Abstract

There were three biogeographic provinces in Japan, Sakhalin, and Taiwan during Paleogene time: Taiwan-South Japan, Central Japan, and North Japan-Western Okhotsk Provinces. In the middle Eocene, tropical or subtropical Tethyan Indo-Pacific elements migrated northward to southern and northern Japan. The Central Japan Province was formed by the southward migration of the Asagai-Poronaian molluscs of the North Japan-Western Okhotsk Province. In addition, the Asagai-Poronaian molluscs of the North Japan-Western Okhotsk (and Central Japan) Provinces migrated southward to Kyushu, Southern Japan, which are found in the Ashiya fauna of late early Oligocene to earliest Miocene age. Furthermore, the Asagai-Poronaian molluscs survived into the Acilana tokunagai fauna (late early to early middle Miocene) of Northern and Central Japan and indicate an offshore, cold-water mud-bottom environment.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.