Later "salinity crises" took place further north.

This was during the Messinian salinity crisis, when drainage basins throughout the Mediterranean region changed their course.

A major event was the Messinian salinity crisis or dry Mediterranean.

Some karst formations were created during earlier sea level drops, most notably the Messinian salinity crisis.

It was formed during the Messinian salinity crisis.

It is estimated that some karst formations are from earlier sea level drops, most notably the Messinian salinity crisis.

It is presumed to have arrived from Italy during the Messinian salinity crisis 5-7 million years ago.

The most significant known evaporite depositions happened during the Messinian salinity crisis in the basin of the Mediterranean.

Both are a result of events after the Messinian salinity crisis.

For more information, see the Eonile as well as the Messinian salinity crisis.