Centennial-scale hydrogeomorphic evolution associated with the Indian summer monsoon during the late Holocene on the southern Qinghai–Tibetan Plateau: evidence from a rare shallow lake

A 2.16 m ZGC21 core was drilled from the Drigu Co on the southern QTP. Meanwhile, physical and chemical indicators, including the water content, grain size, LOI, TOC, TN, pollen, carbonate δ18O, and AMS-14C age, were analyzed. The dataset include all data of above experiments results in this study.