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EXTINCT RODENTS Among extinct rodents, only a few of the more important types may be noticed. As to the origin of the See also:order, we are still to a See also:great extent in the dark; and even the relations of the Duplicidentata to the Simplicidentata are not yet fully understood. With regard to the latter point, it is, however, considered probable that both are branches of a See also:common stock, which diverged from each other before See also:ali the typical rodent characters were acquired. As to the ancestral stock of the order, it has been suggested that this is re-presented by certain See also:Lower See also:Eocene See also:European and See also:North See also:American mammals, at one See also:time regarded as See also:primitive See also:Primates. In See also:Europe these include Plesiadapis and Protoadapis, and in North See also:America Mixodectes, Microsyops and Cynodontomys; the last three constituting the See also:family Mixodectidae. Possibly the European forms, in which the dental See also:formula has been given as i. , c. 8, pi, m. I, and there is a See also:gap between the incisors and the cheek-See also:teeth, are more nearly related to See also:modern rodents than the American types, and may indeed belong to the same order. On the other See also:hand, the American forms, which have one pair of large See also:chisel-like incisors in the lower See also:jaw, also possess a lower canine, and show no marked gap in front of the cheek-teeth, nor any indication of the characteristic rodent backwards See also:movement of the lower jaw. On these grounds, while admitting that they are allied to the rodents, it has been pointed out that they can scarcely be included in the See also:Rodentia, and the order Proglires has in consequence been proposed for their reception. Whatever may be the true See also:affinity of these problematical mammals, undoubted rodents are known from the Lower Eocene of both Europe and North America. In Europe these See also:form the genus Ischyromys and the family Ischyromyidae, and have premolars 't, and all the cheek-teeth See also:low-crowned, with See also:simple cusps or ridges. Possibly they are akin to the Sciuridae. In America, Paramys, with transversely ridged Molars, is allied ; and the European Sciuromys should perhaps find a See also:place in the same neighbourhood. A more advanced phase is represented in the European Lower Oligocene by the Pseudosciuridae, with the genera Pseudosciurus, Sciuroides, Trechomys, Theridomys, &c., in which See also:part of the masseter passes through the broad infra-orbital See also:canal, and the premolars are i ; the molars being low-crowned, many-rooted and either cusped or ridged. These rodents are thought to be allied to the Anomaluridae ; and it is partly on their See also:evidence that the family Pedetidae is placed next the latter. Here it may be mentioned that Leithia, from the See also:Pleistocene of See also:Malta, originally regarded as a See also:giant See also:dormouse, seems near akin to Anomalurus. In the highly specialized mastoid region of the See also:skull, the North American Oligocene Protoptychus approaches to Dipopodomys, while the contemporary Gymnoptychus and Entoptychus likewise appear referable to the Geomyidae. The Upper Oligocene Cricetodon in Europe and Eumys in America are the earliest known forerunners of the cricetine Muridae; while at the same time primitive beavers appear in the form of Steneofiber, to be succeeded in the European Pleistocene by the gigantic Trogontherium. The still larger North American Pleistocene Castoroides, known by one See also:species of the See also:size of a See also:bear, and the allied See also:West See also:Indian Amblyrhiza, appear to be specialized beavers, although they have been referred to a family by themselves. Near akin is the North American See also:Miocene family Mylagaulidae, typified by Mylagaulus, but including Mesogaulus and Protogaulus. Although showing some dental characters approximating to the porcupines, these rodents are regarded as allied to the Castoridae, although forming an isolated type. The prominent feature, writes Mr E. S. Riggs, is the unusual development of the premolar to the exclusion of the posterior teeth. Associated with this is the strength and sharpness of the lower jaw, the prominence and anterior pcsition of the masseteric See also:ridge, and the See also:depth of the See also:ramus from the alveolar See also:line to the See also:angle. These indicate unusual capacity for crushing or grinding; while the last premolar is a crushing See also:implement, which has reached the highest degree of specialization known in Rodentia. It is suggested that these teeth may have been employed for cracking nuts or hard seeds, although also used for grinding. The remarkable North American Ceratogaulus, with a large bony nasal See also:horn, belongs to the same family. To discuss the remaining Miocene and later fossil Simplicidentata would be doing little more than adding to the generic names referable to the various existing families. It may be mentioned, however, that the See also:distribution of these later See also:Tertiary types accords very closely with that of their existing relatives; the families of See also:South American hystricoids being represented by a number of extinct genera in the formations of See also:Argentina and .See also:Brazil. See also:Special mention may be made of Megamys, from the caves of Brazil, which, while apparently allied to the living See also:viscacha, attained dimensions approximating to those of a See also:hippopotamus. As regards the Duplicidentata, it appears that the families Ochotonidae and Leporidae had become differentiated as See also:early as the Lower Miocene. Titanomys is the earliest form, from the See also:Middle Miocene, succeeded by Lagopsis, and then by the modern Ochotona. In this line there is a tendency to lose the last upper molar, but in Prolagus, which ranges in the See also:Pliocene from See also:Sardinia and See also:Corsica to See also:Spain, and forms a See also:side-See also:branch, the corresponding lower toothhas likewise disappeared. In contradistinction to Titanomys, in which the cheek-teeth are rooted, is the North American Upper Oligocene Palaeolagus, where they are rootless. In See also:general dental characters, especially the retention of three pairs of molars, this genus approximates to the Leporidae, although in the See also:absence of See also:post-orbital processes and the See also:pattern of the molars it departs less widely from the modern Ochotonidae than does Prolagus. Additional information and CommentsThere are no comments yet for this article.
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