“…The Mersin Ophiolitic Complex (Moix et al, ; Moix, Kozur, Stampfli, & Mostler, ; Pampal, ; Parlak & Robertson, ) comprises two units; the Mersin Mélange (MM) and the Mersin Ophiolite with its sub‐ophiolitic metamorphic sole in southern Turkey (Figure b). According to Tekin, Bedi, Okuyucu, Göncüoglu, and Sayit (), Tekin, Bedi, Okuyucu, Göncüoglu, and Sayit et al (), and Sayit, Bedi, Tekin, Göncüoglu, and Okuyucu (), the Mersin Mélange is of sedimentary origin and contains mainly remnants of the Beysehir–Hoyran nappes sensu Brunn et al (, ) that originated from the IAE Ocean of the Neotethys (equals ‘Bozkir Unit’ by Özgül, , , ). Previously detailed studies performed on the Mersin Mélange revealed that it includes blocks/tectonic slices of Early Carboniferous to early Late Cretaceous ages (Moix et al, , ; Tekin, Bedi, Okuyucu, Göncüoglu, Sayit, et al, 2016).…”