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See also:TITANOTHERIIDAE (also known as Menodontidae and Brontotheriidae) , a See also:family of large See also:rhinoceros-like perissodactyl ungulate mammals from the Oligocene and See also:Eocene strata of See also:North See also:America. The cheek-See also:teeth are See also:low-crowned, with the See also:external cones of the upper molars fused into a W-like See also:outer See also:wall, and the inner ones retaining a See also:regular conical See also:form; while in the See also:lower teeth the See also:crown is formed of crescentic ridges, of which there are three in the last and two each in the other teeth. There is generally little See also:gap between the canines and the premolars. Titanotherium, of the Oligocene of the Dakotas and neighbouring districts, was a huge beast, with the hinder upper premolars similar in See also:character to the molars, a pair of See also:horn-cores, arising from the maxilla, overhanging the See also:nose-cavity, four front and three See also:hind toes, only twenty dorso-lumbar vertebrae, and an almost continuous and unbroken See also:series of teeth, in which the canines are See also:short; the dental See also:formula being i. I, c. p. -, m. The muzzle probably formed a snout in See also:life; and there is presumptive See also:evidence that these animals were very See also:long-lived. Brontops seem scarcely separated from the type genus; but the name Brontotherium is applied to See also:species with two pairs of incisor teeth in both jaws. The length of the largest species was about 14 ft.; and the height about 8 ft. The alleged occurrence of remains of members of the See also:group in the Balkans apparently rests on insufficient evidence. A second group is typified by Palaeosyops, of the Bridger Eocene of North America; P. paludosus being an See also:animal about the See also:size of a See also:tapir. The See also:skull, which has a longer See also:face than in Titanotherium, lacks horn-cores, while all the upper premolars are simpler than the molars, and the full series of 44 teeth was See also:present. The limbs were relatively slender, and the See also:brain was small. In the lower, or Wasatch, Eocene the group was represented by the still more See also:primitive Lambdotherium. On the other See also:hand, Palaeosyops is connected with Titanotherium by means of Telmatotherium of the upper Bridger and Washakia Eocene, a larger animal, with a longer and flatter skull, showing rudiments of horn-cores, only two pairs of lower incisors, and a See also:general approximation in dental character to Titanotherium. Another of these titanotheroid forms is Diplacodon, from the Upper or Uinta Eocene; an animal the size of a rhinoceros, with the last two upper premolars molar-like. It was probably off the See also:direct ancestral See also:line of Titanotherium. These intermediate forms render the reference of the group to a distinct family—Palaeosyopidaeunnecessary. See also:Professor H. F. See also:Osborn, who recognises four genera, Titanotherium, Megacerops, Symborodon and Brontotherium, in the typical See also:section of the family, considers that each of these represents a distinct line of descent from the Palaeosyops-like group. The whole assemblage forms one of the four See also:main sections of the See also:Perissodactyla, namely the Titanotheroidea. See H. F. Osborn, " The See also:Cranial See also:Evolution of Titanotherium." See also:Bull. Amer. See also:Mus. (1896), viii., 137, and the " Four Phyla of Oligocene Titanotheres," op. cit. (1903), xvi. 91; C. H. See also:Earle, " A Memoir on the Genus Palaeosyops and its See also:Allies," Journ. Acad. See also:Philadelphia (1892), ix. 267. (R. Additional information and CommentsThere are no comments yet for this article.
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