Bone is intimately involved in systemic mineral ion homeostasis by virtue of its interplay with parathyroid gland and kidney [1]. The extracellular calcium ion concentration (Cao ) in a compartment between actively resorbing osteoclasts and the underlying bone matrix (“a sealing zone”), which is isolated from the general extracellular space, is known to rise as high as 40 mM, while a pH value reaches as low as 4.7, by an experiment using a combination H and Ca double-barreled electrode [2]. Therefore, it is likely that Cao 2+ within the immediate microenvironment of such osteoclasts would change substantially when this high concentration of Ca is released. Indeed, during uncontrolled osteoclastic release of skeletal Ca, as in cases where there is extensive skeletal metastases of certain malignancies promoting bone resorption via osteoclast-activating, hormonal factors, such as parathyroid hormone-related peptide (PTHrP) (e.g., breast), even the levels of systemic Cao 2+ can increase well above normal and become life threatening [3]. Cao 2+ in the local skeletal microenvironment is likely to be even higher in this setting. On the other hand, several hundred milligrams of Cao 2+ enter the skeleton owing to de novo formation of bone by osteoblasts on a daily basis. Local depletion of Cao 2+ will likely take place in the immediate vicinity of osteoblasts actively forming bone. Thus, it is possible that the G protein-coupled, extracellular calcium (Cao )-sensing receptor (CaR) cloned by Brown et al. [4], which is mainly expressed in the parathyroid gland and the kidney and plays an important role in Ca homeostasis by sensing changes in Cao 2+ in the circulation [4,5], may also play some role within the skeleton by sensing such local changes in Cao 2+ caused by bone remodeling. Bone formation during the normal process of skeletal remodeling is initiated by the migration of preosteoblasts to sites of osteoclastic bone resorption, which precedes the laying down of new bone [6]. These preosteoblasts subsequently differentiate into mature osteoblasts and eventually deposit and mineralize osteoid protein. The bone resorption-induced local increases in Cao 2+ within the immediate vicinity of osteoclasts could, therefore, provide preosteoblasts with a signal that modulates their subsequent physiological responses, such as migration and proliferation. In fact, in vitro studies have showed that high Cao 2+ induces chemotaxis as well as DNA synthesis of mouse osteoblastic MC3T3-E1 cells [7–10]. MC3T3-E1 cells have the capacity to differentiate from preosteoblasts to mature osteoblasts in culture [11]. In this article, we review recent work documenting the expression of the CaR in a variety of bone cells including osteoblasts, stromal cells, monocytesmacrophages, osteoclasts, chondrocytes, and hematopoietic stem cells, as well as the involvement of the CaR in their physiological responses to the local high Cao 2+ in the skeletal microenvironment (Fig. 1).
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