Fossil foraminiferal and ostracode assemblages from the Pleistocene Tokyo Formation in cores GS-SE-1, Kami-Yoga and GS-SE-3, Komazawa, Setagaya, Tokyo, central Japan

Author:

KANEKO Minoru1,ISHIKAWA Hiroyuki2,HARASHIMA Mai3,NOMURA Masahiro4,NAKAZAWA Tsutomu5

Affiliation:

1. Research Fellow of Gunma Museum of Natural History

2. No affiliation

3. University of Tsukuba, Graduate School of Science and Technology, Degree Programs in Life and Earth Sciences

4. Surugadai University, Faculty of Media and Information Resources

5. AIST, Geological Survey of Japan, Geoinformation Service Center

Publisher

National Institute of Advanced Industrial Science

Subject

General Medicine

Reference32 articles.

1. 秋元和實・長谷川四郎(1989)日本近海における現生底生有孔虫の深度分布—古水深尺度の確立に向けて—. 地質学論集no. 32229–240

2. 千地万造(1969)Ammonia beccariiグル−プによる内湾性堆積環境推定の試み.日本地質学会第76年学術大会シンポジウム海岸平野75–81

3. Harrington, G. L. (1960) A Recent foraminiferal faunule from Honshu, Japan. Science Reports of the Tohoku University, 2nd series (Geology), Special Volume, no. 4, 45–55.

4. 樋口 雄(1953)宮田層の有孔虫化石群について.地質学雑誌,60,138–144 10.5575/geosoc.60.138

5. Ikeya, N. (1977) Ecology of foraminifera in the Hamana Lake region of the Pacific coast of Japan. Reports of Faculty of Science, Shizuoka University, 11, 131–159.

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