Identification of an Archean marine oxygen oasis
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Sedimentary marine carbonates appear from 3.52 Ga ago onward.
“In fact, sedimentary marine carbonates appear from 3.52 Ga ago onward [(98) and references therein].”
From The Archean atmosphere (2020) · cites this paper as [98]
Fractionated iron and molybdenum isotopes and levels of redox-sensitive metals suggest marine photic zone O2 at 3.2 to 3.0 Ga ago.
“Fractionated iron and molybdenum isotopes and levels of redox-sensitive metals suggest marine photic zone O2 (96–99).”
From The Archean atmosphere (2020) · cites this paper as [98]
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Self-citation
- Authors
- Riding, R., Fralick, P., & Liang, L.
- Affiliations
- University of Tennessee at Knoxville (US)
- Lakehead University (CA)
- Oak Ridge National Laboratory (US)
- Corresponding author
- Riding, Robert
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 2014-09
- Volume
- 251
- Pages
- 232-237
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W2076647823
- Cited by
- 132
- References
- 49
- Citations by year
- 2026: 1 · 2025: 16 · 2024: 16 · 2023: 8 · 2022: 12 · 2021: 12 · 2020: 12 · 2019: 7 · 2018: 20 · 2017: 13 · 2016: 10 · 2015: 5
- FWCI
- 6.81
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Precambrian Research (publishedVersion)
- Funders
- U.S. Department of Energy
- Lakehead University
- Natural Sciences and Engineering Research Council of Canada
- Oak Ridge National Laboratory
- 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
- oxygenic photosynthesis, seawater oxygen, rare earth elements, iron oxyhydroxide, iron-rich sediments, cyanobacteria, stromatolites, organic carbon isotopes
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