A redox-stratified ocean 3.2 billion years ago
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Satkoski et al. calculated shallow photic zone O2 contents at ~10 μM (between 10^-3 and 10^-2 POL) and deep-water O2 contents at ~0.4 μM.
“Based on modelling of Fe isotopes in the Manzimnyama jasper, Satkoski et al. (2015) calculated shallow photic zone O2 contents at ~10 µM (between 10 -3 and 10 -2 POL, or Present Ocean Level; Fig. 10), and deep-water O2 contents at ~0.4 µM.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Satkoski et al., 2015
Satkoski et al. used stable Fe and radiogenic U-Th-Pb isotope data from the 3.2 Ga Manzimnyama IF to demonstrate that proximal, shallow-water samples record precipitation under more oxic conditions compared to the distal, deeper-water facies, and that U enrichment in the shallow-water samples indicates the presence of free oxygen in the photic zone.
“Satkoski et al. (2015) used a combination of stable Fe and radiogenic UTh-Pb isotope data from the 3.2 Ga Manzimnyama IF of the Fig Tree Group, South Africa to demonstrate that proximal, shallow-water samples record precipitation under more oxic conditions compared to the distal, deeper-water facies, and that the presence of U enrichment in the shallowwater samples indicates the”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Satkoski et al., 2015
Estimates of maximum O2 contents in shallow oceans potentially provide evidence that the shallow oceans had significant free O2 levels by 3.2 Ga, hundreds of millions of years prior to the rise in atmospheric O2.
“potentially provide evidence that the shallow oceans had significant free O2 levels by 3.2 Ga, hundreds of millions of years prior to the rise in atmospheric O2.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Satkoski et al., 2015
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- Authors
- Satkoski, A. M., Beukes, N. J., Li, W., Beard, B. L., & Johnson, C. M.
- Affiliations
- University of Wisconsin–Madison (US)
- University of Johannesburg (ZA)
- Nanjing University (CN)
- Corresponding author
- Satkoski, Aaron M.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2015-11
- Volume
- 430
- Pages
- 43-53
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W1129004991
- Cited by
- 152
- References
- 54
- Citations by year
- 2026: 6 · 2025: 11 · 2024: 10 · 2023: 14 · 2022: 19 · 2021: 15 · 2020: 11 · 2019: 19 · 2018: 15 · 2017: 17 · 2016: 14 · 2015: 1
- FWCI
- 11.88
- Type
- journal article
- Language
- en
- Update notices
- erratum (2017-02-15)
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- University of Johannesburg
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- Great Oxidation Event, banded iron formations, Fig Tree Group, U-Th-Pb geochronology, iron isotopes, uranium, redox stratification
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