干旱区生态环境知识资源中心(Arid): Holocene paleosols and paleoclimate for the arid upper Minjiang River valley in the eastern Tibetan Plateau

Arid

DOI	10.1016/j.catena.2021.105555
	Holocene paleosols and paleoclimate for the arid upper Minjiang River valley in the eastern Tibetan Plateau
	Zhou, Ruyu; Wen, Xingyue; Lu, Lu; Li, Yunxiang; Huang, Chengmin
通讯作者	Wen, XY (corresponding author), China West Normal Univ, Coll Environm Sci & Engn, Nanchong 637002, Sichuan, Peoples R China.
来源期刊	CATENA
ISSN	0341-8162
EISSN	1872-6887
出版年	2021
卷号	206
英文摘要	The pedogenic features of Holocene paleosols and their paleoclimatic significance in the arid upper Minjiang River valley of the eastern Tibetan Plateau, southwest China, were investigated using elemental geochemistry, particle size distribution, and magnetic susceptibility indices in combination with the min-max normalization and paleoclimate reconstruction methods. Paleosols developed in a semi-humid environment and were classified as Inceptisols and Entisols. Pedogenic intensity of these paleosols was higher in the Middle Holocene and lower in the Early and Late Holocene. Mean annual precipitation (MAP) and mean annual temperature (MAT) inferred from the paleosols formed in the Middle Holocene are similar to 700 mm and similar to 13 degrees C, respectively. Modern climate is cooler and drier than that of the Middle Holocene and resembles that of the Early Holocene and the period after the last glacial maximum. Climatic changes in the study region were sensitive to the Asian monsoon evolution, which was controlled by orbital forcing. Relative warmer and wetter conditions perhaps triggered the ancient cultural immigration and prosperity at similar to 6000 cal. yr BP in the arid valley region.
英文关键词	Paleosol Pedogenesis Normalized pedogenic index Paleoclimate reconstruction Eastern Tibetan Plateau Holocene
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000688449100062
WOS关键词	CHINESE LOESS PLATEAU ; HIGH-RESOLUTION ; CLIMATE-CHANGE ; GLACIER FLUCTUATIONS ; MONSOON ; SOILS ; STRATIGRAPHY ; DEPOSITS ; OPTIMUM ; RECORDS
WOS类目	Geosciences, Multidisciplinary ; Soil Science ; Water Resources
WOS研究方向	Geology ; Agriculture ; Water Resources
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/368253
作者单位	[Zhou, Ruyu] China West Normal Univ, Coll Land & Resources, Nanchong 637002, Sichuan, Peoples R China; [Wen, Xingyue; Lu, Lu; Li, Yunxiang] China West Normal Univ, Coll Environm Sci & Engn, Nanchong 637002, Sichuan, Peoples R China; [Huang, Chengmin] Sichuan Univ, Dept Environm Sci & Engn, Chengdu 610065, Peoples R China
推荐引用方式 GB/T 7714	Zhou, Ruyu,Wen, Xingyue,Lu, Lu,et al. Holocene paleosols and paleoclimate for the arid upper Minjiang River valley in the eastern Tibetan Plateau[J],2021,206.
APA	Zhou, Ruyu,Wen, Xingyue,Lu, Lu,Li, Yunxiang,&Huang, Chengmin.(2021).Holocene paleosols and paleoclimate for the arid upper Minjiang River valley in the eastern Tibetan Plateau.CATENA,206.
MLA	Zhou, Ruyu,et al."Holocene paleosols and paleoclimate for the arid upper Minjiang River valley in the eastern Tibetan Plateau".CATENA 206(2021).