@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 {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 {482,
	title = {Sustained removal of uranium from contaminated groundwater following stimulation of dissimilatory metal reduction.},
	journal = {Environ Sci Technol},
	volume = {42},
	year = {2008},
	month = {2008 Apr 15},
	pages = {2999-3004},
	abstract = {Previous field studies on in situ bioremediation of uranium-contaminated groundwater in an aquifer in Rifle, Colorado identified two distinct phases following the addition of acetate to stimulate microbial respiration. In phase I, Geobacter species are the predominant organisms, Fe(III) is reduced, and microbial reduction of soluble U(VI) to insoluble U(IV) removes uranium from the groundwater. In phase II, Fe(III) is depleted, sulfate is reduced, and sulfate-reducing bacteria predominate. Long-term monitoring revealed an unexpected third phase during which U(VI) removal continues even after acetate additions are stopped. All three of these phases were successfully reproduced in flow-through sediment columns. When sediments from the third phase were heat sterilized, the capacity for U(VI) removal was lost. In the live sediments U(VI) removed from the groundwater was recovered as U(VI) in the sediments. This contrasts to the recovery of U(IV) in sediments resulting from the reduction of U(VI) to U(IV) during the Fe(III) reduction phase in acetate-amended sediments. Analysis of 16S rRNA gene sequences in the sediments in which U(VI) was being adsorbed indicated that members of the Firmicutes were the predominant organisms whereas no Firmicutes sequences were detected in background sediments which did not have the capacity to sorb U(VI), suggesting that the U(VI) adsorption might be due to the presence of these living organisms or at least their intact cell components. This unexpected enhanced adsorption of U(VI) onto sediments following the stimulation of microbial growth in the subsurface may potentially enhance the cost effectiveness of in situ uranium bioremediation.},
	keywords = {Acetates, Adsorption, Bacteria, Colorado, Geologic Sediments, Oxidation-Reduction, RNA, Ribosomal, 16S, Sulfates, Uranium, Water Pollutants, Radioactive, Water Supply},
	issn = {0013-936X},
	author = {N{\textquoteright}guessan, Lucie A and Vrionis, Helen A and Resch, Charles T and Long, Philip E 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}
}
