Constraints on hydrogen levels in the Archean atmosphere based on detrital magnetite
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This provides an upper limit of pH2 ≤ 10^-2 bar.
“Detrital magnetite carried in rivers 3.0- to 2.7-Ga ago would have dissolved at high pH2 via microbial reduction of Fe3+ to soluble Fe2+ using H2 (199), providing an upper limit of pH2 ≤ 10−2 bar (200).”
From The Archean atmosphere (2020) · cites this paper as [200]
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“7-Ga ago would have dissolved at high pH2 via microbial reduction of Fe(3) + to soluble Fe(2) + using H2 (199), providing an upper limit of pH2 ≤ 10 −2 bar (200).”
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- Authors
- Kadoya, S., & Catling, D. C.
- Affiliations
- University of Washington (US)
- Corresponding author
- Kadoya, Shintaro
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2019-10
- Volume
- 262
- Pages
- 207-219
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2964880290
- Cited by
- 16
- References
- 47
- Citations by year
- 2026: 3 · 2025: 4 · 2024: 1 · 2023: 1 · 2022: 2 · 2020: 5
- FWCI
- 1.33
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Funders
- Simons Foundation
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Geomagnetism and Paleomagnetism Studies
- Keywords
- atmospheric hydrogen, Archean atmosphere, detrital magnetite, early Earth, greenhouse gases, riverbed, prebiotic chemistry, methanogenic archaea, atmospheric lifetime
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