During the Messinian salinity crisis (MSC) (from 5.97 to 5.33 Ma), the Mediterranean Sea becamedisconnected from the world’s oceans and a fast and continuous evaporation resulted in its partial desiccation.One of the theories for the end of the MSC postulates that a large volume of Atlantic waters entered theMediterranean Sea through the Gibraltar Strait and rapidly refilled the Mediterranean basin in an event welldocumentedknown as the Zanclean Flood. The pathway of the Zanclean flood during its passage from thewestern to the eastern Mediterranean Sea is unclear. The aim of this study is to understand the effects ofthe Messinian palaeotopography of the southern Tyrrhenian Sea on the dynamics of the Zanclean flood. Weanalysed a large number of multichannel seismic reflection profiles acquired in the Northern Sicily ContinentalMargin (NSCM), calibrated with stratigraphic log from the Agip/ENI wells, and high-resolution multibeamdata showing the present-day morphology. A detailed seismostratigraphic and structural analysis of these dataallowed us to identify two different types of chaotic bodies in the Plio-Pleistocene sedimentary succession. Thefirst type consists of a very thick deposit characterised by chaotic to transparent seismic facies, deposited nonconforminglyabove an older substrate with a very high-amplitude reflector along its top. This older substratecorrelates to the MES horizon (Lofi et al. 2011). The second type consists of thinner bodies having smallervolumes and chaotic seismic facies interbedded with the well-stratified Pleistocene-Holocene deposits. Weinterpret the Pleistocene-Holocene chaotic bodies as small-scale mass transport deposits (MTDs) that are mainlylocated at the foot of steep escarpments and partly triggered by the compressional, extensional, and strike-slipPlio-Pleistocene tectonics. We hypothesise that the larger chaotic body is a flood deposit, possibly emplacedby a branch that separated from the main flow transferring water and sediment through the Sicily Channel(Micallef et al., 2018). Based on the reconstructed Messinian palaeotopography of the southern TyrrhenianSea, the Zanclean flood flowed from west to east across an elongated depression that is now bordered by the“Elimi Chain” to the north and the Sicilian coastline to the south. The material transferred was finally depositedat the toe of Scuso bank and Solunto high.
|Numero di pagine||1|
|Stato di pubblicazione||Published - 2018|