Cited by 376Paleontology and Stratigraphy of FossilsGeological and Geochemical AnalysisEarth Systems and Cosmic Evolution

How Earth's atmosphere evolved to an oxic state: A status report

Catling, David C., Claire, Mark W.·2005·Earth and Planetary Science Letters

Integrity signals

Registry

Crossref · 10.1016/j.epsl.2005.06.013

Cites

125 of 125 references verified0 citation errors · 0 not checkable

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  • These O2 levels would have only been attained when the O2 flux from the burial of organic carbon exceeded the kinetically efficient sink from O2-consuming gases from volcanism and metamorphism plus fluxes of reducing cations such as Fe2+ from seafloor vents.

    “These O2 levels would have only been attained when the O2 flux from the burial of organic carbon exceeded the kinetically efficient sink from O2-consuming gases (CO, H2, H2S, and SO2) from volcanism and metamorphism plus fluxes of reducing cations such as Fe2+ from seafloor vents (9, 120, 121, 123, 124).”

    From The Archean atmosphere (2020) · cites this paper as [120]

  • Because the early Earth atmosphere was non-oxidizing, the ocean would not have been oxidized and is believed to have contained high levels of reduced iron (Fe2+), which may have played a significant role in prebiotic redox reactions.

    “As the atmosphere on early Earth was non-oxidizing (Catling and Claire, 2005), the ocean would not have been oxidized, so it is believed to have contained high levels of the reduced form of iron (Fe2+), which may have played a significant role in prebiotic redox reactions.”

    From The Astrobiology Primer v2.0 (2016) · cites this paper as Catling and Claire, 2005

  • On the modern Earth, even if all the surface biomass (4.4 × 1017 Tmol C) were oxidized, only 1% of atmospheric oxygen would be depleted.

    “However, on the modern Earth, even if all the surface biomass (4.4 × 1017 Tmol C) were oxidized, only 1% of atmospheric oxygen would be depleted (69).”

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Authors
Catling, D. C., & Claire, M. W.
Affiliations
University of Washington (US)
Corresponding author
Catling, David C.
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2005-08
Volume
237
Issue
1-2
Pages
1-20
ISSN
0012-821X (ISSN-L)
OpenAlex
W2008608758
Cited by
376
References
129
Citations by year
2026: 7 · 2025: 5 · 2024: 10 · 2023: 24 · 2022: 13 · 2021: 17 · 2020: 21 · 2019: 16 · 2018: 25 · 2017: 27 · 2016: 13 · 2015: 30 · 2014: 12 · 2013: 21 · 2012: 21
FWCI
19.27
Type
journal article
Language
en
Open access
closed
Locations
  • Earth and Planetary Science Letters (publishedVersion)
  • Bristol Research (University of Bristol) (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Earth Systems and Cosmic Evolution
Keywords
atmospheric oxygenation, Great Oxidation, Snowball Earth, methane, greenhouse gases, carbon cycle, oxygenic photosynthesis, early atmosphere, Precambrian

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