An ichthyosaurian forefin from the Lower Cretaceous Zapata Formation of Southern Chile: implications for morphological variability within Platypterygius.

Pardo-Pérez, J.; Frey, E.; Stinnesbeck, W.; Fernández, M.; Rivas, L.; Salazar, C.; Leppe, M.

Keywords: chile, torres del paine, Platypterygius, tyndall glacier, Ichthyosaurs

Abstract

Expeditions to the Tyndall Glacier (Torres del Paine National Park, South Chile) in 2009 and 2010 recov-ered an articulated ichthyosaurian forefin that displayed traits consistent with Platypterygius. The combination of features observed in this forefin has not been observed in other Platypterygius species, i.e.: (1) one preaxial row and three or even four postaxial rows; (2) the distal articulation of ulna with metacarpal five; (3) the shape and the articula-tion context of distal carpal three, metacarpal three and four; (4) the hexagonal shape of the intermedium; and (5) the presence of only two distal articular facets on the humerus. Nevertheless, the forefin is not referred to a new species, because it was found isolated and no other diagnostic skel-etal elements are present. The forefin presented here is the first complete and articulated forefin of a Platypterygius from the South Pacific margin, and together with other ichthyosaurs from the Tyndall area, represents the southern-most occurrence of Early Cretaceous ichthyosaurs in the Americas.

Más información

Título de la Revista: Palaeobiodiversity and Palaeoenvironments
Volumen: 92
Editorial: Springer
Fecha de publicación: 2012
Página de inicio: 287
Página final: 294
Idioma: ingles
DOI:

10.1007/s12549-012-0074-8

Notas: WOS