Gilmore, C. W.
An extinct sea-lizard from western Kansas.
Scientific American, 124:273&280, 3 figs.
Copyright © 2003-2009 by Mike Everhart
ePage created 10/22/2003 - Last updated 07/12/2009
LEFT: An illustration from Gilmore's 1921 article. See a more recent picture of this specimen at the Smithsonian HERE
|Wherein Charles W. Gilmore describes mosasaurs in general and a
new specimen in particular, which, at the time, had recently (1918) been collected by Charles Sternberg. Although the Smithsonian had
acquired many fragmentary mosasaur specimens from the chalk, some as early as the late
1860s that were collected by Dr. George M. Sternberg, they did
not have a complete skeleton until the present exhibit specimen of Tylosaurus proriger
LEFT: (Click to enlarge) "Tylosaurus in life, as reconstructed by the Smithsonian scientists" (Drawing by Charles R. Knight). This drawing, incorrect as it is, probably served as the basis for the life-sized model of a mosasaur at the Sternberg Museum of Natural History. Note that the Knight's addition of dorsal fringe was from a mistaken interpretation by S. W. Williston.
An Extinct Sea Lizard from Western Kansas
By Charles W. Gilmore
THE chalk deposits of western Kansas have long been famous on account of the great number and the fine state of preservation of the fossil remains found in them. For more than fifty years collectors of fossils have searched the chalk exposures for their hidden treasures. Remains of fish, large and small, turtles, toothed birds, lizards, both swimming and flying, and an occasional dinosaurian reptile have been the rewards of these indefatigable hunters.
The United States National Museum numbers among its rarest treasures fossil remains of all of these several kinds of animals, but quite recently there has been added to the exhibition series the very fine specimen of a swimming or sea lizard shown in the accompanying illustration. This animal goes under the name of Tylosaurus proriger, and belongs to a group of extinct reptiles commonly called Mosasaurs. The Mosasaurs were water living reptiles, with long slender bodies having the limbs modified into short swimming paddles, and a long powerful compressed tail with which they propelled themselves through the water. This specimen, after many weeks of the most painstaking care and skilful work, was cleaned from the investing chalk, the broken parts repaired and the missing bones restored, until finally the skeleton was articulated in the pose shown. It forms a wall panel, the skeleton being in half relief, the dark bone of the specimen standing out in bold contrast against the light yellowish color of the background, which has been made in imitation of the yellow chalk in which the specimen was originally found. The pose adopted for the skeleton was largely determined by the curved articulated sections of the backbone as found in the ground.
This specimen was collected for the National Museum by the veteran collector of fossils, Mr. Charles H. Sternberg, on Butte Creek, Logan County, Kansas, in 1917. Mr. Sternberg and his three sons, all of whom have been raised as fossil hunters, have collected hundreds of these ancient monsters and the results of their discoveries are to be found in all of the principal museums of the world, the present specimen being still another contribution to the science to which they have given so much.
The Tylosaurus specimen, as now exhibited, measures about twenty-five feet in length, with a head that is three and one-half feet long. The largest of the Mosasaurs, however, sometimes attained a length of forty feet, and such an animal would have a head fully five feet long. Some of the small adult species were scarcely more than eight feet in length.
The seas that rolled over Kansas in Cretaceous times contained thousands of these animals, and in the chalk bluffs of that region their remains are in such a perfect state of preservation that we are not only acquainted with their skeletal structure but with their external appearance as well. Impressions made by the body in these soft sediments before decomposition had set in have been found, showing that in life they were covered with small overlapping scales. In fact, small areas of skin impressions were found with the Tylosaurus specimen here discussed. The most unusual discovery relating to the appearance in life of an animal long extinct, was the detection of color markings by Doctor Williston, who
(Continued on page 280)
An Extinct Sea Lizard from Western Kansas
(Continued from page 273)
observed on one specimen carbonized pigment, which showed that the sides of the body were marked by narrow, diagonally placed parallel bars.
One of the unique features of Tylosaurus, and for that matter of all mosasaurs, is an articular joint in about the middle of each lower jaw, which permits considerable movement between the front and back parts, both up and down and sideways, though chiefly in the latter direction. This feature in conjunction with their very loose attachment to one another at the forward ends allowed the jaws to expand and thus enabled them to swallow large objects, for it is certain that not all of the animals which the Tylosaurus devoured were small, for since their teeth were not adapted for the rending of bodies they must have been swallowed whole.
While most of the Mosasaurs were predatory animals having the jaws provided with numerous sharply pointed teeth that were well adapted for catching fish - for it is thought fish formed their principal article of diet, since fish bones and scales have been found among the fossilized stomach contents - there was another kind of Mosasaur, Globidens alabamaensis [sic], that formerly lived in North America and enjoyed quite a different kind of food as shown by the very peculiar shape of its teeth. Reference is made to a specimen in the National Museum found some few years ago in the northern part of the State of Alabama which has nearly spherical teeth.
Mosasaur specimens have not only been found in many parts of the United States, but in South America, Belgium, Holland, Russia, France and New Zealand, but nowhere are they more abundant or are their remains found in a more perfect state of preservation than in the chalk deposits of western Kansas.
Everhart, M. J. 2000. Mosasaurs: Last of the great marine reptiles. Prehistoric Times. 44:29-31.
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 Academy of Science, Transactions 104(1-2):56-75. (Web version)
Everhart, M. J. 2002. New data on cranial measurements and body length of the mosasaur, Tylosaurus nepaeolicus (Squamata; Mosasauridae), from the Niobrara Formation of western Kansas. Kansas Academy of Science, Transactions 105(1-2):33-43.
Everhart, M. J. 2004. Plesiosaurs as the food of mosasaurs; new data on the stomach contents of a Tylosaurus proriger (Squamata; Mosasauridae) from the Niobrara Formation of western Kansas. The Mosasaur 7:41-46.
Everhart, M. J. 2005. Oceans of Kansas - A Natural History of the Western Interior Sea. Indiana University Press, 322 pp.
Marsh, O. C. 1872. Discovery of the dermal scutes of mosasaurid reptiles. American Journal of Science, Series 3, 16:290-292 (The scleral ring of mosasaurs)
Marsh, O. C. 1872. Notice of a new species of Hadrosaurus. American Journal of Science, Series 3, 16:301.
Snow, F. H. 1878. On the dermal covering of a mosasauroid reptile. Kansas Academy of Science, Transactions 6:54-58, Fig. 1-2. (The first discovery of mosasaur skin impressions)
Sternberg, C. H. 1909. An armored dinosaur from the Kansas chalk. Kansas Academy of Science, Transactions 22: 257-258.
Sternberg, C. H. 1922. Explorations of the Permian of Texas and the chalk of Kansas. 1918. Kansas Academy of Science, Transactions 30(1):119-120.
Williston, S. W. 1891. Kansas mosasaurs. Science 18(463):345.