Here we present results of 230Th dating, stable isotope and lamina thickness data from two stalagmites (CS01C and SHD1311) from Shihua Cave (latitude 39´47°N, longitude 115´56°E; altitude 251 m a.s.l. at the entrance), northern China, during 11.32 to 10 ka BP. CS01C developed with clear annual lamina. The age model of CS01C is based on lamina counting. The age model of SHD1311 is established using the COPRA algorithm. The variability of stalagmite δ18O records is interpreted as a proxy of regional summer monsoon precipitation and/or EASM intensity. Stalagmite δ18O records show two weak summer monsoon events at 10.9 and 10.3 ka. The 10.9-ka event occurred from 10.93–10.79 ka BP for ~140 yr and features a “W”-shaped structure. The 10.3-ka event, also known as the ice-rafted debris event 7 in the North Atlantic, lasted ~260 yr with an asymmetric double-plunging structure.

Dataset1: 230Th dating results for stalagmites CS01C and SHD1311; Dataset2: CS01C δ18O and δ13C record and lamina counting age model; Dataset3: CS01C lamina thickness; Dataset4: SHD1311 δ18O record and COPRA age model; Dataset5: age ensemble of CS01C δ18O calculated by BAM algorithm; Dataset6: age ensemble of CS01C lamina thickness calculated by BAM algorithm; Dataset7: age ensemble of SHD1311 δ18O calculated by COPRA algorithm.

{"references": ["Li, M., Wang, F., Cai, B., Cao, Q., Cheng, H., Shen, C.-C., et al. (2022). Timing and structure of 10.9 and 10.3 ka BP events revealed by annually laminated stalagmite records from Shihua Cave, northern China. Paleoceanography and Paleoclimatology, 37, e2022PA004459. https://doi.org/10.1029/2022PA004459"]}