| → specifically distinct, by others as varieties; but some are certainly identical, and many, though closely related to northern forms, must be ranked as distinct species. 1859 1860 1861 |
| closely allied to, but specifically distinct from, their northern representatives. 1866 |
|
| → what light can be thrown 1859 1860 1861 1866 |
| 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 1869 |
| whether Mr. Croll's 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 1872 |
|
| → 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 during the Glacial period simultaneously much colder than at present. 1860 1861 |
| 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 during the Glacial period simulta- neously much colder than at present. 1859 |
| 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. 1866 |
| present apparently inexplicable distribution of various organisms in the temperate parts of both hemispheres, and on mountains of the tropics. 1869 |
| present apparently inexplicable distribution of various organisms in the temperate parts of both hemispheres, and on the mountains of the tropics. 1872 |
|
| → came slowly on, all the tropical plants and other productions will have retreated from both sides towards the equator, followed in the rear by 1859 1860 1861 |
| came slowly on, the tropical plants and animals will have retreated from both sides towards the equator, followed in the rear by 1866 |
| became more and more intense, we know that Arctic forms invaded 1869 1872 |
|
| → these by the arctic; but with the latter we are not now concerned. 1859 1860 1861 1866 |
| 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. 1869 |
| from the facts just given, there can hardly be a doubt that some of the more vigorous, dominant and widest-spreading temperate forms invaded the equatorial lowlands. 1872 |
|
| ↑ 5 blocks not present in 1859 1860 1861 1869 1872; present in 1866 |
| 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 humidity, &c.; and various animals and plants will have migrated in different proportions and at different rates.
So that altogether during the Glacial period the inhabitants of the tropics must have been greatly disturbed in all their relations of life.
|
|
| ↑ 4 blocks not present in 1859 1860 1861 1866; present in 1869 1872 |
| The inhabitants of these lowlands
would at the same time migrate
to the tropical and sub-tropical regions of the south, for the southern hemisphere was at this period warmer.
On the decline of the Glacial period, as both hemispheres gradually recovered their former temperatures, the northern temperate forms living on the lowlands under the equator, would be
driven to their former homes or be
destroyed, being replaced by the equatorial forms returning from the south.
Some, however, of the northern temperate forms would almostc
ertainly
ascend
any adjoining high land, where, if sufficiently lofty, they would long
survive,
like the Arctic forms on the mountains of Europe.
They might survive,
even if the climate was not perfectly fitted for them, for the change of temperature must have been very slow, and plants undoubtedly possess a certain capacity for acclimatisation, as shown by their transmitting to their offspring different constitutional powers of resisting heat and cold.
|
|
| → The tropical plants probably 1859 1860 1861 |
| Hence they will have 1866 |
|
| → see 1859 1860 1861 |
| now see crowded together 1866 |
|
| → present day crowded together at the 1859 1860 1861 |
| OMIT 1866 |
|
| → lowest, most protected, and warmest districts. 1860 1861 1866 |
| warmest spots. 1859 |
|
| ↑ 2 blocks not present in 1859 1860 1861 1869 1872; present in 1866 |
| Nor must it be overlooked that, as the cold will have come on very slowly, it is almost certain that many of the inhabitants of the tropics will have become in some degree acclimatised; in the same manner as the same species of plant when living on lowlands and highlands certainly transmit to their seedlings different constitutional powers of resisting cold.
Nevertheless, it cannot be denied that all tropical productions will have greatly suffered, and the chief difficulty is to understand how they can have escaped entire annihilation.
|
|
