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- W2045809224 abstract "Abstract Typical Upper Villafranchian assemblages survive with slight changes up to the end of the Lower Pleistocene. One of these, near Imola, can be correlated with a marine fauna attributed to the Upper Calabrian by Gignoux (1916), and overlies the Plio-Pleistocene boundary by more than 1,000 m. Another faunal assemblage from Farneta, southern Tuscany, is perhaps the youngest assemblage with Villafranchian affinities in Italy. The beginning of the Cromerian is marked by a spectacular faunal revolution. In the surroundings of Rome the Cromerian can be correlated with the marine Sicilian. Other Cromerian faunas are recorded from Tuscany (San Gimignano and Farneta) and from Piedmont (Cogtiglione Monferrato)." @default.
- W2045809224 created "2016-06-24" @default.
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- W2045809224 date "1970-11-01" @default.
- W2045809224 modified "2023-09-27" @default.
- W2045809224 title "Late villafranchian and early mid-pleistocene faunas in Italy" @default.
- W2045809224 doi "https://doi.org/10.1016/0031-0182(70)90004-0" @default.
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