INVESTIGADORES
POL Diego
congresos y reuniones científicas
Título:
Biogeographical distribution patterns during the Jurassic: new information from the Cañadón Asfalto Basin, Patagonia, Argentina
Autor/es:
POL, D.; CARBALLIDO, J.L.; RAUHUT, O.W.; ROUGIER, G.W.; STERLI, J.
Lugar:
Los Angeles
Reunión:
Congreso; 73° Annual Meeting of the Society of Vertebrate Paleontology; 2013
Resumen:
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The Jurassic vertebrate fauna of the
Cañadón Asfalto Basin is one of the most diverse in the world, in particular
due to the highly fossiliferous Cañadón Asfalto Formation (late Early ? early
Middle Jurassic). Described taxa from this unit include members of different
clades of sauropod and theropod dinosaurs, heterodontosaurid ornithischians,
sphenodontians, turtles, crocodylomorphs, and mammals. Recent studies on the
phylogenetic affinities of these taxa have shed light on the evolutionary
affinities of the taxa recorded in the Cañadón Asfalto Basin, allowing the
evaluation of the biogeographic signal through quantitative methods. Several
studies have suggested the existence of groups endemic to the southern
hemisphere during the Jurassic whereas others have postulated a pangeic
distribution as the null hypothesis for the distribution of tetrapods during
this period. Here we present a series of quantitative analyses applying
Dispersal Extinction Cladogenesis (DEC) in the software packages DIVA and VIP
on phylogenetic hypotheses of all the above-mentioned groups in which fifteen
taxa of the Cañadón Asfalto Basin (some of which have been recently published)
have been included. The analyses indicate that eight eleven of the fifteen
lineages recorded in the Cañadón Asfalto Basin belong to clades in which the
ancestral reconstruction is restricted to the southern hemisphere, indicating
the existence of a marked provincialism of these groups of vertebrates during
Pangean times. Four of the taxa recorded in the Cañadón Asfalto Basin belong to
lineages that, in contrast, have a non-gondwanan ancestral distribution. These
results indicate the new records from the Jurassic of Patagonia are showing a
previously undetected and regionalization of the distribution of continental
vertebrates at least since the late Early Jurassic, before the effective
separation of the northern and southern land masses. The common biogeographic
pattern detected from this study suggests therefore the existence of
biogeographic barriers that determined the distribution of continental
vertebrates in Pangea during the Jurassic. These barriers likely were
environmental or climatic, such as the postulated existence of the Central
Gondwanan Desert.