New rhynchocephalian specimen in the Late Triassic of southern Brazil and comments on the palatine bone of Brazilian rhynchocephalians

2019 ◽  
pp. 1-9 ◽  
Author(s):  
Paulo R. Romo-de-Vivar-Martínez ◽  
Agustín G. Martinelli ◽  
Voltaire D. Paes Neto ◽  
Camila A. Scartezini ◽  
Marcel B. Lacerda ◽  
...  
2021 ◽  
pp. 1-16
Author(s):  
Arymathéia Santos Franco ◽  
Rodrigo Temp Müller ◽  
Agustín G. Martinelli ◽  
Carolina A. Hoffmann ◽  
Leonardo Kerber

Abstract Traversodontidae is a group of Triassic herbivorous/omnivorous cynodonts that represents the most diversified lineage within Cynognathia. In southern Brazil, a rich fossil record of late Middle/mid-Late Triassic cynodonts has been documented, with Exaeretodon riograndensis Abdala, Barberena, and Dornelles, 2002 and Siriusgnathus niemeyerorum Pavanatto et al., 2018 representing two abundant and well-documented traversodontids. The present study provides a comparative analysis of the morphology of the nasal cavity, nasal recesses, nasolacrimal duct, and maxillary canals of both species using computed tomography, highlighting the changes that occurred in parallel to the origin of mammaliaforms. Our results show that there were no ossified turbinals or a cribriform plate delimiting the posterior end of the nasal cavity, suggesting these structures were probably cartilaginous as in nonmammaliaform cynodonts. Both species show lateral ridges on the internal surface of the roof of the nasal cavity, but the median ridge for the attachment of a nasal septum is absent. Exaeretodon riograndensis and S. niemeyerorum show recesses on the dorsal region of the nasal cavity, which increase the volume of the nasal cavity, potentially enhancing the olfactory chamber and contributing to the sense of smell. On the lateral sides of the nasal cavity, the analyzed taxa show a well-developed maxillary recess. Although E. riograndensis and S. niemeyerorum have roughly similar nasal cavities, in the former taxon, the space between the left and right dorsal recesses of the nasal cavity is uniform along its entire extension, whereas this space narrows posteriorly in S. niemeyerorum. Finally, the nasolacrimal duct of S. niemeyerorum is more inclined anteroposteriorly than in E. riograndensis.


2020 ◽  
Vol 18 (13) ◽  
pp. 1103-1126 ◽  
Author(s):  
Paulo R. Romo de Vivar ◽  
Agustín G. Martinelli ◽  
Annie Schmaltz Hsiou ◽  
Marina Bento Soares

PLoS ONE ◽  
2019 ◽  
Vol 14 (2) ◽  
pp. e0212543 ◽  
Author(s):  
Max Cardoso Langer ◽  
Blair Wayne McPhee ◽  
Júlio César de Almeida Marsola ◽  
Lúcio Roberto-da-Silva ◽  
Sérgio Furtado Cabreira

Geobios ◽  
2015 ◽  
Vol 48 (4) ◽  
pp. 331-340 ◽  
Author(s):  
Rodrigo Temp Müller ◽  
Hermínio Ismael de Araújo-Júnior ◽  
Alex Sandro Schiller Aires ◽  
Lúcio Roberto-da-Silva ◽  
Sérgio Dias-da-Silva

2013 ◽  
Vol 33 (1) ◽  
pp. 67-84 ◽  
Author(s):  
Felipe Chinaglia Montefeltro ◽  
Jonathas Souza Bittencourt ◽  
Max Cardoso Langer ◽  
Cesar Leandro Schultz

2018 ◽  
Vol 63 ◽  
Author(s):  
Júlio Marsola ◽  
Jonathas Bittencourt ◽  
Átila Da Rosa ◽  
Agustin Martinelli ◽  
Ana Maria Ribeiro ◽  
...  

2021 ◽  
Vol 118 (8) ◽  
pp. e2020778118
Author(s):  
Dennis V. Kent ◽  
Lars B. Clemmensen

The earliest dinosaurs (theropods and sauropodomorphs) are found in fossiliferous early Late Triassic strata dated to about 230 million years ago (Ma), mainly in northwestern Argentina and southern Brazil in the Southern Hemisphere temperate belt of what was Gondwana in Pangea. Sauropodomorphs, which are not known for the entire Triassic in then tropical North America, eventually appear 15 million years later in the Northern Hemisphere temperate belt of Laurasia. The Pangea supercontinent was traversable in principle by terrestrial vertebrates, so the main barrier to be surmounted for dispersal between hemispheres was likely to be climatic; in particular, the intense aridity of tropical desert belts and unstable climate in the equatorial humid belt accompanying high atmospheric pCO2 that characterized the Late Triassic. We revisited the chronostratigraphy of the dinosaur-bearing Fleming Fjord Group of central East Greenland and, with additional data, produced a correlation of a detailed magnetostratigraphy from more than 325 m of composite section from two field areas to the age-calibrated astrochronostratigraphic polarity time scale. This age model places the earliest occurrence of sauropodomorphs (Plateosaurus) in their northernmost range to ∼214 Ma. The timing is within the 215 to 212 Ma (mid-Norian) window of a major, robust dip in atmospheric pCO2 of uncertain origin but which may have resulted in sufficiently lowered climate barriers that facilitated the initial major dispersal of the herbivorous sauropodomorphs to the temperate belt of the Northern Hemisphere. Indications are that carnivorous theropods may have had dispersals that were less subject to the same climate constraints.


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