The concept of a geologically istantaneous earliest Zanclean reflooding of the Mediterranean Basin after the Messinian drawdown has dominated geological thinking and is ingrained in the scientific literature. The base of the Trubi Formation in southern Italy -formally defined as the Zanclean Global Boundary Stratotype Section and Point (GSSP) at 5.33 Ma- has traditionally been considered as marking the marine reflooding of the Mediterranean. However, several studies provide evidence that marine reflooding occurred prior to the Zanclean GSSP, the most reliable of which comes from southern Calabria. Here, we show that the sedimentary coastal prism cropping out extensively right below the base of the Trubi Formation in this region and correlatable with the Arenazzolo Unit in Sicily, contains a fully marine micropaleontological association of calcareous nannofossils and dinoflagellate cysts, thus pointing to both a high sea level and marine conditions before deposition of the Trubi Formation, i.e., in the latest Messinian.

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