Fig. 1From: A new shark and ray fauna from the Middle Miocene of Mazan, Vaucluse (southern France) and its importance in interpreting the paleoenvironment of marine deposits in the southern Rhodanian Basin Left. Map of the major Miocene deposits of Vaucluse with selachian teeth: 1,“Bonpas”; 2, “Caumont”; 3, “Mazan”; 4, “Saint-Didier”; 5, “Cabrières d’Aigues” (redraw after Demarcq, 1970 modified and Besson et al. 2005 for the Latest Burdigalian network of fluvial valleys: L. Burd fluvial valleys). Right. Early-Middle Miocene Lithostratigraphic framework of the Rhone–Provence Molassic series, simplified from Besson et al., 2005. Black: continental surfaces, grey: Bioclastic limestone-dominated deposits (“molasse” s.s.), white: Sand and marl-dominated deposits. Fl.In: Major Fluvial incisionsBack to article page