Weak hydrothermal carbonation of the Ongeluk volcanics : evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation

• 資料種別: 記事
• タイトル: Weak hydrothermal carbonation of the Ongeluk volcanics : evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation
• 著者・編者: Takazo Shibuya; Tsuyoshi Komiya; Ken Takai
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2017-10-23
• 出版年（W3CDTF）: 2017-10-23
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 4(31)
• 掲載巻: 4(31)
• 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/s40645-017-0145-6; https://doi.org/10.1186/s40645-017-0145-6
• 国立国会図書館永続的識別子: info:ndljp/pid/10980298; https://dl.ndl.go.jp/pid/10980298
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• コレクション（障害者向け資料：レベル1）: テキストデータ
• 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; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2017-10-30T20:11:03+09:00
• 保存日（W3CDTF）: 2017-10-27
• 記録形式（IMT）: application/pdf
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• 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（URI）: https://progearthplanetsci.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/10369577; https://dl.ndl.go.jp/pid/10369577
• 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; https://dl.ndl.go.jp

• 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/s40645-017-0145-6; https://doi.org/10.1186/s40645-017-0145-6
• オンライン閲覧公開範囲: インターネット公開
• 関連情報: Weak hydrothermal carbonation of the Ongeluk volcanics: evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation; https://cir.nii.ac.jp/crid/2120870839449507456
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/10980298; https://dl.ndl.go.jp/pid/10980298; http://link.springer.com/content/pdf/10.1186/s40645-017-0145-6.pdf; http://link.springer.com/article/10.1186/s40645-017-0145-6/fulltext.html
• 参照: Composition 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 Pressures; https://cir.nii.ac.jp/crid/1360290617759212288; The use of combined C Mg isotope compositions of carbonates from orogenic Sb Au deposits as a tracer of fluid interaction with sea-floor altered crust; https://cir.nii.ac.jp/crid/1360306906068791936; Ar–Ar dating for hydrothermal quartz from the 2.4 Ga Ongeluk Formation, South Africa: implications for seafloor hydrothermal circulation; https://cir.nii.ac.jp/crid/1360848659848762624; Liquid and supercritical CO2 as an organic solvent in Hadean seafoor hydrothermal systems : implications for prebiotic chemical evolution; https://cir.nii.ac.jp/crid/2050307417136231424
• 参照: Hydrothermal carbonate chimneys from a continental rift (Afar Rift): Mineralogy, geochemistry, and mode of formation; https://cir.nii.ac.jp/crid/1360002215857649408; Depth 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 Archean; https://cir.nii.ac.jp/crid/1360004232135238656; Estimates of atmospheric CO2 in the Neoarchean–Paleoproterozoic from paleosols; https://cir.nii.ac.jp/crid/1360004232166640640; The uptake of carbon during alteration of ocean crust; https://cir.nii.ac.jp/crid/1360011142940211968; Decrease of seawater CO2 concentration in the Late Archean: An implication from 2.6 Ga seafloor hydrothermal alteration; https://cir.nii.ac.jp/crid/1360011143500032512; Origin and mechanisms of K–Si-metasomatism of ca. 3.4–3.3Ga volcaniclastic deposits and implications for Archean seawater evolution: Examples from cherts of Kittys Gap (Pilbara craton, Australia) and Msauli (Barberton Greenstone Belt, South Africa); https://cir.nii.ac.jp/crid/1360011143582272768; Timing and tempo of the Great Oxidation Event; https://cir.nii.ac.jp/crid/1360011145602865664; Hydrothermal and oceanic pH conditions of possible relevance to the origin of life; https://cir.nii.ac.jp/crid/1360011146087824640; Evidence from massive siderite beds for a CO2-rich atmosphere before ~ 1.8 billion years ago; https://cir.nii.ac.jp/crid/1360011146206795648; Low-latitude glaciation in the Palaeoproterozoic era; https://cir.nii.ac.jp/crid/1360011146305192576; Free energy distribution and hydrothermal mineral precipitation in Hadean submarine