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Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

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

Fig. 7

δ18O variability in Japanese caves during the Holocene and last glacial period. a Fukugaguchi Cave in Niigata Prefecture. The Holocene profile is based on FG01 data (Sone et al. 2013). b Maboroshi Cave in Hiroshima Prefecture (Hori et al. 2014; Shen et al. 2010). c Ohtaki Cave in Gifu Prefecture (Mori et al. 2018). d Kiriana Cave in Mie Prefecture (Mori et al. 2018)

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