Teti A, Blair H C, Teitelbaum S L, Kahn A J, Koziol C, Konsek J, Zambonin-Zallone A, Schlesinger P H
Institute of Human Anatomy, University of Bari Medical School, Italy.
J Clin Invest. 1989 Jan;83(1):227-33. doi: 10.1172/JCI113863.
Osteoclasts resorb bone by first attaching to the bone surface and then secreting protons into an isolated extracellular compartment formed at the cell-bone attachment site. This secretion of protons (local acidification) is required to solubilize bone hydroxyapatite crystals and for activity of bone collagen-degrading acid proteases. However, the large quantity of protons required, 2 mol/mol of calcium, would result in an equal accumulation of cytosolic base equivalents. This alkaline load must be corrected to maintain cytosolic pH within physiologic limits. In this study, we have measured cytoplasmic pH with pH-sensitive fluorescent compounds, while varying the extracellular ionic composition of the medium, to determine the nature of the compensatory mechanism used by osteoclasts during bone resorption. Our data show that osteoclasts possess a chloride/bicarbonate exchanger that enables them to maintain normal intracellular pH in the face of a significant proton efflux. This conclusion follows from the demonstration of a dramatic cytoplasmic acidification when osteoclasts that have been incubated in bicarbonate-containing medium are transferred into bicarbonate-free medium. This acidification is absolutely dependent on and proportional to medium [Cl-]. Furthermore, acidification is inhibited by the classic inhibitor of red cell anion exchange, 4,4'-diisothiocyanatostilbene-2,2'-disulfonate, and by diphenylamine-2-carboxylate, an inhibitor of chloride specific channels. However, the acidification process is neither energy nor sodium dependent. The physiologic importance of chloride/bicarbonate exchange is demonstrated by the chloride dependence of recovery from an endogenous or exogenous alkaline load in osteoclasts. We conclude that chloride/bicarbonate exchange is in large part responsible for cytoplasmic pH homeostasis of active osteoclasts, showing that these cells are similar to renal tubular epithelial cells in their regulation of intracellular pH.
破骨细胞通过首先附着于骨表面,然后将质子分泌到在细胞 - 骨附着位点形成的孤立细胞外隔室来吸收骨。质子的这种分泌(局部酸化)是溶解骨羟基磷灰石晶体以及骨胶原降解酸性蛋白酶活性所必需的。然而,所需的大量质子(每摩尔钙2摩尔)会导致等量的胞质碱基当量积累。必须纠正这种碱性负荷以将胞质pH维持在生理限度内。在本研究中,我们使用对pH敏感的荧光化合物测量细胞质pH,同时改变培养基的细胞外离子组成,以确定破骨细胞在骨吸收过程中使用的补偿机制的性质。我们的数据表明,破骨细胞拥有一种氯/碳酸氢盐交换体,使其能够在大量质子外流的情况下维持正常细胞内pH。这一结论源于以下证明:当在含碳酸氢盐的培养基中孵育的破骨细胞转移到无碳酸氢盐的培养基中时,会出现显著的细胞质酸化。这种酸化绝对依赖于培养基[Cl-]并与之成比例。此外,酸化受到红细胞阴离子交换的经典抑制剂4,4'-二异硫氰基芪-2,2'-二磺酸盐以及氯特异性通道抑制剂二苯胺-2-羧酸盐的抑制。然而,酸化过程既不依赖能量也不依赖钠。破骨细胞中内源性或外源性碱性负荷恢复对氯的依赖性证明了氯/碳酸氢盐交换的生理重要性。我们得出结论,氯/碳酸氢盐交换在很大程度上负责活性破骨细胞的细胞质pH稳态,表明这些细胞在细胞内pH调节方面与肾小管上皮细胞相似。