The Vertebrate SkeletonReynolds, Sidney H. (Sidney Hugh)
Science
The Vertebrate Skeleton
Reynolds, Sidney H. (Sidney Hugh)
Skeleton
LABYRINTHODONTIA. The skull in Labyrinthodontia is remarkable for its
extreme solidity, the large number of bones which are present, and the
extent to which the roofing over of the temporal and other fossae has
taken place. In many forms the surface of the bones is as in
Crocodiles, strongly sculptured (fig. 27, right half) with ridges and
grooves which probably lodged sensory organs. The bones forming the
roof of the skull are generally very uniform in size, perhaps the most
noticeable of them being the paired dermo-supra-occipitals (fig. 27,
19). Paired dermo-supra-occipitals occur also in certain Ganoids. The
Labyrinthodont skull also bears resemblance to that of many fish in
the development of a pair of long pointed epi-otics (fig. 27, 18),
which remain permanently distinct from the surrounding bones. The
parietals are small and enclose between them the interparietal foramen
(fig. 27, 13). In some forms in which the head is protected with an
armour of scutes, these do not roof over the interparietal foramen,
and from this fact it has been inferred that the Labyrinthodonts had a
functional pineal eye. Both supra- and infra-temporal fossae are
partially or completely roofed over by the postorbitals and large
supra-temporals (fig. 27, 15).
There is generally a ring of bones in the sclerotic coat of the eye.
The pterygoids do not meet in the middle line, being separated by the
parasphenoid. The palatines bear teeth, and in some genera
(_Archegosaurus_) form long splints lying along the inner side of the
maxillae and more or less surrounding the posterior nares. In others
(_Nyrania_) they lie in the normal position near the middle line, one
on each side of the parasphenoid. The vomers bear teeth and sometimes
meet in the middle line; they are sometimes confluent with the
parasphenoid. On the ventral surface of the cranium there are
generally large palatal vacuities.
In the mandible there is often a well-marked postglenoid process, and
the articular is generally completely ossified.
[Illustration FIG. 28. A, VENTRAL VIEW OF THE CRANIUM; B, LATERAL VIEW
OF THE CRANIUM AND MANDIBLE OF _Siphonops annulatus_ (after
WIEDERSHEIM).
1. anterior nares.
2. naso-premaxillae.
3. frontal.
4. parietal.
5. maxillae.
6. vomer.
7. orbit.
8. quadrate united with the pterygoid in front.
9. squamosal.
10. exoccipital.
11. dentary.
12. angular.
13. basi-occipital and basisphenoid fused.
14. posterior narial opening surrounded by the palatine.
X. pneumogastric foramen.]
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