ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
贵州荔波1200年来石笋高分辨率的古气候环境记录
  
关键词:stalagmite  age dating of ICP-MS  high resolution  paleoclimate environment  Longquan Cave in Libo  Guizhou Province
基金项目:国家自然科学基金项目(编号: 90511004 和40772216)、科技部所控项目(编号:200903)和岩溶动力学重点实验室(编号:桂科能0842008)及岩溶动力系统与碳循环(编号:1212010911062)
作者单位E-mail
张美良 中国地质科学院岩溶地质研究所岩溶动力学重点实验室中国地质大学地球科学与资源学院 mlzh@karst.edu.cn 
朱晓燕 中国地质科学院岩溶地质研究所岩溶动力学重点实验室  
程海 美国明尼苏达大学地质与地球物理系  
林玉石 中国地质科学院岩溶地质研究所岩溶动力学重点实验室  
覃嘉铭 中国地质科学院岩溶地质研究所岩溶动力学重点实验室  
冉景丞 贵州荔波茂兰喀斯特国家自然保护管理局  
王华 中国地质科学院岩溶地质研究所岩溶动力学重点实验室  
何师意 中国地质科学院岩溶地质研究所岩溶动力学重点实验室  
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摘要:
A High Resolution Paleoclimate Record of the Last 1,200 Years in Stalagmite L2 from the Longquan Cave, Guizhou Province
      The time sequence of high resolution paleoclimatic change since 1200 a BP was reconstructed by age dating of the high precision ICP-MS-230Th-U series and an analysis of stable isotopes for a stalagmite of Longquan Cave in Libo, Guizhou. The results show that the monsoon climate from stalagmite L2 record since 1200 a BP has experienced eight stages, i.e., the warm stage of 1200~1100 a BP, the cold stage of 1100~940 a BP, the warm stage of 940~840 a BP, the cold stage of 840~700 a BP, the warm stage of 700~450 a BP, the cold stage of 450~300 a BP, the warm stage of 300~200 a BP and the cold stage of 200~70 a BP on the century time scale of dry-humid and cold-warm changes. In addition, a series of decade time scales of climate changes were superimposed on the century time scale of monsoon climate undulation. The records from stalagmite L2 reveal the instability of the climate of the East Asian monsoon and the periodical change since 1200 a BP. Being very similar to ice core records, the climate changes suggest that the century time scale of the monsoon climate changes from stalagmite records in the low latitude region has a wonderful correlation with the climate change in the high latitude region and the Arctic pole, and that the monsoon rainfall of the century time scale stalagmite record is mainly driven and controlled by the solar action and radiation. Moreover, the rainfall or drought events of the East Asian monsoon are closely related to the solar radiation intensity. The understanding of the changes of modern climate systems is of important scientific significance in forecasting the driving mechanism of climatic evolution in future.
ZHANG Mei-liang,ZHU Xiao-yan,CHENG Hai,LIN Yu-shi,QIN Jia-ming,RAN Jing-cheng,WANG Hua,HE Shi-yi.2009.A High Resolution Paleoclimate Record of the Last 1,200 Years in Stalagmite L2 from the Longquan Cave, Guizhou Province[J].Acta Geoscientica Sinica,30(6):831-840.
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