A Late Miocene Terrestrial Temperature History for the Northeastern Tibetan Plateau's Period of Tectonic Expansion
Chihao ChenCAS Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research Chinese Academy of Sciences (CAS) Beijing ChinaYan BaiCAS Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences (CAS) Beijing ChinaXiaomin FangCAS Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences (CAS) Beijing ChinaHaichao GuoCAS Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research Chinese Academy of Sciences (CAS) Beijing ChinaQingquan MengSchool of Earth Sciences and Key Laboratory of Western China's Mineral Resources of Gansu Province Lanzhou University Lanzhou ChinaWeilin ZhangCAS Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences (CAS) Beijing ChinaPengchao ZhouCAS Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research Chinese Academy of Sciences (CAS) Beijing ChinaMurodov AzamdzhonCAS Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research Chinese Academy of Sciences (CAS) Beijing China
2019en
ABI
Аннотация
Key Points The uplift event (~10.5–8 Ma) revealed by glycerol dialkyl glycerol tetraethers temperature records from the Xining Basin is synchronous with regional drying The cooling amplitude over land is less than that over the ocean during the CO 2 ‐dominated Late Miocene cooling event (~7–5.4 Ma) Tectonic forcing, rather than p CO 2 , dominated regional continental climate patterns and ecosystem transitions during the Late Miocene
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