Transitional changes in microfossil assemblages in the Japan Sea from the Late Pliocene to Early Pleistocene related to global climatic and local tectonic events

Author:

Itaki Takuya

Funder

Japan Society for the Promotion of Science

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference125 articles.

1. Akiba F (2001) Fossil diatom assemblages from the Mochikubetsu Formation in the Tenpoku-Haboro areas, northwestern Hokkaido, and their geological implications. Bull Technol Lab JAPEX 15:27–51 (in Japanese with English abstract)

2. Akiba F, Hiramatsu C (1988) Neogene diatom biostratigraphy in Ajiga-sawa, Gosyogawara, and Shimokita area of Aomori Prefecture. In: Iijima A (ed) Comprehensive study of Tertiary siliceous shale –Reports of Grant-in-Aid for Scientific Research during 1987 fiscal year–., pp 35–52, in Japanese

3. Alexandrovich J (1992) Radiolarians from sites 794, 795, 796, and 797 (Japan Sea). In: Pisciotto KA, Ingle JC Jr, von Breymann MT, Barron J, et al (eds) Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 127/128, Pt. 1, 291-307

4. Amano K, Suzuki M, Sato T (2000) Warm-water influx into Japan Sea in the middle Pliocene—molluscan fauna from the Tentokuji Formation around Mt. Taihei in Akita Prefecture. J Geol Soc Jpn 106:299–307

5. Blow WH (1969) Late Middle Eocene to recent planktonic foraminiferal biostratigraphy. In Bronimann P and Renz HR (eds) Proc. 1st lnternat. Conf. Planktonic Microfossils, Gcncva, 1967, 1, 199-422, E.J. Brill, Leiden

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