必须声明标量变量 "@Script_ID"。 福建仙云洞石笋记录的Termination I事件缓变特征-《地球科学与环境学报》
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[1]马乐,肖海燕,张鑫,等.福建仙云洞石笋记录的Termination I事件缓变特征[J].地球科学与环境学报,2019,41(05):604-612.
 MA Le,XIAO Hai-yan,ZHANG Xin,et al.Gradual Changes of the Termination I Inferred from Stalagmite Records in Xianyun Cave of Fujian, China[J].Journal of Earth Sciences and Environment,2019,41(05):604-612.

福建仙云洞石笋记录的Termination I事件缓变特征(PDF)




Gradual Changes of the Termination I Inferred from Stalagmite Records in Xianyun Cave of Fujian, China
(1. 福建师范大学 地理科学学院,福建 福州 350007; 2. 福建师范大学 湿润亚热带生态地理过程 教育部重点实验室,福建 福州 350007; 3. 福建师范大学 地理研究所,福建 福州 350007)
MA Le1 XIAO Hai-yan1 ZHANG Xin1 JIANG Xiu-yang123* CAI Bing-gui123
(1. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, Fujian, China; 2. Key Laboratory of Humid Subtropical Eco-geographical Processes of Ministry of Education, Fujian Normal University, Fuzhou 350007, Fujian, China; 3. Institute of Geography, Fujian Normal University, Fuzhou 350007, Fujian, China)
Termination I事件 东亚季风 石笋 转型特征 区域差异 驱动机制 仙云洞 福建
Termination I East Asian monsoon stalagmite transitional characteristic regional difference driving mechanism Xianyun cave Fujian
末次冰期终止事件(Termination I,简称TI)是发生在末次冰消期约14.7 ka B.P.北半球最显著的一次快速升温事件,其气候突变的全球响应及转型特征是末次冰消期研究的重点。基于中国东南地区福建西部仙云洞两支石笋(样品编号为XY11和XYⅢ-21)17个高精度230Th年龄和567个氧同位素数据,建立了12.67~16.10 ka B.P.时段内平均分辨率达十年际的东亚夏季风强度演变序列,捕捉到了Termination I转型缓变特征。仙云洞石笋记录揭示Termination I事件缓变特征持续时间达800 a,明显比也门(约13 a)以及中国西南地区(约35 a)和长江中下游地区(约200 a)石笋记录的转型时间长很多,存在显著的区域差异。仙云洞石笋记录的Termination I转型时段季风开始增强响应于北高纬气候,但仙云洞石笋记录的Termination I缓变特征指示其可能受到热带低纬西太平洋暖池水文循环过程的影响。
The Termination I(TI)is the most significant abrupt warming event in the northern hemisphere during the last deglaciation of about 14.7 ka B.P., and its transitional characteristics and global response to climate change are the focus of the research. Based on 17 high-resolution 230Th ages and 567 oxygen isotope data from two stalagmites(XY11 and XYⅢ-21)in Xianyun cave of western Fujian, southeastern China, the East Asian summer monsoon intensity evolution sequence with an average resolution of ten years covering the period of 12.67-16.10 ka B.P. was established. It is characterized by slow transitional process over 800 a, which is much longer than that in Yemen(~13 a), the southwestern China(~35 a)and the middle-lower reaches of Yangtze River, China(~200 a), showing obvious regional differences. The onset of intensified monsoon mainly responses to the north high latitude climate during the Termination I inferred from stalagmite records in Xianyun cave. The slow transitional characteristic implies that the hydrology processes over the tropical low latitude West Pacific warm pool may exert significant impact on the monsoon climate.


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收稿日期:2019-04-25; 修回日期:2019-05-28投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41672170); 福建省自然科学基金项目(2017J01654); 福建省高校新世纪优秀人才支持计划项目
作者简介:马 乐(1995-),男,山西孝义人,理学硕士研究生,E-mail:1372350526@qq.com。
更新日期/Last Update: 2019-09-19