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Table 1 The age model derived from a comparison between the oxygen isotopic record from the Chiba composite section (this study and Suganuma et al. 2015) and the record of sea level change by Elderfield et al. (2012)

From: Paleomagnetic direction and paleointensity variations during the Matuyama–Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan

Sample Thickness from Byk-E (m) Thickness without sand (m) Age (ka) Sedimentation rate (m/kyr)
KG03 65.90 63.23 749 4.74
KG27 28.00 28.00 757 2.60
YG05 4.60 4.60 766 0.61
TB15 −1.45 −1.45 776 0.46
TB83 −8.30 −8.30 791 2.33
YW02 −19.94 −13.92 796