Supplemental Material: Asynchronous Holocene lake evolution in arid mid-latitude Asia is driven by glacial meltwater and variations in Westerlies and the East Asian summer monsoon
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摘要
This document presents details on luminescence dating sample preparation, analytical facilities (Supplemental Text S1) and quartz and K-feldspar luminescence dating measurement, and dose rate determination (Supplemental Text S2), the photograph, locational information and luminescence dating results of the paleoshorelines at Aibi Lake Basin (Figures S1-S4 and Table S1-S6), and the reconstructed lake area changes of Aibi Lake during past 18 ka (Figure S5).
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