The whole text of this page (from paragraph 4000, sentence 1000, word 15 to paragraph 4100, sentence 200, word 32) is not present in 1869 |
by a dry climate; for Dr. Falconer informs me that it is the damp with the heat of the tropics which is so destructive to perennial plants from a temperate climate. On the other hand, the most humid and hottest districts
will will 1859 1860 1861 | would 1866 |
have afforded an asylum
to to 1859 1860 1861 | for 1866 |
the
tropical tropical 1859 1860 1861 | tropical 1866 |
natives. The mountain-ranges north-west of the Himalaya, and the long line of the Cordillera, seem to have afforded two great lines of invasion: and it is a striking fact,
lately lately 1859 1860 1861 | lately 1866 |
communicated to me by Dr. Hooker, that all the flowering plants, about forty-six in number, common to Tierra del Fuego and to
Europe Europe 1859 1860 | Europe, 1861 1866 |
still exist in North America, which must have lain on the line of march. ↑1 blocks not present in 1859 1860 1861 1869 1872; present in 1866 | We might of course speculate on the land having been formerly higher than at present in various parts of the tropics, where temperate forms apparently have crossed; but as the lines of migration have been so numerous, such speculations would be rash.
|
But But 1859 1860 1861 | Hence 1866 |
I
do not doubt that do not doubt that 1859 1860 1861 |
am forced to believe that in certain regions, as in India, 1866 |
some temperate productions entered and crossed even the
lowlands
lowlands
1859 1860 1866 | lowlands 1861 |
of the tropics at the period when the cold was most intense,— when arctic forms
had migrated some had migrated some 1859 1860 1861 |
in Europe had migrated over at least 1866 |
twenty-five degrees of
latitude latitude 1859 1860 1861 | latitude, 1866 |
from their native country from their native country 1859 1860 |
from their native country, 1861 |
OMIT 1866 |
and covered the land at the foot of the Pyrenees. At this period of extreme cold, I believe that the climate under the equator at the level of the sea was about the same with that now felt there at the height of
six or seven six or seven 1859 1860 1861 |
from five to six 1866 |
thousand feet. During this the coldest period,
I suppose that I suppose that 1859 1860 |
OMIT 1861 1866 |
large spaces of the tropical lowlands were
clothed clothed 1859 1860 | probably clothed 1861 1866 |
with a mingled tropical and temperate vegetation, like that now growing with strange luxuriance at the base of the Himalaya,
as as 1859 1860 1861 |
at the height of four or five thousand feet, as so 1866 |
graphically described by Hooker. |
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Thus, as I believe, a considerable number of plants, a few terrestrial animals, and some marine productions, migrated during the Glacial period from the northern and southern temperate zones into the intertropical regions, and some even crossed the equator. As the warmth returned, these temperate forms would naturally ascend the higher mountains, being exterminated on the
lowlands; lowlands; 1859 1861 | low- lands; 1860 |
those which had not reached the
equator, equator, 1859 | equator 1860 1861 |
would re-migrate northward or southward towards their former
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