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

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chap. VII.] MAMMALIA OF THE NEW WORLD. 131inhabited North America at a comparatively recent epoch, ismost remarkable. In Europe, we found a striking changein <strong>the</strong> fauna at <strong>the</strong> same period; but that consisted almostwholly in <strong>the</strong> presence <strong>of</strong> <strong>animals</strong> now inhabiting countriesimmediately to <strong>the</strong> north or south. Here we have <strong>the</strong> appearance<strong>of</strong> two new assemblages <strong>of</strong> <strong>animals</strong>, <strong>the</strong> one now confinedto <strong>the</strong> Old World—horses, camels, and elephants ; <strong>the</strong>o<strong>the</strong>r exclusively <strong>of</strong> South American type—Hamas, tapirs,capybaras, Galera, and gigantic Edentata. <strong>The</strong> age <strong>of</strong> <strong>the</strong>various deposits in which <strong>the</strong>se remains are found is somewhatuncertain, and probably extends over a considerable period <strong>of</strong>time, inclusive <strong>of</strong> <strong>the</strong> Glacial epoch, and perhaps both anteriorand subsequent to it. We have here, as in Europe, <strong>the</strong> presenceand apparent co-existence in <strong>the</strong> same area, <strong>of</strong> Arctic andSou<strong>the</strong>rn forms—<strong>the</strong> walrus and <strong>the</strong> manatee— <strong>the</strong> musksheepand <strong>the</strong> gigantic sloths. Unfortunately, as we shall see,<strong>the</strong> immediately preceding Pliocene deposits<strong>of</strong> North Americaare ra<strong>the</strong>r poor in organic remains ;yet it can hardly be owingto <strong>the</strong> imperfection <strong>of</strong> <strong>the</strong> record <strong>of</strong> this period,<strong>the</strong> South American types above numerated occursthat not one <strong>of</strong><strong>the</strong>re, whilea considerable number <strong>of</strong> Old World forms are represented.Nei<strong>the</strong>r in <strong>the</strong> preceding wonderfully rich Miocene or Eoceneperiods, does any one <strong>of</strong> <strong>the</strong>se forms occur ;or, <strong>with</strong> <strong>the</strong> exception<strong>of</strong> Moro<strong>the</strong>rium, from Pliocene deposits west <strong>of</strong> <strong>the</strong> RockyMountains, any apparent ancestor <strong>of</strong> <strong>the</strong>m ! Wehave hereunmistakable evidence <strong>of</strong> an extensive immigration from Southinto North America, not very long before <strong>the</strong> beginning <strong>of</strong> <strong>the</strong>Glacial epoch. It was an immigration <strong>of</strong> types altoge<strong>the</strong>r newto <strong>the</strong> country, which spread over all <strong>the</strong> sou<strong>the</strong>rn and centralportions <strong>of</strong> it, and established <strong>the</strong>mselves sufficiently to leaveabundance <strong>of</strong> remains in <strong>the</strong> few detached localities where <strong>the</strong>yhave been discovered. How such large yet defenceless <strong>animals</strong>as tapirs and great terrestrial sloths, could have made <strong>the</strong>ir wayinto a country abounding in large felines equal in size anddestructiveness to <strong>the</strong> lion and <strong>the</strong> tiger, <strong>with</strong> numerous wolvesand bears <strong>of</strong> <strong>the</strong> largest size, is a great mystery. But it isnever<strong>the</strong>less certain that <strong>the</strong>y did so ;and <strong>the</strong> fact that no such

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