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氟斑牙:化学与生物学

Dental fluorosis: chemistry and biology.

作者信息

Aoba T, Fejerskov O

机构信息

The Nippon Dental University, Department of Pathology, 1-9-20 Fujimi, Chiyoda-ku, Tokyo 102, Japan.

出版信息

Crit Rev Oral Biol Med. 2002;13(2):155-70. doi: 10.1177/154411130201300206.

Abstract

This review aims at discussing the pathogenesis of enamel fluorosis in relation to a putative linkage among ameloblastic activities, secreted enamel matrix proteins and multiple proteases, growing enamel crystals, and fluid composition, including calcium and fluoride ions. Fluoride is the most important caries-preventive agent in dentistry. In the last two decades, increasing fluoride exposure in various forms and vehicles is most likely the explanation for an increase in the prevalence of mild-to-moderate forms of dental fluorosis in many communities, not the least in those in which controlled water fluoridation has been established. The effects of fluoride on enamel formation causing dental fluorosis in man are cumulative, rather than requiring a specific threshold dose, depending on the total fluoride intake from all sources and the duration of fluoride exposure. Enamel mineralization is highly sensitive to free fluoride ions, which uniquely promote the hydrolysis of acidic precursors such as octacalcium phosphate and precipitation of fluoridated apatite crystals. Once fluoride is incorporated into enamel crystals, the ion likely affects the subsequent mineralization process by reducing the solubility of the mineral and thereby modulating the ionic composition in the fluid surrounding the mineral. In the light of evidence obtained in human and animal studies, it is now most likely that enamel hypomineralization in fluorotic teeth is due predominantly to the aberrant effects of excess fluoride on the rates at which matrix proteins break down and/or the rates at which the by-products from this degradation are withdrawn from the maturing enamel. Any interference with enamel matrix removal could yield retarding effects on the accompanying crystal growth through the maturation stages, resulting in different magnitudes of enamel porosity at the time of tooth eruption. Currently, there is no direct proof that fluoride at micromolar levels affects proliferation and differentiation of enamel organ cells. Fluoride does not seem to affect the production and secretion of enamel matrix proteins and proteases within the dose range causing dental fluorosis in man. Most likely, the fluoride uptake interferes, indirectly, with the protease activities by decreasing free Ca(2+) concentration in the mineralizing milieu. The Ca(2+)-mediated regulation of protease activities is consistent with the in situ observations that (a) enzymatic cleavages of the amelogenins take place only at slow rates through the secretory phase with the limited calcium transport and that, (b) under normal amelogenesis, the amelogenin degradation appears to be accelerated during the transitional and early maturation stages with the increased calcium transport. Since the predominant cariostatic effect of fluoride is not due to its uptake by the enamel during tooth development, it is possible to obtain extensive caries reduction without a concomitant risk of dental fluorosis. Further efforts and research are needed to settle the currently uncertain issues, e.g., the incidence, prevalence, and causes of dental or skeletal fluorosis in relation to all sources of fluoride and the appropriate dose levels and timing of fluoride exposure for prevention and control of dental fluorosis and caries.

摘要

本综述旨在探讨牙釉质氟斑牙的发病机制,涉及成釉细胞活动、分泌的釉质基质蛋白与多种蛋白酶、生长中的釉质晶体以及包括钙和氟离子在内的流体成分之间的假定联系。氟化物是牙科领域最重要的防龋剂。在过去二十年中,多种形式和载体导致的氟化物暴露增加,很可能是许多社区中轻度至中度牙釉质氟斑牙患病率上升的原因,尤其是在那些已实施可控水氟化的社区。氟化物对人类牙釉质形成导致氟斑牙的影响是累积性的,并非需要特定的阈值剂量,这取决于来自所有来源的总氟摄入量以及氟化物暴露的持续时间。牙釉质矿化对游离氟离子高度敏感,游离氟离子独特地促进酸性前体如磷酸八钙的水解以及氟化磷灰石晶体的沉淀。一旦氟化物掺入牙釉质晶体中,该离子可能通过降低矿物质的溶解度从而调节矿物质周围流体中的离子组成,进而影响随后的矿化过程。根据人类和动物研究获得的证据,现在很可能氟斑牙中牙釉质矿化不全主要是由于过量氟化物对基质蛋白分解速率和/或这种降解副产物从成熟牙釉质中清除速率的异常影响。对牙釉质基质清除的任何干扰都可能在成熟阶段对伴随的晶体生长产生阻滞作用,导致牙齿萌出时牙釉质孔隙率出现不同程度的变化。目前,没有直接证据表明微摩尔水平的氟化物会影响牙釉质器官细胞的增殖和分化。在导致人类牙釉质氟斑牙的剂量范围内,氟化物似乎不会影响牙釉质基质蛋白和蛋白酶的产生与分泌。很可能氟化物的摄取通过降低矿化环境中的游离Ca(2+)浓度间接干扰蛋白酶活性。Ca(2+)介导的蛋白酶活性调节与原位观察结果一致,即(a) 在分泌阶段,随着钙转运有限,釉原蛋白的酶促裂解仅以缓慢速率发生;(b) 在正常牙釉质形成过程中,随着钙转运增加,釉原蛋白降解在过渡和早期成熟阶段似乎会加速。由于氟化物的主要防龋作用并非源于其在牙齿发育过程中被牙釉质摄取,因此有可能在不伴随牙釉质氟斑牙风险的情况下大幅降低龋齿发病率。需要进一步努力和研究来解决当前不确定的问题,例如与所有氟化物来源相关的牙釉质或骨骼氟中毒的发病率、患病率和病因,以及预防和控制牙釉质氟斑牙和龋齿的氟化物暴露的适当剂量水平和时间。

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