@article {3143,
	title = {Fluctuations in species-level protein expression occur during element and nutrient cycling in the subsurface.},
	journal = {PLoS One},
	volume = {8},
	year = {2013},
	month = {2013},
	pages = {e57819},
	abstract = {<p>While microbial activities in environmental systems play a key role in the utilization and cycling of essential elements and compounds, microbial activity and growth frequently fluctuates in response to environmental stimuli and perturbations. To investigate these fluctuations within a saturated aquifer system, we monitored a carbon-stimulated in situ Geobacter population while iron reduction was occurring, using 16S rRNA abundances and high-resolution tandem mass spectrometry proteome measurements. Following carbon amendment, 16S rRNA analysis of temporally separated samples revealed the rapid enrichment of Geobacter-like environmental strains with strong similarity to G. bemidjiensis. Tandem mass spectrometry proteomics measurements suggest high carbon flux through Geobacter respiratory pathways, and the synthesis of anapleurotic four carbon compounds from acetyl-CoA via pyruvate ferredoxin oxidoreductase activity. Across a 40-day period where Fe(III) reduction was occurring, fluctuations in protein expression reflected changes in anabolic versus catabolic reactions, with increased levels of biosynthesis occurring soon after acetate arrival in the aquifer. In addition, localized shifts in nutrient limitation were inferred based on expression of nitrogenase enzymes and phosphate uptake proteins. These temporal data offer the first example of differing microbial protein expression associated with changing geochemical conditions in a subsurface environment.</p>},
	keywords = {Biomass, Carbon, Environment, Gene Expression Regulation, Bacterial, Geobacter, Groundwater, Humic Substances, Iron, Oxidation-Reduction, Phosphates, Plankton, Proteomics, RNA, Ribosomal, 16S, Tandem Mass Spectrometry, Uranium, Vanadium, Water Microbiology},
	issn = {1932-6203},
	doi = {10.1371/journal.pone.0057819},
	author = {Wilkins, Michael J and Wrighton, Kelly C and Nicora, Carrie D and Williams, Kenneth H and McCue, Lee Ann and Handley, Kim M and Miller, Chris S and Giloteaux, Ludovic and Montgomery, Alison P and Lovley, Derek R and Banfield, Jillian F and Long, Philip E and Lipton, Mary S}
}
@article {438,
	title = {Genome-scale dynamic modeling of the competition between Rhodoferax and Geobacter in anoxic subsurface environments.},
	journal = {ISME J},
	volume = {5},
	year = {2011},
	month = {2011 Feb},
	pages = {305-16},
	abstract = {The advent of rapid complete genome sequencing, and the potential to capture this information in genome-scale metabolic models, provide the possibility of comprehensively modeling microbial community interactions. For example, Rhodoferax and Geobacter species are acetate-oxidizing Fe(III)-reducers that compete in anoxic subsurface environments and this competition may have an influence on the in situ bioremediation of uranium-contaminated groundwater. Therefore, genome-scale models of Geobacter sulfurreducens and Rhodoferax ferrireducens were used to evaluate how Geobacter and Rhodoferax species might compete under diverse conditions found in a uranium-contaminated aquifer in Rifle, CO. The model predicted that at the low rates of acetate flux expected under natural conditions at the site, Rhodoferax will outcompete Geobacter as long as sufficient ammonium is available. The model also predicted that when high concentrations of acetate are added during in situ bioremediation, Geobacter species would predominate, consistent with field-scale observations. This can be attributed to the higher expected growth yields of Rhodoferax and the ability of Geobacter to fix nitrogen. The modeling predicted relative proportions of Geobacter and Rhodoferax in geochemically distinct zones of the Rifle site that were comparable to those that were previously documented with molecular techniques. The model also predicted that under nitrogen fixation, higher carbon and electron fluxes would be diverted toward respiration rather than biomass formation in Geobacter, providing a potential explanation for enhanced in situ U(VI) reduction in low-ammonium zones. These results show that genome-scale modeling can be a useful tool for predicting microbial interactions in subsurface environments and shows promise for designing bioremediation strategies.},
	keywords = {Acetates, Anaerobiosis, Biodegradation, Environmental, Biomass, Comamonadaceae, Genome, Genome, Bacterial, Geobacter, Models, Biological, Nitrogen Fixation, Quaternary Ammonium Compounds, RNA, Ribosomal, 16S, Uranium, Water Microbiology, Water Pollutants, Radioactive},
