@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 {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 {419, title = {Genome-scale analysis of anaerobic benzoate and phenol metabolism in the hyperthermophilic archaeon Ferroglobus placidus.}, journal = {ISME J}, volume = {6}, year = {2012}, month = {2012 Jan}, pages = {146-57}, abstract = {Insight into the mechanisms for the anaerobic metabolism of aromatic compounds by the hyperthermophilic archaeon Ferroglobus placidus is expected to improve understanding of the degradation of aromatics in hot (>80{\textdegree} C) environments and to identify enzymes that might have biotechnological applications. Analysis of the F. placidus genome revealed genes predicted to encode enzymes homologous to those previously identified as having a role in benzoate and phenol metabolism in mesophilic bacteria. Surprisingly, F. placidus lacks genes for an ATP-independent class II benzoyl-CoA (coenzyme A) reductase (BCR) found in all strictly anaerobic bacteria, but has instead genes coding for a bzd-type ATP-consuming class I BCR, similar to those found in facultative bacteria. The lower portion of the benzoate degradation pathway appears to be more similar to that found in the phototroph Rhodopseudomonas palustris, than the pathway reported for all heterotrophic anaerobic benzoate degraders. Many of the genes predicted to be involved in benzoate metabolism were found in one of two gene clusters. Genes for phenol carboxylation proceeding through a phenylphosphate intermediate were identified in a single gene cluster. Analysis of transcript abundance with a whole-genome microarray and quantitative reverse transcriptase polymerase chain reaction demonstrated that most of the genes predicted to be involved in benzoate or phenol metabolism had higher transcript abundance during growth on those substrates vs growth on acetate. These results suggest that the general strategies for benzoate and phenol metabolism are highly conserved between microorganisms living in moderate and hot environments, and that anaerobic metabolism of aromatic compounds might be analyzed in a wide range of environments with similar molecular targets.}, keywords = {Acetates, Archaea, Bacteria, Anaerobic, Benzoates, Metabolic Networks and Pathways, Phenol, Rhodopseudomonas}, issn = {1751-7370}, doi = {10.1038/ismej.2011.88}, author = {Holmes, Dawn E and Risso, Carla and Smith, Jessica A and Lovley, Derek R} } @article {1206, title = {Hydrogen-limited growth of hyperthermophilic methanogens at deep-sea hydrothermal vents.}, journal = {Proc Natl Acad Sci U S A}, volume = {109}, year = {2012}, month = {2012 Aug 21}, pages = {13674-9}, abstract = {

Microbial productivity at hydrothermal vents is among the highest found anywhere in the deep ocean, but constraints on microbial growth and metabolism at vents are lacking. We used a combination of cultivation, molecular, and geochemical tools to verify pure culture H(2) threshold measurements for hyperthermophilic methanogenesis in low-temperature hydrothermal fluids from Axial Volcano and Endeavour Segment in the northeastern Pacific Ocean. Two Methanocaldococcus strains from Axial and Methanocaldococcus jannaschii showed similar Monod growth kinetics when grown in a bioreactor at varying H(2) concentrations. Their H(2) half-saturation value was 66 μM, and growth ceased below 17-23 μM H(2), 10-fold lower than previously predicted. By comparison, measured H(2) and CH(4) concentrations in fluids suggest that there was generally sufficient H(2) for Methanocaldococcus growth at Axial but not at Endeavour. Fluids from one vent at Axial (Marker 113) had anomalously high CH(4) concentrations and contained various thermal classes of methanogens based on cultivation and mcrA/mrtA analyses. At Endeavour, methanogens were largely undetectable in fluid samples based on cultivation and molecular screens, although abundances of hyperthermophilic heterotrophs were relatively high. Where present, Methanocaldococcus genes were the predominant mcrA/mrtA sequences recovered and comprised \~{}0.2-6\% of the total archaeal community. Field and coculture data suggest that H(2) limitation may be partly ameliorated by H(2) syntrophy with hyperthermophilic heterotrophs. These data support our estimated H(2) threshold for hyperthermophilic methanogenesis at vents and highlight the need for coupled laboratory and field measurements to constrain microbial distribution and biogeochemical impacts in the deep sea.

