Loess deposits since early Pleistocene in northeast China and implications for desert evolution in east China. (15th April 2018)

• Record Type: Journal Article
• Authors: Sun, Miao; Zhang, Xujiao; Tian, Mingzhong; Liu, Ru; He, Zexin; Qi, Lin; Qiao, Yansong
• Is Part Of: Journal of Asian earth sciences. Volume 155(2018)
• Page Start: 164
• Page End: 173
• Publication Date: 2018-04-15
• Subjects: Northeast China -- Loess -- Magnetostratigraphy -- Early Pleistocene -- Desert evolution; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2017.09.013
• Languages: English
• ISSNs: 1367-9120

Abstract

Graphical abstract: Highlights: A new loess section in northeast China since the early Pleistocene was reported. The desert evolution in east China was divided into three stages since ∼1.0 Ma. The evolution of desert in east China was mainly controlled by global ice volume. Abstract: Loess deposits and deserts are regarded as coupled geological systems and loess deposits on the periphery of deserts can often be used to reconstruct desert evolution. Previous studies of desert evolution in Asia are mainly concentrated in northwest China and the China Loess Plateau, and little is known about long-term desert evolution in east China. In this study, we selected the Sishijiazi loess section in the Chifeng area in northeast China to study the long-term evolution of the desert in east China. A high-resolution magnetostratigraphy combined with optically stimulated luminescence dating indicated that the age of the section base is approximately 1.02 Ma. The Brunhes-Matuyama boundary is at the depth of 39.8 m in loess unit L8, and the upper boundary of the Jaramillo Subchron is at the depth of 60.8 m in paleosol S10. The results of grain-size analysis indicate a coarsening grain-size trend in the past 1.0 Ma. In addition, based on grain-size variations, the desert evolution in east China since ∼1.0 Ma can be divided into three stages: stability from 1.0 to 0.8 Ma, desert recession from 0.8 to 0.5 Ma, and gradual expansion since 0.5 Ma. Our results further indicate that the evolution of desert in east China was mainly controlled by changes in global ice volume, and that the uplift of the Tibetan Plateau may have had an additional effect.