摘要
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.
| 源语言 | 英语 |
|---|---|
| 文章编号 | eabi9275 |
| 期刊 | Science Advances |
| 卷 | 7 |
| 期 | 48 |
| DOI | |
| 出版状态 | 已出版 - 11月 2021 |
联合国可持续发展目标
此成果有助于实现下列可持续发展目标:
-
可持续发展目标 13 气候行动
学术指纹
探究 'Collapse of the Liangzhu and other Neolithic cultures in the lower Yangtze region in response to climate change' 的科研主题。它们共同构成独一无二的指纹。引用此
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