The Vertebrate SkeletonReynolds, Sidney H. (Sidney Hugh)
Science
The Vertebrate Skeleton
Reynolds, Sidney H. (Sidney Hugh)
Skeleton
The majority of Teleosteans have thin flattened scales which differ
from those of Ganoids in being entirely mesodermal in origin,
containing no enamel. There are two principal types of Teleostean
scales, the cycloid and ctenoid. A =cycloid= scale is a flat thin
scale with concentric markings and an entire posterior margin. A
=ctenoid= scale differs in having its posterior margin pectinate. The
Dipnoi have overlapping cycloid scales. The rounded scales of _Amia_
and of many fossil ganoids such as _Holoptychius_ are shaped like
cycloid scales, but differ from them in being more or less coated with
enamel. In Eels and some other Teleosteans the scales are completely
degenerate and have almost disappeared. Some Teleosteans, like _Diodon
hystrix_, have scales with triradiate roots from which arise long
sharp spines directed backwards. These scales, which resemble teeth,
contain no enamel; they become erect when the fish inflates its body
into a globular form. Many Siluroids have dermal armour in the form of
large bony plates which are confined to the anterior part of the body.
In _Ostracion_ the whole body is covered by hexagonal plates, closely
united together.
The =fin-rays= are structures of dermal origin which entirely or
partially support the unpaired fins, and assist the bony or
cartilaginous endoskeleton in the support of the paired fins.
In Elasmobranchs, Dipnoi, and Chondrosteous ganoids the skeletons of
the fins are, as a rule, about half of exoskeletal, half of
endoskeletal origin, the proximal and inner portion being
cartilaginous and endoskeletal, the distal and outer portion being
exoskeletal, and consisting of horny or of more or less calcified
fin-rays. In bony Ganoids and Teleosteans the endoskeletal parts are
greatly reduced and the fins come to consist mainly of the fin-rays,
which are ossified and frequently become flattened at their distal
ends.
The fin-rays of the ventral part of the caudal fin are carried by the
haemal arches; those of the dorsal and anal fins and of the dorsal
part of the caudal fin generally by interspinous bones, which in adult
Teleosteans alternate with the neural and haemal spines. In Dipnoi
these interspinous bones articulate with the neural and haemal spines.
In many Siluroids the anterior rays of the dorsal and pectoral fins
are developed into large spines which often articulate with the
endoskeleton, or are sometimes fused with the dermal armour plates.
Similar spines may occur in Ganoids in front of both the dorsal and
anal fins. _Polypterus_ has a small spine or _fulcrum_ in front of
each segment of the dorsal fin. Such spines are often found
fossilised, and are known as _ichthyodorulites_.
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