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Lucianovenator bonoi
Topic Started: May 19 2017, 08:30 PM (63 Views)
Taipan
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Lucianovenator bonoi

Posted Image


Temporal range: Late Triassic (late Norian—Rhaetian)

Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Dinosauria
Order: Saurischia
Suborder: Theropoda
Superfamily: †Coelophysoidea
Family: †Coelophysidae
Genus: †Lucianovenator
Species:Lucianovenator bonoi

The Coelophysidae are a family of primitive carnivorous theropod dinosaurs. Most species were relatively small in size. The family flourished in the Late Triassic and Early Jurassic periods.

Posted Image
The skeleton of the carnivore that lived 205 million years ago, 2.40 m high and 40 kilos.




Journal Reference:
Ricardo N. Martínez; Cecilia Apaldetti (2017). "A late Norian-Rhaetian coelophysid neotheropod (Dinosauria, Saurischia) from the Quebrada del Barro Formation, northwestern Argentina". Ameghiniana. in press. doi:10.5710/AMGH.09.04.2017.3065

Abstract
Coelophysoids are the most abundant theropod dinosaurs known from the Late Triassic through Early Jurassic represent the earliest major radiation of Neotheropoda. Within Coelophysoidea sensu lato the most stable clade is Coelophysidae, small theropods characterized by long neck and light and kinetic skull. Coelophysids are the most abundant basal non-Tetanurae neotheropods known worldwide, but until recently they were unknown from South America. We report here a new coelophysid neotheropod, Lucianovenator bonoi gen. et sp. nov., from the late Norian-Rhaetian Quebrada del Barro Formation, northwestern Argentina. A phylogenetic analysis recovers Lucianovenator bonoi nested into the monophyletic group Coelophysidae in an unresolved clade together with Coelophysis rhodesiensis and Camposaurus arizonensis. The presence of Lucianovenator in the late Norian-Rhaetian of Argentina increases the poor and scarce record of Triassic South American neotheropods, suggesting that the virtual absence of theropods in the fossil record during the Rhaetian is probably a taphonomic/stratigraphic bias instead of a decline in diversity and abundance after the Norian. Finally, the new find corroborates the American endemism in the Late Triassic and worldwide distribution during the Early Jurassic of coelophysid neotheropods, supporting the extreme faunal homogeneity hypothesized for Early Jurassic continental biotas.

http://www.ameghiniana.org.ar/index.php/ameghiniana/article/view/1003
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