A review of 6000-5000 cal BP climatic anomalies in China
文献类型：期刊论文
| 作者 | Hou, Mei1,2,3; Wu, Wen Xiang1,3 |
| 刊名 | QUATERNARY INTERNATIONAL
 |
| 出版日期 | 2021-01-10 |
| 卷号 | 571页码:58-72 |
| 关键词 | 6000-5000 cal BP climatic anomalies China Proxy records Asia summer monsoon Forcing mechanisms |
| ISSN号 | 1040-6182 |
| DOI | 10.1016/j.quaint.2020.12.004 |
| 通讯作者 | Wu, Wen Xiang(wuwx@igsnrr.ac.cn) |
| 英文摘要 | Studies of the abrupt climate events that punctuated the warm Holocene epoch allow us to understand the climate system, forecast future climate change, and interpret the cultural transformations. Paleoclimate records around the world show manifestations of prominent climate anomalies between 6000 and 5000 calibrated years before present (cal BP). However, a comprehensive review of these anomalies remains unavailable in China. In this article, we collected, compiled, and analyzed proxy climate evidence from 49 sites recorded by a variety of natural archives, including lacustrine sequences, speleothems, peat profiles, an ice core, and marine sediments, to document these changes. Our synthesis results indicate that pronounced climatic anomalies generally characterized by cold and dry conditions occurred during 6000-5000 cal BP, which were associated with weakening of the Asian summer monsoon. However, these anomalies show a lack of absolute synchronicity or equality by various proxy records because of the different proxy sensitivities and/or dating uncertainties. Such 6000-5000 cal BP climatic anomalies also have possible equivalents in proxy records from various regions around the world. Comparison of paleoclimate records with climate forcing time series suggests that both the reduced solar activity and a long-term trend of orbitally-driven insolation change are the main driving mechanisms for these short-lived climate changes. More quantitative and higher-resolution palaeoclimatic reconstructions are needed to fully capture the magnitude, timing, and mechanism of the 6000-5000 cal BP climatic anomalies. |
| WOS关键词 | EAST-ASIAN MONSOON ; INDIAN-SUMMER MONSOON ; INTERTROPICAL CONVERGENCE ZONE ; NORTHEASTERN INNER-MONGOLIA ; NORTH-ATLANTIC CLIMATE ; BASIN WESTERN TIBET ; ICE CORE RECORDS ; HIGH-RESOLUTION ; HOLOCENE VEGETATION ; LATEST PLEISTOCENE |
| 资助项目 | National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41672176] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA20040201] |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000612111700002 |
| 出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
| 资助机构 | National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/160597]  |
| 专题 | 中国科学院地理科学与资源研究所 |
| 通讯作者 | Wu, Wen Xiang |
| 作者单位 | 1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China |
| 推荐引用方式 GB/T 7714 | Hou, Mei,Wu, Wen Xiang. A review of 6000-5000 cal BP climatic anomalies in China[J]. QUATERNARY INTERNATIONAL,2021,571:58-72. |
| APA | Hou, Mei,&Wu, Wen Xiang.(2021).A review of 6000-5000 cal BP climatic anomalies in China.QUATERNARY INTERNATIONAL,571,58-72. |
| MLA | Hou, Mei,et al."A review of 6000-5000 cal BP climatic anomalies in China".QUATERNARY INTERNATIONAL 571(2021):58-72. |
入库方式： OAI收割
来源：地理科学与资源研究所
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