The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and PlantsDawson, John William, Sir
Science
The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and Plants
Dawson, John William, Sir
Paleobotany; Paleontology
The first leads to snake-like creatures, destitute of limbs, and which
must have been functionally the representatives of the serpents in the
Palæozoic, though batrachian in their affinities (Fig. 135). They are
found both in Europe and America; and Huxley describes one from Ireland
more than twenty-one inches long, and with over one hundred
vertebræ.[57] Some extraordinary traces are found on the sandstones of
the coal-formation,[58] which appear to indicate that there may have
been species of this type much larger than any represented by
skeletons, and with bodies perhaps six inches in diameter. It is not
unlikely that they had the habits of the modern water snakes.
[Illustration: FIG. 136.—A large Carboniferous Labyrinthodont
(_Baphetes planiceps_, Owen).
_a_, Anterior part of the skull, viewed from beneath. One-sixth natural
size, _b_, One of the largest teeth, natural size.]
A second line leads upward to large crocodile-like creatures, with
formidable teeth, strong bony armour, and well-developed limbs
(_Labyrinthodontia_, Figs. 136, 137). Some of them must have attained a
length of ten feet. They were lizard-like in form, could walk well, as
is seen from the footprints of some of the species which present a
considerable stride, and moved over mud without the belly touching the
ground. Their tails were long, and probably useful in swimming. Their
heads were flat and massive, and their teeth were strengthened by a
remarkable folding inward of the outer plate of enamel (Fig. 137 _b_).
The belly was protected by bony plates and closely imbricated scales. In
some of the species at least the upper parts were clothed with horny
scales, and the throat and sides were ornamented with pendent scaly
fringes or lappets.[59] Their general aspect and mode of life must have
resembled those of modern alligators; and in the vast swamps of the
Coal-period, full of ponds and sluggish streams swarming with fish, they
must have found a most suitable abode. While rigid anatomy may ally
these animals rather with the batrachians than the true reptiles, it is
evident that their great size, their capacity for walking with the body
borne well above the ground, their bony and scaly armour, their powerful
teeth and their capacious chests, with well-developed ribs, indicate
conditions of respiration and general vitality quite comparable with
those of the highest modern members of the class Reptilia.
[Illustration: FIG. 137.—_Baphetes planiceps_ (Owen).
_a_, Fragment of maxillary bone showing sculpture, four outer teeth, and
one inner tooth. Natural size. _b_, Section of inner tooth. Magnified,
_c_, Dermal scale. Natural size.]
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