights into rates of carbon and electron flux in methanogenic environments.

}, keywords = {Acetates, Anaerobiosis, Bioreactors, Ecosystem, Electron Transport, Ethanol, Genome, Archaeal, Hydrogen, Methane, Methanosarcina, Phylogeny}, issn = {1098-5336}, doi = {10.1128/AEM.00731-21}, author = {Zhou, Jinjie and Holmes, Dawn E and Tang, Hai-Yan and Lovley, Derek R} } @article {3055, title = {Extracellular Electron Exchange Capabilities of and .}, journal = {Environ Sci Technol}, volume = {55}, year = {2021}, month = {2021 Dec 07}, pages = {16195-16203}, abstract = {

Microbial extracellular electron transfer plays an important role in diverse biogeochemical cycles, metal corrosion, bioelectrochemical technologies, and anaerobic digestion. Evaluation of electron uptake from pure Fe(0) and stainless steel indicated that, in contrast to previous speculation in the literature, and are not able to directly extract electrons from solid-phase electron-donating surfaces. grew with Fe(III) as the electron acceptor, but did not. reduced Fe(III) oxide occluded within porous alginate beads, suggesting that it released a soluble electron shuttle to promote Fe(III) oxide reduction. Conductive atomic force microscopy revealed that the pili are electrically conductive and the expression of a gene encoding an aromatics-rich putative pilin was upregulated during growth on Fe(III) oxide. The expression of genes for multi-heme -type cytochromes was not upregulated during growth with Fe(III) as the electron acceptor, and genes for a porin-cytochrome conduit across the outer membrane were not apparent in the genome. The results suggest that has adopted a novel combination of strategies to enable extracellular electron transport, which may be of biogeochemical and technological significance.

}, keywords = {Desulfovibrio, Electron Transport, Electrons, Ferric Compounds, Geobacter, Oxidation-Reduction}, issn = {1520-5851}, doi = {10.1021/acs.est.1c04071}, author = {Liang, Dandan and Liu, Xinying and Woodard, Trevor L and Holmes, Dawn E and Smith, Jessica A and Nevin, Kelly P and Feng, Yujie and Lovley, Derek R} } @article {3056, title = {Mechanisms for Electron Uptake by Methanosarcina acetivorans during Direct Interspecies Electron Transfer.}, journal = {mBio}, volume = {12}, year = {2021}, month = {2021 Oct 26}, pages = {e0234421}, abstract = {

Direct interspecies electron transfer (DIET) between bacteria and methanogenic archaea appears to be an important syntrophy in both natural and engineered methanogenic environments. However, the electrical connections on the outer surface of methanogens and the subsequent processing of electrons for carbon dioxide reduction to methane are poorly understood. Here, we report that the genetically tractable methanogen Methanosarcina acetivorans can grow via DIET in coculture with Geobacter metallireducens serving as the electron-donating partner. Comparison of gene expression patterns in grown in coculture versus pure-culture growth on acetate revealed that transcripts for the outer-surface multiheme type cytochrome MmcA were higher during DIET-based growth. Deletion of inhibited DIET. The high aromatic amino acid content of archaellins suggests that they might assemble into electrically conductive archaella. A mutant that could not express archaella was deficient in DIET. However, this mutant grew in DIET-based coculture as well as the archaellum-expressing parental strain in the presence of granular activated carbon, which was previously shown to serve as a substitute for electrically conductive pili as a conduit for long-range interspecies electron transfer in other DIET-based cocultures. Transcriptomic data suggesting that the membrane-bound Rnf, Fpo, and HdrED complexes also play a role in DIET were incorporated into a charge-balanced model illustrating how electrons entering the cell through MmcA can yield energy to support growth from carbon dioxide reduction. The results are the first genetics-based functional demonstration of likely outer-surface electrical contacts for DIET in a methanogen. The conversion of organic matter to methane plays an important role in the global carbon cycle and is an effective strategy for converting wastes to a useful biofuel. The reduction of carbon dioxide to methane accounts for approximately a third of the methane produced in anaerobic soils and sediments as well as waste digesters. Potential electron donors for carbon dioxide reduction are H or electrons derived from direct interspecies electron transfer (DIET) between bacteria and methanogens. Elucidating the relative importance of these electron donors has been difficult due to a lack of information on the electrical connections on the outer surfaces of methanogens and how they process the electrons received from DIET. Transcriptomic patterns and gene deletion phenotypes reported here provide insight into how a group of organisms that play an important role in methane production in soils and sediments participate in DIET.

}, keywords = {Archaeal Proteins, Electron Transport, Electrons, Methane, Methanosarcina, Transcriptome}, issn = {2150-7511}, doi = {10.1128/mBio.02344-21}, author = {Holmes, Dawn E and Zhou, Jinjie and Ueki, Toshiyuki and Woodard, Trevor and Lovley, Derek R} } @article {3062, title = {Stainless steel corrosion via direct iron-to-microbe electron transfer by Geobacter species.}, journal = {ISME J}, volume = {15}, year = {2021}, month = {2021 Oct}, pages = {3084-3093}, abstract = {

Microbial corrosion of iron-based materials is a substantial economic problem. A mechanistic understanding is required to develop mitigation strategies, but previous mechanistic studies have been limited to investigations with relatively pure Fe(0), which is not a common structural material. We report here that the mechanism for microbial corrosion of stainless steel, the metal of choice for many actual applications, can be significantly different from that~for Fe(0). Although H is often an intermediary electron carrier between the metal and microbes during Fe(0) corrosion, we found that H is not abiotically produced from stainless steel, making this corrosion mechanism unlikely. Geobacter sulfurreducens and Geobacter metallireducens, electrotrophs that are known to directly accept electrons from other microbes or electrodes, extracted electrons from stainless steel via direct iron-to-microbe electron transfer. Genetic modification to prevent H consumption did not negatively impact on stainless steel corrosion. Corrosion was inhibited when genes for outer-surface cytochromes that are key electrical contacts were deleted. These results indicate that a common model of microbial Fe(0) corrosion~by hydrogenase-positive microbes, in which H serves as an intermediary electron carrier between the metal surface and the microbe, may not apply to the microbial corrosion of stainless steel. However, direct iron-to-microbe electron transfer is a~feasible route for stainless steel corrosion.

}, keywords = {Corrosion, Electrons, Geobacter, Iron, Stainless Steel}, issn = {1751-7370}, doi = {10.1038/s41396-021-00990-2}, author = {Tang, Hai-Yan and Yang, Chuntian and Ueki, Toshiyuki and Pittman, Conor C and Xu, Dake and Woodard, Trevor L and Holmes, Dawn E and Gu, Tingyue and Wang, Fuhui and Lovley, Derek R} } @article {3068, title = {Protein Nanowires: the Electrification of the Microbial World and Maybe Our Own.}, journal = {J Bacteriol}, volume = {202}, year = {2020}, month = {2020 Sep 23}, abstract = {

Electrically conductive protein nanowires appear to be widespread in the microbial world and are a revolutionary "green" material for the fabrication of electronic devices. Electrically conductive pili (e-pili) assembled from type IV pilin monomers have independently evolved multiple times in microbial history as have electrically conductive archaella (e-archaella) assembled from homologous archaellin monomers. A role for e-pili in long-range (micrometer) extracellular electron transport has been demonstrated in some microbes. The surprising finding of e-pili in syntrophic bacteria and the role of e-pili as conduits for direct interspecies electron transfer have necessitated a reassessment of routes for electron flux in important methanogenic environments, such as anaerobic digesters and terrestrial wetlands. Pilin monomers similar to those found in e-pili may also be a major building block of the conductive "cables" that transport electrons over centimeter distances through continuous filaments of cable bacteria consisting of a thousand cells or more. Protein nanowires harvested from microbes have many functional and sustainability advantages over traditional nanowire materials and have already yielded novel electronic devices for sustainable electricity production, neuromorphic memory, and sensing. e-pili can be mass produced with an chassis, providing a ready source of material for electronics as well as for studies on the basic mechanisms for long-range electron transport along protein nanowires. Continued exploration is required to better understand the electrification of microbial communities with microbial nanowires and to expand the "green toolbox" of sustainable materials for wiring and powering the emerging "Internet of things."

}, keywords = {Electric Conductivity, Electron Transport, Fimbriae Proteins, Fimbriae, Bacterial, Geobacter, Microscopy, Electron, Nanowires, Protein Engineering}, issn = {1098-5530}, doi = {10.1128/JB.00331-20}, author = {Lovley, Derek R and Holmes, Dawn E} } @article {3072, title = {Syntrophus conductive pili demonstrate that common hydrogen-donating syntrophs can have a direct electron transfer option.}, journal = {ISME J}, volume = {14}, year = {2020}, month = {2020 Mar}, pages = {837-846}, abstract = {

Syntrophic interspecies electron exchange is essential for the stable functioning of diverse anaerobic microbial communities. Hydrogen/formate interspecies electron transfer (HFIT), in which H and/or formate function as diffusible electron carriers, has been considered to be the primary mechanism for electron transfer because most common syntrophs were thought to lack biochemical components, such as electrically conductive pili (e-pili), necessary for direct interspecies electron transfer (DIET). Here we report that Syntrophus aciditrophicus, one of the most intensively studied microbial models for HFIT, produces e-pili and can grow via DIET. Heterologous expression of the putative S. aciditrophicus type IV pilin gene in Geobacter sulfurreducens yielded conductive pili of the same diameter (4 nm) and conductance of the native S. aciditrophicus pili and enabled long-range electron transport in G. sulfurreducens. S. aciditrophicus lacked abundant c-type cytochromes often associated with DIET. Pilin genes likely to yield e-pili were found in other genera of hydrogen/formate-producing syntrophs. The finding that DIET is a likely option for diverse syntrophs that are abundant in many anaerobic environments necessitates a reexamination of the paradigm that HFIT is the predominant mechanism for syntrophic electron exchange within anaerobic microbial communities of biogeochemical and practical significance.

}, keywords = {Deltaproteobacteria, Electric Conductivity, Electron Transport, Electrons, Fimbriae Proteins, Fimbriae, Bacterial, Formates, Geobacter, Hydrogen}, issn = {1751-7370}, doi = {10.1038/s41396-019-0575-9}, author = {Walker, David J F and Nevin, Kelly P and Holmes, Dawn E and Rotaru, Amelia-Elena and Ward, Joy E and Woodard, Trevor L and Zhu, Jiaxin and Ueki, Toshiyuki and Nonnenmann, Stephen S and McInerney, Michael J and Lovley, Derek R} } @article {3079, title = {The Archaellum of Methanospirillum hungatei Is Electrically Conductive.}, journal = {mBio}, volume = {10}, year = {2019}, month = {2019 Apr 16}, abstract = {

Microbially produced electrically conductive protein filaments are of interest because they can function as conduits for long-range biological electron transfer. They also show promise as sustainably produced electronic materials. Until now, microbially produced conductive protein filaments have been reported only for bacteria. We report here that the archaellum of is electrically conductive. This is the first demonstration that electrically conductive protein filaments have evolved in Furthermore, the structure of the archaellum was previously determined (N. Poweleit, P. Ge, H. N. Nguyen, R. R. O. Loo, et al., Nat Microbiol 2:16222, 2016, https://doi.org/10.1038/nmicrobiol.2016.222). Thus, the archaellum of is the first microbially produced electrically conductive protein filament for which a structure is known. We analyzed the previously published structure and identified a core of tightly packed phenylalanines that is one likely route for electron conductance. The availability of the archaellum structure is expected to substantially advance mechanistic evaluation of long-range electron transport in microbially produced electrically conductive filaments and to aid in the design of "green" electronic materials that can be microbially produced with renewable feedstocks. Microbially produced electrically conductive protein filaments are a revolutionary, sustainably produced, electronic material with broad potential applications. The design of new protein nanowires based on the known archaellum structure could be a major advance over the current empirical design of synthetic protein nanowires from electrically conductive bacterial pili. An understanding of the diversity of outer-surface protein structures capable of electron transfer is important for developing models for microbial electrical communication with other cells and minerals in natural anaerobic environments. Extracellular electron exchange is also essential in engineered environments such as bioelectrochemical devices and anaerobic digesters converting wastes to methane. The finding that the archaellum of is electrically conductive suggests that some archaea might be able to make long-range electrical connections with their external environment.

