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. 2012 Aug 31;2:619. doi: 10.1038/srep00619

Figure 3. Comparison of Lake Qinghai records with other records since 11.5 ka.

Figure 3

(a) NGRIP δ18O26; (b) North Atlantic ice-rafted hematite stained grains (HSG)29; (c) Lake Qinghai Westerlies climate index (WI, flux of >25 μm fraction); (d) Lake Qinghai Asian summer monsoon index (SMI); (e) δ18O record of ostracods from Lake Qinghai: dark brown, Limnocythere inopinata; orange, Eucypris mareotica; (f) Dongge cave speleothem δ18O21; (g) atmosphere Δ14C38. The shaded blue bars indicate correlations of various proxies for climatic events. The triangles indicate the 14C dates used for the age model for core 1Fs (Supplementary Fig. S5).