Pengchao Zhou scite author profile

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 CO2‐dominated Late Miocene cooling event (~7–5.4 Ma) Tectonic forcing, rather than pCO2, dominated regional continental climate patterns and ecosystem transitions during the Late Miocene

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Pengchao Zhou

Extreme weather events recorded by daily to hourly resolution biogeochemical proxies of marine giant clam shells

A Late Miocene Terrestrial Temperature History for the Northeastern Tibetan Plateau's Period of Tectonic Expansion

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