Ancient water wells reveal a prolonged drought in the lower Yellow River area about 2800 years ago

作     者：Shiyong Yu Xuexiang Chen Xiuling Liu Zhen Fang Junfeng Guo Senyang Zhan Hui Fang Fahu Chen 

作者机构：School of GeographyGeomaticsand PlanningJiangsu Normal UniversityXuzhou 221116China Joint International Research Laboratory for Environmental and Social Archaeology5handong Universityfinan 250100China Jinan Municipal Institute of Archaeologyjinan 250062China Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China 

出 版 物：《Science Bulletin》 (科学通报（英文版）)

年 卷 期：2018年第63卷第20期

页      面：1324-1327页

核心收录：

学科分类：07[理学] 

基　　金：supported by the start-up grant of Jiangsu Normal University the Chinese Program to Introduce Disciplinary Talents to Universities (111-2-09) 

主　　题：water wells drought Yellow River area 

摘      要：Proxy records from the North Atlantic realm reveal that large and rapid cooling known as the Bond events continued into the Holocene [1],repeatedly punctuating what is conventionally thought to have been a relatively stable climate.Given that the Holocene is the most recent interglacial period that has spurred the development of modern societies,scrutinizing climate variabil- ity during this period is important not only for predicting the trend of future climate changes,but also for better understanding the driving forces behind the rise and fall of ancient civilizations.