Cteniogenys

''Cteniogenys'' is a genus of choristodere, a morphologically diverse group of aquatic reptiles. It is part of the monotypic family Cteniogenidae. The type and only named species, ''C. antiquus'', was named in 1928 by Charles W. Gilmore. The holotype, VP.001088, was collected in the Morrison Formation (Como Bluff), Wyoming in 1881 by William H. Reed. More specimens have been discovered since then, including specimens from the Late Jurassic of Portugal and Middle Jurassic of Britain, which have not been assigned to species.

Description

''Cteniogenys'' was long, and probably weighed less than . The skull of this genus was long and slender, and the jaws had numerous conical teeth. ''Cteniogenys'' in the Morrison probably fed on insects and small fish. It is mostly known from freshwater sites (rivers and ponds), and is a rare find in the formation (only 60 specimens out of over 2,800 total vertebrate specimens known from the formation), mostly known from northern outcrops (particularly Wyoming); this may reflect a preservation bias against small animals in terrestrial settings, rather than an accurate reflection of ''Cteniogenys'' populations in the Morrison.

Distribution

Fossils of ''Cteniogenys'' are known from the upper Middle Jurassic ( Bathonian) aged Forest Marble Formation and Kilmaluag Formation of Britain, the Late Jurassic (Kimmeridgian) aged Alcobaça Formation of Portugal, and the Late Jurassic-age Morrison Formation of western North America, indeterminate similar remains are also known from the Callovian aged Balabansai Formation of Kyrgyzstan and the Bathonian aged Itat Formation of western Siberia, and the Berriasian aged Angeac-Charente bonebed in France.Ronan Allain, Romain Vullo, Lee Rozada, Jérémy Anquetin, Renaud Bourgeais, et al.
Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary
Geodiversitas, Museum National d’Histoire Naturelle Paris, In press. ffhal-03264773f

A handful of skull and jaw fragments from the Late Cretaceous Oldman Formation and Dinosaur Park Formation in Canada were assigned to ''Cteniogenys'' by Gao and Fox (1998). Given the long gap in time, however, Gao et al. (2005) cautioned that these remains could constitute a different, as-yet undetermined genus. In their description of new material of '' Khurendukhosaurus'', Matsumoto et al. (2009) agreed that the putative Cretaceous occurrence of ''Cteniogenys'' did not belong to that genus and represents an indeterminate choristoderan, possibly a new genus.

Systematics

The genus was named in 1928 by Charles W. Gilmore on the basis of a lower jaw collected during the late 19th century by Othniel Charles Marsh's workers at Como Bluff. He tentatively described the genus as a lizard, noting that it could instead be a frog. New material of ''Cteniogenys'' from Europe prompted Susan E. Evans to reclassify it as an early choristodere in 1989. To date it is only known from fragmentary specimens. In phylogenic analyses it has been found to the basal most choristodere.

See also

* Paleobiota of the Morrison Formation

References

Choristodera
Jurassic reptiles
Late Jurassic reptiles of North America
Jurassic Colorado
Jurassic geology of Oklahoma
Jurassic geology of South Dakota
Jurassic geology of Utah
Jurassic geology of Wyoming
Late Cretaceous reptiles of North America
Fossil taxa described in 1928
Prehistoric reptile genera

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