Linde A, Lussi A, Crenshaw M A
Dental Research Center, University of North Carolina, Chapel Hill.
Calcif Tissue Int. 1989 Apr;44(4):286-95. doi: 10.1007/BF02553763.
The purpose of this study was to investigate the mineral induction capacity in vitro of polyanionic proteins covalently bound to a surface. Rat dentin gamma-carboxyglutamate-containing protein of the osteocalcin type (Gla-protein), proteoglycan (PG), and phosphoprotein (PP-H), as well as phosvitin (PhV) and bovine serum albumin (BSA), were covalently linked to agarose beads. There were incubated at 37 degrees C in solutions with a Ca/P molar ratio of 1.67, [Ca][P] molar products in the range 1.0-1.8 mM2, and an ionic strength of 0.165. The incubations were performed at constant pH and composition conditions; no spontaneous precipitation occurred under these conditions. Mineral formation, as monitored by scanning electron microscopy (SEM), was induced by all immobilized polyanions, including enzymatically dephosphorylated PP-H and PhV. No mineral was induced by BSA. The mineral inductive capacity of immobilized polyanionic proteins, as judged by the SEM after identical incubations, was found to differ between the different ligands. The mineral induced by PP-H and PG was shown by X-ray diffraction to be apatitic. It was concluded that, although polyanionic proteins in solution may inhibit mineral induction and growth, very minute quantities of such molecules, when immobilized on a surface, induce mineral at physiological concentrations of calcium and phosphate ions. The data presented may be taken to suggest that PP-H and PG, and perhaps other polyanions, may possibly be responsible for mineral nucleation in dentin and bone. The results, however, also point to the rather limited specificity in this type of reaction.
本研究的目的是调查共价结合于表面的聚阴离子蛋白的体外矿物质诱导能力。骨钙素型含γ-羧基谷氨酸的大鼠牙本质蛋白(Gla蛋白)、蛋白聚糖(PG)和磷蛋白(PP-H),以及卵黄高磷蛋白(PhV)和牛血清白蛋白(BSA),被共价连接到琼脂糖珠上。将它们在37℃下于钙磷摩尔比为1.67、钙磷摩尔积在1.0 - 1.8 mM²范围内且离子强度为0.165的溶液中孵育。孵育在恒定的pH和组成条件下进行;在这些条件下未发生自发沉淀。通过扫描电子显微镜(SEM)监测,所有固定化的聚阴离子,包括经酶促去磷酸化的PP-H和PhV,均诱导了矿物质形成。BSA未诱导矿物质形成。在相同孵育后通过SEM判断,固定化聚阴离子蛋白的矿物质诱导能力在不同配体之间存在差异。X射线衍射显示PP-H和PG诱导形成的矿物质为磷灰石。得出的结论是,尽管溶液中的聚阴离子蛋白可能抑制矿物质诱导和生长,但当极少量的此类分子固定在表面时,在生理浓度的钙离子和磷酸根离子条件下可诱导矿物质形成。所呈现的数据可能表明PP-H和PG,或许还有其他聚阴离子,可能是牙本质和骨中矿物质成核的原因。然而,结果也表明这类反应的特异性相当有限。