→ throughout the world, the 1859 1860 1861 |
throughout the world, 1866 |
certain 1869 1872 |
|
→ and on the temperate lowlands 1859 1860 1861 1866 |
OMIT 1869 1872 |
|
→ northern and southern hemispheres, are sometimes identically 1859 1860 1861 1866 |
tropics in all parts of the world, and on the temperate plains of the north and south, are either 1869 1872 |
|
→ but they are much oftener specifically distinct, though related to each other in a most remarkable manner. 1859 1860 1861 |
but much oftener they are specifically distinct, though plainly related to each other in a remarkable manner. 1866 |
identical species or varieties of the same species. 1869 |
species or varieties of the same species. 1872 |
|
↑ 2 blocks not present in 1859 1860 1861 1866; present in 1869 1872 |
It should, however, be observed that these plants are not strictly Arctic
forms; for, as Mr. H. C. Watson has remarked, "in receding from polar towards equatorial latitudes, the Alpine or mountain floras really become less and less Arctic."
Besides these identical and closely allied forms, many species inhabiting the same widely sundered areas, belong to genera not now found in the intermediate tropical lowlands.
|
|
→ some strictly 1859 1860 1861 1866 |
but some few 1869 1872 |
|
→ on the distribution of 1859 1860 1861 1866 |
in regard to 1869 1872 |
|
↑ 5 blocks not present in 1859 1860 1861 1866; present in 1869 1872 |
From the foregoing facts, namely
the presence of temperate forms on the highlands across the whole of equatorial Africa, and along the Peninsula of India
to Ceylon and the Malay archipelago,
and in a less well-marked manner across the wide expanse of tropical South America, it appears almost certain that at some former period, no doubt during the most severe part of the
Glacial period, the lowlands of these great continents were everywhere tenanted under the equator by a considerable number of temperate forms.
At this period the equatorial climate at the level of the sea was probably about the same with that now experienced at the height of from five to six thousand feet under the same latitudes,
or perhaps even rather cooler.
During this, the coldest period, the lowlands under the equator must have been clothed with a mingled tropical and temperate vegetation, like that described by Hooker as growing luxuriantly at the height of from four to five thousand feet on the lower slopes of the Himalaya, but with perhaps a still greater preponderance of temperate forms.
So again,
on
the mountainous island of Fernando Po, in the Gulf of Guinea, Mr. Mann found temperate European forms beginning to appear at the height of about five thousand feet.
On the mountains of Panama, at the height of only two thousand feet, Dr. Seemann found the vegetation like that of Mexico, "with forms of the torrid zone harmoniously blended with those of the temperate."
|
|
→ southern hemisphere, and on the mountain-ranges of the 1859 1860 1861 |
OMIT 1866 |
|
→ are not arctic, but belong to 1859 1860 1861 |
and in 1866 |
|
→ temperate 1859 1860 1861 |
parts of the southern hemisphere are not arctic, but belong to the temperate 1866 |
|
→ Many of the forms living on the mountains of the warmer reigons of the earth and in the southern hemisphere are of doubtful value, being 1861 |
Many of the forms living on the mountains of the warmer regions of the earth and in the southern hemisphere are of doubtful value, being 1859 1860 |
Of these forms, some few are identical with northern temperate species, or are varieties of them, whilst others are 1866 |
|