Dj. Gower, THE TARSUS OF ERYTHROSUCHID ARCHOSAURS, AND IMPLICATIONS FOR EARLY DIAPSID PHYLOGENY, Zoological journal of the Linnean Society, 116(4), 1996, pp. 347-375
The morphology of the erythrosuchid ankle joint is reassessed. Two spe
cimens, recently thought to have been incorrectly referred to Erythros
uchus africanus, are shown without doubt to belong to this taxon. Furt
hermore, the morphology is essentially similar to that of other early
archosaurs. The tarsus of Erythrosuchus is poorly ossified and consist
s of a calcaneum, astragalus, and two distal tarsals. The calcanea of
Erythrosuchus, Vjushkovia triplicostata, and Shansisuchus shansisuchus
are all similar in being dorsoventrally compressed, possessing a late
ral tuber, and lacking a perforating foramen. The astragalus of V. tri
plicostata is currently unknown. The astragalus of Shansisuchus is app
arently unique in form. The erythrosuchid pes is therefore more derive
d than has been recently proposed. The tarsal morphology of several ot
her archosauromorph taxa is reviewed and many details are found to be
at variance with the literature. The plesiomorphic condition for the A
rchosauromorpha consists of four distal tarsals and a proximal row of
three elements; two of which articulate with the tibia. These proximal
elements are interpreted as the astragalus, calcaneum, and a centrale
, and the same pattern is retained in the earliest archosaurs. This re
assessed tarsal morphology has implications for the homology of the ce
ntrale and reconstruction of early diapsid phylogeny. (C) 1996 The Lin
nean Society of London