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
The shoulder-girdle or pectoral arch is strangely unlike that of any
other reptiles. There is no breast bone, since the breast bone is a
comparatively late development in reptiles, not appearing, probably,
until after the plesiosaurs had begun their existence. Taking the
place of the sternum, the very large and broad coracoidsjoin each
other in the middle, forming a sort of subdermal armor on the under
side of the body in front. In some of the largest plesiosaurs these
two bones measured together about six feet in length by four in
width. Though so very large they are thick only in front between the
articulations of the forelegs. The shoulder-blades are much reduced
in size and are extraordinarily modified. The blade proper, that is,
that part extending backward and upward, is narrow and small, affording
but little surface for the attachment of muscles. On the inner side,
extending toward the middle in front of the coracoids, there is another
projection, often broad and large, to which was attached the clavicles
when present, and often this projection met its mate of the opposite
scapula in the middle in front of the coracoids in a broad union. The
clavicles or collar-bones are small and thin, and sometimes absent;
they also are united in the middle posteriorly with the coracoids when
the scapula did not intervene. And the interclavicle also is sometimes
wanting. Altogether the pectoral bones form a very large, broad, and
concave trough inclosing the whole of the under side of the anterior
part of the body. This extensive surface must have furnished attachment
to stout and strong muscles controlling the downward and inward motion
of the paddles.
There is a well-developed sacrum of three vertebrae for the support
of the pelvis or hip bones. The reason for its persistence in animals
so thoroughly adapted for life in the water will be understood later.
The ilium is slender; it was attached to the sides of the sacrum by
ligaments, only, not forming a firm union, but strong nevertheless.
The pubes and ischia, the other bones of the pelvis on the under side
of the body, like the corresponding bones of the pectoral girdle, were
enormously enlarged, forming great flat, bony plates.
Besides these large bony plates of the shoulder and pelvic girdles,
the short abdominal region was inclosed by numerous series of strong
ventral ribs, that is, overlapping rod-like bones on each side,
connected with a central piece. It will be seen that the whole under
side of the body, from the base of the neck to the base of the tail,
was well protected by bones, rigid and unyielding in front and behind,
flexible for a short space below the abdomen; this surface, however,
was not flat like the under shell of a turtle, but rounded from side to
side.
[Illustration: FIG. 36.—Pelvic girdle from above of _Trinacromerum
osborni_, an Upper Cretaceous plesiosaur: _p_, pubis; _is_, ischium;
_il_, ilium.]
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