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The geographical distribution of animals, with a study of the relations ...

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———140 DISTRIBUTION OF EXTINCT ANIMALS. [part ii.seven species allied to Tillo<strong>the</strong>rium and Anchippodus, and havingalso <strong>relations</strong>, as Pr<strong>of</strong>essor Cope believes, <strong>with</strong> <strong>the</strong> South AmericanToxodontidse.Rodentia.—This order is represented in <strong>the</strong> Pliocene by abeaver, a porcupine, and an American mouse (Hespervmys), allextinct species <strong>of</strong> living genera, <strong>the</strong> Hystrix being an Old Worldtype ; and Pr<strong>of</strong>essor Cope has recently described Panolax, anew genus <strong>of</strong> hares from <strong>the</strong> Pliocene <strong>of</strong> New Mexico. <strong>The</strong>Miocene deposits have furnished an extinct genus allied to <strong>the</strong>haresPalccolagus ; one <strong>of</strong> <strong>the</strong> squirrel familya small extinct form <strong>of</strong> beavermouseIschyromys ;Palceocastor ; and an extinctEumys. <strong>The</strong> Eocene strata <strong>of</strong> Wyoming have latelyfurnished two extinct forms <strong>of</strong> squirrel, Paramys and Sciuravus ;and ano<strong>the</strong>r <strong>of</strong> <strong>the</strong> Muridse (or mouse family), Mysops.Cetacea.—Numerous remains <strong>of</strong> dolphins and whales, belongingto no less than twelve genera, mostly extinct, have beenfound in <strong>the</strong> Miocene deposits <strong>of</strong> <strong>the</strong> Atlantic and Gulf States,from New Jersey to South Carolina and Louisiana ;while sevengenera <strong>of</strong> <strong>the</strong> extinct family, Zeuglodontidse, have been found inMiocene and Eocene beds <strong>of</strong> <strong>the</strong> same districts. Some remainsassociated <strong>with</strong> <strong>the</strong>se are doubtfully referred to <strong>the</strong> Seal family(Phocidae) among <strong>the</strong> Carnivora.Edentata.—Tillquite recently no remains <strong>of</strong> this order haveoccurred in any North American deposits below <strong>the</strong> Post- Pliocene;but in 1874 Pr<strong>of</strong>. Marsh described some remains allied toMegalonyx and Mylodon, from <strong>the</strong> Pliocene beds <strong>of</strong> Californiaand Idaho, and forming a new genus, Moro<strong>the</strong>rinm. As <strong>the</strong>seremains have only occurred to <strong>the</strong> west <strong>of</strong> <strong>the</strong> Eocky Mountains,and in Pliocene deposits whose exact age is not ascertained, <strong>the</strong>yhardly affect <strong>the</strong> remarkable absence <strong>of</strong> this group from <strong>the</strong>whole <strong>of</strong> <strong>the</strong> exceedingly rich Tertiary deposits in all o<strong>the</strong>r parts<strong>of</strong> North America.General Relations <strong>of</strong> <strong>the</strong> extinct Tertiary Mammalia <strong>of</strong> NorthAmerica and Europe.—Having now given a sketch <strong>of</strong> <strong>the</strong> extinctMammalia which inhabited Europe and North Americaduring <strong>the</strong> Tertiary period, we are enabled by comparing <strong>the</strong>m,

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