Tectonics and sedimentation of the Lower and Middle Pleistocene mixed siliciclastic/bioclastic sedimentary successions of the Ionian Peloritani Mts (NE Sicily, Southern Italy): the onset of opening of the Messina Strait

Biostratigraphic analyses carried out on siliciclastic/bioclastic deposits discontinuously cropping out along theIonian flank of NE Sicily, indicate that they form two sedimentary events of Early and Middle Pleistocene, respec-tively. Vertical facies successions, showing transgressive trends, suggest that sedimentation occurred withinsemi-enclosed marine embayments, where sublittoral coastal wedges developed on steep ramp-type shelves.Sediments accumulated in shoreface to offshore transitions along steep bottom profiles. This depositional sce-nario was strongly conditioned by the tectonic activity of the rift zone linking Western Calabria and Eastern Sicily.The effects of glacio-eustatism were also recognized. According to our reconstruction, the study area was con-trolled by a transfer fault system which affected the coastal margin producing major episodes of uplift and sub-sidence. Block-faulting was responsible for significant cannibalization and recycling of older deposits during theMiddle Pleistocene. Such a tectonic setting can be considered the precursor scenario for the formation of theMessina Strait between Calabria and Sicily. This narrow, linear basin influences the hydrodynamic setting ofsublittoral deposits along the Ionian coast of Sicily, giving rise to strong flood/ebb tidal currents. The uppermostpart of the Middle Pleistocene succession recognized in the study area is indeed dominated by tide-influencedassociations of sedimentary structures which most likely record the first stage of the opening of this ‘seaway’ ofthe central Mediterranean Sea.