Partially disarticulated shark vertebrae from the Lower Cretaceous Too
lebuc Formation in central Queensland arid the Bathurst Island Formati
on in the Northern Territory provide probable evidence of the Anacorac
idae in Australia, and are possibly referable to Pseudocorax. Associat
ed with large shark vertebrae from Canary Station, near Boulia, Queens
land, are numerous placoid scales of four primary types which indicate
a large pelagic shark. The Canary specimen is one of the few Mesozoic
sharks known where, scales have been found associated with vertebrae.
Problems in referring the new shark material to the Anacoracidae and
Pseudocorax are discussed. The significance of vertebral structure and
scale morphology in Mesozoic shark evolution and ecology ia examined.
'Lamna daviesii' Etheridge 1888 is considered a nomen dubium as verte
brae of this kind also occur in other genera in the Lamniformes, Orect
olobiformes, and Carcharhinidae.