Articles | Volume 20, issue 6
https://doi.org/10.5194/cp-20-1401-2024
https://doi.org/10.5194/cp-20-1401-2024
Research article
 | 
27 Jun 2024
Research article |  | 27 Jun 2024

A series of climate oscillations around 8.2 ka revealed through multi-proxy speleothem records from North China

Pengzhen Duan, Hanying Li, Zhibang Ma, Jingyao Zhao, Xiyu Dong, Ashish Sinha, Peng Hu, Haiwei Zhang, Youfeng Ning, Guangyou Zhu, and Hai Cheng

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Latest update: 05 Jun 2025
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Short summary
We use multi-proxy speleothem records to reveal a two droughts–one pluvial pattern during 8.5–8.0 ka. The different rebounded rainfall quantity after two droughts causes different behavior of δ13C, suggesting the dominant role of rainfall threshold on the ecosystem. A comparison of different records suggests the prolonged 8.2 ka event is a globally common phenomenon rather than a regional signal. The variability of the AMOC strength is mainly responsible for these climate changes.
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