Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 ℃ and 500 bar
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- 資料種別
- 記事
- 著者・編者
- Takazo ShibuyaMotoko YoshizakiMasahiko Sato
- 出版年月日等
- 2015-12-21
- 出版年（W3CDTF）
- 2015-12-21
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 2(46)
- 掲載巻
- 2(46)
- 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/s40645-015-0076-z
- 国立国会図書館永続的識別子
- info:ndljp/pid/10016349
- 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）
- 2016-01-20
- 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
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- 遠隔複写可否（NDL）
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- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/9381655
- 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
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- 遠隔複写可否（NDL）
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- 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/2364984
- 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）
- 10016349
- 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/s40645-015-0076-z
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報
- Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300°C and 500bar
- 関連情報（URI）
- 参照
- Reactions between olivine and CO2-rich seawater at 300 °C: Implications for H2 generation and CO2 sequestration on the early EarthConstraints on the Source of the Martian Magnetic Anomalies Inferred From Relaxation Time of Remanent MagnetizationUnique H2-utilizing lithotrophy in serpentinite-hosted systemsExperimental Hydrothermal Alteration of Rhyolite and Andesite at 325 °C and 300 Bar: Implications for a Potential Role of Volcanic Glass in the Fluid Composition in the Okinawa TroughSimulating Serpentinization as It Could Apply to the Emergence of Life Using the JPL Hydrothermal ReactorComposition of the Primordial Ocean Just after Its Formation: Constraints from the Reactions between the Primitive Crust and a Strongly Acidic, CO2-Rich Fluid at Elevated Temperatures and PressuresFluid chemistry in the Solitaire and Dodo hydrothermal fields of the Central Indian RidgeBoron-assisted abiotic polypeptide synthesisEnceladus: Evidence and Unsolved Questions for an Ice-Covered Habitable WorldDeepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama KnollMetals likely promoted protometabolism in early ocean alkaline hydrothermal systemsUnique metabolic strategies in Hadean analogues reveal hints for primordial physiologyThe role of hydrothermal sulfate reduction in the sulfur cycles within Europa: Laboratory experiments on sulfate reduction at 100 MPaStable Abiotic Production of Ammonia from Nitrate in Komatiite-Hosted Hydrothermal Systems in the Hadean and Archean OceansChemical Nature of Hydrothermal Fluids Generated by Serpentinization and Carbonation of Komatiite: Implications for H<sub>2</sub>‐Rich Hydrothermal System and Ocean Chemistry in the Early EarthSupercritical carbon dioxide likely served as a prebiotic source of methanethiol in primordial ocean hydrothermal systemsExperimental and Simulation Efforts in the Astrobiological Exploration of ExooceansCharacteristics of hydrogen production with carbon storage by CO2-rich hydrothermal alteration of olivine in the presence of Mg–Al spinelPeptide Synthesis under the Alkaline Hydrothermal Conditions on Enceladus初期地球の蛇紋岩熱水系冥王代の「生きた微化石」OD1と超還元場の歴史Reactions between komatiite and CO2-rich seawater at 250 and 350 °C, 500 bars : implications for hydrogen generation in the Hadean seafloor hydrothermal systemLiquid and supercritical CO2 as an organic solvent in Hadean seafoor hydrothermal systems : implications for prebiotic chemical evolutionWeak hydrothermal carbonation of the Ongeluk volcanics : evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation
- 参照
- Geological background of the Kairei and Edmond hydrothermal vent fields along the Central Indian Ridge: Insights into the distinct chemistry between their vent fluidsDepth variation of carbon and oxygen isotopes of calcites in Archean altered upperoceanic crust: Implications for the CO2 flux from ocean to oceanic crust in the ArcheanVanadium partitioning between orthopyroxene, spinel and silicate melt and the redox states of mantle source regions for primary magmasAbiogenic methanogenesis during experimental komatiite serpentinization: Implications for the evolution of the early Precambrian atmosphereThermal evolution of the Earth as recorded by komatiitesRedox evolution and mass transfer during serpentinization: An experimental and theoretical study at 200°C, 500bar with implications for ultramafic-hosted hydrothermal systems at Mid-Ocean RidgesThermodynamic constraints on hydrogen generation during serpentinization of ultramafic rocksOngoing hydrothermal activities within EnceladusHighly alkaline, high-temperature hydrothermal fluids in the early Archean oceanGeochemical controls on hydrothermal fluids from the Kairei and Edmond Vent Fields, 23°–25°S, Central Indian RidgeGeochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR)KomatiiteWere komatiites wet?Pre–1 Ga (pre-Rodinian) ophiolites: Their tectonic and environmental implicationsMagnetic Properties of Rocks and MineralsHigh-temperature water–rock interactions and