@article {3059, title = {Electromicrobiology: the ecophysiology of phylogenetically diverse electroactive microorganisms.}, journal = {Nat Rev Microbiol}, volume = {20}, year = {2022}, month = {2022 Jan}, pages = {5-19}, abstract = {

Electroactive microorganisms markedly affect many environments in which they establish outer-surface electrical contacts with other cells and minerals or reduce soluble extracellular redox-active molecules such as flavins and humic substances. A growing body of research emphasizes their broad phylogenetic diversity and shows that these microorganisms have key roles in multiple biogeochemical cycles, as well as the microbiome of the gut, anaerobic waste digesters and metal corrosion. Diverse bacteria and archaea have independently evolved cytochrome-based strategies for electron exchange between the outer cell surface and the cell interior, but cytochrome-free mechanisms are also prevalent. Electrically conductive protein filaments, soluble electron shuttles and non-biological conductive materials can substantially extend the electronic reach of microorganisms beyond the surface of the cell. The growing appreciation of the diversity of electroactive microorganisms and their unique electronic capabilities is leading to a broad range of applications.

}, keywords = {Archaea, Bacteria, Bacterial Physiological Phenomena, Cytochromes, Electron Transport, Oxidation-Reduction, Phylogeny}, issn = {1740-1534}, doi = {10.1038/s41579-021-00597-6}, author = {Lovley, Derek R and Holmes, Dawn E} } @article {3053, title = {Microbial nanowires.}, journal = {Curr Biol}, volume = {32}, year = {2022}, month = {2022 Feb 07}, pages = {R110-R112}, abstract = {

In this Quick guide, Derek Lovley introduces microbial nanowires-conductive extracellular appendages made by some bacteria and archaea.

}, keywords = {Bacteria, Electric Conductivity, Electron Transport, Fimbriae, Bacterial, Nanowires}, issn = {1879-0445}, doi = {10.1016/j.cub.2021.12.019}, author = {Lovley, Derek R} } @article {3097, title = {Happy together: microbial communities that hook up to swap electrons.}, journal = {ISME J}, volume = {11}, year = {2017}, month = {2017 Feb}, pages = {327-336}, abstract = {

The discovery of direct interspecies electron transfer (DIET) and cable bacteria has demonstrated that microbial cells can exchange electrons over long distances (μm-cm) through electrical connections. For example, in the presence of cable bacteria electrons are rapidly transported over centimeter distances, coupling the oxidation of reduced sulfur compounds in anoxic sediments to oxygen reduction in overlying surficial sediments. Bacteria and archaea wired for DIET are found in anaerobic methane-producing and methane-consuming communities. Electrical connections between gut microbes and host cells have also been proposed. Iterative environmental and defined culture studies on methanogenic communities revealed the importance of electrically conductive pili and c-type cytochromes in natural electrical grids, and demonstrated that conductive carbon materials and magnetite can substitute for these biological connectors to facilitate DIET. This understanding has led to strategies to enhance and stabilize anaerobic digestion. Key unknowns warranting further investigation include elucidation of the archaeal electrical connections facilitating DIET-based methane production and consumption; and the mechanisms for long-range electron transfer through cable bacteria. A better understanding of mechanisms for cell-to-cell electron transfer could facilitate the hunt for additional electrically connected microbial communities with omics approaches and could advance spin-off applications such as the development of sustainable bioelectronics materials and bioelectrochemical technologies.

}, keywords = {Archaea, Bacteria, Electron Transport, Methane, Microbial Consortia, Microbial Interactions, Models, Biological, Oxidation-Reduction}, issn = {1751-7370}, doi = {10.1038/ismej.2016.136}, author = {Lovley, Derek R} } @article {3099, title = {Enhancing anaerobic digestion of complex organic waste with carbon-based conductive materials.}, journal = {Bioresour Technol}, volume = {220}, year = {2016}, month = {2016 Nov}, pages = {516-522}, abstract = {

The aim of this work was to study the methanogenic metabolism of dog food, a food waste surrogate, in laboratory-scale reactors with different carbon-based conductive materials. Carbon cloth, carbon felt, and granular activated carbon all permitted higher organic loading rates and promoted faster recovery of soured reactors than the control reactors. Microbial community analysis revealed that specific and substantial enrichments of Sporanaerobacter and Methanosarcina were present on the carbon cloth surface. These results, and the known ability of Sporanaerobacter species to transfer electrons to elemental sulfur, suggest that Sporanaerobacter species can participate in direct interspecies electron transfer with Methanosarcina species when carbon cloth is available as an electron transfer mediator.

}, keywords = {Anaerobiosis, Animals, Bacteria, Bioreactors, Carbon, Carbon Fiber, Charcoal, Dogs, Electric Conductivity, Fatty Acids, Volatile, Hydrogen-Ion Concentration, Methane, Organic Chemicals, Waste Products}, issn = {1873-2976}, doi = {10.1016/j.biortech.2016.08.114}, author = {Dang, Yan and Holmes, Dawn E and Zhao, Zhiqiang and Woodard, Trevor L and Zhang, Yaobin and Sun, Dezhi and Wang, Li-Ying and Nevin, Kelly P and Lovley, Derek R} } @article {1421, title = {Biodegradation of low concentrations of 1,2-dibromoethane in groundwater is enhanced by phenol.}, journal = {Appl Microbiol Biotechnol}, volume = {98}, year = {2014}, month = {2014 Feb}, pages = {1329-38}, abstract = {

The lead scavenger 1,2-dibromoethane (EDB), a former additive to leaded gasoline, is a common groundwater contaminant, yet not much knowledge is available for its targeted bioremediation, especially under in situ conditions. The study site was an aviation gas spill site, which, although all hydrocarbons and most of the EDB were remediated in the mid-1990s, still exhibits low levels of EDB remaining in the groundwater (about 11 \μg EDB/l). To evaluate the effect of phenol on biostimulation of low concentration of EDB, microcosms were established from an EDB-contaminated aquifer. After 300 days at environmentally relevant conditions (12\ \±\ 2 \°C, static incubation), EDB was not significantly removed from unamended microcosms compared to the abiotic control. However, in treatments amended with phenol, up to 80 \% of the initial EDB concentration had been degraded, while added phenol was removed completely. Microbial community composition in unamended and phenol-amended microcosms remained unchanged, and Polaromonas sp. dominated both types of microcosms, but total bacterial abundance and numbers of the gene for phenol hydroxylase were higher in phenol-amended microcosms. Dehalogenase, an indicator suggesting targeted aerobic biodegradation of EDB, was not detected in either treatment. This finding suggests phenol hydroxylase, rather than a dehalogenation reaction, may be responsible for 1,2-dibromoethane oxidation under in situ conditions. In addition, biostimulation of EDB is possible through the addition of low levels of phenol in aerobic groundwater sites.

}, keywords = {Bacteria, Biota, Ethylene Dibromide, Groundwater, Metabolic Networks and Pathways, Phenol, Water Pollutants}, issn = {1432-0614}, doi = {10.1007/s00253-013-4963-1}, author = {Baek, Kyunghwa and Wang, Meng and McKeever, Robert and Rieber, Kahlil and Park, Chul and N{\"u}sslein, Klaus} } @article {3113, title = {Correlation between microbial community and granule conductivity in anaerobic bioreactors for brewery wastewater treatment.}, journal = {Bioresour Technol}, volume = {174}, year = {2014}, month = {2014 Dec}, pages = {306-10}, abstract = {

Prior investigation of an upflow anaerobic sludge blanket (UASB) reactor treating brewery wastes suggested that direct interspecies electron transfer (DIET) significantly contributed to interspecies electron transfer to methanogens. To investigate DIET in granules further, the electrical conductivity and bacterial community composition of granules in fourteen samples from four different UASB reactors treating brewery wastes were investigated. All of the UASB granules were electrically conductive whereas control granules from ANAMMOX (ANaerobic AMMonium OXidation) reactors and microbial granules from an aerobic bioreactor designed for phosphate removal were not. There was a moderate correlation (r=0.67) between the abundance of Geobacter species in the UASB granules and granule conductivity, suggesting that Geobacter contributed to granule conductivity. These results, coupled with previous studies, which have demonstrated that Geobacter species can donate electrons to methanogens that are typically predominant in anaerobic digesters, suggest that DIET may be a widespread phenomenon in UASB reactors treating brewery wastes.

}, keywords = {Alcoholic Beverages, Anaerobiosis, Bacteria, Bioreactors, Electric Conductivity, Ethanol, Sequence Analysis, DNA, Sewage, Waste Disposal, Fluid, Wastewater, Water Purification}, issn = {1873-2976}, doi = {10.1016/j.biortech.2014.10.004}, author = {Shrestha, Pravin Malla and Malvankar, Nikhil S and Werner, Jeffrey J and Franks, Ashley E and Elena-Rotaru, Amelia and Shrestha, Minita and Liu, Fanghua and Nevin, Kelly P and Angenent, Largus T and Lovley, Derek R} } @article {1420, title = {Response of free-living nitrogen-fixing microorganisms to land use change in the Amazon rainforest.}, journal = {Appl Environ Microbiol}, volume = {80}, year = {2014}, month = {2014 Jan}, pages = {281-8}, abstract = {

The Amazon rainforest, the largest equatorial forest in the world, is being cleared for pasture and agricultural use at alarming rates. Tropical deforestation is known to cause alterations in microbial communities at taxonomic and phylogenetic levels, but it is unclear whether microbial functional groups are altered. We asked whether free-living nitrogen-fixing microorganisms (diazotrophs) respond to deforestation in the Amazon rainforest, using analysis of the marker gene nifH. Clone libraries were generated from soil samples collected from a primary forest, a 5-year-old pasture originally converted from primary forest, and a secondary forest established after pasture abandonment. Although diazotroph richness did not significantly change among the three plots, diazotroph community composition was altered with forest-to-pasture conversion, and phylogenetic similarity was higher among pasture communities than among those in forests. There was also 10-fold increase in nifH gene abundance following conversion from primary forest to pasture. Three environmental factors were associated with the observed changes: soil acidity, total N concentration, and C/N ratio. Our results suggest a partial restoration to initial levels of abundance and community structure of diazotrophs following pasture abandonment, with primary and secondary forests sharing similar communities. We postulate that the response of diazotrophs to land use change is a direct consequence of changes in plant communities, particularly the higher N demand of pasture plant communities for supporting aboveground plant growth.

