Asynchronous Climate Changes in the North Atlantic and Japan During the Last Termination
-
- Takeshi Nakagawa
- International Research Center for Japanese Studies, 3-2 Oeyama-cho, Goryo, Nishikyo-ku, Kyoto 610-1192, Japan.
-
- Hiroyuki Kitagawa
- Institute for Hydrospheric Atmospheric Sciences, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8601, Japan.
-
- Yoshinori Yasuda
- International Research Center for Japanese Studies, 3-2 Oeyama-cho, Goryo, Nishikyo-ku, Kyoto 610-1192, Japan.
-
- Pavel E. Tarasov
- Department of Geography, Moscow State University, Vorob'evy Gory, Moscow 119899, Russia.
-
- Kotoba Nishida
- Department of Mathematics and Computer Science, Faculty of Science, Kagoshima University, 1-21-35 Koorimoto, Kagoshima 890-0065, Japan.
-
- Katsuya Gotanda
- International Research Center for Japanese Studies, 3-2 Oeyama-cho, Goryo, Nishikyo-ku, Kyoto 610-1192, Japan.
-
- Yuki Sawai
- International Research Center for Japanese Studies, 3-2 Oeyama-cho, Goryo, Nishikyo-ku, Kyoto 610-1192, Japan.
書誌事項
- 公開日
- 2003-01-31
- DOI
-
- 10.1126/science.1078235
- 公開者
- American Association for the Advancement of Science (AAAS)
この論文をさがす
説明
<jats:p>Pollen records from the annually laminated sediment sequence in Lake Suigetsu, Japan, suggest a sequence of climate changes during the Last Termination that resembles that of the North Atlantic region but with noticeable differences in timing. An interstadial interval commenced a few centuries earlier [∼15,000 years before the present (yr B.P.)] than the North Atlantic GI-1 (Bölling) event. Conversely, the onset of a Younger Dryas (YD)–like cold reversal (12,300 to 11,250 yr B.P.) postdated the North Atlantic GS-1 (YD) event by a few centuries. Climate in the Far East during the Last Termination reflected solar insolation changes as much as Atlantic influences.</jats:p>
収録刊行物
-
- Science
-
Science 299 (5607), 688-691, 2003-01-31
American Association for the Advancement of Science (AAAS)