Fig. 7From: Cyclostratigraphy of the Late Miocene to Pliocene sediments at IODP sites U1425 and U1430 in the Japan Sea and paleoceanographic implicationsRelationship between GRA and estimated sea level. GRA data are from sites U1425 and U1430 and resampled every 100 kyr. Sea level is converted from oxygen isotope values using a calibration ratio of 0.1‰/10 m (Miller et al. 2005). Estimated sea level is also evenly sampled every 100 kyr. Regression line is applied to the all data during the last 9 Myr. Red circles are the data from 6.6 to 3.6 MaBack to article page