}, keywords = {Archaea, Biodiversity, Coculture Techniques, DNA, Ribosomal, Ecosystem, Gases, Geography, Hydrogen, Hydrothermal Vents, Kinetics, Methane, Molecular Sequence Data, Temperature, Time Factors, Water Microbiology}, issn = {1091-6490}, doi = {10.1073/pnas.1206632109}, author = {Ver Eecke, Helene C and Butterfield, David A and Huber, Julie A and Lilley, Marvin D and Olson, Eric J and Roe, Kevin K and Evans, Leigh J and Merkel, Alexandr Y and Cantin, Holly V and Holden, James F} } @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 {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 {1208, title = {Production of hydrogen from α-1,4- and β-1,4-linked saccharides by marine hyperthermophilic Archaea.}, journal = {Appl Environ Microbiol}, volume = {77}, year = {2011}, month = {2011 May}, pages = {3169-73}, abstract = {

Nineteen hyperthermophilic heterotrophs from deep-sea hydrothermal vents, plus the control organism Pyrococcus furiosus, were examined for their ability to grow and produce H$_{2}$ on maltose, cellobiose, and peptides and for the presence of the genes encoding proteins that hydrolyze starch and cellulose. All of the strains grew on these disaccharides and peptides and converted maltose and peptides to H$_{2}$ even when elemental sulfur was present as a terminal electron acceptor. Half of the strains had at least one gene for an extracellular starch hydrolase, but only P. furiosus had a gene for an extracellular β-1,4-endoglucanase. P. furiosus was serially adapted for growth on CF11 cellulose and H$_{2}$ production, which is the first reported instance of hyperthermophilic growth on cellulose, with a doubling time of 64 min. Cell-specific H$_{2}$ production rates were 29 fmol, 37 fmol, and 54 fmol of H$_{2}$ produced cell$^{-}${\textonesuperior} doubling$^{-}${\textonesuperior} on α-1,4-linked sugars, β-1,4-linked sugars, and peptides, respectively. The highest total community H$_{2}$ production rate came from growth on starch (2.6 mM H$_{2}$ produced h$^{-}${\textonesuperior}). Hyperthermophilic heterotrophs may serve as an important alternate source of H$_{2}$ for hydrogenotrophic microorganisms in low-H$_{2}$ hydrothermal environments, and some are candidates for H$_{2}$ bioenergy production in bioreactors.

}, keywords = {Archaea, Carbohydrate Metabolism, Hot Springs, Hydro-Lyases, Hydrogen, Peptides, Seawater}, issn = {1098-5336}, doi = {10.1128/AEM.01366-10}, author = {Oslowski, Daniel M and Jung, Jong-Hyun and Seo, Dong-Ho and Park, Cheon-Seok and Holden, James F} } @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 {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 {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 {744, title = {Salinity constraints on subsurface archaeal diversity and methanogenesis in sedimentary rock rich in organic matter.}, journal = {Appl Environ Microbiol}, volume = {73}, year = {2007}, month = {2007 Jul}, pages = {4171-9}, abstract = {The diversity of microorganisms active within sedimentary rocks provides important controls on the geochemistry of many subsurface environments. In particular, biodegradation of organic matter in sedimentary rocks contributes to the biogeochemical cycling of carbon and other elements and strongly impacts the recovery and quality of fossil fuel resources. In this study, archaeal diversity was investigated along a salinity gradient spanning 8 to 3,490 mM Cl(-) in a subsurface shale rich in CH(4) derived from biodegradation of sedimentary hydrocarbons. Shale pore waters collected from wells in the main CH(4)-producing zone lacked electron acceptors such as O(2), NO(3)(-), Fe(3+), or SO(4)(2-). Acetate was detected only in high-salinity waters, suggesting that acetoclastic methanogenesis is inhibited at Cl(-) concentrations above approximately 1,000 mM. Most-probable-number series revealed differences in methanogen substrate utilization (acetate, trimethylamine, or H(2)/CO(2)) associated with chlorinity. The greatest methane production in enrichment cultures was observed