Dynamic sulfur and carbon cycling through the end-Ordovician extinction revealed by paired sulfate–pyrite δ34S
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This finding is broadly consistent with the sulfur isotope record, which shows a marked decline through the Silurian-Early Devonian from ∼30 to ∼18‰, although available data also suggest an earlier Late Ordovician-Early Silurian rise from ∼25 to ∼30‰, which the present model does not capture.
“This finding is broadly consistent with the sulfur isotope ( δ 34 S) record (38 -40), which shows a marked decline through the Silurian -Early Devonian from ∼ 30 to ∼ 18 ‰ , although available data also suggest an earlier Late Ordovician -Early Silurian rise from ∼ 25 to ∼ 30 ‰ , which the present model does not capture.”
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- Authors
- Jones, D. S., & Fike, D. A.
- Affiliations
- Amherst College (US)
- Washington University in St. Louis (US)
- Corresponding author
- Jones, David S.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2013-02
- Volume
- 363
- Pages
- 144-155
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2069112811
- Cited by
- 123
- References
- 101
- Citations by year
- 2026: 6 · 2025: 8 · 2024: 7 · 2023: 11 · 2022: 7 · 2021: 9 · 2020: 13 · 2019: 11 · 2018: 15 · 2017: 14 · 2016: 10 · 2015: 8 · 2014: 1 · 2013: 3
- FWCI
- 4.99
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- Agouron Institute
- Amherst College
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- end-Ordovician mass extinction, pyrite sulfur isotopes, carbonate-associated sulfate, microbial sulfur cycling, sulfur isotope fractionation, ocean anoxia, carbon isotope excursion, pyrite burial, sediment reworking
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