著者
安田 喜憲
出版者
地理科学学会
雑誌
地理科学 (ISSN:02864886)
巻号頁・発行日
vol.42, no.2, pp.113-119, 1987
被引用文献数
1

A comparative study of the Japanese pollen records to the oxgen and carbon-isotope/pollen records from the Arabian Sea, Bengal Bay and Andaman Sea suggests the following summer monsoon fluctuations since the last glacial age in Japan. Ca. 120,000-70,000 years B.P.; Monsoon is active. 70, OO0-50, OOO years B.P.; Monsoon is not active. 50,000-33,000 years B.P.; Monsoon is rather active. 33,000-12,000 years B.P.; Monsoon is not active. But from 28,000 to 25,000 years B.P. is slightly active. 12,000-10,000 years B.P.; Monsoon is to move active. after 10,000 years B.P.; Monsoon is active.

言及状況

外部データベース (DOI)

Twitter (1 users, 1 posts, 0 favorites)

CiNii 論文 -  最終氷期以降の気候変動とモンスーン https://t.co/3hgtmNlzgq #CiNii

収集済み URL リスト