Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
In the case of many groups of marine animals, as, for example, the
shell-fish and the corals, and I may add the bivalve crustaceans, so
admirably worked up by my friend Prof. Rupert Jones, we have very
complete series. With the and snails the case is altogether different.
As stated in another paper of this series, a few species of these
animals appear in the later Palæozoic age, and after that they have no
successors known to us in all the great periods covered by the Permian,
the Trias, and the earlier Jurassic. A few air-breathing water-snails
appear in the upper Jurassic, and true land snails are not met with
again until the Tertiary. Were there no land snails in this vast lapse
of time? Have we two successive creations, so to speak, of these
creatures at distant intervals? Were they only diminished in numbers
and distribution in the intervening time? Is the hiatus owing merely
to the unlikelihood of such shells being preserved? Or is it owing to
the lack of diligence and care in collecting?
In this particular case we are, no doubt, disposed to say that the
series must have been continuous. But we cannot be sure of this. In
whatever way a few species of land snails were so early introduced in
the time of the Devonian or of the Coal formation, if from physical
vicissitudes or lack of proper pabulum they became extinct, there is
no reason known to us why, when circumstances again became favourable,
they should not be reintroduced in the same manner as at first, whether
by development from allied types or otherwise. The fact that the few
Devonian and Carboniferous species are very like those that still
exist, perhaps makes against this supposition, but does not exclude it.
If we suppose that new forms of life of low grade are introduced from
time to time in the course of the geological ages, and if we adopt the
Darwinian hypothesis of evolution, we arrive, as Naegeli has so well
pointed out, at the strange paradox, that the highest forms of life
must be the oldest of all, since they will be the descendants of the
earliest of the lower animals, whereas the animals now of low grade
may have been introduced later, and may not have had time to improve.
But all our attempts to reduce nature to one philosophic expression
necessarily lead to such paradoxes.
Public-domain text, read in full here on John Shaqi.
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