| Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts | |
Chen, Jinxia1,3; Nan, Qingyun2,3; Li, Tiegang1,3 ; Sun, Rongtao4; Sun, Hanjie2,3; Lu, Jian2,3
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| 2019-09-01 | |
| Source Publication | JOURNAL OF ASIAN EARTH SCIENCES
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| ISSN | 1367-9120 |
| Volume | 181Pages:12 |
| Corresponding Author | Nan, Qingyun(nanqingyun@qdio.ac.cn) |
| Abstract | Changes in paleoenvironments from 3500 to 1300 cal. yr BP have been documented by a high-resolution grain-size and organic carbon isotope record in core Z8 from the Shandong mud wedge in the southern Yellow Sea (YS). The sensitive grain-size component, sorting coefficients and delta C-13(org) values were used to identify the paleohydrologic variations and the intensity of the East Asian winter monsoon (EAWM). The coarse fraction of sediment, together with organic isotope and sea surface temperature (SST) data, shows a weak EAWM during 3500-2300 cal. yr BP, a gradual increase in the EAWM from 2300 to 1700 cal. yr BP and an enhanced EAWM since 1700 cal. yr BP. Superimposed on this general trend, several prominent short-lived strong EAWM episodes peaked at approximately 3300, 3100, 2900, 2750, 2620, 2220, 1900, 1700 and 1400 cal. yr BP. The paleoenvironmental record matches ancient Chinese historical climate records as well as socioeconomic changes, with lower economic levels occurring during stronger EAWM episodes. The results show that prosperous stages of ancient Chinese dynasties mainly occurred in weak EAWM periods, while collapses and/or changes in ancient Chinese dynasties generally occurred during cold periods with a strong EAWM. We suggest that the persistent short-lived strengthening of the EAWM could have exerted a remarkable influence on ancient agricultural societies through decreases in both winter temperature and monsoonal precipitation. |
| Keyword | Grain size Organic carbon Isotope East Asian winter monsoon Ancient Chinese dynasties Yellow Sea |
| DOI | 10.1016/j.jseaes.2019.103912 |
| Indexed By | SCI |
| Language | 英语 |
| Funding Project | National Natural Science Foundation of China[41576054] ; National Natural Science Foundation of China[41830539] ; Shandong Provincial Natural Science Foundation, China[ZR2016DM12] ; National Natural Science Foundation of China[41576054] ; National Natural Science Foundation of China[41830539] ; Shandong Provincial Natural Science Foundation, China[ZR2016DM12] |
| WOS Research Area | Geology |
| WOS Subject | Geosciences, Multidisciplinary |
| WOS ID | WOS:000482496600010 |
| Publisher | PERGAMON-ELSEVIER SCIENCE LTD |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.qdio.ac.cn/handle/337002/162784 |
| Collection | 海洋地质与环境重点实验室 |
| Corresponding Author | Nan, Qingyun |
| Affiliation | 1.SOA, Key Lab Marine Sediment Logy & Environm Geol, Inst Oceanog 1, Qingdao 266061, Shandong, Peoples R China 2.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Shandong, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Shandong, Peoples R China 4.Shandong Univ Technol, Sch Resources & Environm Engn, Zibo, Peoples R China |
| Corresponding Author Affilication | Institute of Oceanology, Chinese Academy of Sciences |
| Recommended Citation GB/T 7714 | Chen, Jinxia,Nan, Qingyun,Li, Tiegang,et al. Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,181:12. |
| APA | Chen, Jinxia,Nan, Qingyun,Li, Tiegang,Sun, Rongtao,Sun, Hanjie,&Lu, Jian.(2019).Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts.JOURNAL OF ASIAN EARTH SCIENCES,181,12. |
| MLA | Chen, Jinxia,et al."Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts".JOURNAL OF ASIAN EARTH SCIENCES 181(2019):12. |
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| Chen-2019-Variations（3248KB） | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | View | |
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