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 form, _Dendrerpeton Acadianum_ was probably lizard-like; with a
broad flat head, short stout limbs and an elongated tail; and having
its skin, and more particularly that of the belly, protected by small
bony plates closely overlapping each other, and arranged _en chevron_,
in oblique rows meeting on the mesial line, where in front was a
thoracic plate. It may have attained the length of two feet. The form
of the head is not unlike that of _Baphetes_, but longer in proportion;
and much resembles that of the labyrinthodont reptiles of the Trias.
The bones of the skull are sculptured as in Baphetes, but in a smaller
pattern.
The fore limb of the adult animal, including the toes, must have been
four or five inches in length, and is of massive proportions. The bones
were hollow, and in the case of the phalanges the bony walls were thin,
so that they are often crushed flat. The humerus, or arm bone, however,
was a strong bone, with thick walls and a cancellated structure toward
its extremities; still even these have sometimes yielded to the great
pressure to which they have been subjected. The cavity of the interior
of the limb bones is usually filled with calc-spar stained with organic
matter, but showing no structure; and the inner side of the bony wall
is smooth without any indication of cartilaginous matter lining it.
The vertebræ, in the external aspect of their bodies, remind one of
those of fishes, expanding toward the extremities, and being deeply
hollowed by conical cavities, which appear even to meet in the centre.
There is, however, a large and flattened neural spine. The vertebræ are
usually much crushed, and it is almost impossible to disengage them
from the stone. The ribs are long and curved, showing a reptilian style
of chest. The posterior limb seems to have been not larger than the
anterior, perhaps smaller. The tibia, or principal bone of the fore leg
is much flattened at the extremity, as in some Labyrinthodonts, and the
foot must have been broad, and probably suited for swimming, or walking
on soft mud, or both. That the hind limb was adapted for walking is
shown, not merely by the form of the bones, but also by that of the
pelvis.
The external scales are thin, oblique-rhomboidal or elongated-oval,
marked with slight concentric lines, but otherwise smooth, and
having a thickened ridge or margin, in which they resemble those of
Archegosaurus, and also those of _Pholidogaster pisciformis_, described
by Huxley from the Edinburgh coal field,--an animal which indeed
appears in most respects to have a close affinity with _Dendrerpeton_.
The microscopic structure of the scales is quite similar to that of the
other bones, and different from that of the scales of ganoid fishes,
the shape of the cells being batrachian. For other particulars of its
structure reference may be made to the papers named at the end of the
chapter.
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