alkaline vent systems: Importance of iron redox reactions under anoxic conditions; https://cir.nii.ac.jp/crid/1360283690913939200; Highly alkaline, high-temperature hydrothermal fluids in the early Archean ocean; https://cir.nii.ac.jp/crid/1360285707432905728; PIXE and microthermometric analyses of fluid inclusions in hydrothermal quartz from the 2.2Ga Ongeluk Formation, South Africa: Implications for ancient seawater salinity; https://cir.nii.ac.jp/crid/1360285707433013120; Evidence and implications for a widespread magmatic shutdown for 250 My on Earth; https://cir.nii.ac.jp/crid/1360292620789795968; Phosphate oxygen isotopic evidence for a temperate and biologically active Archaean ocean; https://cir.nii.ac.jp/crid/1360574094032728320; Precambrian paleosols and atmospheric CO2 levels; https://cir.nii.ac.jp/crid/1360574094758426368; Pb, O, and C isotopes in silicified Mooidraai dolomite (Transvaal Supergroup, South Africa): implications for the composition of Paleoproterozoic seawater and ‘dating’ the increase of oxygen in the Precambrian atmosphere; https://cir.nii.ac.jp/crid/1360574094822606464; Paleoproterozoic snowball Earth: Extreme climatic and geochemical global change and its biological consequences; https://cir.nii.ac.jp/crid/1360574094835951744; Transition to an oxygen-rich atmosphere with an extensive overshoot triggered by the Paleoproterozoic snowball Earth; https://cir.nii.ac.jp/crid/1360848657065539584; Progressive metamorphism of the Taitao ophiolite; evidence for axial and off-axis hydrothermal alterations; https://cir.nii.ac.jp/crid/1360855568912341120; Geologic evidence for Archean atmospheric and climatic evolution: Fluctuating levels of CO2, CH4, and O2 with an overriding tectonic control; https://cir.nii.ac.jp/crid/1360855569634869248; The geology and geochemistry of the Palaeoproterozoic Makganyene diamictite; https://cir.nii.ac.jp/crid/1360855569883230848; Geological sulfur isotopes indicate elevated OCS in the Archean atmosphere, solving faint young sun paradox; https://cir.nii.ac.jp/crid/1360855569886058880; Oxygen Isotope Fractionation in Divalent Metal Carbonates; https://cir.nii.ac.jp/crid/1360855570149312128; Carbonatization of oceanic crust by the seafloor hydrothermal activity and its significance as a CO2 sink in the Early Archean; https://cir.nii.ac.jp/crid/1361137044064791808; The Drive to Life on Wet and Icy Worlds; https://cir.nii.ac.jp/crid/1361137044158073088; Seafloor hydrothermal alteration at an Archaean mid‐ocean ridge; https://cir.nii.ac.jp/crid/1361137045004651776; Theoretical constraints on oxygen and carbon dioxide concentrations in the Precambrian atmosphere; https://cir.nii.ac.jp/crid/1361137045310374016; Oxygen isotope composition of the oceanic crust and its bearing on seawater; https://cir.nii.ac.jp/crid/1361418518627274368; Multiple causes of Earth's earliest global glaciation; https://cir.nii.ac.jp/crid/1361418518955069824; Water-rock interaction between basalt and high-salinity fluids in the Asal Rift, Republic of Djibouti; https://cir.nii.ac.jp/crid/1361418519577275520; The Ongeluk basaltic andesite formation in Griqualand West, South Africa: submarine alteration in a 2222 Ma proterozoic sea; https://cir.nii.ac.jp/crid/1361418520729492864; Earth's Early Atmosphere; https://cir.nii.ac.jp/crid/1361418521124425344; Seafloor weathering controls on atmospheric CO2 and global climate; https://cir.nii.ac.jp/crid/1361699994485955968; GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic time; https://cir.nii.ac.jp/crid/1361699995004844288; Methane-rich Proterozoic atmosphere?; https://cir.nii.ac.jp/crid/1361699995113355904; Precambrian supercontinents, glaciations, atmospheric oxygenation, metazoan evolution and an impact that may have changed the second half of Earth history; https://cir.nii.ac.jp/crid/1361699995744988288; Ancient sub-seafloor alteration of basaltic andesites of the Ongeluk Formation, South Africa: implications for the chemistry of Paleoproterozoic