Equilibrium vs. kinetic fractionation of oxygen isotopes in two low-temperature travertine-depositing systems with differing hydrodynamic conditions at Baishuitai, Yunnan, SW China
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We chose only vent and pool samples, which have been shown to be least affected by kinetic fractionation due to progressive degassing.
“We chose only vent and pool samples, which have been shown to be least affected by kinetic fractionation due to progressive degassing (Yan et al., 2012; Wang 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 Yan et al., 2012
Data of the Baishuitai travertine samples are taken from Yan et al. (2012).
“Data of the Baishuitai travertine samples are taken from Yan et al. (2012).”
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 Yan et al. (2012)
Vent and pool travertines, in relation to their clumped isotope composition, probably represent close to equilibrium precipitation over the entire 5.6-95°C temperature range.
“these data suggest that vent and pool travertines, which are the least likely to be affected by kinetic fractionation based on previous stable isotope studies (Kele et al., 2008; Kele et al., 2011; Yan et al., 2012; Wang et al., 2014), in relation to their clumped isotope composition probably represent close to equilibrium precipitation in the entire 5.6-95°C temperature”
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 Yan et al., 2012
Vent and pool travertines are the least likely among the studied samples to be affected by kinetic fractionation, based on previous stable isotope studies.
“vent and pool travertines, which are the least likely to be affected by kinetic fractionation based on previous stable isotope studies (Kele et al., 2008; Kele et al., 2011; Yan et al., 2012; Wang 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 Yan et al., 2012
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References 59 · Cited by 38
- Authors
- Yan, H., Sun, H., & Liu, Z.
- Affiliations
- Chinese Academy of Sciences (CN)
- Corresponding author
- Liu, Zaihua
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2012-10
- Volume
- 95
- Pages
- 63-78
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2077801996
- Cited by
- 38
- References
- 59
- Citations by year
- 2025: 3 · 2024: 5 · 2023: 2 · 2022: 2 · 2021: 2 · 2020: 3 · 2019: 6 · 2018: 1 · 2017: 2 · 2016: 6 · 2015: 2 · 2014: 1 · 2013: 3
- FWCI
- 2.31
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Funders
- National Natural Science Foundation of China
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Karst Systems and Hydrogeology
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- oxygen isotope fractionation, travertine, isotopic equilibrium, kinetic isotope fractionation, paleotemperature reconstruction, Rayleigh distillation, dissolved carbonate, hydrodynamic conditions, water residence time, CO2 degassing, paleoclimate proxies
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