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

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;chat, vi.] MAMMALIA OF THE OLD WORLD. 113A more interesting fact for us is <strong>the</strong> occurrence <strong>of</strong> <strong>the</strong> genusTapirus in <strong>the</strong> Newer Pliocene <strong>of</strong> France and in <strong>the</strong> older beds<strong>of</strong> both France and England, since this genus is now isolatedin <strong>the</strong> remotest parts <strong>of</strong> <strong>the</strong> eastern and western tropics. <strong>The</strong>genera Rhinoceros, Hippopotamus, and Sus, occur here asin <strong>the</strong>preceding epoch.We next come to <strong>the</strong> deer genus {Cervus), which appears tohave been at its maximum in this period, no less than eightspecies occurring in <strong>the</strong> Norwich Crag, and Forest-beds. Among<strong>the</strong> Bovidae, <strong>the</strong> antelopes, ox, and bison, are <strong>the</strong> only forms representedhere, as in <strong>the</strong> Post- Pliocene period. Passing on to <strong>the</strong>Proboscidea, we find three species <strong>of</strong> elephants and two <strong>of</strong> Mastodonpreserved in European beds <strong>of</strong> this period, all distinct fromthose <strong>of</strong> Post-Pliocene times.Rodentia.—In this order we find representatives <strong>of</strong> manyliving European forms ; as Cricetus (hamster), Arvicola (vole),Castor (beaver), Arctomys (marmot), Hystrix (porcupine),Lepus (hare), and Lagomys (pika) ; and a few that are extinct,<strong>the</strong> most important being Chalicomys, allied to <strong>the</strong> beaverand Issiodromys, said to come nearest to <strong>the</strong> remarkablePedetes <strong>of</strong> South Africa, both found in <strong>the</strong> Pliocene formations<strong>of</strong> France.General Conclusions as to Pliocene and Post-Pliocene Faunas <strong>of</strong>Europe.—This completes <strong>the</strong> series <strong>of</strong> fossil forms <strong>of</strong> <strong>the</strong> Pliocenedeposits <strong>of</strong> Europe. <strong>The</strong>y show us that <strong>the</strong> presence <strong>of</strong> numerouslarge carnivora and ungulates (now almost wholly tropical) in<strong>the</strong> Post- Pliocene period, was due to no exceptional or temporarycause, but was <strong>the</strong> result <strong>of</strong> a natural succession from similarraces which had inhabited <strong>the</strong> same countries for long precedingages. In order to understand <strong>the</strong> vast periods <strong>of</strong> time coveredbv <strong>the</strong> Pliocene and Post-Pliocene formations, <strong>the</strong> works <strong>of</strong> SirCharles Lyell must be studied. We shall <strong>the</strong>n come to see, that<strong>the</strong> present condition <strong>of</strong> <strong>the</strong> fauna <strong>of</strong> Europe is wholly new andexceptional. For a long succession <strong>of</strong> ages, various* forms <strong>of</strong>monkeys, hyaenas, lions, horses, hipparions, tapirs, rhinoceroses,hippopotami, elephants, mastodons, deer, and antelopes, toge<strong>the</strong>r

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