Reactions between komatiite and CO2-rich seawater at 250 and 350 °C, 500 bars : implications for hydrogen generation in the Hadean seafloor hydrothermal system
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- 資料種別
- 記事
- 著者・編者
- Hisahiro UedaTakazo ShibuyaYusuke Sawaki
- 出版年月日等
- 2016-11-18
- 出版年（W3CDTF）
- 2016-11-18
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 3(35)
- 掲載巻
- 3(35)
- 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/s40645-016-0111-8
- 国立国会図書館永続的識別子
- info:ndljp/pid/10265318
- 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）
- 2017-01-19T19:10:18+09:00
- 保存日（W3CDTF）
- 2017-01-18
- 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
- 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/s40645-016-0111-8
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報
- Reactions between komatiite and CO2-rich seawater at 250 and 350°C, 500 bars: implications for hydrogen generation in the Hadean seafloor hydrothermal system
- 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 EarthAbiotic Methane Generation via CO<sub>2</sub> Hydrogenation With Natural Chromitite Under Hydrothermal ConditionsExperimental 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 TroughGeoelectrochemical CO production: Implications for the autotrophic origin of lifeSimulating 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 PressuresCharacterization of groundwater chemistry beneath Gale Crater on early Mars by hydrothermal experimentsExtreme accumulation of ammonia on electroreduced mackinawite: An abiotic ammonia storage mechanism in early ocean hydrothermal systemsEnceladus: Evidence and Unsolved Questions for an Ice-Covered Habitable WorldStable 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 EarthClumped 13C–13C isotopologue signatures of thermogenic ethaneSupercritical carbon dioxide likely served as a prebiotic source of methanethiol in primordial ocean hydrothermal systemsExperimental and Simulation Efforts in the Astrobiological Exploration of ExooceansRemoval of organic contaminants from iron sulfides as a pretreatment for mineral-mediated chemical synthesis under prebiotic hydrothermal conditions冥王代の「生きた微化石」OD1と超還元場の歴史Weak 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 ArcheanDecrease of seawater CO2 concentration in the Late Archean: An implication from 2.6 Ga seafloor hydrothermal alterationAbiogenic methanogenesis during experimental komatiite serpentinization: Implications for the evolution of the early Precambrian atmosphereGeochemistry of some ultramafic komatiite lava flows from the Barberton Mountain Land, South AfricaInorganic species in geologic fluids: Correlations among standard molal thermodynamic properties of aqueous ions and hydroxide complexesRedox 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 RidgesSubseafloor Processes in Mid-Ocean Ridge Hydrothennal SystemsHydrothermal and oceanic pH conditions of possible relevance to the origin of lifeThermodynamic constraints on hydrogen generation during serpentinization of ultramafic rocksEvidence from massive siderite beds for a CO2-rich atmosphere before ~ 1.8 billion years agoFree energy distribution and hydrothermal mineral precipitation in Hadean submarine alkaline vent systems: Importance of iron redox reactions under anoxic conditionsHighly alkaline, high-temperature hydrothermal fluids in the early Archean oceanCalculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Correlation algorithms for ionic species and equation of state predictions to 5 kb and 1000°CGeochemical 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)Pre–1 Ga (pre-Rodinian) ophiolites: Their tectonic and environmental implicationsCrystal chemistry, and thermodynamic and kinetic properties of calcite, dolomite, apatite, and biogenic silica: applications to petrologic problemsSUPCRT92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5000 bar and 0 to 1000°CA Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal FieldThermodynamics of hydrothermal systems at elevated temperatures and pressuresGeochemical and Biogeochemical Reaction ModelingDirect Nanoscale Observations of CO<sub>2</sub> Sequestration during Brucite [Mg(OH)<sub>2</sub>] DissolutionSerpentinized troctolites exposed near the Kairei Hydrothermal Field, Central Indian Ridge: Insights into the