The geochemistry of the stable carbon isotopes
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For carbon isotopes, laboratory experiments suggest a KFF between -13.7 ±0.1‰ and -17.2 ±0.6‰.
“For carbon isotopes, laboratory experiments suggest a KFF between -13.7 ±0.1‰ and -17.2 ±0.6‰ (Table 7, Fig. 13a, Craig, 1953; Usdowski and Hoefs, 1986; Clark et al., 1992; Dietzel et al., 2009; Böttcher et al., 2018)”
From Isotopic fractionation accompanying CO2 hydroxylation and carbonate precipitation from high pH waters at The Cedars, California, USA (2021) · cites this paper as Craig, 1953
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- Authors
- Craig, H.
- Affiliations
- University of Chicago (US)
- Corresponding author
- Craig, Harmon
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1953-02
- Volume
- 3
- Issue
- 2-3
- Pages
- 53-92
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W1990783861
- Cited by
- 1,965
- References
- 47
- Citations by year
- 2026: 18 · 2025: 37 · 2024: 45 · 2023: 30 · 2022: 40 · 2021: 50 · 2020: 60 · 2019: 58 · 2018: 47 · 2017: 38 · 2016: 36 · 2015: 38 · 2014: 44 · 2013: 46 · 2012: 23
- FWCI
- 49.10
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- 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 › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- stable carbon isotopes, terrestrial organic carbon, carbonate rocks, marine organic carbon, atmospheric CO2, fossil wood, coal, limestone, petroleum origin, black shales, graphite, diamond, igneous rock, Yellowstone National Park, meteorites, isotope fractionation, cementite
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