A vertebrate assemblage from the Coniacian-Santonian Ibeceten Formatio
n of southern Niger includes pipid frogs, which are described herein.
The fossils occur within fluviatile-lacustrine strata and consist of d
isarticulated elements. Two pipid taxa are present: the hyperossified
Pachybatrachus taqueti gen. et sp. nov., and another unidentified taxo
n. The phylogenetic relationships of both are discussed in the context
of recent hypotheses of pipid evolution. Pachybatrachus exhibits some
derived features unknown in other pipids. These include supplementary
accretion of bone on the atlantal centrum, which is involved in an ad
ditional articulation with the skull, as well as on the ventral surfac
e of other vertebral centra. Following cladistic analysis, it is propo
sed that Pachybatrachus is a pipine closely related to the living Afri
can forms Hymenochirus and Pseudhymenochirus. The presence of the prim
itive state for some hymenochirine synapomorphies suggests that Pachyb
atrachus is their sister taxon. The relationships of the unidentified
taxon remain equivocal owing to the fragmentary condition of available
remains.