The recovery of material of a small theropod from the Early Maastrichtian, Cape Lamb Member of the Snow
Hill Island Formation is an unusual occurrence from primarily marine sediments. The pedal morphology of the
specimen that includes a Metatarsal II with a lateral expansion caudal to Metatarsal III, a third metatarsal that is
proximally narrow and distally wide, a Metatarsal III with a distal end that is incipiently ginglymoidal and a second
pedal digit with sickle-like ungual are all diagnostic of a theropod that belongs to the family of predatory dinosaurs, the
Dromaeosauridae. Yet this Antarctic dromaeosaur retains plesiomorphic features in its ankle and foot morphology. As
new dromaeosaur species are being recovered from the mid-Cretaceous of South America and the retention of primitive
characters in the Antarctic dromaeosaur, a new biogeographic hypothesis on dromaeosaur distribution has been
generated. Gondwanan dromaeosaurs are not North America immigrants into South America and Antarctica; rather
they are the relicts of a cosmopolitan dromaeosaur distribution, which has been separated by the vicariant break up of
Pangea and created an endemic clade of dromaeosaurs in Gondwana.
