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重庆金佛洞石笋记录的410 ka弱季风事件

许奕滨 杨勋林 袁道先 胡明广 葛晓艳 龚萌

中国岩溶2024,Vol.43Issue(2):219-238,20.
中国岩溶2024,Vol.43Issue(2):219-238,20.DOI:10.11932/karst2024y019

重庆金佛洞石笋记录的410 ka弱季风事件

410 ka weak monsoon event recorded by stalagmites in Jinfo Cave of Chongqing

许奕滨 1杨勋林 2袁道先 3胡明广 1葛晓艳 1龚萌1

作者信息

  • 1. 西南大学地理科学学院/重庆金佛山喀斯特生态系统国家野外科学观测研究站,重庆 400715
  • 2. 西南大学地理科学学院/重庆金佛山喀斯特生态系统国家野外科学观测研究站,重庆 400715||重庆岩溶环境开放实验室,重庆 400715||自然资源部岩溶生态环境—重庆南川野外基地,重庆 400715
  • 3. 西南大学地理科学学院/重庆金佛山喀斯特生态系统国家野外科学观测研究站,重庆 400715||重庆岩溶环境开放实验室,重庆 400715||中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室,广西桂林 541004
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摘要

Abstract

The freshwater discharge from melting ice sheets in the deglaciation or glaciation is prone to anomalies in ocean-atmosphere transport between different latitudes,which can lead to a series of abrupt millennial-scale climate events,either obvious or not,such as the Younger Dryas(YD)events and YD-like events.Marine Isotope Stage 11c(MIS 11c)serves as one of the best references for the current Holocene,and the studies of possible YD-like events and their triggering mechanisms during Holocene are conducive to the understanding of the occurrence pattern of extreme climate events.In this paper,the results of the study on the J33 δ18O sequence records of stalagmites in Jinfo Cave,Chongqing,are shown:(1)Stalagmites in the Asian monsoon climate zone reveal a millennial-scale weak monsoon event that occurred around 410 ka BP prior to the Glacial Maximum of MIS 11 interglacial period.(2)Both the 410 ka weak monsoon event and the YD event occurred during the gradual strengthening of the monsoon and ascending branch of summer insolation in the Northern Hemisphere prior to the Glacial Maximum of interglacial period.This was also a time when Atlantic Meridional Overturning Circulation(AMOC)disturbance occurred.The duration,internal structure,and pattern of the events were similar,with differences in the change magnitude and ice volume conditions.(3)The weak monsoon event that occurred in 410 ka BP was primarily influenced by the combined effects of insolation and AMOC.This event was characterized by a sustained warming process that accelerated the melting of the Greenland ice sheet,leading to the destabilization of this ice sheet.The continuous flowing of freshwater into the North Atlantic resulted in a short-lived AMOC oscillation.The weakening of the AMOC resulted in a cold anomaly over the North Atlantic.As a result of atmospheric telecorrelation,the weaker AMOC led to a weaker Asian Summer Monsoon(ASM)

关键词

亚洲夏季风/MIS 11c/石笋δ18O/弱季风事件/金佛洞/中国西南

Key words

Asian Summer Monsoon/MIS 11c/stalagmite δ18O/weak monsoon event/Jinfo Cave/Southwest China

分类

天文与地球科学

引用本文复制引用

许奕滨,杨勋林,袁道先,胡明广,葛晓艳,龚萌..重庆金佛洞石笋记录的410 ka弱季风事件[J].中国岩溶,2024,43(2):219-238,20.

基金项目

国家自然科学基金项目(41971109,41572158) (41971109,41572158)

国家重点研发计划子课题项目(2016YFC0502301-1) (2016YFC0502301-1)

中国岩溶

OA北大核心CSTPCD

1001-4810

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