Boyan B D, Schwartz Z, Swain L D, Khare A
University of Texas Health Science Center, San Antonio 78284.
Anat Rec. 1989 Jun;224(2):211-9. doi: 10.1002/ar.1092240210.
This review addresses the role of lipids and membranes in biologic calcification and examines their regulation during endochondral ossification. The close association of lipids with mineral deposition has been well established. Early observations indicated that lipids, particularly phospholipids, can not be totally extracted from calcified tissues until the tissues are decalcified. Phospholipids associated with mineral are also enriched in extracellular membrane vesicles, called matrix vesicles. Numerous studies indicate that mineral deposits in calcifying cartilage are first seen in these phosphatidylserine and alkaline phosphatase enriched vesicles and that the process of endochondral calcification of epiphyseal growth plate is possibly mediated by them. Matrix vesicles, and the phospholipids present in them, appear to be involved in initial formation of calcium hydroxyapatite crystals via the interaction of calcium and phosphate ions with phosphatidylserine to form phospholipid:Ca:Pi complexes (CPLX). CPLX is present in tissues which are undergoing initial mineral deposition but are absent from nonmineralizing tissues. Evidence suggests that CPLX resides in the interior of matrix vesicles where the earliest mineral crystals are formed in association with the vesicle membrane. More recently, it has been determined that specific membrane proteins, called proteolipids, participate in CPLX formation and hydroxyapatite deposition, in part by structuring phosphatidylserine in an appropriate conformation. Phosphatidylserine involvement in the initiation of mineralization has been extensively investigated because of its extremely high binding affinity for Ca2+. In addition to structuring a specific phospholipid environment, proteolipids may also act as ionophores, promoting export of protons and import of calcium and phosphate, both requirements of biologic calcification.(ABSTRACT TRUNCATED AT 250 WORDS)
本综述阐述了脂质和膜在生物钙化中的作用,并研究了它们在软骨内成骨过程中的调节机制。脂质与矿物质沉积之间的密切关联已得到充分证实。早期观察表明,脂质,尤其是磷脂,在组织脱钙之前无法从钙化组织中完全提取出来。与矿物质相关的磷脂在称为基质小泡的细胞外膜小泡中也很丰富。大量研究表明,钙化软骨中的矿物质沉积首先出现在这些富含磷脂酰丝氨酸和碱性磷酸酶的小泡中,并且骨骺生长板的软骨内钙化过程可能由它们介导。基质小泡及其所含的磷脂似乎通过钙离子和磷酸根离子与磷脂酰丝氨酸相互作用形成磷脂:钙:磷酸根复合物(CPLX)参与了羟基磷灰石晶体的初始形成。CPLX存在于正在经历初始矿物质沉积的组织中,而在非矿化组织中不存在。有证据表明,CPLX存在于基质小泡内部,最早的矿物质晶体在那里与小泡膜结合形成。最近,已确定一种称为蛋白脂质的特定膜蛋白参与CPLX的形成和羟基磷灰石的沉积,部分原因是它将磷脂酰丝氨酸构造成适当的构象。由于磷脂酰丝氨酸对Ca2+具有极高的结合亲和力,因此对其参与矿化起始的过程进行了广泛研究。除了构建特定的磷脂环境外,蛋白脂质还可能作为离子载体,促进质子的输出以及钙和磷的输入,这两者都是生物钙化的必要条件。(摘要截选至250词)