Comparison with 1861 |
|
same classes; or
that the geological succession of extinct forms is
in some degree parallel to in some degree parallel to 1859 1860 1861 |
in some degree parallel with 1866 |
nearly parallel with 1869 1872 |
the embryological development of recent
forms. ↑1 blocks not present in 1859 1860 1861 1866; present in 1869 1872 | This view accords admirably well with our theory.
|
I must follow Pictet and Huxley in thinking that the truth of this doctrine is
very very 1859 1860 1861 | very 1866 |
far from proved. Yet I fully expect to see it hereafter confirmed, at least in regard to subordinate
groups, groups, 1859 1860 1861 | groups 1866 |
which have branched off from each other within comparatively recent times. For this doctrine of Agassiz accords
well well 1859 1860 1861 | admirably well 1866 |
with the theory of natural selection. In a future chapter I shall attempt to show that the adult differs from its embryo, owing to variations supervening
at a not early age, and being
inherited at a corresponding age. This process, whilst it leaves the embryo almost unaltered, continually adds, in the course of successive generations, more and more difference to the adult. |
|
Thus the embryo comes to be left as a sort of picture, preserved by nature, of the ancient
and less modified condition of each animal.
This view may be true, and yet it
may never be capable of full
proof. Seeing, for instance, that the oldest known mammals, reptiles, and fish
strictly belong to their own
proper classes, though some of these old forms are in a slight degree less distinct from each other than are the typical members of the same groups at the present day, it would be vain to look for animals having the common embryological character of the Vertebrata, until beds
far far 1860 1861 |
rich in fossils are discovered far 1866 1869 1872 |
beneath the lowest
Silurian strata are discovered— Silurian strata are discovered— 1860 1861 |
Silurian stratum— 1866 1869 |
Cambrian strata— 1872 |
a discovery of which the chance is
very very 1860 1861 | very 1866 1869 1872 |
small. |
On
On
1859 1860 1861 |
On
1866 1869 1872 |
the
the
1859 1860 1861 |
the
1866 1869 1872 |
Succession
Succession
1859 1860 1861 |
Succession
1866 1869 1872 |
of
of
1859 1860 1861 |
of
1866 1869 1872 |
the
the
1859 1860 1861 |
the
1866 1869 1872 |
same
same
1859 1860 1861 |
same
1866 1869 1872 |
Types
Types
1859 1860 1861 |
Types
1866 1869 1872 |
within
within
1859 1860 1861 |
within
1866 1869 1872 |
the
the
1859 1860 1861 |
the
1866 1869 1872 |
same
same
1859 1860 1861 |
same
1866 1869 1872 |
areas
,
areas
,
1859 1861 |
areas
.
1860 |
Areas,
1866 1869 |
Areas
,
1872 |
during
during
1859 1860 1861 |
during
1866 1869 1872 |
the
the
1859 1860 1861 |
the
1866 1869 1872 |
later
later
1859 1860 1861 |
later
1866 1869 1872 |
tertiary
tertiary
1859 1860 1861 |
tertiary
1866 |
Tertiary
1869 1872 |
periods.
—
periods.
—
1860 1861 |
periods
.—
1859 |
periods
. 1866 |
periods. 1869 |
periods 1872 |
|
Mr. Clift many years ago showed that the fossil mammals from the Australian caves were closely allied to the living marsupials of that continent. In South
|
same classes;
or or 1859 1860 1861 1866 | and 1869 1872 |
that the geological succession of extinct forms is
in some degree parallel with in some degree parallel with 1866 |
in some degree parallel to 1859 1860 1861 |
nearly parallel with 1869 1872 |
the embryological development of
recent recent 1859 1860 1861 1866 | existing 1869 1872 |
forms. ↑1 blocks not present in 1859 1860 1861 1866; present in 1869 1872 | This view accords admirably well with our theory.