}, keywords = {Agriculture, Bacteria, Biota, Carbon, Cluster Analysis, Conservation of Natural Resources, Human Activities, Hydrogen-Ion Concentration, Molecular Sequence Data, Nitrogen, Nitrogen Fixation, Oxidoreductases, Phylogeny, Sequence Analysis, DNA, Soil, Soil Microbiology, South America, Trees}, issn = {1098-5336}, doi = {10.1128/AEM.02362-13}, author = {Mirza, Babur S and Potisap, Chotima and N{\"u}sslein, Klaus and Bohannan, Brendan J M and Rodrigues, Jorge L M} } @article {1423, title = {Conversion of the Amazon rainforest to agriculture results in biotic homogenization of soil bacterial communities.}, journal = {Proc Natl Acad Sci U S A}, volume = {110}, year = {2013}, month = {2013 Jan 15}, pages = {988-93}, abstract = {

The Amazon rainforest is the Earth\&$\#$39;s largest reservoir of plant and animal diversity, and it has been subjected to especially high rates of land use change, primarily to cattle pasture. This conversion has had a strongly negative effect on biological diversity, reducing the number of plant and animal species and homogenizing communities. We report here that microbial biodiversity also responds strongly to conversion of the Amazon rainforest, but in a manner different from plants and animals. Local taxonomic and phylogenetic diversity of soil bacteria increases after conversion, but communities become more similar across space. This homogenization is driven by the loss of forest soil bacteria with restricted ranges (endemics) and results in a net loss of diversity. This study shows homogenization of microbial communities in response to human activities. Given that soil microbes represent the majority of biodiversity in terrestrial ecosystems and are intimately involved in ecosystem functions, we argue that microbial biodiversity loss should be taken into account when assessing the impact of land use change in tropical forests.

}, keywords = {Agriculture, Animals, Bacteria, Biodiversity, Brazil, Cattle, Ecosystem, Humans, Phylogeny, Rain, Soil Microbiology, Trees, Tropical Climate}, issn = {1091-6490}, doi = {10.1073/pnas.1220608110}, author = {Rodrigues, Jorge L M and Pellizari, Vivian H and Mueller, Rebecca and Baek, Kyunghwa and Jesus, Ederson da C and Paula, Fabiana S and Mirza, Babur and Hamaoui, George S and Tsai, Siu Mui and Feigl, Brigitte and Tiedje, James M and Bohannan, Brendan J M and N{\"u}sslein, Klaus} } @article {369, title = {Phylogenetic clustering of soil microbial communities by 16S rRNA but not 16S rRNA genes.}, journal = {Appl Environ Microbiol}, volume = {78}, year = {2012}, month = {2012 Apr}, pages = {2459-61}, abstract = {We evaluated phylogenetic clustering of bacterial and archaeal communities from redox-dynamic subtropical forest soils that were defined by 16S rRNA and rRNA gene sequences. We observed significant clustering for the RNA-based communities but not the DNA-based communities, as well as increasing clustering over time of the highly active taxa detected by only rRNA.}, keywords = {Archaea, Bacteria, Biodiversity, Cluster Analysis, Ecosystem, Genes, rRNA, Oligonucleotide Array Sequence Analysis, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Soil Microbiology, Trees, Tropical Climate}, issn = {1098-5336}, doi = {10.1128/AEM.07547-11}, author = {Deangelis, Kristen M and Firestone, Mary K} } @article {414, title = {Supercapacitors based on c-type cytochromes using conductive nanostructured networks of living bacteria.}, journal = {Chemphyschem}, volume = {13}, year = {2012}, month = {2012 Feb}, pages = {463-8}, abstract = {Supercapacitors have attracted interest in energy storage because they have the potential to complement or replace batteries. Here, we report that c-type cytochromes, naturally immersed in a living, electrically conductive microbial biofilm, greatly enhance the device capacitance by over two orders of magnitude. We employ genetic engineering, protein unfolding and Nernstian modeling for in vivo demonstration of charge storage capacity of c-type cytochromes and perform electrochemical impedance spectroscopy, cyclic voltammetry and charge-discharge cycling to confirm the pseudocapacitive, redox nature of biofilm capacitance. The biofilms also show low self-discharge and good charge/discharge reversibility. The superior electrochemical performance of the biofilm is related to its high abundance of cytochromes, providing large electron storage capacity, its nanostructured network with metallic-like conductivity, and its porous architecture with hydrous nature, offering prospects for future low cost and environmentally sustainable energy storage devices.}, keywords = {Bacteria, Biofilms, Cytochrome c Group, Dielectric Spectroscopy, Electric Capacitance, Electrodes, Geobacter, Nanostructures, Oxidation-Reduction}, issn = {1439-7641}, doi = {10.1002/cphc.201100865}, author = {Malvankar, Nikhil S and Mester, T{\"u}nde and Tuominen, Mark T and Lovley, Derek R} } @article {374, title = {Effects of selected root exudate components on soil bacterial communities.}, journal = {FEMS Microbiol Ecol}, volume = {77}, year = {2011}, month = {2011 Sep}, pages = {600-10}, abstract = {Low-molecular-weight organic compounds in root exudates play a key role in plant-microorganism interactions by influencing the structure and function of soil microbial communities. Model exudate solutions, based on organic acids (OAs) (quinic, lactic, maleic acids) and sugars (glucose, sucrose, fructose), previously identified in the rhizosphere of Pinus radiata, were applied to soil microcosms. Root exudate compound solutions stimulated soil dehydrogenase activity and the addition of OAs increased soil pH. The structure of active bacterial communities, based on reverse-transcribed 16S rRNA gene PCR, was assessed by denaturing gradient gel electrophoresis and PhyloChip microarrays. Bacterial taxon richness was greater in all treatments than that in control soil, with a wide range of taxa (88-1043) responding positively to exudate solutions and fewer (<24) responding negatively. OAs caused significantly greater increases than sugars in the detectable richness of the soil bacterial community and larger shifts of dominant taxa. The greater response of bacteria to OAs may be due to the higher amounts of added carbon, solubilization of soil organic matter or shifts in soil pH. Our results indicate that OAs play a significant role in shaping soil bacterial communities and this may therefore have a significant impact on plant growth.}, keywords = {Bacteria, DNA, Bacterial, Molecular Sequence Data, Organic Chemicals, Phylogeny, Pinus, Plant Exudates, Plant Roots, Rhizosphere, RNA, Ribosomal, 16S, Soil, Soil Microbiology}, issn = {1574-6941}, doi = {10.1111/j.1574-6941.2011.01150.x}, author = {Shi, Shengjing and Richardson, Alan E and O{\textquoteright}Callaghan, Maureen and Deangelis, Kristen M and Jones, Eirian E and Stewart, Alison and Firestone, Mary K and Condron, Leo M} } @article {1569, title = {Field application of nitrogen and phenylacetylene to mitigate greenhouse gas emissions from landfill cover soils: effects on microbial community structure.}, journal = {Appl Microbiol Biotechnol}, volume = {89}, year = {2011}, month = {2011 Jan}, pages = {189-200}, abstract = {

Landfills are large sources of CH(4), but a considerable amount of CH(4) can be removed in situ by methanotrophs if their activity can be stimulated through the addition of nitrogen. Nitrogen can, however, lead to increased N(2)O production. To examine the effects of nitrogen and a selective inhibitor on CH(4) oxidation and N(2)O production in situ, 0.5 M of NH(4)Cl and 0.25 M of KNO(3), with and without 0.01\% (w/v) phenylacetylene, were applied to test plots at a landfill in Kalamazoo, MI from 2007 November to 2009 July. Nitrogen amendments stimulated N(2)O production but had no effect on CH(4) oxidation. The addition of phenylacetylene stimulated CH(4) oxidation while reducing N(2)O production. Methanotrophs possessing particulate methane monooxygenase and archaeal ammonia-oxidizers (AOAs) were abundant. The addition of nitrogen reduced methanotrophic diversity, particularly for type I methanotrophs. The simultaneous addition of phenylacetylene increased methanotrophic diversity and the presence of type I methanotrophs. Clone libraries of the archaeal amoA gene showed that the addition of nitrogen increased AOAs affiliated with Crenarchaeal group 1.1b, while they decreased with the simultaneous addition of phenylacetylene. These results suggest that the addition of phenylacetylene with nitrogen reduces N(2)O production by selectively inhibiting AOAs and/or type II methanotrophs.

