“…The Campanian is also characterized by significant fluctuations of the sea level [10,26,27], a major shift in the δ15 N of marine organic matter [28], clay mineralogical changes, and the occurrence of positive and negative carbon isotope events: the Santonian/Campanian Boundary Event (SCBE) [1,27], the Mid Campanian Event (MCE) [1,3,27], the Conica Event [29], the Late Campanian Event (LCE) [1,3,4,5,27], the Epsilon Event (EE) (also called C1-Event) [3,30], and the Campanian/Maastrichtian Boundary Event (CMBE) [3,5,30].…”