FIGURE 2 in New species of Deinogalerix (Mammalia, Eulipotyphla) from the late Miocene of Scontrone (Abruzzo, central Italy)

FIGURE 2. Schematic stratigraphy of the early Tortonian site of Scontrone (from Patacca et al., 2008a, modified). Succession showing the stratigraphic position of the bonebeds within the Scontrone Member of the Lithothamnium Limestone Formation. RC Rudist-bearing Calcarenite; SC Scontrone Member of the Lithothamnium Limestone Formation; SCa–SCd facies units of the Scontrone Member recording major shifts in the depositional setting and biotic associations (SCa = costal bar deposits; SCb = tidal creek deposits; SCc = marsh deposits; SCd = lagoon deposits). 1-Calcareous marls; 2-Bioclastic calcarenites; 3-Bioclastic calcarenites with oversized well-rounded lithoclast lags; 4- Lithoclastic calcirudites; 5-Major disconformity; 6-Low-angle cross-bedding; 7-Trough cross-bedding; 8-Root traces; 9-Oyster shell lags; 10-Hydrobiids; 11-Bonebeds; 12-Rudists. For further details see Patacca et al. (2008a).