Articles | Volume 12, issue 7
https://doi.org/10.5194/cp-12-1473-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1473-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Palynological evidence for late Miocene stepwise aridification on the northeastern Tibetan Plateau
Jia Liu
MOE Key Laboratory of Western China's Environmental Systems &
College of Earth and Environmental Sciences, Lanzhou University,
Lanzhou 730000, China
Ji Jun Li
CORRESPONDING AUTHOR
MOE Key Laboratory of Western China's Environmental Systems &
College of Earth and Environmental Sciences, Lanzhou University,
Lanzhou 730000, China
Chun Hui Song
Key Laboratory of Western
China's Mineral Resources of Gansu Province & School of Earth Sciences,
Lanzhou University, Lanzhou 730000, China
Hao Yu
MOE Key Laboratory of Western China's Environmental Systems &
College of Earth and Environmental Sciences, Lanzhou University,
Lanzhou 730000, China
Ting Jiang Peng
MOE Key Laboratory of Western China's Environmental Systems &
College of Earth and Environmental Sciences, Lanzhou University,
Lanzhou 730000, China
Zheng Chuang Hui
MOE Key Laboratory of Western China's Environmental Systems &
College of Earth and Environmental Sciences, Lanzhou University,
Lanzhou 730000, China
Xi Yan Ye
MOE Key Laboratory of Western China's Environmental Systems &
College of Earth and Environmental Sciences, Lanzhou University,
Lanzhou 730000, China
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Short summary
The late Cenozoic basins in the northeastern Tibetan Plateau document both the tectonic uplift process and its associated environmental changes. Here, we investigated a late Miocene sporopollen record from the Tianshui Basin in the northeastern Tibetan Plateau. The results show that a persistent aridification trend parallels the global cooling of the late Miocene, and the stepwise vegetation succession is consistent with the major uplift events of the Tibetan Plateau.
The late Cenozoic basins in the northeastern Tibetan Plateau document both the tectonic uplift...