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  2. 地质与地球物理研究所
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  4. 中国科学院新生代地质与环境重点实验室
Middle-Holocene sea-level fluctuations interrupted the developing Hemudu culture in the lower Yangtze River, China

文献类型：期刊论文

作者He, Keyang1,3; Lu, Houyuan1,2,3; Zheng, Yunfei4; Zhang, Jianping1,2; Xu, Deke1,2; Huan, Xiujia1,3; Wang, Jiehua5; Lei, Shao5
刊名QUATERNARY SCIENCE REVIEWS
出版日期2018-05-15
卷号188页码:90-103
关键词Cultural interruptions Sea-level fluctuations Rice domestication Middle-Holocene Hemudu culture Lower Yangtze river
ISSN号0277-3791
DOI10.1016/j.quascirev.2018.03.034
文献子类Article
英文摘要The eastern coastal zone of China is densely populated and widely recognized as a center of rice domestication, which has undergone dramatic sea-level fluctuation during the Holocene epoch. Hemudu culture is distributed mainly in the eastern coastal area and was once presumed as a mature agricultural economy based on rice, making it an ideal case for examining the remarkable human-environment interaction in the Lower Yangtze River. Though numerous studies have been conducted on the cultural evolution, ecological environment, and rice domestication of Hemudu culture, the impact of sea-level fluctuation on human settlement and food production remains controversial. In this study, we report high-resolution pollen, phytolith, and diatom records, and accurately measured elevation from the Yushan site, which is the closest site of Hemudu culture to the modern coastline. Based on the data gathered, we suggest that the Hemudu culture and subsequent Liangzhu culture developed in the context of regression and were interrupted by two transgressions that occurred during 6300-5600 BP and 5000-4500 BP. The regional ecological environment of the Yushan site alternated between intertidal mudflat and freshwater wetlands induced by sea-level fluctuations in the mid-late Holocene. Though rice was cultivated in the wetland as early as 6700 BP, this cultivation was subsequently discontinued due to the transgression; thus, full domestication of rice did not occur until 5600 BP in this region. Comprehensive analysis of multiple proxies in this study promote the understanding of the relationship between environmental evolution, cultural interruption, and rice domestication. (C) 2018 Elsevier Ltd. All rights reserved.
WOS关键词EAST CHINA ; ENVIRONMENTAL-CHANGE ; HUMAN SETTLEMENT ; COASTAL ZONES ; RICE DOMESTICATION ; POLLEN MORPHOLOGY ; CULTIVATED RICE ; NINGSHAO PLAIN ; CLIMATE-CHANGE ; DELTA
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000432770600008
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Basic Research Program of China(2015CB953801) ; National Basic Research Program of China(2015CB953801) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; National Natural Science Foundation of China(41430103) ; National Natural Science Foundation of China(41430103) ; National Basic Research Program of China(2015CB953801) ; National Basic Research Program of China(2015CB953801) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; National Natural Science Foundation of China(41430103) ; National Natural Science Foundation of China(41430103) ; National Basic Research Program of China(2015CB953801) ; National Basic Research Program of China(2015CB953801) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; National Natural Science Foundation of China(41430103) ; National Natural Science Foundation of China(41430103) ; National Basic Research Program of China(2015CB953801) ; National Basic Research Program of China(2015CB953801) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; "Macroevolutionary Processes and Paleoenvironments of Major Historical Biota" of the Chinese Academy of Sciences(XDPB0503) ; National Natural Science Foundation of China(41430103) ; National Natural Science Foundation of China(41430103)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88238]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者He, Keyang; Lu, Houyuan
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Zhejiang Prov Inst Cultural Rel & Archaeol, Hangzhou 310014, Zhejiang, Peoples R China
5.Ningbo Municipal Inst Cultural Rel & Archaeol, Ningbo 315012, Zhejiang, Peoples R China
推荐引用方式
GB/T 7714		 He, Keyang,Lu, Houyuan,Zheng, Yunfei,et al. Middle-Holocene sea-level fluctuations interrupted the developing Hemudu culture in the lower Yangtze River, China[J]. QUATERNARY SCIENCE REVIEWS,2018,188:90-103.
APA He, Keyang.,Lu, Houyuan.,Zheng, Yunfei.,Zhang, Jianping.,Xu, Deke.,...&Lei, Shao.(2018).Middle-Holocene sea-level fluctuations interrupted the developing Hemudu culture in the lower Yangtze River, China.QUATERNARY SCIENCE REVIEWS,188,90-103.
MLA He, Keyang,et al."Middle-Holocene sea-level fluctuations interrupted the developing Hemudu culture in the lower Yangtze River, China".QUATERNARY SCIENCE REVIEWS 188(2018):90-103.

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来源：地质与地球物理研究所

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