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