Fig. 10From: Pliocene integrated chronostratigraphy from the Anno Formation, Awa Group, Boso Peninsula, central Japan, and its paleoceanographic implicationsAge versus thickness diagram for the Anno Formation. Data points are based on the polarity reversal events and marine isotope stages (MISs) listed in Tables 1 and 2, in addition to calcareous nannofossil bioevents (Kameo and Sekine 2013) and radiometric ages (Makinouchi et al. 1983; Tokuhashi et al. 2000; Ueki et al. 2018). The Geomagnetic Polarity Time Scale (GPTS) 2012 is based on Ogg (2012)Back to article page