CORDIS Project
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This project explores the link between the uplift of the Tibetan Plateau and global climate cooling during the Cenozoic era. It investigates how Asian Monsoons may have influenced this transition from a warm greenhouse climate to the current icehouse conditions.
Unraveling the cause for Cenozoic global climate cooling is one of the most important unresolved questions challenging the Earth and Environmental sciences community today.
Increased erosion and weathering of the uplifted Tibetan Plateau and Himalayas, is advocated as the primary cause for the enigmatic pCO2 drawdown, that led to global cooling 50 to 34 Myrs ago from the warm ice-free Greenhouse world to the bi-polar Icehouse conditions still prevailing today.
Asian Monsoons are genetically link…
CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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