干旱区生态环境知识资源中心(Arid): 毛乌素沙地东南缘全新世气候不稳定性

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	毛乌素沙地东南缘全新世气候不稳定性
其他题名	Holocene climatic instability record in the southeastern margin of Mu Us Desert
	李想 1; 苏志珠 2; 马义娟 3; 张彩霞 4; 柳苗苗 1
来源期刊	中国沙漠
ISSN	1000-694X
出版年	2020
卷号	40 期号:2 页码:109-117
中文摘要	毛乌素沙地处于中国季风区的西北边缘,对气候变化敏感,是古气候演化和古环境变迁研究的理想场所。全新世气温回暖期,气候整体稳定但存在暖湿冷干的次级波动,不同类型沉积相组成的地层序列记录了全新世千年、百年尺度的气候不稳定性。对毛乌素沙地不同沉积序列的研究表明:( 1)毛乌素沙地东南缘的沙漠/黄土边界带DLT、NB剖面粒度及Rb /Sr比值可作为气候变化的代用指标。>63 mum砂含量增加,Rb /Sr比值降低,揭示东亚冬季风增强,风成砂堆积,风沙活动加剧,气候干冷;反之,东亚夏季风增强,降水增多,风化成壤程度加大,气候暖湿。( 2)毛乌素沙地东南缘沙漠/黄土边界带及低洼沟谷区年代概率密度函数的分析显示,全新世早期~ 8.5 ka BP风成砂堆积,风沙活动加剧,气候表现为干冷;全新世中期8.5 ka ~ 3.0 ka BP地势较高处古土壤广泛发育,地势低洼处发育湖沼相/泥炭层,但在6.0 ka BP左右存在气候转冷过程;全新世晚期3.0 ka BP以来气候波动频繁。( 3)毛乌素沙地气候变化与北大西洋冰筏冷事件、董哥洞石笋、季风边缘区湖泊、东部沙地等记录具有可对比性和相对一致性,反映出全新世千年和百年尺度上的气候变化主要受全球变化的影响,这对预测和模拟未来气候变化具有借鉴意义。
英文摘要	Since Holocene,the temperature has risen and the climate is generally stable,but there are still climate fluctuations. Located in the northwestern edge of the East Asian monsoon,Mu Us Desert stratigraphic sedimentary sequence reveals the climatic instability on the millennium and centennial scales in Holocene. The result shows: ( 1) The grain and Rb /Sr ratio of DLT and NB section in the desert /loess boundary zone can be used as climate and environment index. The increase of >63 mum sand content and the decrease of Rb /Sr ratio revealed the east Asian winter monsoon enhanced,aeolian sand accumulated,aeolian sand activity intensified and the climate was cold and dry. Controversially,the east Asian summer monsoon strengthened,precipitation increased,pedogenesis strengthened, and the climate was warm and humid. ( 2) The analysis of the age probability density of the desert /loess boundary zone and low -lying valley in the southeast margin of the Mu Us Desert indicated that the aeolian sand accumulated at -8.5 ka BP in the early Holocene,aeolian sand activity intensified and the climate was cold and dry. In the middle of Holocene,the paleosol strata were widely developed between 8.5 ka and 3.0 ka BP in the highland,and the lacustrine /peat layers were generally deposited in the low -lying areas. While there were sedimentary interruption near 6.0 ka BP and the climate turned cold. After 3.0 ka BP,climate fluctuated frequently in the late Holocene. ( 3) The climate change in Mu Us Desert is consistent with the records of ice-raft cold events in the North Atlantic, Dongge Cave stalagmite,lakes and eastern sandy land in the monsoon marginal areas in China. The millennium / centennial scale climate change in Mu Us Desert during Holocene is influenced by the global and regional climate change,which is significance for predicting climate change.
中文关键词	气候变化 ; 年代数据 ; 概率密度 ; 全新世 ; 毛乌素沙地
英文关键词	climate change chronological data probability density Holocene the Mu Us Desert
语种	中文
收录类别	CSCD
WOS类目	GEOLOGY
WOS研究方向	Geology
CSCD记录号	CSCD:6691926
来源机构	中国科学院西北生态环境资源研究院
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/318420
作者单位	1.山西大学环境与资源学院, 太原, 山西 030006, 中国; 2.山西大学历史文化学院, 太原, 山西 030006, 中国; 3.太原师范学院地理科学学院, 晋中, 山西 030619, 中国; 4.中国科学院西北生态环境资源研究院, 中国科学院沙漠与沙漠化重点实验室, 兰州, 甘肃 730000, 中国
推荐引用方式 GB/T 7714	李想,苏志珠,马义娟,等. 毛乌素沙地东南缘全新世气候不稳定性[J]. 中国科学院西北生态环境资源研究院,2020,40(2):109-117.
APA	李想,苏志珠,马义娟,张彩霞,&柳苗苗.(2020).毛乌素沙地东南缘全新世气候不稳定性.中国沙漠,40(2),109-117.
MLA	李想,et al."毛乌素沙地东南缘全新世气候不稳定性".中国沙漠 40.2(2020):109-117.