Stable Carbon Isotope Fractionation by Methanosarcina barkeri during Methanogenesis from Acetate, Methanol, or Carbon Dioxide-Hydrogen.
about
Thermodynamic and hydrochemical controls on CH4 in a coal seam gas and overlying alluvial aquifer: new insights into CH4 originsActivation of methanogenesis in arid biological soil crusts despite the presence of oxygenInvestigation of the microbial metabolism of carbon dioxide and hydrogen in the kangaroo foregut by stable isotope probingTrimethylamine and Organic Matter Additions Reverse Substrate Limitation Effects on the δ13C Values of Methane Produced in Hypersaline Microbial Mats.Complementary Microorganisms in Highly Corrosive Biofilms from an Offshore Oil Production Facility.Rerouting Cellular Electron Flux To Increase the Rate of Biological Methane Production.Carbon isotope effects associated with aceticlastic methanogenesis.Solute Concentrations Influence Microbial Methanogenesis in Coal-bearing Strata of the Cherokee Basin, USA.Carbon isotope fractionation of 11 acetogenic strains grown on H2 and CO2.Physiology, Biochemistry, and Applications of F420- and Fo-Dependent Redox Reactions.Stable hydrogen and carbon isotope fractionation during microbial toluene degradation: mechanistic and environmental aspects.Carbon Isotope Fractionation during Catabolism and Anabolism in Acetogenic Bacteria Growing on Different Substrates.Stable isotope fractionation caused by glycyl radical enzymes during bacterial degradation of aromatic compounds.Stable carbon isotope fractionation by methylotrophic methanogenic archaea.Carbon isotope fractionation during acetoclastic methanogenesis by Methanosaeta concilii in culture and a lake sediment.Effect of substrate concentration on carbon isotope fractionation during acetoclastic methanogenesis by Methanosarcina barkeri and M. acetivorans and in rice field soil.Methanogenic archaea are globally ubiquitous in aerated soils and become active under wet anoxic conditions.Description of an estuarine methylotrophic methanogen which grows on dimethyl sulfide.The deep-subsurface sulfate reducer Desulfotomaculum kuznetsovii employs two methanol-degrading pathways.Conductive Particles Enable Syntrophic Acetate Oxidation between Geobacter and Methanosarcina from Coastal Sediments.
P2860
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P2860
Stable Carbon Isotope Fractionation by Methanosarcina barkeri during Methanogenesis from Acetate, Methanol, or Carbon Dioxide-Hydrogen.
description
1987 nî lūn-bûn
@nan
1987年の論文
@ja
1987年論文
@yue
1987年論文
@zh-hant
1987年論文
@zh-hk
1987年論文
@zh-mo
1987年論文
@zh-tw
1987年论文
@wuu
1987年论文
@zh
1987年论文
@zh-cn
name
Stable Carbon Isotope Fraction ...... l, or Carbon Dioxide-Hydrogen.
@ast
Stable Carbon Isotope Fraction ...... l, or Carbon Dioxide-Hydrogen.
@en
type
label
Stable Carbon Isotope Fraction ...... l, or Carbon Dioxide-Hydrogen.
@ast
Stable Carbon Isotope Fraction ...... l, or Carbon Dioxide-Hydrogen.
@en
prefLabel
Stable Carbon Isotope Fraction ...... l, or Carbon Dioxide-Hydrogen.
@ast
Stable Carbon Isotope Fraction ...... l, or Carbon Dioxide-Hydrogen.
@en
P2093
P2860
P1476
Stable Carbon Isotope Fraction ...... ol, or Carbon Dioxide-Hydrogen
@en
P2093
P2860
P304
P407
P577
1987-10-01T00:00:00Z