“…The Triassic/ Jurassic boundary is marked by a subaerial exposure surface associated with a sea-level drop that can be traced across the entire Apennine Platform (Berra, 2012;Cirilli et al, 2015;Todaro et al, 2017). et al, 1997), the Transdanubian Range in Hungary (Pálfy et al, 2021), the central and northern Apennines of Italy (Barattolo & Romano, 2005;Brandano et al, 2016;Mancinelli et al, 2005), western Sicily (Todaro et al, 2017(Todaro et al, , 2018, Greece (Romano et al, 2008), and Turkey (Coskun Tunaboylu et al, 2014). The recovery of skeletal abundance to pre-extinction levels in shallow-marine environments across western Tethyan carbonate platforms occurred in upper Hettangian-Sinemurian limestones with an increase in skeletal contribution from protists and mollusks.…”