Climate change recorded by the grain size end member since MIS 3 in Jingbian area
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摘要: 黄土作为典型的多物源沉积物，粒度分布常呈现多峰分布。端元分析可以从复杂的沉积物粒度中分离出代表不同沉积物源和沉积动力的端元组分，在黄土研究中得到了广泛应用。利用Paterson参数化端元模型对处于毛乌素沙漠东南缘的靖边三道沟剖面粒度进行端元分离与解释，并讨论其代表的环境意义。靖边三道沟黄土可分为4个端元：EM1（众数粒径8.93 μm）为背景粉尘；EM2（众数粒径25.18 μm）为与季风环流有关的组分；EM3（众数粒径39.91 μm）和EM4（众数粒径56.37 μm）都是与冬季风有关的组分，其中EM3为黄土高原黄土主要组分，EM4与现代沙尘暴的粒级大致相同。通过对各端元组分随年龄变化的曲线进行分析，得到以下结论：该剖面记录了靖边地区自MIS 3以来经历了MIS 3（32.8~29.8 ka BP）、LGM（29.8~22.8 ka BP）、冰消期（22.8~11.3 ka BP）和全新世（8.7~1.7 ka BP）共4个气候时期。端元组分还记录了冰消期H 1事件（16.2~13.8 ka BP）、B/A事件（13.8~12.8 ka BP）、YD事件（12.8~11.3 ka BP）共3次气候快速变化事件和D-O旋回。该剖面还记录了毛乌素沙漠末次冰期经历的3次主要的扩张-收缩旋回以及全新世8.7~8.2，6.0~5.0，3.5~2.5 ka共3次干旱沙进事件。Abstract: As a typical multisource sediment, the grain size distribution of loess presents multi-peak distribution.End member analysis can be used to separate the end member components representing different sediment sources and sedimentary dynamics from the complex sediment size, which has been widely used in loess research.In this paper, Paterson parametric end member model was used to separate and explained the end member size of Sandaogou profile located in the southeastern margin of the Mu Us Desert.The analyzed results indicated that the Sandaogou loess in Jingbian was divided into four end members: EM1(8.93 μm) was the background dust; EM2(25.18 μm) was a component related to monsoon circulation.EM3(39.91 μm) and EM4(56.37 μm) were components related to winter wind.Among them, EM3 was the main component of loess in the loess plateau and EM4 was roughly the same grain size as modern sandstorms.Through the analysis of the curves of the end member components with age, the following conclusions were drawn: the profile recorded that the Jingbian area had experienced MIS 3(32.8-29.8 ka BP), LGM(29.8-22.8 ka BP), last deglacial(22.8-11.3 ka BP) and Holocene(8.7-1.7 ka BP) since MIS 3. Three climatic rapid change evented and cycles Dansgaard-Oeschger in deglaciation Heinrich 1(16.2-13.8 ka BP), Bølling-Allerød(13.8-12.8 ka BP) and Younger Dryas(12.8-11.3 ka BP) were recorded.The profile also recorded three major expansion-contraction cycles during last glacial period of the Mu Us Desert, and three dry sand events during the Holocene(8.7-8.2 ka, 6.0-5.0 ka, and 3.5-2.5 ka).
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Key words:
- loess /
- grain size /
- end member component /
- climate change /
- desert expansion and contraction /
- Jingbian area
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图 3 n=4时，样品拟合的线性相关性(a)和角度偏差(b)
Figure 3. Linear correlation(a), and angular deviation (b) of sample fitting when n=4
图 4 三道沟剖面黄土粒度参数化端元分解
Figure 4. Parameterized end-element decomposition of loess particle size in Sandaogou profile
图 5 三道沟剖面端元含量及中值粒径(Md)含量变化曲线图
YD.Younger Dryas事件；B/A.Bølling-Allerød暖期；D-O.Dansgaard-Deschger旋回；H1.Heinrich 1事件；LGM.末次冰盛期
Figure 5. Graph of end member content and median particle size(Md) content in the Sandaogou profile
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