	issn = {1751-7370},
	doi = {10.1038/ismej.2010.117},
	author = {Zhuang, Kai and Izallalen, Mounir and Mouser, Paula and Richter, Hanno and Risso, Carla and Mahadevan, Radhakrishnan 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 {433,
	title = {Analysis of biostimulated microbial communities from two field experiments reveals temporal and spatial differences in proteome profiles.},
	journal = {Environ Sci Technol},
	volume = {44},
	year = {2010},
	month = {2010 Dec 1},
	pages = {8897-903},
	abstract = {Stimulated by an acetate-amendment field experiment conducted in 2007, anaerobic microbial populations in the aquifer at the Rifle Integrated Field Research Challenge site in Colorado reduced mobile U(VI) to insoluble U(IV). During this experiment, planktonic biomass was sampled at various time points to quantitatively evaluate proteomes. In 2008, an acetate-amended field experiment was again conducted in a similar manner to the 2007 experiment. As there was no comprehensive metagenome sequence available for use in proteomics analysis, we systematically evaluated 12 different organism genome sequences to generate sets of aggregate genomes, or "pseudo-metagenomes", for supplying relative quantitative peptide and protein identifications. Proteomics results support previous observations of the dominance of Geobacteraceae during biostimulation using acetate as sole electron donor, and revealed a shift from an early stage of iron reduction to a late stage of iron reduction. Additionally, a shift from iron reduction to sulfate reduction was indicated by changes in the contribution of proteome information contributed by different organism genome sequences within the aggregate set. In addition, the comparison of proteome measurements made between the 2007 field experiment and 2008 field experiment revealed differences in proteome profiles. These differences may be the result of alterations in abundance and population structure within the planktonic biomass samples collected for analysis.},
	keywords = {Bacteria, Biodiversity, Biomass, Fresh Water, Plankton, Proteome, Water Microbiology},
	issn = {1520-5851},
	doi = {10.1021/es101029f},
	author = {Callister, Stephen J and Wilkins, Michael J and Nicora, Carrie D and Williams, Kenneth H and Banfield, Jillian F and VerBerkmoes, Nathan C and Hettich, Robert L and N{\textquoteright}Guessan, Lucie and Mouser, Paula J and Elifantz, Hila and Smith, Richard D and Lovley, Derek R and Lipton, Mary S and Long, Philip E}
}
@article {457,
	title = {Proteogenomic monitoring of Geobacter physiology during stimulated uranium bioremediation.},
	journal = {Appl Environ Microbiol},
	volume = {75},
	year = {2009},
	month = {2009 Oct},
	pages = {6591-9},
	abstract = {Implementation of uranium bioremediation requires methods for monitoring the membership and activities of the subsurface microbial communities that are responsible for reduction of soluble U(VI) to insoluble U(IV). Here, we report a proteomics-based approach for simultaneously documenting the strain membership and microbial physiology of the dominant Geobacter community members during in situ acetate amendment of the U-contaminated Rifle, CO, aquifer. Three planktonic Geobacter-dominated samples were obtained from two wells down-gradient of acetate addition. Over 2,500 proteins from each of these samples were identified by matching liquid chromatography-tandem mass spectrometry spectra to peptides predicted from seven isolate Geobacter genomes. Genome-specific peptides indicate early proliferation of multiple M21 and Geobacter bemidjiensis-like strains and later possible emergence of M21 and G. bemidjiensis-like strains more closely related to Geobacter lovleyi. Throughout biostimulation, the proteome is dominated by enzymes that convert acetate to acetyl-coenzyme A and pyruvate for central metabolism, while abundant peptides matching tricarboxylic acid cycle proteins and ATP synthase subunits were also detected, indicating the importance of energy generation during the period of rapid growth following the start of biostimulation. Evolving Geobacter strain composition may be linked to changes in protein abundance over the course of biostimulation and may reflect changes in metabolic functioning. Thus, metagenomics-independent community proteogenomics can be used to diagnose the status of the subsurface consortia upon which remediation biotechnology relies.},
	keywords = {Amino Acid Sequence, Bacterial Proteins, Biodegradation, Environmental, Genomics, Geobacter, Molecular Sequence Data, Oxidation-Reduction, Peptide Mapping, Plankton, Proteomics, Uranium, Water Microbiology, Water Pollutants, Radioactive},
	issn = {1098-5336},
