Comparison with 1872 |
|
of B and C, and yet
would would 1872 | might 1859 1860 1861 1866 1869 |
not
....... 1866 1869 1872 | at all 1859 1860 1861 |
necessarily be strictly intermediate between them in all
respects. respects. 1866 1869 1872 |
points of structure. 1859 1860 1861 |
So that we might obtain the parent-species and its several modified descendants from the lower and upper beds of
the same the same 1869 1872 | a 1859 1860 1861 1866 |
formation, and unless we obtained numerous transitional gradations, we should not recognise their
blood-relationship, blood-relationship, 1861 1866 1869 1872 | relationship, 1859 1860 |
and should consequently
...OMIT 1872 |
be compelled to 1859 1860 1861 1866 1869 |
rank them
....... 1869 1872 | all 1859 1860 1861 1866 |
as distinct species. |
|
It is notorious on what excessively slight differences many palæontologists have founded their species; and they do this the more readily if the specimens come from different sub-stages of the same formation. Some experienced conchologists are now sinking many of the very fine species of D'Orbigny
and others into the rank of varieties; and on this view we do find the kind of evidence of change which on
the the 1869 1872 | my 1859 1860 1861 1866 |
theory we ought to find. Look again at the later tertiary deposits, which include many shells believed by the majority of naturalists to be identical with existing species; but some 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
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 modification
of form of
the kind required.
If If 1861 1866 1869 1872 | Moreover, if 1859 1860 |
we look to rather wider
intervals intervals 1861 1866 1869 1872 | intervals, 1859 1860 |
of time, namely, of time, namely, 1861 1866 1869 1872 |
namely, 1859 1860 |
to distinct but consecutive stages of the same great formation, we find that the embedded fossils, though
....... 1872 | almost 1859 1860 1861 1866 1869 |
universally ranked as specifically different, yet are far more closely
related related 1861 1866 1869 1872 | allied 1859 1860 |
to each other than are the species found in more widely separated formations;
so that here again we have undoubted evidence of change 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 |
in the
direction required by the theory; but to this latter subject I shall return in the following 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 |
chapter. |
|
...OMIT 1866 1869 1872 |
One other consideration is worth notice: 1859 1860 1861 |
With With 1866 1869 1872 | with 1859 1860 1861 |
animals and plants that
....... 1866 1869 1872 | can 1859 1860 1861 |
propagate rapidly and
do do 1866 1869 1872 | are 1859 1860 1861 |
not
wander much, wander much, 1866 1869 1872 | highly locomotive, 1859 1860 1861 |
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 forms,
is small, for the successive changes are supposed to have been local or
|
of B and C, and yet
might might 1859 1860 1861 1866 1869 | would 1872 |
not
at all at all 1859 1860 1861 | at all 1866 1869 1872 |
necessarily be strictly intermediate between them in all
points of structure. points of structure. 1859 1860 1861 |
respects. 1866 1869 1872 |
So that we might obtain the parent-species and its several modified descendants from the lower and upper beds of
a a 1859 1860 1861 1866 | the same 1869 1872 |
formation, and unless we obtained numerous transitional gradations, we should not recognise their
relationship, relationship, 1859 1860 | blood-relationship, 1861 1866 1869 1872 |
and should consequently
be compelled to be compelled to 1859 1860 1861 1866 1869 |
OMIT 1872 |
rank them
all all 1859 1860 1861 1866 | all 1869 1872 |
as distinct species. |
|
It is notorious on what excessively slight differences many palæontologists have founded their species; and they do this the more readily if the specimens come from different sub-stages of the same formation. Some experienced conchologists are now sinking many of the very fine species of
D'Orbigny D'Orbigny 1859 1860 1861 1866 1872 | D''Orbigny 1869 |
and others into the rank of varieties; and on this view we do find the kind of evidence of change which on
my my 1859 1860 1861 1866 | the 1869 1872 |
theory we ought to find. ↑1 blocks not present in 1859 1860; present in 1861 1866 1869 1872 | Look again at the later tertiary deposits, which include many shells believed by the majority of naturalists to be identical with existing species; but some 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
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 modification
of form of
the kind required.
|
Moreover, if Moreover, if 1859 1860 | If 1861 1866 1869 1872 |
we look to rather wider
intervals, intervals, 1859 1860 | intervals 1861 1866 1869 1872 |
namely, namely, 1859 1860 |
of time, namely, 1861 1866 1869 1872 |
to distinct but consecutive stages of the same great formation, we find that the embedded fossils, though
almost almost 1859 1860 1861 1866 1869 | almost 1872 |
universally ranked as specifically different, yet are far more closely
allied allied 1859 1860 | related 1861 1866 1869 1872 |
to each other than are the species found in more widely separated formations;
but to this subject I shall have to return 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 |
so that here again we have undoubted evidence of change 1869 1872 |
in the
following 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 |
direction required by the theory; but to this latter subject I shall return in the following 1872 |
chapter. |
|
One other consideration is worth notice: One other consideration is worth notice: 1859 1860 1861 |
OMIT 1866 1869 1872 |
with with 1859 1860 1861 | With 1866 1869 1872 |
animals and plants that
can can 1859 1860 1861 | can 1866 1869 1872 |
propagate rapidly and
are are 1859 1860 1861 | do 1866 1869 1872 |
not
highly locomotive, highly locomotive, 1859 1860 1861 | wander much, 1866 1869 1872 |
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
forms, forms, 1859 1860 1861 1872 | such forms, 1866 1869 |
is small, for the successive changes are supposed to have been local or
|