Holocene Lake Evolution and Glacial Fluctuations Indicated by Carbonate Minerals and Their Isotopic Compositions in the Sediments of a Glacial Melt Recharge Lake on the Northwestern Tibetan Plateau

Holocene Lake Evolution and Glacial Fluctuations Indicated by Carbonate Minerals and Their Isotopic Compositions in the Sediments of a Glacial Melt Recharge Lake on the Northwestern Tibetan Plateau

Lakes and glaciers are widely distributed on the Tibetan Plateau and are linked via hydrological processes. They are experiencing rapid changes due to global warming, but their relationships during the Holocene are less well known due to limited coupled geological records. Here, we analyzed the δ13C...

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Bibliographic Details
Main Authors: Minghui Li, Liping Zhu, Junbo Wang, Jianting Ju, Chong Liu, Qingfeng Ma, Teng Xu, Baojin Qiao, Xiaoxiao Wang
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-06-01
Series:Frontiers in Earth Science
Subjects:
carbonate minerals
oxygen and carbon isotopes
lake water temperature
glacial fluctuations
climatic events
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.656281/full

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