Postdoctoral Fellowship: EAR-PF: Reconstructing and Modeling Hydrology, Vegetation, and Ocean Temperatures at the Mio-Pliocene Re-Flooding of the Mediterranean
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Six million years ago (6 Ma), during the late Miocene epoch, tectonic activity closed the Mediterranean Sea. During this “Messinian Salinity Crisis (MSC),” the Mediterranean dried up, becoming a warm, windy desert around isolated brackish lakes. At the end of the Crisis (5.3 Ma), the Straits of Gibraltar opened, rapidly reflooding the…
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