	doi = {10.1128/AEM.01064-09},
	author = {Wilkins, Michael J and VerBerkmoes, Nathan C and Williams, Kenneth H and Callister, Stephen J and Mouser, Paula J and Elifantz, Hila and N{\textquoteright}guessan, Lucie A and Thomas, Brian C and Nicora, Carrie D and Shah, Manesh B and Abraham, Paul and Lipton, Mary S and Lovley, Derek R and Hettich, Robert L and Long, Philip E and Banfield, Jillian F}
}
@article {565,
	title = {Extending the upper temperature limit for life.},
	journal = {Science},
	volume = {301},
	year = {2003},
	month = {2003 Aug 15},
	pages = {934},
	keywords = {Archaea, Culture Media, Ferric Compounds, Hot Temperature, Oxidation-Reduction, Pacific Ocean, Water Microbiology},
	issn = {1095-9203},
	doi = {10.1126/science.1086823},
	author = {Kashefi, Kazem and Lovley, Derek R}
}
@article {566,
	title = {Metabolism of organic compounds in anaerobic, hydrothermal sulphate-reducing marine sediments.},
	journal = {Environ Microbiol},
	volume = {5},
	year = {2003},
	month = {2003 Jul},
	pages = {583-91},
	abstract = {Previous studies of hot (>80 degrees C) microbial ecosystems have primarily relied on the study of pure cultures or analysis of 16S rDNA sequences. In order to gain more information on anaerobic metabolism by natural communities in hot environments, sediments were collected from a shallow marine hydrothermal vent system in Baia di Levante, Vulcano, Italy and incubated under strict anaerobic conditions at 90 degrees C. Sulphate reduction was the predominant terminal electron-accepting process in the sediments. The addition of molybdate inhibited sulphate reduction in the sediments and resulted in a linear accumulation of acetate and hydrogen over time. [U-14C]- acetate was completely oxidized to 14CO2, and the addition of molybdate inhibited 14CO2 production by 60\%. [U-14C]-glucose was oxidized to 14CO2, and this was inhibited when molybdate was added. When the pool sizes of short-chain fatty acids were artificially increased, radiolabel from [U-14C]-glucose accumulated in the acetate pool. L-[U-14C]-glutamate, [ring-14C]-benzoate and [U-14C]-palmitate were also anaerobically oxidized to 14CO2 in the sediments, but molybdate had little effect on the oxidation of these compounds. These results demonstrate that natural microbial communities living in a hot, microbial ecosystem can oxidize acetate and a range of other organic electron donors under sulphate-reducing conditions and suggest that acetate is an important extracellular intermediate in the anaerobic degradation of organic matter in hot microbial ecosystems.},
	keywords = {Acetates, Anaerobiosis, Bacteria, Anaerobic, Benzoates, Carbon Dioxide, Ecosystem, Geologic Sediments, Glucose, Glutamic Acid, Hot Temperature, Hydrogen, Italy, Molybdenum, Organic Chemicals, Oxidation-Reduction, Palmitates, Seawater, Sulfates, Water Microbiology},
	issn = {1462-2912},
	author = {Tor, Jason M and Amend, Jan P 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 {589,
	title = {A hydrogen-based subsurface microbial community dominated by methanogens.},
	journal = {Nature},
	volume = {415},
	year = {2002},
	month = {2002 Jan 17},
	pages = {312-5},
	abstract = {The search for extraterrestrial life may be facilitated if ecosystems can be found on Earth that exist under conditions analogous to those present on other planets or moons. It has been proposed, on the basis of geochemical and thermodynamic considerations, that geologically derived hydrogen might support subsurface microbial communities on Mars and Europa in which methanogens form the base of the ecosystem. Here we describe a unique subsurface microbial community in which hydrogen-consuming, methane-producing Archaea far outnumber the Bacteria. More than 90\% of the 16S ribosomal DNA sequences recovered from hydrothermal waters circulating through deeply buried igneous rocks in Idaho are related to hydrogen-using methanogenic microorganisms. Geochemical characterization indicates that geothermal hydrogen, not organic carbon, is the primary energy source for this methanogen-dominated microbial community. These results demonstrate that hydrogen-based methanogenic communities do occur in Earth{\textquoteright}s subsurface, providing an analogue for possible subsurface microbial ecosystems on other planets.},
	keywords = {Bacteria, DNA, Archaeal, DNA, Bacterial, Ecosystem, Euryarchaeota, Exobiology, Hydrogen, Molecular Sequence Data, Phylogeny, RNA, Ribosomal, 16S, Water Microbiology},
	issn = {0028-0836},
	doi = {10.1038/415312a},
	author = {Chapelle, Francis H and O{\textquoteright}Neill, Kathleen and Bradley, Paul M and Meth{\'e}, Barbara A and Ciufo, Stacy A and Knobel, LeRoy L and Lovley, Derek R}
}
