Weak hydrothermal carbonation of the Ongeluk volcanics : evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation
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- Material Type
- 記事
- Author/Editor
- Takazo ShibuyaTsuyoshi KomiyaKen Takai
- Publication, Distribution, etc.
- Publication Date
- 2017-10-23
- Publication Date (W3CDTF)
- 2017-10-23
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 4(31)
- Volume
- 4(31)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-017-0145-6
- Persistent ID (NDL)
- info:ndljp/pid/10980298
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2017-10-30T20:11:03+09:00
- Date Captured (W3CDTF)
- 2017-10-27
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/10369577
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- 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
- Access Restrictions
- インターネット公開
- Related Material
- Weak hydrothermal carbonation of the Ongeluk volcanics: evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation
- Related Material (URI)
- Is Referenced By
- 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 PressuresThe use of combined C Mg isotope compositions of carbonates from orogenic Sb Au deposits as a tracer of fluid interaction with sea-floor altered crustAr–Ar dating for hydrothermal quartz from the 2.4 Ga Ongeluk Formation, South Africa: implications for seafloor hydrothermal circulationLiquid and supercritical CO2 as an organic solvent in Hadean seafoor hydrothermal systems : implications for prebiotic chemical evolution
- References
- Hydrothermal carbonate chimneys from a continental rift (Afar Rift): Mineralogy, geochemistry, and mode of formationDepth 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 ArcheanEstimates of atmospheric CO2 in the Neoarchean–Paleoproterozoic from paleosolsThe uptake of carbon during alteration of ocean crustDecrease of seawater CO2 concentration in the Late Archean: An implication from 2.6 Ga seafloor hydrothermal alterationOrigin 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)Timing and tempo of the Great Oxidation EventHydrothermal and oceanic pH conditions of possible relevance to the origin of lifeEvidence from massive siderite beds for a CO2-rich atmosphere before ~ 1.8 billion years agoLow-latitude glaciation in the Palaeoproterozoic eraFree 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 oceanPIXE and microthermometric analyses of fluid inclusions in hydrothermal quartz from the 2.2Ga Ongeluk Formation, South Africa: Implications for ancient seawater salinityEvidence and implications for a widespread magmatic shutdown for 250 My on EarthPhosphate oxygen isotopic evidence for a temperate and biologically active Archaean oceanPrecambrian paleosols and atmospheric CO2 levelsPb, 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 atmospherePaleoproterozoic snowball Earth: Extreme climatic and geochemical global change and its biological consequencesTransition to an oxygen-rich atmosphere with an extensive overshoot triggered by the Paleoproterozoic snowball EarthProgressive metamorphism of the Taitao ophiolite; evidence for axial and off-axis hydrothermal alterationsGeologic evidence for Archean atmospheric and climatic evolution: Fluctuating levels of CO2, CH4, and O2 with an overriding tectonic controlThe geology and geochemistry of the Palaeoproterozoic Makganyene diamictiteGeological sulfur isotopes indicate elevated OCS in the Archean atmosphere, solving faint young sun paradoxOxygen Isotope Fractionation in Divalent Metal CarbonatesCarbonatization of oceanic crust by the seafloor hydrothermal activity and its significance as a CO2 sink in the Early ArcheanThe Drive to Life on Wet and Icy WorldsSeafloor hydrothermal alteration at an Archaean mid‐ocean ridgeTheoretical constraints on oxygen and carbon dioxide concentrations in the Precambrian atmosphereOxygen isotope composition of the oceanic crust and its bearing on seawaterMultiple causes of Earth's earliest global glaciationWater-rock interaction between basalt and high-salinity fluids in the Asal Rift, Republic of DjiboutiThe Ongeluk basaltic andesite formation in Griqualand West, South Africa: submarine alteration in a 2222 Ma proterozoic seaEarth's Early AtmosphereSeafloor weathering controls on atmospheric CO2 and global climateGEOCARB III: A revised model of atmospheric CO2 over Phanerozoic timeMethane-rich Proterozoic atmosphere?Precambrian supercontinents, glaciations, atmospheric oxygenation, metazoan evolution and an impact that may have changed the second half of Earth historyAncient sub-seafloor alteration of basaltic andesites of the Ongeluk Formation, South Africa: implications for the chemistry of Paleoproterozoic seawaterSubsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256Reactions 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 oceanA lower limit for atmospheric carbon dioxide levels 3.2 billion years agoWarm Archaean oceans reconstructed from oxygen isotope composition of early-life remnantsArchean ocean-floor metamorphism in the North Pole area, Pilbara Craton, Western AustraliaSolar interior structure and luminosity variationsDistribution of alteration zones in the upper oceanic crustEarth and Mars: Evolution of Atmospheres and Surface TemperaturesFormation of jasper and andradite during low-temperature hydrothermal seafloor metamorphism, Ongeluk Formation, South Africaδ <sup>13</sup> C and δ <sup>18</sup> O isotopic composition of CaCO <sub>3</sub> measured by continuous flow isotope ratio mass spectrometry: statistical evaluation and verification by application to Devils Hole core DH‐11 calciteHigh Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South AfricaThe Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesisSilica alteration zones in the Barberton greenstone belt: A window into subseafloor processes 3.5–3.3 Ga agoSecular variation in carbon uptake into the ocean crustPaleoclimates, ocean depth, and the oxygen isotopic composition of seawaterSerpentinization as a source of energy at the origin of lifeThe <sup>18</sup> O/ <sup>16</sup> O Ratio of 2-Billion-Year-Old Seawater Inferred from Ancient Oceanic CrustNo climate paradox under the faint early SunCarbon dioxide cycling and implications for climate on ancient EarthLinking basement carbonate vein compositions to porewater geochemistry across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in chertsDecoupling photochemical Fe(II) oxidation from shallow-water BIF depositionThe Great Oxidation and a Siderian snowball Earth: MIF-S based correlation of Paleoproterozoic glacial epochsMiddle Archean ocean ridge hydrothermal metamorphism and alteration recorded in the Cleaverville area, Pilbara Craton, Western AustraliaA 400 million year carbon isotope record of pedogenic carbonate; implications for paleoatomospheric carbon dioxideUltramafics–Hydrothermalism–Hydrogenesis–HyperSLiME (UltraH3) linkage: a key insight into early microbial ecosystem in the Archean deep-sea hydrothermal systemsReactions between komatiite and CO2-rich seawater at 250 and 350 °C, 500 bars : implications for hydrogen generation in the Hadean seafloor hydrothermal systemHydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 ℃ and 500 bar
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 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CrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10980298