Ferrari S, Rizzoli R, Bonjour J P
WHO Collaborating Center for Osteoporosis and Bone Diseases, Department of Internal Medicine, University Hospital, Geneva, Switzerland.
Aging (Milano). 1998 Jun;10(3):205-13. doi: 10.1007/BF03339654.
Osteoporosis is the net result of the maximal amount of bone mineral mass achieved by the end of pubertal growth (peak bone mass) minus post-menopausal and elderly bone losses. Peak bone mineral mass is determined from early childhood by both heritable and environmental factors. Recent developments in the molecular epidemiology of osteoporosis have shown the interest, but also the limitations, of specific molecular markers, such as the vitamin D receptor gene polymorphisms Bsm 1 and Fok 1, to explain bone mineral density differences across the population. Importantly, however, interactions between VDR gene polymorphisms and environmental factors, particularly dietary calcium, have provided new insights into the complex determination of bone mineral mass.
骨质疏松症是青春期生长结束时所达到的最大骨矿物质含量(峰值骨量)减去绝经后和老年期骨质流失后的最终结果。峰值骨量从儿童早期就由遗传和环境因素决定。骨质疏松症分子流行病学的最新进展表明,特定分子标记物,如维生素D受体基因多态性Bsm 1和Fok 1,在解释人群中骨矿物质密度差异方面既有意义,也有局限性。然而,重要的是,VDR基因多态性与环境因素,特别是膳食钙之间的相互作用,为骨矿物质含量的复杂决定因素提供了新的见解。