快速干湿气候振荡与中国古代大规模社会动荡（英文）
作者机构：State Key Laboratory of Lake Science and Environment Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Department of Earth Science University of California Ministry of Education Key Laboratory of Surficial Geochemistry School of Earth Sciences and Engineering Nanjing University
出 版 物：《Science Bulletin》 (科学通报(英文版))
年 卷 期：2024年第3期
页 面：314-318页
核心收录：
学科分类：060204[历史学-中国古代史] 06[历史学] 07[理学] 070601[理学-气象学] 0706[理学-大气科学] 0602[历史学-中国史]
基 金：supported by the National Natural Science Foundation of China (42025707 and 41888101) the Strategic Priority Research Program of Chinese Academy of Sciences (XDB40010200) the Science and Technology Planning Project of Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences (NIGLAS2022TJ11) the Key Laboratory of Surficial Geochemistry,Ministry of Education,Nanjing University
摘 要：Climate conditions have long been acknowledged as a pivotal factor shaping regional productivity and influencing available resources,consequently playing an important role in driving social changes throughout human history [1-3].In ancient East Asia,the Chinese agrarian civilization emerged around 4000 years ago in northern China,the region termed theCentral Plains.This region faced recurrent episodes of large-scale social unrest,profoundly impacting the societal structure and dynastic cycles [4].These episodes were marked by extended civil peasant uprisings and/or incursions from northern nomadic tribes,often spanning decades to centuries [5].Both the agrarian societies in the Central Plains and the husbandry-based nomadic tribes in the vast northern grasslands,characterized by semi-arid and semi-humid climates,were notably sensitive to climate variations [6].
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