MSC

E905194

MSC refers to the Messinian Salinity Crisis, a geological event about 5–6 million years ago when the Mediterranean Sea nearly dried up due to restricted connection with the Atlantic Ocean.

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All labels observed (1)

Label Occurrences
MSC canonical 1

Statements (49)

Predicate Object
instanceOf geological event
paleoceanographic event
paleoclimatic event
alsoKnownAs MSC NERFINISHED
cause global sea-level changes
restriction of connection between Mediterranean Sea and Atlantic Ocean
tectonic uplift at the Gibraltar region
chronostratigraphicUnit Messinian NERFINISHED
effect changes in marine biota of the Mediterranean region
erosion of deep canyons by rivers flowing into the Mediterranean
isolation of Mediterranean marine fauna from Atlantic fauna
major drop in Mediterranean Sea level
massive salt deposition
near desiccation of the Mediterranean Sea
precipitation of thick evaporite deposits
strong increase in Mediterranean water salinity
endTime about 5.33 million years ago
evidence deep drill cores from the Mediterranean seafloor
onshore Messinian evaporite outcrops
seismic reflection profiles in the Mediterranean basin
followedBy Pliocene marine conditions in the Mediterranean
Zanclean flood NERFINISHED
reflooding of the Mediterranean Sea
geologicalPeriod Late Miocene NERFINISHED
hasUncertainty degree of complete versus partial desiccation of the Mediterranean basin
exact duration and timing of individual desiccation phases
impact hydrological cycle in the Mediterranean region
paleogeography of southern Europe and North Africa
regional climate around the Mediterranean
sedimentary architecture of Mediterranean margins
location Eastern Mediterranean Basin NERFINISHED
Gibraltar Arc region NERFINISHED
Western Mediterranean Basin NERFINISHED
mainDeposits anhydrite
evaporites
gypsum
halite
potash salts
namedAfter Messinian age NERFINISHED
partOf Neogene tectonic and climatic evolution of the Mediterranean region NERFINISHED
precededBy Tortonian stage NERFINISHED
relatedTo Gibraltar Strait closure NERFINISHED
Mediterranean-Atlantic gateway evolution
startTime about 5.96 million years ago
studiedBy geologists
paleoceanographers
paleoclimatologists
timeSpan Late Messinian
tookPlaceIn Mediterranean Sea NERFINISHED

Referenced by (1)

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

Messinian Salinity Crisis (late Miocene) alsoKnownAs MSC
subject surface form: Messinian Salinity Crisis