→ direction required by the theory; but to this latter subject I shall have to return in the following 1869 |
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 return in the following 1872 |
|
→ 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 have 1869 |
those which have 1859 1860 1861 1866 |
that those which 1872 |
|
→ each species underwent 1869 1872 |
species have been undergoing 1866 |
|
→ was, from the reasons lately assigned, probably 1869 |
have probably been 1866 |
was probably 1872 |
|
→ 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.
|
|
in the
→direction required by the theory; but to this latter subject I shall have to return in the following
chapter. |
|
→OMIT
animals and plants that
propagate rapidly and
not
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
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
with shells and other marine animals, it is
→probable
→that those which have
had the widest range, far exceeding the limits of the known geological formations of Europe,
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
geological formation. |
|
It is a more important consideration,
leading to the same result, as lately insisted on by Dr. Falconer, namely, that the
during which
→each species underwent
modification, though
long as measured by years,
→was, from the reasons lately assigned, probably
short in comparison with
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
and thus proved to be the same species, until many specimens
|