@article {3106, title = {Functional environmental proteomics: elucidating the role of a c-type cytochrome abundant during uranium bioremediation.}, journal = {ISME J}, volume = {10}, year = {2016}, month = {2016 Feb}, pages = {310-20}, abstract = {

Studies with pure cultures of dissimilatory metal-reducing microorganisms have demonstrated that outer-surface c-type cytochromes are important electron transfer agents for the reduction of metals, but previous environmental proteomic studies have typically not recovered cytochrome sequences from subsurface environments in which metal reduction is important. Gel-separation, heme-staining and mass spectrometry of proteins in groundwater from in situ uranium bioremediation experiments identified a putative c-type cytochrome, designated Geobacter subsurface c-type cytochrome A (GscA), encoded within the genome of strain M18, a Geobacter isolate previously recovered from the site. Homologs of GscA were identified in the genomes of other Geobacter isolates in the phylogenetic cluster known as subsurface clade 1, which predominates in a diversity of Fe(III)-reducing subsurface environments. Most of the gscA sequences recovered from groundwater genomic DNA clustered in a tight phylogenetic group closely related to strain M18. GscA was most abundant in groundwater samples in which Geobacter sp. predominated. Expression of gscA in a strain of Geobacter sulfurreducens that lacked the gene for the c-type cytochrome OmcS, thought to facilitate electron transfer from conductive pili to Fe(III) oxide, restored the capacity for Fe(III) oxide reduction. Atomic force microscopy provided evidence that GscA was associated with the pili. These results demonstrate that a c-type cytochrome with an apparent function similar to that of OmcS is abundant when Geobacter sp. are abundant in the subsurface, providing insight into the mechanisms for the growth of subsurface Geobacter sp. on Fe(III) oxide and suggesting an approach for functional analysis of other Geobacter proteins found in the subsurface.

}, keywords = {Amino Acid Sequence, Bacterial Proteins, Biodegradation, Environmental, Cytochrome c Group, Electron Transport, Ferric Compounds, Geobacter, Groundwater, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, Proteomics, Sequence Alignment, Uranium}, issn = {1751-7370}, doi = {10.1038/ismej.2015.113}, author = {Yun, Jiae and Malvankar, Nikhil S and Ueki, Toshiyuki and Lovley, Derek R} } @article {3138, title = {Field evidence of selenium bioreduction in a uranium-contaminated aquifer.}, journal = {Environ Microbiol Rep}, volume = {5}, year = {2013}, month = {2013 Jun}, pages = {444-52}, abstract = {

Removal of selenium from groundwater was documented during injection of acetate into a uranium-contaminated aquifer near Rifle, Colorado (USA). Bioreduction of aqueous selenium to its elemental form (Se0) concentrated it within mineralized biofilms affixed to tubing used to circulate acetate-amended groundwater. Scanning and transmission electron microscopy revealed close association between Se0 precipitates and cell surfaces, with Se0 aggregates having a diameter of 50-60 nm. Accumulation of Se0 within biofilms occurred over a three-week interval at a rate of c. 9 mg Se0 m(-2) tubing day(-1). Removal was inferred to result from the activity of a mixed microbial community within the biofilms capable of coupling acetate oxidation to the reduction of oxygen, nitrate and selenate. Phylogenetic analysis of the biofilm revealed a community dominated by strains of Dechloromonas sp. and Thauera sp., with isolates exhibiting genetic similarity to the latter known to reduce selenate to Se0. Enrichment cultures of selenate-respiring microorganisms were readily established using Rifle site groundwater and acetate, with cultures dominated by strains closely related to D. aromatica (96-99\% similarity). Predominance of Dechloromonas sp. in recovered biofilms and enrichments suggests this microorganism may play a role in the removal of selenium oxyanions present in Se-impacted groundwaters and sediments.

}, keywords = {Acetates, Betaproteobacteria, Biodegradation, Environmental, Biofilms, Colorado, Groundwater, Humans, Microbial Consortia, Oxidation-Reduction, Oxygen, Phylogeny, RNA, Ribosomal, 16S, Selenic Acid, Selenium, Selenium Compounds, Thauera, Uranium, Water Pollutants, Chemical}, issn = {1758-2229}, doi = {10.1111/1758-2229.12032}, author = {Williams, Kenneth H and Wilkins, Michael J and N{\textquoteright}Guessan, A Lucie and Arey, Bruce and Dodova, Elena and Dohnalkova, Alice and Holmes, Dawn and Lovley, Derek R and Long, Philip E} } @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 = {

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.