|
I must follow Pictet and Huxley in thinking that the truth of this doctrine is
....... 1866 | very 1859 1860 1861 |
far from proved. Yet I fully expect to see it hereafter confirmed, at least in regard to subordinate
groups groups 1866 | groups, 1859 1860 1861 |
which have branched off from each other within comparatively recent times. For this doctrine of Agassiz accords
admirably well admirably well 1866 | well 1859 1860 1861 |
with the theory of natural selection. In a future chapter I shall attempt to show that the adult differs from its embryo, owing to variations
supervening supervening 1859 1860 1861 1866 1869 | having supervened 1872 |
at a not early age, and
being being 1859 1860 1861 1866 1869 | having been 1872 |
inherited at a corresponding age. This process, whilst it leaves the embryo almost unaltered, continually adds, in the course of successive generations, more and more difference to the adult. |
|
Thus the embryo comes to be left as a sort of picture, preserved by nature, of the
ancient ancient 1859 1860 1861 1866 1869 | former 1872 |
and less modified condition of
each animal. each animal. 1859 1860 1861 1866 | the animal. 1869 | the species. 1872 |
This view may be true, and yet
it it 1859 1860 1861 1866 | it 1869 1872 |
may never be capable of
full full 1859 1860 1861 1866 1869 | full 1872 |
proof. proof. 1860 1861 1866 1869 1872 |
proof. Seeing, for instance, that the oldest known mammals, reptiles, and fish strictly belong to their own proper classes, though some of these old forms are in a slight degree less distinct from each other than are the typical members of the same groups at the present day, it would be vain to look for animals having the common embryological character of the Vertebrata, until beds far beneath the lowest Silurian strata are discovered— a discovery of which the chance is very small. 1859 |
Seeing, for instance, that the oldest known mammals, reptiles, and
fish fish 1860 1861 1866 | fishes 1869 1872 |
strictly belong to their
own own 1860 1861 1866 | own 1869 1872 |
proper classes, though some of these old forms are in a slight degree less distinct from each other than are the typical members of the same groups at the present day, it would be vain to look for animals having the common embryological character of the Vertebrata, until beds
rich in fossils are discovered far rich in fossils are discovered far 1866 1869 1872 |
far 1860 1861 |
beneath the lowest
Silurian stratum— Silurian stratum— 1866 1869 |
Silurian strata are discovered— 1860 1861 |
Cambrian strata— 1872 |
a discovery of which the chance is
....... 1866 1869 1872 | very 1860 1861 |
small. |
On
On
1866 1869 1872 |
On
1859 1860 1861 |
the
the
1866 1869 1872 |
the
1859 1860 1861 |
Succession
Succession
1866 1869 1872 |
Succession
1859 1860 1861 |
of
of
1866 1869 1872 |
of
1859 1860 1861 |
the
the
1866 1869 1872 |
the
1859 1860 1861 |
same
same
1866 1869 1872 |
same
1859 1860 1861 |
Types
Types
1866 1869 1872 |
Types
1859 1860 1861 |
within
within
1866 1869 1872 |
within
1859 1860 1861 |
the
the
1866 1869 1872 |
the
1859 1860 1861 |
same
same
1866 1869 1872 |
same
1859 1860 1861 |
Areas,
Areas,
1866 1869 |
areas
,
1859 1861 |
areas
.
1860 |
Areas
,
1872 |
during
during
1866 1869 1872 |
during
1859 1860 1861 |
the
the
1866 1869 1872 |
the
1859 1860 1861 |
later
later
1866 1869 1872 |
later
1859 1860 1861 |
tertiary
tertiary
1866 |
tertiary
1859 1860 1861 |
Tertiary
1869 1872 |
periods
.
periods
. 1866 |
periods
.—
1859 |
periods.
—
1860 1861 |
periods. 1869 |
periods 1872 |
|
Mr. Clift many years ago showed that the fossil mammals from the Australian caves were closely allied to the living marsupials of that continent. In South
|