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1 September 2010 The Role of the Calcaneal ‘Heel’ as a Propulsive Lever in Basal Archosaurs and Extant Monitor Lizards
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The structurally complex ankles of Triassic archosaurs (Reptilia: Diapsida) have been repeatedly described, and tarsal characters have played an important role in analyses of archosaur phylogeny. Morphological variations in the ankle joint undoubtedly had a major impact on locomotion, but the functional implications of many ankle features remain poorly understood. This paper investigates the function of one such structure, the prominent and highly distinctive lateral to posterolateral calcaneal process that occurs throughout basal archosaurs and is homologous to the heel-like calcaneal tuber of pseudosuchians. A morphologically analogous lateral process occurs in extant varanid lizards, and X-ray rotoscopic analysis of the limb movements of savannah monitors (Varanus exanthematicus) indicates that the lateral process rotates into a vertical orientation as the limb retracts. As the varanid lateral process approaches the vertical, it becomes increasingly effective in adding to the propulsive moment arm of m. peroneus longus. A computer model of the ankle was compared to modified versions in which the lateral process and the associated proximal expansion of the fifth metatarsal were eliminated, and this virtual experiment demonstrated that the combination of the two structures increases the peak propulsive moment arm of the varanid m. peroneus longus by over 26%. The lateral calcaneal process of basal archosaurs probably acted similarly, enhancing the ability of the peroneus musculature to contribute to propulsion during walking. Like the calcaneal tuber of pseudosuchian archosaurs, the primitive lateral process was a lever that contributed to locomotion by allowing ankle plantarflexion to generate a greater propulsive moment.
© 2010 by the Society of Vertebrate Paleontology
and Corwin Sullivan "The Role of the Calcaneal ‘Heel’ as a Propulsive Lever in Basal Archosaurs and Extant Monitor Lizards," Journal of Vertebrate Paleontology 30(5), (1 September 2010).
Received: 13 October 2009; Accepted: 1 February 2010; Published: 1 September 2010

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