Atmospheric sulfur rearrangement 2.7 billion years ago: Evidence for oxygenic photosynthesis
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More recent studies suggest a more complex and dynamic evolution scenario for pO2.
“More recent studies, most of which were driven by the emergence of redox-sensitive trace element proxies, suggest a more complex and dynamic evolution scenario for pO2 (7–11).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [9]
The decrease in Δ33S values in the transitional interval was caused by an increase of pO2, which weakened the preservation of Δ33S signals from photochemistry through mixing different atmospheric sulfur pools, but this homogenization was incomplete.
“we suggest that the decrease in Δ33S values in the transitional interval was caused by an increase of pO2, which weakened the preservation of Δ33S signals from photochemistry through mixing different atmospheric sulfur pools; however, this homogenization was incomplete (9, 25).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [9]
The Δ36S/Δ33S slope of −0.9 is widespread in Neoarchean sedimentary rocks and interpreted to be of atmospheric origin.
“This is also supported by the Δ36S/Δ33S slope of −0.9, which is widespread in Neoarchean sedimentary rocks and interpreted to be of atmospheric origin (9, 25, 30, 43).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [9]
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- Authors
- Kurzweil, F., Claire, M., Thomazo, C., Peters, M., Hannington, M., & Strauss, H.
- Affiliations
- University of Münster (DE)
- University of East Anglia (GB)
- Centre National de la Recherche Scientifique (FR)
- Chinese Academy of Sciences (CN)
- University of Ottawa (CA)
- Corresponding author
- Kurzweil, Florian
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2013-03
- Volume
- 366
- Pages
- 17-26
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2005976476
- Cited by
- 91
- References
- 69
- Citations by year
- 2026: 4 · 2025: 7 · 2024: 5 · 2023: 3 · 2022: 6 · 2021: 6 · 2020: 5 · 2019: 1 · 2018: 12 · 2017: 7 · 2016: 11 · 2015: 13 · 2014: 5 · 2013: 5
- FWCI
- 7.70
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
- HAL (submittedVersion)
- Funders
- Deutsche Forschungsgemeinschaft (Str 281/30-1)
- 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 › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- oxygenic photosynthesis, Great Oxidation Event, Archean atmosphere, atmospheric oxygen, methane, Neoarchean, sulfur isotope fractionation, primary productivity
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