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

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328 ZOOLOGICAL GEOGRAPHY. [part hi.Insects.—<strong>The</strong> insects <strong>of</strong> Ceylon also furnish some curiousexamples <strong>of</strong> its distinctness from Hindostan, and its affinity <strong>with</strong>Malaya. Among its butterflies we find Papilio jophon, closelyallied to P. antiphus <strong>of</strong> Malaya. <strong>The</strong> remarkable genus Hestia, socharacteristic <strong>of</strong> <strong>the</strong> Malay archipelago, only occurs elsewhere on<strong>the</strong> mountains <strong>of</strong> Ceylon ; while its Cynthia and Parthcnos areAmongclosely allied to, if not identical <strong>with</strong>, Malayan species.Coleoptera we have yet more strikiDg examples. <strong>The</strong> highly characteristicMalayan genus Tricondyla is represented in Ceylon byno less than 10 species ;and among Longicorns we find <strong>the</strong> generaTetraommatus, Thranius, Cacia, Praonetha, Ropica, and Serixia,allexclusively Malayan or only just entering <strong>the</strong> Indo-Chinesepeninsula, yet all represented in Ceylon, while not a singlespecies occurs in any part <strong>of</strong> India or <strong>the</strong> Himalayas.<strong>The</strong> Past History <strong>of</strong> Ceylon and South-India as indicated by itsFauna.—In our account <strong>of</strong> <strong>the</strong> Ethiopian region we have alreadyhad occasion to refer to an ancient connection between this subregionand Madagascar, in order to explain <strong>the</strong> <strong>distribution</strong> <strong>of</strong><strong>the</strong> Lemurine type, and some o<strong>the</strong>r curious affinities between <strong>the</strong>two countries. This view is supported by <strong>the</strong> geology <strong>of</strong> India,which shows us Ceylon and South India consisting mainly <strong>of</strong>granitic and old metamorphic rocks, while <strong>the</strong> greater part <strong>of</strong> <strong>the</strong>peninsula, forming our first sub-region, is <strong>of</strong> tertiary formation,<strong>with</strong> a few isolated patches <strong>of</strong> secondary rocks. It is evident<strong>the</strong>refore, that during much <strong>of</strong> <strong>the</strong> tertiary period, Ceylon andSouth India were bounded on <strong>the</strong> north by a considerable extent<strong>of</strong> sea, and probably formed part <strong>of</strong> an extensive sou<strong>the</strong>rn continentor great island. <strong>The</strong> very numerous and remarkable cases<strong>of</strong> affinity <strong>with</strong> Malaya, require however some closer approximationto <strong>the</strong>se islands, which probably occurred at a later period.When, stilllater, <strong>the</strong> great plains and table-lands <strong>of</strong> Hindostanwere formed, and a permanent land communication effected <strong>with</strong><strong>the</strong> rich and highly developed Himalo-Chinese fauna, a rapid immigration<strong>of</strong> new types took place, and many <strong>of</strong> <strong>the</strong> less specialisedforms <strong>of</strong> mammalia and birds (particularly those <strong>of</strong> ancientAmong reptiles and insects <strong>the</strong>Ethiopian type) became extinct.competition was less severe, or <strong>the</strong> older forms were too well

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