}, keywords = {Acetylene, Archaea, Archaeal Proteins, Bacteria, Bacterial Proteins, Gases, Greenhouse Effect, Methane, Molecular Sequence Data, Nitrogen, Refuse Disposal, Soil, Soil Microbiology}, issn = {1432-0614}, doi = {10.1007/s00253-010-2811-0}, author = {Im, Jeongdae and Lee, Sung-Woo and Bodrossy, Levente and Barcelona, Michael J and Semrau, Jeremy D} } @article {372, title = {Metagenomic analysis of a permafrost microbial community reveals a rapid response to thaw.}, journal = {Nature}, volume = {480}, year = {2011}, month = {2011 Dec 15}, pages = {368-71}, abstract = {Permafrost contains an estimated 1672 Pg carbon (C), an amount roughly equivalent to the total currently contained within land plants and the atmosphere. This reservoir of C is vulnerable to decomposition as rising global temperatures cause the permafrost to thaw. During thaw, trapped organic matter may become more accessible for microbial degradation and result in greenhouse gas emissions. Despite recent advances in the use of molecular tools to study permafrost microbial communities, their response to thaw remains unclear. Here we use deep metagenomic sequencing to determine the impact of thaw on microbial phylogenetic and functional genes, and relate these data to measurements of methane emissions. Metagenomics, the direct sequencing of DNA from the environment, allows the examination of whole biochemical pathways and associated processes, as opposed to individual pieces of the metabolic puzzle. Our metagenome analyses reveal that during transition from a frozen to a thawed state there are rapid shifts in many microbial, phylogenetic and functional gene abundances and pathways. After one week of incubation at 5 {\textdegree}C, permafrost metagenomes converge to be more similar to each other than while they are frozen. We find that multiple genes involved in cycling of C and nitrogen shift rapidly during thaw. We also construct the first draft genome from a complex soil metagenome, which corresponds to a novel methanogen. Methane previously accumulated in permafrost is released during thaw and subsequently consumed by methanotrophic bacteria. Together these data point towards the importance of rapid cycling of methane and nitrogen in thawing permafrost.}, keywords = {Alaska, Arctic Regions, Bacteria, Carbon, Carbon Cycle, DNA, Freezing, Genes, rRNA, Metagenome, Metagenomics, Methane, Nitrogen, Nitrogen Cycle, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Soil, Soil Microbiology, Temperature, Time Factors}, issn = {1476-4687}, doi = {10.1038/nature10576}, author = {Mackelprang, Rachel and Waldrop, Mark P and Deangelis, Kristen M and David, Maude M and Chavarria, Krystle L and Blazewicz, Steven J and Rubin, Edward M and Jansson, Janet K} } @article {425, title = {A shift in the current: new applications and concepts for microbe-electrode electron exchange.}, journal = {Curr Opin Biotechnol}, volume = {22}, year = {2011}, month = {2011 Jun}, pages = {441-8}, abstract = {Perceived applications of microbe-electrode interactions are shifting from production of electric power to other technologies, some of which even consume current. Electrodes can serve as stable, long-term electron acceptors for contaminant-degrading microbes to promote rapid degradation of organic pollutants in anaerobic subsurface environments. Solar and other forms of renewable electrical energy can be used to provide electrons extracted from water to microorganisms on electrodes at suitably low potentials for a number of groundwater bioremediation applications as well as for the production of fuels and other organic compounds from carbon dioxide. The understanding of how microorganisms exchange electrons with electrodes has improved substantially and is expected to be helpful in optimizing practical applications of microbe-electrode interactions, as well as yielding insights into related natural environmental phenomena.}, keywords = {Bacteria, Biodegradation, Environmental, Biofuels, Carbon Dioxide, Electricity, Electrodes, Electrons, Environmental Pollutants, Fungi, Microbiological Phenomena, Organic Chemicals}, issn = {1879-0429}, doi = {10.1016/j.copbio.2011.01.009}, author = {Lovley, Derek R and Nevin, Kelly P} } @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 {376, title = {Microbial communities acclimate to recurring changes in soil redox potential status.}, journal = {Environ Microbiol}, volume = {12}, year = {2010}, month = {2010 Dec}, pages = {3137-49}, abstract = {Rapidly fluctuating environmental conditions can significantly stress organisms, particularly when fluctuations cross thresholds of normal physiological tolerance. Redox potential fluctuations are common in humid tropical soils, and microbial community acclimation or avoidance strategies for survival will in turn shape microbial community diversity and biogeochemistry. To assess the extent to which indigenous bacterial and archaeal communities are adapted to changing in redox potential, soils were incubated under static anoxic, static oxic or fluctuating redox potential conditions, and the standing (DNA-based) and active (RNA-based) communities and biogeochemistry were determined. Fluctuating redox potential conditions permitted simultaneous CO$_{2}$ respiration, methanogenesis, N$_{2}$O production and iron reduction. Exposure to static anaerobic conditions significantly changed community composition, while 4-day redox potential fluctuations did not. Using RNA:DNA ratios as a measure of activity, 285 taxa were more active under fluctuating than static conditions, compared with three taxa that were more active under static compared with fluctuating conditions. These data suggest an indigenous microbial community adapted to fluctuating redox potential.}, keywords = {Acclimatization, Archaea, Bacteria, Carbon Dioxide, DNA, Archaeal, DNA, Bacterial, Iron, Oligonucleotide Array Sequence Analysis, Oxidation-Reduction, RNA, Archaeal, RNA, Bacterial, Soil, Soil Microbiology, Trees}, issn = {1462-2920}, doi = {10.1111/j.1462-2920.2010.02286.x}, author = {Deangelis, Kristen M and Silver, Whendee L and Thompson, Andrew W and Firestone, Mary K} } @article {730, title = {Phytoprotective influence of bacteria on growth and cadmium accumulation in the aquatic plant Lemna minor.}, journal = {Water Res}, volume = {44}, year = {2010}, month = {2010 Sep}, pages = {4970-9}, abstract = {Certain plants are known to accumulate heavy metals, and can be used in remediation of polluted soil or water. Plant-associated bacteria, especially those that are metal tolerant, may enhance the total amount of metal accumulated by the plant, but this process is still unclear. In this study, we investigated metal enhancement vs. exclusion by plants, and the phytoprotective role plant-associated bacteria might provide to plants exposed to heavy metal. We isolated cadmium-tolerant bacteria from the roots of the aquatic plant Lemna minor grown in heavy metal-polluted waters, and tested these isolates for tolerance to cadmium. The efficiency of plants to accumulate heavy metal from their surrounding environment was then tested by comparing L. minor plants grown with added metal tolerant bacteria to plants grown axenically to determine, whether bacteria associated with these plants increase metal accumulation in the plant. Unexpectedly, cadmium tolerance was not seen in all bacterial isolates that had been exposed to cadmium. Axenic plants accumulated slightly more cadmium than plants inoculated with bacterial isolates. Certain isolates promoted root growth, but overall, addition of bacterial strains did not enhance plant cadmium uptake, and in some cases, inhibited cadmium accumulation by plants. This suggests that bacteria serve a phytoprotective role in their relationship with Lemna minor, preventing toxic cadmium from entering plants.}, keywords = {Adaptation, Physiological, Araceae, Bacteria, Biodegradation, Environmental, Cadmium, Hydrogen-Ion Concentration, Molecular Sequence Data, Plant Roots, Siderophores, Water}, issn = {1879-2448}, doi = {10.1016/j.watres.2010.07.073}, author = {Stout, Lisa M and Dodova, Elena N and Tyson, Julian F and N{\"u}sslein, Klaus} } @article {377, title = {Bacterial diversity analysis of Huanglongbing pathogen-infected citrus, using PhyloChip arrays and 16S rRNA gene clone library sequencing.}, journal = {Appl Environ Microbiol}, volume = {75}, year = {2009}, month = {2009 Mar}, pages = {1566-74}, abstract = {The bacterial diversity associated with citrus leaf midribs was characterized for citrus groves that contained the Huanglongbing (HLB) pathogen, which has yet to be cultivated in vitro. We employed a combination of high-density phylogenetic 16S rRNA gene microarrays and 16S rRNA gene clone library sequencing to determine the microbial community composition for symptomatic and asymptomatic citrus midribs. Our results revealed that citrus leaf midribs can support a diversity of microbes. PhyloChip analysis indicated that 47 orders of bacteria in 15 phyla were present in the citrus leaf midribs, while 20 orders in 8 phyla were observed with the cloning and sequencing method. PhyloChip arrays indicated that nine taxa were significantly more abundant in symptomatic midribs than in asymptomatic midribs. "Candidatus Liberibacter asiaticus" was detected at a very low level in asymptomatic plants but was over 200 times more abundant in symptomatic plants. The PhyloChip analysis results were further verified by sequencing 16S rRNA gene clone libraries, which indicated the dominance of "Candidatus Liberibacter asiaticus" in symptomatic leaves. These data implicate "Candidatus Liberibacter asiaticus" as the pathogen responsible for HLB disease.}, keywords = {Bacteria, Biodiversity, Citrus, DNA, Bacterial, DNA, Ribosomal, Genes, rRNA, Microarray Analysis, Molecular Sequence Data, Phylogeny, Plant Diseases, Plant Leaves, Rhizobiaceae, RNA, Bacterial, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Sequence Homology, Nucleic Acid}, issn = {1098-5336}, doi = {10.1128/AEM.02404-08}, author = {Sagaram, Uma Shankar and Deangelis, Kristen M and Trivedi, Pankaj and Andersen, Gary L and Lu, Shi-En and Wang, Nian} } @article {735, title = {Biological perchlorate reduction in packed bed reactors using elemental sulfur.}, journal = {Environ Sci Technol}, volume = {43}, year = {2009}, month = {2009 Jun 15}, pages = {4466-71}, abstract = {Sulfur-utilizing perchlorate (ClO4-)-reducing bacteria were enriched from a denitrifying wastewater seed with elemental sulfur (S0) as an electron donor. The enrichment was composed of a diverse microbial community, with the majority identified as members of the phylum Proteobacteria. Cultures were inoculated into bench-scale packed bed reactors (PBR) with S0 and crushed oyster shell packing media. High ClO4-concentrations (5-8 mg/L) were reduced to < 0.5 mg/L at an empty bed contact time (EBCT) of 13 h. Low C1O4- concentrations (60-120 microg/L), more typical of contaminated groundwater sites, were reduced to < 4 microg/L at an EBCT of 7.5 h. PBR performance decreased when effluent recirculation was applied or when smaller S0 particle sizes were used, indicating that mass transfer of ClO4- to the attached biofilm was not the limiting mechanism in this process, and that biofilm acclimation and growth were key factors in overall reactor performance. The presence of nitrate (6.5 mg N/L) inhibited ClO4- reduction. The microbial community composition was found to change with ClO4- availability from a majority of Beta-Proteobacteria near the influent end of the reactor to primarily sulfur-oxidizing bacteria near the effluent end of the reactor.}, keywords = {Bacteria, Bioreactors, Environmental Pollutants, Medical Waste Disposal, Oxidation-Reduction, Perchloric Acid, Sulfur}, issn = {0013-936X}, author = {Sahu, Ashish K and Conneely, Teresa and N{\"u}sslein, Klaus R and Ergas, Sarina J} } @article {739, title = {Comparison of facially amphiphilic versus segregated monomers in the design of antibacterial copolymers.}, journal = {Chemistry}, volume = {15}, year = {2009}, month = {2009}, pages = {433-9}, abstract = {A direct comparison of two strategies for designing antimicrobial polymers is presented. Previously, we published several reports on the use of facially amphiphilic (FA) monomers which led to polynorbornenes with excellent antimicrobial activities and selectivities. Our polymers obtained by copolymerization of structurally similar segregated monomers, in which cationic and non-polar moieties reside on separate repeat units, led to polymers with less pronounced activities. A wide range of polymer amphiphilicities was surveyed by pairing a cationic oxanorbornene with eleven different non-polar monomers and varying the comonomer feed ratios. Their properties were tested using antimicrobial assays and copolymers possessing intermediate hydrophobicities were the most active. Polymer-induced leakage of dye-filled liposomes and microscopy of polymer-treated bacteria support a membrane-based mode of action. From these results there appears to be profound differences in how a polymer made from FA monomers interacts with the phospholipid bilayer compared with copolymers from segregated monomers. We conclude that a well-defined spatial relationship of the whole polymer is crucial to obtain synthetic mimics of antimicrobial peptides (SMAMPs): charged and non-polar moieties need to be balanced locally, for example, at the monomer level, and not just globally. We advocate the use of FA monomers for better control of biological properties. It is expected that this principle will be usefully applied to other backbones such as the polyacrylates, polystyrenes, and non-natural polyamides.}, keywords = {Anti-Bacterial Agents, Bacteria, Cell Membrane, Drug Design, Hemolysis, Plastics, Polymers, Surface-Active Agents}, issn = {1521-3765}, doi = {10.1002/chem.200801233}, author = {Gabriel, Gregory J and Maegerlein, Janet A and Nelson, Christopher F and Dabkowski, Jeffrey M and Eren, Tarik and N{\"u}sslein, Klaus and Tew, Gregory N} } @article {1570, title = {Effect of nutrient and selective inhibitor amendments on methane oxidation, nitrous oxide production, and key gene presence and expression in landfill cover soils: characterization of the role of methanotrophs, nitrifiers, and denitrifiers.}, journal = {Appl Microbiol Biotechnol}, volume = {85}, year = {2009}, month = {2009 Nov}, pages = {389-403}, abstract = {

