Water Reptiles of the Past and PresentWilliston, Samuel Wendell
Science
Water Reptiles of the Past and Present
Williston, Samuel Wendell
Aquatic reptiles; Aquatic reptiles, Fossil
In all early reptiles the ends of the body or centrum are concave,
as they are in nearly all fishes. Such a conformation, called
amphicoelous, gives great flexibility to the spinal column, but only
moderate strength, since the intervening spaces are filled with
cartilage in life. In all living reptiles, with few exceptions, the
body is concave, like a saucer, in front and correspondingly convex
behind, and the intervening cartilage has largely disappeared. Such a
mode of union, called procoelous, adds greatly to the strength of the
backbone, enabling it to receive greater shocks or greater pressure
without dislocation; or to sustain the greater strain of muscles used
in running swiftly or in climbing. Among living reptiles, only the
gecko lizards and the tuatera have biconcave vertebrae. Some extinct
reptiles, such as some of the dinosaurs, animals that walked erect upon
their legs, had their vertebrae convex in front and concave behind
(opisthocoelous). Birds, though walking erect, have a very different
and more complicated articulation of the cervical vertebrae, and
certain reptiles, like the turtles, have very complicated cervical
vertebrae.
In the embryos of all vertebrate animals there appears first an
elongated fibrous rod, called the notochord, in the place of the future
spinal column. This rod may persist through life, never ossifying, as
was the case with all the earliest fishes, and is the condition in some
living ones. As the embryo grows, however, the separate segments, or
vertebrae, ossify about this rod in all reptiles, forming bony rings,
perforate at first in the middle for the more or less constricted
notochord. This stage was the permanent condition in all the earliest
reptiles and in some later ones. Such animals are said to have
notochordal vertebrae, the notochord more or less continuous, like a
string of beads, the beads representing the enlargements between the
contiguous vertebrae.
[Illustration: FIG. 13.—Notochordal cervical vertebrae, with
intercentra, of _Ophiacodon_, a primitive theromorph reptile from the
Permocarboniferous of New Mexico: _pa_, proatlas; _an_, arch of atlas;
_o_, odontoid; _ax_, axis.]
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