1996. Journal of Vertebrate Paleontology, Abstracts of Papers, 16(3):24.
CAMPANIAN (UPPER CRETACEOUS) CROCODYLIFORMS FROM MADAGASCAR AND THEIR BIOGEOGRAPHIC IMPLICATION
BUCKLEY, Gregory A., Department of Geology, Field Museum of Natural History, Chicago IL 60605; BROCHU, Christopher A., Department of Geological Sciences, University of Texas at Austin, Austin TX 78712.
Recent expeditions to the Mahajanga Basin of northwestern Madagascar have
resulted in the discovery of several species of crocodyliforms in the
terrestrial Campanian deposits of the Maevarano Formation. These taxa offer
important clues in discerning the biogeographic history of the Mesozoic Malagasy
biota.
The discoveries include four loosely articulated skeletons of
the metasuchian Araripesuchus. Like other members of this taxon, the
Malagasy form is small at maturity (approximate skull length 80 mm) and
possesses a short snout with large orbit, a large antorbital fenestra, a robust
internarial bar, and very gracile limb elements. A second discovery was a
partial skeleton of Trematochampsa oblita, previously known from the area
by several dentary fragments. Postcranial material is remarkably well preserved,
which is important in that trematochampsids as a whole are very poorly known.
These specimens will no doubt help resolve relationships at the base of the
Metasuchia.
The presence of Araripesuchus (known only from the
Aptian of Brazil and Niger) and Trematochampsa (known only from the early
Senonian of Niger) in the Campanian Malagasy fauna is interesting, because
Madagascar is understood to have separated from mainland Africa during the Mid-
to Late Jurassic. Although dispersal of taxa to Madagascar during the late Early
to Late Cretaceous is the most feasible hypothesis, the exact dispersal route is
still unknown.