@article {3088, title = {Syntrophy Goes Electric: Direct Interspecies Electron Transfer.}, journal = {Annu Rev Microbiol}, volume = {71}, year = {2017}, month = {2017 Sep 08}, pages = {643-664}, abstract = {

Direct interspecies electron transfer (DIET) has biogeochemical significance, and practical applications that rely on DIET or DIET-based aspects of microbial physiology are growing. Mechanisms for DIET have primarily been studied in defined cocultures in which Geobacter species are one of the DIET partners. Electrically conductive pili (e-pili) can be an important electrical conduit for DIET. However, there may be instances in which electrical contacts are made between electron transport proteins associated with the outer membranes of the partners. Alternatively, DIET partners can plug into conductive carbon materials, such as granular activated carbon, carbon cloth, and biochar, for long-range electron exchange without the need for e-pili. Magnetite promotes DIET, possibly by acting as a substitute for outer-surface c-type cytochromes. DIET is the primary mode of interspecies electron exchange in some anaerobic digesters converting wastes to methane. Promoting DIET with conductive materials shows promise for stabilizing and accelerating methane production in digesters, permitting higher organic loading rates. Various lines of evidence suggest that DIET is important in terrestrial wetlands, which are an important source of atmospheric methane. DIET may also have a role in anaerobic methane oxidation coupled to sulfate reduction, an important control on methane releases. The finding that DIET can serve as the source of electrons for anaerobic photosynthesis further broadens its potential environmental significance. Microorganisms capable of DIET are good catalysts for several bioelectrochemical technologies and e-pili are a promising renewable source of electronic materials. The study of DIET is in its early stages, and additional investigation is required to better understand the diversity of microorganisms that are capable of DIET, the importance of DIET to carbon and electron flow in anaerobic environments, and the biochemistry and physiology of DIET.

}, keywords = {Anaerobiosis, Cytochromes, Electron Transport, Environmental Microbiology, Geobacter, Industrial Microbiology, Methane, Oxidation-Reduction}, issn = {1545-3251}, doi = {10.1146/annurev-micro-030117-020420}, author = {Lovley, Derek R} } @article {413, title = {Microbial functional gene diversity with a shift of subsurface redox conditions during In Situ uranium reduction.}, journal = {Appl Environ Microbiol}, volume = {78}, year = {2012}, month = {2012 Apr}, pages = {2966-72}, abstract = {To better understand the microbial functional diversity changes with subsurface redox conditions during in situ uranium bioremediation, key functional genes were studied with GeoChip, a comprehensive functional gene microarray, in field experiments at a uranium mill tailings remedial action (UMTRA) site (Rifle, CO). The results indicated that functional microbial communities altered with a shift in the dominant metabolic process, as documented by hierarchical cluster and ordination analyses of all detected functional genes. The abundance of dsrAB genes (dissimilatory sulfite reductase genes) and methane generation-related mcr genes (methyl coenzyme M reductase coding genes) increased when redox conditions shifted from Fe-reducing to sulfate-reducing conditions. The cytochrome genes detected were primarily from Geobacter sp. and decreased with lower subsurface redox conditions. Statistical analysis of environmental parameters and functional genes indicated that acetate, U(VI), and redox potential (E(h)) were the most significant geochemical variables linked to microbial functional gene structures, and changes in microbial functional diversity were strongly related to the dominant terminal electron-accepting process following acetate addition. The study indicates that the microbial functional genes clearly reflect the in situ redox conditions and the dominant microbial processes, which in turn influence uranium bioreduction. Microbial functional genes thus could be very useful for tracking microbial community structure and dynamics during bioremediation.}, keywords = {Biodegradation, Environmental, Biota, Environmental Microbiology, Environmental Pollutants, Genetic Variation, Microarray Analysis, Oxidation-Reduction, Uranium}, issn = {1098-5336}, doi = {10.1128/AEM.06528-11}, author = {Liang, Yuting and Van Nostrand, Joy D and N{\textquoteright}guessan, Lucie A and Peacock, Aaron D and Deng, Ye and Long, Philip E and Resch, C Tom and Wu, Liyou and He, Zhili and Li, Guanghe and Hazen, Terry C and Lovley, Derek R and Zhou, Jizhong} } @article {373, title = {PCR amplification-independent methods for detection of microbial communities by the high-density microarray PhyloChip.