Zhang Haiwei, Cheng Hai, Sinha Ashish, Spötl Christoph, Cai Yanjun, Liu Bin, Kathayat Gayatri, Li Hanying, Tian Ye, Li Youwei, Zhao Jingyao, Sha Lijuan, Lu Jiayu, Meng Binglin, Niu Xiaowen, Dong Xiyu, Liang Zeyuan, Zong Baoyun, Ning Youfeng, Lan Jianghu, Edwards R Lawrence
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710054, China.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China.
Sci Adv. 2021 Nov 26;7(48):eabi9275. doi: 10.1126/sciadv.abi9275. Epub 2021 Nov 24.
The Liangzhu culture in the Yangtze River Delta (YRD) was among the world’s most advanced Neolithic cultures. Archeological evidence suggests that the Liangzhu ancient city was abandoned, and the culture collapsed at ~4300 years ago. Here, we present speleothem records from southeastern China in conjunction with other paleoclimatic and archeological data to show that the Liangzhu culture collapsed within a short and anomalously wet period between 4345 ± 32 and 4324 ± 30 years ago, supporting the hypothesis that the city was abandoned after large-scale flooding and inundation. We further show that the demise of Neolithic cultures in the YRD occurred within an extended period of aridity that started at ~4000 ± 45 years ago. We suggest that the major hydroclimatic changes between 4300 and 3000 years ago may have resulted from an increasing frequency of the El Niño–Southern Oscillation in the context of weakened Northern Hemisphere summer insolation.
长江三角洲地区的良渚文化是世界上最先进的新石器时代文化之一。考古证据表明,良渚古城在约4300年前被废弃,该文化也随之衰落。在此,我们结合中国东南部的洞穴沉积物记录以及其他古气候和考古数据,表明良渚文化在公元前4345 ± 32年至4324 ± 30年之间的一个短暂且异常湿润的时期内衰落,这支持了该城市在遭受大规模洪水和淹没后被废弃的假说。我们进一步表明,长江三角洲地区新石器时代文化的消亡发生在始于约4000 ± 45年前的一段长期干旱时期内。我们认为,公元前4300年至3000年之间主要的水文气候变化可能是由于在北半球夏季日照减弱的背景下,厄尔尼诺 - 南方涛动频率增加所致。