Messinian Salinity Crisis (late Miocene)

E262867

The Messinian Salinity Crisis (late Miocene) was a geological event during which the Mediterranean Sea nearly dried up after becoming isolated from the Atlantic, leading to massive salt deposition and dramatic environmental changes.

Try in SPARQL Jump to: Surface forms Statements Referenced by

All labels observed (5)

Statements (49)

Predicate Object
instanceOf Cenozoic event
geological event
paleoclimatic event
salinity crisis
alsoKnownAs MSC
cause global sea‑level changes
restriction of Atlantic–Mediterranean seaway
tectonic uplift at the Strait of Gibraltar region
characterizedBy cyclic evaporite sequences
exposed deep Mediterranean basin floors
extreme hypersalinity in remaining water bodies
large peripheral brine lakes and playas
duration about 630,000 years
effect deep erosion of Mediterranean margins
extinctions and turnovers in marine biota
formation of thick salt layers
incision of deep canyons by rivers flowing into the Mediterranean
isolation of Mediterranean marine fauna from the Atlantic
major changes in regional climate
major changes in regional ecosystems
massive evaporite deposition
near desiccation of the Mediterranean Sea
endTime about 5.33 million years ago
evidence Messinian erosional surfaces on continental margins
deep drill cores from the Mediterranean seafloor
seismic reflection profiles in the Mediterranean
submarine canyons at river mouths
followedBy Messinian Salinity Crisis (late Miocene) self-linksurface differs
surface form: Zanclean flood

opening of the modern Strait of Gibraltar connection
refilling of the Mediterranean Sea
hasStage evaporitic drawdown phase
reflooding phase
locatedIn Mediterranean Basin
Mediterranean Sea
namedAfter Messinian Salinity Crisis (late Miocene) self-linksurface differs
surface form: Messinian age
partOf Cenozoic
surface form: Cenozoic Era

Neogene
surface form: Neogene period

late Miocene
produced anhydrite deposits
gypsum deposits
halite deposits
potash deposits
startTime about 5.96 million years ago
studiedBy marine geology
paleoclimatology
stratigraphy
tectonics
temporalContext end of the Messinian age
just before the Pliocene epoch

Referenced by (5)

Full triples — surface form annotated when it differs from this entity's canonical label.

Neogene hasMajorEvent Messinian Salinity Crisis (late Miocene)
Messinian Salinity Crisis (late Miocene) namedAfter Messinian Salinity Crisis (late Miocene) self-linksurface differs
subject surface form: Messinian Salinity Crisis
this entity surface form: Messinian age
Messinian Salinity Crisis (late Miocene) followedBy Messinian Salinity Crisis (late Miocene) self-linksurface differs
subject surface form: Messinian Salinity Crisis
this entity surface form: Zanclean flood
Miocene notableEvent Messinian Salinity Crisis (late Miocene)
this entity surface form: Messinian Salinity Crisis in the Mediterranean
Late Miocene associatedWith Messinian Salinity Crisis (late Miocene)
this entity surface form: Messinian Salinity Crisis