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

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a) There is no substitute for morphological description. Principal Components<br />

Analysis can reveal variance and covariance of an arbitrarily large number of<br />

measurements. However, subtle or retrospectively obvious details of morphology<br />

may be missed when one is initially choosing landmarks. Accounting for al1<br />

informative landmarks is time wnsuming in terms of experimental design and<br />

measurement, while qualitative inspection of a specimen often quickly reveals<br />

morphological novelty. Examples in this study indude the shape of the<br />

mesotarsal articular surface of MT III in Plateosaurus, and the distal MT II<br />

articulation of the third metatarsal of Deinonychus.<br />

b) PCA can uncover not only patterns of morphological dustering, but also the<br />

importance of qualitatively unremarkabfe specimens. Carnosaurian and<br />

tyrannosaurid third metatarsals aggregate strongly in this study, and Troodon<br />

and the putatively herbivorous f ms are outliers at opposite ends of the<br />

robustness scale. CIear patterns do not emerge among smaller non-<br />

arctometatarsaiian coelurosaurs in third metatarsal morphology. The MT Ill of<br />

Elaphrosaums approximates the average morphology in ternis of size and<br />

shape.<br />

c) Proximal constriction distinguishes the arctometatarsalian MT III from other<br />

morphoIogies, but this element is variable in taxa that possess it. Third<br />

metatarsals traditionally recognized as arctometatarsalian occur above 0.22<br />

along PC2, which is an index of proximal gracility (Figure 2.1 5). No non-derived<br />

morphologies duster wÏth them. Specimens of tyrannosaurids and the<br />

ornithomirnid have very simifar vaIues for PC2. Troodon displays an extremity of

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