Methane and nitrous oxide are both potent greenhouse gasses, with global warming potentials approximately 25 and 298 times that of carbon dioxide. A matrix of soil microcosms was constructed with landfill cover soils collected from the King Highway Landfill in Kalamazoo, Michigan and exposed to geochemical parameters known to affect methane consumption by methanotrophs while also examining their impact on biogenic nitrous oxide production. It was found that relatively dry soils (5\% moisture content) along with 15 mg NH (4) (+) (kg soil)(-1) and 0.1 mg phenylacetylene(kg soil)(-1) provided the greatest stimulation of methane oxidation while minimizing nitrous oxide production. Microarray analyses of pmoA showed that the methanotrophic community structure was dominated by Type II organisms, but Type I genera were more evident with the addition of ammonia. When phenylacetylene was added in conjunction with ammonia, the methanotrophic community structure was more similar to that observed in the presence of no amendments. PCR analyses showed the presence of amoA from both ammonia-oxidizing bacteria and archaea, and that the presence of key genes associated with these cells was reduced with the addition of phenylacetylene. Messenger RNA analyses found transcripts of pmoA, but not of mmoX, nirK, norB, or amoA from either ammonia-oxidizing bacteria or archaea. Pure culture analyses showed that methanotrophs could produce significant amounts of nitrous oxide, particularly when expressing the particulate methane monooxygenase (pMMO). Collectively, these data suggest that methanotrophs expressing pMMO played a role in nitrous oxide production in these microcosms.

