“…The ca. 100 m-scale glacio-eustatic changes related to the 100 kyr eccentricity cycle, accompanied by lower-rank sea-level variations related to the obliquity-and precession-driven periodicities, were concomitant with the uplift of Calabria since latest early Pleistocene, producing flights of marine terraces along both the Ionian and Tyrrhenian coasts (Dumas et al, 1982;Gliozzi, 1987;Carobene and Dai Pra, 1990;Miyauchi et al, 1994;Carobene, 2003;Cucci, 2004;Dumas and Raffy, 2004;Zecchin et al, 2004b;Nalin et al, 2007;Zecchin et al, 2009Zecchin et al, , 2010aZecchin et al, ,b, 2011b.…”