Abstract
Changes in orbital-scale stalagmite δ 18 O (δ 18 O s ) recorded from two caves in southern China reveal a clear precessional cycle during Marine Isotope Stage (MIS) 5 and from MIS 9.3 to MIS 8.3. At these sites, δ 18 O s values in MIS 5.5 and MIS 9 were relatively lower than MIS 5.3, 5.1 and MIS 8, and gradually increased towards MIS 5.1 and MIS 8.3, respectively. A similar pattern of variability of δ 18 O s can be observed in other cave records south of 30° N. This southern mode of variability of δ 18 O s closely mimics changes in northern summer insolation, the areal extent of continental ice sheets and atmospheric CO 2 concentrations, suggesting that the direct forcing of summer insolation on landward transport of monsoonal moisture can be further modulated by the Earth's boundary conditions. In contrast, δ 18 O s records around 30° N or northward register a relatively stable precessional cycle, among which δ 18 O s values during the precession minimum (P min ) are similar. This regional disparity implies that during the P min , the strength of northward propagation of monsoonal moisture probably remained constant at northern sites. Moreover, a dampening effect may have limited 18 O-depleted moisture transfer to mid- and high-latitude cave sites, especially during peak interglacials (i.e., MIS 5.5, MIS 9), which may be associated with shifts in the southern edge of the Westerly jet and the average position of the Intertropical Convergence Zone. Another possibility could be that more locally-recycled or near-sourced (isotopically-enriched) moisture contributed to precipitation changes at the northern sites. • A gradual enrichment of δ 18 O s values in Pmin in southern China • A stable precessional cycle in δ 18 O s records around 30°N and northward • Control of NHSI and Earth's boundary conditions on southern δ 18 O s variability • Interplay of Westerly wind and ITCZ on stalagmite δ 18 O records at northern sites
Published Version
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