}, 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 {465, title = {Future shock from the microbe electric.}, journal = {Microb Biotechnol}, volume = {2}, year = {2009}, month = {2009 Mar}, pages = {139-41}, keywords = {Bacteria, Bioelectric Energy Sources, Biotechnology, Electricity, Energy-Generating Resources}, issn = {1751-7915}, doi = {10.1111/j.1751-7915.2009.00090_9.x}, author = {Lovley, Derek R} } @article {492, title = {Fluorescent properties of c-type cytochromes reveal their potential role as an extracytoplasmic electron sink in Geobacter sulfurreducens.}, journal = {Environ Microbiol}, volume = {10}, year = {2008}, month = {2008 Feb}, pages = {497-505}, abstract = {A novel fluorescence technique for monitoring the redox status of c-type cytochromes in Geobacter sulfurreducens was developed in order to evaluate the capacity of these extracytoplasmic cytochromes to store electrons during periods in which an external electron acceptor is not available. When intact cells in which the cytochromes were in a reduced state were excited at a wavelength of 350 nm, they fluoresced with maxima at 402 and 437 nm. Oxidation of the cytochromes resulted in a loss of fluorescence. This method was much more sensitive than the traditional approach of detecting c-type cytochromes via visible light absorbance. Furthermore, fluorescence of reduced cytochromes in individual cells could be detected via fluorescence microscopy, and the cytochromes in a G. sulfurreducens biofilm, remotely excited with an optical fibre, could be detected at distances as far as 5 cm. Fluorescence analysis of cytochrome oxidation and reduction of the external electron acceptor, anthraquinone-2,6-disulfonate, suggested that the extracytoplasmic cytochromes of G. sulfurreducens could store approximately 10(7) electrons per cell. Independent analysis of the haem content of the cells determined from analysis of incorporation of (55)Fe into cytochromes provided a similar estimate of cytochrome electron-storage capacity. This electron-storage capacity could, in the absence of an external electron acceptor, permit continued electron transfer across the inner membrane sufficient to supply the maintenance energy requirements for G. sulfurreducens for up to 8 min or enough proton motive force to power flagella motors for G. sulfurreducens motility. The fluorescence approach described here provides a sensitive method for evaluating the redox status of Geobacter species in culture and/or its environments. Furthermore, these results suggest that the periplasmic and outer-membrane cytochromes of Geobacter species act as capacitors, allowing continued electron transport, and thus viability and motility, for Geobacter species as they move between heterogeneously dispersed Fe(III) oxides during growth in the subsurface.}, keywords = {Anthraquinones, Cytochromes c, Electron Transport, Ferric Compounds, Flagella, Fluorescence, Geobacter, Microscopy, Fluorescence, Oxidation-Reduction}, issn = {1462-2920}, doi = {10.1111/j.1462-2920.2007.01470.x}, author = {Esteve-N{\'u}{\~n}ez, Abraham and Sosnik, Julian and Visconti, Pablo and Lovley, Derek R} } @article {578, title = {Fulvic acid oxidation state detection using fluorescence spectroscopy.}, journal = {Environ Sci Technol}, volume = {36}, year = {2002}, month = {2002 Jul 15}, pages = {3170-5}, abstract = {Humic substances are a heterogeneous class of moderate molecular weight, yellow-colored biomolecules present in all soils, sediments, and natural waters. Although humic substances are generally resistant to microbial degradation under anaerobic conditions, some microorganisms in soils and sediments can use quinone moieties in humic substances as electron acceptors. Laboratory experiments have shown that humic substances can act as electron shuttles in the microbial reduction of ferric iron. Field studies of electron shuttling processes have been constrained by the lack of methods to characterize the oxidation state of quinone moieties in humic substances at natural concentrations. All humic substances have fluorescent properties, and fluorescence spectroscopy can indicate differences in precursor organic source of humic substances. Here we show that the quinone moieties responsible for electron transfer reactions contribute significantly to the fluorescence of humic substances. Further we use fluorescence spectroscopy to elucidate the oxidation state of quinone moieties in humic substances at natural concentrations found in sediment interstitial waters.}, keywords = {Benzopyrans, Environmental Monitoring, Iron, Oxidation-Reduction, Spectrometry, Fluorescence}, issn = {0013-936X}, author = {Klapper, Lisa and McKnight, Diane M and Fulton, J Robin and Blunt-Harris, Elizabeth L and Nevin, Kelly P and Lovley, Derek R and Hatcher, Patrick G} }