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

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

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surface that is smooth and slightly concave (Doglo-Saburoff 1929), and fom<br />

wrresponding facets on adjacent elements.<br />

Using these aiteria I sought to identify osteological carrelates along<br />

intermetatarsal articular surfaces. Results of the type and extent of correlates,<br />

and the apparent range of motion between metatarsals, reciprocally contributed<br />

to an overall understanding of arctometatarsus functional arthrology.<br />

MATERIALS AND METHODS<br />

In order to explore interelement dynamics in the arctometatarsus and in other<br />

theropod metapodia, 1 took a comparative approach removed from absolute<br />

statements about performance, but which promised insight into functional<br />

variation in the pes of large theropods. For comparison, specimens of large and<br />

smalt arctometatarsalian forrns were examined at UCMP, MOR, and RTMP.<br />

Metatarsal specimens of Allosaurus fragilis (MOR 693), and others at MOR and<br />

RTMP, provided control representatives of the primitive condition for theropods.<br />

The specimens (Table 3.1 ) were sutficiently complete and well preserved for<br />

evaluation of ligament scar position, andlor to resolve possible interrnetatarsat<br />

rnovement.<br />

Assesment of metapodial dynamics in tyrannosaurids themselves entailed<br />

three related lines of inquiry: 1) To ascertain the probable range of motion<br />

between elements in physical specirnens, I manipulated casts of Tyrannosaunrs<br />

rex rnetatarsals. 2) To evaluate intermetatarsal Freedom of movement in other<br />

tyrannosaurids, 1 examined computed tomographie (CT) images of AIberfosaurus<br />

sarcophagus and Gorgosaunrs Iibratus metatarsals. 3) Investigation of

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