Millennial-Scale Asian Monsoon Influenced Longjie Lake Evolution during Marine Isotope Stage 3, Upper Stream of Changjiang (Yangtze) River, China

Figure 7

Comparison of grain size in Longjie Section (a) with stalagmite δ¹⁸O in Hulu Cave [36–39] (b), mean grain size of the Gulang loess sequence, Chinese Loess Plateau [12] (c), and Greenland ice core δ¹⁸O [40] (d). Thin lines represent original data, and bold lines were filtered from 1.5 ka low-frequency pass process. Numbers labeled in (a) represent possible warm-wet events regarding Dansgaard-Oeschger (DO) events.