Darío Estraviz-López , Aurora Grandal-d’Anglade , María Ríos
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引用次数: 0
Abstract
The Epivillafranchian (1.2 to 0.8 Ma) fossil vertebrate assemblages of Portugal are extremely poorly known compared with to those from the eastern half of Iberia. We review material from one of the two localities of this age previously known in Portugal, Algoz, and present a new microvertebrate locality, Santa Margarida. Both localities are situated in Algarve (South Portugal). The fauna of Algoz includes Hippopotamus antiquus, Eucladoceros sp., Metacervocerus rhenanus and an indeterminate leporid. There are remains of at least two individuals of each deer species from Algoz, although most of the remains are from the same juvenile individual of Eucladoceros sp., about 6 months old. The age of Algoz is determined to be ∼1.2 Ma given the combination of species and their biometrical and morphological characters. Santa Margarida has at least ten species of microvertebrates: Lacertidae indet., Crocidura sp., Sorex sp., Oryctolagus cf. cuniculus, Eliomys cf. quercinus, Apodemus cf. sylvaticus, Allocricetus bursae, Victoriamys chalinei, Iberomys huescarensis, and Iberomys brecciensis. This is the first occurrence of Victoriamys chalinei and Iberomys huescarensis –two vole species typical from the Early Pleistocene – in Portugal. Santa Margarida is younger than Algoz, ranging between ∼0.9 and ∼0.6 Ma, which means that the Early-Middle Pleistocene transition could be represented by this locality.
期刊介绍:
Geobios publishes bimonthly in English original peer-reviewed articles of international interest in any area of paleontology, paleobiology, paleoecology, paleobiogeography, (bio)stratigraphy and biogeochemistry. All taxonomic groups are treated, including microfossils, invertebrates, plants, vertebrates and ichnofossils.
Geobios welcomes descriptive papers based on original material (e.g. large Systematic Paleontology works), as well as more analytically and/or methodologically oriented papers, provided they offer strong and significant biochronological/biostratigraphical, paleobiogeographical, paleobiological and/or phylogenetic new insights and perspectices. A high priority level is given to synchronic and/or diachronic studies based on multi- or inter-disciplinary approaches mixing various fields of Earth and Life Sciences. Works based on extant data are also considered, provided they offer significant insights into geological-time studies.