Hydrogen and carbon isotope systematics in hydrogenotrophic methanogenesis under H2-limited and H2-enriched conditions : implications for the origin of methane and its isotopic diagnosis
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DOI[10.1186/s40645-016-0088-3]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Tomoyo OkumuraShinsuke KawagucciYayoi Saito
- Publication, Distribution, etc.
- Publication Date
- 2016-05-12
- Publication Date (W3CDTF)
- 2016-05-12
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 3(14)
- Volume
- 3(14)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-016-0088-3
- Persistent ID (NDL)
- info:ndljp/pid/10016366
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2016-06-22T20:22:58+09:00
- Date Captured (W3CDTF)
- 2016-06-21
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/10016350
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Collection (particular)
- 国立国会図書館デジタルコレクション > デジタル化資料 > 雑誌
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象
- Availability of remote photoduplication service
- 可
- Holding library
- 国立国会図書館
- Call No.
- Z17-136
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/2364989
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- Bibliographic ID (NDL)
- 10016366
- Bibliographic Record Category (NDL)
- 632
- Summary, etc.
- コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- DOI
- 10.1186/s40645-016-0088-3
- Access Restrictions
- インターネット公開
- Related Material
- Additional file 2: of Hydrogen and carbon isotope systematics in hydrogenotrophic methanogenesis under H2-limited and H2-enriched conditions: implications for the origin of methane and its isotopic diagnosisAdditional file 1: of Hydrogen and carbon isotope systematics in hydrogenotrophic methanogenesis under H2-limited and H2-enriched conditions: implications for the origin of methane and its isotopic diagnosis
- Related Material (URI)
- Is Referenced By
- Methane sources and sinks in continental sedimentary systems: New insights from paired clumped isotopologues 13CH3D and 12CH2D2Isolation of an archaeon at the prokaryote–eukaryote interfaceAbiotic Methane Generation via CO<sub>2</sub> Hydrogenation With Natural Chromitite Under Hydrothermal ConditionsCultivable microbial community in 2-km-deep, 20-million-year-old subseafloor coalbeds through ~1000 days anaerobic bioreactor cultivationEvaluation of nutrient and energy sources of the deepest known serpentinite-hosted ecosystem using stable carbon, nitrogen, and sulfur isotopesHadal water biogeochemistry over the Izu–Ogasawara Trench observed with a full-depth CTD-CMSDeepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama KnollClumped 13C–13C isotopologue signatures of thermogenic ethaneDeep Subseafloor Biogeochemical Processes and Microbial Populations Potentially Associated with the 2011 Tohoku-oki Earthquake at the Japan Trench Accretionary Wedge (IODP Expedition 343)
- References
- Isotopic variation of molecular hydrogen in 20°–375°C hydrothermal fluids as detected by a new analytical methodGeochemical origin of hydrothermal fluid methane in sediment-associated fields and its relevance to the geographical distribution of whole hydrothermal circulationExploring deep microbial life in coal-bearing sediment down to ~2.5 km below the ocean floorHydrogen isotope systematics among H2–H2O–CH4 during the growth of the hydrogenotrophic methanogen Methanothermobacter thermautotrophicus strain ΔHObservational, Experimental, and Theoretical Constraints on Carbon Cycling in Mid-Ocean Ridge Hydrothermal SystemsDistinguishing and understanding thermogenic and biogenic sources of methane using multiply substituted isotopologuesOngoing hydrothermal activities within EnceladusCarbon and hydrogen isotope systematics of bacterial formation and oxidation of methaneGeochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR)Carbon and hydrogen isotope fractionation by moderately thermophilic methanogens 1 1Associate editor: N. E. OstromHydrogen isotopic fractionation in lipid biosynthesis by H2-consuming Desulfobacterium autotrophicumPossible influence of hydrogen concentration on microbial methane stable hydrogen isotopic compositionMinimum Threshold for Hydrogen Metabolism in Methanogenic BacteriaVariation of carbon isotope fractionation in hydrogenotrophic methanogenic microbial cultures and environmental samples at different energy statusLaboratory Simulations of Abiotic Hydrocarbon Formation in Earth's Deep SubsurfaceUsing gas chromatography/isotope ratio mass spectrometry to determine the