in sand or gravel,
will | will 1859 1860 1861 1866 1869 | | will, 1872 |
when the beds are
upraised | upraised 1859 1860 1861 1866 1869 | | upraised, 1872 |
generally be dissolved by the percolation of
rain-water charged with carbonic acid. | rain-water charged with carbonic acid. 1861 1866 1869 1872 |
| rain-water. 1859 1860 |
Some | Some 1861 1866 1869 1872 |
| I suspect that but few 1859 1860 |
of the
..| ..... 1861 1866 1869 1872 | | very 1859 1860 |
many
kinds of animals | kinds of animals 1861 1866 1869 1872 |
| animals 1859 1860 |
which live on the beach between high and low
water mark | water mark 1861 1866 1869 1872 | | watermark 1859 1860 |
seem to be rarely | seem to be rarely 1861 1866 1869 1872 |
| are 1859 1860 |
preserved. For instance, the several species of the Chthamalinæ (a
sub-family | sub-family 1859 1861 1866 1869 1872 | | subfamily 1860 |
of sessile cirripedes) coat the rocks all over the world in infinite numbers: they are all strictly littoral, with the exception of a single Mediterranean species, which inhabits deep
water, | water, 1861 1866 1869 1872 | | water 1859 1860 |
and
has | has 1859 1860 1861 1866 | | this has 1869 1872 |
been found fossil in Sicily, whereas not one other species has hitherto been found in any tertiary
formation: | formation: 1859 1860 1861 1866 1869 | | formation; 1872 |
yet it is
now | now 1859 1860 1861 1866 1869 | now 1872 |
known that the genus Chthamalus existed during the
Chalk | Chalk 1866 1869 1872 | | chalk 1859 1860 1861 |
period. ↑| 1 blocks not present in 1866 1869 1872; present in 1859 1860 1861 | | The molluscan genus Chiton offers a partially analogous case.
|
|
|
With respect to the terrestrial productions which lived during the Secondary and Palæozoic periods, it is superfluous to state that our evidence
from fossil remains | from fossil remains 1859 1860 1861 1866 1869 |
| OMIT 1872 |
is fragmentary in an extreme degree. For instance,
not | not 1859 1860 1861 1866 1869 |
| until recently not 1872 |
a land shell
is | is 1859 1860 1861 1866 |
| until quite recently was 1869 |
| was 1872 |
known belonging to either of these vast periods, with
the | the 1860 1861 1866 1869 1872 | | one 1859 |
exception
of one species discovered | of one species discovered 1860 1861 1866 1869 1872 |
| discovered 1859 |
by Sir C. Lyell
and Dr. Dawson in | and Dr. Dawson in 1860 1861 1866 1869 1872 |
| in 1859 |
the carboniferous strata of North
America, of which shell above a hundred specimens have now been collected. | America, of which shell above a hundred specimens have now been collected. 1861 1866 1869 |
| America. 1859 |
| America, of which shell several specimens have now been collected. 1860 |
| America; but now land-shells have been found in the lias. 1872 |
In regard to mammiferous remains, a
single | single 1859 1860 1861 1866 1869 | single 1872 |
glance at the historical table published in
...| OMIT 1866 1869 1872 |
| the Supplement to 1859 1860 1861 |
Lyell's | Lyell's 1859 1860 1861 1866 1872 | | Lyells 1869 |
Manual | Manual 1866 1869 1872 | | Manual, 1859 1860 1861 |
will bring home the truth, how accidental and rare is their preservation, far better than pages of detail. Nor is their rarity surprising, when we remember how large a proportion of the bones of tertiary mammals have been discovered either in caves or in lacustrine deposits; and that not a cave or true lacustrine bed is
know | know 1866 | | known 1859 1860 1861 1869 1872 |
belonging to the age of our secondary or palæozoic formations. |
|
But the imperfection in the geological record
largely | largely 1861 1866 1869 1872 | | mainly 1859 1860 |
results from another and more important cause than any of the foregoing; namely, from the several
forma- tions | forma- tions 1866 | | formations 1859 1860 1861 1869 1872 |
|