How Earth's atmosphere evolved to an oxic state: A status report
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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).”
From Disequilibrium biosignatures over Earth history and implications for detecting exoplanet life (2018) · cites this paper as [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
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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