Articles | Volume 20, issue 11
https://doi.org/10.5194/cp-20-2399-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.Rapid topographic growth of Diancang Shan, southeastern margin of the Tibetan Plateau, since 5.0–3.5 Ma
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Subject: Vegetation Dynamics | Archive: Terrestrial Archives | Timescale: Cenozoic
Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene
Palynological evidence for late Miocene stepwise aridification on the northeastern Tibetan Plateau
Climate-vegetation modelling and fossil plant data suggest low atmospheric CO2 in the late Miocene
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