Geological Literature Search (GEOLIS) (Geological Survey of Japan / AIST)

The cause of the temporal changes in the Tsushima Current during interglacial periods in the late Pliocene-early Pleistocene Japan Sea. - reexamination of the early Pleistocene occurrences of the planktonic foraminifer Globoconella inflata

Authors=KITAMURA Akihisa

Journal/Book_names=Fossils

number=82

pages=52-59

Publish_year=2007

Publish_Country=JPN

Publisher=The Palaeontological Society of Japan

Language_of_Text=JA

Language_of_Abs=EN

ISSN=00229202

DOI=10.14825/kaseki.82.0_52

ID=200726656

@id=https://gbank.gsj.jp/ld/resource/geolis/200726656