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THE UNIVERSITY OF CALGARY Eric Snively A ... - Ohio University

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ABST RACT<br />

The arctometatarsus is a metapodial structure exclusive to Cret- PC~OUS<br />

melurosaurian dinosaurs. The central third metatarsal (MT III) of the<br />

arctometatarsus is proximally constricted between the second and fourth (MT II<br />

and MT IV), MT III is also triangular in distal cross section, with the apex towards<br />

the plantar surface. Descriptive morphology and Principal Components Analysis<br />

(PCA) segregate the arctometatarsus from other morphologies, and suggest<br />

hypotheses of function for tyrannosaurid metatarsi and similar forms. Through CT<br />

analysis of metatarsal shape, physical manipulation of casts, assessrnent of<br />

osteological correlates of ligaments, and camparison with the equid carpus, two<br />

hypotheses are evaluated for the tyrannosaurid arctometatarsus. First, ligament<br />

anatomy provides a rnechanism for a previously proposed hypothesis, that axial<br />

Iocomotor energies were transferred from MT III to the outer elements. Second,<br />

the tensional keystone hypothesis holds that upon angled footfalls during linear<br />

locomotion, distal intermetatarsal figaments would prevent anterodorsôl<br />

displacement of MT III, and unrfy the metapodium. Finite element analysis of<br />

strain energy in Gorgosaurus libratus metatarsals strongly supports the energy<br />

transference hypothesis, and indiredy supports the tensional keystone<br />

hypothesis. From the perspective of this evaluation of the tyrannosaurid<br />

arctometatarsus, functional hypotheses are proposed for the metatarsi of other<br />

theropods. Mapping the arctometatarsus ont0 two phylogenies of theropods<br />

suggests a tentative sœnario for the structure's evolution and biological rote.<br />

iii

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