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

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chap, vi.] MAMMALIA OF THE OLD WORLD. 123<strong>of</strong> mastodons ranged over India, <strong>the</strong>ir remains being found in all<strong>the</strong> deposits from <strong>the</strong> Siwalik Hills to Burmah. A large Dino<strong>the</strong>riumhas also been found at Perim Island.Beptiles.—Many remains <strong>of</strong> birds were found, but <strong>the</strong>se havenot been determined. Reptiles were numerous and interesting,<strong>the</strong> most remarkable being <strong>the</strong> huge tortoise, Golossochclys, whoseshell was twelve feet long and head and neck eight feet more.O<strong>the</strong>r small tortoises <strong>of</strong> <strong>the</strong> genera Testudo, Emys, Trionyxand Emydida were found, <strong>the</strong> Emys being a living species.<strong>The</strong>re were three extinct and one living species <strong>of</strong> crocodile,and one <strong>of</strong> <strong>the</strong>m was larger than any now living. <strong>The</strong> onlyo<strong>the</strong>r reptile <strong>of</strong> importance was a large lizard <strong>of</strong> <strong>the</strong> genusVaranus.General Observations on <strong>the</strong> Miocene faunas <strong>of</strong> Europe andAsia.— Comparing <strong>the</strong> three faunas <strong>of</strong> approximately <strong>the</strong> sameperiod, and allowing for <strong>the</strong> necessarily imperfect record <strong>of</strong>each, we find a wonderful similarity <strong>of</strong> general type over <strong>the</strong>enormous areabetween France on <strong>the</strong> west and <strong>the</strong> Irawaddyriver in Burmah on <strong>the</strong> east. We may even extend our comparisonto Nor<strong>the</strong>rn China, where remains <strong>of</strong> Hywna, Tapir,Rhinoceros, Chalico<strong>the</strong>rium, and Elephas, have been recentlyfound, closely resembling those from <strong>the</strong> Miocene or Pliocenedeposits <strong>of</strong> Europe or India, and showing that <strong>the</strong> Palasarcticregion had <strong>the</strong>n <strong>the</strong> same great extent from west to eastthat it has now. Of about forty genera comprised in <strong>the</strong>Indian Miocene fauna, no less than twenty-seven inhabitedCentral and Western Europe during <strong>the</strong> same epoch. <strong>The</strong> IndianMiocene fossils are much what we should expect as <strong>the</strong> forerunners<strong>of</strong> <strong>the</strong> existing fauna, <strong>the</strong> giraffes and hippopotamibeing <strong>the</strong> only additions from <strong>the</strong> present Ethiopian fauna.<strong>The</strong> numerous forms <strong>of</strong> <strong>the</strong> restricted bovine type, show that<strong>the</strong>se probably originated in India ; while <strong>the</strong> monkeys appearto be altoge<strong>the</strong>r <strong>of</strong> Oriental types.In Europe, however, we meet <strong>with</strong> a totally different assemblage<strong>of</strong> <strong>animals</strong> from those that form <strong>the</strong> existing fauna. Wefind apes and monkeys, many large Felidse, numerous civets

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