中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 中国科学院新生代地质与环境重点实验室
Role of the mid-Holocene environmental transition in the decline of late Neolithic cultures in the deserts of NE China

文献类型：期刊论文

作者Guo, Licheng1,2,3; Xiong, Shangfa1,2,3; Ding, Zhongli1,2,3; Jin, Guiyun4; Wu, Jiabin1,2,3; Ye, Wei5
刊名QUATERNARY SCIENCE REVIEWS
出版日期2018-06-15
卷号190页码:98-113
关键词Mid-Holocene environmental transition Archaeological sites Neolithic cultures Monsoon Desert China
ISSN号0277-3791
DOI10.1016/j.quascirev.2018.04.017
文献子类Article
英文摘要The mid-Holocene environmental transition was characterised by global cooling and the abrupt weakening of the Northern Hemisphere monsoon systems. It is generally considered the key driver of the collapse of several mid-Holocene agricultural societies, on a global scale. However, only a few previous studies have tried to verify the climatic origin of the collapse of these societies, using the compilation of spatiotemporal data at a large scale. Especially, the nature of mid-Holocene human-environment interactions in the climatically-sensitive margin of the East Asian summer monsoon front remains to be thoroughly understood. However, a systematic compilation of archaeological data at a regional scale can be used to verify the role the mid-Holocene environmental transition played in the collapse of late Neolithic cultures in China. Here, we present a regional compilation of Holocene records from sub-aerial sedimentary deposits, lake sediments, and archaeological sites in the deserts of NE China and the adjacent regions to explore human-environment interactions during the mid-Holocene. Comparison of the records of Holocene climate change with the evolution of archaeological sites reveals that the mid Holocene environmental transition resulted in ecosystem degradation in the deserts of NE China, rendering these areas much less habitable. Faced with substantially increased environmental pressures, the late Neolithic inhabitants used several subsistence strategies to adapt to the environmental transition, including change in agricultural practices and ultimately migration. Overall, our results support the view that a widespread mid-Holocene drought destroyed the rain-fed agricultural and/or plant-based subsistence economies, ultimately contributing to the collapse of late Neolithic cultures in NE China. (C) 2018 Elsevier Ltd. All rights reserved.
WOS关键词ASIAN SUMMER MONSOON ; HOLOCENE CLIMATE-CHANGE ; INNER-MONGOLIA PLATEAU ; CAL. YR BP ; AFRICAN HUMID PERIOD ; MULTI-PROXY RECORD ; DALI-NOR AREA ; NORTHERN CHINA ; BRONZE-AGE ; ARCHAEOLOGICAL SITES
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000435050400008
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构"Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDA19050104 ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Key R&D Program of China(2017YFA0603404) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; National Nature Science Foundation of China(41272206) ; XDPB0503) ; XDPB0503) ; XDPB0503) ; XDPB0503)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88201]  
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Guo, Licheng; Xiong, Shangfa
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
4.Shandong Univ, Inst Cultural Heritage, Dept Archaeol, Jinan 250100, Shandong, Peoples R China
5.Zhejiang Normal Univ, Coll Geog & Environm Sci, Jinhua 321004, Peoples R China
推荐引用方式
GB/T 7714		 Guo, Licheng,Xiong, Shangfa,Ding, Zhongli,et al. Role of the mid-Holocene environmental transition in the decline of late Neolithic cultures in the deserts of NE China[J]. QUATERNARY SCIENCE REVIEWS,2018,190:98-113.
APA Guo, Licheng,Xiong, Shangfa,Ding, Zhongli,Jin, Guiyun,Wu, Jiabin,&Ye, Wei.(2018).Role of the mid-Holocene environmental transition in the decline of late Neolithic cultures in the deserts of NE China.QUATERNARY SCIENCE REVIEWS,190,98-113.
MLA Guo, Licheng,et al."Role of the mid-Holocene environmental transition in the decline of late Neolithic cultures in the deserts of NE China".QUATERNARY SCIENCE REVIEWS 190(2018):98-113.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。