INVESTIGADORES
PREVOSTI Francisco Juan
artículos
Título:
Taxonomy and systematic of fossil hog-nosed skunks, genus Conepatus (Carnivora: Mephitidae) from Argentina
Autor/es:
SCHIAFFINI, MAURO IGNACIO; PREVOSTI, FRANCISCO JUAN
Revista:
JOURNAL OF SOUTH AMERICAN EARTH SCIENCES
Editorial:
PERGAMON-ELSEVIER SCIENCE LTD
Referencias:
Año: 2019 vol. 89 p. 140 - 157
ISSN:
0895-9811
Resumen:
There are three extant species of hog-nosed skunks widely distributed from North to South America, with a dubious number of fossil species. The oldest record comes from the early Pliocene of Mexico, while several Pleistocene species were registered from Argentina (Conepatus cordubensis, C. mercedensis and C. primaevus, plus C. altiramus with a dubious provenance). Conepatus talarae and C. semistriatus were recovered in Late Pleistocene levels of other countries of South America. Unfortunately, there is no recent review of South American fossil Conepatus?, thus the status of several species is not clear. We review the systematics of fossil Conepatus species from Argentina, using morphological descriptions, geometric morphometric analyses and taking into account recent intraspecific variation. We also performed a cladistic analysis to explore the phylogenetic position of the valid fossil species. Morphological variation and morphometric analyses allowed us to recognize three extinct valid species for Argentina: C. altiramus, C. mercedensis and C. primaevus, with varying degrees of overlap between fossil and extant species. Phylogenetic analyses showed that Mydaus is the sister extant group of the other three genera, Mephitis is the sister group of Conepatus, and within this genus there is a ?northern? clade that departs from a ?southern? clade, as previously reported; the southern clade does not have internal resolution. Fossil records with confident stratigraphic provenance indicate that Conepatus is present in South America after 1.8 Ma jointly with several clades that migrated during the Great American Biotic Interchange, and has first confirmed records in the Ensenadan (early-Middle Pleistocene).