}, keywords = {Electric Conductivity, Electricity, Electron Transport, Flagella, Methanospirillum, Phenylalanine}, issn = {2150-7511}, doi = {10.1128/mBio.00579-19}, author = {Walker, David J F and Martz, Eric and Holmes, Dawn E and Zhou, Zimu and Nonnenmann, Stephen S and Lovley, Derek R} } @article {3077, title = {Iron Corrosion via Direct Metal-Microbe Electron Transfer.}, journal = {mBio}, volume = {10}, year = {2019}, month = {2019 May 14}, abstract = {

The concept that anaerobic microorganisms can directly accept electrons from Fe(0) has been controversial because direct metal-microbe electron transfer has previously only been indirectly inferred. Fe(0) oxidation was studied with strain ACL, an autotrophic strain that was previously shown to grow with electrons derived from a graphite cathode as the sole electron donor. Strain ACL grew with Fe(0) as the sole electron donor and fumarate as the electron acceptor. However, it appeared that at least a portion of the electron transfer was via H produced nonenzymatically from the oxidation of Fe(0) to Fe(II). H, which accumulated in abiotic controls, was consumed during the growth of strain ACL, the cells were predominately planktonic, and genes for the uptake hydrogenase were highly expressed. Strain ACL was constructed to prevent growth on H or formate by deleting the genes for the uptake of hydrogenase and formate dehydrogenases from strain ACL. Strain ACL also grew with Fe(0) as the sole electron donor, but H accumulated in the culture, and cells heavily colonized Fe(0) surfaces with no visible planktonic growth. Transcriptomics suggested that the outer surface -type cytochromes OmcS and OmcZ were important during growth of strain ACL on Fe(0). Strain ACL did not grow on Fe(0) if the gene for either of these cytochromes was deleted. The specific attachment of strain ACL to Fe(0), coupled with requirements for known extracellular electrical contacts, suggest that direct metal-microbe electron transfer is the most likely option for Fe(0) serving as an electron donor. The anaerobic corrosion of iron structures is expensive to repair and can be a safety and environmental concern. It has been known for over 100 years that the presence of anaerobic respiratory microorganisms can accelerate iron corrosion. Multiple studies have suggested that there are sulfate reducers, methanogens, and acetogens that can directly accept electrons from Fe(0) to support sulfate or carbon dioxide reduction. However, all of the strains studied can also use H as an electron donor for growth, which is known to be abiotically produced from Fe(0). Furthermore, no proteins definitely shown to function as extracellular electrical contacts with Fe(0) were identified. The studies described here demonstrate that direct electron transfer from Fe(0) can support anaerobic respiration. They also map out a simple genetic approach to the study of iron corrosion mechanisms in other microorganisms. A better understanding of how microorganisms promote iron corrosion is expected to lead to the development of strategies that can help reduce adverse impacts from this process.

}, keywords = {Anaerobiosis, Corrosion, Cytochromes, Electron Transport, Formate Dehydrogenases, Geobacter, Iron, Oxidation-Reduction, Oxidoreductases, Transcriptome}, issn = {2150-7511}, doi = {10.1128/mBio.00303-19}, author = {Tang, Hai-Yan and Holmes, Dawn E and Ueki, Toshiyuki and Palacios, Paola A and Lovley, Derek R} } @article {3074, title = {A Membrane-Bound Cytochrome Enables To Conserve Energy from Extracellular Electron Transfer.}, journal = {mBio}, volume = {10}, year = {2019}, month = {2019 Aug 20}, abstract = {

Extracellular electron exchange in species and closely related plays an important role in the global carbon cycle and enhances the speed and stability of anaerobic digestion by facilitating efficient syntrophic interactions. Here, we grew with methanol provided as the electron donor and the humic analogue, anthraquione-2,6-disulfonate (AQDS), provided as the electron acceptor when methane production was inhibited with bromoethanesulfonate. AQDS was reduced with simultaneous methane production in the absence of bromoethanesulfonate. Transcriptomics revealed that expression of the gene for the transmembrane, multiheme, -type cytochrome MmcA was higher in AQDS-respiring cells than in cells performing methylotrophic methanogenesis. A strain in which the gene for MmcA was deleted failed to grow via AQDS reduction but grew with the conversion of methanol or acetate to methane, suggesting that MmcA has a specialized role as a conduit for extracellular electron transfer. Enhanced expression of genes for methanol conversion to methyl-coenzyme M and the Rnf complex suggested that methanol is oxidized to carbon dioxide in AQDS-respiring cells through a pathway that is similar to methyl-coenzyme M oxidation in methanogenic cells. However, during AQDS respiration the Rnf complex and reduced methanophenazine probably transfer electrons to MmcA, which functions as the terminal reductase for AQDS reduction. Extracellular electron transfer may enable the survival of methanogens in dynamic environments in which oxidized humic substances and Fe(III) oxides are intermittently available. The availability of tools for genetic manipulation of makes it an excellent model microbe for evaluating -type cytochrome-dependent extracellular electron transfer in The discovery of a methanogen that can conserve energy to support growth solely from the oxidation of organic carbon coupled to the reduction of an extracellular electron acceptor expands the possible environments in which methanogens might thrive. The potential importance of -type cytochromes for extracellular electron transfer to syntrophic bacterial partners and/or Fe(III) minerals in some was previously proposed, but these studies with provide the first genetic evidence for cytochrome-based extracellular electron transfer in The results suggest parallels with Gram-negative bacteria, such as and species, in which multiheme outer-surface -type cytochromes are an essential component for electrical communication with the extracellular environment. offers an unprecedented opportunity to study mechanisms for energy conservation from the anaerobic oxidation of one-carbon organic compounds coupled to extracellular electron transfer in with implications not only for methanogens but possibly also for that anaerobically oxidize methane.

}, keywords = {Acetates, Anthraquinones, Cytochromes, Electron Transport, Electrons, Ferric Compounds, Gene Expression Regulation, Archaeal, Gram-Negative Bacteria, Membranes, Mesna, Methane, Methanol, Methanosarcina, Oxidation-Reduction, Oxidoreductases, Transcriptome}, issn = {2150-7511}, doi = {10.1128/mBio.00789-19}, author = {Holmes, Dawn E and Ueki, Toshiyuki and Tang, Hai-Yan and Zhou, Jinjie and Smith, Jessica A and Chaput, Gina and Lovley, Derek R} } @article {3083, title = {Construction of a Strain With Exceptional Growth on Cathodes.}, journal = {Front Microbiol}, volume = {9}, year = {2018}, month = {2018}, pages = {1512}, abstract = {

Insoluble extracellular electron donors are important sources of energy for anaerobic respiration in biogeochemical cycling and in diverse practical applications. The previous lack of a genetically tractable model microorganism that could be grown to high densities under anaerobic conditions in pure culture with an insoluble extracellular electron donor has stymied efforts to better understand this form of respiration. We report here on the design of a strain of , designated strain ACL, which grows as thick (ca. 35 μm) confluent biofilms on graphite cathodes poised at -500 mV ( Ag/AgCl) with fumarate as the electron acceptor. Sustained maximum current consumption rates were >0.8 A/m, which is >10-fold higher than the current consumption of the wild-type strain. The improved function on the cathode was achieved by introducing genes for an ATP-dependent citrate lyase, completing the complement of enzymes needed for a reverse TCA cycle for the synthesis of biosynthetic precursors from carbon dioxide. Strain ACL provides an important model organism for elucidating the mechanisms for effective anaerobic growth with an insoluble extracellular electron donor and may offer unique possibilities as a chassis for the introduction of synthetic metabolic pathways for the production of commodities with electrons derived from electrodes.

}, issn = {1664-302X}, doi = {10.3389/fmicb.2018.01512}, author = {Ueki, Toshiyuki and Nevin, Kelly P and Woodard, Trevor L and Aklujkar, Muktak A and Holmes, Dawn E and Lovley, Derek R} } @article {3087, title = {Electrically conductive pili from pilin genes of phylogenetically diverse microorganisms.}, journal = {ISME J}, volume = {12}, year = {2018}, month = {2018 Jan}, pages = {48-58}, abstract = {

The possibility that bacteria other than Geobacter species might contain genes for electrically conductive pili (e-pili) was investigated by heterologously expressing pilin genes of interest in Geobacter sulfurreducens. Strains of G. sulfurreducens producing high current densities, which are only possible with e-pili, were obtained with pilin genes from Flexistipes sinusarabici, Calditerrivibrio nitroreducens and Desulfurivibrio alkaliphilus. The conductance of pili from these strains was comparable to native G. sulfurreducens e-pili. The e-pili derived from C. nitroreducens, and D. alkaliphilus pilin genes are the first examples of relatively long (>100 amino acids) pilin monomers assembling into e-pili. The pilin gene from Candidatus Desulfofervidus auxilii did not yield e-pili, suggesting that the hypothesis that this sulfate reducer wires itself with e-pili to methane-oxidizing archaea to enable anaerobic methane oxidation should be reevaluated. A high density of aromatic amino acids and a lack of substantial aromatic-free gaps along the length of long pilins may be important characteristics leading to e-pili. This study demonstrates a simple method to screen pilin genes from difficult-to-culture microorganisms for their potential to yield e-pili; reveals new sources for biologically based electronic materials; and suggests that a wide phylogenetic diversity of microorganisms may use e-pili for extracellular electron exchange.

}, keywords = {Deltaproteobacteria, Electric Conductivity, Fimbriae Proteins, Fimbriae, Bacterial, Methane, Oxidation-Reduction, Phylogeny}, issn = {1751-7370}, doi = {10.1038/ismej.2017.141}, author = {Walker, David Jf and Adhikari, Ramesh Y and Holmes, Dawn E and Ward, Joy E and Woodard, Trevor L and Nevin, Kelly P and Lovley, Derek R} } @article {3080, title = {Electron and Proton Flux for Carbon Dioxide Reduction in During Direct Interspecies Electron Transfer.}, journal = {Front Microbiol}, volume = {9}, year = {2018}, month = {2018}, pages = {3109}, abstract = {

Direct interspecies electron transfer (DIET) is important in diverse methanogenic environments, but how methanogens participate in DIET is poorly understood. Therefore, the transcriptome of grown via DIET in co-culture with was compared with its transcriptome when grown via H interspecies transfer (HIT) with . Notably, transcripts for the FH dehydrogenase, Fpo, and the heterodisulfide reductase, HdrABC, were more abundant during growth on DIET. A model for CO reduction was developed from these results in which electrons delivered to methanophenazine in the cell membrane are transferred to Fpo. The external proton gradient necessary to drive the otherwise thermodynamically unfavorable reverse electron transport for Fpo-catalyzed F reduction is derived from protons released from metabolism. Reduced F is a direct electron donor in the carbon dioxide reduction pathway and also serves as the electron donor for the proposed HdrABC-catalyzed electron bifurcation reaction in which reduced ferredoxin (also required for carbon dioxide reduction) is generated with simultaneous reduction of CoM-S-S-CoB. Expression of genes for putative redox-active proteins predicted to be localized on the outer cell surface was higher during growth on DIET, but further analysis will be required to identify the electron transfer route to methanophenazine. The results indicate that the pathways for electron and proton flux for CO reduction during DIET are substantially different than for HIT and suggest that gene expression patterns may also be useful for determining whether are directly accepting electrons from other extracellular electron donors, such as corroding metals or electrodes.

}, issn = {1664-302X}, doi = {10.3389/fmicb.2018.03109}, author = {Holmes, Dawn E and Rotaru, Amelia-Elena and Ueki, Toshiyuki and Shrestha, Pravin M and Ferry, James G and Lovley, Derek R} } @article {3085, title = {Potential for Methanosarcina to Contribute to Uranium Reduction during Acetate-Promoted Groundwater Bioremediation.}, journal = {Microb Ecol}, volume = {76}, year = {2018}, month = {2018 Oct}, pages = {660-667}, abstract = {

Previous studies of acetate-promoted bioremediation of uranium-contaminated aquifers focused on Geobacter because no other microorganisms that can couple the oxidation of acetate with U(VI) reduction had been detected in situ. Monitoring the levels of methyl CoM reductase subunit A (mcrA) transcripts during an acetate-injection field experiment demonstrated that acetoclastic methanogens from the genus Methanosarcina were enriched after 40~days of acetate amendment. The increased abundance of Methanosarcina corresponded with an accumulation of methane in the groundwater. In order to determine whether Methanosarcina species could be participating in U(VI) reduction in the subsurface, cell suspensions of Methanosarcina barkeri were incubated in the presence of U(VI) with acetate provided as the electron donor. U(VI) was reduced by metabolically active M. barkeri cells; however, no U(VI) reduction was observed in inactive controls. These results demonstrate that Methanosarcina species could play an important role in the long-term bioremediation of uranium-contaminated aquifers after depletion of Fe(III) oxides limits the growth of Geobacter species. The results also suggest that Methanosarcina have the potential to influence uranium geochemistry in a diversity of anaerobic sedimentary environments.

