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

δ18O of speleothems are a widely used paleoclimate proxy. Here, the authors conduct a global analysis of cave drip water δ18O compositions and find that drip waters from warmer climates have a seasonal bias toward precipitation δ18O of recharge periods, unlike in cooler climates where drip waters ma...

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Autores principales:	Andy Baker, Andreas Hartmann, Wuhui Duan, Stuart Hankin, Laia Comas-Bru, Mark O. Cuthbert, Pauline C. Treble, Jay Banner, Dominique Genty, Lisa M. Baldini, Miguel Bartolomé, Ana Moreno, Carlos Pérez-Mejías, Martin Werner
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/796cc0681a8a466a8d693c8cf617b6a6
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spelling	oai:doaj.org-article:796cc0681a8a466a8d693c8cf617b6a62021-12-02T14:39:00ZGlobal analysis reveals climatic controls on the oxygen isotope composition of cave drip water10.1038/s41467-019-11027-w2041-1723https://doaj.org/article/796cc0681a8a466a8d693c8cf617b6a62019-07-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-11027-whttps://doaj.org/toc/2041-1723δ18O of speleothems are a widely used paleoclimate proxy. Here, the authors conduct a global analysis of cave drip water δ18O compositions and find that drip waters from warmer climates have a seasonal bias toward precipitation δ18O of recharge periods, unlike in cooler climates where drip waters match well with recharge-weighted δ18O.Andy BakerAndreas HartmannWuhui DuanStuart HankinLaia Comas-BruMark O. CuthbertPauline C. TrebleJay BannerDominique GentyLisa M. BaldiniMiguel BartoloméAna MorenoCarlos Pérez-MejíasMartin WernerNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-7 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Andy Baker Andreas Hartmann Wuhui Duan Stuart Hankin Laia Comas-Bru Mark O. Cuthbert Pauline C. Treble Jay Banner Dominique Genty Lisa M. Baldini Miguel Bartolomé Ana Moreno Carlos Pérez-Mejías Martin Werner Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
description	δ18O of speleothems are a widely used paleoclimate proxy. Here, the authors conduct a global analysis of cave drip water δ18O compositions and find that drip waters from warmer climates have a seasonal bias toward precipitation δ18O of recharge periods, unlike in cooler climates where drip waters match well with recharge-weighted δ18O.
format	article
author	Andy Baker Andreas Hartmann Wuhui Duan Stuart Hankin Laia Comas-Bru Mark O. Cuthbert Pauline C. Treble Jay Banner Dominique Genty Lisa M. Baldini Miguel Bartolomé Ana Moreno Carlos Pérez-Mejías Martin Werner
author_facet	Andy Baker Andreas Hartmann Wuhui Duan Stuart Hankin Laia Comas-Bru Mark O. Cuthbert Pauline C. Treble Jay Banner Dominique Genty Lisa M. Baldini Miguel Bartolomé Ana Moreno Carlos Pérez-Mejías Martin Werner
author_sort	Andy Baker
title	Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
title_short	Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
title_full	Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
title_fullStr	Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
title_full_unstemmed	Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
title_sort	global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/796cc0681a8a466a8d693c8cf617b6a6
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Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water

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