for incubations with salinity at or close to the native pore water salinity of the inoculum. Restriction fragment length polymorphism analyses of archaeal 16S rRNA genes from seven wells indicated that there were links between archaeal communities and pore water salinity. Archaeal clone libraries constructed from sequences from 16S rRNA genes isolated from two wells revealed phylotypes similar to a halophilic methylotrophic Methanohalophilus species and a hydrogenotrophic Methanoplanus species at high salinity and a single phylotype closely related to Methanocorpusculum bavaricum at low salinity. These results show that several distinct communities of methanogens persist in this subsurface, CH(4)-producing environment and that each community is adapted to particular conditions of salinity and preferential substrate use and each community induces distinct geochemical signatures in shale formation waters.}, keywords = {Archaea, Base Sequence, Cloning, Molecular, DNA Primers, Genes, Archaeal, Genetic Variation, Geologic Sediments, Methane, Michigan, Molecular Sequence Data, Organic Chemicals, Phylogeny, RNA, Archaeal, RNA, Ribosomal, 16S, Sodium Chloride, Soil, Soil Microbiology, Water Microbiology}, issn = {0099-2240}, doi = {10.1128/AEM.02810-06}, author = {Waldron, Patricia J and Petsch, Steven T and Martini, Anna M and N{\"u}sslein, Klaus and N{\"u}slein, Klaus} } @article {545, title = {Dissimilatory Fe(III) and Mn(IV) reduction.}, journal = {Adv Microb Physiol}, volume = {49}, year = {2004}, month = {2004}, pages = {219-86}, abstract = {Dissimilatory Fe(III) and Mn(IV) reduction has an important influence on the geochemistry of modern environments, and Fe(III)-reducing microorganisms, most notably those in the Geobacteraceae family, can play an important role in the bioremediation of subsurface environments contaminated with organic or metal contaminants. Microorganisms with the capacity to conserve energy from Fe(III) and Mn(IV) reduction are phylogenetically dispersed throughout the Bacteria and Archaea. The ability to oxidize hydrogen with the reduction of Fe(III) is a highly conserved characteristic of hyperthermophilic microorganisms and one Fe(III)-reducing Archaea grows at the highest temperature yet recorded for any organism. Fe(III)- and Mn(IV)-reducing microorganisms have the ability to oxidize a wide variety of organic compounds, often completely to carbon dioxide. Typical alternative electron acceptors for Fe(III) reducers include oxygen, nitrate, U(VI) and electrodes. Unlike other commonly considered electron acceptors, Fe(III) and Mn(IV) oxides, the most prevalent form of Fe(III) and Mn(IV) in most environments, are insoluble. Thus, Fe(III)- and Mn(IV)-reducing microorganisms face the dilemma of how to transfer electrons derived from central metabolism onto an insoluble, extracellular electron acceptor. Although microbiological and geochemical evidence suggests that Fe(III) reduction may have been the first form of microbial respiration, the capacity for Fe(III) reduction appears to have evolved several times as phylogenetically distinct Fe(III) reducers have different mechanisms for Fe(III) reduction. Geobacter species, which are representative of the family of Fe(III) reducers that predominate in a wide diversity of sedimentary environments, require direct contact with Fe(III) oxides in order to reduce them. In contrast, Shewanella and Geothrix species produce chelators that solubilize Fe(III) and release electron-shuttling compounds that transfer electrons from the cell surface to the surface of Fe(III) oxides not in direct contact with the cells. Electron transfer from the inner membrane to the outer membrane in Geobacter and Shewanella species appears to involve an electron transport chain of inner-membrane, periplasmic, and outer-membrane c-type cytochromes, but the cytochromes involved in these processes in the two organisms are different. In addition, Geobacter species specifically express flagella and pili during growth on Fe(III) and Mn(IV) oxides and are chemotactic to Fe(II) and Mn(II), which may lead Geobacter species to the oxides under anoxic conditions. The physiological characteristics of Geobacter species appear to explain why they have consistently been found to be the predominant Fe(III)- and Mn(IV)-reducing microorganisms in a variety of sedimentary environments. In comparison with other respiratory processes, the study of Fe(III) and Mn(IV) reduction is in its infancy, but genome-enabled approaches are rapidly advancing our understanding of this environmentally significant physiology.