}, keywords = {Archaea, Bacteria, Base Sequence, DNA, DNA Primers, DNA, Archaeal, DNA, Bacterial, Global Warming, Greenhouse Effect, Inorganic Chemicals, Methane, Nitrites, Nitrogen, Nitrogen Oxides, Nitrous Oxide, Oxidation-Reduction, Polymerase Chain Reaction, Reverse Transcriptase Polymerase Chain Reaction, RNA, Bacterial, RNA, Messenger, Soil, Water Pollutants, Chemical}, issn = {1432-0614}, doi = {10.1007/s00253-009-2238-7}, author = {Lee, Sung-Woo and Im, Jeongdae and Dispirito, Alan A and Bodrossy, Levente and Barcelona, Michael J and Semrau, Jeremy D} } @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 {738, title = {Hydrophilic modifications of an amphiphilic polynorbornene and the effects on its hemolytic and antibacterial activity.}, journal = {Biomacromolecules}, volume = {10}, year = {2009}, month = {2009 Feb 9}, pages = {353-9}, abstract = {Here we report the modification of an amphiphilic antibacterial polynorbornene, Poly3, via incorporation of hydrophilic, biocompatible groups. The sugar, zwitterionic, and polyethylene glycol based moieties were incorporated in varying ratios by copolymerization and postpolymerization techniques. Well-defined copolymers with molecular weights of 3 kDa and narrow polydispersity indices ranging from 1.08 to 1.15 were obtained. The effects of these modifications on the biological activity of these polymers were analyzed by determining their minimum inhibitory concentrations (MIC) and their hemolytic activities (HC50).}, keywords = {Anti-Bacterial Agents, Bacteria, Biocompatible Materials, Carbohydrates, Hemolysis, Microbial Sensitivity Tests, Plastics, Polyethylene, Static Electricity}, issn = {1526-4602}, doi = {10.1021/bm801129y}, author = {Colak, Semra and Nelson, Christopher F and N{\"u}sslein, Klaus and Tew, Gregory N} } @article {378, title = {Selective progressive response of soil microbial community to wild oat roots.}, journal = {ISME J}, volume = {3}, year = {2009}, month = {2009 Feb}, pages = {168-78}, abstract = {Roots moving through soil induce physical and chemical changes that differentiate rhizosphere from bulk soil, and the effects of these changes on soil microorganisms have long been a topic of interest. The use of a high-density 16S rRNA microarray (PhyloChip) for bacterial and archaeal community analysis has allowed definition of the populations that respond to the root within the complex grassland soil community; this research accompanies compositional changes reported earlier, including increases in chitinase- and protease-specific activity, cell numbers and quorum sensing signal. PhyloChip results showed a significant change compared with bulk soil in relative abundance for 7\% of the total rhizosphere microbial community (147 of 1917 taxa); the 7\% response value was confirmed by16S rRNA terminal restriction fragment length polymorphism analysis. This PhyloChip-defined dynamic subset was comprised of taxa in 17 of the 44 phyla detected in all soil samples. Expected rhizosphere-competent phyla, such as Proteobacteria and Firmicutes, were well represented, as were less-well-documented rhizosphere colonizers including Actinobacteria, Verrucomicrobia and Nitrospira. Richness of Bacteroidetes and Actinobacteria decreased in soil near the root tip compared with bulk soil, but then increased in older root zones. Quantitative PCR revealed rhizosphere abundance of beta-Proteobacteria and Actinobacteria at about 10(8) copies of 16S rRNA genes per g soil, with Nitrospira having about 10(5) copies per g soil. This report demonstrates that changes in a relatively small subset of the soil microbial community are sufficient to produce substantial changes in functions observed earlier in progressively more mature rhizosphere zones.}, keywords = {Avena sativa, Bacteria, Biodiversity, Colony Count, Microbial, Microarray Analysis, Oligonucleotide Array Sequence Analysis, Plant Roots, Polymerase Chain Reaction, RNA, Bacterial, RNA, Ribosomal, 16S, Soil Microbiology}, issn = {1751-7370}, doi = {10.1038/ismej.2008.103}, author = {Deangelis, Kristen M and Brodie, Eoin L and DeSantis, Todd Z and Andersen, Gary L and Lindow, Steven E and Firestone, Mary K} } @article {497, title = {Growth of thermophilic and hyperthermophilic Fe(III)-reducing microorganisms on a ferruginous smectite as the sole electron acceptor.}, journal = {Appl Environ Microbiol}, volume = {74}, year = {2008}, month = {2008 Jan}, pages = {251-8}, abstract = {Recent studies have suggested that the structural Fe(III) within phyllosilicate minerals, including smectite and illite, is an important electron acceptor for Fe(III)-reducing microorganisms in sedimentary environments at moderate temperatures. The reduction of structural Fe(III) by thermophiles, however, has not previously been described. A wide range of thermophilic and hyperthermophilic Archaea and Bacteria from marine and freshwater environments that are known to reduce poorly crystalline Fe(III) oxides were tested for their ability to reduce structural (octahedrally coordinated) Fe(III) in smectite (SWa-1) as the sole electron acceptor. Two out of the 10 organisms tested, Geoglobus ahangari and Geothermobacterium ferrireducens, were not able to conserve energy to support growth by reduction of Fe(III) in SWa-1 despite the fact that both organisms were originally isolated with solid-phase Fe(III) as the electron acceptor. The other organisms tested were able to grow on SWa-1 and reduced 6.3 to 15.1\% of the Fe(III). This is 20 to 50\% less than the reported amounts of Fe(III) reduced in the same smectite (SWa-1) by mesophilic Fe(III) reducers. Two organisms, Geothermobacter ehrlichii and archaeal strain 140, produced copious amounts of an exopolysaccharide material, which may have played an active role in the dissolution of the structural iron in SWa-1 smectite. The reduction of structural Fe(III) in SWa-1 by archaeal strain 140 was studied in detail. Microbial Fe(III) reduction was accompanied by an increase in interlayer and octahedral charges and some incorporation of potassium and magnesium into the smectite structure. However, these changes in the major element chemistry of SWa-1 smectite did not result in the formation of an illite-like structure, as reported for a mesophilic Fe(III) reducer. These results suggest that thermophilic Fe(III)-reducing organisms differ in their ability to reduce and solubilize structural Fe(III) in SWa-1 smectite and that SWa-1 is not easily transformed to illite by these organisms.}, keywords = {Archaea, Bacteria, Ferric Compounds, Geologic Sediments, Hot Temperature, Oxidation-Reduction, Silicates}, issn = {1098-5336}, doi = {10.1128/AEM.01580-07}, author = {Kashefi, Kazem and Shelobolina, Evgenya S and Elliott, W Crawford and Lovley, Derek R} } @article {468, title = {The microbe electric: conversion of organic matter to electricity.}, journal = {Curr Opin Biotechnol}, volume = {19}, year = {2008}, month = {2008 Dec}, pages = {564-71}, abstract = {Broad application of microbial fuel cells will require substantial increases in current density. A better understanding of the microbiology of these systems may help. Recent studies have greatly expanded the range of microorganisms known to function either as electrode-reducing microorganisms at the anode or as electrode-oxidizing microorganisms at the cathode. Microorganisms that can completely oxidize organic compounds with an electrode serving as the sole electron acceptor are expected to be the primary contributors to power production. Several mechanisms for electron transfer to anodes have been proposed including: direct electron transfer via outer-surface c-type cytochromes, long-range electron transfer via microbial nanowires, electron flow through a conductive biofilm matrix containing cytochromes, and soluble electron shuttles. Which mechanisms are most important depend on the microorganisms and the thickness of the anode biofilm. Emerging systems biology approaches to the study, design, and evolution of microorganisms interacting with electrodes are expected to contribute to improved microbial fuel cells.}, keywords = {Bacteria, Bioelectric Energy Sources, Electricity, Electrodes, Organic Chemicals, Oxidation-Reduction}, issn = {1879-0429}, doi = {10.1016/j.copbio.2008.10.005}, author = {Lovley, Derek R} } @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 {746, title = {Comparative bacterial diversity in recent Hawaiian volcanic deposits of different ages.}, journal = {FEMS Microbiol Ecol}, volume = {60}, year = {2007}, month = {2007 Apr}, pages = {60-73}, abstract = {Volcanic activity creates new landforms that can change dramatically over time as a consequence of biotic succession. Nonetheless, volcanic deposits present severe constraints for microbial colonization and activity. We have characterized bacterial diversity on four recent deposits at Kilauea volcano, Hawaii (KVD). Much of the diversity was either closely related to uncultured organisms or distinct from any reported 16S rRNA gene sequences. Diversity indices suggested that diversity was highest in a moderately vegetated 210-year-old ash deposit (1790-KVD), and lowest for a 79-year-old lava flow (1921-KVD). Diversity for a 41-year-old tephra deposit (1959-KVD) and a 300-year-old rainforest (1700-KVD) reached intermediate values. The 1959-KVD and 1790-KVD communities were dominated by Acidobacteria, Alpha- and Gammaproteobacteria, Actinobacteria, Cyanobacteria, and many unclassified phylotypes. The 1921-KVD, an unvegetated low pH deposit, was dominated by unclassified phylotypes. In contrast, 1700-KVD was primarily populated by Alphaproteobacteria with very few unclassified phylotypes. Similar diversity indices and levels of trace gas flux were found for 1959-KVD and 1790-KVD; however, statistical analyses indicated significantly different communities. This study not only showed that microorganisms colonize recent volcanic deposits and are able to establish diverse communities, but also that their composition is governed by variations in local deposit parameters.}, keywords = {Bacteria, DNA, Bacterial, Ecosystem, Genes, rRNA, Genetic Variation, Hawaii, Molecular Sequence Data, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Soil Microbiology, Time Factors, Volcanic Eruptions}, issn = {0168-6496}, doi = {10.1111/j.1574-6941.2006.00253.x}, author = {Gomez-Alvarez, Vicente and King, Gary M and N{\"u}sslein, Klaus} } @article {519, title = {Bug juice: harvesting electricity with microorganisms.}, journal = {Nat Rev Microbiol}, volume = {4}, year = {2006}, month = {2006 Jul}, pages = {497-508}, abstract = {It is well established that some reduced fermentation products or microbially reduced artificial mediators can abiotically react with electrodes to yield a small electrical current. This type of metabolism does not typically result in an efficient conversion of organic compounds to electricity because only some metabolic end products will react with electrodes, and the microorganisms only incompletely oxidize their organic fuels. A new form of microbial respiration has recently been discovered in which microorganisms conserve energy to support growth by oxidizing organic compounds to carbon dioxide with direct quantitative electron transfer to electrodes. These organisms, termed electricigens, offer the possibility of efficiently converting organic compounds into electricity in self-sustaining systems with long-term stability.}, keywords = {Bacteria, Bioelectric Energy Sources, Electricity, Electrodes, Electron Transport, Oxidation-Reduction}, issn = {1740-1526}, doi = {10.1038/nrmicro1442}, author = {Lovley, Derek R} } @article {748, title = {Distribution of extensive nifH gene diversity across physical soil microenvironments.}, journal = {Microb Ecol}, volume = {51}, year = {2006}, month = {2006 May}, pages = {441-52}, abstract = {The diversity of nitrogen-fixing bacteria is well described for aquatic environments; however, terrestrial analyses remain mostly biased to rhizobial plant-microbe associations. We maximized the level of resolution for this study through the use of nucleotide sequence information extracted from a series of soil microenvironments, ranging from macroaggregates at 2000 microm to the clay fraction at < 75 microm in diameter. In addition, we attempted to create an overview of the distribution of terrestrial nitrogen fixers across such microenvironments by combining culture-independent techniques with a suite of natural soil environments from uniquely different origins. Soil diazotroph diversity was analyzed phylogenetically for 600 terrestrial nifH sequences from 12 midsized clone libraries based on microenvironments of three separate soils across a global scale. Statistical analyses of nifH gene clone libraries were used to estimate coverage, establish degrees of sequence overlap, and compare cluster distributions. These analyses revealed an extensive diversity in a tropical (19 phylotypes) and an arctic soil (17 phylotypes), and moderate diversity in a temperate soil (11 phylotypes). Within each soil, comparisons across aggregate size fractions delineated nifH gene cluster shifts within populations and degrees of sequence overlap that ranged from significantly different (arctic, tropical) to significantly similar (temperate). We suggest that this is due to population separation across aggregates of different size classes, which results from differences in the temporal stability of aggregates as niches for microbial communities. This study not only provides new knowledge of the arrangement of diazotrophic communities at the soil microscale, but it also contributes to the underrepresented knowledge of soil nifH sequences in the public databases.}, keywords = {Bacteria, Base Sequence, DNA Primers, Genes, Bacterial, Multigene Family, Oxidoreductases, Phylogeny, Polymerase Chain Reaction, Soil Microbiology}, issn = {0095-3628}, doi = {10.1007/s00248-006-9044-x}, author = {Izquierdo, Javier A and N{\"u}sslein, Klaus} } @article {540, title = {Evidence for involvement of an electron shuttle in electricity generation by Geothrix fermentans.}, journal = {Appl Environ Microbiol}, volume = {71}, year = {2005}, month = {2005 Apr}, pages = {2186-9}, abstract = {In experiments performed using graphite electrodes poised by a potentiostat (+200 mV versus Ag/AgCl) or in a microbial fuel cell (with oxygen as the electron acceptor), the Fe(III)-reducing organism Geothrix fermentans conserved energy to support growth by coupling the complete oxidation of acetate to reduction of a graphite electrode. Other organic compounds, such as lactate, malate, propionate, and succinate as well as components of peptone and yeast extract, were utilized for electricity production. However, electrical characteristics and the results of shuttling assays indicated that unlike previously described electrode-reducing microorganisms, G. fermentans produced a compound that promoted electrode reduction. This is the first report of complete oxidation of organic compounds linked to electrode reduction by an isolate outside of the Proteobacteria.}, keywords = {Acetates, Bacteria, Bioelectric Energy Sources, Electricity, Electrodes, Electron Transport, Graphite, Microscopy, Electron, Scanning, Oxidation-Reduction}, issn = {0099-2240}, doi = {10.1128/AEM.71.4.2186-2189.2005}, author = {Bond, Daniel R and Lovley, Derek R} } @article {751, title = {Shifts in rhizoplane communities of aquatic plants after cadmium exposure.}, journal = {Appl Environ Microbiol}, volume = {71}, year = {2005}, month = {2005 May}, pages = {2484-92}, abstract = {In this study we present the comparative molecular analysis of bacterial communities of the aquatic plant Lemna minor from a contaminated site (RCP) and from a laboratory culture (EPA), as well as each of these with the addition of cadmium. Plants were identified as L. minor by analysis of the rpl16 chloroplast region. Comparative bacterial community studies were based on the analyses of 16S rRNA clone libraries, each containing about 100 clones from the root surfaces of plants. Bacterial communities were compared at three phylogenetic levels of resolution. At the level of bacterial divisions, differences in diversity index scores between treatments, with and without cadmium within the same plant type (EPA or RCP), were small, indicating that cadmium had little effect. When we compared genera within the most dominant group, the beta-proteobacteria, differences between unamended and cadmium-amended libraries were much larger. Bacterial diversity increased upon cadmium addition for both EPA and RCP libraries. Analyses of diversity at the phylotype level showed parallel shifts to more even communities upon cadmium addition; that is, percentage changes in diversity indices due to cadmium addition were the same for either plant type, indicating that contamination history might be independent of disturbance-induced diversity shifts. At finer phylogenetic levels of resolution, the effects of cadmium addition on bacterial communities were very noticeable. This study is a first step in understanding the role of aquatic plant-associated microbial communities in phytoremediation of heavy metals.}, keywords = {Araceae, Bacteria, Base Sequence, Cadmium, Molecular Sequence Data, Phylogeny, Plant Roots, RNA, Ribosomal, 16S}, issn = {0099-2240}, doi = {10.1128/AEM.71.5.2484-2492.2005}, author = {Stout, Lisa M and N{\"u}sslein, Klaus} } @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 {1216, title = {Microbe-metal interactions in marine hydrothermal environments.}, journal = {Curr Opin Chem Biol}, volume = {7}, year = {2003}, month = {2003 Apr}, pages = {160-5}, abstract = {

