Geology and Sedimentary Environments of the Pleistocene Setana Formation in the Kuromatsunai District, Southwestern Hokkaido

The Pleistocene Setana Formation is exposed along the axial zone of the Kuromatsunai district, southwestern Hokkaido Island, and is divided into the Nakasato Conglomerate Member and Soe-betsu Sandstone Member. The Nakasato Conglomerate Member consists of medium- to coarse-grained sandstone that accumulated in shoreface, delta, and channel systems. This member is correlated with the overlapping interval between the CN13b calcareous nannofossil zone and the Neogloboquadrina pachyderma (s) / Neogloboquadrina incompta planktonic foraminiferan zone, which indicates an age of 1.2–1.0 Ma. The Soebetsu Sandstone Member is made up of sandy silt-stone to very fine-grained sandstone and includes several beds of shell concentrations. This mem-ber is correlated with the CN14a calcareous nannofossil zone and is thought to range in age from 1.0–0.6 Ma. The Setana Formation contains abundant and well-preserved molluscs, bryozoans, and planktonic and benthic foraminifera. Paleoclimatic reconstructions based on the molluscan and planktonic foraminiferan faunas, and on oxygen isotope ratios from planktonic foraminifera, indi-cate that the basal part of the Nakasato Sandstone Member was deposited during a cooler climate than that of the present Kuromatsunai district, while the lower and middle parts of the Soebets