}, keywords = {Acetates, Biodegradation, Environmental, Geobacter, Groundwater, Methane, Methanosarcina, Oxidation-Reduction, Uranium, Water Pollutants, Chemical}, issn = {1432-184X}, doi = {10.1007/s00248-018-1165-5}, author = {Holmes, Dawn E and Orelana, Roberto and Giloteaux, Ludovic and Wang, Li-Ying and Shrestha, Pravin and Williams, Kenneth and Lovley, Derek R and Rotaru, Amelia-Elena} } @article {3092, title = {Metatranscriptomic Evidence for Direct Interspecies Electron Transfer between Geobacter and Methanothrix Species in Methanogenic Rice Paddy Soils.}, journal = {Appl Environ Microbiol}, volume = {83}, year = {2017}, month = {2017 May 01}, abstract = {

The possibility that (formerly ) and species cooperate via direct interspecies electron transfer (DIET) in terrestrial methanogenic environments was investigated in rice paddy soils. Genes with high sequence similarity to the gene for the PilA pilin monomer of the electrically conductive pili (e-pili) of accounted for over half of the PilA gene sequences in metagenomic libraries and 42\% of the mRNA transcripts in RNA sequencing (RNA-seq) libraries. This abundance of e-pilin genes and transcripts is significant because e-pili can serve as conduits for DIET. Most of the e-pilin genes and transcripts were affiliated with species, but sequences most closely related to putative e-pilin genes from genera such as , , , and , were also detected. Approximately 17\% of all metagenomic and metatranscriptomic bacterial sequences clustered with species, and the finding that spp. were actively transcribing growth-related genes indicated that they were metabolically active in the soils. Genes coding for e-pilin were among the most highly transcribed genes. In addition, homologs of genes encoding OmcS, a -type cytochrome associated with the e-pili of and required for DIET, were also highly expressed in the soils. species in the soils highly expressed genes for enzymes involved in the reduction of carbon dioxide to methane. DIET is the only electron donor known to support CO reduction in Thus, these results are consistent with a model in which species were providing electrons to species for methane production through electrical connections of e-pili. species are some of the most important microbial contributors to global methane production, but surprisingly little is known about their physiology and ecology. The possibility that DIET is a source of electrons for in methanogenic rice paddy soils is important because it demonstrates that the contribution that makes to methane production in terrestrial environments may extend beyond the conversion of acetate to methane. Furthermore, defined coculture studies have suggested that when species receive some of their energy from DIET, they grow faster than when acetate is their sole energy source. Thus, growth and metabolism in methanogenic soils may be faster and more robust than generally considered. The results also suggest that the reason that species are repeatedly found to be among the most metabolically active microorganisms in methanogenic soils is that they grow syntrophically in cooperation with spp., and possibly other methanogens, via DIET.

}, keywords = {Carbon Dioxide, Electron Transport, Fimbriae Proteins, Gene Expression Profiling, Geobacter, Metagenome, Methane, Methanosarcinaceae, Oryza, Soil Microbiology}, issn = {1098-5336}, doi = {10.1128/AEM.00223-17}, author = {Holmes, Dawn E and Shrestha, Pravin M and Walker, David J F and Dang, Yan and Nevin, Kelly P and Woodard, Trevor L and Lovley, Derek R} } @article {3091, title = {The electrically conductive pili of pecies are a recently evolved feature for extracellular electron transfer.}, journal = {Microb Genom}, volume = {2}, year = {2016}, month = {2016 Aug}, pages = {e000072}, abstract = {

The electrically conductive pili (e-pili) of have environmental and practical significance because they can facilitate electron transfer to insoluble Fe(III) oxides; to other microbial species; and through electrically conductive biofilms. E-pili conductivity has been attributed to the truncated PilA monomer, which permits tight packing of aromatic amino acids to form a conductive path along the length of e-pili. In order to better understand the evolution and distribution of e-pili in the microbial world, type IVa PilA proteins from various Gram-negative and Gram-positive bacteria were examined with a particular emphasis on Fe(III)-respiring bacteria. E-pilin genes are primarily restricted to a tight phylogenetic group in the order Desulfuromonadales. The downstream gene in all but one of the Desulfuromonadales that possess an e-pilin gene is a gene previously annotated as {\textquoteright}{\textquoteright} that has characteristics suggesting that it may encode an outer-membrane protein. Other genes associated with pilin function are clustered with e-pilin and {\textquoteright}{\textquoteright} genes in the Desulfuromonadales. In contrast, in the few bacteria outside the Desulfuromonadales that contain e-pilin genes, the other genes required for pilin function may have been acquired through horizontal gene transfer. Of the 95 known Fe(III)-reducing micro-organisms for which genomes are available, 80 \% lack e-pilin genes, suggesting that e-pili are just one of several mechanisms involved in extracellular electron transport. These studies provide insight into where and when e-pili are likely to contribute to extracellular electron transport processes that are biogeochemically important and involved in bioenergy conversions.

}, keywords = {Electromagnetic Phenomena, Electron Transport, Ferric Compounds, Fimbriae Proteins, Fimbriae, Bacterial, Geobacter, Phylogeny}, issn = {2057-5858}, doi = {10.1099/mgen.0.000072}, author = {Holmes, Dawn E and Dang, Yan and Walker, David J F and Lovley, Derek R} } @article {3099, title = {Enhancing anaerobic digestion of complex organic waste with carbon-based conductive materials.}, journal = {Bioresour Technol}, volume = {220}, year = {2016}, month = {2016 Nov}, pages = {516-522}, abstract = {

The aim of this work was to study the methanogenic metabolism of dog food, a food waste surrogate, in laboratory-scale reactors with different carbon-based conductive materials. Carbon cloth, carbon felt, and granular activated carbon all permitted higher organic loading rates and promoted faster recovery of soured reactors than the control reactors. Microbial community analysis revealed that specific and substantial enrichments of Sporanaerobacter and Methanosarcina were present on the carbon cloth surface. These results, and the known ability of Sporanaerobacter species to transfer electrons to elemental sulfur, suggest that Sporanaerobacter species can participate in direct interspecies electron transfer with Methanosarcina species when carbon cloth is available as an electron transfer mediator.

}, keywords = {Anaerobiosis, Animals, Bacteria, Bioreactors, Carbon, Carbon Fiber, Charcoal, Dogs, Electric Conductivity, Fatty Acids, Volatile, Hydrogen-Ion Concentration, Methane, Organic Chemicals, Waste Products}, issn = {1873-2976}, doi = {10.1016/j.biortech.2016.08.114}, author = {Dang, Yan and Holmes, Dawn E and Zhao, Zhiqiang and Woodard, Trevor L and Zhang, Yaobin and Sun, Dezhi and Wang, Li-Ying and Nevin, Kelly P and Lovley, Derek R} } @article {3104, title = {Potential enhancement of direct interspecies electron transfer for syntrophic metabolism of propionate and butyrate with biochar in up-flow anaerobic sludge blanket reactors.}, journal = {Bioresour Technol}, volume = {209}, year = {2016}, month = {2016 Jun}, pages = {148-56}, abstract = {

Promoting direct interspecies electron transfer (DIET) to enhance syntrophic metabolism may be a strategy for accelerating the conversion of organic wastes to methane, but microorganisms capable of metabolizing propionate and butyrate via DIET under methanogenic conditions have yet to be identified. In an attempt to establish methanogenic communities metabolizing propionate or butyrate with DIET, enrichments were initiated with up-flow anaerobic sludge blanket (UASB), similar to those that were previously reported to support communities that metabolized ethanol with DIET that relied on direct biological electrical connections. In the absence of any amendments, microbial communities enriched were dominated by microorganisms closely related to pure cultures that are known to metabolize propionate or butyrate to acetate with production of H2. When biochar was added to the reactors there was a substantial enrichment on the biochar surface of 16S rRNA gene sequences closely related to Geobacter and Methanosaeta species known to participate in DIET.

}, keywords = {Acetates, Bioreactors, Butyric Acid, Charcoal, Electron Transport, Geobacter, Methane, Microbial Consortia, Propionates, RNA, Ribosomal, 16S, Sewage, Waste Disposal, Fluid}, issn = {1873-2976}, doi = {10.1016/j.biortech.2016.03.005}, author = {Zhao, Zhiqiang and Zhang, Yaobin and Holmes, Dawn E and Dang, Yan and Woodard, Trevor L and Nevin, Kelly P and Lovley, Derek R} } @article {3120, title = {Evidence of Geobacter-associated phage in a uranium-contaminated aquifer.}, journal = {ISME J}, volume = {9}, year = {2015}, month = {2015 Feb}, pages = {333-46}, abstract = {

Geobacter species may be important agents in the bioremediation of organic and metal contaminants in the subsurface, but as yet unknown factors limit the in situ growth of subsurface Geobacter well below rates predicted by analysis of gene expression or in silico metabolic modeling. Analysis of the genomes of five different Geobacter species recovered from contaminated subsurface sites indicated that each of the isolates had been infected with phage. Geobacter-associated phage sequences were also detected by metagenomic and proteomic analysis of samples from a uranium-contaminated aquifer undergoing in situ bioremediation, and phage particles were detected by microscopic analysis in groundwater collected from sediment enrichment cultures. Transcript abundance for genes from the Geobacter-associated phage structural proteins, tail tube Gp19 and baseplate J, increased in the groundwater in response to the growth of Geobacter species when acetate was added, and then declined as the number of Geobacter decreased. Western blot analysis of a Geobacter-associated tail tube protein Gp19 in the groundwater demonstrated that its abundance tracked with the abundance of Geobacter species. These results suggest that the enhanced growth of Geobacter species in the subsurface associated with in situ uranium bioremediation increased the abundance and activity of Geobacter-associated phage and show that future studies should focus on how these phages might be influencing the ecology of this site.

}, keywords = {Bacteriophages, Biodegradation, Environmental, Genes, Viral, Geobacter, Groundwater, Metagenome, Proteomics, Transcriptome, Uranium, Viral Proteins, Water Pollutants, Radioactive}, issn = {1751-7370}, doi = {10.1038/ismej.2014.128}, author = {Holmes, Dawn E and Giloteaux, Ludovic and Chaurasia, Akhilesh K and Williams, Kenneth H and Luef, Birgit and Wilkins, Michael J and Wrighton, Kelly C and Thompson, Courtney A and Comolli, Luis R and Lovley, Derek R} } @article {3107, title = {Protozoan grazing reduces the current output of microbial fuel cells.}, journal = {Bioresour Technol}, volume = {193}, year = {2015}, month = {2015 Oct}, pages = {8-14}, abstract = {

Several experiments were conducted to determine whether protozoan grazing can reduce current output from sediment microbial fuel cells. When marine sediments were amended with eukaryotic inhibitors, the power output from the fuel cells increased 2-5-fold. Quantitative PCR showed that Geobacteraceae sequences were 120 times more abundant on anodes from treated fuel cells compared to untreated fuel cells, and that Spirotrichea sequences in untreated fuel cells were 200 times more abundant on anode surfaces than in the surrounding sediments. Defined studies with current-producing biofilms of Geobacter sulfurreducens and pure cultures of protozoa demonstrated that protozoa that were effective in consuming G. sulfurreducens reduced current production up to 91\% when added to G. sulfurreducens fuel cells. These results suggest that anode biofilms are an attractive food source for protozoa and that protozoan grazing can be an important factor limiting the current output of sediment microbial fuel cells.