Marine hydrothermal microorganisms respond rapidly to changes in the concentrations and availability of metals within their environment. Hyperthermophilic archaea appear to possess novel mechanisms for metal detoxification, dissimilatory metal reduction and metal assimilation that may be absent in their mesophilic and bacterial counterparts. For example, tungsten was found in high concentrations in a hydrothermal sulfide deposit where hyperthermophiles were also most abundant, consistent with the unique requirement of these organisms for this element. Furthermore, newly isolated genera of iron-reducing hyperthermophiles expand the scope of carbon cycling in hydrothermal environments. The advent of genome sequences and new molecular techniques will facilitate our further understanding of microbe-mineral interactions in these environments.

}, keywords = {Archaea, Bacteria, Environment, Marine Biology, Metals, Seawater, Temperature}, issn = {1367-5931}, author = {Holden, James F and Adams, Michael W W} } @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 {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} } @article {401, title = {Measuring beta-galactosidase activity in bacteria: cell growth, permeabilization, and enzyme assays in 96-well arrays.}, journal = {Biochem Biophys Res Commun}, volume = {290}, year = {2002}, month = {2002 Jan 11}, pages = {397-402}, abstract = {We describe a high-throughput procedure for measuring beta-galactosidase activity in bacteria. This procedure is unique because all manipulations, including bacterial growth and cell permeabilization, are performed in a 96-well format. Cells are permeabilized by chloroform/SDS treatment directly in the 96-well blocks and then transferred to 96-well microplates for standard colorimetric assay of beta-galactosidase activity as described by Miller [J. H. Miller (1972) Experiments in Molecular Genetics, Cold Spring Harbor Laboratory Press, Cold Spring Harbor, NY]. Absorbance data are collected with a microplate reader and analyzed using a Microsoft Excel spreadsheet. The beta-galactosidase specific activity values obtained with the high-throughput procedure are identical to those obtained by the traditional single-tube method of Miller. Thus, values obtained with this procedure may be expressed as Miller units and compared directly to Miller units reported in the literature. The 96-well format for permeabilization and assay of enzyme specific activity together with the use of 12-channel and repeater pipettors enables efficient processing of hundreds of samples in an 8-h day.}, keywords = {Bacteria, beta-Galactosidase, Biochemistry, Cell Division, Chloroform, Escherichia coli, Polypropylenes, Sodium Dodecyl Sulfate, Software, Spectrophotometry, Time Factors}, issn = {0006-291X}, doi = {10.1006/bbrc.2001.6152}, author = {Griffith, Kevin L and Wolf, Richard E} } @article {584, title = {Mechanisms for accessing insoluble Fe(III) oxide during dissimilatory Fe(III) reduction by Geothrix fermentans.}, journal = {Appl Environ Microbiol}, volume = {68}, year = {2002}, month = {2002 May}, pages = {2294-9}, abstract = {Mechanisms for Fe(III) oxide reduction were investigated in Geothrix fermentans, a dissimilatory Fe(III)-reducing microorganism found within the Fe(III) reduction zone of subsurface environments. Culture filtrates of G. fermentans stimulated the reduction of poorly crystalline Fe(III) oxide by washed cell suspensions, suggesting that G. fermentans released one or more extracellular compounds that promoted Fe(III) oxide reduction. In order to determine if G. fermentans released electron-shuttling compounds, poorly crystalline Fe(III) oxide was incorporated into microporous alginate beads, which prevented contact between G. fermentans and the Fe(III) oxide. G. fermentans reduced the Fe(III) within the beads, suggesting that one of the compounds that G. fermentans releases is an electron-shuttling compound that can transfer electrons from the cell to Fe(III) oxide that is not in contact with the organism. Analysis of culture filtrates by thin-layer chromatography suggested that the electron shuttle has characteristics similar to those of a water-soluble quinone. Analysis of filtrates by ion chromatography demonstrated that there was as much as 250 microM dissolved Fe(III) in cultures of G. fermentans growing with Fe(III) oxide as the electron acceptor, suggesting that G. fermentans released one or more compounds capable of chelating and solubilizing Fe(III). Solubilizing Fe(III) is another strategy for alleviating the need for contact between cells and Fe(III) oxide for Fe(III) reduction. This is the first demonstration of a microorganism that, in defined medium without added electron shuttles or chelators, can reduce Fe(III) derived from Fe(III) oxide without directly contacting the Fe(III) oxide. These results are in marked contrast to those with Geobacter metallireducens, which does not produce electron shuttles or Fe(III) chelators. These results demonstrate that phylogenetically distinct Fe(III)-reducing microorganisms may use significantly different strategies for Fe(III) reduction. Thus, it is important to know which Fe(III)-reducing microorganisms predominate in a given environment in order to understand the mechanisms for Fe(III) reduction in the environment of interest.}, keywords = {Bacteria, Electrons, Ferric Compounds, Iron Chelating Agents, Oxidation-Reduction, Solubility}, issn = {0099-2240}, author = {Nevin, Kelly P and Lovley, Derek R} } @article {596, title = {Microbial detoxification of metals and radionuclides.}, journal = {Curr Opin Biotechnol}, volume = {12}, year = {2001}, month = {2001 Jun}, pages = {248-53}, abstract = {Microorganisms have important roles in the biogeochemical cycling of toxic metals and radionuclides. Recent advances have been made in understanding metal-microbe interactions and new applications of these processes to the detoxification of metal and radionuclide contamination have been developed.}, keywords = {Bacteria, Biodegradation, Environmental, Biotechnology, Environmental Pollution, Genetic Engineering, Geologic Sediments, Metals, Heavy, Radioisotopes}, issn = {0958-1669}, author = {Lloyd, J R and Lovley, D R} } @article {594, title = {Reductive precipitation of gold by dissimilatory Fe(III)-reducing bacteria and archaea.}, journal = {Appl Environ Microbiol}, volume = {67}, year = {2001}, month = {2001 Jul}, pages = {3275-9}, abstract = {Studies with a diversity of hyperthermophilic and mesophilic dissimilatory Fe(III)-reducing Bacteria and Archaea demonstrated that some of these organisms are capable of precipitating gold by reducing Au(III) to Au(0) with hydrogen as the electron donor. These studies suggest that models for the formation of gold deposits in both hydrothermal and cooler environments should consider the possibility that dissimilatory metal-reducing microorganisms can reductively precipitate gold from solution.}, keywords = {Archaea, Bacteria, Chemical Precipitation, Ferric Compounds, Gold, Oxidation-Reduction}, issn = {0099-2240}, doi = {10.1128/AEM.67.7.3275-3279.2001}, author = {Kashefi, K and Tor, J M and Nevin, K P and Lovley, D R} } @article {612, title = {Hexadecane decay by methanogenesis.}, journal = {Nature}, volume = {404}, year = {2000}, month = {2000 Apr 13}, pages = {722-3}, keywords = {Alkanes, Anaerobiosis, Bacteria, Biodegradation, Environmental, Geologic Sediments, Methane, Petroleum}, issn = {0028-0836}, doi = {10.1038/35008145}, author = {Anderson, R T and Lovley, D R} } @article {828, title = {The importance of repairing stalled replication forks.}, journal = {Nature}, volume = {404}, year = {2000}, month = {2000 Mar 2}, pages = {37-41}, abstract = {The bacterial SOS response to unusual levels of DNA damage has been recognized and studied for several decades. Pathways for re-establishing inactivated replication forks under normal growth conditions have received far less attention. In bacteria growing aerobically in the absence of SOS-inducing conditions, many replication forks encounter DNA damage, leading to inactivation. The pathways for fork reactivation involve the homologous recombination systems, are nonmutagenic, and integrate almost every aspect of DNA metabolism. On a frequency-of-use basis, these pathways represent the main function of bacterial DNA recombination systems, as well as the main function of a number of other enzymatic systems that are associated with replication and site-specific recombination.}, keywords = {Bacteria, Bacterial Proteins, Chromosomes, Bacterial, DNA Replication, DNA, Bacterial, Escherichia coli, Recombination, Genetic, Replication Origin, SOS Response (Genetics)}, issn = {0028-0836}, doi = {10.1038/35003501}, author = {Cox, M M and Goodman, M F and Kreuzer, K N and Sherratt, D J and Sandler, S J and Marians, K J} } @article {832, title = {Diversity of radA genes from cultured and uncultured archaea: comparative analysis of putative RadA proteins and their use as a phylogenetic marker.