Cteniogenys is a genus of choristodere, a morphologically diverse group of aquatic reptiles. It is part of the monotypic family Cteniogenidae.[1] The type and only named species, C. antiquus, was named in 1928 by Charles W. Gilmore.[2] 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.
| Cteniogenys Temporal range: Middle-Late Jurassic,
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| Dentary of the holotype specimen VP.001088 | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Order: | †Choristodera |
| Family: | †Cteniogenidae Gilmore, 1928 |
| Genus: | †Cteniogenys Seiffert, 1975 |
| Species: | †C. antiquus
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| Binomial name | |
| †Cteniogenys antiquus Gilmore, 1928
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Description
editCteniogenys was 25 to 50 centimetres (9.8 to 19.7 in) long, and probably weighed less than 500 grams (1.1 lb). 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.[3]
Distribution
editFossils 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[4] the Bathonian aged Itat Formation of western Siberia,[5] and the Berriasian aged Angeac-Charente bonebed in France.[6]
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).[7] 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.[8][9]
Systematics
editThe 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.[3] New material of Cteniogenys from Europe prompted Susan E. Evans to reclassify it as an early choristodere in 1989.[10] To date it is only known from fragmentary specimens.[8] In phylogenic analyses it has been found to the basal most choristodere.[11]
| Choristodera |
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See also
editReferences
edit- ^ J. Seiffert. 1975. Upper Jurassic lizards from central Portugal. Contribuição para o conhecimento da Fauna do Kimerridgiano da Mina de Lignito Guimarota (Leiria, Portugal). Serviços Geológicos de Portugal, Memória (Nova Série) 22:7-85
- ^ C. W. Gilmore. 1928. Fossil lizards of North America. Memoirs of the National Academy of Sciences. 22(3):1-201
- ^ a b Foster, John (2007). Jurassic West: The Dinosaurs of the Morrison Formation and Their World. Bloomington, Indiana: Indiana University Press. pp. 146–148. ISBN 978-0-253-34870-8. OCLC 77830875.
- ^ Matsumoto, R.; Evans, S. E. (2010). "Choristoderes and the freshwater assemblages of Laurasia". Journal of Iberian Geology. 36 (2): 253–274. doi:10.5209/rev_JIGE.2010.v36.n2.11. ISSN 1698-6180.
- ^ "Middle Jurassic vertebrate assemblage of Berezovsk coal mine in western Siberia (Russia)". Global Geology. 19 (4): 187–204. 2016. doi:10.3969/j.issn.1673-9736.2016.04.01.
- ^ 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
- ^ Gao, K, and Fox, R.C., 1998. New choristoderes (Reptilia: Diapsida) from the Upper Cretaceous and Paleocene, Alberta and Saskatchewan, Canada, and phylogenetic relationships of the Choristodera. Zool J Linn Soc. 124:303–353.
- ^ a b Gao, Keqin; Brinkman, Donald E. (2005). "Choristoderes from the Park and its vicinity". In Currie, Phillip J.; Koppelhus, Eva (eds.). Dinosaur Provincial Park: A Spectacular Ancient Ecosystem Revealed. Bloomington: Indiana University Press. pp. 221–234. ISBN 0-253-34595-2.
- ^ Matsumoto, R, Suzuki, S, Tsogtbaatar, K, Evans, SE, 2009. New material of the enigmatic reptile Khurendukhosaurus (Diapsida: Choristodera) from Mongolia. Naturwissenschaften 96:233–242.
- ^ Evans, Susan E. (1989). "New material of Cteniogenys (Reptilia: Diapsida) and a reassessment of the phylogenetic position of the genus". Neues Jahrbuch für Geologie und Paläontologie, Monatshefte. 1989 (10): 577–589. doi:10.1127/njgpm/1989/1989/577.
- ^ Matsumoto, Ryoko; Dong, Liping; Wang, Yuan; Evans, Susan E. (2019-06-18). "The first record of a nearly complete choristodere (Reptilia: Diapsida) from the Upper Jurassic of Hebei Province, People's Republic of China". Journal of Systematic Palaeontology. 17 (12): 1031–1048. doi:10.1080/14772019.2018.1494220. ISSN 1477-2019. S2CID 92421503.
