Fig. 4: Middle Holocene SST record in comparison with EAWM index, precipitation and temperature as well as coporstanol index. | Communications Earth & Environment

Fig. 4: Middle Holocene SST record in comparison with EAWM index, precipitation and temperature as well as coporstanol index.

From: Marine sedimentary evidence reveals East Asian Winter Monsoon forcing on Neolithic Cultural transitions in Central and Eastern China

Fig. 4: Middle Holocene SST record in comparison with EAWM index, precipitation and temperature as well as coporstanol index.The alternative text for this image may have been generated using AI.

Middle Holocene SST in Core SD-01 (A, G), Speleothem δ13C in Magou of Henan Province5 (‰) (B, K), Stacked normalized mean grain size (MGS) from Chinese Loess12 (C), mean atmospheric temperature anomaly (MATA) in Shandong Province71 (MATA in Shandong) (D), Mean annual precipitation (MAP) in Yazihai72 (E, J) and Gonghai2 (F), Coporstanol (H) and 5β-stigmastanol (I) flux in Core SD-01 and Speleothem δ13C in Wuya at Loess Plateau (‰)73 (L).

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