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Atmosphere oxygen cycling through the Proterozoic and Phanerozoic
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“Levels higher than 1% PAL have also been suggested based on trace element contents of pyrite (Large et al., 2019; Steadman et al., 2020; Yierpan et al., 2020).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Large et al., 2019
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Metadata
- Authors
- Large, R. R., Mukherjee, I., Gregory, D., Steadman, J., Corkrey, R., & Danyushevsky, L. V.
- Affiliations
- University of Tasmania (AU)
- University of Toronto (CA)
- Corresponding author
- Large, Ross R.
- Venue
- Mineralium Deposita
- Published
- 2019-03-12
- Volume
- 54
- Issue
- 4
- Pages
- 485-506
- ISSN
- 0026-4598 (ISSN-L)
- 1432-1866
- OpenAlex
- W2920932569
- Cited by
- 122
- References
- 143
- Citations by year
- 2026: 6 · 2025: 20 · 2024: 15 · 2023: 17 · 2022: 21 · 2021: 20 · 2020: 17 · 2019: 6
- FWCI
- 12.20
- Type
- journal article
- Language
- en
- Open access
- green
- figshare.com
- Locations
- Mineralium Deposita (publishedVersion)
- UTAS Research Repository (submittedVersion)
- Figshare (submittedVersion, cc-by)
- Funders
- Australian Research Council (DP 150102578)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- atmospheric oxygen, Proterozoic, Phanerozoic, redox-sensitive elements, sedimentary pyrite, mass extinction, stratiform copper deposits, evaporite formation, ore genesis
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