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Por favor, use este identificador para citar o enlazar a este item:http://hdl.handle.net/10261/171952
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logo citeasBellucci, L., Biddittu, I., Brilli, M., Conti, J., Germani, M., Giustini, F., … Soriga, I. M. (2019, February). First occurrence of the short-faced bear Agriotherium (Ursidae, Carnivora) in Italy: biochronological and palaeoenvironmental implications. Italian Journal of Geosciences. Societa Geologica Italiana. http://doi.org/10.3301/ijg.2018.31
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Título

First occurrence of the short-faced bear Agriotherium (Ursidae, Carnivora) in Italy: biochronological and palaeoenvironmental implications

AutorBelluci, Luca;Biddittu, Italo;Brilli, Mauro;Conti, Jacopo;Germani, Marco;Giustini, Francesca;Iurino, Dawid Adam;Mazzini, Ilaria;Sardella, Raffaele
FinanciadoresEuropean Commission
Palabras clavePliocene
Villafranchian
Travertine
Ernici Mountains
Ursidae
Fecha de publicación2019
EditorSocietà Geologica Italiana
CitaciónItalian Journal of Geosciences 138: 124-135 (2019)
ResumenIn 1981, a large mammal assemblage was recovered from a laminated travertine exposed in the region of the village of Collepardo (Frosinone, central Italy). The Collepardo mammal assemblage reported in the literature included ungulates and carnivorans. It was referred to the middle Villafranchian for its similarities with the Saint Vallier (France) faunal assemblage. Some authors suggested a slightly older age (?Montopoli FU). Up to now, only cervids were studied, whereas the other remains were never illustrated nor investigated. Since the fossiliferous site was never described in detail and its location roughly defined, a series of field surveys were carried out with the aim of better depict the continental deposit containing this large mammal assemblage. During these surveys, a block containing several mammal bones was discovered. Among them, an hemimandible of a large short-faced bear Agriotherium was found, a carnivoran never reported before from Italy and very rare in the European fossil record. Its occurrence, together with the cervid Pseudodama lyra and Sus arvernensis, suggests an Early Villafranchian age (Triversa F.U.) for the Collepardo assemblage that therefore has to be referred to the Pliocene. Finally, carbon and oxygen isotope ratios were determined to understand the palaeoenvironmental condition of the depositional system.
Versión del editorhttps://doi.org/10.3301/IJG.2018.31
URIhttp://hdl.handle.net/10261/171952
DOI10.3301/IJG.2018.31
ISSN2038-1719
E-ISSN2038-1727
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