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大鼠磨牙牙周膜和牙龈中碱性磷酸酶活性:其与牙骨质形成的关系。

Alkaline phosphatase activity in the periodontal ligament and gingiva of the rat molar: its relation to cementum formation.

作者信息

Groeneveld M C, Everts V, Beertsen W

机构信息

Department of Periodontology, Academic Centre for Dentistry (ACTA), Amsterdam, The Netherlands.

出版信息

J Dent Res. 1995 Jul;74(7):1374-81. doi: 10.1177/00220345950740070901.

Abstract

Alkaline phosphatase (ALP) is a glycoprotein thought to be involved in processes leading to mineral formation in tissues like bone and cementum. In the rat molar periodontium, several regions are associated with the formation of cementum (periodontal ligament, inner part of the gingiva), whereas other areas are not (e.g., the outer part of the gingiva just beneath the outer oral epithelium). In an attempt to establish how the spatial distribution of ALP activity relates to cementum formation, we assessed the activity of the enzyme quantitatively in the periodontium of the rat maxillary molars, by using the indoxyl-tetrazolium salt method. It appeared that the distribution of enzyme activity in the ligament was heterogeneous, indicating local variations in the phosphate household. Highest activity was found in areas related to mineralization, adjacent to the alveolar bone and cementum. Enzyme activity was higher adjacent to cellular cementum than to acellular cementum. With respect to acellular cementum, a highly significant positive correlation was found between ALP activity and cementum thickness, which indicates a close relationship between local phosphate production and cementum formation rate. An interesting observation in the connective tissue of the gingiva mesial to the first molar was a sharp demarcation between an ALP-positive inner part, adjacent to the tooth, and an ALP-negative outer part, underneath the outer oral epithelium. In the interdental gingiva, the entire connective tissue proved positive for the enzyme, suggesting that this region consists of the combined inner gingival parts of two adjacent teeth.

摘要

碱性磷酸酶(ALP)是一种糖蛋白,被认为参与了诸如骨骼和牙骨质等组织中矿物质形成的过程。在大鼠磨牙牙周组织中,几个区域与牙骨质的形成有关(牙周韧带、牙龈内部),而其他区域则无关(例如,紧邻口腔外侧上皮下方的牙龈外部)。为了确定碱性磷酸酶活性的空间分布与牙骨质形成之间的关系,我们采用吲哚酚四氮唑盐法,对大鼠上颌磨牙牙周组织中的该酶活性进行了定量评估。结果显示,韧带中酶活性的分布是不均匀的,这表明磷酸盐代谢存在局部差异。在与矿化相关的区域,即紧邻牙槽骨和牙骨质处,发现了最高的活性。细胞牙骨质附近的酶活性高于无细胞牙骨质。对于无细胞牙骨质,碱性磷酸酶活性与牙骨质厚度之间存在高度显著的正相关,这表明局部磷酸盐生成与牙骨质形成速率之间存在密切关系。在第一磨牙近中的牙龈结缔组织中,一个有趣的观察结果是,紧邻牙齿的碱性磷酸酶阳性内部与口腔外侧上皮下方的碱性磷酸酶阴性外部之间有明显的界限。在牙龈乳头中,整个结缔组织对该酶呈阳性反应,这表明该区域由相邻两颗牙齿的牙龈内部组合而成。

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