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Rhinocerotidae (Mammalia, Perissodactyla) from the middle pleistocene site of ponte milvio, central Italy
Three rhinoceros species have been identified at Ponte Milvio: Stephanorhinus hundsheimensis (Toula, 1902), Stephanorhinus hemitoechus (Falconer, 1859) and Stephanorhinus kirchbergensis (Jäger, 1839). Remains ascribed to S. hundsheimensis were collected in gravels and sands deposits. They show morphological and morphometric affinities with the small-sized populations of the latest Early Pleistocene from Vallonnet. The occurrence of these small-sized specimens suggests the presence of a faunal assemblage chronologically related with the Early-Middle Pleistocene transition. The remains of S. hemitoechus and S. kirchbergensis were collected in volcanoclastic deposits. The specimens ascribed to S. hemitoechus show morphometric characters close to the small-sized specimens of the latest Middle Pleistocene. Moreover, S. kirchbergensis seems to be common in Italy during the late Middle Pleistocene and it has never been collected with certainty from Late Pleistocene sites. The co-occurrence of S. kirchbergensis and the small-sized S. hemitoechus suggests the presence of a faunal assemblage chronologically referable to a time span between MIS10 and MIS8
The skull of Stephanorhinus hemitoechus (FALCONER, 1859) from Fosso Malafede (Vitinia, Rome) with notes on the first occurrence of the species in Italy
In this work a well-preserved skull of rhinoceros is described. It has been discovered in the upper Middle Pleistocene fluvial deposits outcropping at Fosso Malafede (Vitinia, Rome, Central Italy) and it is preserved in the Museum of Paleontology in Sapienza, University of Rome. Comparative analysis of the morphological characters allow to ascribed the skull to Stephanorhinus hemitoechus. The specimen shows a well-developed occipital crest, toothrows shifted forward and an extended nasal groove. The degree of wear of the second and third upper molars suggests an about 30-36 year-old individual. S. hemitoechus has been named for the first time by Falconer in 1859 from several remains discovered in Great Britain. This species is present at about 0.500-0.450 million years in Continental Europe and it is one of the components of the Italian late Middle and Late Pleistocene assemblages (Aurelian Mammal Age). The early Middle Pleistocene remains from Slivia, Torrente Stirone and Ponte Galeria which are ascribed here to S. hundsheimensis, had been previously assigned to S. hemitoechus. To the latter can be ascribed a mandible discovered in the Tiber River terraces at Monte Verde, referred to the Fontana Ranuccio Faunal Unit. However, the chronological correlation of the site is very doubtful
A critical overview on Early Pleistocene Eurasian Stephanorhinus (Mammalia, Rhinocerotidae): Implications for taxonomy and paleobiogeography
The skull of Stephanorhinus hemitoechus (FALCONER, 1859) from Fosso Malafede (Vitinia, Rome) with notes on the first occurrence of the species in Italy
In this work a well-preserved skull of rhinoceros is described. It has been discovered in the upper Middle Pleistocene fluvial deposits outcropping at Fosso Malafede (Vitinia, Rome, Central Italy) and it is preserved in the Museum of Paleontology in Sapienza, University of Rome. Comparative analysis of the morphological characters allow to ascribed the skull to Stephanorhinus hemitoechus. The specimen shows a well-developed occipital crest, toothrows shifted forward and an extended nasal groove. The degree of wear of the second and third upper molars suggests an about 30-36 year-old individual. S. hemitoechus has been named for the first time by Falconer in 1859 from several remains discovered in Great Britain. This species is present at about 0.500-0.450 million years in Continental Europe and it is one of the components of the Italian late Middle and Late Pleistocene assemblages (Aurelian Mammal Age). The early Middle Pleistocene remains from Slivia, Torrente Stirone and Ponte Galeria which are ascribed here to S. hundsheimensis, had been previously assigned to S. hemitoechus. To the latter can be ascribed a mandible discovered in the Tiber River terraces at Monte Verde, referred to the Fontana Ranuccio Faunal Unit. However, the chronological correlation of the site is very doubtful
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