An explanation of the effect of seawater carbonate concentration on foraminiferal oxygen isotopes
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The δ18O and Δ47 of dissolved inorganic carbon species decrease in the sequence CO2(aq) > HCO3− > CO3 2−.
“The d 18 O - and the D 47 of the DIC species decrease in this sequence (Zeebe, 1999; Hill et al., 2014).”
From Temperature dependence of oxygen- and clumped isotope fractionation in carbonates: A study of travertines and tufas in the 6-95 °C temperature range (2015) · cites this paper as Zeebe, 1999
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- Authors
- Zeebe, R. E.
- Affiliations
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE)
- Corresponding author
- Zeebe, Richard E.
- ORCID
- Zeebe, Richard E.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1999-07
- Volume
- 63
- Issue
- 13-14
- Pages
- 2001-2007
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2081330634
- Cited by
- 368
- References
- 3
- Citations by year
- 2026: 5 · 2025: 7 · 2024: 18 · 2023: 8 · 2022: 17 · 2021: 17 · 2020: 10 · 2019: 11 · 2018: 15 · 2017: 14 · 2016: 10 · 2015: 20 · 2014: 17 · 2013: 22 · 2012: 23
- FWCI
- 4.24
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Keywords
- planktonic foraminifera, Orbulina universa, oxygen isotopes, carbonate system, pH, oxygen isotope fractionation, calcium carbonate precipitation, paleoceanography, paleotemperature proxies
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