Fig. 4From: Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the Japan Sea during the last glacial periodIsotopic behaviors of FG02. a Hendy test results for δ18OC at three growth lines, 26 mm (red), 60 mm (black), and 120 mm (blue) from the top. Subsamples were collected at 1-mm intervals from the central growth axis. b Covariance between δ18O and δ13CBack to article page