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The Holocene stalagmite FG01 collected at the Fukugaguchi Cave in Itoigawa, central Japan provides a unique high‐resolution record of the East Asian winter monsoon. Because of the climate conditions on the Japan Sea side of the Japanese islands, the volume of precipitation during the winter is strongly reflected in the stalagmite δ18O signal. Examination of the carbon isotopes and the Mg/Ca ratio...
Stalagmite oxygen stable isotopic records from Chinese and Japanese caves have described the intensity of the East Asian summer monsoon (EASM) in the late Quaternary. In this study, we present a stalagmite δ 18 O record over the past 10,000 years from Fukugaguchi Cave, Itoigawa, Honshu, Japan, facing the Japan Sea. The regional climate is characteristically wet in winter and nearly 60% of...
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