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Text in this page (from paragraph 3900, sentence 100, word 1 to paragraph 3900, sentence 300, word 31) is not present in 1869
Now let us see whether Mr. Crolls conclusion that when the northern hemisphere suffered from the extreme cold of the great Glacial period, the southern hemisphere was actually warmer, throws any clear light on the present apparently inexplicable distribution of various organisms in the temperate parts of both hemispheres, and on mountains of the tropics. The Glacial period, as measured by years, must have been very long; and when we remember over what vast spaces some naturalised plants and animals have spread within a few centuries, this period will have been ample for any amount of migration. As the cold became more and more intense, we know that Arctic forms invaded the temperate regions; and, from the facts just given, there can hardly be a doubt that some of the more vigorous, dominant, and widest-spreading temperate forms actually then invaded the equatorial lowlands.
Text in this page (from paragraph 4000, sentence 310 to paragraph 4000, sentence 340, word 23) is not present in 1869
It should be observed that the northern .. forms found on the mountain-ranges of the ... intertropical regions and in the southern parts of the southern hemisphere are not arctic, but belong to the temperate zones: as Mr. H. C. Watson has recently remarked, "in receding from polar towards equatorial latitudes, the Alpine or mountain floras really become less and less arctic." Of these forms, some few are identical with northern temperate species, or are varieties of them, whilst others are ranked by all naturalists as closely allied to, but specifically distinct from, their northern representatives.
Now let us see what light can be thrown on the foregoing facts, on the belief, supported as it is by a large body of geological evidence, that the whole world, or a large part of it, was simultaneously colder during the Glacial period than at present. The Glacial period, as measured by years, must have been very long; and when we remember over what vast spaces some naturalised plants and animals have spread within a few centuries, this period will have been ample for any amount of migration. As the cold came slowly on, the tropical plants and animals will have retreated from both sides towards the equator, followed in the rear by the temperate productions, and these by the arctic; but with the latter we are not now concerned. The whole problem of what will have occurred is excessively complex. The probable existence before the Glacial period of a pleistocene equatorial flora and fauna, fitted for a hotter climate than any now existing, must not be over-looked. This old equatorial flora will have been almost wholly destroyed, and the two pleistocene sub-tropical floras, commingled and reduced in number, will then have formed the equatorial flora. There will also probably have been during the Glacial period great changes in the precise nature of the climate, in the degree of