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Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: Cyclostratigraphy of the Late Miocene to Pliocene sediments at IODP sites U1425 and U1430 in the Japan Sea and paleoceanographic implications

Fig. 7

Relationship 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 Ma

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