A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological MonumentsLyell, Charles, Sir
Science
A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments
Lyell, Charles, Sir
Geology
In like manner, when we see thousands of full-grown shells dispersed every
where throughout a long series of strata, we cannot doubt that time was
required for the multiplication of successive generations; and the evidence
of slow accumulation is rendered more striking from the proofs, so often
discovered, of fossil bodies having lain for a time on the floor of the
ocean after death before they were imbedded in sediment. Nothing, for
example, is more common than to see fossil oysters in clay, with serpulae,
or barnacles (acorn-shells), or corals, and other creatures, attached to
the inside of the valves, so that the mollusk was certainly not buried in
argillaceous mud the moment it died. There must have been an interval
during which it was still surrounded with clear water, when the testacea,
now adhering to it, grew from an embryo state to full maturity. Attached
shells which are merely external, like some of the serpulae (_a_) in the
annexed figure (fig. 10.), may often have grown upon an oyster or other
shell while the animal within was still living; but if they are found on
the inside, it could only happen after the death of the inhabitant of the
shell which affords the support. Thus, in fig. 10., it will be seen that
two serpulae have grown on the interior, one of them exactly on the place
where the adductor muscle of the _Gryphaea_ (a kind of oyster) was fixed.
Some fossil shells, even if simply attached to the _outside_ of others,
bear full testimony to the conclusion above alluded to, namely, that an
interval elapsed between the death of the creature to whose shell they
adhere, and the burial of the same in mud or sand. The sea-urchins or
_Echini_, so abundant in white chalk, afford a good illustration. It is
well known that these animals, when living, are invariably covered with
numerous spines, which serve as organs of motion, and are supported by rows
of tubercles, which last are only seen after the death of the sea-urchin,
when the spines have dropped off. In fig. 12. a living species of
_Spatangus_, common on our coast, is represented with one half of its shell
stripped of the spines. In fig. 11. a fossil of the same genus from the
white chalk of England shows the naked surface which the individuals of
this family exhibit when denuded of their bristles. The full-grown
_Serpula_, therefore, which now adheres externally, could not have begun to
grow till the _Spatangus_ had died, and the spines were detached.
[Illustration: Fig. 11. _Serpula_ attached to a fossil _Spatangus_
from the chalk.]
[Illustration: Fig. 12. Recent _Spatangus_ with the spines removed
from one side.
_b._ Spine and tubercles, nat. size.
_a._ The same magnified.]
[Illustration: Fig. 13.
_a._ _Echinus_ from the chalk, with lower valve of the _Crania_ attached.
_b._ Upper valve of the _Crania_ detached.]
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