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

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CHAPTER VIII.VARIOUS EXTINCT ANIMALS;—AND ON THE ANTIQUITYGENEEA OF INSECTS AND LAND MOLLUSCA.OF THEEXTINCT MAMMALIA OF AUSTRALIA.<strong>The</strong>se have all been obtained from caves and late Tertiary orPost-Tertiary deposits, and consist <strong>of</strong> a large number <strong>of</strong> extinctforms, some <strong>of</strong> gigantic size, but all marsupials and allied to <strong>the</strong>existing fauna. <strong>The</strong>re are numerous forms <strong>of</strong> kangaroos, somelarger than any living species ;and among <strong>the</strong>se are two genera,Protemnodon and S<strong>the</strong>nurus, which Pr<strong>of</strong>essor Garrod has latelyshown to have been allied, not to any Australian forms, but to<strong>the</strong> Dmdrolagi or tree-kangaroos <strong>of</strong> New Guinea. We havealso remains <strong>of</strong> Thylacinus and Dasyurus, which now only existin Tasmania ; and extinct species <strong>of</strong> Hypsiprymnus and Phasco-Among <strong>the</strong> more remarkablelomys, <strong>the</strong> latter as large as a tapir.extinct genera are Diprotodon, a huge thick-limbed animalallied to <strong>the</strong> kangaroos, but nearly as large as an elephant;Noto<strong>the</strong>rivm, having characters <strong>of</strong> Macropus and Phascolarctoscombined, and as large as a rhinoceros ; and Thylacoho, a phaianger-likemarsupial nearly as large as a lion, and supposed byPr<strong>of</strong>essor Owen to have been <strong>of</strong>opinion isnot held by o<strong>the</strong>r naturalists.Here <strong>the</strong>n we find <strong>the</strong> same phenomena as incarnivorous habits, though this<strong>the</strong> o<strong>the</strong>r countrieswe have already discussed,—<strong>the</strong> very recent disappearance<strong>of</strong> a large number <strong>of</strong> peculiar forms, many <strong>of</strong> <strong>the</strong>m far surpassingin size any that continue to exist. It hardly seems probablethat in this case <strong>the</strong>ir disappearance can have been due to <strong>the</strong>direct effects <strong>of</strong> <strong>the</strong> Glacial epoch, since no very extensive glacia-

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