The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert

• Published in: Geochemistry International
• Main Authors: Liu Haibo, Li Baosheng, Zheng Chunhong, Si Yuejun, Wen Xiaohao, Niu Dongfeng, Du Shuhuan, Shu Peixian
• Format: Article in Journal/Newspaper
• Language: English
• Published: MAIK NAUKA/INTERPERIODICA/SPRINGER 2017
• Subjects: Shenmu Section; Early Holocene; Trace Elements; Paleo Climate Changes; Science & Technology; Physical Sciences; NORTH-ATLANTIC CLIMATE; HIGH-RESOLUTION; ASIAN MONSOON; CYCLES; CHINA; Geochemistry & Geophysics; North Atlantic
• Online Access: http://ir.ieecas.cn/handle/361006/15635; http://ir.ieecas.cn/handle/361006/15636; https://doi.org/10.1134/S0016702917140038

Through nine trace elements of the Shenmu section, Mu Us Desert is analyzed for the climate changes during Early Holocene. Except Sr, a migration process of P, Mn, Cr, Rb, Nb, Cu, Zn, and V is found in the dune sands, indicating the accumulation processes of the Asian winter monsoon-driven wind erosion and transport and deposition under the cold climatic phase. And accumulation of these elements in different layers of paleo sol dune sands is related to regional geomorphology and element properties. 8.5 winter-summer monsoon cycles in the early Holocene are observed. The duration time and climate of the stronger winter monsoon phases can be compared with the cold climate in the North Atlantic and other parts of China. The result of Red fit 3.8 power spectra shows 310a, 210a, 90a, and 70a centennial cycles for the element, which are consistent with the solar oscillation cycles. These suggest that the external solar activities of the Earth may have great influences on driving the winter and summer monsoon cycles during early Holocene.