}, keywords = {Archaea, Biodegradation, Environmental, Ferric Compounds, Geobacter, Manganese, Manganese Compounds, Oxidation-Reduction, Oxides, Shewanella, Soil Microbiology, Soil Pollutants}, issn = {0065-2911}, doi = {10.1016/S0065-2911(04)49005-5}, author = {Lovley, Derek R and Holmes, Dawn E and Nevin, Kelly P} } @article {561, title = {Biotechnological application of metal-reducing microorganisms.}, journal = {Adv Appl Microbiol}, volume = {53}, year = {2003}, month = {2003}, pages = {85-128}, keywords = {Archaea, Biodegradation, Environmental, Bioreactors, Environmental Microbiology, Geobacter, Gram-Negative Anaerobic Bacteria, Metals, Heavy, Water Pollutants, Chemical}, issn = {0065-2164}, author = {Lloyd, Jonathan R and Lovley, Derek R and Macaskie, Lynne E} } @article {565, title = {Extending the upper temperature limit for life.}, journal = {Science}, volume = {301}, year = {2003}, month = {2003 Aug 15}, pages = {934}, keywords = {Archaea, Culture Media, Ferric Compounds, Hot Temperature, Oxidation-Reduction, Pacific Ocean, Water Microbiology}, issn = {1095-9203}, doi = {10.1126/science.1086823}, author = {Kashefi, Kazem and Lovley, Derek R} } @article {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 {581, title = {Geoglobus ahangari gen. nov., sp. nov., a novel hyperthermophilic archaeon capable of oxidizing organic acids and growing autotrophically on hydrogen with Fe(III) serving as the sole electron acceptor.}, journal = {Int J Syst Evol Microbiol}, volume = {52}, year = {2002}, month = {2002 May}, pages = {719-28}, abstract = {A novel, regular to irregular, coccoid-shaped, anaerobic, Fe(III)-reducing microorganism was isolated from the Guaymas Basin hydrothermal system at a depth of 2000 m. Isolation was carried out with a new technique using Fe(III) oxide as the electron acceptor for the recovery of colonies on solid medium. The isolate, designated strain 234T, was strictly anaerobic and exhibited a tumbling motility. The cells had a single flagellum. Strain 234T grew at temperatures between 65 and 90 degrees C, with an optimum at about 88 degrees C. The optimal salt concentration for growth was around 19 g l(-1). The isolate was capable of growth with H2 as the sole electron donor coupled to the reduction of Fe(III) without the need for an organic carbon source. This is the first example of a dissimilatory Fe(III)-reducing micro-organism capable of growing autotrophically on hydrogen. In addition to molecular hydrogen, strain 234T oxidizes pyruvate, acetate, malate, succinate, peptone, formate, fumarate, yeast extract, glycerol, isoleucine, arginine, serine, glutamine, asparagine, stearate, palmitate, valerate, butyrate and propionate with the reduction of Fe(III). This isolate is the first example of a hyperthermophile capable of oxidizing long-chain fatty acids anaerobically. Isolate 234T grew exclusively with Fe(III) as the sole electron acceptor. The G+C content was 58.7 mol\%. Based on detailed analysis of its 16S rDNA sequence, G+C content, distinguishing physiological features and metabolism, strain 234T is proposed to represent a novel genus within the Archaeoglobales. The name proposed for strain 234T is Geoglobus ahangari gen. nov., sp. nov..