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Isotope geochemistry of sedimentary sulfates
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“The d34Ssulfate variations in 'Phanerozoic' oceans, based on evaporites (Claypool et al., 1980; Holser and Kaplan, 1966), form an overall trough-like trend similar to strontium isotopes (Figure 30).”
From Evolution of Sedimentary Rocks (2014) · cites this paper as Holser and Kaplan, 1966
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“can be explained by (1) precipitation of evaporites in a restricted basin in the presence of organic matter (McKibben and Eldridge, 1989; Utrilla et al., 1992); and/or (2) supply of sulfates of continental origin to the restricted basin that would enrich the basin in light S-isotopes ( Holster and Kaplan, 1966 ).”
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The rise of oxygen and siderite oxidation during the Lomagundi Event
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“for the isotopic composition of limestones as a function of the siderite oxidation flux (see SI Appendix): δcarb1⁄2‰ = Fsid δsid + e α′ Fin + α′ F w sid [10] where α′= 13 7 − 6 7 α.”
Metadata
- Authors
- Holser, W. T., & Kaplan, I. R.
- Affiliations
- University of California System (US)
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 1966
- Volume
- 1
- Pages
- 93-135
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2019135021
- Cited by
- 550
- References
- 0
- Citations by year
- 2026: 10 · 2025: 11 · 2024: 7 · 2023: 7 · 2022: 16 · 2021: 13 · 2020: 15 · 2019: 12 · 2018: 11 · 2017: 10 · 2016: 9 · 2015: 5 · 2014: 9 · 2013: 10 · 2012: 10
- FWCI
- 12.91
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- 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 › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- anhydrite, gypsum, sulfur isotopes, δ34S, paleoceanography, sulfur cycling, Late Paleozoic, Mesozoic, Tertiary, Late Permian, evaporites, paleogeography, tectonic change
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