}, keywords = {Bioelectric Energy Sources, Biofilms, Electricity, Electrodes, Eukaryota, Geobacter, Geologic Sediments}, issn = {1873-2976}, doi = {10.1016/j.biortech.2015.06.056}, author = {Holmes, Dawn E and Nevin, Kelly P and Snoeyenbos-West, Oona L and Woodard, Trevor L and Strickland, Justin N and Lovley, Derek R} } @article {3119, title = {Methane production from protozoan endosymbionts following stimulation of microbial metabolism within subsurface sediments.}, journal = {Front Microbiol}, volume = {5}, year = {2014}, month = {2014}, pages = {366}, abstract = {

Previous studies have suggested that protozoa prey on Fe(III)- and sulfate-reducing bacteria that are enriched when acetate is added to uranium contaminated subsurface sediments to stimulate U(VI) reduction. In order to determine whether protozoa continue to impact subsurface biogeochemistry after these acetate amendments have stopped, 18S rRNA and {\ss}-tubulin sequences from this phase of an in situ uranium bioremediation field experiment were analyzed. Sequences most similar to Metopus species predominated, with the majority of sequences most closely related to M. palaeformis, a cilitated protozoan known to harbor methanogenic symbionts. Quantification of mcrA mRNA transcripts in the groundwater suggested that methanogens closely related to Metopus endosymbionts were metabolically active at this time. There was a strong correlation between the number of mcrA transcripts from the putative endosymbiotic methanogen and Metopus {\ss}-tubulin mRNA transcripts during the course of the field experiment, suggesting that the activity of the methanogens was dependent upon the activity of the Metopus species. Addition of the eukaryotic inhibitors cyclohexamide and colchicine to laboratory incubations of acetate-amended subsurface sediments significantly inhibited methane production and there was a direct correlation between methane concentration and Metopus {\ss}-tubulin and putative symbiont mcrA gene copies. These results suggest that, following the stimulation of subsurface microbial growth with acetate, protozoa harboring methanogenic endosymbionts become important members of the microbial community, feeding on moribund biomass and producing methane.

}, issn = {1664-302X}, doi = {10.3389/fmicb.2014.00366}, author = {Holmes, Dawn E and Giloteaux, Ludovic and Orellana, Roberto and Williams, Kenneth H and Robbins, Mark J and Lovley, Derek R} } @article {3154, title = {Characterization and transcription of arsenic respiration and resistance genes during in situ uranium bioremediation.}, journal = {ISME J}, volume = {7}, year = {2013}, month = {2013 Feb}, pages = {370-83}, abstract = {

The possibility of arsenic release and the potential role of Geobacter in arsenic biogeochemistry during in situ uranium bioremediation was investigated because increased availability of organic matter has been associated with substantial releases of arsenic in other subsurface environments. In a field experiment conducted at the Rifle, CO study site, groundwater arsenic concentrations increased when acetate was added. The number of transcripts from arrA, which codes for the α-subunit of dissimilatory As(V) reductase, and acr3, which codes for the arsenic pump protein Acr3, were determined with quantitative reverse transcription-PCR. Most of the arrA (>60\%) and acr3-1 (>90\%) sequences that were recovered were most similar to Geobacter species, while the majority of acr3-2 (>50\%) sequences were most closely related to Rhodoferax ferrireducens. Analysis of transcript abundance demonstrated that transcription of acr3-1 by the subsurface Geobacter community was correlated with arsenic concentrations in the groundwater. In contrast, Geobacter arrA transcript numbers lagged behind the major arsenic release and remained high even after arsenic concentrations declined. This suggested that factors other than As(V) availability regulated the transcription of arrA in situ, even though the presence of As(V) increased the transcription of arrA in cultures of Geobacter lovleyi, which was capable of As(V) reduction. These results demonstrate that subsurface Geobacter species can tightly regulate their physiological response to changes in groundwater arsenic concentrations. The transcriptomic approach developed here should be useful for the study of a diversity of other environments in which Geobacter species are considered to have an important influence on arsenic biogeochemistry.

}, keywords = {Acetates, Arsenate Reductases, Arsenic, Biodegradation, Environmental, Colorado, Gene Expression Regulation, Bacterial, Genes, Bacterial, Geobacter, Groundwater, Transcriptome, Uranium}, issn = {1751-7370}, doi = {10.1038/ismej.2012.109}, author = {Giloteaux, Ludovic and Holmes, Dawn E and Williams, Kenneth H and Wrighton, Kelly C and Wilkins, Michael J and Montgomery, Alison P and Smith, Jessica A and Orellana, Roberto and Thompson, Courtney A and Roper, Thomas J and Long, Philip E and Lovley, Derek R} } @article {3145, title = {Enrichment of specific protozoan populations during in situ bioremediation of uranium-contaminated groundwater.}, journal = {ISME J}, volume = {7}, year = {2013}, month = {2013 Jul}, pages = {1286-98}, abstract = {

The importance of bacteria in the anaerobic bioremediation of groundwater polluted with organic and/or metal contaminants is well recognized and in some instances so well understood that modeling of the in situ metabolic activity of the relevant subsurface microorganisms in response to changes in subsurface geochemistry is feasible. However, a potentially significant factor influencing bacterial growth and activity in the subsurface that has not been adequately addressed is protozoan predation of the microorganisms responsible for bioremediation. In field experiments at a uranium-contaminated aquifer located in Rifle, CO, USA, acetate amendments initially promoted the growth of metal-reducing Geobacter species, followed by the growth of sulfate reducers, as observed previously. Analysis of 18S rRNA gene sequences revealed a broad diversity of sequences closely related to known bacteriovorous protozoa in the groundwater before the addition of acetate. The bloom of Geobacter species was accompanied by a specific enrichment of sequences most closely related to the ameboid flagellate, Breviata anathema, which at their peak accounted for over 80\% of the sequences recovered. The abundance of Geobacter species declined following the rapid emergence of B. anathema. The subsequent growth of sulfate-reducing Peptococcaceae was accompanied by another specific enrichment of protozoa, but with sequences most similar to diplomonadid flagellates from the family Hexamitidae, which accounted for up to 100\% of the sequences recovered during this phase of the bioremediation. These results suggest a prey-predator response with specific protozoa responding to increased availability of preferred prey bacteria. Thus, quantifying the influence of protozoan predation on the growth, activity and composition of the subsurface bacterial community is essential for predictive modeling of in situ uranium bioremediation strategies.

}, keywords = {Acetates, Biodegradation, Environmental, Eukaryota, Geobacter, Groundwater, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, RNA, Ribosomal, 18S, Uranium}, issn = {1751-7370}, doi = {10.1038/ismej.2013.20}, author = {Holmes, Dawn E and Giloteaux, Ludovic and Williams, Kenneth H and Wrighton, Kelly C and Wilkins, Michael J and Thompson, Courtney A and Roper, Thomas J and Long, Philip E and Lovley, Derek R} } @article {3147, title = {Molecular analysis of the in situ growth rates of subsurface Geobacter species.}, journal = {Appl Environ Microbiol}, volume = {79}, year = {2013}, month = {2013 Mar}, pages = {1646-53}, abstract = {

Molecular tools that can provide an estimate of the in situ growth rate of Geobacter species could improve understanding of dissimilatory metal reduction in a diversity of environments. Whole-genome microarray analyses of a subsurface isolate of Geobacter uraniireducens, grown under a variety of conditions, identified a number of genes that are differentially expressed at different specific growth rates. Expression of two genes encoding ribosomal proteins, rpsC and rplL, was further evaluated with quantitative reverse transcription-PCR (qRT-PCR) in cells with doubling times ranging from 6.56 h to 89.28 h. Transcript abundance of rpsC correlated best (r(2) = 0.90) with specific growth rates. Therefore, expression patterns of rpsC were used to estimate specific growth rates of Geobacter species during an in situ uranium bioremediation field experiment in which acetate was added to the groundwater to promote dissimilatory metal reduction. Initially, increased availability of acetate in the groundwater resulted in higher expression of Geobacter rpsC, and the increase in the number of Geobacter cells estimated with fluorescent in situ hybridization compared well with specific growth rates estimated from levels of in situ rpsC expression. However, in later phases, cell number increases were substantially lower than predicted from rpsC transcript abundance. This change coincided with a bloom of protozoa and increased attachment of Geobacter species to solid phases. These results suggest that monitoring rpsC expression may better reflect the actual rate that Geobacter species are metabolizing and growing during in situ uranium bioremediation than changes in cell abundance.

