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硫酸软骨素参与牛牙本质小管周有机基质的过度钙化。

Chondroitin sulfate is involved in the hypercalcification of the organic matrix of bovine peritubular dentin.

作者信息

Dorvee Jason R, Gerkowicz Lauren, Bahmanyar Sara, Deymier-Black Alix, Veis Arthur

机构信息

Northwestern University, Feinberg School of Medicine, Chicago, IL 60611, USA.

Northwestern University, Feinberg School of Medicine, Chicago, IL 60611, USA.

出版信息

Arch Oral Biol. 2016 Feb;62:93-100. doi: 10.1016/j.archoralbio.2015.11.008. Epub 2015 Nov 12.

Abstract

Apatitic mineral of dentin forms within the collagenous matrix (intertubular dentin, ITD) secreted from the odontoblastic processes (OP). Highly calcified mineral (peritubular dentin, PTD) is deposited at the interface between the ITD and each process membrane, creating a tubular system penetrating the dentin that extends from the dentino-enamel junction to the predentin-dentin junction. We focus on determining the composition of the PTD both with regard to its organic matrix and the inorganic phase. A laser capture technique has been adapted for the isolation of the mineralized PTD free from the ITD, and for the analysis of the PTD by SEM, TEM, and energy dispersive spectrometry (EDS), these data were subsequently compared with similar analyses of intact dentin slices containing ITD bounded-PTD annuli. Elemental line scans reveal clearly marked boundaries between ITD, PTD, and OP components, and illustrate the differences in composition, and topographical surface roughness. The organic matrix of the PTD was shown to be sulfur rich, and further antibody labeling showed the sulfated organic component to be chondroitin sulfate [corrected]. In this PTD organic matrix the S/Ca and Ca/P ratios were distinctly higher than in the ITD, indicating that polysaccharide bound S supplies the anionic counterion facilitating the formation of the apatitic PTD mineral.

摘要

牙本质的无定形矿物在成牙本质细胞突起(OP)分泌的胶原基质(管间牙本质,ITD)内形成。高度钙化的矿物(管周牙本质,PTD)沉积在ITD与每个突起膜之间的界面处,形成一个贯穿牙本质的管状系统,该系统从牙本质-釉质界延伸至前期牙本质-牙本质界。我们专注于确定PTD在有机基质和无机相方面的组成。一种激光捕获技术已被用于从ITD中分离矿化的PTD,并通过扫描电子显微镜(SEM)、透射电子显微镜(TEM)和能量色散光谱(EDS)对PTD进行分析,随后将这些数据与对含有与ITD结合的PTD环的完整牙本质切片的类似分析进行比较。元素线扫描清楚地显示了ITD、PTD和成牙本质细胞突起成分之间明显的边界,并说明了组成和表面形貌粗糙度的差异。结果表明,PTD的有机基质富含硫,进一步的抗体标记显示硫酸化有机成分是硫酸软骨素[校正后]。在这种PTD有机基质中,S/Ca和Ca/P比值明显高于ITD,表明多糖结合的S提供了促进磷灰石PTD矿物形成的阴离子抗衡离子。

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