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Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water

Abstract : The oxygen isotope composition of speleothems is a widely used proxy for past climate change. Robust use of this proxy depends on understanding the relationship between precipitation and cave drip water δ 18 O. Here, we present the first global analysis, based on data from 163 drip sites, from 39 caves on five continents, showing that drip water δ 18 O is most similar to the amount-weighted precipitation δ 18 O where mean annual temperature (MAT) is < 10°C. By contrast, for seasonal climates with MAT > 10°C and < 16°C, drip water δ 18 O records the recharge-weighted δ 18 O. This implies that the δ 18 O of speleothems (formed in near isotopic equilibrium) are most likely to directly reflect meteoric precipitation in cool climates only. In warmer and drier environments, speleothems will have a seasonal bias toward the precipitation δ 18 O of recharge periods and, in some cases, the extent of evaporative fractionation of stored karst water.
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Contributor : Dominique Genty Connect in order to contact the contributor
Submitted on : Monday, December 28, 2020 - 2:13:07 PM
Last modification on : Tuesday, January 5, 2021 - 3:09:33 AM
Long-term archiving on: : Monday, March 29, 2021 - 6:42:38 PM


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Andy Baker, Andreas Hartmann, Wuhui Duan, Stuart Hankin, Laia Comas-Bru, et al.. Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water. Nature Communications, Nature Publishing Group, 2019, 10, ⟨10.1038/s41467-019-11027-w⟩. ⟨hal-03089444⟩



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