}, keywords = {Acetates, Biodegradation, Environmental, DNA, Bacterial, Gene Expression Profiling, Geobacter, Groundwater, In Situ Hybridization, Fluorescence, Molecular Sequence Data, Ribosomal Proteins, Sequence Analysis, DNA, Uranium}, issn = {1098-5336}, doi = {10.1128/AEM.03263-12}, author = {Holmes, Dawn E and Giloteaux, Ludovic and Barlett, Melissa and Chavan, Milind A and Smith, Jessica A and Williams, Kenneth H and Wilkins, Michael and Long, Philip and Lovley, Derek R} } @article {419, title = {Genome-scale analysis of anaerobic benzoate and phenol metabolism in the hyperthermophilic archaeon Ferroglobus placidus.}, journal = {ISME J}, volume = {6}, year = {2012}, month = {2012 Jan}, pages = {146-57}, abstract = {Insight into the mechanisms for the anaerobic metabolism of aromatic compounds by the hyperthermophilic archaeon Ferroglobus placidus is expected to improve understanding of the degradation of aromatics in hot (>80{\textdegree} C) environments and to identify enzymes that might have biotechnological applications. Analysis of the F. placidus genome revealed genes predicted to encode enzymes homologous to those previously identified as having a role in benzoate and phenol metabolism in mesophilic bacteria. Surprisingly, F. placidus lacks genes for an ATP-independent class II benzoyl-CoA (coenzyme A) reductase (BCR) found in all strictly anaerobic bacteria, but has instead genes coding for a bzd-type ATP-consuming class I BCR, similar to those found in facultative bacteria. The lower portion of the benzoate degradation pathway appears to be more similar to that found in the phototroph Rhodopseudomonas palustris, than the pathway reported for all heterotrophic anaerobic benzoate degraders. Many of the genes predicted to be involved in benzoate metabolism were found in one of two gene clusters. Genes for phenol carboxylation proceeding through a phenylphosphate intermediate were identified in a single gene cluster. Analysis of transcript abundance with a whole-genome microarray and quantitative reverse transcriptase polymerase chain reaction demonstrated that most of the genes predicted to be involved in benzoate or phenol metabolism had higher transcript abundance during growth on those substrates vs growth on acetate. These results suggest that the general strategies for benzoate and phenol metabolism are highly conserved between microorganisms living in moderate and hot environments, and that anaerobic metabolism of aromatic compounds might be analyzed in a wide range of environments with similar molecular targets.}, keywords = {Acetates, Archaea, Bacteria, Anaerobic, Benzoates, Metabolic Networks and Pathways, Phenol, Rhodopseudomonas}, issn = {1751-7370}, doi = {10.1038/ismej.2011.88}, author = {Holmes, Dawn E and Risso, Carla and Smith, Jessica A and Lovley, Derek R} } @article {421, title = {Anaerobic oxidation of benzene by the hyperthermophilic archaeon Ferroglobus placidus.}, journal = {Appl Environ Microbiol}, volume = {77}, year = {2011}, month = {2011 Sep}, pages = {5926-33}, abstract = {Anaerobic benzene oxidation coupled to the reduction of Fe(III) was studied in Ferroglobus placidus in order to learn more about how such a stable molecule could be metabolized under strict anaerobic conditions. F. placidus conserved energy to support growth at 85{\textdegree}C in a medium with benzene provided as the sole electron donor and Fe(III) as the sole electron acceptor. The stoichiometry of benzene loss and Fe(III) reduction, as well as the conversion of [(14)C]benzene to [(14)C]carbon dioxide, was consistent with complete oxidation of benzene to carbon dioxide with electron transfer to Fe(III). Benzoate, but not phenol or toluene, accumulated at low levels during benzene metabolism, and [(14)C]benzoate was produced from [(14)C]benzene. Analysis of gene transcript levels revealed increased expression of genes encoding enzymes for anaerobic benzoate degradation during growth on benzene versus growth on acetate, but genes involved in phenol degradation were not upregulated during growth on benzene. A gene for a putative carboxylase that was more highly expressed in benzene- than in benzoate-grown cells was identified. These results suggest that benzene is carboxylated to benzoate and that phenol is not an important intermediate in the benzene metabolism of F. placidus. This is the first demonstration of a microorganism in pure culture that can grow on benzene under strict anaerobic conditions and for which there is strong evidence for degradation of benzene via clearly defined anaerobic metabolic pathways. Thus, F. placidus provides a much-needed pure culture model for further studies on the anaerobic activation of benzene in microorganisms.}, keywords = {Anaerobiosis, Archaeoglobales, Benzene, Carbon Radioisotopes, Ferric Compounds, Gene Expression Profiling, Hot Temperature, Isotope Labeling, Oxidation-Reduction}, issn = {1098-5336}, doi = {10.1128/AEM.05452-11}, author = {Holmes, Dawn E and Risso, Carla and Smith, Jessica A and Lovley, Derek R} } @article {415, title = {Geobacter: the microbe electric{\textquoteright}s physiology, ecology, and practical applications.}, journal = {Adv Microb Physiol}, volume = {59}, year = {2011}, month = {2011}, pages = {1-100}, abstract = {Geobacter species specialize in making electrical contacts with extracellular electron acceptors and other organisms. This permits Geobacter species to fill important niches in a diversity of anaerobic environments. Geobacter species appear to be the primary agents for coupling the oxidation of organic compounds to the reduction of insoluble Fe(III) and Mn(IV) oxides in many soils and sediments, a process of global biogeochemical significance. Some Geobacter species can anaerobically oxidize aromatic hydrocarbons and play an important role in aromatic hydrocarbon removal from contaminated aquifers. The ability of Geobacter species to reductively precipitate uranium and related contaminants has led to the development of bioremediation strategies for contaminated environments. Geobacter species produce higher current densities than any other known organism in microbial fuel cells and are common colonizers of electrodes harvesting electricity from organic wastes and aquatic sediments. Direct interspecies electron exchange between Geobacter species and syntrophic partners appears to be an important process in anaerobic wastewater digesters. Functional and comparative genomic studies have begun to reveal important aspects of Geobacter physiology and regulation, but much remains unexplored. Quantifying key gene transcripts and proteins of subsurface Geobacter communities has proven to be a powerful approach to diagnose the in situ physiological status of Geobacter species during groundwater bioremediation. The growth and activity of Geobacter species in the subsurface and their biogeochemical impact under different environmental conditions can be predicted with a systems biology approach in which genome-scale metabolic models are coupled with appropriate physical/chemical models. The proficiency of Geobacter species in transferring electrons to insoluble minerals, electrodes, and possibly other microorganisms can be attributed to their unique "microbial nanowires," pili that conduct electrons along their length with metallic-like conductivity. Surprisingly, the abundant c-type cytochromes of Geobacter species do not contribute to this long-range electron transport, but cytochromes are important for making the terminal electrical connections with Fe(III) oxides and electrodes and also function as capacitors, storing charge to permit continued respiration when extracellular electron acceptors are temporarily unavailable. The high conductivity of Geobacter pili and biofilms and the ability of biofilms to function as supercapacitors are novel properties that might contribute to the field of bioelectronics. The study of Geobacter species has revealed a remarkable number of microbial physiological properties that had not previously been described in any microorganism. Further investigation of these environmentally relevant and physiologically unique organisms is warranted.}, keywords = {Biotechnology, Ecology, Environmental Remediation, Ferric Compounds, Geobacter}, issn = {0065-2911}, doi = {10.1016/B978-0-12-387661-4.00004-5}, author = {Lovley, Derek R and Ueki, Toshiyuki and Zhang, Tian and Malvankar, Nikhil S and Shrestha, Pravin M and Flanagan, Kelly A and Aklujkar, Muktak and Butler, Jessica E and Giloteaux, Ludovic and Rotaru, Amelia-Elena and Holmes, Dawn E and Franks, Ashley E and Orellana, Roberto and Risso, Carla and Nevin, Kelly P} } @article {444, title = {Expression of acetate permease-like (apl ) genes in subsurface communities of Geobacter species under fluctuating acetate concentrations.}, journal = {FEMS Microbiol Ecol}, volume = {73}, year = {2010}, month = {2010 Sep}, pages = {441-9}, abstract = {The addition of acetate to uranium-contaminated aquifers in order to stimulate the growth and activity of Geobacter species that reduce uranium is a promising in situ bioremediation option. Optimizing this bioremediation strategy requires that sufficient acetate be added to promote Geobacter species growth. We hypothesized that under acetate-limiting conditions, subsurface Geobacter species would increase the expression of either putative acetate symporters genes (aplI and aplII). Acetate was added to a uranium-contaminated aquifer (Rifle, CO) in two continuous amendments separated by 5 days of groundwater flush to create changing acetate concentrations. While the expression of aplI in monitoring well D04 (high acetate) weakly correlated with the acetate concentration over time, the transcript levels for this gene were relatively constant in well D08 (low acetate). At the lowest acetate concentrations during the groundwater flush, the transcript levels of aplII were the highest. The expression of aplII decreased 2-10-fold upon acetate reintroduction. However, the overall instability of acetate concentrations throughout the experiment could not support a robust conclusion regarding the role of apl genes in response to acetate limitation under field conditions, in contrast to previous chemostat studies, suggesting that the function of a microbial community cannot be inferred based on lab experiments alone.}, keywords = {Acetates, Bacterial Proteins, Biodegradation, Environmental, Fresh Water, Gene Expression Regulation, Bacterial, Gene Library, Geobacter, Membrane Transport Proteins, Multigene Family, RNA, Bacterial, Uranium, Water Pollutants, Radioactive}, issn = {1574-6941}, doi = {10.1111/j.1574-6941.2010.00907.x}, author = {Elifantz, Hila and N{\textquoteright}guessan, Lucie A and Mouser, Paula J and Williams, Kenneth H and Wilkins, Michael J and Risso, Carla and Holmes, Dawn E and Long, Philip E and Lovley, Derek R} } @article {459, title = {Influence of heterogeneous ammonium availability on bacterial community structure and the expression of nitrogen fixation and ammonium transporter genes during in situ bioremediation of uranium-contaminated groundwater.}, journal = {Environ Sci Technol}, volume = {43}, year = {2009}, month = {2009 Jun 15}, pages = {4386-92}, abstract = {The influence of ammonium availability on bacterial community structure and the physiological status of Geobacter species during in situ bioremediation of uranium-contaminated groundwater was evaluated. Ammonium concentrations varied by 2 orders of magnitude (< 4 to 400 microM) across th study site. Analysis of 16S rRNA sequences suggested that ammonium may have been one factor influencing the community composition prior to acetate amendment with Rhodoferax species predominating over Geobacter species with higher ammonium and Dechloromonas species dominating at the site with lowest ammonium. However, once acetate was added and dissimilatory metal reduction was stimulated, Geobacter species became the predominant organisms at all locations. Rates of U(VI) reduction appeared to be more related to acetate concentrations rather than ammonium levels. In situ mRNA transcript abundance of the nitrogen fixation gene, nifD, and the ammonium transporter gene, amtB, in Geobacter species indicated that ammonium was the primary source of nitrogen during uranium reduction. The abundance of amtB was inversely correlated to ammonium levels, whereas nifD transcript levels were similar across all sites examined. These results suggest that nifD and amtB expression are closely regulated in response to ammonium availability to ensure an adequate supply of nitrogen while conserving cell resources. Thus, quantifying nifD and amtB transcript expression appears to be a useful approach for monitoring the nitrogen-related physiological status of subsurface Geobacter species. This study also emphasizes the need for more detailed analysis of geochemical and physiological interactions at the field scale in order to adequately model subsurface microbial processes during bioremediation.}, keywords = {Carrier Proteins, DNA, Bacterial, Environmental Remediation, Gene Expression Regulation, Bacterial, Gene Library, Geobacter, Nitrogen Fixation, Quaternary Ammonium Compounds, Time Factors, Uranium, Water, Water Pollutants, Radioactive}, issn = {0013-936X}, author = {Mouser, Paula J and N{\textquoteright}guessan, Lucie A and Elifantz, Hila and Holmes, Dawn E and Williams, Kenneth H and Wilkins, Michael J and Long, Philip E and Lovley, Derek R} } @article {467, title = {Quantifying expression of Geobacter spp. oxidative stress genes in pure culture and during in situ uranium bioremediation.