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1859
1860
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1866
1869
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1859
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1869
1872

1 blocks not present in 1866 1869 1872; present in 1859 1860 1861
If the climate, since the Glacial period, has ever been in any degree warmer than at present (as some geologists in the United States believe to have been the case, chiefly from the distribution of the fossil Gnathodon), then the arctic and temperate productions will at a very late period have marched a little further north, and subsequently have retreated to their present homes; but I have met with no satisfactory evidence with respect to this intercalated slightly warmer period, since the Glacial period.

moved first southward and afterwards backwards to the north, in unison with the changing climate, they will not 1866 1869 1872
during their long southern migration and re-migration northward, will 1859 1860 1861

during their long migrations to any great diversity of temperature, 1866
to nearly the same climate, 1859 1860 1861
during their long migrations to any great diversity of temperature; 1869 1872

they will all have migrated 1866
is especially to be noticed, they will have kept 1859 1860 1861
they all migrated 1869 1872

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

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

migration across the
low
....
intervening
tracts, since
lowlands, now
become too warm for their existence.
The
As the
arctic
forms,
forms
moved first southward and afterwards backwards to the north, in unison with the changing climate, they will not have been exposed during their long migrations to any great diversity of temperature,
and,
and
as they will all have migrated in a body
together;
together,
consequently
....
their mutual relations will not have been much
disturbed,
disturbed.
and,
Hence,
in accordance with the principles inculcated in this volume,
they
these forms
will not have been liable to much modification. But with
our
the
Alpine productions, left isolated from the moment of the returning warmth, first at the bases and ultimately on the summits of the mountains, the case will have been 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
remain
still 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 illustrating what, as I believe, actually took place during the Glacial period, I
assumed
have assumed
that at
the
its
commencement