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
国立国会図書館館内限定公開
収録元データベースで確認する
国立国会図書館デジタルコレクション
デジタルデータあり
公開元のウェブサイトで確認する
DOI[10.1186/s40645-016-0088-3]のデータに遷移します
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
書誌情報
この資料の詳細や典拠（同じ主題の資料を指すキーワード、著者名）等を確認できます。
- 資料種別
- 記事
- 著者・編者
- Tomoyo OkumuraShinsuke KawagucciYayoi Saito
- 出版年月日等
- 2016-05-12
- 出版年（W3CDTF）
- 2016-05-12
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 3(14)
- 掲載巻
- 3(14)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-016-0088-3
- 国立国会図書館永続的識別子
- info:ndljp/pid/10016366
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 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
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2016-06-22T20:22:58+09:00
- 保存日（W3CDTF）
- 2016-06-21
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/10016350
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- コレクション（個別）
- 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
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象
- 遠隔複写可否（NDL）
- 可
- 所蔵機関
- 国立国会図書館
- 請求記号
- Z17-136
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/2364989
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- 書誌ID（NDLBibID）
- 10016366
- 整理区分コード
- 632
- 要約等
- 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
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報
- 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
- 関連情報（URI）
- 参照
- 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)
- 参照
- 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
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 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
- 書誌ID（NDLBibID）
- 10016366