See page in:
1859
1860
1861
1866
1869
1872

Compare with:
1859
1860
1861
1869
1872

With 1859 1860 1861 1866 1869
We may safely infer that with 1872

we may safely infer 1859 1860 1861 1866 1869
there has been 1872

assign due proportional weight to the following considerations.
Although each formation may mark a very long lapse of years, each
perhaps
probably
is short compared with the period requisite to change one species into another. I am aware that two palæontologists, whose opinions are worthy of much deference, namely Bronn and
Woodward,
Wood- ward,
Wood-ward,
have concluded that the average duration of each formation is twice or thrice as long as the average duration of specific forms. But insuperable difficulties, as it seems to me, prevent us
coming
from coming
to any just conclusion on this head. When we see a species first appearing in the middle of any formation, it would be rash in the extreme to infer that it had not elsewhere previously existed. So again when we find a species disappearing before the
uppermost
last
layers have been deposited, it would be equally rash to suppose that it then became
wholly
....
extinct. We forget how small the area of Europe is compared with the rest of the world; nor have the several stages of the same formation throughout Europe been correlated with perfect accuracy.
With marine animals of all
kinds
kinds,
we may safely infer a large amount of migration
due to
during
climatal and other changes; and when we see a species first appearing in any formation, the probability is that it only then first immigrated into that area. It is
well-known,
well known,
for instance, that several species appeared
somewhat
some-what
earlier in the palæozoic beds of North America than in those of Europe; time having apparently been required for their migration from the American to the European seas. In examining the latest deposits
of
in
various quarters of the world, it has everywhere been noted, that some few still existing species are common in the deposit, but have become extinct in the immediately surrounding sea; or, conversely, that some are