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

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CHAPTER 2: Descriptive and quantitative morphology of the arctometatarsalian<br />

third metatarsal<br />

INTRODUCTION<br />

As explained in Chapter 1, HoItz (1 994a,b) investigated the phylogenetic and<br />

functional implications of the proximal constriction of the third metatarsal (MT III)<br />

in several clades of Cretaceous coelurosaurs. He designated the<br />

arctometatarsus, in which MT 111 is proximally pinctied, as a character state<br />

present in taxa that also display relatively long lower limb elements (see Figures<br />

1.1, 1.2, and 1.5, Chapter 1). Those taxa that Holtz qualitatively assessed to<br />

have a full arctometatarsus are the Tyrannosauridae, Omithomimidae,<br />

Troodontidae, and Elmisauridae (Hoitz 1994a). This chapter explores qualitative<br />

differences between the third metatarsals of these taxa, to extend Holtz's work<br />

on pedal variation within "arctometatarsalian" clades. Building upon this<br />

qualitative framework, a Principal Cornponents shape analysis statistically<br />

crystallizes divisions between theropod metatarsal morphologies. l then<br />

synthesize and discuss statistical and qualitative data for resultant subgroupings<br />

of metatarsal shape. Once the comparative morphology of the tyrannosaurid<br />

arctometatarsus has been estabtished observationally and statistically, the thesis<br />

logically proceeds into detaited questions of its function and evolution (Chapters<br />

3-4 and Chapter 5, respectively).<br />

Conceptions of arctometatarsus morphology<br />

The terni arctometatarsus has been used imprecisely in the literature and in<br />

public scientific discourse. This confusion anses primarily because Holtz (1994b)

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