hydrothermal environments in the chondrite-like core of EnceladusA Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal FieldConstraints on deformation conditions and the origin of oceanic detachments: The Mid‐Atlantic Ridge core complex at 15°45′NSerpentinized troctolites exposed near the Kairei Hydrothermal Field, Central Indian Ridge: Insights into the origin of the Kairei hydrothermal fluid supporting a unique microbial ecosystemAn off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30° NDiffuse flow hydrothermal fluids from 9° 50′ N East Pacific Rise: Origin, evolution and biogeochemical controlsThermal history of the Earth and its petrological expressionDepth and degree of melting of komatiitesThe Drive to Life on Wet and Icy WorldsHigh Pressure Melting of Pyrolite Under Hydrous Condition and its Geophysical ImplicationsThe influence of carbon source on abiotic organic synthesis and carbon isotope fractionation under hydrothermal conditionsDistinguishing ultramafic‐from basalt‐hosted submarine hydrothermal systems by comparing calculated vent fluid compositionsElevated concentrations of formate, acetate and dissolved organic carbon found at the Lost City hydrothermal fieldControls on the Chemistry and Temporal Variability of Seafloor Hydrothermal FluidsLow temperature volatile production at the Lost City Hydrothermal Field, evidence from a hydrogen stable isotope geothermometerMaterial circulation model including chemical differentiation within the mantle and secular variation of temperature and composition of the mantleOxidation state of iron in komatiitic melt inclusions indicates hot Archaean mantleGarnet fractionation in a hydrous magma ocean and the origin of Al-depleted komatiites: melting experiments of hydrous pyrolite with REEs at high pressureGenesis of Archean komatiites from Munro Township, Ontario: Trace-element evidenceVanadium partitioning and the oxidation state of Archaean komatiite magmasReactions between basalt and CO2-rich seawater at 250 and 350 °C, 500 bars: Implications for the CO2 sequestration into the modern oceanic crust and the composition of hydrothermal vent fluid in the CO2-rich early oceanTemperature and salinity history of the Precambrian ocean: implications for the course of microbial evolutionMelting of peridotite to 14 GPa and the genesis of komatiiteField occurrence, geochemistry and petrogenesis of the Archean Mid-Oceanic Ridge Basalts (AMORBs) of the Cleaverville area, Pilbara Craton, Western AustraliaSerpentinite and the dawn of lifeReduced Gases and Bacteria in Hydrothermal Fluids: The Galapagos Spreading Center and 21°N East Pacific RiseHydrothermal vents and the origin of lifeCompared geochemical signatures and the evolution of Menez Gwen (37°50′N) and Lucky Strike (37°17′N) hydrothermal fluids, south of the Azores Triple Junction on the Mid-Atlantic RidgeCatabolic and anabolic energy for chemolithoautotrophs in deep-sea hydrothermal systems hosted in different rock typesHydrothermal serpentinization of peridotite within the oceanic crust: Experimental investigations of mineralogy and major element chemistryMagmatic events can produce rapid changes in hydrothermal vent chemistry<i>In vitro</i> growth of iron sulphide chimneys: possible culture chambers for origin‐of‐life experimentsMelting in an Archaean mantle plume: heads it's basalts, tails it's komatiitesSerpentinization as a source of energy at the origin of lifeMineral and gas chemistry of hydrothermal fluids on an ultrafast spreading ridge: East Pacific Rise, 17° to 19°S (Naudur cruise, 1993) phase separation processes controlled by volcanic and tectonic activityPhase relations of aluminum‐undepleted and aluminum‐depleted komatiites at pressures of 4–12 GPaInsights into early Earth from Barberton komatiites: Evidence from lithophile isotope and trace element systematicsGases and helium isotopes in high temperature solutions sampled before and after ODP Leg 158 drilling at TAG Hydrothermal Field (26°N, MAR)Experimental and Theoretical Constraints on Hydrothermal Alteration Processes at Mid-Ocean RidgesCr-spinel, an excellent micro-container for retaining primitive melts – implications for a hydrous plume origin for komatiitesCompositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 barsMiddle Archean ocean ridge hydrothermal metamorphism and alteration recorded in the Cleaverville area, Pilbara Craton, Western AustraliaMagnetic properties of the magnetite-spinel solid solution; Curie temperatures, magnetic susceptibilities, and cation orderingUltramafics–Hydrothermalism–Hydrogenesis–HyperSLiME (UltraH3) linkage: a key insight into early microbial ecosystem in the Archean deep-sea hydrothermal systemsH2 generation by experimental hydrothermal alteration of komatiitic glass at 300°C and 500 bars: A preliminary result from on-going experimentElemental dissolution of basalts with ultra-pure water at 340°C and 40 Mpa in a newly developed flow-type hydrothermal apparatusTheoretical constraints of physical and chemical properties of hydrothermal fluids on variations in chemolithotrophic microbial communities in seafloor hydrothermal systems
- 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学術機関リポジトリデータベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 10016349