Organic Carbon Cycling and the Lithosphere
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The carbon isotope decoupling observed in the Neoproterozoic δ13C record, where δ13Ccarb varies but δ13Corg is near constant, can be explained by the recycling of detrital organic carbon.
“The carbon isotope decoupling observed in the Neoproterozoic δ13C record61 (where δ13Ccarb varies but δ13Corg is near constant) can, as previously proposed496162, be explained by the recycling of detrital organic carbon.”
From Atmospheric oxygen regulation at low Proterozoic levels by incomplete oxidative weathering of sedimentary organic carbon (2017) · cites this paper as [49]
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- Authors
- Derry, L. A.
- Affiliations
- Canadian Institute for Advanced Research (CA)
- Corresponding author
- Derry, L.A.
- ORCID
- Derry, L.A.
- Venue
- Treatise on Geochemistry
- Publisher
- Elsevier
- Published
- 2014
- Pages
- 239-249
- OpenAlex
- W2491832751
- Cited by
- 24
- References
- 91
- Citations by year
- 2024: 6 · 2022: 1 · 2021: 5 · 2020: 7 · 2018: 2 · 2017: 3
- FWCI
- 0.00
- Type
- book chapter
- Language
- en
- Open access
- closed
- Locations
- Treatise on Geochemistry (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 › Geophysics › Geological and Geochemical Analysis
- Keywords
- organic carbon cycling, lithosphere, upper crust, marine sediment, carbon mass balance, carbon isotopes, mantle carbon, Precambrian atmosphere
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