Contrasting responses of monsoon rainfall and speleothem oxygen isotope between Northeast Asia and North China during the early-mid Holocene

This is the Supporting Information for Wang et al. "Contrasting responses of monsoon rainfall and speleothem oxygen isotope between Northeast Asia and North China during the early-mid Holocene" published in Geophysical Research Letters. The data comes from two stalagmite northeastern Vladivostok in the southern Russian Far East. The dataset includes the carbon and oxygen isotope data (Table S1). The Supporting Information S1 includes a pdf file contains Text S1 for details on the climate model, Text S2 for details on the methods of all the lab work, Figure S1 for age models, Figure S2 for the results of the Hendy test, Figure S3 for the results of Tetukhe-T1 and Sadovaya-S1 speleothem records, Figure S4 for the relationship between moisture source and regional δ¹⁸O, Figure S5 for the relationship between regional precipitation and δ¹⁸O, Figure S6 for the moisture source analyses for North China and Northeast Asia, Figure S7 for the vertical Structure of Wind Fields During Mid-Holocene (6 ka) and Early Holocene (9 ka), Figure S8 for the comparison of δ¹⁸O values, precipitation from the isoGSM model, and GNIP Terney station (1996–2000), Table S1 for the 230Th dating results, Table S2 for experiment details performed in COSMOS-wiso.