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1859
1860
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this we find has been the case; 1859 1860 1861 1866 1869
they have been modified; 1872

one with another, though 1866 1869 1872
though very 1859 1860 1861

or sub-species, and some as certainly 1866 1869
and some few are 1859 1860
and many are 1861
or sub-species, and some as 1872

each other on the several ranges. 1866 1869 1872
species. 1859 1860 1861

the foregoing illustration I have 1869 1872
illustrating what, as I believe, actually took place during the Glacial period, I 1859 1860 1861 1866

of our imaginary Glacial period, the 1869 1872
the 1859 1860 1861 1866

it is necessary also to 1869
the foregoing remarks on distribution apply not only to strictly arctic forms, but also to 1859 1860 1861 1866
it is also necessary to assume that 1872

for some of these are 1859 1860 1861 1866 1869
were 1872

lower mountain-slopes and 1866 1869
lower mountains and 1859 1860 1861
world, for some of the species which now exist 1872

plains 1859 1860 1861 1866 1869
lower mountain-slopes and on the plains 1872

and 1859 1860 1861 1866 1869
are the same; and 1872

somewhat
dif-
....
ferent;
different;
for it is not likely that all the same arctic species will have been left on
mountain ranges
mountain-ranges
distant
far distant
from each other, and have survived there ever since; they
will
will,
also
also,
in all
probability
probability,
have become mingled with ancient Alpine species, which must have existed on the mountains before the commencement of the Glacial epoch, and which during
the
its
coldest period will have been temporarily driven down to the plains; they will, also, have been
subsequently exposed
exposed
to somewhat different climatal influences. Their mutual relations will thus have been in some degree disturbed; consequently they will have been liable to modification; and this we find has been the case; for if we compare the present Alpine plants and animals of the several great European
mountain-ranges,
mountain-ranges
one with another, though many of the species
are
still remain
remain
identically the same, some
present
exist as
varieties, some
are ranked
....
as doubtful
forms,
forms
or sub-species, and some as certainly distinct yet closely allied
or
species
representative
representing
each other on the several ranges.
In the foregoing illustration I have
have assumed
assumed
that at
its
the
commencement of our imaginary Glacial period, the arctic productions were as uniform round the polar regions as they are at the present day. But it is necessary also to
many
include many
sub-arctic and
to
....
some few
northern
....
temperate
forms
forms,
for some of these are the same
round
on
the lower mountain-slopes and on the plains of North America and
Europe
Europe;
and it may be
reasonably
....
asked how I account for
the necessary
this
degree of uniformity
of
in
the sub-arctic and
northern
....
temperate forms round the world, at the commencement of the
Glacial
real Glacial
period. At the present day, the sub-arctic and northern temperate productions of the Old and New Worlds are separated from each other by the
Atlantic
whole Atlantic
Ocean and by the
extreme
....
northern part of the Pacific. During the Glacial period, when the
in-
....
habitants
inhabitants
of the Old and New Worlds lived