}, keywords = {Anaerobiosis, Archaea, Bacterial Typing Techniques, DNA, Ribosomal, Electron Transport, Fatty Acids, Ferric Compounds, Hot Temperature, Hydrogen, Molecular Sequence Data, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Water Microbiology}, issn = {1466-5026}, author = {Kashefi, Kazem and Tor, Jason M and Holmes, Dawn E and Gaw Van Praagh, Catherine V and Reysenbach, Anna-Louise and Lovley, Derek R} } @article {603, title = {Acetate oxidation coupled to Fe(iii) reduction in hyperthermophilic microorganisms.}, journal = {Appl Environ Microbiol}, volume = {67}, year = {2001}, month = {2001 Mar}, pages = {1363-5}, abstract = {No hyperthermophilic microorganisms have previously been shown to anaerobically oxidize acetate, the key extracellular intermediate in the anaerobic oxidation of organic matter. Here we report that two hyperthermophiles, Ferroglobus placidus and "Geoglobus ahangari," grow at 85 degrees C by oxidizing acetate to carbon dioxide, with Fe(III) serving as the electron acceptor. These results demonstrate that acetate could potentially be metabolized within the hot microbial ecosystems in which hyperthermophiles predominate, rather than diffusing to cooler environments prior to degradation as has been previously proposed.}, keywords = {Acetates, Anaerobiosis, Archaea, Ferric Compounds, Hot Temperature, Oxidation-Reduction}, issn = {0099-2240}, doi = {10.1128/AEM.67.3.1363-1365.2001}, author = {Tor, J M and Kashefi, K and Lovley, D R} } @article {598, title = {Anaerobic degradation of aromatic compounds coupled to Fe(III) reduction by Ferroglobus placidus.}, journal = {Environ Microbiol}, volume = {3}, year = {2001}, month = {2001 Apr}, pages = {281-7}, abstract = {Aromatic compounds are an important component of the organic matter in some of the anaerobic environments that hyperthermophilic microorganisms inhabit, but the potential for hyperthermophilic microorganisms to metabolize aromatic compounds has not been described previously. In this study, aromatic metabolism was investigated in the hyperthermophile Ferroglobus placidus. F. placidus grew at 85 degrees C in anaerobic medium with a variety of aromatic compounds as the sole electron donor and poorly crystalline Fe(III) oxide as the electron acceptor. Growth coincided with Fe(III) reduction. Aromatic compounds supporting growth included benzoate, phenol, 4-hydroxybenzoate, benzaldehyde, p-hydroxybenzaldehyde and t-cinnamic acid (3-phenyl-2-propenoic acid). These aromatic compounds did not support growth when nitrate was provided as the electron acceptor, even though nitrate supports the growth of this organism with Fe(II) or H2 as the electron donor. The stoichiometry of benzoate and phenol uptake and Fe(III) reduction indicated that F. placidus completely oxidized these aromatic compounds to carbon dioxide, with Fe(III) serving as the sole electron acceptor. This is the first example of an Archaea that can anaerobically oxidize an aromatic compound. These results also demonstrate for the first time that hyperthermophilic microorganisms can anaerobically oxidize aromatic compounds and suggest that hyperthermophiles may metabolize aromatic compounds in hot environments such as the deep hot subsurface and in marine and terrestrial hydrothermal zones in which Fe(III) is available as an electron acceptor.}, keywords = {Anaerobiosis, Archaea, Electron Transport, Ferric Compounds, Hot Temperature, Hydrocarbons, Aromatic, Oxidation-Reduction}, issn = {1462-2912}, author = {Tor, J M 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 {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 {1197, title = {Overview of hyperthermophiles and their heat-shock proteins.}, journal = {Adv Protein Chem}, volume = {48}, year = {1996}, month = {1996}, pages = {1-34}, keywords = {Archaea, Bacterial Proteins, Heat-Shock Proteins, Hot Temperature, Phylogeny}, issn = {0065-3233}, author = {Baross, J A and Holden, J F} } @article {835, title = {recA-like genes from three archaean species with putative protein products similar to Rad51 and Dmc1 proteins of the yeast Saccharomyces cerevisiae.