0000000000532888
AUTHOR
A. C. Marra
Bio-chronology of pleistocene vertebrate faunas of sicily and correlation of vertebrate bearing deposits with marine deposits
The rich Pleistocene fossil record of Sicily allowed the construction of a fairly detailed bio-chronological frame that is dated by correlation of vertebrate bearing deposits with marine deposits by geochemical and radiometric dating too. Actually, an important category of deposits is representative of transitional and neritic environments, frequently associated with a lagoon or swamp. Limnic deposits related to small freshwater basins also occur, often in relation to coastal and fully marine deposits. Numerous relationships have been found between the vertebrate bearing deposits and marine deposits, which can be correlated with the δ18O isotopic record and the main palaeogeographic events …
A revision of medium and small sized deer from the Middle and Late Pleistocene of Calabria and Sicily
The remains of Megaceroides calabriae from Middle Pleistocene deposits at locality Bovetto (Southern Calabria) and of Megaceroides carburangelensis from the late Middle and Late Pleistocene locality Cimillà (South-eastern Sicily) are revised. These deer were considered as endemic species of strongly reduced size, related to genus Megaceroides (=Praemegaceros), which evolved in insular environment similarly to the endemic megaceroids from Sardinia, Corsica and Crete, M, cazioti and M. cretensis. The comparison of M. calabriae and M. carburangelensis with representatives of genera Megaceroides and Dama, carried out in the present study, shows that the Calabrian and Sicilian deer belong to Dam…
A new late pleistocene vertebrate faunal complex from Sicily (S. Teodoro Cave, North-Eastern Sicily, Italy)
Previous excavations at the S. Teodoro Cave were carried on mainly in the upper unit, Late Glacial in age, containing late Upper Palaeolithic stone artefacts and no endemic mammals remains belonging to the Castello Faunal complex, the youngest of the Pleistocene Sicilian faunal complexes. This unit overlies an older deposit of clay and sands which contain Pleistocene endemic mammal remains. During 1998 excavations a maximum depth of m 1.50 over an area of about 12 sq. m has been exploited. Scarce evidences of the Late Glacial have been encountered during excavations. The investigated lower unit (unit B) is made of clayey sands and gravels containing a highly diversified assemblage of verteb…