The osteoclast precursor arises principally in the marrow as an early mononuclear macrophage; it circulates and binds to the bone surface [
8]. Whether the site to which the osteoclast precursor attaches, and which the differentiated osteoclast will ultimately resorb, is a selective or stochastic process is unknown. The process of bone remodeling must, however, replace effete bone with new to prevent brittleness and tendency to fracture, a condition that may be compromising long-term anti-bone resorptive therapy [
9].
Once attached to bone, the mononuclear osteoclast precursor fuses with its sister cells to form a terminally differentiated polykaryon, which no longer has the capacity to replicate. Indirect evidence indicates that the life span of the osteoclast, in vivo, is about 2 weeks.
Although the osteoclast, like the foreign body giant cell, is multinucleate and the product of macrophage fusion, the two are distinct. The osteoclast, upon contact with bone, uniquely polarizes, which endows it with the capacity to degrade both the organic and the inorganic components of the skeleton [
8]. This polarization process involves reorganization of the osteoclast cytoskeleton. Thus, under the influence of the Rho family of GTPases [
10], the osteoclast's fibrillar actin forms a novel circular anchoring structure at the cell/bone interface, known as the 'actin ring' or 'sealing zone', that isolates the resorptive microenvironment from the general extracellular space [
11]. At the same time, cytosol-residing acidified vesicles track to the resorptive surface of the cell [
12], where they fuse with the bone-apposed plasma membrane under the aegis of Rab3D [
13]. This insertion of large numbers of acidifiying vesicles into the plasma membrane results in the formation of a complex villous structure unique to, and diagnostic of, the resorbing osteoclast: the 'ruffled membrane' [
14]. Once it has accomplished its resorptive mission at a particular location in bone, the osteoclast disassembles its actin ring and ruffled membrane, and migrates to its next site of activity, where it once again reorganizes its cytoskeleton to the resorptive phenotype [
11]. Thus, changes in the osteoclast cytoskeleton are diagnostic of, and essential to, various steps in its bone degradative cycle (Fig. ).
The study of murine and human models of osteopetrosis established a paradigm by which the osteoclast first mobilizes the mineralized and, then, the organic phase of bone. Having generated the isolated extracellular microenvironment at its interface with bone, the osteoclast acidifies it by means of an electrogenic H
+-ATPase that has been inserted into the ruffled membrane by polarized cytosolic vesicles [
14]. This proton pump, which is similar to that residing in clathrin-coated vesicles [
15], is essential to the resorptive process, and its dysfunction is the principal known cause of human osteopetrosis [
16]. The massive extracellular transport of protons by the osteoclast has the potential for intracellular alkalization, which the cell prevents by a chloride–bicarbonate exchange mechanism located in the anti-resorptive plasma membrane [
17]. The Cl
- entering the cell moves transcellularly to the ruffled membrane and is transported into the resorptive microenvironment by an anion channel, which is charge-coupled to the H
+-ATPase [
18]. Interestingly, mutation of this Cl
- channel also prompts osteopetrosis in humans [
19]. Thus, by the generation of HCl, the osteoclast creates a pH of about 4.5 in the isolated microenvironment, the initial impact of which is to degrade the mineralized component of bone, thereby exposing its organic matrix consisting largely of type 1 collagen [
20]. After mobilization of its mineral phase, the collagenous component of bone is degraded by the lysosomal enzyme cathepsin K, whose loss of function is responsible for the sclerosing skeletal disease pyknodysostosis [
21].
The fact that contact with bone organizes the osteoclast cytoskeleton, and endows the cell with its resorptive capacity, indicates that molecules that mediate bone–cell recognition must be central to osteoclast formation and function. Integrins are heterodimeric transmembrane matrix receptors whose intracellular domains interact with signaling molecules and cytoskeletal proteins. In fact, integrins transmit extracellular matrix-derived signals that organize the osteoclast's fibrillar actin and prompt acidifying vesicles to migrate towards the ruffled membrane [
12].
α
vβ
3 is the principal integrin mediating osteoclast function; it is specifically expressed when macrophage precursors commit to the bone resorptive but not the host defense phenotype [
22]. This heterodimeric receptor, in osteoclasts, is localized within mobile matrix recognition structures known as podosomes, which also contain actin and other cytoskeletal proteins [
23]. The location of podosomes within the osteoclast varies with the phase of the resorptive cycle, because these structures participate in the cell's migratory and bone degradative activities [
23]. The fact that osteoclasts derived from mice lacking the integrin are dysfunctional, largely because of failure to organize their actin cytoskeleton and generate a normal ruffled membrane, establishes that α
vβ
3 transmits essential signals to the cell's interior [
24]. These observations indicate that the α
vβ
3 integrin is a candidate anti-bone resorptive target, and small-molecule drugs that compete for the matrix receptor are in clinical trial [
9,
25,
26]. Whether, as proposed, they arrest the bone loss of inflammatory arthritis [
27] is yet to be determined.
α
vβ
3 occupancy organizes the osteoclast cytoskeleton by activating a series of signaling pathways. These include prolonged induction of the mitogen-activated protein (MAP) kinase Erk1/2 leading to enhanced expression of the activator protein-1 (AP-1) transcription factor, c-Fos [
28]. c-Fos is essential for osteoclast generation [
29], and mice deleted of the molecule are resistant to the bone loss of inflammatory arthritis. Interestingly, c-Fos overexpression in α
vβ
3-deficient osteoclasts substantially rescues the cells' capacity to organize their cytoskeleton [
28]. In contrast, the integrin is itself necessary for the cell to adequately degrade bone [
28].
The best characterized method by which α
vβ
3 mediates the resorptive process is through the Rho GTPase, Rac [
30]. In this paradigm, α
vβ
3 occupancy recruits the proto-oncogene c-Src, which in turn phosphorylates the tyrosine kinase Syk. Activated Syk stimulates the guanine nucleotide exchange factor Vav3, the dominant isoform in osteoclasts, which transits Rac from its inactive GDP-bound form to active Rac-GTP [
31]. Deletion of any of the above-mentioned signaling molecules results in a disturbance of the osteoclast cytoskeleton and the cell's capacity to resorb bone [
24,
31-
33]. Like α
vβ
3, c-Src appears coincidentally with osteoclast differentiation [
34,
35] and is currently an anti-resorptive therapeutic target [
36].