Beniash Elia, Metzler Rebecca A, Lam Raymond S K, Gilbert P U P A
University of Pittsburgh School of Dental Medicine, Department of Oral Biology, Pittsburgh, PA 15261, USA.
J Struct Biol. 2009 May;166(2):133-43. doi: 10.1016/j.jsb.2009.02.001. Epub 2009 Feb 13.
Enamel, the hardest tissue in the body, begins as a three-dimensional network of nanometer size mineral particles, suspended in a protein gel. This mineral network serves as a template for mature enamel formation. To further understand the mechanisms of enamel formation we characterized the forming enamel mineral at an early secretory stage using X-ray absorption near-edge structure (XANES) spectromicroscopy, transmission electron microscopy (TEM), FTIR microspectroscopy and polarized light microscopy. We show that the newly formed enamel mineral is amorphous calcium phosphate (ACP), which eventually transforms into apatitic crystals. Interestingly, the size, shape and spatial organization of these amorphous mineral particles and older crystals are essentially the same, indicating that the mineral morphology and organization in enamel is determined prior to its crystallization. Mineralization via transient amorphous phases has been previously reported in chiton teeth, mollusk shells, echinoderm spicules and spines, and recent reports strongly suggest the presence of transient amorphous mineral in forming vertebrate bones. The present finding of transient ACP in murine tooth enamel suggests that this strategy might be universal.
牙釉质是人体中最坚硬的组织,最初是由纳米级矿物颗粒构成的三维网络,悬浮在蛋白质凝胶中。这种矿物网络是成熟牙釉质形成的模板。为了进一步了解牙釉质形成的机制,我们使用X射线吸收近边结构(XANES)光谱显微镜、透射电子显微镜(TEM)、傅里叶变换红外光谱显微镜和偏光显微镜,对早期分泌阶段正在形成的牙釉质矿物进行了表征。我们发现新形成的牙釉质矿物是无定形磷酸钙(ACP),最终会转变为磷灰石晶体。有趣的是,这些无定形矿物颗粒和较老晶体的大小、形状和空间组织基本相同,这表明牙釉质中的矿物形态和组织在结晶之前就已确定。先前在石鳖牙齿、软体动物贝壳、棘皮动物的骨针和刺中报道过通过短暂无定形相进行矿化,最近的报道有力地表明在正在形成的脊椎动物骨骼中存在短暂无定形矿物。在小鼠牙釉质中发现短暂存在的ACP表明这种策略可能具有普遍性。