Tectonic forcing of late Cenozoic climate

作者: M. E. Raymo , W. F. Ruddiman

DOI: 10.1038/359117A0

关键词: Earth scienceCenozoicErosion and tectonicsIce sheetPaleoclimatologyGeologyPlateauOceanographyGlobal coolingForcing (mathematics)Climate change

摘要: Global cooling in the Cenozoic, which led to the growth of large continental ice sheets in both hemispheres, may have been caused by the uplift of the Tibetan plateau and the positive feedbacks initiated by this event. In particular, tectonically driven increases in chemical weathering may have resulted in a decrease of atmospheric C02 concentration over the past 40 Myr.

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