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Progress in Earth and Planetary Science
Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

From: Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the Japan Sea during the last glacial period

Fig. 6

Comparison of FG02 δ18O data and climate interpretation with other paleoclimatic studies in the period 20–25 ka. a Greenland ice core δ18O (Seierstad et al. 2014) and b Ca2+ (Rasmussen et al. 2014). c FG02 δ18O data (this study). Climate interpretation is according to case 1. d Grain size variation of quartz in loess sediments from the Chinese Loess Plateau (Sun et al. 2012). e δ18O variability in Hulu Cave (south China; Wang et al. 2001). f δ18O variability in Kiriana Cave (Mie Prefecture, Japan; Mori et al. 2018)

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