|
Queensland Museum, Queensland Cultural Centre, PO Box 300 South Brisbane, Queensland, 4101 Australia
The fossil record of continental vertebrates from Antarctica is practically nonexistent, hence the composition of the supposed Mesozoic terrestrial vertebrate fauna must be inferred indirectly. This may be done using the reconstructed positions of the continents during the Mesozoic. These positions suggest the presence in Antarctica of primitive sauropods, large theropods, hypsilophodontian and iguanodontid ornithopods, ankylosaurs, pterosaurs, crocodilians, lungfish and possibly birds. In the absence of evidence to the contrary, monotremes are considered endemic Australian forms during the Cretaceous. The discovery of hypsilophodontian material in New Zealand corroborates the inference of Antarctic hypsilophodontians from their occurrence in Australia. The existence in the Australian Early Cretaceous of relict taxa and taxa that seem unusual compared to their overseas relatives suggests that the south polar tetrapod fauna was characterized by singular forms.
