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Rapid and cyclic dust accumulation during MIS 2 in Central Asia inferred from loess OSL dating and grain-size analysis

机译:从黄土OSL测年和粒度分析推断中亚MIS 2期间快速而周期性的积尘

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摘要

Due to lack of reliable proxies from the Westerlies-dominant region, the strength change of Northern Hemisphere Westerlies remains poorly understood. The aim of this study is to provide a reliable paleoclimatic proxy about the Northern Hemisphere Westerlies change. Here we report a 30.7 m thick loess section from the Ili basin directly controlled by the Westerlies. Based on optically stimulated luminescence (OSL) and high resolution grain-size records, we reconstruct the change history of the Westerlies strength during the last glacial period (mainly Marine Isotope Stages 2, MIS2), being similar with the Westerlies index recorded in the Qinghai Lake sediments. Within error limits, all ages are in stratigraphic order. We further compare the climatic records among the Ili loess, Qinghai Lake and the NGRIP, their similarity shows a good climatic coupling relationship among the Central Asia, East Asia and the North Atlantic, and the Westerlies plays a critical influence in transporting the North Atlantic signal to Central and East Asia.
机译:由于缺乏来自西部地区主导地区的可靠代理,对北半球西部地区的强度变化仍然知之甚少。这项研究的目的是提供有关北半球西风变化的可靠的古气候代名词。在这里,我们报告了由西风带直接控制的伊犁盆地30.7μm厚的黄土剖面。基于光激发发光(OSL)和高分辨率粒度记录,我们重建了上一个冰期(主要是海洋同位素第2阶段,MIS2)西风强度的变化历史,与青海记录的西风指数相似湖底沉积物。在误差范围内,所有年龄段均按地层顺序排列。我们进一步比较了伊犁黄土,青海湖和NGRIP之间的气候记录,它们的相似性表明中亚,东亚和北大西洋之间存在良好的气候耦合关系,而西风在传递北大西洋信号方面起着关键作用到中亚和东亚。

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