“…The lithostratigraphy of the Sarıalan section shows similarities with other Mediterranean Late Miocene sedimentary sections, especially in its distinct lithologic change in the uppermost part of the section. Abrupt changes in lithology from carbonates to diatomites/sapropels and then to evaporites are recorded in upper Tortonian‐Messinian successions throughout the Mediterranean, including sections in Spain [ Pérez ‐ Folgado et al , 2003] Crete [ Santarelli et al , 1998; Faranda et al , 2008], Cyprus [ Krijgsman et al , 2002; Kouwenhoven et al , 2006; Orszag ‐ Sperber et al , 2009], Sicily [ Krijgsman et al , 1995; Bellanca et al , 2001; Rouchy and Caruso , 2006], the central Apennines [ Sampalmieri et al , 2010], and the northern Apennines [ Roveri et al , 2003; Roveri and Manzi , 2006]. These basin‐wide lithologic changes are mainly due to discrete steps of restriction of the connection between the Mediterranean Basin and the Atlantic Ocean [ Kouwenhoven et al , 2006] and related changes in basin‐wide circulation patterns.…”