The Vertebrate SkeletonReynolds, Sidney H. (Sidney Hugh)
Science
The Vertebrate Skeleton
Reynolds, Sidney H. (Sidney Hugh)
Skeleton
=Bone= consists of a series of lamellae of ossified substance between
which are oval spaces, the =lacunae=, giving rise to numerous fine
channels, the =canaliculi=, which radiate off in all directions. The
lacunae are occupied by the =bone cells= which correspond to cartilage
cells, from which if the bone is young, processes pass off into the
canaliculi. It is obvious that the ossified substance of bone is
intercellular in character, and corresponds to the matrix of
cartilage.
Bone may be compact, or loose and spongy in character, when it is
known as =cancellous bone=. In compact bone many of the lamellae are
arranged concentrically round cavities, the =Haversian canals=, which
in life are occupied by blood-vessels. Each Haversian canal with its
lamellae forms a =Haversian system=. In spongy bone instead of
Haversian canals there occur large irregular spaces filled with
marrow, which consists chiefly of blood-vessels and fatty tissue. The
centre of a long bone is generally occupied by one large continuous
marrow cavity. The whole bone is surrounded by a fibrous connective
tissue membrane, =the periosteum=.
THE DEVELOPMENT OF BONE.
=Periosteal ossification.= An example of a bone entirely formed in
this way is afforded by the parietal. The first trace of ossification
is shown by the appearance, below the membrane which occupies the
place of the bone in the early embryo, of calcareous spicules of bony
matter, which are laid down round themselves by certain large cells,
the =osteoblasts=. These osteoblasts gradually get surrounded by the
matter which they secrete and become converted into bone cells, and in
this way a mass of spongy bone is gradually produced. Meanwhile a
definite periosteum has been formed round the developing bone, and on
its inner side fresh osteoblasts are produced, and these with the
others gradually render the bone larger and more and more compact.
Finally, the middle layer of the bone becomes again hollowed out and
rendered spongy by the absorption of part of the bony matter.
=Endochondral ossification=[5]. This is best studied in the case of a
long bone like the femur or humerus. Such a long bone consists of a
shaft, which forms the main part, and two terminal portions, which
form the =epiphyses=, or portions ossifying from centres distinct from
that forming the shaft or main part of the bone.
In the earliest stage the future bone consists of hyaline cartilage
surrounded by a vascular sheath, the perichondrium.
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