@article {3054,
	title = {Electrotrophy: Other microbial species, iron, and electrodes as electron donors for microbial respirations.},
	journal = {Bioresour Technol},
	volume = {345},
	year = {2022},
	month = {2022 Feb},
	pages = {126553},
	abstract = {<p>Electrotrophy, the growth of microbes on extracellular electron donors, drives important biogeochemical cycles and has practical applications. Studies of Fe(II)-based electrotrophy have provided foundational cytochrome-based mechanistic models for electron transport into cells. Direct electron uptake from other microbial species, Fe(0), or cathodes is of intense interest due to its potential roles in the production and anaerobic oxidation of methane, corrosion, and bioelectrochemical technologies. Other cells or Fe(0) can serve as the sole electron donor supporting the growth of several Geobacter and methanogen strains that are unable to use H as an electron donor, providing strong evidence for electrotrophy. Additional evidence for electrotrophy in Geobacter strains and Methanosarcina acetivorans is a requirement for outer-surface c-type cytochromes. However, in most instances claims for electrotrophy in anaerobes are based on indirect inference and the possibility that H is actually the electron donor supporting growth has not been rigorously excluded.</p>},
	keywords = {Electrodes, Electron Transport, Electrons, Geobacter, Iron, Oxidation-Reduction, Soil Microbiology},
	issn = {1873-2976},
	doi = {10.1016/j.biortech.2021.126553},
	author = {Lovley, Derek R}
}
@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 = {<p>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.</p>},
	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 {423,
	title = {Monitoring the metabolic status of geobacter species in contaminated groundwater by quantifying key metabolic proteins with Geobacter-specific antibodies.},
	journal = {Appl Environ Microbiol},
	volume = {77},
	year = {2011},
	month = {2011 Jul},
	pages = {4597-602},
	abstract = {Simple and inexpensive methods for assessing the metabolic status and bioremediation activities of subsurface microorganisms are required before bioremediation practitioners will adopt molecular diagnosis of the bioremediation community as a routine practice for guiding the development of bioremediation strategies. Quantifying gene transcripts can diagnose important aspects of microbial physiology during bioremediation but is technically challenging and does not account for the impact of translational modifications on protein abundance. An alternative strategy is to directly quantify the abundance of key proteins that might be diagnostic of physiological state. To evaluate this strategy, an antibody-based quantification approach was developed to investigate subsurface Geobacter communities. The abundance of citrate synthase corresponded with rates of metabolism of Geobacter bemidjiensis in chemostat cultures. During in situ bioremediation of uranium-contaminated groundwater the quantity of Geobacter citrate synthase increased with the addition of acetate to the groundwater and decreased when acetate amendments stopped. The abundance of the nitrogen-fixation protein, NifD, increased as ammonium became less available in the groundwater and then declined when ammonium concentrations increased. In a petroleum-contaminated aquifer, the abundance of BamB, an enzyme subunit involved in the anaerobic degradation of mono-aromatic compounds by Geobacter species, increased in zones in which Geobacter were expected to play an important role in aromatic hydrocarbon degradation. These results suggest that antibody-based detection of key metabolic proteins, which should be readily adaptable to standardized kits, may be a feasible method for diagnosing the metabolic state of microbial communities responsible for bioremediation, aiding in the rational design of bioremediation strategies.},
	keywords = {Acetates, Antibodies, Bacterial, Bacterial Proteins, Geobacter, Petroleum, Quaternary Ammonium Compounds, Soil Microbiology, Water Microbiology},
	issn = {1098-5336},
	doi = {10.1128/AEM.00114-11},
	author = {Yun, Jiae and Ueki, Toshiyuki and Miletto, Marzia and Lovley, Derek R}
}
@article {447,
	title = {Role of Geobacter sulfurreducens outer surface c-type cytochromes in reduction of soil humic acid and anthraquinone-2,6-disulfonate.},
	journal = {Appl Environ Microbiol},
	volume = {76},
	year = {2010},
	month = {2010 Apr},
	pages = {2371-5},
	abstract = {Deleting individual genes for outer surface c-type cytochromes in Geobacter sulfurreducens partially inhibited the reduction of humic substances and anthraquinone-2,6,-disulfonate. Complete inhibition was obtained only when five of these genes were simultaneously deleted, suggesting that diverse outer surface cytochromes can contribute to the reduction of humic substances and other extracellular quinones.},
	keywords = {Anthraquinones, Bacterial Proteins, Cytochromes, Gene Deletion, Genes, Bacterial, Geobacter, Humic Substances, Oxidation-Reduction, Soil, Soil Microbiology},
	issn = {1098-5336},
	doi = {10.1128/AEM.02250-09},
	author = {Voordeckers, James W and Kim, Byoung-Chan and Izallalen, Mounir 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 {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 {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}
}