}, journal = {J Bacteriol}, volume = {181}, year = {1999}, month = {1999 Feb}, pages = {907-15}, abstract = {Archaea-specific radA primers were used with PCR to amplify fragments of radA genes from 11 cultivated archaeal species and one marine sponge tissue sample that contained essentially an archaeal monoculture. The amino acid sequences encoded by the PCR fragments, three RadA protein sequences previously published (21), and two new complete RadA sequences were aligned with representative bacterial RecA proteins and eucaryal Rad51 and Dmc1 proteins. The alignment supported the existence of four insertions and one deletion in the archaeal and eucaryal sequences relative to the bacterial sequences. The sizes of three of the insertions were found to have taxonomic and phylogenetic significance. Comparative analysis of the RadA sequences, omitting amino acids in the insertions and deletions, shows a cladal distribution of species which mimics to a large extent that obtained by a similar analysis of archaeal 16S rRNA sequences. The PCR technique also was used to amplify fragments of 15 radA genes from uncultured natural sources. Phylogenetic analysis of the amino acid sequences encoded by these fragments reveals several clades with affinity, sometimes only distant, to the putative RadA proteins of several species of Crenarcheota. The two most deeply branching archaeal radA genes found had some amino acid deletion and insertion patterns characteristic of bacterial recA genes. Possible explanations are discussed. Finally, signature codons are presented to distinguish among RecA protein family members.}, keywords = {Amino Acid Sequence, Archaea, Archaeal Proteins, Bacteria, Bacterial Proteins, Cloning, Molecular, DNA Primers, DNA Repair, DNA-Binding Proteins, Evolution, Molecular, Humans, Molecular Sequence Data, Phylogeny, Polymerase Chain Reaction, Recombinant Proteins, RNA, Ribosomal, 16S, Saccharomyces cerevisiae, Sequence Alignment}, issn = {0021-9193}, author = {Sandler, S J and Hugenholtz, P and Schleper, C and DeLong, E F and Pace, N R and Clark, A J} } @article {605, title = {Humics as an electron donor for anaerobic respiration.}, journal = {Environ Microbiol}, volume = {1}, year = {1999}, month = {1999 Feb}, pages = {89-98}, abstract = {The possibility that microorganisms might use reduced humic substances (humics) as an electron donor for the reduction of electron acceptors with a more positive redox potential was investigated. All of the Fe(III)- and humics-reducing microorganisms evaluated were capable of oxidizing reduced humics and/or the reduced humics analogue anthrahydroquinone-2,6,-disulphonate (AHODS), with nitrate and/or fumarate as the electron acceptor. These included Geobacter metallireducens, Geobacter sulphurreducens, Geothrix fermentans, Shewanella alga, Wolinella succinogenes and {\textquoteright}S. barnesii{\textquoteright}. Several of the humics-oxidizing microorganisms grew in medium with AHQDS as the sole electron donor and fumarate as the electron acceptor. Even though it does not reduce Fe(III) or humics, Paracoccus denitrificans could use AHQDS and reduced humics as electron donors for denitrification. However, another denitrifier, Pseudomonas denitrificans, could not. AHODS could also serve as an electron donor for selenate and arsenate reduction by W. succinogenes. Electron spin resonance studies demonstrated that humics oxidation was associated with the oxidation of hydroquinone moieties in the humics. Studies with G. metallireducens and W. succinogenes demonstrated that the anthraquinone-2,6-disulphonate (AQDS)/AHQDS redox couple mediated an interspecies electron transfer between the two organisms. These results suggest that, as microbially reduced humics enter less reduced zones of soils and sediments, the reduced humics may serve as electron donors for microbial reduction of several environmentally significant electron acceptors.}, keywords = {Aerobiosis, Anaerobiosis, Anthraquinones, Arsenates, Bacteria, Electron Transport, Fumarates, Humic Substances, Selenium Compounds, Tumor Cells, Cultured}, issn = {1462-2912}, author = {Lovley, D R and Fraga, J L and Coates, J D and Blunt-Harris, E L} } @article {831, title = {Replication fork assembly at recombination intermediates is required for bacterial growth.}, journal = {Proc Natl Acad Sci U S A}, volume = {96}, year = {1999}, month = {1999 Mar 30}, pages = {3552-5}, abstract = {PriA, a 3{\textquoteright} --> 5{\textquoteright} DNA helicase, directs assembly of a primosome on some bacteriophage and plasmid DNAs. Primosomes are multienzyme replication machines that contribute both the DNA-unwinding and Okazaki fragment-priming functions at the replication fork. The role of PriA in chromosomal replication is unclear. The phenotypes of priA null mutations suggest that the protein participates in replication restart at recombination intermediates. We show here that PriA promotes replication fork assembly at a D loop, an intermediate formed during initiation of homologous recombination. We also show that DnaC810, encoded by a naturally arising intergenic suppressor allele of the priA2::kan mutation, bypasses the need for PriA during replication fork assembly at D loops in vitro. These findings underscore the essentiality of replication fork restart at recombination intermediates under normal growth conditions in bacteria.}, keywords = {Bacteria, Bacteriophage phi X 174, Base Sequence, DNA Polymerase III, DNA Replication, DNA-Binding Proteins, Escherichia coli, Molecular Sequence Data, Oligodeoxyribonucleotides, Open Reading Frames, Recombination, Genetic, Replication Protein A, Templates, Genetic}, issn = {0027-8424}, author = {Liu, J and Xu, L and Sandler, S J and Marians, K J} } @article {753, title = {Soil bacterial community shift correlated with change from forest to pasture vegetation in a tropical soil.}, journal = {Appl Environ Microbiol}, volume = {65}, year = {1999}, month = {1999 Aug}, pages = {3622-6}, abstract = {The change in vegetative cover of a Hawaiian soil from forest to pasture led to significant changes in the composition of the soil bacterial community. DNAs were extracted from both soil habitats and compared for the abundance of guanine-plus-cytosine (G+C) content, by analysis of abundance of phylotypes of small-subunit ribosomal DNA (SSU rDNA) amplified from fractions with 63 and 35\% G+C contents, and by phylogenetic analysis of the dominant rDNA clones in the 63\% G+C content fraction. All three methods showed differences between the forest and pasture habitats, providing evidence that vegetation had a strong influence on microbial community composition at three levels of taxon resolution. The forest soil DNA had a peak in G+C content of 61\%, while the DNA of the pasture soil had a peak in G+C content of 67\%. None of the dominant phylotypes found in the forest soil were detected in the pasture soil. For the 63\% G+C fraction SSU rDNA sequence analysis of the three most dominant members revealed that their phyla changed from Fibrobacter and Syntrophomonas assemblages in the forest soil to Burkholderia and Rhizobium-Agrobacterium assemblages in the pasture soil.}, keywords = {Agriculture, Bacteria, Base Composition, DNA, Bacterial, Ecosystem, Molecular Sequence Data, Soil Microbiology, Trees, Tropical Climate}, issn = {0099-2240}, author = {N{\"u}sslein, K and Tiedje, J M} } @article {622, title = {Humic acids as electron acceptors for anaerobic microbial oxidation of vinyl chloride and dichloroethene.}, journal = {Appl Environ Microbiol}, volume = {64}, year = {1998}, month = {1998 Aug}, pages = {3102-5}, abstract = {Anaerobic oxidation of [1,2-14C]vinyl chloride and [1, 2-14C]dichloroethene to 14CO2 under humic acid-reducing conditions was demonstrated. The results indicate that waterborne contaminants can be oxidized by using humic acid compounds as electron acceptors and suggest that natural aquatic systems have a much larger capacity for contaminant oxidation than previously thought.}, keywords = {Aerobiosis, Anaerobiosis, Bacteria, Biodegradation, Environmental, Geologic Sediments, Humic Substances, Oxidation-Reduction, Vinyl Chloride, Water Microbiology, Water Pollutants}, issn = {0099-2240}, author = {Bradley, P M and Chapelle, F H and Lovley, D R} } @article {629, title = {Bioremediation of metal contamination.}, journal = {Curr Opin Biotechnol}, volume = {8}, year = {1997}, month = {1997 Jun}, pages = {285-9}, abstract = {Recent studies have demonstrated that microbes might be used to remediate metal contamination by removing metals from contaminated water or waste streams, sequestering metals in soils and sediments or solubilizing metals to aid in their extraction. This is primarily accomplished either by biosorption of metals or enzymatically catalyzed changes in the metal redox state. Bioremediation of metals is still primarily a research problem with little large-scale application of this technology.}, keywords = {Adsorption, Bacteria, Biomass, Biotechnology, Environmental Pollutants, Metals, Oxidation-Reduction}, issn = {0958-1669}, author = {Lovley, D R and Coates, J D} } @article {834, title = {Evolutionary comparisons of RecA-like proteins across all major kingdoms of living organisms.}, journal = {J Mol Evol}, volume = {44}, year = {1997}, month = {1997 May}, pages = {528-41}, abstract = {Protein sequences with similarities to Escherichia coli RecA were compared across the major kingdoms of eubacteria, archaebacteria, and eukaryotes. The archaeal sequences branch monophyletically and are most closely related to the eukaryotic paralogous Rad51 and Dmc1 groups. A multiple alignment of the sequences suggests a modular structure of RecA-like proteins consisting of distinct segments, some of which are conserved only within subgroups of sequences. The eukaryotic and archaeal sequences share an N-terminal domain which may play a role in interactions with other factors and nucleic acids. Several positions in the alignment blocks are highly conserved within the eubacteria as one group and within the eukaryotes and archaebacteria as a second group, but compared between the groups these positions display nonconservative amino acid substitutions. Conservation within the RecA-like core domain identifies possible key residues involved in ATP-induced conformational changes. We propose that RecA-like proteins derive evolutionarily from an assortment of independent domains and that the functional homologs of RecA in noneubacteria comprise an array of RecA-like proteins acting in series or cooperatively.