Skip to main content
Progress in Earth and Planetary Science
Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: Reconstruction of monsoon evolution in southernmost Sumatra over the past 35 kyr and its response to northern hemisphere climate changes

Fig. 7

Paleoclimatic proxies and referenced data plotted as a function of age (ka B.P.): (a) mean grain size of sensitive component I from core SO184-10043 (this study); (b) CaO/MgO from core SO184-10043 (this study); (c) CIA from core SO184-10043 (this study); (d) Ba/Sr from core SO184-10043 (this study); (e) records of speleothem δ18O from Dongge Cave in the southern China (Yuan et al. 2004) and Hulu Cave in the eastern China (Wang et al. 2001); (f) records of ice core (NGRIP) δ18O from Greenland (Andersen et al. 2006; Rasmussen et al. 2006); (g) integrated summer insolation variations at 30° N over June, July, and August (Berger 1978). Grey, yellow, and orange bars in this figure represent global cold events recorded in our core SO184-10043

Back to article page