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“Consistent with a rise in oxygen, the carbon isotope record (17) (Fig. 1) indicates a fundamental shift in baseline from ≤ 0 ‰ before the Late Ordovician to ∼ 2 ‰ from ∼ 445 Ma onward.”
From Earliest land plants created modern levels of atmospheric oxygen (2016) · cites this paper as [17]
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“Though there are many subsequent δ 13 C fluctuations, including drops back to 0 ‰ , for example, at ∼ 400 Ma, the long-term mean δ 13 C remains ∼ 2 ‰ throughout the rest of the Paleozoic, the Mesozoic, and the Early Cenozoic (17), indicating a sustained increase in global organic carbon burial.”
From Earliest land plants created modern levels of atmospheric oxygen (2016) · cites this paper as [17]
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Metadata
- Authors
- Saltzman, M. R., & Thomas, E.
- Venue
- The Geologic Time Scale
- Publisher
- Elsevier
- Published
- 2012
- Pages
- 207-232
- OpenAlex
- W41374818
- Cited by
- 436
- References
- 301
- Citations by year
- 2026: 11 · 2025: 29 · 2024: 29 · 2023: 25 · 2022: 38 · 2021: 56 · 2020: 53 · 2019: 40 · 2018: 38 · 2017: 30 · 2016: 23 · 2015: 23 · 2014: 16 · 2013: 13 · 2012: 8
- FWCI
- 24.91
- Type
- book chapter
- Language
- en
- Open access
- closed
- Locations
- Elsevier eBooks (publishedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
- Keywords
- carbon isotope stratigraphy, total dissolved inorganic carbon, carbon cycle, platform carbonates, pelagic carbonates, diagenesis, Proterozoic, Phanerozoic, Jurassic, Cenozoic
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