日本地球惑星科学連合2022年大会

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[E] 口頭発表

セッション記号 U (ユニオン) » ユニオン

[U-05] Advanced understanding of Quaternary and Anthropocene hydroclimate changes in East Asia

2022年5月25日(水) 15:30 〜 17:00 302 (幕張メッセ国際会議場)

コンビーナ:窪田 薫(神戸大学大学院人間発達環境学研究科)、コンビーナ:横山 祐典(東京大学 大気海洋研究所 高解像度環境解析研究センター)、Chuan-Chou Shen(National Taiwan University)、コンビーナ:Lo Li(Department of Geosciences, National Taiwan University)、座長:窪田 薫(海洋研究開発機構海域地震火山部門)、Li Lo(Department of Geosciences, National Taiwan University)、横山 祐典(東京大学 大気海洋研究所 高解像度環境解析研究センター)、Chuan-Chou Shen(National Taiwan University)

16:24 〜 16:42

[U05-04] Climatic changes around 4,200 years BP in western Japan and eastern China: Potential influence on the introduction of paddy rice cultivation to Japan

★Invited Papers

*梶田 展人1,2,3,4,5伊左治 雄太2、加藤 凛太郎3、西倉 葉子4村山 雅史6大河内 直彦2、Yang Shouye7、Zheng Hongbo8、Wang Ke8,3、中西 利典9、佐々木 猛智3前田 歩3,4,5鈴木 淳5川幡 穂高3,4,5 (1.国立極地研究所地圏研究グループ、2.海洋研究開発機構生物地球化学センター、3.東京大学理学系研究科地球惑星科学専攻、4.東京大学大気海洋研究所、5.産業技術総合研究所地質調査総合センター、6.高知大学海洋コア研究センター、7.上海同済大学、8.雲南大学、9.ふじのくに地球環境史ミュージアム)

キーワード:完新世、稲作、4.2kaイベント

Climate change during the Holocene is thought to have had a significant impact on human migration and development. In Japan, the earliest prehistoric culture based on hunting and gathering began about 16,000 years ago (the Jomon era). At least 3,000 years ago, people with paddy rice cultivation skills migrated from mainland China, causing an explosion of population growth, lifestyle changes, and changes to the level of civilisation (the Yayoi era). To clarify the climatic changes that led to the movement of the Yayoi people to Japan, we analysed the palaeotemperature changes recorded in coastal marine sediment cores obtained from the Zhejiang coast in China, where the first paddy rice cultivation occurred, and northern Kyushu Island, where it was introduced to Japan. The reconstructed temperature fluctuations over the past 7,000 years from both sites were similar on the scale of hundreds to thousands of years. The cold periods that occurred approximately 300 and 4,200 years ago, which are related to the Little Ice Age and 4.2 ka events, respectively, may have been caused by modulations of the East Asian summer monsoon. Our study suggests that enhanced coastal upwelling may have amplified the cold climate of the 4.2 ka event on the Zhejiang coast. Our results support the recently proposed hypothesis that climate change prompted the collapse of the Yangtze civilisation and the migration of paddy rice farmers to other parts of Asia, including Japan. In contrast, the Jomon people, who still survived mainly based on hunting and gathering at that time, might have avoided a major population collapse. The differences in climatic changes and their possible impacts on human civilisations on both sides of the East China Sea can explain the migration-related population changes that have been observed in analyses of their DNA haplogroups.