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“GeoSUB – Underwater geology” – Ustica, 13-17 September 2016











































              Fig 1: A section of the speleothem sampled at Favignana. 1) Continental layer; 2) Marine overgrowth; 3)
                                                      Phreatic layer.



            References
            ANTONIOLI F., MOURTZAS N., ANZIDEI M., AURIEMMA R., GALILI E. Y.  KOLAITI E., LO PRESTI V.,
            MASTRONUZZI G., SCICCHITANO G., SPAMPINATO C., VACCHI M., VECCHIO A., submitted. Millstone
            quarries along the Mediterranean coast: Chronology, morphological variability and relationships
            with past sea levels QUATINT_2016_152.

            LAMBECK K, ANTONIOLI F., ANZIDEI M., FERRANTI L., LEONI G., SCICCHITANO G., SILENZI S. 2011.
            Sea level change along italian coast during Holocene and a proiection for the future Quat. Int. 232,1-
            2, 250-257 doi:10.1016/j.quaint.2010.04.026.

            PAGLIARULO R., ANTONIOLI F., ANZIDEI M. 2012. Sea Level Changes since the Middle Ages along the
            Coast  of  the  Adriatic  Sea:  the  Case  of  St.  Nicholas  Basilica,  Bari,  Southern  Italy.  Quarernary
            International, 2012 Sea Level Changes since the Middle Ages along the Coast of the Adriatic Sea: the
            Case of St. Nicholas Basilica, Bari, Southern Italy. Quat. Int. doi:10.1016/j.quaint.2012.01.011.

            TOKER, E., SIVAN, D., STERN, E., SHIRMAN, B., TSIMPLIS, M., SPADA, G. 2011. Evidence for centennial
            scale sea level variability during the Medieval Climate Optimum (Crusader Period) in Israel, eastern
            Mediterranean. Earth and Planetary Science Letters, 315-316, 51-61.







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