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Carbon Isotope Stratigraphy

Saltzman, M.R., Thomas, E.·2012·The Geologic Time Scale

DOI 10.1016/b978-0-444-59425-9.00011-1

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“Carbon isotopes are also relatively resistant to major diagenetic processes (Saltzman et al., 2012) and in sufficiently continuous rock successions the resulting isotopic signature tends to remain recognizable despite any potential local diagenetic overprinting (Weissert et al., 2008; Kouchinsky et…”
Background
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Authors: Saltzman, M. R., & Thomas, E.
ORCID: Saltzman, M.R.
Thomas, E.
Venue: The Geologic Time Scale
Publisher: Elsevier
Published: 2012
Pages: 207-232
DOI: 10.1016/b978-0-444-59425-9.00011-1
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
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
www.elsevier.com/legal/tdmrep-license (tdm)
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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