No organism wholly soft can
be preserved. Shells and bones decay and disappear when left on the bottom
of the sea, where sediment is not accumulating. We probably take a quite
erroneous view, when we assume that sediment is being deposited over nearly
the whole bed of the sea, at a rate sufficiently quick to embed and
preserve fossil remains. Throughout an enormously large proportion of the
ocean, the bright blue tint of the water bespeaks its purity. The many
cases on record of a formation conformably covered, after an immense
interval of time, by another and later formation, without the underlying
bed having suffered in the interval any wear and tear, seem explicable only
on the view of the bottom of the sea not rarely lying for ages in an
unaltered condition. The remains which do become embedded, if in sand or
gravel, will, when the beds are upraised, generally be dissolved by the
percolation of rain water charged with carbonic acid. Some of the many
kinds of animals which live on the beach between high and low water mark
seem to be rarely preserved. For instance, the several species of the
Chthamalinae (a sub-family 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 and
this has been found fossil in Sicily, whereas not one other species has
hitherto been found in any tertiary formation: yet it is known that the
genus Chthamalus existed during the Chalk period.
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