4.6 Article

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

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Summary: This study proposes using authigenic carbonate δ18O from glacial lakes as a quantitative proxy to estimate glacier meltwater variations. It reveals significant fluctuations in glacier meltwater in the Western Kunlun Mountain region over different time periods and suggests that about 20% of regional glaciers melted from the Early to Late Holocene, likely influenced by summer temperatures and melting potential accumulation. The study also warns of severe threats to Tibetan Plateau glaciers due to current rates of global warming.

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