globalchange  > 气候减缓与适应
DOI: 10.1016/j.quascirev.2018.03.034
Scopus记录号: 2-s2.0-85045049442
论文题名:
Middle-Holocene sea-level fluctuations interrupted the developing Hemudu culture in the lower Yangtze River, China
作者: He K.; Lu H.; Zheng Y.; Zhang J.; Xu D.; Huan X.; Wang J.; Lei S.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 188
起始页码: 90
结束页码: 103
语种: 英语
英文关键词: Cultural interruptions ; Hemudu culture ; Lower Yangtze river ; Middle-Holocene ; Rice domestication ; Sea-level fluctuations
Scopus关键词: Coastal zones ; Cultivation ; Ecology ; Rivers ; Wetlands ; Cultural interruptions ; Holocenes ; Lower yangtze rivers ; Rice domestication ; Sea-level fluctuations ; Sea level ; agricultural economics ; agricultural history ; coastal zone ; cultural change ; diatom ; domestication ; food production ; Holocene ; human settlement ; palynology ; phytolith ; rice ; sea level change ; China ; Yangtze River ; Yushan Island ; Zhejiang ; Bacillariophyta
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. © 2018 Elsevier Ltd
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被引频次[WOS]:62   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112212
Appears in Collections:气候减缓与适应

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作者单位: Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Centre for Excellence in Tibetan Plateau Earth Science, Chinese Academy of Sciences, Beijing, 100101, China; University of Chinese Academy of Sciences, Beijing, 100049, China; Zhejiang Provincial Institute of Cultural Relics and Archaeology, Hangzhou, 310014, China; Ningbo Municipal Institute of Cultural Relics and Archaeology, Ningbo, 315012, China

Recommended Citation:
He K.,Lu H.,Zheng Y.,et al. Middle-Holocene sea-level fluctuations interrupted the developing Hemudu culture in the lower Yangtze River, China[J]. Quaternary Science Reviews,2018-01-01,188
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