方一帆^1,2,3,,
刘树双^1,2,3,
邹凌哲^1,2,3,
刘殿兵^1,2,3,,
1. 南京师范大学地理科学学院, 江苏 南京 210023
2. 虚拟地理环境教育部重点实验室(南京师范大学), 江苏 南京 210023
3. 江苏省地理信息资源开发与利用协同创新中心, 江苏 南京 210023

基金项目: 国家自然科学基金面上项目（批准号：41672161）资助


详细信息

作者简介: 方一帆, 女, 24岁, 硕士研究生, 自然地理学专业, E-mail:fyifan0810@163.com

通讯作者: 刘殿兵, E-mail:ldb9921@njnu.edu.cn

中图分类号: P597⁺.2;P532

收稿日期:2020-01-21
修回日期:2020-04-29
刊出日期:2020-07-30

Regional characteristics of abrupt monsoon changes in late MIS3 and its global significance

Fang Yifan^1,2,3,,
Liu Shushuang^1,2,3,
Zou Lingzhe^1,2,3,
Liu Dianbing^1,2,3,,
1. School of Geography, Nanjing Normal University, Nanjing 210023, Jiangsu
2. Key Laboratory of Virtual Geographic Environment(Nanjing Normal University), Ministry of Education, Nanjing 210023, Jiangsu
3. Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, Jiangsu


More Information

Corresponding author: Liu Dianbing,E-mail:ldb9921@njnu.edu.cn

MSC: P597⁺.2;P532

--> Received Date: 21 January 2020
Revised Date: 29 April 2020
Publish Date: 30 July 2020


摘要
摘要:末次冰期晚期短尺度气候突变事件异常显著，对其研究有助于认识相似边界条件下气候突变规律。通过MIS3晚期亚洲季风区8支石笋记录总结分析发现，因受洞穴微环境、渗水通道、生长动力等影响，DO5~DO3事件振幅差最大可达0.9 ‰，持续时间差最大达到900年，这可能反映局地环境对同一气候信号的改造作用或与各记录分辨率及测年精度有关。同时，统计分析发现，这些短尺度DO事件具有一定相似性，其持续时间集中分布于特定范围，说明石笋同位素信号在某种程度上可以反映真实气候信号。高、低纬记录对比显示，石笋记录与低纬气候信号呈现诸多相似性，反映亚洲季风区石笋记录具有显著的"低纬特色"。因此，无论亚洲季风突变的"开关"是否归因于北高纬气候，低纬过程确实是不可或缺的"塑造者"。
关键词: MIS3晚期/
石笋/
短尺度DO事件/
差异性分析/
全球联系

Abstract:In this study, eight stalagmite δ¹⁸O records were chosen from seven caves from the Asian Summer Monsoon (ASM) region. The geographical location of these cave sites ranges from 26°N to 33°N, and 105°E to 120°E, with a sufficient spatial coverage. From north to south, sample MSD is from Hulu Cave (32°30'N, 119°10'E), XR025 from Xianren Cave (32°24'N, 107°10'E), SB46 from Sanbao Cave (31°40'N, 110°26'E), YX51 from Yongxing Cave (31°35'N, 111°14'E), QT15 from Qingtian Cave (31°20'N, 110°22'E), DSB3 from Dashibao Cave (26°05'N, 105°03'E), Wu3 and Wu32 from Wulu Cave (26°03'N, 105°05'E). Apparently, site-specific karstic conditions, microclimate, soil cover and vegetation types, etc., are strikingly different at these sites, probably inducing contrasting expressions of regional climate events. These stalagmite records, mainly spanning the late MIS3 (34~27 ka B.P.), are characterized by high-resolution data and precisely-constrained chronologies, which are suitable for detecting the internal structure of short-lived abrupt ASM changes. Generally, in our studied interval, the chronologies of these records were constrained by more than three U/Th dating results, with dating uncertainties of less than 200 years. Sampling resolution is better than 40 years or even 5 years on QT15. Millennial-scale climate events in these stalagmite records, include Dansgaard-Oeschger (DO) 5 to DO3 and Heinrich event (H) 3. Regardless of the observed resemblance between DO events, regional differences can be observed in amplitude and duration. By statistical analysis, a deviation of 0.7 ‰ in amplitude and 400 years in duration was estimated between different records. To some degree, different microclimates, karstic and environmental conditions can result in these contrasting estimations. At the same time, most (over 60%) of calculated values fall within a narrow envelope, suggesting that DO events from these stalagmite records more likely reflect a true climate signal. δ¹⁸O records of samples Wu3 from Wulu Cave, Southern China and SB46 from Sanbao Cave, Central China can be a template for these abrupt ASM changes in the late MIS3.
When compared with high-and low-latitude records, the timing and frequency of ASM changes agree well with Greenland temperature variations. In detail, a high level of ASM intensity and a gradual ASM rise are evident during Stadial 5 (between DO5.1 and DO4.1) and late H3, respectively, significantly different from Greenland temperature. Such ASM response is further supported by the ice-core Ca²⁺ record, during which Asian winter monsoon broadly weakened. Hence, a negative correlation can be expected between Asian summer and winter monsoons. The atmospheric CH₄ concentration, believed to represent tropical wetlands, however, exhibits a detailed structure similar to Greenland temperature changes during Stadial 5 and H3. It is possible that a southern hemispheric source is important for CH₄ changes during cooling episodes. At the tropical Atlantic, the sediment reflectance from Cariaco Basin shows a striking resemblance to ASM variability, including those during Stadial 5 and late H3. Consequently, millennial-scale ASM variability is intimately linked to thermal and hydrological activities in low latitudes, although the initial trigger might be attributed to that around the North Atlantic.
Key words:late MIS3/
stalagmites/
short-lived DO events/
regional disparity/
global teleconnection



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