气候变化领域集成服务门户(CCPortal): Spatial and altitudinal variations in the magnetic properties of eolian deposits in the northern Tibetan Plateau and its adjacent regions: Implications for delineating the climatic boundary

CCPortal

DOI	10.1016/j.earscirev.2020.103271
	Spatial and altitudinal variations in the magnetic properties of eolian deposits in the northern Tibetan Plateau and its adjacent regions: Implications for delineating the climatic boundary
	Zan J.; Fang X.; Kang J.; Li X.; Yan M.
发表日期	2020
ISSN	00128252
卷号	208
英文摘要	Delineating the climatic boundary (i.e., of precipitation and temperature) in the northern Tibetan Plateau and along its margins is important for understanding the dynamics of global atmospheric circulation and the processes of dust production in central Asia. To date, however, meteorological data are scarce for this vast region, which limits our understanding of regional climatic patterns and past climatic changes in Eurasia. In the present study, we use a synthesis of both new and published rock magnetic data from the late Pliocene, the last glacial-interglacial cycle, and modern eolian sediments to identify the climatic boundary in the northern Tibetan Plateau and its adjacent areas. The results demonstrate that eolian deposits under different environmental scenarios exhibit a clear contrast in the type and grain-size distribution of magnetic minerals. With the transition from humid to arid climatic regimes, a gradual shift from magnetic minerals of predominantly pedogenic origin to predominantly detrital origin can be observed in the surface soils. The spatial and altitudinal variations in the magnetic properties of surface soils reveal a distinct boundary of pedogenic intensity in the eastern Qilian Mountains, the western Pamir Plateau and the northern Tianshan Mountains. The inferred variations in pedogenic intensity, combined with analysis of the available meteorological data, demonstrate that the pedogenic boundary represents a critical climatic boundary between sub-humid to semi-arid and arid regions in the northern Tibetan Plateau and the adjacent regions. Stronger pedogenesis occurs in surface soils at higher altitudes on the windward side of the major mountains of the northern Tibetan Plateau, supporting the conclusion that precipitation rather than temperature exerts the dominant effect on the magnetic enhancement of surface soils. In addition, a comparison of several late Pliocene-Pleistocene and last glacial-interglacial loess-red clay sequences suggests that the modern spatial pattern of the climatic gradients in the northeastern Tibetan Plateau and the adjacent regions has been maintained since at least the late Pliocene or early Pleistocene. Moreover, the results demonstrate that during the warm and humid interglacial periods, a steepened rainfall gradient occurred in the northern Tibetan Plateau and its adjacent regions. In the future, detailed rock magnetic investigations of eolian deposits or surface soils could provide new insights into the dynamics of atmospheric circulation and the natural boundary conditions for paleoclimate modeling in the northern Tibetan Plateau. © 2020 Elsevier B.V.
关键词	Climatic gradients Eolian deposits Magnetic properties Northern Tibetan Plateau Precipitation boundary Surface soils
英文关键词	climate change; climate effect; eolian deposit; glacial-interglacial cycle; magnetic property; Pliocene-Pleistocene boundary; sediment transport; spatial variation; China; Qinghai-Xizang Plateau
语种	英语
来源期刊	Earth Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/203949
作者单位	Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
推荐引用方式 GB/T 7714	Zan J.,Fang X.,Kang J.,et al. Spatial and altitudinal variations in the magnetic properties of eolian deposits in the northern Tibetan Plateau and its adjacent regions: Implications for delineating the climatic boundary[J],2020,208.
APA	Zan J.,Fang X.,Kang J.,Li X.,&Yan M..(2020).Spatial and altitudinal variations in the magnetic properties of eolian deposits in the northern Tibetan Plateau and its adjacent regions: Implications for delineating the climatic boundary.Earth Science Reviews,208.
MLA	Zan J.,et al."Spatial and altitudinal variations in the magnetic properties of eolian deposits in the northern Tibetan Plateau and its adjacent regions: Implications for delineating the climatic boundary".Earth Science Reviews 208(2020).