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1859
1860
1861
1866
1869
1872

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1859
1860
1866
1869
1872

believe that the great majority of naturalists are wrong and that the 1861 1869
believe that the great majority of naturalists are wrong and that that the 1866
admit, in opposition to the judgment of most naturalists, that these 1872

a very general 1861
frequent occurrence of 1866
the frequent occurrence of 1869 1872

of time, namely, 1861 1866 1869 1872
namely, 1859 1860

so that here again we have undoubted evidence of change, though not strictly of variation, 1861 1866
but to this subject I shall have to return 1859 1860
so that here again we have undoubted evidence of change 1869 1872

direction required by my theory; but to this latter subject I shall have to return in the following 1861 1866
following 1859 1860
direction required by the theory; but to this latter subject I shall have to return in the following 1869
direction required by the theory; but to this latter subject I shall return in the following 1872

One other consideration is worth notice: 1859 1860 1861
OMIT 1866 1869 1872

excellent naturalists, as Agassiz and Pictet, maintain that all these tertiary species are specifically distinct, though the distinction is admitted to be very slight; so that here, unless we believe that these eminent naturalists have been misled by their
imaginations,
imaginations
and that these late tertiary species really present no difference whatever from their living representatives, or unless we believe that the great majority of naturalists are wrong and that the tertiary species are all truly distinct from the recent, we have evidence of a very general slight
modifications
modification
of
form of
form of
the kind required.
Moreover, if
If
we look to rather wider
intervals,
intervals
of time, namely, to distinct but consecutive stages of the same great formation, we find that the embedded fossils, though
almost
almost
universally ranked as specifically different, yet are far more closely
allied
related
to each other than are the species found in more widely separated formations; so that here again we have undoubted evidence of change, though not strictly of variation, in the direction required by my theory; but to this latter subject I shall have to return in the following chapter.
One other consideration is worth notice:
With
with
animals and plants that
can
can
propagate rapidly and
do
are
not
wander much,
highly locomotive,
there is reason to suspect, as we have formerly seen, that their varieties are generally at first local; and that such local varieties do not spread widely and supplant their parent-forms until they have been modified and perfected in some considerable degree. According to this view, the chance of discovering in a formation in any one country all the early stages of transition between any two
such forms,
forms,
is small, for the successive changes are supposed to have been local or confined to some one spot. Most marine animals have a wide range; and we have seen that with plants it is those which have the widest range, that oftenest present