Facility for Electron Microscopy Research, Department of Anatomy and Cell Biology and Faculty of Dentistry, McGill University, Montreal, Quebec H3A 2B2, Canada.
J Biol Chem. 2011 May 20;286(20):18149-60. doi: 10.1074/jbc.M110.194258. Epub 2011 Mar 23.
Enamel formation depends on a triad of tissue-specific matrix proteins (amelogenin, ameloblastin, and enamelin) to help initiate and stabilize progressively elongating, thin mineral ribbons of hydroxyapatite formed during an appositional growth phase. Subsequently, these proteins are eradicated to facilitate lateral expansion of the hydroxyapatite crystallites. The purpose of this study was to investigate changes in enamel mineralization occurring in mice unable to produce kallikrein 4 (Klk4), a proteinase associated with terminal extracellular degradation of matrix proteins during the maturation stage. Mice lacking functional matrix metalloproteinase 20 (Mmp20), a proteinase associated with early cleavage of matrix proteins during the secretory stage, were also analyzed as a frame of reference. The results indicated that mice lacking Klk4 produce enamel that is normal in thickness and overall organization in terms of layers and rod/inter-rod structure, but there is a developmental defect in enamel rods where they first form near the dentinoenamel junction. Mineralization is normal up to early maturation after which the enamel both retains and gains additional proteins and is unable to mature beyond 85% mineral by weight. The outmost enamel is hard, but inner regions are soft and contain much more protein than normal. The rate of mineral acquisition overall is lower by 25%. Mice lacking functional Mmp20 produce enamel that is thin and structurally abnormal. Relatively high amounts of protein remain throughout maturation, but the enamel is able to change from 67 to 75% mineral by weight during maturation. These findings reaffirm the importance of secreted proteinases to enamel mineral acquisition.
牙釉质的形成依赖于一组组织特异性基质蛋白(釉原蛋白、釉基质蛋白和釉蛋白),这些蛋白有助于启动和稳定逐渐延长的、薄的羟基磷灰石矿物质带的形成,这些矿物质带是在增生期形成的。随后,这些蛋白被清除,以促进羟基磷灰石晶体的侧向扩展。本研究的目的是研究不能产生激肽释放酶 4(Klk4)的小鼠中牙釉质矿化的变化,Klk4 是一种与基质蛋白成熟阶段的细胞外终末降解相关的蛋白水解酶。还分析了缺乏功能基质金属蛋白酶 20(Mmp20)的小鼠,Mmp20 是一种与基质蛋白分泌阶段早期裂解相关的蛋白水解酶。结果表明,缺乏 Klk4 的小鼠产生的牙釉质在厚度和整体组织方面都是正常的,在层次和杆/杆间结构方面也是正常的,但牙釉质杆的发育存在缺陷,牙釉质杆首先在牙本质-釉质交界处附近形成。矿化在早期成熟之前是正常的,之后牙釉质既保留又获得额外的蛋白,并且不能超过 85%的重量达到成熟。最外层的牙釉质是坚硬的,但内层是柔软的,并且比正常情况下含有更多的蛋白。总体上矿物质的获得率低了 25%。缺乏功能性 Mmp20 的小鼠产生的牙釉质很薄,结构异常。在成熟过程中相对大量的蛋白仍然存在,但牙釉质在成熟过程中能够从 67%到 75%的重量变化。这些发现再次证实了分泌蛋白水解酶对牙釉质矿化的重要性。