origin of the Kairei hydrothermal fluid supporting a unique microbial ecosystemPetrology and Geochemistry of MORB and OIB in the Mid-Archean North Pole Region, Pilbara Craton, Western Australia: Implications for the Composition and Temperature of the Upper Mantle at 3.5 GaGeologic evidence for Archean atmospheric and climatic evolution: Fluctuating levels of CO2, CH4, and O2 with an overriding tectonic controlMetal-organic complexes in geochemical processes: Estimation of standard partial molal thermodynamic properties of aqueous complexes between metal cations and monovalent organic acid ligands at high pressures and temperaturesThe Drive to Life on Wet and Icy WorldsThermophilic Microspheres of Peptide-Like Polymers and Silicates Formed at 250°CPervasive magnesium loss by marine weathering of peridotiteTheoretical prediction of the thermodynamic behavior of aqueous electrolytes at high pressures and temperatures; II, Debye-Huckel parameters for activity coefficients and relative partial molal propertiesDistinguishing ultramafic‐from basalt‐hosted submarine hydrothermal systems by comparing calculated vent fluid compositionsEarth's Early AtmosphereCompositional controls on hydrogen generation during serpentinization of ultramafic rocksGeochemical constraints on chemolithoautotrophic metabolism by microorganisms in seafloor hydrothermal systemsAqueous Carbonation of Natural Brucite: Relevance to CO<sub>2</sub> SequestrationOlivine alteration and H2 production in carbonate-rich, low temperature aqueous environmentsMaterial circulation model including chemical differentiation within the mantle and secular variation of temperature and composition of the mantleCrystal radii and effective ionic radii of the rare earth ionsVanadium partitioning and the oxidation state of Archaean komatiite magmasPhase equilibria constraints on the chemistry of hot spring fluids at mid-ocean ridgesReactions 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 oceanCalculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Standard partial molal properties of inorganic neutral speciesTemperature and salinity history of the Precambrian ocean: implications for the course of microbial evolutionCarbon dioxide on the early earthHydrothermal Fe fluxes during the Precambrian: Effect of low oceanic sulfate concentrations and low hydrostatic pressure on the composition of black smokersCalcite-Dolomite-Magnesite Stability Relations in Solutions at Elevated TemperaturesHexagonal plate-like magnetite nanocrystals produced in komatiite–H<sub>2</sub>O–CO<sub>2</sub>reaction system at 450°CMagnetite in seafloor serpentinite--Some like it hotField occurrence, geochemistry and petrogenesis of the Archean Mid-Oceanic Ridge Basalts (AMORBs) of the Cleaverville area, Pilbara Craton, Western AustraliaHydrothermal 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 RidgeFrom serpentinization to carbonation: New insights from a CO2 injection experimentPrediction of the thermodynamic properties of aqueous metal complexes to 1000°C and 5 kbK2GWB: Utility for generating thermodynamic data files for The Geochemist's Workbench® at 0–1000°C and 1–5000bar from UT2K and the UNITHERM databaseSerpentinization as a source of energy at the origin of lifeThe emergence of life from iron monosulphide bubbles at a submarine hydrothermal redox and pH frontCarbon dioxide cycling and implications for climate on ancient EarthGeochemical and microbiological evidence for a hydrogen-based, hyperthermophilic subsurface lithoautotrophic microbial ecosystem (HyperSLiME) beneath an active deep-sea hydrothermal fieldPhase relations of aluminum‐undepleted and aluminum‐depleted komatiites at pressures of 4–12 GPaGases and helium isotopes in high temperature solutions sampled before and after ODP Leg 158 drilling at TAG Hydrothermal Field (26°N, MAR)Compositional 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 AustraliaCalcite-dolomite-magnesite stability relations in solutions: the effect of ionic strengthUltramafics–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 experimentHydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 ℃ and 500 barPreface to the first volume of PEPS
- 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学術機関リポジトリデータベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 10265318