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
If we could affirm that the Air-breathers of the coal period were
really the first species of their families, they might acquire
additional interest by their bearing on this question of origin of
species. We cannot affirm this; but it may be a harmless and not
uninstructive play of fancy to suppose for a moment that they actually
are so, and to inquire on this supposition as to the mode of their
introduction. Looking at them from this point of view, we shall first
be struck with the fact that they belong to all of the three great
leading types of animals which include our modern Air-breathers the
Vertebrates, the Arthropods, and the Mollusks. We have besides to
consider in this connection that the breathing organs of an insect are
air tubes opening laterally (tracheæ), those of a land snail merely a
modification of the chamber which in marine species holds the gills,
while those of the reptiles represent the air bladder of the fishes.
Thus, in the three groups the breathing organs are quite distinct in
their nature and affinities. This at once excludes the supposition that
they can all have been derived from each other within the limits of the
coal period. No transmutationist can have the hardihood to assert the
convertibility, by any direct method, of a snail into a millipede or
an insect, or of either into a reptile. The plan of structure in these
creatures is not only different, but contrasted in its most essential
features. It would be far more natural to suppose that these animals
sprang from aquatic species of their respective types. We should then
seek for the ancestors of the snail in aquatic Gasteropods, for those
of the millipede in worms or Crustaceans, and for those of the reptiles
in the fishes of the period. It would be easy to build up an imaginary
series of stages, on the principle of natural selection, whereby these
results might be effected; but the hypothesis would be destitute of
any support from fact, and would be beset by more difficulties than it
removes. Why should the result of the transformation of water-snails
breathing by gills be a _Pupa ?_ Would it not much more likely be an
_Auricula_ or a _Limnea ?_ It will not solve this difficulty to say
that the intermediate forms became extinct, and so are lost. On the
contrary, they exist to this day, though they were not, in so far
as we know, introduced so early. But negative evidence must not be
relied on; the record is very imperfect, and such creatures may have
existed, though unknown to us. It may be answered that they could not
have existed in any considerable numbers, else some of their shells
would have appeared in the coal-formation beds, so rich in crustaceans
and bivalve mollusks. Further, the little Pupa remained unchanged
during a very long time, and shows no tendency to resolve itself into
anything higher, or to descend to anything lower, while in the lowest
bed in which it occurs it is associated with a round snail of quite
different type.
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