FIG. 2 in A Messinian (latest Miocene) occurrence for Albanerpeton Estes & Hoffstetter, 1976 (Lissamphibia: Albanerpetontidae) at Moncucco Torinese, Piedmont Basin, northwestern Italy, and a review of the European Cenozoic record for albanerpetontids

FIG. 2. — Stratigraphic section for the Miocene through Pliocene succession at Moncucco Torinese, Piedmont Basin, northwestern Italy. Arrows indicate the main biostratigraphic events and the Messinian-Zanclean (Miocene-Pliocene) boundary, all of which help constrain the age of the fossil-bearing interval within the Cassano Spinola Conglomerates. Numbered layers yielding isolated Albanerpeton Estes & Hoffstetter, 1976 bones are indicated by Albanerpeton silhouettes to the right of the stratigraphic log. Modified from Colombero et al. (2017: fig. 2); for details see Dela Pierre et al. (2007, 2011). Abbreviations for rock units exposed within the section (left side of stratigraphic logs) (from top-to-bottom): AAF, Argille Azzurre Formation; CSC, Cassano Spinola Conglomerates; VVC, Valle Versa chaotic complex; PLG, Primary Lower Gypsum; SAF, Sant'Agata Fossili Marls.