4.5 Article

Vegetation climate and marine environmental reconstruction in the western Mediterranean (southern Rifian corridor, Morocco) over the Tortonian-Messinian transition

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Summary: By conducting detailed foraminifer-based biostratigraphy, micro-paleontological, and geochemical analyses combined with new seismic stratigraphy, researchers have successfully established a new and revised Upper Tortonian-Lower Pliocene chronostratigraphic framework for the Alboran Sea, and estimated the extent of Zanclean erosion. The findings suggest the possible existence of a proto-Gibraltar Strait in the late Tortonian-early Messinian, with the restriction of the Mediterranean from the Atlantic Ocean beginning around 7.2 Ma based on changes in foraminifer assemblages and elemental compositions. Precessional cyclicity and reduced ventilation in the Eastern Mediterranean are also highlighted in the later periods.

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