}, journal = {Nucleic Acids Res}, volume = {24}, year = {1996}, month = {1996 Jun 1}, pages = {2125-32}, abstract = {The process of homologous recombination has been documented in bacterial and eucaryotic organisms. The Escherichia coli RecA and Saccharomyces cerevisiae Rad51 proteins are the archetypal members of two related families of proteins that play a central role in this process. Using the PCR process primed by degenerate oligonucleotides designed to encode regions of the proteins showing the greatest degree of identity, we examined DNA from three organisms of a third phylogenetically divergent group, Archaea, for sequences encoding proteins similar to RecA and Rad51. The archaeans examined were a hyperthermophilic acidophile, Sulfolobus sofataricus (Sso); a halophile, Haloferax volcanii (Hvo); and a hyperthermophilic piezophilic methanogen, Methanococcus jannaschii (Mja). The PCR generated DNA was used to clone a larger genomic DNA fragment containing an open reading frame (orf), that we refer to as the radA gene, for each of the three archaeans. As shown by amino acid sequence alignments, percent amino acid identities and phylogenetic analysis, the putative proteins encoded by all three are related to each other and to both the RecA and Rad51 families of proteins. The putative RadA proteins are more similar to the Rad51 family (approximately 40\% identity at the amino acid level) than to the RecA family (approximately 20\%). Conserved sequence motifs, putative tertiary structures and phylogenetic analysis implied by the alignment are discussed. The 5{\textquoteright} ends of mRNA transcripts to the Sso radA were mapped. The levels of radA mRNA do not increase after treatment with UV irradiation as do recA and RAD51 transcripts in E.coli and S.cerevisiae. Hence it is likely that radA in this organism is a constitutively expressed gene and we discuss possible implications of the lack of UV-inducibility.}, keywords = {Amino Acid Sequence, Archaea, Base Sequence, Cell Cycle Proteins, DNA-Binding Proteins, Escherichia coli, Halobacteriaceae, Methanococcus, Models, Molecular, Molecular Sequence Data, Phylogeny, Rad51 Recombinase, Rec A Recombinases, Saccharomyces cerevisiae, Saccharomyces cerevisiae Proteins, Sequence Alignment, Sulfolobus}, issn = {0305-1048}, author = {Sandler, S J and Satin, L H and Samra, H S and Clark, A J} } @article {1196, title = {Enhanced thermotolerance and temperature-induced changes in protein composition in the hyperthermophilic archaeon ES4.}, journal = {J Bacteriol}, volume = {175}, year = {1993}, month = {1993 May}, pages = {2839-43}, abstract = {

The hyperthermophilic archaeon ES4, a heterotrophic sulfur reducer isolated from a deep-sea hydrothermal vent, is capable of protecting itself from thermal stress at temperatures above its optimum for growth. The thermotolerance of ES4 was determined by exposing log-phase cells to various lethal high temperatures. When ES4 was shifted from 95 to 102 degrees C, it displayed recovery from an exponential rate of death, followed by transient thermotolerance. When ES4 was shifted directly from 95 to either 105 or 108 degrees C, only exponential death occurred. However, a shift from 95 to 105 degrees C with an intermediate incubation at 102 degrees C also gave ES4 transient thermotolerance to 105 degrees C. The protein composition of ES4 was examined at temperatures ranging from 75 to 102 degrees C by one-dimensional electrophoresis. Two proteins with molecular masses of approximately 90 and 150 kDa significantly decreased in abundance with increasing growth temperature, while a 98-kDa protein, present at very low levels at normal growth temperatures (76 to 99 degrees C), was more abundant at higher temperatures. The enhanced tolerance to hyperthermal conditions after a mild hyperthermal exposure and the increased abundance of the 98-kDa protein at above-optimal temperatures imply that ES4 is capable of a heat shock-like response previously unseen in hyperthermophilic archaea.

}, keywords = {Archaea, Bacterial Proteins, Blotting, Western, Electrophoresis, Polyacrylamide Gel, Hot Temperature}, issn = {0021-9193}, author = {Holden, J F and Baross, J A} }