}, journal = {Appl Environ Microbiol}, volume = {77}, year = {2011}, month = {2011 Sep}, pages = {6313-22}, abstract = {Environmental microbial community analysis typically involves amplification by PCR, despite well-documented biases. We have developed two methods of PCR-independent microbial community analysis using the high-density microarray PhyloChip: direct hybridization of 16S rRNA (dirRNA) or rRNA converted to double-stranded cDNA (dscDNA). We compared dirRNA and dscDNA communities to PCR-amplified DNA communities using a mock community of eight taxa, as well as experiments derived from three environmental sample types: chromium-contaminated aquifer groundwater, tropical forest soil, and secondary sewage in seawater. Community profiles by both direct hybridization methods showed differences that were expected based on accompanying data but that were missing in PCR-amplified communities. Taxon richness decreased in RNA compared to that in DNA communities, suggesting a subset of 20\% in soil and 60\% in groundwater that is active; secondary sewage showed no difference between active and inactive populations. Direct hybridization of dscDNA and RNA is thus a viable alternative to PCR-amplified microbial community analysis, providing identification of the active populations within microbial communities that attenuate pollutants, drive global biogeochemical cycles, or proliferate disease states.}, keywords = {Biodiversity, DNA, Complementary, Environmental Microbiology, Metagenomics, Microarray Analysis, Oligonucleotide Array Sequence Analysis, RNA, Ribosomal, 16S, Sensitivity and Specificity}, issn = {1098-5336}, doi = {10.1128/AEM.05262-11}, author = {Deangelis, Kristen M and Wu, Cindy H and Beller, Harry R and Brodie, Eoin L and Chakraborty, Romy and DeSantis, Todd Z and Fortney, Julian L and Hazen, Terry C and Osman, Shariff R and Singer, Mary E and Tom, Lauren M and Andersen, Gary L} } @article {434, title = {The genome of Geobacter bemidjiensis, exemplar for the subsurface clade of Geobacter species that predominate in Fe(III)-reducing subsurface environments.}, journal = {BMC Genomics}, volume = {11}, year = {2010}, month = {2010}, pages = {490}, abstract = {BACKGROUND: Geobacter species in a phylogenetic cluster known as subsurface clade 1 are often the predominant microorganisms in subsurface environments in which Fe(III) reduction is the primary electron-accepting process. Geobacter bemidjiensis, a member of this clade, was isolated from hydrocarbon-contaminated subsurface sediments in Bemidji, Minnesota, and is closely related to Geobacter species found to be abundant at other subsurface sites. This study examines whether there are significant differences in the metabolism and physiology of G. bemidjiensis compared to non-subsurface Geobacter species. RESULTS: Annotation of the genome sequence of G. bemidjiensis indicates several differences in metabolism compared to previously sequenced non-subsurface Geobacteraceae, which will be useful for in silico metabolic modeling of subsurface bioremediation processes involving Geobacter species. Pathways can now be predicted for the use of various carbon sources such as propionate by G. bemidjiensis. Additional metabolic capabilities such as carbon dioxide fixation and growth on glucose were predicted from the genome annotation. The presence of different dicarboxylic acid transporters and two oxaloacetate decarboxylases in G. bemidjiensis may explain its ability to grow by disproportionation of fumarate. Although benzoate is the only aromatic compound that G. bemidjiensis is known or predicted to utilize as an electron donor and carbon source, the genome suggests that this species may be able to detoxify other aromatic pollutants without degrading them. Furthermore, G. bemidjiensis is auxotrophic for 4-aminobenzoate, which makes it the first Geobacter species identified as having a vitamin requirement. Several features of the genome indicated that G. bemidjiensis has enhanced abilities to respire, detoxify and avoid oxygen. CONCLUSION: Overall, the genome sequence of G. bemidjiensis offers surprising insights into the metabolism and physiology of Geobacteraceae in subsurface environments, compared to non-subsurface Geobacter species, such as the ability to disproportionate fumarate, more efficient oxidation of propionate, enhanced responses to oxygen stress, and dependence on the environment for a vitamin requirement. Therefore, an understanding of the activity of Geobacter species in the subsurface is more likely to benefit from studies of subsurface isolates such as G. bemidjiensis than from the non-subsurface model species studied so far.}, keywords = {Aldehyde Oxidoreductases, Biodegradation, Environmental, Carbohydrate Metabolism, Carbon Dioxide, Cell Wall, Electrons, Environmental Microbiology, Fatty Acids, Frameshift Mutation, Fumarates, Genes, Bacterial, Genome, Bacterial, Geobacter, Glucose, Iron, Metabolic Networks and Pathways, Multienzyme Complexes, Multigene Family, Osmosis, Oxidation-Reduction, Oxo-Acid-Lyases, Propionic Acids, Pyruvic Acid, Species Specificity, Surface Properties}, issn = {1471-2164}, doi = {10.1186/1471-2164-11-490}, author = {Aklujkar, Muktak and Young, Nelson D and Holmes, Dawn and Chavan, Milind and Risso, Carla and Kiss, Hajnalka E and Han, Cliff S and Land, Miriam L and Lovley, Derek R} } @article {469, title = {Polar lipid fatty acids, LPS-hydroxy fatty acids, and respiratory quinones of three Geobacter strains, and variation with electron acceptor.