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1859
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1859
1860
1861
1866
1872

alternations of the Glacial 1869 1872
Glacial 1859 1860 1861 1866

were 1859 1860 1861 1869 1872
will have been 1866

the more powerful and were able to hold their places on the mountains, and afterwards to migrate southward with the 1869 1872
enabled to beat the less powerful 1859 1860 1861 1866

forms; but not so the southern in regard to the northern forms. 1869 1872
forms. 1859 1860 1861 1866

we see 1869
as we see 1859 1860 1861 1866
OMIT 1872

that 1859 1860 1861 1866 1869
we see that 1872

New Zealand, and to 1869 1872
and in 1859 1860 1861 1866

OMIT 1869 1872
to a certain extent 1859 1860 1861 1866

the northern hemisphere, 1866 1869 1872
Europe, 1859 1860 1861

Before the last great Glacial period, no doubt 1869 1872
Something of the same kind must have occurred on 1859 1860 1861
Before the Glacial period, no doubt 1866

OMIT 1866 1869 1872
no doubt before the Glacial period they 1859 1860 1861

those which have become naturalised; 1869 1872
the naturalised; 1859 1860 1861
those which have become naturalised there; 1866

OMIT 1869 1872
if the natives have not been actually exterminated, their numbers have been greatly reduced, and 1859 1860 1861 1866

their inhabitants have 1869 1872
the intertropical mountains before the Glacial period must have been completely isolated; and I believe that the productions of these islands on the land 1859 1860 1861
the intertropical mountains before the Glacial period must have been completely isolated; and I believe that the inhabitants of these islands on the land 1866

yielded and are still yielding to continental forms 1869 1872
lately yielded to continental forms, 1859 1860 1861
yielded to continental forms lately 1866

the alternations of the Glacial
period,
periods,
the northern forms were the more powerful and were able to hold their places on the mountains, and afterwards to migrate southward with the southern forms; but not so the southern in regard to the northern forms.
Just in
In
the same manner we see at the present day, that very many European productions cover the ground in La Plata, New Zealand, and to a lesser degree in Australia, and have OMIT beaten the natives; whereas extremely few southern forms have become naturalised in any part of the northern hemisphere, though hides, wool, and other objects likely to carry seeds have been largely imported into Europe during the last two or three centuries from La Plata, and during the last
forty
thirty
or
fifty
forty
years from Australia. The Neilgherrie mountains in India, however, offer a partial exception; for here, as I hear from Dr. Hooker, Australian forms are rapidly sowing themselves and becoming naturalised. Before the last great Glacial period, no doubt the intertropical
mountains:
mountains
OMIT were stocked with endemic Alpine forms; but these have almost
every-where
everywhere
largely
....
yielded to the more dominant forms, generated in the larger areas and more efficient workshops of the north. In many islands the native productions are nearly
equalled
equalled,
or even
outnumbered
out-numbered,
outnumbered,
by those which have become naturalised; and OMIT this is the first stage towards
extinction.
their extinction.
A
....
mountain
Mountains
is an
are
island
islands
on the
land;
land,
and their inhabitants have
have yielded
yielded
to those produced within the larger areas of the north, just in the same way as the
productions
inhabitants
of real islands have everywhere yielded and are still yielding to continental forms naturalised
by
there through
through
man's
mans
agency.
The same principles apply to the distribution of terrestrial animals and of marine productions, in the