Wuthier R E, Rice G S, Wallace J E, Weaver R L, LeGeros R Z, Eanes E D
Calcif Tissue Int. 1985 Jul;37(4):401-10. doi: 10.1007/BF02553710.
Release of mitochondrial calcium has been shown to occur concomitant with mineral ion loading of matrix vesicles at the onset of mineralization in epiphyseal growth plate cartilage. Matrix vesicles contain amorphous calcium phosphate (ACP), a mineral form that usually results from rapid precipitation at high initial levels of Ca2+ and/or inorganic P (Pi). Since the cytosol of growth plate chondrocytes has been found to contain high levels of Pi, rapid release of mitochondrial Ca2+ into the cytosol may cause local precipitation of calcium phosphate and thus be coupled with matrix vesicle formation. Studies were carried out to determine the kinetics and nature of mineral formation that occur when small amounts of Ca2+ are added under various conditions to a Pi buffer composed of electrolytes matched in concentrations and pH to that of the cytosol of epiphyseal chondrocytes. Depending on the manner in which Ca2+ was added, ACP, dicalcium phosphate dihydrate (DCPD), or apatite (HA) first formed. In the presence of ATP, ACP was the only solid phase detected, being stable for at least 24 h. However, in its absence, ACP rapidly transformed into DCPD. Increasing the pH of the reaction buffer from 6.9 to 7.5 increased the amount of ACP initially formed, but DCPD was consistently found upon ACP transformation. Yet at pH 8.0, ACP persisted for at least 24 h. The amount of precipitate formed was proportional to the level of added Ca2+; precipitates formed when as little as 1.0 mmole was added per liter of buffer. Our findings support the possibility that rapid release of mitochondrial Ca2+ may cause localized intracellular precipitation of ACP. Since nascent ACP is known to stimulate membrane fusion and blebbing of vesicles, these findings may explain the presence of ACP in matrix vesicles. The rapid conversion of ACP to DCPD in the absence of ATP under these conditions may also explain the reported occurrence of DCPD in samples of early mineralizing tissue.
在骨骺生长板软骨矿化开始时,线粒体钙的释放已被证明与基质小泡的矿物质离子负载同时发生。基质小泡含有无定形磷酸钙(ACP),这种矿物质形式通常是在高初始水平的Ca2+和/或无机磷(Pi)下快速沉淀产生的。由于已发现生长板软骨细胞的细胞质中含有高水平的Pi,线粒体Ca2+快速释放到细胞质中可能会导致磷酸钙的局部沉淀,从而与基质小泡的形成相关联。开展了多项研究,以确定在各种条件下向由浓度和pH值与骨骺软骨细胞细胞质相匹配的电解质组成的Pi缓冲液中添加少量Ca2+时发生的矿物质形成动力学和性质。根据添加Ca2+的方式,首先形成了ACP、二水磷酸二钙(DCPD)或磷灰石(HA)。在ATP存在的情况下,ACP是唯一检测到的固相,至少稳定24小时。然而,在没有ATP的情况下,ACP会迅速转化为DCPD。将反应缓冲液的pH值从6.9提高到7.5会增加最初形成的ACP的量,但在ACP转化后始终会发现DCPD。然而,在pH 8.0时,ACP至少持续24小时。形成的沉淀量与添加的Ca2+水平成正比;每升缓冲液添加低至1.0毫摩尔时就会形成沉淀。我们的研究结果支持线粒体Ca2+的快速释放可能导致细胞内ACP局部沉淀的可能性。由于已知新生的ACP会刺激小泡的膜融合和出泡,这些研究结果可能解释了基质小泡中ACP的存在。在这些条件下,在没有ATP的情况下ACP迅速转化为DCPD,这也可能解释了早期矿化组织样本中报道的DCPD的出现。