See page in:
1859
1860
1861
1866
1869
1872

Compare with:
1859
1860
1861
1866
1869

admit, in opposition to the judgment of most naturalists, that these 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

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

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

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

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

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

probable 1869 1872
probably 1859 1860
highly probable that 1861 1866

that those which 1872
those which have 1859 1860 1861 1866
that those which have 1869

each species underwent 1869 1872
species have been undergoing 1866

was probably 1872
have probably been 1866
was, from the reasons lately assigned, probably 1869

it 1869 1872
these same species 1866

2 blocks not present in 1859 1860 1861 1869 1872; present in 1866
We may infer that this has been the case, from there being no inherent tendency in organic beings to become modified or to progress in structure, and from all modifications depending, firstly on long-continued variability, and secondly on changes in the physical conditions of life, or on changes in the habits and structure of competing species, or on the immigration of new forms; and such contingencies will supervene in most cases only after long intervals of time and at a slow rate. These changes, moreover, in the organic and inorganic conditions of life will affect only a limited number of the inhabitants of any one area or country.

with 1872
in the case of 1859 1860 1861 1866 1869

done. 1872
effected by palæontologists. 1859 1860 1861 1866 1869

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 admit, in opposition to the judgment of most naturalists, that these tertiary species are all truly distinct from the recent, we have evidence of the frequent occurrence of slight
modification
modifications
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
....
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 in the direction required by the theory; but to this latter subject I shall return in the following chapter.
OMIT
with
With
animals and plants that
can
....
propagate rapidly and
are
do
not
highly locomotive,
wander much,
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 varieties; so
that
that,
with shells and other marine animals, it is probable that those which had the widest range, far exceeding the limits of the known geological formations of Europe,
which
....
have oftenest given rise, first to local varieties and ultimately to new species; and this again would greatly lessen the chance of our being able to trace the stages of transition in any
ony
one
geological formation.
It is a more important consideration,
clearly
....
leading to the same result, as lately insisted on by Dr. Falconer, namely, that the
periods
period
during which each species underwent modification, though
very
....
long as measured by years, was probably short in comparison with
the periods
that
during which it remained without undergoing any change.
It should not be forgotten, that at the present day, with perfect specimens for examination, two forms can seldom be connected by intermediate
varieties
varieties,
and thus proved to be the same species, until many specimens
have been
are
collected from many places; and with fossil species this
could
can
rarely be done. We shall, perhaps, best perceive the improbability of our being enabled to connect species