Pedostratigraphic notes on the middle - late pleistocene of capo san vito peninsula (NW sicily)

The available data about Quaternary pedostratigraphic of North-Western Sicily are mainly obtained when fossil vertebrate assemblages are studied. These are often found in caves or in other morphological "traps", where the products of the erosion of soils developed outside these features are redeposited. Soils that may have originated these deposits were found on the marine terraces that are typical of the coast areas of Sicily. Two sequences, called "K22" and "Isolidda", that crop out in the North-Western side of the San Vito lo Capo peninsula -to the West of Palermo -are examined in this work. The first one is a karstic cave infilling, situated near the eastern rim of the old falaise that …