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腾格里沙漠南缘土门剖面末次间冰阶层段的粒度特征及其反映的气候-沉积环境
其他题名Grain Size Characteristics and Sedimentary Environment of the Tumen Section in Southern Tengger Desert during the Interstadial of the Last Glacial
杨庆江1; 温小浩1; 李保生2; 陈敏1; 马佳丽1; 李芳1; 牛东风1
来源期刊中国沙漠
ISSN1000-694X
出版年2017
卷号37期号:4页码:666-677
中文摘要腾格里沙漠南缘土门剖面末次间冰阶层段(TMS 3)由风成砂、黄土状亚砂土、砂黄土、古土壤、湖相沉积物和冲积黄土等6种沉积相相互叠覆构成。粒度分析结果显示,该层段以砂质沉积物为主,粉砂次之,黏土最少,平均值分别为65.45%、26.72%和8.83%;在砂粒级中,以细砂含量最高,其次为极细砂,其余为中砂-粗砂颗粒。粉砂含量、黏土含量、Mz和sigma在风成砂中呈现谷值,在其他沉积相为峰值,中砂-粗砂和细砂则相反。粒度指标指示腾格里沙漠南缘土门剖面末次间冰阶至少经历了13次暖湿和12次冷干的气候波动,且可划分为TMS 3e(54 200~ 59 750aBP)、TMS 3d(54 200~40 800aBP)、TMS 3c(40 800~32 800aBP)、TMS 3b(32 800~25 400aBP)和TMS 3a(25 400~22 940aBP)等5个亚段,25次冷暖波动与格陵兰冰芯和中国南方石笋记录的D/O事件以及北大西洋深海沉积物记录的H事件具有很高的同步性。
英文摘要The MIS 3 sequence of Tumen Section(TMS 3)in the southern margin of Tengger Desert was composed by paleo-aeolian sand,loess-like sandy loams,sandy loess,paleosoil,lacustrine and alluvial loess. The results of grain size analysis showed the sand contents were dominants,silty sand contents were in second place,and clay contents were minimal in TMS 3,and their contents in average are 65.45%,26.72%and 8.83%,respectively;based on the sequence decreasingly in content,the sand contents can also be divided three portions,and they are fine sand,very fine sand and medium sand-coarse sand.The contents of medium sand-coarse sand and fine sand in paleo-aeolian sands were higher than other 5 sediments in TMS 3.These grain size cycles indicated the climate during MIS3in this area at least went through 13 warm-wet events and 12 cold-dry events and could divided into five substages:TMS3e(54 200-59 750 BP),TMS3d(54 200- 40 800 BP),TMS 3c(40 800-32 800 BP),TMS 3b(32 800-25 400 BP)and TMS 3a(25 400-22 940 BP).These fluctuations show a strong coherence with D/O events recorded in Greenland ice core and southern China stalagmites,as well,H events recorded in North Atlantic sediments.
中文关键词腾格里沙漠南缘 ; 土门剖面 ; 末次间冰阶 ; 粒度特征 ; 古气候
英文关键词southern margin of Tengger Desert Tumen Section interstadial of the glacial grain size characteristics paleoclimate
语种中文
国家中国
收录类别CSCD
WOS类目GEOLOGY
WOS研究方向Geology
CSCD记录号CSCD:6013833
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/237116
作者单位1.华南师范大学地理科学学院, 广州, 广东 510631, 中国;
2.华南师范大学地理科学学院, 黄土与第四纪地质国家重点实验室, 广州, 广东 510631, 中国
推荐引用方式
GB/T 7714
杨庆江,温小浩,李保生,等. 腾格里沙漠南缘土门剖面末次间冰阶层段的粒度特征及其反映的气候-沉积环境[J],2017,37(4):666-677.
APA 杨庆江.,温小浩.,李保生.,陈敏.,马佳丽.,...&牛东风.(2017).腾格里沙漠南缘土门剖面末次间冰阶层段的粒度特征及其反映的气候-沉积环境.中国沙漠,37(4),666-677.
MLA 杨庆江,et al."腾格里沙漠南缘土门剖面末次间冰阶层段的粒度特征及其反映的气候-沉积环境".中国沙漠 37.4(2017):666-677.
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