seawater; https://cir.nii.ac.jp/crid/1361981468750221440; Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256; https://cir.nii.ac.jp/crid/1362262945355529216; Reactions 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 ocean; https://cir.nii.ac.jp/crid/1362262945619005312; A lower limit for atmospheric carbon dioxide levels 3.2 billion years ago; https://cir.nii.ac.jp/crid/1362262945739074048; Warm Archaean oceans reconstructed from oxygen isotope composition of early-life remnants; https://cir.nii.ac.jp/crid/1362262946168591104; Archean ocean-floor metamorphism in the North Pole area, Pilbara Craton, Western Australia; https://cir.nii.ac.jp/crid/1362544418911614720; Solar interior structure and luminosity variations; https://cir.nii.ac.jp/crid/1362544419944281600; Distribution of alteration zones in the upper oceanic crust; https://cir.nii.ac.jp/crid/1362544420242662400; Earth and Mars: Evolution of Atmospheres and Surface Temperatures; https://cir.nii.ac.jp/crid/1362544420842780544; Formation of jasper and andradite during low-temperature hydrothermal seafloor metamorphism, Ongeluk Formation, South Africa; https://cir.nii.ac.jp/crid/1363107368715119872; δ ¹³ C and δ ¹⁸ O isotopic composition of CaCO ₃ measured by continuous flow isotope ratio mass spectrometry: statistical evaluation and verification by application to Devils Hole core DH‐11 calcite; https://cir.nii.ac.jp/crid/1363107369381405824; High Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South Africa; https://cir.nii.ac.jp/crid/1363107370462720000; The Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis; https://cir.nii.ac.jp/crid/1363107371363410816; Silica alteration zones in the Barberton greenstone belt: A window into subseafloor processes 3.5–3.3 Ga ago; https://cir.nii.ac.jp/crid/1363388844467860864; Secular variation in carbon uptake into the ocean crust; https://cir.nii.ac.jp/crid/1363388844604489856; Paleoclimates, ocean depth, and the oxygen isotopic composition of seawater; https://cir.nii.ac.jp/crid/1363388846067501568; Serpentinization as a source of energy at the origin of life; https://cir.nii.ac.jp/crid/1363388846336194304; The ¹⁸ O/ ¹⁶ O Ratio of 2-Billion-Year-Old Seawater Inferred from Ancient Oceanic Crust; https://cir.nii.ac.jp/crid/1363670318869862144; No climate paradox under the faint early Sun; https://cir.nii.ac.jp/crid/1363670319553636096; Carbon dioxide cycling and implications for climate on ancient Earth; https://cir.nii.ac.jp/crid/1363670320407814528; Linking basement carbonate vein compositions to porewater geochemistry across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168; https://cir.nii.ac.jp/crid/1363951794440306688; A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts; https://cir.nii.ac.jp/crid/1363951796219705472; Decoupling photochemical Fe(II) oxidation from shallow-water BIF deposition; https://cir.nii.ac.jp/crid/1364233268545774208; The Great Oxidation and a Siderian snowball Earth: MIF-S based correlation of Paleoproterozoic glacial epochs; https://cir.nii.ac.jp/crid/1364233268890398848; Middle Archean ocean ridge hydrothermal metamorphism and alteration recorded in the Cleaverville area, Pilbara Craton, Western Australia; https://cir.nii.ac.jp/crid/1364233269460639744; A 400 million year carbon isotope record of pedogenic carbonate; implications for paleoatomospheric carbon dioxide; https://cir.nii.ac.jp/crid/1364233269990599936; Ultramafics–Hydrothermalism–Hydrogenesis–HyperSLiME (UltraH3) linkage: a key insight into early microbial ecosystem in the Archean deep-sea hydrothermal systems; https://cir.nii.ac.jp/crid/1390001204086725376; Reactions between komatiite and CO2-rich seawater at 250 and 350 °C, 500 bars : implications for hydrogen generation in the Hadean seafloor hydrothermal system; https://cir.nii.ac.jp/crid/2050025942005882880; Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 ℃ and 500 bar; https://cir.nii.ac.jp/crid/2051714791861480448
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja; 学術機関リポジトリデータベース; https://irdb.nii.ac.jp
• 書誌ID（NDLBibID）: 10980298; http://id.ndl.go.jp/bib/10980298