}, journal = {J Ind Microbiol Biotechnol}, volume = {36}, year = {2009}, month = {2009 Feb}, pages = {205-9}, abstract = {The polar lipid fatty acids, lipopolysaccharide hydroxy-fatty acids, and respiratory quinones of Geobacter metallireducens str. GS-15, Geobacter sulfurreducens str. PCA, and Geobacter bemidjiensis str. Bem are reported. Also, the lipids of G. metallireducens were compared when grown with Fe(3+) or nitrate as electron acceptors and G. sulfurreducens with Fe(3+) or fumarate. In all experiments, the most abundant polar lipid fatty acids were 14:0, i15:0, 16:1 omega 7c, 16:1 omega 5c, and 16:0; lipopolysaccharide hydroxy-fatty acids were dominated by 3oh16:0, 3oh14:0, 9oh16:0, and 10oh16:0; and menaquinone-8 was the most abundant respiratory quinone. Some variation in lipid profiles with strain were observed, but not with electron acceptor.}, keywords = {Culture Media, Electrons, Environmental Microbiology, Fatty Acids, Ferrous Compounds, Geobacter, Lipids, Lipopolysaccharides, Nitrates, Quinones, Vitamin K 2}, issn = {1476-5535}, doi = {10.1007/s10295-008-0486-7}, author = {Hedrick, D B and Peacock, A D and Lovley, D R and Woodard, T L and Nevin, K P and Long, P E and White, D C} } @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 {557, title = {Geobacter sulfurreducens can grow with oxygen as a terminal electron acceptor.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Apr}, pages = {2525-8}, abstract = {Geobacter sulfurreducens, previously classified as a strict anaerobe, tolerated exposure to atmospheric oxygen for at least 24 h and grew with oxygen as the sole electron acceptor at concentrations of 10\% or less in the headspace. These results help explain how Geobacter species may survive in oxic subsurface environments, being poised to rapidly take advantage of the development of anoxic conditions.}, keywords = {Aerobiosis, Anaerobiosis, Electron Transport, Environmental Microbiology, Geobacter, Oxygen}, issn = {0099-2240}, author = {Lin, W C and Coppi, M V and Lovley, D R} } @article {561, title = {Biotechnological application of metal-reducing microorganisms.}, journal = {Adv Appl Microbiol}, volume = {53}, year = {2003}, month = {2003}, pages = {85-128}, keywords = {Archaea, Biodegradation, Environmental, Bioreactors, Environmental Microbiology, Geobacter, Gram-Negative Anaerobic Bacteria, Metals, Heavy, Water Pollutants, Chemical}, issn = {0065-2164}, author = {Lloyd, Jonathan R and Lovley, Derek R and Macaskie, Lynne E} } @article {558, title = {Cleaning up with genomics: applying molecular biology to bioremediation.}, journal = {Nat Rev Microbiol}, volume = {1}, year = {2003}, month = {2003 Oct}, pages = {35-44}, abstract = {Bioremediation has the potential to restore contaminated environments inexpensively yet effectively, but a lack of information about the factors controlling the growth and metabolism of microorganisms in polluted environments often limits its implementation. However, rapid advances in the understanding of bioremediation are on the horizon. Researchers now have the ability to culture microorganisms that are important in bioremediation and can evaluate their physiology using a combination of genome-enabled experimental and modelling techniques. In addition, new environmental genomic techniques offer the possibility for similar studies on as-yet-uncultured organisms. Combining models that can predict the activity of microorganisms that are involved in bioremediation with existing geochemical and hydrological models should transform bioremediation from a largely empirical practice into a science.}, keywords = {Bacteria, Bacterial Physiological Phenomena, Biodegradation, Environmental, Ecology, Environmental Microbiology, Fungi, Genetic Vectors, Genome, Bacterial, Genome, Fungal, Genomics, Models, Biological, Molecular Biology}, issn = {1740-1526}, doi = {10.1038/nrmicro731}, author = {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 {620, title = {Microbiological evidence for Fe(III) reduction on early Earth.}, journal = {Nature}, volume = {395}, year = {1998}, month = {1998 Sep 3}, pages = {65-7}, abstract = {It is generally considered that sulphur reduction was one of the earliest forms of microbial respiration, because the known microorganisms that are most closely related to the last common ancestor of modern life are primarily anaerobic, sulphur-reducing hyperthermophiles. However, geochemical evidence indicates that Fe(III) is more likely than sulphur to have been the first external electron acceptor of global significance in microbial metabolism. Here we show that Archaea and Bacteria that are most closely related to the last common ancestor can reduce Fe(III) to Fe(II) and conserve energy to support growth from this respiration. Surprisingly, even Thermotoga maritima, previously considered to have only a fermentative metabolism, could grow as a respiratory organism when Fe(III) was provided as an electron acceptor. These results provide microbiological evidence that Fe(III) reduction could have been an important process on early Earth and suggest that microorganisms might contribute to Fe(III) reduction in modern hot biospheres. Furthermore, our discovery that hyperthermophiles that had previously been thought to require sulphur for cultivation can instead be grown without the production of toxic and corrosive sulphide, should aid biochemical investigations of these poorly understood organisms.}, keywords = {Earth (Planet), Electron Transport, Environmental Microbiology, Ferric Compounds, Gram-Negative Anaerobic Bacteria, Oxidation-Reduction, Thermoproteaceae}, issn = {0028-0836}, doi = {10.1038/25720}, author = {Vargas, M and Kashefi, K and Blunt-Harris, E L and Lovley, D R} }