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.