A change in the warm water Kuroshio current system from the final glacial age end to the interglacial period, it is based on diatom fossil in the western north Pacific during the R/V Mirai cruise [MR99-K04]
Yamamoto, H. (2000). A change in the warm water Kuroshio current system from the final glacial age end to the interglacial period, it is based on diatom fossil in the western north Pacific during the R/V Mirai cruise [MR99-K04]. Rep. Japan Mar. Sci. Technol. Cent. 42: 21-27
In: Report of Japan Marine Science and Technology Center = Kaiyo Kagaku Gijutsu Senta Shiken Kenkyu Hokoku. JAMSTEC: Yokosuka; Yokohama. ISSN 0387-382X, meer
|
