FIGURE 5. Palaeogeographical setting of the considered sector during the Sinemurian (Early Jurassic). High-standing blocks (Trento and Friuli platforms) are separated by troughs (Belluno and Northern Adriatic basins). The Coste dell'Anglone ichnosite was located on the on the sandy barrier complex that separates the open sea (Lombardy basin) from the Trento carbonate platform.