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
as eight or ten individuals have been obtained from three erect
Sigillariæ, indicating that these creatures were quite abundant, as
well as active and terrestrial in their mode of life.
With respect to the affinities of this species, I think it is
abundantly manifest that it presents no close relationship with any
reptile hitherto discovered in the Carboniferous system, except perhaps
some of the smaller forms in the Permian of Europe, with which Credner
and Fritsch have compared it. It is scarcely necessary to say that
the characters above described entirely remove this animal from the
Labyrinthodonts. Equal difficulties attend the attempt to place it in
any other group of recent or extinct Batrachians or proper reptiles.
The structures of the skull, and of some points in the vertebræ,
certainly resemble those of Batrachians; but, on the other hand,
the well-developed ribs, evidently adapted to enlarge the chest in
respiration, the pelvis, and the cutaneous covering, are unexampled in
modern Batrachians, and assimilate the creature to the true lizards.
I have already, in my original description of the animal in 1859,
expressed my belief that _Hylonomus_ may have had lacertian affinities,
but I do not desire to speak too positively in this matter;[137] and
shall content myself with stating the following alternatives as to
the probable relations of these animals, (1) They may have been true
reptiles of low type, and with batrachian tendencies. (2) They may have
been representatives of a new family of Batrachians, exhibiting in some
points lacertian affinities. (3) They may have been the young of some
larger reptile, too large and vigorous to be entrapped in the pitfalls
presented by the hollow Sigillaria stumps, and in its adult state
losing the batrachian peculiarities apparent in the young. Whichever of
these views we may adopt, the fact remains, that in the structure of
this curious little creature we have peculiarities both batrachian and
lacertian, in so far as our experience of modern animals is concerned.
It would, however, accord with observed facts in relation to other
groups of extinct animals, that the primitive Batrachians of the
coal period should embrace in their structures points in after times
restricted to the true reptiles. On the other hand, it would equally
accord with such facts that the first-born of Lacertians should lean
towards a lower type, by which they may have been preceded. My present
impression is, that they may constitute a separate family or order, to
which I would give the name of Microsauria, and which may be regarded
as allied, on the one hand, to certain of the humbler lizards, as the
Gecko or Agama, and, on the other, to the tailed Batrachians.
[137] I am glad to say that Fritsch and Credner now lean to the same
view.
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