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Journal of Paleontology; January 2007; v. 81; no. 1; p. 163-175; DOI: 10.1666/0022-3360(2007)81[163:TROTDA]2.0.CO;2
© 2007 Paleontological Society
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ARTICLE

TAXONOMIC REVISION OF THE DYROSAURID ASSEMBLAGE (CROCODYLIFORMES: MESOEUCROCODYLIA) FROM THE PALEOCENE OF THE IULLEMMEDEN BASIN, WEST AFRICA

STEPHANE JOUVE1

1 Muséum National d'Histoire Naturelle de Paris, Département Histoire de la Terre, CNRS UMR 5143, C.P. 38, 8 rue Buffon, 75005 Paris, France, <jouvestephane{at}yahoo.fr>

The dyrosaurids of the Iullemmeden Basin (West Africa) are mainly represented by two genera, Hyposaurus and Rhabdognathus. Hyposaurus has been recognized in the Paleocene of Mali and Nigeria with two species, H. nopcsai and H. wilsoni. Diagnostic characters given by previous authors for these species do not enable their distinction from each other, nor from North American species. It is therefore reasonable to consider H. nopcsai and H. wilsoni as nomina dubia. In 1930, Swinton erected the new genus and species Rhabdognathus rarus on the basis of mandibular remains, and Buffetaut referred a skull to this species in 1980. A new skull was described in 2002 by Brochu et al., and referred to Rhabdognathus sp. Unfortunately, it is impossible to refer either skull to the type species, the mandibular remains having no diagnostic characters at the specific level. Thus, R. rarus is a nomen dubium, and two new names are erected for the two skulls: R. keiniensis n. sp. and R. aslerensis n. sp., all the mandibular remains being referred to Rhabdognathus sp. The species Rhabdognathus compressus is reassigned to the genus Congosaurus, since its mandible is higher than that of Hyposaurus, shorter than that of Rhabdognathus, and the lateromedially compressed teeth demonstrate that C. compressus and C. bequaerti are closely related.




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J. A. Barbosa, A. W. A. Kellner, and M. S. S. Viana
New dyrosaurid crocodylomorph and evidences for faunal turnover at the K-P transition in Brazil
Proc R Soc B, June 22, 2008; 275(1641): 1385 - 1391.
[Abstract] [Full Text] [PDF]




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