δ18O of O2 in a Tibetan Ice Core Constrains Its Chronology to the Holocene

Abstract Dating of the Tibetan ice cores is often challenging with great uncertainties. The significant age difference between the Guliya ice core (∼760 ka [thousand years]) and other Tibetan ice cores (Holocene origin) necessitates new approaches to resolve the inconsistency. Here, we present the a...

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Auteurs principaux:	Huanting Hu, Qiuyu Li, Wangbin Zhang, Shuang‐ye Wu, Jing Song, Ke Liu, Xiang Zou, Hongxi Pang, Maojun Yan, Shugui Hou
Format:	Artigo
Langue:	Inglês
Publié:	Wiley 2022-11-01
Collection:	Geophysical Research Letters
Sujets:	Tibetan ice core trapped air delta‐18O chronology oxygen isotopes Holocene
Accès en ligne:	https://doi.org/10.1029/2022GL098368
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