Atmospheric oxygenation of the early earth and earth-like planets driven by competition between land and seafloor weathering
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- 資料種別
- 記事
- 著者・編者
- Yasuto WatanabeEiichi Tajika
- 出版年月日等
- 2021-10-18
- 出版年（W3CDTF）
- 2021-10-18
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 73(188)
- 掲載巻
- 73(188)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-021-01527-9
- 国立国会図書館永続的識別子
- info:ndljp/pid/12287020
- 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）
- 2022-05-18T20:14:28+09:00
- 保存日（W3CDTF）
- 2022-04-27
- 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/11667897
- 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/s40623-021-01527-9
- 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 1 of Atmospheric oxygenation of the early earth and earth-like planets driven by competition between land and seafloor weathering
- 関連情報（URI）
- 参照
- Biogeochemical transformations after the emergence of oxygenic photosynthesis and conditions for the first rise of atmospheric oxygenEvolution of iron and oxygen biogeochemical cycles during the PrecambrianRelative Abundances of CO<sub>2</sub>, CO, and CH<sub>4</sub> in Atmospheres of Earth-like Lifeless PlanetsMechanistic links between intense volcanism and the transient oxygenation of the Archean atmosphereControls of Atmospheric Methane on Early Earth and Inhabited Earth-like Terrestrial Exoplanets
- 参照
- The rise of oxygen in Earth’s early ocean and atmosphereGlobal water cycle and the coevolution of the Earth’s interior and surface environmentBiogeochemical modelling of the rise in atmospheric oxygenBiomass recycling and Earth’s early phosphorus cycleOceanographic Considerations for Exoplanet Life DetectionThe oxygen content of ocean bottom waters, the burial efficiency of organic carbon, and the regulation of atmospheric oxygenPhotochemical modelling of atmospheric oxygen levels confirms two stable statesDetectability of Life Using Oxygen on Pelagic Planets and Water WorldsCycling phosphorus on the Archean Earth: Part I. Continental weathering and riverine transport of phosphorusAnoxygenic photosynthesis and the delayed oxygenation of Earth’s atmosphereEffects of primitive photosynthesis on Earth’s early climate systemThe HITRAN2012 molecular spectroscopic databaseGreat Oxidation and Lomagundi events linked by deep cycling and enhanced degassing of carbonEvolution of the continental crustConstraining climate sensitivity and continental versus seafloor weathering using an inverse geological carbon cycle modelThe evolution of the 87Sr/86Sr of marine carbonates does not constrain continental growthCarbonate-silicate cycle predictions of Earth-like planetary climates and testing the habitable zone conceptHigh Organic Burial Efficiency Is Required to Explain Mass Balance in Earth's Early Carbon CycleThe future lifespan of Earth’s oxygenated atmosphereAlteration of ocean crust provides a strong temperature dependent feedback on the geological carbon cycle and is a primary driver of the Sr-isotopic composition of seawaterPhosphate removal by oceanic hydrothermal processes: An update of the phosphorus budget in the oceansThe Oceanic Phosphorus CycleLinking the rise of atmospheric oxygen to growth in the continental phosphorus inventoryWaterworlds May Have Better Climate Buffering Capacities than Their Continental CounterpartsA small marine biosphere in the ProterozoicTwo-step rise of atmospheric oxygen linked to the growth of continentsTransition to an oxygen-rich atmosphere with an extensive overshoot triggered by the Paleoproterozoic snowball EarthPrimary Production of the Biosphere: Integrating Terrestrial and Oceanic ComponentsThe oxygenation of the atmosphere and oceansA bistable organic-rich atmosphere on the Neoarchaean EarthThe Great Oxygenation Event as a consequence of ecological dynamics modulated by planetary changeThe effect of widespread early aerobic marine ecosystems on methane cycling and the Great OxidationThe Archean atmosphereThe rise of atmospheric oxygenMantle data imply a decline of oxidizable volcanic gases could have triggered the Great OxidationAtmospheric oxygenation caused by a change in volcanic degassing pressureA Revised, Hazy Methane Greenhouse for the Archean EarthEvolution of the global phosphorus cycleBistability of atmospheric oxygen and the Great OxidationThe role of the vertical fluxes of particulate organic matter and calcite in the oceanic carbon cycle: Studies using an ocean biogeochemical general circulation modelWhat caused the rise of atmospheric O2?The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean EarthUV shielding of NH<sub>3</sub>and O<sub>2</sub>by organic hazes in the Archean atmosphereBiogenic Methane, Hydrogen Escape, and the Irreversible Oxidation of Early EarthA coupled atmosphere–ecosystem model of the early Archean EarthThe relative influences of nitrogen and phosphorus on oceanic primary productionChemical weathering of silicate rocks as a function of elevation in the southern Swiss AlpsSinks for Anthropogenic CarbonEarly anaerobic metabolismsGEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic timeA negative feedback mechanism for the long‐term stabilization of Earth's surface temperatureEarliest land plants created modern levels of atmospheric oxygenSedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years agoTectonic control of chemical and isotopic composition of ancient oceans; the impact of continental growthConstraining the climate and ocean pH of the early Earth with a geological carbon cycle modelBiological regulation of atmospheric chemistry en route to planetary oxygenationThe geochemical evolution of the continental crustCycling phosphorus on the Archean Earth: Part II. Phosphorus limitation on primary production in Archean ecosystemsExoplanet Biosignatures: Understanding Oxygen as a Biosignature in the Context of Its EnvironmentErosional and climatic effects on long-term chemical weathering rates in granitic landscapes spanning diverse climate regimes
- 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CrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 12287020