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Clidastes propython: A small mosasaur from the Upper Smoky Hill Chalk Copyright © 2001-2008 by Mike Everhart Created 01/14/01- Updated 01/07/2008 |
Clidastes mosasaurs were the smallest in size of the three major groups of mosasaurs found in the Western Interior Sea during the deposition of the Smoky Hill Chalk and are among the most primitive of the known mosasaurs. Maximum length was about 4 meters in the chalk and slightly larger in the Pierre Shale. Clidastes was much more common along the Gulf Coast than in the Western Interior Sea.
Clidastes liodontus is found in the lower section of the chalk (late Coniacian) and may actually be one of the first mosasaurs to enter the seaway (see Martin and Stewart, 1977) during the Turonian. Clidastes propython, however, arrived much later and is only found in the upper sections of the chalk. According to Williston and others, it may have preferred to live much closer to shore and thus would not be well represented in the mid-ocean area where the chalk was deposited.
This specimen was collected from Logan County in the Zone of Hesperornis (Stewart, 1990), in the vicinity of Hattin's (1982) Marker Unit 22 (early Campanian). It consists of most of the skull and about 25 vertebrae. Some of the specimen had eroded out before being discovered and was weathered into many fragments. Other parts were recovered in situ. The specimen is currently in a private collection.

The skull of Clidastes propython adapted from Williston (1898).
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Five views of the quadrates of Clidastes propython. (left to right) 1). Anterior aspects of the left and right quadrates. 2) Posterior view of the left and right quadrates. 3) A posterior view of the left quadrate laying against the right quadrate. 4) A posterior view of the right quadrate showing the stapedial pit. 5) A ventral view of the right quadrate showing the surface of the condyle that articulates with the lower jaw.


The type specimen of Clidastes propython was described by E. D. Cope in 1869 from a specimen found in Alabama. The specimen is curated in the Academy of Natural Sciences in Philadelphia. These pictures were shot during my visit in November of 2002.
Additional reading about Clidastes:
Bell, G. L. Jr., 1997. A phylogenetic revision of North American and Adriatic Mosasauroidea. pp. 293-332 In Callaway J. M. and E. L Nicholls, (eds.), Ancient Marine Reptiles, Academic Press.
Cope, E. D., 1869. [Remarks on fossil reptiles, Clidastes propython, Polycotylus latipinnis, Ornithotarsus immanis.]. Proc. Amer. Philos. Soc. xi p. 117.
Everhart, M. J., P. A. Everhart and J. Bourdon, 1997 Earliest documented occurrence of the mosasaur, Clidastes liodontus, in the Smoky Hill Chalk (upper Cretaceous) of western Kansas. Kansas Acad. Sci. Trans. 16(Abstracts):14.
Everhart, M. J., 2001. Revisions to the Biostratigraphy of the Mosasauridae (Squamata) in the Smoky Hill Chalk Member of the Niobrara Chalk (Late Cretaceous) of Kansas. Kansas Acad. Sci. Trans 104(1-2):56-75.
Hattin, D. E., 1982. Stratigraphy and depositional environment of the Smoky Hill Chalk Member, Niobrara Chalk (Upper Cretaceous) of the type area, western Kansas. Kansas Geological Survey Bulletin 225, 108 pp.
Kiernan, C. R., 1992. Clidastes Cope, 1868 (Reptilia, Sauria): Proposed designation of Clidastes propython Cope, 1869 as the type species. Bull. Zool. Nomencl. 49 p. 137-139.
Martin, L. D. and J. D. Stewart, 1977.The oldest (Turonian) mosasaurs from Kansas, Jour. Paleon., 51(5):973-975.
Russell, D. A., 1967. Systematics and morphology of American mosasaurs. Peabody
Museum of Natural History, Yale University, Bulletin 23.
Williston, S. W., 1893. Mosasaurs, Part II: Restoration of Clidastes, Kans. Univ.
Quart., 2(2):83-84, 1 plate.
Williston, S. W., 1898. Mosasaurs. The University Geological Survey of Kansas, Volume IV, Paleontology, Part V, pp. 81-347.
Wright, K. R., 1987. The mosasaur Clidastes: new specimens and new
problems. Jour. Alabama Acad. Sci. 58(3):99. (Abs.)
Wright, K. R., 1988. The first record of Clidastes liodontus (Squamata,
Mosasauridae) from the eastern United States, Jour. Vert. Paleon., 8(3):343-345.