The Cambridge natural history, Vol. 08 (of 10)Gadow, Hans
Science
The Cambridge natural history, Vol. 08 (of 10)
Gadow, Hans
Animals
{310}_Dicynodon_, with many species from the Karroo formation of South
Africa, reached formidable dimensions. The thick, curved skull is in size
and outline not unlike that of a large lion, hence _D. leoniceps_, _D.
tigriceps_, etc. The zygomatic arch is almost mammalian, except that the
posterior boundary of the orbit is formed by a distinct postfrontal bone.
The nostrils are lateral. The canine tusks (Fig. 54, E, p. 280) are very
large. The choanae open behind the rhomboid vomer and between the separated
palatine bones, which are posteriorly confluent with the medially united
pterygoids. The latter send out flat extensions, along the lateral side of
the palatines; these extensions reach the maxillaries and probably
represent the ectopterygoids. The occipital condyle is distinctly triple,
being equally composed of the basi- and latero-occipital bones.
The three bones of the shoulder-girdle meet at the glenoid fossa; the
scapula has the indication of a spine. The pelvis is stout, attached to
four or five vertebrae, converting the latter into a very Mammalian-like
sacrum, the position of which lies distinctly in front of the acetabulum.
The latter is closed, composed by the three pelvic bones. The pubes and
ischia are fused together, leaving only a very small obturator-foramen. The
limbs are plantigrade and pentadactyle, very stout; the humerus and femur
have enormous crests.
_Oudenodon_, of which several species have been described, is so much like
_Dicynodon_, except for the complete absence of teeth, that it has been
suggested that these skulls belong to females of this genus. This view is
strengthened by the fact that tusk-like canines exist, or are absent in
some of the species which have been described as _Cistecephalus_, a genus
closely allied to _Dicynodon_. The latter, which, like _Oudenodon_ and
_Cistecephalus_, occurred in Africa, extended also into India, _D.
orientalis_ having been found in the Panchet formation of Bengal, of
transitional age between the Permian and Triassic epochs. _Oudenodon
rugosus_, on the other hand, has been described from the Ural.
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