}, journal = {ISME J}, volume = {3}, year = {2009}, month = {2009 Apr}, pages = {454-65}, abstract = {As part of an effort to diagnose the physiological status of Geobacter species during in situ bioremediation of uranium-contaminated groundwater, transcript levels for two genes potentially associated with oxidative stress, cydA and sodA, were quantified throughout a bioremediation field study in Rifle, CO, USA. Despite the accumulation of Fe(II) in the groundwater, which is inconsistent with the presence of dissolved oxygen, both genes were highly expressed during the bioremediation process. Therefore, the response to oxidative stress was further evaluated with Geobacter uraniireducens, an isolate from the Rifle site. When G. uraniireducens cultured with fumarate as the electron acceptor was exposed to 5\% oxygen for 8 h, there was a significant increase in cydA and sodA transcripts as well as other genes associated with oxygen respiration or oxidative stress. Oxygen-exposed cells had lower transcript abundance for genes associated with anaerobic respiration, metabolism and motility. Short-term oxygen exposure had little impact on cydA transcript levels, as more than 1 h was required for increases to levels comparable to the subsurface. Abundance of cydA and sodA transcripts for the isolate G. sulfurreducens were always higher in cells cultured with Fe(III) compared with fumarate as an electron acceptor, even when fumarate-grown cells were exposed to oxygen, and Fe(III)-grown cells were grown anaerobically. These results suggest that the apparently high Geobacter cydA and sodA expression during bioremediation cannot necessarily be attributed to oxidative stress and demonstrate that diagnosis of the metabolic status of subsurface microorganisms through transcript analysis should be coupled with appropriate geochemical analyses.}, keywords = {Anaerobiosis, Bacterial Proteins, Biodegradation, Environmental, Colorado, Ferric Compounds, Fumarates, Gene Expression Profiling, Geobacter, Oxidative Stress, Soil Microbiology, Uranium}, issn = {1751-7370}, doi = {10.1038/ismej.2008.126}, author = {Mouser, Paula J and Holmes, Dawn E and Perpetua, Lorrie A and DiDonato, Raymond and Postier, Brad and Liu, Anna and Lovley, Derek R} } @article {471, title = {Transcriptome of Geobacter uraniireducens growing in uranium-contaminated subsurface sediments.}, journal = {ISME J}, volume = {3}, year = {2009}, month = {2009 Feb}, pages = {216-30}, abstract = {To learn more about the physiological state of Geobacter species living in subsurface sediments, heat-sterilized sediments from a uranium-contaminated aquifer in Rifle, Colorado, were inoculated with Geobacter uraniireducens, a pure culture representative of the Geobacter species that predominates during in situ uranium bioremediation at this site. Whole-genome microarray analysis comparing sediment-grown G. uraniireducens with cells grown in defined culture medium indicated that there were 1084 genes that had higher transcript levels during growth in sediments. Thirty-four c-type cytochrome genes were upregulated in the sediment-grown cells, including several genes that are homologous to cytochromes that are required for optimal Fe(III) and U(VI) reduction by G. sulfurreducens. Sediment-grown cells also had higher levels of transcripts, indicative of such physiological states as nitrogen limitation, phosphate limitation and heavy metal stress. Quantitative reverse transcription PCR showed that many of the metabolic indicator genes that appeared to be upregulated in sediment-grown G. uraniireducens also showed an increase in expression in the natural community of Geobacter species present during an in situ uranium bioremediation field experiment at the Rifle site. These results demonstrate that it is feasible to monitor gene expression of a microorganism growing in sediments on a genome scale and that analysis of the physiological status of a pure culture growing in subsurface sediments can provide insights into the factors controlling the physiology of natural subsurface communities.}, keywords = {Colorado, DNA, Bacterial, Environmental Microbiology, Gene Expression Profiling, Geobacter, Geologic Sediments, Molecular Sequence Data, Oligonucleotide Array Sequence Analysis, Sequence Analysis, DNA, Uranium}, issn = {1751-7370}, doi = {10.1038/ismej.2008.89}, author = {Holmes, Dawn E and O{\textquoteright}Neil, Regina A and Chavan, Milind A and N{\textquoteright}guessan, Lucie A and Vrionis, Helen A and Perpetua, Lorrie A and Larrahondo, M Juliana and DiDonato, Raymond and Liu, Anna and Lovley, Derek R} } @article {488, title = {Gene transcript analysis of assimilatory iron limitation in Geobacteraceae during groundwater bioremediation.}, journal = {Environ Microbiol}, volume = {10}, year = {2008}, month = {2008 May}, pages = {1218-30}, abstract = {Limitations on the availability of Fe(III) as an electron acceptor are thought to play an important role in restricting the growth and activity of Geobacter species during bioremediation of contaminated subsurface environments, but the possibility that these organisms might also be limited in the subsurface by the availability of iron for assimilatory purposes was not previously considered because copious quantities of Fe(II) are produced as the result of Fe(III) reduction. Analysis of multiple Geobacteraceae genomes revealed the presence of a three-gene cluster consisting of homologues of two iron-dependent regulators, fur and dtxR (ideR), separated by a homologue of feoB, which encodes an Fe(II) uptake protein. This cluster appears to be conserved among members of the Geobacteraceae and was detected in several environments. Expression of the fur-feoB-ideR cluster decreased as Fe(II) concentrations increased in chemostat cultures. The number of Geobacteraceae feoB transcripts in groundwater samples from a site undergoing in situ uranium bioremediation was relatively high until the concentration of dissolved Fe(II) increased near the end of the field experiment. These results suggest that, because much of the Fe(II) is sequestered in solid phases, Geobacter species, which have a high requirement for iron for iron-sulfur proteins, may be limited by the amount of iron available for assimilatory purposes. These results demonstrate the ability of transcript analysis to reveal previously unsuspected aspects of the in situ physiology of microorganisms in subsurface environments.}, keywords = {Bacterial Proteins, Biodegradation, Environmental, Culture Media, Ferric Compounds, Ferrous Compounds, Fresh Water, Gene Expression Regulation, Bacterial, Geobacter, Iron, Multigene Family, Phylogeny, Polymerase Chain Reaction, Repressor Proteins, Reverse Transcriptase Polymerase Chain Reaction, Transcription, Genetic, Uranium, Water Pollution, Radioactive}, issn = {1462-2920}, doi = {10.1111/j.1462-2920.2007.01537.x}, author = {O{\textquoteright}Neil, Regina A and Holmes, Dawn E and Coppi, Maddalena V and Adams, Lorrie A and Larrahondo, M Juliana and Ward, Joy E and Nevin, Kelly P and Woodard, Trevor L and Vrionis, Helen A and N{\textquoteright}guessan, Lucie A 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 {472, title = {Highly conserved genes in Geobacter species with expression patterns indicative of acetate limitation.}, journal = {Microbiology}, volume = {154}, year = {2008}, month = {2008 Sep}, pages = {2589-99}, abstract = {Analysis of the genome of Geobacter sulfurreducens revealed four genes encoding putative symporters with homology to ActP, an acetate transporter in Escherichia coli. Three of these genes, aplA, aplB and aplC, are highly similar (over 90 \% identical) and fell within a tight phylogenetic cluster (Group I) consisting entirely of Geobacter homologues. Transcript levels for all three genes increased in response to acetate limitation. The fourth gene, aplD, is phylogenetically distinct (Group II) and its expression was not influenced by acetate availability. Deletion of any one of the three genes in Group I did not significantly affect acetate-dependent growth, suggesting functional redundancy. Attempts to recover mutants in which various combinations of two of these genes were deleted were unsuccessful, suggesting that at least two of these three transporter genes are required to support growth. Closely related Group I apl genes were found in the genomes of other Geobacter species whose genome sequences are available. Furthermore, related genes could be detected in genomic DNA extracted from a subsurface environment undergoing in situ uranium bioremediation. The transporter genes recovered from the subsurface were most closely related to Group I apl genes found in the genomes of cultured Geobacter species that were isolated from contaminated subsurface environments. The increased expression of these genes in response to acetate limitation, their high degree of conservation among Geobacter species and the ease with which they can be detected in environmental samples suggest that Group I apl genes of the Geobacteraceae may be suitable biomarkers for acetate limitation. Monitoring the expression of these genes could aid in the design of strategies for acetate-mediated in situ bioremediation of uranium-contaminated groundwater.}, keywords = {Acetates, Biodegradation, Environmental, DNA, Bacterial, Escherichia coli, Escherichia coli Proteins, Gene Deletion, Gene Expression, Genes, Bacterial, Genome, Bacterial, Geobacter, Membrane Transport Proteins, Phylogeny, Uranium}, issn = {1350-0872}, doi = {10.1099/mic.0.2008/017244-0}, author = {Risso, Carla and Meth{\'e}, Barbara A and Elifantz, Hila and Holmes, Dawn E 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 {506, title = {Reclassification of Trichlorobacter thiogenes as Geobacter thiogenes comb. nov.}, journal = {Int J Syst Evol Microbiol}, volume = {57}, year = {2007}, month = {2007 Mar}, pages = {463-6}, abstract = {Reclassification of the species Trichlorobacter thiogenes as Geobacter thiogenes comb. nov. is proposed on the basis of physiological traits and phylogenetic position. Characteristics additional to those provided in the original description revealed that the type strain (strain K1(T)=ATCC BAA-34(T)=JCM 14045(T)) has the ability to use Fe(III) as an electron acceptor for acetate oxidation and has an electron donor and acceptor profile typical of a Geobacter species, contains abundant c-type cytochromes, and has a temperature optimum of 30 degrees C and a pH optimum near pH 7.0; traits typical of members of the genus Geobacter. Phylogenetic analysis of nifD, recA, gyrB, rpoB, fusA and 16S rRNA genes further indicated that T. thiogenes falls within the Geobacter cluster of the family Geobacteraceae. Based on extensive phylogenetic evidence and the fact that T. thiogenes has the hallmark physiological characteristics of a Geobacter species, Trichlorobacter thiogenes should be reclassified as a member of the genus Geobacter.}, keywords = {DNA, Bacterial, DNA, Ribosomal, Genes, Bacterial, Geobacter, Phylogeny, RNA, Ribosomal, 16S, Temperature}, issn = {1466-5026}, doi = {10.1099/ijs.0.63408-0}, author = {Nevin, Kelly P and Holmes, Dawn E and Woodard, Trevor L and Covalla, Sean F 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 {515, title = {c-Type cytochromes in Pelobacter carbinolicus.}, journal = {Appl Environ Microbiol}, volume = {72}, year = {2006}, month = {2006 Nov}, pages = {6980-5}, abstract = {Previous studies failed to detect c-type cytochromes in Pelobacter species despite the fact that other close relatives in the Geobacteraceae, such as Geobacter and Desulfuromonas species, have abundant c-type cytochromes. Analysis of the recently completed genome sequence of Pelobacter carbinolicus revealed 14 open reading frames that could encode c-type cytochromes. Transcripts for all but one of these open reading frames were detected in acetoin-fermenting and/or Fe(III)-reducing cells. Three putative c-type cytochrome genes were expressed specifically during Fe(III) reduction, suggesting that the encoded proteins may participate in electron transfer to Fe(III). One of these proteins was a periplasmic triheme cytochrome with a high level of similarity to PpcA, which has a role in Fe(III) reduction in Geobacter sulfurreducens. Genes for heme biosynthesis and system II cytochrome c biogenesis were identified in the genome and shown to be expressed. Sodium dodecyl sulfate-polyacrylamide gel electrophoresis gels of protein extracted from acetoin-fermenting P. carbinolicus cells contained three heme-staining bands which were confirmed by mass spectrometry to be among the 14 predicted c-type cytochromes. The number of cytochrome genes, the predicted amount of heme c per protein, and the ratio of heme-stained protein to total protein were much smaller in P. carbinolicus than in G. sulfurreducens. Furthermore, many of the c-type cytochromes that genetic studies have indicated are required for optimal Fe(III) reduction in G. sulfurreducens were not present in the P. carbinolicus genome. These results suggest that further evaluation of the functions of c-type cytochromes in the Geobacteraceae is warranted.}, keywords = {Bacterial Proteins, Cytochromes c, Deltaproteobacteria, Heme, Polymerase Chain Reaction, Proteomics, Reverse Transcriptase Polymerase Chain Reaction, RNA, Messenger}, issn = {0099-2240}, doi = {10.1128/AEM.01128-06}, author = {Haveman, Shelley A and Holmes, Dawn E and Ding, Yan-Huai R and Ward, Joy E and Didonato, Raymond J and Lovley, Derek R} } @article {513, title = {Microarray and genetic analysis of electron transfer to electrodes in Geobacter sulfurreducens.}, journal = {Environ Microbiol}, volume = {8}, year = {2006}, month = {2006 Oct}, pages = {1805-15}, abstract = {Whole-genome analysis of gene expression in Geobacter sulfurreducens revealed 474 genes with transcript levels that were significantly different during growth with an electrode as the sole electron acceptor versus growth on Fe(III) citrate. The greatest response was a more than 19-fold increase in transcript levels for omcS, which encodes an outer-membrane cytochrome previously shown to be required for Fe(III) oxide reduction. Quantitative reverse transcription polymerase chain reaction and Northern analyses confirmed the higher levels of omcS transcripts, which increased as power production increased. Deletion of omcS inhibited current production that was restored when omcS was expressed in trans. Transcript expression and genetic analysis suggested that OmcE, another outer-membrane cytochrome, is also involved in electron transfer to electrodes. Surprisingly, genes for other proteins known to be important in Fe(III) reduction such as the outer-membrane c-type cytochrome, OmcB, and the electrically conductive pilin "nanowires" did not have higher transcript levels on electrodes, and deletion of the relevant genes did not inhibit power production. Changes in the transcriptome suggested that cells growing on electrodes were subjected to less oxidative stress than cells growing on Fe(III) citrate and that a number of genes annotated as encoding metal efflux proteins or proteins of unknown function may be important for growth on electrodes. These results demonstrate for the first time that it is possible to evaluate gene expression, and hence the metabolic state, of microorganisms growing on electrodes on a genome-wide basis and suggest that OmcS, and to a lesser extent OmcE, are important in electron transfer to electrodes. This has important implications for the design of electrode materials and the genetic engineering of microorganisms to improve the function of microbial fuel cells.