Artículo
The Late Jurassic pterosaurs from northern Patagonia, Argentina
Fecha de publicación:
09/2013
Editorial:
Royal Society of Edinburgh
Revista:
Earth and Environmental Science Transactions of the Royal Society of Edinburgh
ISSN:
1755-6910
Idioma:
Inglés
Tipo de recurso:
Artículo publicado
Clasificación temática:
Resumen
Records of flying Jurassic reptiles are very scarce in the Southern Hemisphere. Upper Jurassic pterosaurs have been discovered in marine Tithonian sediments of the Vaca Muerta Formation, in the Neuquén Basin, Patagonia, Argentina. Only four specimens are known so far: the first from Arroyo Picún Leufú, and the other three from the lithographic limestones of Los Catutos. Here, we update knowledge of Late Jurassic pterosaurs from northwest Patagonia. We revise the diagnosis and description of a previously described pterodactyloid, which is named as a new genus and species, Wenupteryx uzi. This small-sized pterosaur shows affinities with Euctenochasmatia or Archaeopterodactyloidea, and represents the most complete Jurassic pterosaur so far known from the Southern Hemisphere. We also report a recent finding suggesting that the new specimen belongs to a new species of pterodactyloid pterosaur. These records show that at least three different taxa of pterosaurs coexisted in the Neuquén Basin: Herbstosaurus, Wenupteryx and a more derived pterodactyloid that represents the largest pterosaur known from the Upper Jurassic of Gondwana.
Palabras clave:
NORTHWEST PATAGONIA
,
PTERODACTYLOIDEA
,
SYSTEMATICS
,
TITHONIAN
,
UPPER JURASSIC
Archivos asociados
Licencia
Identificadores
Colecciones
Articulos(CCT - SAN LUIS)
Articulos de CTRO.CIENTIFICO TECNOL.CONICET - SAN LUIS
Articulos de CTRO.CIENTIFICO TECNOL.CONICET - SAN LUIS
Articulos(SEDE CENTRAL)
Articulos de SEDE CENTRAL
Articulos de SEDE CENTRAL
Citación
Codorniú Dominguez, Laura Susana; Brandoni, Zulma Nelida; The Late Jurassic pterosaurs from northern Patagonia, Argentina; Royal Society of Edinburgh; Earth and Environmental Science Transactions of the Royal Society of Edinburgh; 103; 3-4; 9-2013; 399-408
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