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Explaining the Structure of the Archean Mass-Independent Sulfur Isotope Record
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Modeling suggests that volcanic output and microorganisms created a distinctive profile of sulfur isotopes on early Earth.
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“The high, spatially heterogeneous, and temporally variable Δ33S values and the large area of the Transvaal Basin where these rocks were deposited suggest that the photochemical products of SO2 in an anoxic atmosphere were the primary origin of these signals.”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [45]
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- H. D. Holland in Treatise on Geochemistry vol. 6 K. K. Turekian H. D. Holland Eds. (Elsevier-Pergamon Oxford 2004) pp. 583– 625.
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Metadata
- Authors
- Halevy, I., Johnston, D. T., & Schrag, D. P.
- Affiliations
- Harvard University (US)
- Corresponding author
- Halevy, Itay
- Venue
- Science
- Published
- 2010-07-09
- Volume
- 329
- Issue
- 5988
- Pages
- 204-207
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W1986579555
- Cited by
- 141
- References
- 27
- Citations by year
- 2026: 3 · 2025: 5 · 2024: 6 · 2023: 4 · 2022: 9 · 2021: 5 · 2020: 6 · 2019: 16 · 2018: 13 · 2017: 9 · 2016: 8 · 2015: 9 · 2014: 11 · 2013: 16 · 2012: 14
- FWCI
- 8.31
- Type
- journal article
- Language
- en
- Open access
- green
- nrs.harvard.edu
- Licence
- cc-by
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- Digital Access to Scholarship at Harvard (DASH) (Harvard University) (submittedVersion, cc-by)
- 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
- Archean, sulfur cycling, sulfur isotope fractionation, biogeochemical modeling, continental crust formation, bacterial sulfate reduction, redox state, early Earth atmosphere
- MeSH terms
- Atmosphere, Bacteria, Iron, Models, Theoretical, Oceans and Seas, Oxidation-Reduction, Photolysis, Seawater, Sulfates, Sulfides, Sulfur, Sulfur Dioxide, Sulfur Isotopes, Time, Volcanic Eruptions, Geologic Sediments, Evolution, Planetary
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