The Vertebrate SkeletonReynolds, Sidney H. (Sidney Hugh)
Science
The Vertebrate Skeleton
Reynolds, Sidney H. (Sidney Hugh)
Skeleton
The exoskeleton consists principally of calcifications forming dorsal
and ventral shields which cover the head and abdominal region; the
dorsal shield is formed of a few plates firmly united, the ventral
shield of a single plate. The shields are composed of three layers,
the middle layer being traversed by canals belonging to the dermal
sense organs which open to the exterior by a series of pores. The tail
is sometimes covered by scales. The orbits are widely separated and
laterally placed. Paired appendages are absent. These curious forms
are found in beds of Upper Silurian and Lower Devonian age. One of the
best known genera is _Pteraspis_.
_Suborder_ (2). OSTEOSTRACI.
The exoskeleton as in the Heterostraci consists of shields and scales,
the shields being divisible into three layers. The anterior part of
the body is covered dorsally by a single large shield which differs
from those of the Heterostraci in having the inner layer ossified. The
middle layer contains canals for the passage of blood vessels, but the
exoskeleton shows no impressions of dermal sense organs. The posterior
part of the body is covered by large quadrangular scales. Paired
appendages are absent, but median dorsal and caudal fins occur
supported by scales, not fin-rays. _Cephalaspis_, the best known of
these animals, occurs in beds of Lower Devonian age.
_Suborder_ (3). ANTIARCHA.
The exoskeleton is formed of bony plates, the dorsal and ventral
shields each consisting of several symmetrically arranged pieces. The
tail may be covered with small scales or may be naked. The head is
articulated with the trunk, and its angles are drawn out into a pair
of segmented paddle-like appendages, covered with dermal plates. The
orbits are close together. A dorsal fin and traces of mouth parts
occur in _Pterichthys_, but the endoskeleton is unknown. The best
known forms _Pterichthys_[26] and _Asterolepis_ occur in beds of Lower
Devonian age.
GENERAL ACCOUNT OF THE SKELETON OF MARSIPOBRANCHII.
The Marsipobranchii are worm-like animals. The living forms include
two families, the Myxinoidei (Hags)--genera _Myxine_ and
_Bdellostoma_--and the Petromyzontidae (Lampreys).
Three species of _Petromyzon_ are known, _P. fluviatilis_, _P.
marinus_ and _P. planeri_. The larval forms were for a long time
thought to belong to a separate genus and were called _Ammocoetes_.
The Myxinoids, although very highly specialised in their own way, are
at distinctly a lower stage of development than the adult Lamprey, and
come nearer to the larval Lamprey or Ammocoete.
SPINAL COLUMN.
[Illustration FIG. 4. A, DORSAL; B, LATERAL AND C, VENTRAL VIEW OF THE
SKULL OF _Petromyzon marinus_ × 1 (after PARKER).
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