A new erpetosuchid (Pseudosuchia, Archosauria) from the Middle-Late Triassic of Southern Brazil

被引:18
|
作者
Lacerda, Marcel B. [1 ]
De Franca, Marco A. G. [2 ]
Schultz, Cesar L. [1 ,3 ]
机构
[1] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Bento Goncalves Ave 9500, Porto Alegre, RS, Brazil
[2] Univ Fed Vale Sao Francisco, Colegiado Ciencias Biol, Campus Ciencias Agr,Highway BR 407,Km 12,Lote 543, BR-56300990 Petrolina, PE, Brazil
[3] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Bento Goncalves Ave 9500, Porto Alegre, RS, Brazil
关键词
Archosauria; Brazil; Erpetosuchidae; Pagosvenator; Santa Maria Supersequence; South America; Triassic; SANTA-MARIA FORMATION; MANDA BEDS; ORIGIN; DINOSAUR; CLASSIFICATION; REDESCRIPTION; EVOLUTION; ANATOMY; POSTOSUCHUS; PHYTOSAUR;
D O I
10.1093/zoolinnean/zly008
中图分类号
Q95 [动物学];
学科分类号
071002 ;
摘要
The evolution and diversification of Triassic pseudosuchian lineages has been the subject of much interest and revision in the last couple of decades, fuelled by new and important discoveries, which have allowed for better-sampled phylogenetic analysis. In the present contribution, we add to this by describing a new taxon, Pagosvenator candelariensis gen. et sp. nov., for the Middle-Late Triassic Dinodontosaurus Assemblage Zone of the Santa Maria Supersequence of southernmost Brazil. A comparative osteological analysis combined with a phylogenetic analysis supports its inclusion within the clade Erpetosuchidae and provides an insight into the phylogenetic relationship and evolutionary history of this clade, with two possibilities for the Erpetosuchidae relationship: as an early branch of pseudosuchians, being a sister group of Ornithosuchidae; or a closer relationship with the clade composed by Gracilisuchidae and Paracrodylomorpha with respect to Orntithosuchidae and Aetosauria. Additionally, the results presented and discussed here are of biostratigraphical importance, given that the taxon is from the Ladinian/Carnian age and would fill a temporal gap that exists within Erpetosuchidae between Parringtonia gracilis from the Anisian and Erpetosuchus from late the Carnian to Norian. Furthermore, it would be the first occurrence of a member of this clade in South America.
引用
收藏
页码:804 / 824
页数:21
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