Takano Yoshiro, Sakai Hideo, Watanabe Eiko, Ideguchi-Ohma Noriko, Jayawardena Chantha K, Arai Kazumi, Asawa Yukiyo, Nakano Yukiko, Shuda Yoko, Sakamoto Yujiro, Terashima Tatsuo
Division of Biostructural Science, Graduate School, Tokyo Medical and Dental University, 1-5-45 Yushima, Bunkyo-ku, Tokyo 113-8549, Japan.
J Electron Microsc (Tokyo). 2003;52(6):573-80. doi: 10.1093/jmicro/52.6.573.
The mechanism whereby a region-specific deposition of the two types of cementum (cellular cementum and acellular extrinsic fibre cementum) is regulated on the growing root surface was tested using bisphosphonate-affected teeth of young rats and guinea pigs. The animals were injected subcutaneously with 8 or 10 mg P x kg body weight(-1) x day(-1) of 1-hydroxyethylidene-1,1-bisphosphonate (HEBP) for 1 or 2 weeks. In rat molars, HEBP prevented mineralization of newly formed root dentin matrix and totally inhibited de novo deposition of acellular extrinsic fibre cementum. Instead, thick cellular cementum was induced on the non-mineralized root dentin surface, irrespective of the position of the root. In both animals, cellular cementum was also induced on the non-mineralized surface of root analogue dentin in HEBP-affected incisors, where only acellular extrinsic fibre cementum is deposited under normal conditions. In normal rat molars, dentin sialoprotein (DSP) was concentrated along the dentin-cellular cementum border, but not that of dentin and acellular extrinsic fibre cementum. In HEBP-affected rat incisors, DSP was shown to penetrate through the non-mineralized dentin into the surrounding tissues, but not through the mineralized portions. These data suggest that, at the site of cellular cementum formation, putative inducing factors for cellular cementum might diffuse into the periodontal space through the newly deposited mantle dentin matrix before it is mineralized. At earlier stages of root formation, mantle dentin might mineralize more promptly not to allow such diffusion. The timing of mineralization of mantle dentin matrix might be the key determinant of the types of the cementum deposited on the growing root surface.
利用双膦酸盐处理的幼年大鼠和豚鼠牙齿,测试了在生长中的牙根表面两种牙骨质(细胞性牙骨质和无细胞外源性纤维牙骨质)区域特异性沉积的调控机制。给动物皮下注射8或10 mg P×kg体重⁻¹×天⁻¹的1-羟基亚乙基-1,1-双膦酸盐(HEBP),持续1或2周。在大鼠磨牙中,HEBP阻止了新形成的牙根牙本质基质的矿化,并完全抑制了无细胞外源性纤维牙骨质的从头沉积。相反,在未矿化的牙根牙本质表面诱导形成了厚厚的细胞性牙骨质,而与牙根的位置无关。在这两种动物中,在HEBP处理的切牙牙根类似牙本质的未矿化表面也诱导形成了细胞性牙骨质,在正常情况下该部位仅沉积无细胞外源性纤维牙骨质。在正常大鼠磨牙中,牙本质涎蛋白(DSP)沿牙本质-细胞性牙骨质边界聚集,但在牙本质和无细胞外源性纤维牙骨质边界则没有。在HEBP处理的大鼠切牙中,DSP被证明可穿过未矿化的牙本质进入周围组织,但不能穿过矿化部分。这些数据表明,在细胞性牙骨质形成部位,细胞性牙骨质的假定诱导因子可能在新沉积的罩牙本质基质矿化之前通过它扩散到牙周间隙。在牙根形成的早期阶段,罩牙本质可能更快地矿化,以阻止这种扩散。罩牙本质基质矿化的时间可能是生长牙根表面沉积的牙骨质类型的关键决定因素。