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[dinosaur] Analysis of skull shape in Triassic dicynodonts (Therapsida) from South America




Ben Creisler
bcreisler@gmail.com

A new paper:


Maria de los Angeles Ordonez, ÂGuillermo H. Cassini, ÂSergio F. VizcaÃno  & Claudia A. Marsicano (2019)
A geometric morphometric approach to the analysis of skull shape in Triassic dicynodonts (Therapsida, Anomodontia) from South America.
Journal of Morphology (advance online publication)
doi: Âhttps://doi.org/10.1002/jmor.21066
https://onlinelibrary.wiley.com/doi/10.1002/jmor.21066


Dicynodont therapsids were a major component of the PermoâTriassic terrestrial ecosystems across Pangea and have been regarded as specialized herbivores. In South America, the group was represented by several taxa of the clade Kannemeyeriiformes spanning from the Middle to the Late Triassic. In order to evaluate if cranial differences among taxa are potentially related to differences in feeding function, we performed a geometric morphometric analysis on 28 South American dicynodont crania. We digitized 19 cranial landmarks and conducted generalized Procrustes analysis, principal component analysis (PCA), principal component analysis between groups (bgâPCA), and a branch weighted squaredâchange parsimony approach. Phylogenetic inertia was not a significant driver of cranial shape evolution in the group, whereas PCA and bgâPCA support that major morphological shape differences are concentrated in the preorbital region (relative length of the snout and width of the caniniform process), in the position of quadrate condyle in relation to the caniniform process, and in the increase in the intertemporal surface area. In this context, tusked Dinodontosaurus, "Kannemeyeria," and Vinceria have relatively smaller adductor attachment areas and input moment arm than younger taxa lacking tusks, such as Ischigualastia, Stahleckeria, and Jachaleria. Differences in cranial morphology in later dicynodonts reflect modifications in feeding mechanics, probably due to changes in food resources (vegetation) in their habitats toward the end of the Triassic.

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