Osteoblasts : form a cell layer over the forming bone surface and have been proposed to act
as a barrier that controls ion flux into and out of bone. Although there are no junctional
complexes between cells, gap junctions do form and functionally couple adjacent cells.
When bone is no longer forming, osteoblasts flatten substantially, extending along the bone
surface, termed as bone lining cells that contain few synthetic organelles, suggesting that
they are less implicated in production of matrix proteins. They cover most surfaces in adult
skeleton. Bone lining cells retain their gap junctions with osteocytes, creating a network that
functions to control mineral homeostasis and ensure bone vitality.
Osteocytes : As osteoblasts form bone, some become entrapped within the matrix they
secrete, whether mineralized or unmineralized; these cells then are called osteocytes. The
number of osteoblasts that become osteocytes varies depending on the rapidity of bone
formation; more rapid the bone forms more osteocytes are present per unit volume. As a
general rule, embryonic (woven) bone and repair bone have more osteocytes than lamellar
bone.
After their formation, osteocytes become reduced in size. Space in the matrix occupied by
an osteocyte is called osteocytic lacuna. Narrow extensions of these lacunae form enclosed
channels, or canaliculi, that house radiating osteocytic processes. Through these channels,
osteocytes maintain contact with adjacent osteocytes and with the osteoblasts or lining cells
on the bone surfaces. This places osteocytes in an ideal position to sense biochemical and
mechanical environments and transduce signals for maintaining bone integrity and vitality.
Although osteocytes gradually reduce most of their matrix synthesizing machinery, they still
are able to secrete matrix proteins.
Osteoclasts : multinucleated and large cell, often seen in clusters. Characterized
cytochemically by possessing tartrate-resistant acid phosphatase within its cytoplasmic
vesicles and vacuoles, which distinguishes it from multinucleated giant cells. Typically
osteoclasts are found against the bone surface, occupying hollowed out depressions called
Howship’s lacunae that they have created. Howship’s lacunae are shallow troughs with an
irregular shape, reflecting activity and mobility of osteoclasts during active resorption.
Adjacent to the tissue surface, the cell membrane of osteoclast is thrown into a myriad of
deep folds that form a ruffled border. At the periphery of this border, the plasma membrane
is apposed closely to the bone surface; and the adjacent cytoplasm, devoid of cell
organelles, is enriched in actin, vinculin, and talin, proteins associated with integrin-
mediated cell adhesion. This clear or sealing zone not only attaches the cells to the
mineralized surface but also isolates a microenvironment between them and the bone
surface. Several mechanisms bind the osteoclast to surfaces; among these, molecules like
bone sialoprotein and osteopontin on bone surfaces may facilitate osteoclast adhesion and
formation of the sealing zone by means of an αvβ3 mediated mechanism. Another feature of
osteoclasts is a proton pump associated with ruffled border that pumps hydrogen ions into
the sealed compartment.