Figure 10
From: High precise dating on the variation of the Asian summer monsoon since 37 ka BP
Comparison of paleoclimate records of H1-3 in different latitudes. (A) δ18O record of the NGRIP ice core21,55. (B) North Atlantic ocean sediment cores compilation Pa/Th record67. (C) Sea surface temperature records reconstructed from Iberian margin marine sediment cores MD01-2444 and MD01-244368. (D) δ18O record of stalagmite FR5 (this study). (E) Reflectance records of Cariaco Basin sediment cores MD03-262157. (F) CH4 record in the WAIS ice core60. The light blue and orange bands indicate the onset and termination of H events, respectively.
