Cited by 106Paleontology and Stratigraphy of FossilsGeology and Paleoclimatology ResearchGeological and Geochemical Analysis

Estimates of atmospheric CO2 in the Neoarchean–Paleoproterozoic from paleosols

Kanzaki, Yoshiki, Murakami, Takashi·2015·Geochimica et Cosmochimica Acta

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Crossref · 10.1016/j.gca.2015.03.011

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153 of 153 references verified0 citation errors · 0 not checkable

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  • Another study obtained higher pCO2 of 85 to 510 PAL at 2.77 Ga ago, 78 to 2500 PAL at 2.75 Ga ago, and 160 to 490 PAL at 2.46 Ga ago.

    “Another study used an analysis with an estimate of the composition of temperature-dependent aqueous solutions during weathering and, because of a weaker dependence of weathering on pCO2, obtained higher pCO2 of 85 to 510 PAL at 2.77 Ga ago, 78 to 2500 PAL at 2.75 Ga ago, and 160 to 490 PAL at 2.46 Ga ago (Fig. 3A) (43).”

    From The Archean atmosphere (2020) · cites this paper as [43]

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Authors
Kanzaki, Y., & Murakami, T.
Affiliations
The University of Tokyo (JP)
Corresponding author
Murakami, Takashi
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
2015-06
Volume
159
Pages
190-219
ISSN
0016-7037 (ISSN-L)
OpenAlex
W1974110352
Cited by
106
References
154
Citations by year
2026: 8 · 2025: 10 · 2024: 3 · 2023: 10 · 2022: 16 · 2021: 10 · 2020: 11 · 2019: 8 · 2018: 15 · 2017: 8 · 2016: 3 · 2015: 2
FWCI
7.08
Type
journal article
Language
en
Open access
closed
Locations
Geochimica et Cosmochimica Acta (publishedVersion)
Funders
Ministry of Education, Culture, Sports, Science and Technology (24340132)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Keywords
atmospheric CO2, paleosols, paleoweathering, pore water chemistry, cation concentration, partial pressure of CO2, weathering rates, Snowball Earth, faint young Sun, atmospheric oxygen, carbonate weathering, secondary minerals

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