
The Ancient Disappearance of the Mediterranean Sea Explained
A new study reveals that the Messinian Salinity Crisis (MSC), which occurred 5.5 million years ago, led to the evaporation of nearly 70% of the Mediterranean Sea in two phases. Initially, restricted water flow from the Atlantic Ocean caused significant evaporation and salt deposits. In the second phase, complete isolation accelerated these processes, drastically lowering water levels and exposing land bridges. This event, driven by tectonic activity, had significant climatic and geological impacts, and the study provides insights into the Mediterranean's historical evolution.