}, keywords = {Amino Acid Sequence, Animals, Archaeal Proteins, Bacteria, Bacterial Proteins, Cell Cycle Proteins, Consensus Sequence, Conserved Sequence, DNA-Binding Proteins, Escherichia coli Proteins, Evolution, Molecular, Humans, Molecular Sequence Data, Phylogeny, Rad51 Recombinase, Rec A Recombinases, Sequence Alignment}, issn = {0022-2844}, author = {Brendel, V and Brocchieri, L and Sandler, S J and Clark, A J and Karlin, S} } @article {630, title = {Geovibrio ferrireducens, a phylogenetically distinct dissimilatory Fe(III)-reducing bacterium.}, journal = {Arch Microbiol}, volume = {165}, year = {1996}, month = {1996 Jun}, pages = {370-6}, abstract = {A new, phylogenetically distinct, dissimilatory, Fe(III)-reducing bacterium was isolated from surface sediment of a hydrocarbon-contaminated ditch. The isolate, designated strain PAL-1, was an obligately anaerobic, non-fermentative, motile, gram-negative vibrio. PAL-1 grew in a defined medium with acetate as electron donor and ferric pyrophosphate, ferric oxyhydroxide, ferric citrate, Co(III)-EDTA, or elemental sulfur as sole electron acceptor. PAL-1 also used proline, hydrogen, lactate, propionate, succinate, fumarate, pyruvate, or yeast extract as electron donors for Fe(III) reduction. It is the first bacterium known to couple the oxidation of an amino acid to Fe(III) reduction. PAl-1 did not reduce oxygen, Mn(IV), U(VI), Cr(VI), nitrate, sulfate, sulfite, or thiosulfate with acetate as the electron donor. Cell suspensions of PAL-1 exhibited dithionite-reduced minus air-oxidized difference spectra that were characteristic of c-type cytochromes. Analysis of the 16S rRNA gene sequence of PAL-1 showed that the strain is not related to any of the described metal-reducing bacteria in the Proteobacteria and, together with Flexistipes sinusarabici, forms a separate line of descent within the Bacteria. Phenotypically and phylogenetically, strain PAl-1 differs from all other described bacteria, and represents the type strain of a new genus and species, Geovibrio ferrireducens.}, keywords = {Bacteria, Base Composition, Iron, Phylogeny}, issn = {0302-8933}, author = {Caccavo, F and Coates, J D and Rossello-Mora, R A and Ludwig, W and Schleifer, K H and Lovley, D R and McInerney, M J} } @article {641, title = {Bioremediation of organic and metal contaminants with dissimilatory metal reduction.}, journal = {J Ind Microbiol}, volume = {14}, year = {1995}, month = {1995 Feb}, pages = {85-93}, abstract = {Dissimilatory metal reduction has the potential to be a helpful mechanism for both intrinsic and engineered bioremediation of contaminated environments. Dissimilatory Fe(III) reduction is an important intrinsic process for removing organic contaminants from aquifers contaminated with petroleum or landfill leachate. Stimulation of microbial Fe(III) reduction can enhance the degradation of organic contaminants in ground water. Dissimilatory reduction of uranium, selenium, chromium, technetium, and possibly other metals, can convert soluble metal species to insoluble forms that can readily be removed from contaminated waters or waste streams. Reduction of mercury can volatilize mercury from waters and soils. Despite its potential, there has as yet been limited applied research into the use of dissimilatory metal reduction as a bioremediation tool.}, keywords = {Bacteria, Biodegradation, Environmental, Chromium, Hydrocarbons, Iron, Mercury, Metals, Oxidation-Reduction, Selenium, Uranium}, issn = {0169-4146}, author = {Lovley, D R} } @article {652, title = {Dissimilatory metal reduction.}, journal = {Annu Rev Microbiol}, volume = {47}, year = {1993}, month = {1993}, pages = {263-90}, abstract = {Microorganisms can enzymatically reduce a variety of metals in metabolic processes that are not related to metal assimilation. Some microorganisms can conserve energy to support growth by coupling the oxidation of simple organic acids and alcohols, H2, or aromatic compounds to the reduction of Fe(III) or Mn(IV). This dissimilatory Fe(III) and Mn(IV) reduction influences the organic as well as the inorganic geochemistry of anaerobic aquatic sediments and ground water. Microorganisms that use U(VI) as a terminal electron acceptor play an important role in uranium geochemistry and may be a useful tool for removing uranium from contaminated environments. Se(VI) serves as a terminal electron acceptor to support anaerobic growth of some microorganisms. Reduction of Se(VI) to Se(O) is an important mechanism for the precipitation of selenium from contaminated waters. Enzymatic reduction of Cr(VI) to the less mobile and less toxic Cr(III), and reduction of soluble Hg(II) to volatile Hg(O) may affect the fate of these compounds in the environment and might be used as a remediation strategy. Microorganisms can also enzymatically reduce other metals such as technetium, vanadium, molybdenum, gold, silver, and copper, but reduction of these metals has not been studied extensively.}, keywords = {Bacteria, Metals, Oxidation-Reduction}, issn = {0066-4227}, doi = {10.1146/annurev.mi.47.100193.001403}, author = {Lovley, D R} } @article {872, title = {Acetate catabolism in the dissimilatory iron-reducing isolate GS-15.}, journal = {J Bacteriol}, volume = {173}, year = {1991}, month = {1991 Apr}, pages = {2704-6}, abstract = {Acetate-grown GS-15 whole-cell suspensions were disrupted with detergent and assayed for enzymes associated with acetate catabolism. Carbon monoxide dehydrogenase and formate dehydrogenase were not observed in GS-15. Catabolic levels of acetokinase and phosphotransacetylase were observed. Enzyme activities of the citric acid cycle, i.e., isocitrate dehydrogenase, 2-oxoglutarate sythase, succinate dehydrogenase, fumarase, and malate dehydrogenase, were observed.}, keywords = {Acetate Kinase, Acetates, Acetyl Coenzyme A, Bacteria, Carbon Monoxide, Citric Acid Cycle, Electron Transport, Euryarchaeota, Fumarate Hydratase, Isocitrate Dehydrogenase, Ketone Oxidoreductases, Malate Dehydrogenase, Phosphate Acetyltransferase, Pseudomonas aeruginosa, Succinate Dehydrogenase}, issn = {0021-9193}, author = {Champine, J E and Goodwin, S} } @article {656, title = {Dissimilatory Fe(III) and Mn(IV) reduction.}, journal = {Microbiol Rev}, volume = {55}, year = {1991}, month = {1991 Jun}, pages = {259-87}, abstract = {The oxidation of organic matter coupled to the reduction of Fe(III) or Mn(IV) is one of the most important biogeochemical reactions in aquatic sediments, soils, and groundwater. This process, which may have been the first globally significant mechanism for the oxidation of organic matter to carbon dioxide, plays an important role in the oxidation of natural and contaminant organic compounds in a variety of environments and contributes to other phenomena of widespread significance such as the release of metals and nutrients into water supplies, the magnetization of sediments, and the corrosion of metal. Until recently, much of the Fe(III) and Mn(IV) reduction in sedimentary environments was considered to be the result of nonenzymatic processes. However, microorganisms which can effectively couple the oxidation of organic compounds to the reduction of Fe(III) or Mn(IV) have recently been discovered. With Fe(III) or Mn(IV) as the sole electron acceptor, these organisms can completely oxidize fatty acids, hydrogen, or a variety of monoaromatic compounds. This metabolism provides energy to support growth. Sugars and amino acids can be completely oxidized by the cooperative activity of fermentative microorganisms and hydrogen- and fatty-acid-oxidizing Fe(III) and Mn(IV) reducers. This provides a microbial mechanism for the oxidation of the complex assemblage of sedimentary organic matter in Fe(III)- or Mn(IV)-reducing environments. The available evidence indicates that this enzymatic reduction of Fe(III) or Mn(IV) accounts for most of the oxidation of organic matter coupled to reduction of Fe(III) and Mn(IV) in sedimentary environments. Little is known about the diversity and ecology of the microorganisms responsible for Fe(III) and Mn(IV) reduction, and only preliminary studies have been conducted on the physiology and biochemistry of this process.}, keywords = {Bacteria, Electron Transport, Ferric Compounds, Fungi, Geological Phenomena, Geology, Manganese, Oxidation-Reduction, Soil Microbiology, Water Microbiology}, issn = {0146-0749}, author = {Lovley, D R} } @article {1707, title = {Citrate synthase.}, journal = {Curr Top Cell Regul}, volume = {10}, year = {1976}, month = {1976}, pages = {161-204}, keywords = {Adenosine Diphosphate, Adenosine Monophosphate, Adenosine Triphosphate, Amino Acids, Animals, Bacteria, Binding Sites, Cations, Divalent, Cations, Monovalent, Citrate (si)-Synthase, Dithionitrobenzoic Acid, Ketoglutaric Acids, Kinetics, Molecular Weight, NAD, NADP, Oxo-Acid-Lyases, Protein Binding, Species Specificity}, issn = {0070-2137}, author = {Weitzman, P D and Danson, M J} }