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電子書籍・電子雑誌Progress in earth and planetary science
Volume number4
Weak hydro...

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

Call No. (NDL)
Z11-321
Bibliographic ID of National Diet Library
10980298
Persistent ID (NDL)
info:ndljp/pid/10980298
Material type
記事
Author
Takazo Shibuyaほか
Publisher
Springer Nature
Publication date
2017-10-23
Material Format
Paper・Digital
Journal name
Progress in earth and planetary science 4(31)
Publication Page
-
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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(Provided by: CiNii Research)

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Digital

Material Type
記事
Author/Editor
Takazo Shibuya
Tsuyoshi Komiya
Ken 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
Persistent ID (NDL)
info:ndljp/pid/10980298
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
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

Digital

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
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
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 Pressures
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
Ar–Ar dating for hydrothermal quartz from the 2.4 Ga Ongeluk Formation, South Africa: implications for seafloor hydrothermal circulation
Liquid 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 formation
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
Estimates of atmospheric CO2 in the Neoarchean–Paleoproterozoic from paleosols
The uptake of carbon during alteration of ocean crust
Decrease of seawater CO2 concentration in the Late Archean: An implication from 2.6 Ga seafloor hydrothermal alteration
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)
Timing and tempo of the Great Oxidation Event
Hydrothermal and oceanic pH conditions of possible relevance to the origin of life
Evidence from massive siderite beds for a CO2-rich atmosphere before ~ 1.8 billion years ago
Low-latitude glaciation in the Palaeoproterozoic era
Free energy distribution and hydrothermal mineral precipitation in Hadean submarine alkaline vent systems: Importance of iron redox reactions under anoxic conditions
Highly alkaline, high-temperature hydrothermal fluids in the early Archean ocean
PIXE and microthermometric analyses of fluid inclusions in hydrothermal quartz from the 2.2Ga Ongeluk Formation, South Africa: Implications for ancient seawater salinity
Evidence and implications for a widespread magmatic shutdown for 250 My on Earth
Phosphate oxygen isotopic evidence for a temperate and biologically active Archaean ocean
Precambrian paleosols and atmospheric CO2 levels
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
Paleoproterozoic snowball Earth: Extreme climatic and geochemical global change and its biological consequences
Transition to an oxygen-rich atmosphere with an extensive overshoot triggered by the Paleoproterozoic snowball Earth
Progressive metamorphism of the Taitao ophiolite; evidence for axial and off-axis hydrothermal alterations
Geologic evidence for Archean atmospheric and climatic evolution: Fluctuating levels of CO2, CH4, and O2 with an overriding tectonic control
The geology and geochemistry of the Palaeoproterozoic Makganyene diamictite
Geological sulfur isotopes indicate elevated OCS in the Archean atmosphere, solving faint young sun paradox
Oxygen Isotope Fractionation in Divalent Metal Carbonates
Carbonatization of oceanic crust by the seafloor hydrothermal activity and its significance as a CO2 sink in the Early Archean
The Drive to Life on Wet and Icy Worlds
Seafloor hydrothermal alteration at an Archaean mid‐ocean ridge
Theoretical constraints on oxygen and carbon dioxide concentrations in the Precambrian atmosphere
Oxygen isotope composition of the oceanic crust and its bearing on seawater
Multiple causes of Earth's earliest global glaciation
Water-rock interaction between basalt and high-salinity fluids in the Asal Rift, Republic of Djibouti
The Ongeluk basaltic andesite formation in Griqualand West, South Africa: submarine alteration in a 2222 Ma proterozoic sea
Earth's Early Atmosphere
Seafloor weathering controls on atmospheric CO2 and global climate
GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic time
Methane-rich Proterozoic atmosphere?
Precambrian supercontinents, glaciations, atmospheric oxygenation, metazoan evolution and an impact that may have changed the second half of Earth history
Ancient sub-seafloor alteration of basaltic andesites of the Ongeluk Formation, South Africa: implications for the chemistry of Paleoproterozoic seawater
Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256
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
A lower limit for atmospheric carbon dioxide levels 3.2 billion years ago
Warm Archaean oceans reconstructed from oxygen isotope composition of early-life remnants
Archean ocean-floor metamorphism in the North Pole area, Pilbara Craton, Western Australia
Solar interior structure and luminosity variations
Distribution of alteration zones in the upper oceanic crust
Earth and Mars: Evolution of Atmospheres and Surface Temperatures
Formation of jasper and andradite during low-temperature hydrothermal seafloor metamorphism, Ongeluk Formation, South Africa
δ <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 calcite
High Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South Africa
The Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis
Silica alteration zones in the Barberton greenstone belt: A window into subseafloor processes 3.5–3.3 Ga ago
Secular variation in carbon uptake into the ocean crust
Paleoclimates, ocean depth, and the oxygen isotopic composition of seawater
Serpentinization as a source of energy at the origin of life
The <sup>18</sup> O/ <sup>16</sup> O Ratio of 2-Billion-Year-Old Seawater Inferred from Ancient Oceanic Crust
No climate paradox under the faint early Sun
Carbon dioxide cycling and implications for climate on ancient Earth
Linking basement carbonate vein compositions to porewater geochemistry across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168
A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts
Decoupling photochemical Fe(II) oxidation from shallow-water BIF deposition
The Great Oxidation and a Siderian snowball Earth: MIF-S based correlation of Paleoproterozoic glacial epochs
Middle Archean ocean ridge hydrothermal metamorphism and alteration recorded in the Cleaverville area, Pilbara Craton, Western Australia
A 400 million year carbon isotope record of pedogenic carbonate; implications for paleoatomospheric carbon dioxide
Ultramafics–Hydrothermalism–Hydrogenesis–HyperSLiME (UltraH3) linkage: a key insight into early microbial ecosystem in the Archean deep-sea hydrothermal systems
Reactions between komatiite and CO2-rich seawater at 250 and 350 °C, 500 bars : implications for hydrogen generation in the Hadean seafloor hydrothermal system
Hydrogen-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
Bibliographic ID (NDL)
10980298