Diatom biochronology of the horizon of warm water calcareous microfossils in the upper Miocene Funakawa Formation distributed in Shimo-arakawa, Daisen City, Akita Prefecture, Japan.

Author:

YANAGISAWA Yukio1

Affiliation:

1. AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation

Publisher

National Institute of Advanced Industrial Science

Subject

General Medicine

Reference35 articles.

1. Akiba, F. (1986) Middle Miocene to Quaternary diatom biostratigraphy in the Nankai Trough and Japan Trench, and modified Lower Miocene through Quaternary diatom zones for middle-to-high latitudes of the North Pacific. In Kagami, H., Karig, D. E., Coulbourn, W. T. et al., Initial Reports of the Deep Sea Drilling Project, 87, 393–480. U. S.Government Printing Office, Washington D. C.

2. Barron, J. A. (1985) Miocene to Holocene planktic diatoms. In Bolli et al., eds. Plankton Stratigraphy, Cambridge Univ. Press, 763–809.

3. Blow, W. H. (1969) Late Middle Eocene to Recent planktonic foraminiferal biostratigraphy. In Brönnimann, P. and Renz, H. H. eds., Proceedings of the First International Conference on Planktonic Microfossils (Geneve,1976), Leiden, no. 1, 199–421.

4. 平松 力・三輪美智子・井上洋子・深沢知恵(1997)東北地方の日本海沿岸地域における中新統の石灰質ナンノ化石層序.瑞浪市化石博物館研究報告,no. 24,

5. 井上洋子(1995)東北日本油田地域における中~後期中新世の暖海性浮遊性有孔虫化石.平成7年度石油技術協会春期講演会シンポジウム・個人講演要旨集,64

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