Cited by 306Geology and Paleoclimatology ResearchKarst Systems and HydrogeologyMarine and environmental studies

Glacial/interglacial temperature variations in Soreq cave speleothems as recorded by “clumped isotope” thermometry

Affek, Hagit P., Bar-Matthews, Miryam, Ayalon, Avner, Matthews, Alan, Eiler, John M.·2008·Geochimica et Cosmochimica Acta

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Crossref · 10.1016/j.gca.2008.06.031

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  • Clumped isotope constraints on the terrestrial paleoenvironment have advanced understanding of the geosphere, atmosphere, biosphere, and their interactions.

    “Clumped isotope constraints on the terrestrial paleoenvironment have advanced understanding of the geosphere, atmosphere, biosphere, and their interactions, setting the stage for future discoveries.”

    From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Affek et al. 2008

  • Speleothems are a climate archive heavily leveraged for δ18O but displayed complicating disequilibrium signals in 47 due to rapid degassing and rapid precipitation.

    “Speleothems are another climate archive that has been heavily leveraged for δ 18 O but displayed complicating disequilibrium signals in 47 due to rapid degassing and rapid precipitation (Affek et al. 2008, Daëron et al. 2011, Wainer et al. 2011, Kluge & Affek 2012; but see Meckler et al. 2015).”

    From Frontiers of Carbonate Clumped Isotope Thermometry (2023) · cites this paper as Affek et al. 2008

  • In cases of limited degassing and very slow carbonate precipitation, the DIC can approach full oxygen isotope exchange with water, leading to equilibrium δ18O and Δ47 values.

    “In cases of limited degassing and very slow carbonate precipitation, the DIC can approach full oxygen isotope exchange with water, leading to equilibrium δ 18 O and Δ 47 values (Affek et al., 2008).”
  • In pools, with slow carbonate deposition, oxygen isotope exchange between dissolved bicarbonate and H2O drives oxygen and clumped isotope values towards equilibrium.

    “In pools, with slow carbonate deposition, oxygen isotope exchange between dissolved bicarbonate and H2O drives oxygen and clumped isotope values towards equilibrium.”

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Authors
Affek, H. P., Bar-Matthews, M., Ayalon, A., Matthews, A., & Eiler, J. M.
Affiliations
  • Yale University (US)
  • Geological Survey of Israel (IL)
  • Hebrew University of Jerusalem (IL)
  • California Institute of Technology (US)
Corresponding author
Affek, Hagit P.
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
2008-11
Volume
72
Issue
22
Pages
5351-5360
ISSN
0016-7037 (ISSN-L)
OpenAlex
W2133060148
Cited by
306
References
0
Citations by year
2026: 7 · 2025: 5 · 2024: 14 · 2023: 17 · 2022: 12 · 2021: 20 · 2020: 12 · 2019: 19 · 2018: 44 · 2017: 12 · 2016: 19 · 2015: 25 · 2014: 17 · 2013: 21 · 2012: 19
FWCI
8.87
Type
journal article
Language
en
Open access
closed
Locations
  • Geochimica et Cosmochimica Acta (publishedVersion)
  • CaltechAUTHORS (California Institute of Technology) (submittedVersion)
Funders
Israel Science Foundation
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Karst Systems and Hydrogeology
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
Keywords
clumped isotope thermometry, speleothems, Last Glacial Maximum, Holocene temperature, deuterium excess, relative humidity, fluid inclusions, calcite

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