The zoology of the voyage of H.M.S. Beagle [vol. 1 of 5] : $b Fossil mammaliaOwen, Richard
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The zoology of the voyage of H.M.S. Beagle [vol. 1 of 5] : $b Fossil mammalia
Owen, Richard
Beagle Expedition (1831-1836); Mammals, Fossil; Paleontology -- South America; Zoology
The plane of the occipital foramen forms with that of the base of the
skull an angle of 140°, the plane of the posterior surface of the skull
forms with the basal plane an angle of 68°. The occipital condyles are
therefore terminal, or form the most posterior parts of the cranium. The
extent of their convex curvature in the antero-posterior direction,
which equals that of a semicircle, indicates that the Megatherium
possessed considerable freedom and extent of motion of the head. The
condyles are not extended in the lateral direction so far as in the
Toxodon; their axis is more oblique than in the Glossotherium, and their
internal surface is more parallel with the axis of the skull, the
foramen magnum not presenting that infundibuliform expansion which is so
characteristic of the Glossotherium. The occipital condyles resemble
most in form and position those of the Scelidotherium; but in the angle
of the occipital plane the Megatherium is intermediate between the
Scelidothere and Glossothere. The ex-occipitals terminate laterally and
inferiorly, each in a short, but strong obtuse process. The posterior
plane of the skull is traversed by a strong arched intermuscular crest,
which forms the upper boundary of a pretty deep fossa, which is divided
by a median vertical ridge, extending downwards to within an inch of the
upper margin of the foramen magnum. A second strong obtuse transversely
arched ridge curves over the first, and forms the upper boundary of the
posterior or occipital region of the skull: the interspace between the
two transverse ridges is very irregular, and indicates the firm
implantation of powerful nuchal muscles or ligaments, (Pl. XXX. fig. 1.)
In the configuration and angle of the occipital plane the Megatherium
indicates the same general correspondence with the Edentate type, which
has been pointed out in the descriptions of the crania of the
Glossothere and Scelidothere: and the resemblance to the Scelidothere is
not less striking in the small proportional size of the cranium in this
quadruped, which surpasses the rest of its class in so great a degree in
the colossal proportions of its hinder parts.
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