}, keywords = {Bacterial Outer Membrane Proteins, Blotting, Northern, Cytochromes c, Electrodes, Electrophysiology, Gene Expression Regulation, Bacterial, Geobacter, Oligonucleotide Array Sequence Analysis, Oxidation-Reduction, Reverse Transcriptase Polymerase Chain Reaction, RNA, Bacterial, RNA, Messenger}, issn = {1462-2912}, doi = {10.1111/j.1462-2920.2006.01065.x}, author = {Holmes, Dawn E and Chaudhuri, Swades K and Nevin, Kelly P and Mehta, Teena and Meth{\'e}, Barbara A and Liu, Anna and Ward, Joy E and Woodard, Trevor L and Webster, Jennifer 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 {529, title = {Potential for quantifying expression of the Geobacteraceae citrate synthase gene to assess the activity of Geobacteraceae in the subsurface and on current-harvesting electrodes.}, journal = {Appl Environ Microbiol}, volume = {71}, year = {2005}, month = {2005 Nov}, pages = {6870-7}, abstract = {The Geobacteraceae citrate synthase is phylogenetically distinct from those of other prokaryotes and is a key enzyme in the central metabolism of Geobacteraceae. Therefore, the potential for using levels of citrate synthase mRNA to estimate rates of Geobacter metabolism was evaluated in pure culture studies and in four different Geobacteraceae-dominated environments. Quantitative reverse transcription-PCR studies with mRNA extracted from cultures of Geobacter sulfurreducens grown in chemostats with Fe(III) as the electron acceptor or in batch with electrodes as the electron acceptor indicated that transcript levels of the citrate synthase gene, gltA, increased with increased rates of growth/Fe(III) reduction or current production, whereas the expression of the constitutively expressed housekeeping genes recA, rpoD, and proC remained relatively constant. Analysis of mRNA extracted from groundwater collected from a U(VI)-contaminated site undergoing in situ uranium bioremediation revealed a remarkable correspondence between acetate levels in the groundwater and levels of transcripts of gltA. The expression of gltA was also significantly greater in RNA extracted from groundwater beneath a highway runoff recharge pool that was exposed to calcium magnesium acetate in June, when acetate concentrations were high, than in October, when the levels had significantly decreased. It was also possible to detect gltA transcripts on current-harvesting anodes deployed in freshwater sediments. These results suggest that it is possible to monitor the in situ metabolic rate of Geobacteraceae by tracking the expression of the citrate synthase gene.}, keywords = {Acetates, Citrate (si)-Synthase, Deltaproteobacteria, DNA, Ribosomal, Electrodes, Ferric Compounds, Fresh Water, Geobacter, Geologic Sediments, Petroleum, Phylogeny, RNA, Ribosomal, 16S, Uranium, Water Pollutants, Chemical, Water Pollutants, Radioactive}, issn = {0099-2240}, doi = {10.1128/AEM.71.11.6870-6877.2005}, author = {Holmes, Dawn E and Nevin, Kelly P and O{\textquoteright}Neil, Regina A and Ward, Joy E and Adams, Lorrie A and Woodard, Trevor L and Vrionis, Helen A 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 {545, title = {Dissimilatory Fe(III) and Mn(IV) reduction.}, journal = {Adv Microb Physiol}, volume = {49}, year = {2004}, month = {2004}, pages = {219-86}, abstract = {Dissimilatory Fe(III) and Mn(IV) reduction has an important influence on the geochemistry of modern environments, and Fe(III)-reducing microorganisms, most notably those in the Geobacteraceae family, can play an important role in the bioremediation of subsurface environments contaminated with organic or metal contaminants. Microorganisms with the capacity to conserve energy from Fe(III) and Mn(IV) reduction are phylogenetically dispersed throughout the Bacteria and Archaea. The ability to oxidize hydrogen with the reduction of Fe(III) is a highly conserved characteristic of hyperthermophilic microorganisms and one Fe(III)-reducing Archaea grows at the highest temperature yet recorded for any organism. Fe(III)- and Mn(IV)-reducing microorganisms have the ability to oxidize a wide variety of organic compounds, often completely to carbon dioxide. Typical alternative electron acceptors for Fe(III) reducers include oxygen, nitrate, U(VI) and electrodes. Unlike other commonly considered electron acceptors, Fe(III) and Mn(IV) oxides, the most prevalent form of Fe(III) and Mn(IV) in most environments, are insoluble. Thus, Fe(III)- and Mn(IV)-reducing microorganisms face the dilemma of how to transfer electrons derived from central metabolism onto an insoluble, extracellular electron acceptor. Although microbiological and geochemical evidence suggests that Fe(III) reduction may have been the first form of microbial respiration, the capacity for Fe(III) reduction appears to have evolved several times as phylogenetically distinct Fe(III) reducers have different mechanisms for Fe(III) reduction. Geobacter species, which are representative of the family of Fe(III) reducers that predominate in a wide diversity of sedimentary environments, require direct contact with Fe(III) oxides in order to reduce them. In contrast, Shewanella and Geothrix species produce chelators that solubilize Fe(III) and release electron-shuttling compounds that transfer electrons from the cell surface to the surface of Fe(III) oxides not in direct contact with the cells. Electron transfer from the inner membrane to the outer membrane in Geobacter and Shewanella species appears to involve an electron transport chain of inner-membrane, periplasmic, and outer-membrane c-type cytochromes, but the cytochromes involved in these processes in the two organisms are different. In addition, Geobacter species specifically express flagella and pili during growth on Fe(III) and Mn(IV) oxides and are chemotactic to Fe(II) and Mn(II), which may lead Geobacter species to the oxides under anoxic conditions. The physiological characteristics of Geobacter species appear to explain why they have consistently been found to be the predominant Fe(III)- and Mn(IV)-reducing microorganisms in a variety of sedimentary environments. In comparison with other respiratory processes, the study of Fe(III) and Mn(IV) reduction is in its infancy, but genome-enabled approaches are rapidly advancing our understanding of this environmentally significant physiology.}, keywords = {Archaea, Biodegradation, Environmental, Ferric Compounds, Geobacter, Manganese, Manganese Compounds, Oxidation-Reduction, Oxides, Shewanella, Soil Microbiology, Soil Pollutants}, issn = {0065-2911}, doi = {10.1016/S0065-2911(04)49005-5}, author = {Lovley, Derek R and Holmes, Dawn E and Nevin, Kelly P} } @article {559, title = {Electron transfer by Desulfobulbus propionicus to Fe(III) and graphite electrodes.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Feb}, pages = {1234-7}, abstract = {Desulfobulbus propionicus was able to grow with Fe(III), the humic acids analog anthraquinone-2,6-disulfonate (AQDS), or a graphite electrode as an electron acceptor. These results provide an explanation for the enrichment of Desulfobulbaceae species on the surface of electrodes harvesting electricity from anaerobic marine sediments and further expand the diversity of microorganisms known to have the ability to use both sulfate and Fe(III) as an electron acceptor.}, keywords = {Culture Media, Deltaproteobacteria, Electrodes, Electron Transport, Ferric Compounds, Graphite, Oxidation-Reduction, Pyruvic Acid, Sulfates}, issn = {0099-2240}, author = {Holmes, Dawn E and Bond, Daniel R and Lovley, Derek R} } @article {543, title = {In situ expression of nifD in Geobacteraceae in subsurface sediments.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Dec}, pages = {7251-9}, abstract = {In order to determine whether the metabolic state of Geobacteraceae involved in bioremediation of subsurface sediments might be inferred from levels of mRNA for key genes, in situ expression of nifD, a highly conserved gene involved in nitrogen fixation, was investigated. When Geobacter sulfurreducens was grown without a source of fixed nitrogen in chemostats with acetate provided as the limiting electron donor and Fe(III) as the electron acceptor, levels of nifD transcripts were 4 to 5 orders of magnitude higher than in chemostat cultures provided with ammonium. In contrast, the number of transcripts of recA and the 16S rRNA gene were slightly lower in the absence of ammonium. The addition of acetate to organic- and nitrogen-poor subsurface sediments stimulated the growth of Geobacteraceae and Fe(III) reduction, as well as the expression of nifD in Geobacteraceae. Levels of nifD transcripts in Geobacteraceae decreased more than 100-fold within 2 days after the addition of 100 microM ammonium, while levels of recA and total bacterial 16S rRNA in Geobacteraceae remained relatively constant. Ammonium amendments had no effect on rates of Fe(III) reduction in acetate-amended sediments or toluene degradation in petroleum-contaminated sediments, suggesting that other factors, such as the rate that Geobacteraceae could access Fe(III) oxides, limited Fe(III) reduction. These results demonstrate that it is possible to monitor one aspect of the in situ metabolic state of Geobacteraceae species in subsurface sediments via analysis of mRNA levels, which is the first step toward a more global analysis of in situ gene expression related to nutrient status and stress response during bioremediation by Geobacteraceae.}, keywords = {Acetates, Biodegradation, Environmental, Culture Media, DNA, Ribosomal, Fresh Water, Gene Expression Regulation, Bacterial, Geobacter, Geologic Sediments, Nitrogenase, Petroleum, Phylogeny, Polymerase Chain Reaction, Quaternary Ammonium Compounds, Rec A Recombinases, RNA, Ribosomal, 16S, Water Pollutants, Chemical}, issn = {0099-2240}, doi = {10.1128/AEM.70.12.7251-7259.2004}, author = {Holmes, Dawn E and Nevin, Kelly P and Lovley, Derek R} } @article {546, title = {Potential role of a novel psychrotolerant member of the family Geobacteraceae, Geopsychrobacter electrodiphilus gen. nov., sp. nov., in electricity production by a marine sediment fuel cell.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Oct}, pages = {6023-30}, abstract = {Previous studies have shown that members of the family Geobacteraceae that attach to the anodes of sediment fuel cells are directly involved in harvesting electricity by oxidizing organic compounds to carbon dioxide and transferring the electrons to the anode. In order to learn more about this process, microorganisms from the anode surface of a marine sediment fuel cell were enriched and isolated with Fe(III) oxide. Two unique marine isolates were recovered, strains A1(T) and A2. They are gram-negative, nonmotile rods, with abundant c-type cytochromes. Phylogenetic analysis of the 16S rRNA, recA, gyrB, fusA, rpoB, and nifD genes indicated that strains A1(T) and A2 represent a unique phylogenetic cluster within the Geobacteraceae. Both strains were able to grow with an electrode serving as the sole electron acceptor and transferred ca. 90\% of the electrons available in their organic electron donors to the electrodes. These organisms are the first psychrotolerant members of the Geobacteraceae reported thus far and can grow at temperatures between 4 and 30 degrees C, with an optimum temperature of 22 degrees C. Strains A1(T) and A2 can utilize a wide range of traditional electron acceptors, including all forms of soluble and insoluble Fe(III) tested, anthraquinone 2,6-disulfonate, and S(0). In addition to acetate, both strains can utilize a number of other organic acids, amino acids, long-chain fatty acids, and aromatic compounds to support growth with Fe(III) nitrilotriacetic acid as an electron acceptor. The metabolism of these organisms differs in that only strain A1(T) can use acetoin, ethanol, and hydrogen as electron donors, whereas only strain A2 can use lactate, propionate, and butyrate. The name Geopsychrobacter electrodiphilus gen. nov., sp. nov., is proposed for strains A1(T) and A2, with strain A1(T) (ATCC BAA-880(T); DSM 16401(T); JCM 12469) as the type strain. Strains A1(T) and A2 (ATCC BAA-770; JCM 12470) represent the first organisms recovered from anodes that can effectively couple the oxidation of organic compounds to an electrode. Thus, they may serve as important model organisms for further elucidation of the mechanisms of microbe-electrode electron transfer in sediment fuel cells.}, keywords = {Bioelectric Energy Sources, Cytochromes, Deltaproteobacteria, Electron Transport, Genes, Bacterial, Geologic Sediments, Microscopy, Electron, Molecular Sequence Data, Phylogeny, RNA, Bacterial, RNA, Ribosomal, 16S, Temperature}, issn = {0099-2240}, doi = {10.1128/AEM.70.10.6023-6030.2004}, author = {Holmes, Dawn E and Nicoll, Julie S and Bond, Daniel R and Lovley, Derek R} } @article {569, title = {Thermophily in the Geobacteraceae: Geothermobacter ehrlichii gen. nov., sp. nov., a novel thermophilic member of the Geobacteraceae from the "Bag City" hydrothermal vent.