@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 {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 {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 {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 {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}
}
