Merwin D R, Harris E F
Department of Orthodontics, College of Dentistry, University of Tennessee, Memphis 38163, USA.
Arch Oral Biol. 1998 Mar;43(3):205-10. doi: 10.1016/s0003-9969(98)00003-x.
The extent of tooth mineralization is a useful estimate of a child's physiological age it reflects the rate at which the child is developing towards maturity. As it is not known to what degree dental age is regulated by the genotype, this investigation estimated familial resemblance in the tempo of tooth mineralization. Panoramic radiographs of the children in 185 sibships were scored for stages of tooth formation, and dental age was calculated from sex-specific standards. Intraclass correlations of mineralization tempo were computed for maxillary and mandibular canines, premolars, second molars, and third molars. Correlations of mineralization tempo were significantly different than zero for all 10 teeth and ranged from 0.17 (SE = 0.06) for the mandibular second molar to 0.43 (SE = 0.05) for the mandibular second premolar. Intraclass correlations increased significantly when multiple teeth were used to more comprehensively define each child's dental age. Using an unweighted average of all 10 tooth types yielded a correlation of 0.41 (SE = 0.05). It appears, then, that a considerable proportion of the total variability in tooth-mineralization rate can be attributed to transmissible effects operating in the population under investigation.
牙齿矿化程度是对儿童生理年龄的一种有效估计,它反映了儿童向成熟发展的速度。由于尚不清楚牙齿年龄在多大程度上受基因型调控,本研究估计了牙齿矿化速度方面的家族相似性。对185个同胞关系中儿童的全景X线片进行牙齿形成阶段评分,并根据特定性别的标准计算出牙龄。计算了上颌和下颌尖牙、前磨牙、第二磨牙和第三磨牙矿化速度的组内相关系数。所有10颗牙齿的矿化速度相关系数均显著不同于零,范围从下颌第二磨牙的0.17(标准误 = 0.06)到下颌第二前磨牙的0.43(标准误 = 0.05)。当使用多颗牙齿更全面地定义每个儿童的牙龄时,组内相关系数显著增加。使用所有10种牙齿类型的未加权平均值得出的相关系数为0.41(标准误 = 0.05)。因此,牙齿矿化速度总变异性中相当大的一部分似乎可归因于在所研究人群中起作用的可传递效应。