globalchange  > 气候变化与战略
CSCD记录号: CSCD:5553539
论文题名:
MIS 5c向MIS 5b转换期亚洲夏季风的演变特征万象洞石笋记录
其他题名: THE EVOLUTION OF ASIAN SUMMER MONSOON DURING MIS 5c~5b FROM A STALAGMITE RECORD IN WANXIANG CAVE
作者: 王晓锋1; 张平中1; 周鹏超1; 白益军1; 程海2
刊名: 第四纪研究
ISSN: 1001-7410
出版年: 2015
卷: 35, 期:6, 页码:1398-1410
语种: 中文
中文关键词: 万象洞 ; 石笋delta~(18)O ; 亚洲季风
英文关键词: MIS 5c ; stalagmite ; MIS 5c~5b ; Wanxiang Cave ; D/O 23 ; Asian summer monsoon
WOS学科分类: GEOLOGY
WOS研究方向: Geology
中文摘要: 根据亚洲季风边缘区武都万象洞一根长360mm石笋(WX0541A)的6个~(230)Th年代和个delta~(18)O数据,建立了104107~91858a B.P.期间高分辨率和高精度亚洲夏季风变迁的时间序列。通过与中国东部季风腹地湖北三宝洞和现代西风控制区新疆科桑洞的石笋delta~(18)O记录对比发现,三者的变化模式在研究时段内具有相似性。其中,3个洞穴石笋同位素在MIS 5c中期相当于Greenland D/O 23暖阶段的偏负阶段,从南到北显示出逐渐偏负的趋势,是季风降水大陆效应的真实反映;而在96495~92562a B.P.之间的同位素偏重阶段,万象洞和科桑洞石笋同位素组成相近并偏正于三宝洞石笋的delta~(18)O值,偏离了亚洲夏季风的内陆入侵规律,可能与MIS 5b太阳辐射降低时期万象洞和科桑洞地区可变的季节性降水或加入的西风降水有关。
英文摘要: The main purpose of the past global climate change research is to provide reference for the prediction and simulation of future related study. Asian monsoon system, impacts the monsoon region humanity's livelihood and the agricultural development through the interaction of ocean-land-atmosphere,is an important part of the global climate system. Especially, most of the population and agricultural areas in our country are distributed in the monsoon region, the amount of monsoon rainfall is related to all aspects of the national economy and people's livelihood. Hence,the intensity of monsoon forecast will be very urgent and necessary. Here, we present a 360mm-long stalagmite (WX0541A) obtained from Wanxiang Cave, Gansu Province, China (33019'N, 105o00'E; ca. 1200m a.s.l.),located near the northern limit of the Asian summer monsoon (ASM). The ventilation of Wanxiang Cave is weak, with a temperature of 11 ℃ and the relative humidity 100% throughout the year. 828 oxygen isotopic measurements and 6~(230)Th ages characterize high-resolution record of the ASM variability from ca. 104 ~ 92ka B.P., which covers most part of marine isotope stage MIS 5c~5b. The results demonstrate that ASM shows a trend of gradual weakening during 104~92ka B.P. Comparison Wanxiang delta~(18)O record with Sanbao (31°40'N, 110°26'E; 1900m a.s.l.) in Hubei Province and Kesang (42°52'N, 81°45'E; 2000m a.s.l.)in Xinjiang record shows that they exhibit a highly similar variation tendency during the most part of the study period, especially in the MIS 5c, when the ASM significantly enhanced. Hence, it seems reasonable that the fringe of the ASM was far northwest of its current position during the MIS 5c, with above-mentioned 3 caves included within the region controlled by the ASM at the time. However, those stalagmite records do not conform to the negative rule of ASM advance during the extreme weakening period, just like MIS 5b. One possible reason is that it is connected to the change of summer:winter precipitation ratio or the moisture source area.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/149272
Appears in Collections:气候变化与战略

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作者单位: 1.兰州大学地质科学与矿产资源学院, 甘肃省西部矿产资源重点实验室, 兰州, 甘肃 730000, 中国
2.西安交通大学全球变化研究院, 西安, 陕西 710049, 中国

Recommended Citation:
王晓锋,张平中,周鹏超,等. MIS 5c向MIS 5b转换期亚洲夏季风的演变特征万象洞石笋记录[J]. 第四纪研究,2015-01-01,35(6):1398-1410
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