}, journal = {Appl Environ Microbiol}, volume = {69}, year = {2003}, month = {2003 May}, pages = {2985-93}, abstract = {Little is known about the microbiology of the "Bag City" hydrothermal vent, which is part of a new eruption site on the Juan de Fuca Ridge and which is notable for its accumulation of polysaccharide on the sediment surface. A pure culture, designated strain SS015, was recovered from a vent fluid sample from the Bag City site through serial dilution in liquid medium with malate as the electron donor and Fe(III) oxide as the electron acceptor and then isolation of single colonies on solid Fe(III) oxide medium. The cells were gram-negative rods, about 0.5 micro m by 1.2 to 1.5 micro m, and motile and contained c-type cytochromes. Analysis of the 16S ribosomal DNA (rDNA) sequence of strain SS015 placed it in the family Geobacteraceae in the delta subclass of the Proteobacteria. Unlike previously described members of the Geobacteraceae, which are mesophiles, strain SS015 was a thermophile and grew at temperatures of between 35 and 65 degrees C, with an optimum temperature of 55 degrees C. Like many previously described members of the Geobacteraceae, strain SS015 grew with organic acids as the electron donors and Fe(III) or nitrate as the electron acceptor, with nitrate being reduced to ammonia. Strain SS015 was unique among the Geobacteraceae in its ability to use sugars, starch, or amino acids as electron donors for Fe(III) reduction. Under stress conditions, strain SS015 produced copious quantities of extracellular polysaccharide, providing a model for the microbial production of the polysaccharide accumulation at the Bag City site. The 16S rDNA sequence of strain SS015 was less than 94\% similar to the sequences of previously described members of the Geobacteraceae; this fact, coupled with its unique physiological properties, suggests that strain SS015 represents a new genus in the family Geobacteraceae. The name Geothermobacter ehrlichii gen. nov., sp. nov., is proposed (ATCC BAA-635 and DSM 15274). Although strains of Geobacteraceae are known to be the predominant Fe(III)-reducing microorganisms in a variety of Fe(III)-reducing environments at moderate temperatures, strain SS015 represents the first described thermophilic member of the Geobacteraceae and thus extends the known environmental range of this family to hydrothermal environments.}, keywords = {Base Composition, Cytochromes, Deltaproteobacteria, DNA, Bacterial, DNA, Ribosomal, Drug Resistance, Bacterial, Ecosystem, Electron Transport, Geologic Sediments, Hot Temperature, Hydrogen-Ion Concentration, Iron, Microscopy, Electron, Molecular Sequence Data, Oxidation-Reduction, Pacific Ocean, Phylogeny, Seawater, Sodium Chloride, Species Specificity}, issn = {0099-2240}, author = {Kashefi, Kazem and Holmes, Dawn E and Baross, John A and Lovley, Derek R} } @article {588, title = {Electrode-reducing microorganisms that harvest energy from marine sediments.}, journal = {Science}, volume = {295}, year = {2002}, month = {2002 Jan 18}, pages = {483-5}, abstract = {Energy in the form of electricity can be harvested from marine sediments by placing a graphite electrode (the anode) in the anoxic zone and connecting it to a graphite cathode in the overlying aerobic water. We report a specific enrichment of microorganisms of the family Geobacteraceae on energy-harvesting anodes, and we show that these microorganisms can conserve energy to support their growth by oxidizing organic compounds with an electrode serving as the sole electron acceptor. This finding not only provides a method for extracting energy from organic matter, but also suggests a strategy for promoting the bioremediation of organic contaminants in subsurface environments.}, keywords = {Aerobiosis, Anaerobiosis, Anthraquinones, Benzoates, Biodegradation, Environmental, Carbon Dioxide, Colony Count, Microbial, Deltaproteobacteria, DNA, Ribosomal, Electricity, Electrodes, Electrons, Energy Metabolism, Geologic Sediments, Oxidation-Reduction, RNA, Ribosomal, 16S, Seawater, Sodium Acetate}, issn = {1095-9203}, doi = {10.1126/science.1066771}, author = {Bond, Daniel R and Holmes, Dawn E and Tender, Leonard M and Lovley, Derek R} } @article {583, title = {Enrichment of members of the family Geobacteraceae associated with stimulation of dissimilatory metal reduction in uranium-contaminated aquifer sediments.}, journal = {Appl Environ Microbiol}, volume = {68}, year = {2002}, month = {2002 May}, pages = {2300-6}, abstract = {Stimulating microbial reduction of soluble U(VI) to insoluble U(IV) shows promise as a strategy for immobilizing uranium in uranium-contaminated subsurface environments. In order to learn more about which microorganisms might be involved in U(VI) reduction in situ, the changes in the microbial community when U(VI) reduction was stimulated with the addition of acetate were monitored in sediments from three different uranium-contaminated sites in the floodplain of the San Juan River in Shiprock, N.Mex. In all three sediments U(VI) reduction was accompanied by concurrent Fe(III) reduction and a dramatic enrichment of microorganisms in the family Geobacteraceae, which are known U(VI)- and Fe(III)-reducing microorganisms. At the point when U(VI) reduction and Fe(III) reduction were nearing completion, Geobacteraceae accounted for ca. 40\% of the 16S ribosomal DNA (rDNA) sequences recovered from the sediments with bacterial PCR primers, whereas Geobacteraceae accounted for fewer than 5\% of the 16S rDNA sequences in control sediments that were not amended with acetate and in which U(VI) and Fe(III) reduction were not stimulated. Between 55 and 65\% of these Geobacteraceae sequences were most similar to sequences from Desulfuromonas species, with the remainder being most closely related to Geobacter species. Quantitative analysis of Geobacteraceae sequences with most-probable-number PCR and TaqMan analyses indicated that the number of Geobacteraceae sequences increased from 2 to 4 orders of magnitude over the course of U(VI) and Fe(III) reduction in the acetate-amended sediments from the three sites. No increase in Geobacteraceae sequences was observed in control sediments. In contrast to the predominance of Geobacteraceae sequences, no sequences related to other known Fe(III)-reducing microorganisms were detected in sediments. These results compare favorably with an increasing number of studies which have demonstrated that Geobacteraceae are important components of the microbial community in a diversity of subsurface environments in which Fe(III) reduction is an important process. The combination of these results with the finding that U(VI) reduction takes place during Fe(III) reduction and prior to sulfate reduction suggests that Geobacteraceae will be responsible for much of the Fe(III) and U(VI) reduction during uranium bioremediation in these sediments.}, keywords = {Gene Library, Geologic Sediments, Iron, Oxidation-Reduction, Proteobacteria, RNA, Ribosomal, 16S, Soil Pollutants, Uranium}, issn = {0099-2240}, author = {Holmes, Dawn E and Finneran, Kevin T and O{\textquoteright}Neil, Regina A and Lovley, Derek R} } @article {581, title = {Geoglobus ahangari gen. nov., sp. nov., a novel hyperthermophilic archaeon capable of oxidizing organic acids and growing autotrophically on hydrogen with Fe(III) serving as the sole electron acceptor.}, journal = {Int J Syst Evol Microbiol}, volume = {52}, year = {2002}, month = {2002 May}, pages = {719-28}, abstract = {A novel, regular to irregular, coccoid-shaped, anaerobic, Fe(III)-reducing microorganism was isolated from the Guaymas Basin hydrothermal system at a depth of 2000 m. Isolation was carried out with a new technique using Fe(III) oxide as the electron acceptor for the recovery of colonies on solid medium. The isolate, designated strain 234T, was strictly anaerobic and exhibited a tumbling motility. The cells had a single flagellum. Strain 234T grew at temperatures between 65 and 90 degrees C, with an optimum at about 88 degrees C. The optimal salt concentration for growth was around 19 g l(-1). The isolate was capable of growth with H2 as the sole electron donor coupled to the reduction of Fe(III) without the need for an organic carbon source. This is the first example of a dissimilatory Fe(III)-reducing micro-organism capable of growing autotrophically on hydrogen. In addition to molecular hydrogen, strain 234T oxidizes pyruvate, acetate, malate, succinate, peptone, formate, fumarate, yeast extract, glycerol, isoleucine, arginine, serine, glutamine, asparagine, stearate, palmitate, valerate, butyrate and propionate with the reduction of Fe(III). This isolate is the first example of a hyperthermophile capable of oxidizing long-chain fatty acids anaerobically. Isolate 234T grew exclusively with Fe(III) as the sole electron acceptor. The G+C content was 58.7 mol\%. Based on detailed analysis of its 16S rDNA sequence, G+C content, distinguishing physiological features and metabolism, strain 234T is proposed to represent a novel genus within the Archaeoglobales. The name proposed for strain 234T is Geoglobus ahangari gen. nov., sp. nov..}, keywords = {Anaerobiosis, Archaea, Bacterial Typing Techniques, DNA, Ribosomal, Electron Transport, Fatty Acids, Ferric Compounds, Hot Temperature, Hydrogen, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Water Microbiology}, issn = {1466-5026}, author = {Kashefi, Kazem and Tor, Jason M and Holmes, Dawn E and Gaw Van Praagh, Catherine V and Reysenbach, Anna-Louise and Lovley, Derek R} } @article {580, title = {Harnessing microbially generated power on the seafloor.}, journal = {Nat Biotechnol}, volume = {20}, year = {2002}, month = {2002 Aug}, pages = {821-5}, abstract = {In many marine environments, a voltage gradient exists across the water sediment interface resulting from sedimentary microbial activity. Here we show that a fuel cell consisting of an anode embedded in marine sediment and a cathode in overlying seawater can use this voltage gradient to generate electrical power in situ. Fuel cells of this design generated sustained power in a boat basin carved into a salt marsh near Tuckerton, New Jersey, and in the Yaquina Bay Estuary near Newport, Oregon. Retrieval and analysis of the Tuckerton fuel cell indicates that power generation results from at least two anode reactions: oxidation of sediment sulfide (a by-product of microbial oxidation of sedimentary organic carbon) and oxidation of sedimentary organic carbon catalyzed by microorganisms colonizing the anode. These results demonstrate in real marine environments a new form of power generation that uses an immense, renewable energy reservoir (sedimentary organic carbon) and has near-immediate application.}, keywords = {Bacteria, Bioelectric Energy Sources, Biotechnology, Carbon, Conservation of Energy Resources, DNA, Ribosomal, Electricity, Electrodes, Environmental Microbiology, Geologic Sediments, Molecular Sequence Data, New Jersey, Oceans and Seas, Oregon, Oxidation-Reduction, RNA, Bacterial, RNA, Ribosomal, 16S, Sulfides}, issn = {1087-0156}, doi = {10.1038/nbt716}, author = {Tender, Leonard M and Reimers, Clare E and Stecher, Hilmar A and Holmes, Dawn E and Bond, Daniel R and Lowy, Daniel A and Pilobello, Kanoelani and Fertig, Stephanie J and Lovley, Derek R} } @article {587, title = {Use of Fe(III) as an electron acceptor to recover previously uncultured hyperthermophiles: isolation and characterization of Geothermobacterium ferrireducens gen. nov., sp. nov.}, journal = {Appl Environ Microbiol}, volume = {68}, year = {2002}, month = {2002 Apr}, pages = {1735-42}, abstract = {It has recently been recognized that the ability to use Fe(III) as a terminal electron acceptor is a highly conserved characteristic in hyperthermophilic microorganisms. This suggests that it may be possible to recover as-yet-uncultured hyperthermophiles in pure culture if Fe(III) is used as an electron acceptor. As part of a study of the microbial diversity of the Obsidian Pool area in Yellowstone National Park, Wyo., hot sediment samples were used as the inoculum for enrichment cultures in media containing hydrogen as the sole electron donor and poorly crystalline Fe(III) oxide as the electron acceptor. A pure culture was recovered on solidified, Fe(III) oxide medium. The isolate, designated FW-1a, is a hyperthermophilic anaerobe that grows exclusively by coupling hydrogen oxidation to the reduction of poorly crystalline Fe(III) oxide. Organic carbon is not required for growth. Magnetite is the end product of Fe(III) oxide reduction under the culture conditions evaluated. The cells are rod shaped, about 0.5 microm by 1.0 to 1.2 microm, and motile and have a single flagellum. Strain FW-1a grows at circumneutral pH, at freshwater salinities, and at temperatures of between 65 and 100 degrees C with an optimum of 85 to 90 degrees C. To our knowledge this is the highest temperature optimum of any organism in the Bacteria. Analysis of the 16S ribosomal DNA (rDNA) sequence of strain FW-1a places it within the Bacteria, most closely related to abundant but uncultured microorganisms whose 16S rDNA sequences have been previously recovered from Obsidian Pool and a terrestrial hot spring in Iceland. While previous studies inferred that the uncultured microorganisms with these 16S rDNA sequences were sulfate-reducing organisms, the physiology of the strain FW-1a, which does not reduce sulfate, indicates that these organisms are just as likely to be Fe(III) reducers. These results further demonstrate that Fe(III) may be helpful for recovering as-yet-uncultured microorganisms from hydrothermal environments and illustrate that caution must be used in inferring the physiological characteristics of at least some thermophilic microorganisms solely from 16S rDNA sequences. Based on both its 16S rDNA sequence and physiological characteristics, strain FW-1a represents a new genus among the Bacteria. The name Geothermobacterium ferrireducens gen. nov., sp. nov., is proposed (ATCC BAA-426).}, keywords = {Bacterial Typing Techniques, Culture Media, DNA, Ribosomal, Electron Transport, Ferric Compounds, Fresh Water, Geologic Sediments, Gram-Negative Anaerobic Bacteria, Hot Temperature, Molecular Sequence Data, RNA, Ribosomal, 16S, Sequence Analysis, DNA}, issn = {0099-2240}, author = {Kashefi, Kazem and Holmes, Dawn E and Reysenbach, Anna-Louise and Lovley, Derek R} }