2017 Volume 68 Issue 6 Pages 287-339
Marine diatom biostratigraphy has been established for the Neogene sedimentary sequence distributed in the southern Osado Mountains area, Sado Island, Niigata Prefecture, Japan. The Neogene and Pleistocene sediments in this area are composed of the Orito, Hanyugawa, Nakayama, Nozaka, Kawachi, Kaidate and Shichiba formations in ascending order. This study examined diatoms in the Nakayama and Nozaka formations. The Nakayama Formation is composed of lower hard siliceous mudstone and upper diatomaceous mudstone, and correlated to the diatom zones NPD5B to NPD6A, ranging in age from 12.3 to 6.5 Ma. The Nozaka Formation overlies the Nakayama Formation with a glauconite bed and consists of marine massive mudstone. This formation is assigned to the subzones NPD7Ba and 7Bb, and its depositional age is estimated from 6.5 to 4.2 Ma. The age of the Orito Formation is determined to be latest Early Miocene between 17.0 and 16.7 Ma on the basis of the occurrence of the widespread Arcid-Potamid-type molluscan assemblage. The depositional age of the Hanyugawa Formation is dated by the ages of underlying Orito and overlying Nakayama formations to be early Middle Miocene ranging from 16.7 to 12.3 Ma, suggesting a long slow depositional time interval of over 4 million years.
