Prehistoric Eurasia contained the largest mega-lake on Earth, formed after the isolation of a fragmented region of dying seas known as Paratethys. In this realm, tectonics, sea-level fluctuations, and climate change led to ecological crises: brine seas, extinctions, great drying events and mega-floods. How these cataclysmic events were connected remained a mystery. This study shows that central to these catastrophes are the sea-straits. We document how small changes in climate or in sea-level can change the behavior of the straits and then lead to environmental change and even extinction events. Also, we postulate that a large number of previously unexplained anomalies, stretching for thousands of km are marks of a large mega-flood that occ...
The final stage of the Messinian salinity crisis (MSC) was characterized by brackish-water “Lago-mar...
Marine gateways are important for semi-enclosed basins as they control exchange flows and influence ...
The final stage of the Messinian salinity crisis (MSC) was characterized by brackish-water “Lago-mar...
A complex interplay of palaeoclimatic, eustatic and tectonic processes led to fragmentation and dis-...
The largest megalake in the geological record formed in Eurasia during the late Miocene, when the ep...
The Black Sea and Caspian Sea are the present-day remnants of the former Paratethys, a large epicont...
The Black Sea and Caspian Sea are the present-day remnants of a much larger epicontinental sea on th...
Tectonic plates form the Earth’s outer shell and move over the underlying mantle with a speed of a f...
At the time of the Messinian Salinity Crisis in the Mediterranean Sea (i.e., the Pontian stage of th...
International audienceA recently published scenario viewing theMessinian salinity crisis as two evap...
During the late Miocene, the Mediterranean developed into a hypersaline basin wherein ultimately gyp...
Miocene plate tectonic activity created regions of relatively restricted marine sedimentation—the Me...
Forty years after the image of the Mediterranean transformed into a giant salty lake was first conce...
The final stage of the Messinian salinity crisis (MSC) was characterized by brackish-water “Lago-mar...
Marine gateways are important for semi-enclosed basins as they control exchange flows and influence ...
The final stage of the Messinian salinity crisis (MSC) was characterized by brackish-water “Lago-mar...
A complex interplay of palaeoclimatic, eustatic and tectonic processes led to fragmentation and dis-...
The largest megalake in the geological record formed in Eurasia during the late Miocene, when the ep...
The Black Sea and Caspian Sea are the present-day remnants of the former Paratethys, a large epicont...
The Black Sea and Caspian Sea are the present-day remnants of a much larger epicontinental sea on th...
Tectonic plates form the Earth’s outer shell and move over the underlying mantle with a speed of a f...
At the time of the Messinian Salinity Crisis in the Mediterranean Sea (i.e., the Pontian stage of th...
International audienceA recently published scenario viewing theMessinian salinity crisis as two evap...
During the late Miocene, the Mediterranean developed into a hypersaline basin wherein ultimately gyp...
Miocene plate tectonic activity created regions of relatively restricted marine sedimentation—the Me...
Forty years after the image of the Mediterranean transformed into a giant salty lake was first conce...
The final stage of the Messinian salinity crisis (MSC) was characterized by brackish-water “Lago-mar...
Marine gateways are important for semi-enclosed basins as they control exchange flows and influence ...
The final stage of the Messinian salinity crisis (MSC) was characterized by brackish-water “Lago-mar...