Climate transition in the Asia inland at 0.8–0.6 Ma related to astronomically forced ice sheet expansion

• Published in: Quaternary Science Reviews
• Main Authors: Han, Wenxia, Appel, Erwin, Galy, Albert, Rösler, Wolfgang, Fang, Xiaomin, Zhu, Xiuhua, Vandenberghe, Jef, Wang, Jiuyi, Berger, André, Lü, Shuang, Zhang, Tao
• Other Authors: Linyi University, Department of Geosciences Tübingen, Eberhard Karls Universität Tübingen = Eberhard Karls University of Tuebingen, Centre de Recherches Pétrographiques et Géochimiques (CRPG), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Chinese Academy of Sciences Beijing (CAS), Center for Earth System Research and Sustainability (CEN), Universität Hamburg (UHH), Department of Earth Sciences Amsterdam, Vrije Universiteit Amsterdam Amsterdam (VU), Chinese Academy of Geological Sciences Beijing (CAGS), Ministry of Land and Resources (MLR), Centre Georges Lemaître for Earth and Climate Research Louvain (TECLIM), Earth and Life Institute Louvain-La-Neuve (ELI), Université Catholique de Louvain = Catholic University of Louvain (UCL)-Université Catholique de Louvain = Catholic University of Louvain (UCL), Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, China
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2020
• Subjects: Qaidam basin; East asia summer monsoon; Ice sheet expansion; Linear and non-linear time series analysis; Orbital forcing; Westerly jet; [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; Ice Sheet
• Online Access: https://hal.science/hal-03401661; https://doi.org/10.1016/j.quascirev.2020.106580

International audience Knowing the evolution history of the climate systems in the Asian inland dominated by either the Westerlies or the Asian monsoon, and understanding their associated driving mechanisms are crucial for assessing future trends of climate and environmental conditions in this region, but both the evolution and mechanisms are still under debate. In this study, we present a comparative analysis of massive data from an accurately dated drill core retrieved from the Westerlies controlled western Qaidam Basin (QB), with records from the Chinese Loess Plateau (CLP) dominated by the East Asia summer monsoon (EASM), to track the time and frequency domain evolution patterns and dynamic changes of the QB and the CLP systems. The results infer two main conclusions. First, a critical transition in the evolution of Qaidam paleolake occurred at 0.8-0.6 Ma, characterized by striking changes in proxy variations and a system shift from periodic variations to more irregular fluctuations after 0.6 Ma. Second, a similar evolution pattern prevailed in the Qaidam paleolake region and in the EASM-dominated CLP between similar to 2.7 and similar to 1.2 Ma, but a divergence of both systems started at similar to 1.2 Ma and fully established after 0.6 Ma, when largely fluctuating climate conditions in the QB with a distinct drying trend was accompanied by synchronous largely fluctuated EASM with an increasing trend after 0.6 Ma. We suggest that ice sheet expansion in the Northern Hemisphere, promoted by co-occurrence of low obliquity amplitudes and low eccentricity, drove both systems across a threshold at similar to 1.2 Ma, and the internal forcing due to glaciation disturbed the previous response of both systems to solar insolation and led to the divergence of two systems. At similar to 0.9-0.8 Ma, a node of the 1.2-Myr obliquity cycle co-occurred with an eccentricity minimum, which together with coeval decrease in atmospheric CO2 concentration, could have facilitated a striking expansion of ice sheets. The resulting ...