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Spatial and temporal distribution of Neolithic sites in coastal China:Sea level changes, geomorphic evolution and human adaption

查看全文 作  者:ZHENG [1]HongBo;ZHOU [2]YouSheng;YANG [1,2]Qing;HU [2]ZhuJun;LING [2]GuangJiu;ZHANG [3]JuZhong;GU [3]ChunGuang;WANG [2]YingYing;CAO [2]YeTing;HUANG [2]XianRong;CHENG [2]Yue;ZHANG [2]XiaoYu;WU [4]WenXiang 高影响力作者 机构地区:[1]Research Center for Earth System Science, Yunnan University;[2]School of Geography Science, Nanjing Normal University;[3]Department for the History of Science and Scientific Archaeology, University of Science and Technology of China;[4]Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences高影响力机构 出  处:《Science China Earth Sciences》索引2018年第61卷第2期,共11页高影响力期刊 基  金:supported by the National Basic Research Program of China (Grant No. 2015CB953803);the National Natural Science Foundation of China (Grant No. 41672344);the CAS Strategic Priority Research Program (Grant No. XDB03020301) 摘  要:The East China coastal plain is one of the most important Neolithic culture areas in China, where rich archaeological sites including those producing the earliest domesticated rice are observed. It is also a place where landscape has experienced dramatic evolution during the Holocene when both sea level and climate changed, such that it is an ideal place for studying human-environment interaction. This study investigated over 2000 sites of pre-history and Shang and Zhou Dynasties, with 655 of which being Neolithic ages, by using DEM and GIS methods. The results suggest that the spatial and temporal distribution of Neolithic sites has largely been controlled by landscape evolution(particularly changes in coastal line), which ultimately governed by sea level changes. During early Holocene, Neolithic sites sparsely distributed in the intermountain basins of east Zhejiang Province, far from the influence of ocean. Over the period of 9–7 ka, the coastal plain(including the shelf) was largely submerged,only the feet of low hills to the south and southwest of the study area, and islands protruding the estuary, cradled limited number of settlements with characteristic 'maritime components'. At about 7 ka, sea level rise decelerated prominently, while sediments supply in the drainage remained high value, the combination of which led to land formation and propagation. Vast space during this period facilitated the growth of settlements in both size and number. In the mean time, however, the coastal plain was vulnerable to extreme environmental events such as storms and flooding owning to its geomorphic nature, which exerted great influence on the rise and fall of Neolithic culture. 关 键 词:水平变化 地球形状 地点 沿海 空间 时间 进化 中国
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