fractionation factor for H <sub>2</sub> production by hydrogenasesCarbon isotope exchange in the system CO2-CH4 at elevated temperaturesPost‐drilling changes in fluid discharge pattern, mineral deposition, and fluid chemistry in the Iheya North hydrothermal field, Okinawa TroughCell proliferation at 122°C and isotopically heavy CH <sub>4</sub> production by a hyperthermophilic methanogen under high-pressure cultivationThe hydrogen and carbon isotopic composition of methane from natural gases of various originsTransCom model simulations of CH <sub>4</sub> and related species: linking transport, surface flux and chemical loss with CH <sub>4</sub> variability in the troposphere and lower stratosphereThe global influence of the hydrogen isotope composition of water on that of bacteriogenic methane from shallow freshwater environmentsComplete genome sequence of Methanobacterium thermoautotrophicum deltaH: functional analysis and comparative genomicsOrigin of hydrogen in methane produced by Methanobacterium thermoautotrophicumLiquid-vapor fractionation of oxygen and hydrogen isotopes of water from the freezing to the critical temperatureMicrobial methane production in deep aquifer associated with the accretionary prism in Southwest JapanMeasurement of a Doubly Substituted Methane Isotopologue, <sup>13</sup>CH<sub>3</sub>D, by Tunable Infrared Laser Direct Absorption SpectroscopyTrace methane oxidation studied in several Euryarchaeota under diverse conditionsHydrogen and carbon isotope fractionation during experimental production of bacterial methaneThe stable isotopic signature of biologically produced molecular hydrogen (H <sub>2</sub> )Methanogenic archaea: ecologically relevant differences in energy conservationMathematical modeling of stable carbon isotope ratios in natural gasesLow temperature volatile production at the Lost City Hydrothermal Field, evidence from a hydrogen stable isotope geothermometerBiogenic methane formation in marine and freshwater environments: CO2 reduction vs. acetate fermentation—Isotope evidenceA theoretical calculation of the equilibrium constant for the isotopic exchange reaction between water and hydrogen deuterideHydrogen isotope exchange between n-alkanes and water under hydrothermal conditionsHydrogen isotopic composition of bacterial methane: CO2/H2 reduction and acetate fermentationfractionation in the system methane-hydrogen-waterNonequilibrium clumped isotope signals in microbial methaneMicrobial generation of economic accumulations of methane within a shallow organic-rich shaleMethanogenesis as a potential source of chemical energy for primary biomass production by autotrophic organisms in hydrothermal systems on EuropaMultiple origins of methane in the EarthAnaerobic Oxidation of Methane: Progress with an Unknown ProcessH/D exchange reactions and mechanistic aspects of the hydrogenasesSyntrophothermus lipocalidus gen. nov., sp. nov., a novel thermophilic, syntrophic, fatty-acid-oxidizing anaerobe which utilizes isobutyrate.Methanothermococcus okinawensis sp. nov., a thermophilic, methane-producing archaeon isolated from a Western Pacific deep-sea hydrothermal vent system.The carbon and hydrogen stable isotope composition of bacteriogenic methane: A laboratory study using a landfill inoculumHydrogen isotope fractionation by Methanothermobacter thermoautotrophicus in coculture and pure culture conditionsOrigin of methane in the Elk Valley coalfield, southeastern British Columbia, CanadaMethyl-Coenzyme M Reductase from Methanogenic Archaea: Isotope Effects on the Formation and Anaerobic Oxidation of MethaneFormation temperatures of thermogenic and biogenic methaneGeochemical and microbiological evidence for a hydrogen-based, hyperthermophilic subsurface lithoautotrophic microbial ecosystem (HyperSLiME) beneath an active deep-sea hydrothermal fieldMethane hydrate — A major reservoir of carbon in the shallow geosphere?Hydrogen and carbon isotope fractionation by thermophilic hydrogenotrophic methanogens from a deep aquifer under coculture with fermentersDiversity of fluid geochemistry affected by processes during fluid upwelling in active hydrothermal fields in the Izena Hole, the middle Okinawa Trough back-arc basinA High-precision Measurement System for Carbon and Hydrogen Isotopic Ratios of Atmospheric Methane and Its Application to Air Samples Collected in the Western Pacific RegionCultivation of methanogenic community from subseafloor sediments using a continuous-flow bioreactor
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10016366