Role of physical activity in the development of skeletal mass in children.

A group of 118 children, aged 5.3-14 years, were enrolled in a prospective study of calcium supplementation and bone mass. At entry to the study, questionnaires regarding the child's usual physical activity were administered to the children and their mothers. Repeated activity assessments at 6 month intervals indicated good within-person agreement for total activity and for most individual activities. Consistent positive associations were observed between bone mineral densities (BMD) in the radius, spine, and hip and most activities. A summary measure (total hours of weight-bearing activity) was significantly related to BMD in the radius and hip, independently of age or gender effects. Self-reported sports and play activities were associated with BMD, but neither time spent watching television nor hours of physical education classes were associated either positively or negatively with skeletal mass. These data suggest that important increments in skeletal mass may result from physical activity during childhood.

Genetic influences on the urinary excretion of aldosterone in children.

Several studies have shown an inverse relation between blood pressure and plasma aldosterone levels. Since blood pressure is in part genetically regulated, we looked for evidence that genetic factors might also affect aldosterone production. The nocturnal urinary excretion rate was used to estimate aldosterone production, and electrolyte excretion rates were used to estimate sodium and potassium intakes. Studies were carried out in monozygotic (MZ) (n = 37 pairs) and dizygotic (DZ) (n = 26 pairs) twins, aged 6-17 years. Both groups of twins were white. The intraclass correlation coefficient for aldosterone excretion was 0.686 (p = 0.0001) for MZ twins, and 0.290 (p = 0.079) for DZ twins, indicating high heritability for the aldosterone excretion rate. In a second study, we looked for a racial effect on the genetic regulation of aldosterone excretion. Siblings from both black and white families (72 black siblings and 157 white siblings) were selected from an ongoing longitudinal study. Mean values for nocturnal aldosterone excretion, rates measured every 6 months over 1.5-3.5 years, were used in the analysis. The intraclass correlation coefficient for aldosterone excretion, adjusted for sodium and potassium excretion, was 0.510 (p = 0.001) for black siblings and 0.087 (p = 0.228) for white siblings, indicating a strong familial aggregation for aldosterone excretion in black children. In conclusion, studies in twins showed that regulation of urinary aldosterone excretion in children is determined partially by genetic factors. A familial component affecting the aldosterone excretion rate appears to be much stronger in blacks than in whites.

Long-term bone loss in men: effects of genetic and environmental factors.

OBJECTIVE: To identify environmental factors associated with bone loss in adult male twins and to determine the extent to which shared environmental characteristics affect estimates of the genetic influence on bone loss. DESIGN: A 16-year cohort study. SETTING: A midwestern university hospital. PARTICIPANTS: One hundred and eleven male veterans of World War II or the Korean conflict, born between 1916 and 1927. All were twins, with the sample comprising 48 pairs and 15 persons whose twin brothers were deceased or seriously ill. MEASUREMENTS: Bone mass and environmental characteristics (cigarette smoking, alcohol consumption, physical activity, dietary calcium intake, use of thiazide diuretics) measured at baseline and 16 years later. RESULTS: Rates of radial bone loss averaged 0.45% per year. Those who both smoked and used alcohol at levels greater than the median for the population had a rate of bone loss (10% in 16 years) twice the rate of those who were below the median level for both variables (5% bone loss, P = 0.003). Rates of bone loss were correlated within twin pairs, and these correlations were diminished 25% to 35% by adjustments for environmental influences on bone loss. However, statistically significant within-pair correlations remained (r = 0.4), which did not differ between monozygotic and dizygotic twin pairs after adjustments for smoking, alcohol use, dietary calcium intake, and exercise. CONCLUSIONS: Bone loss in men during mid-life is determined, at least in part, by environmental factors, including smoking, alcohol intake, and, possibly, physical activity. Rates of bone loss were similar within twin pairs, apparently because of a shared environment.

The relationship of bone mineral density and anthropometric variables in healthy male and female children.

The relationships among bone mineral measurements at hip, wrist, and spine sites and anthropometric measurements which provided estimates of frame size, skinfold thickness, and muscularity were examined in a population of 140 children. The average age of the children at the time of measurement was 9.5 +/- 2.5 years and all subjects were white. In this study population, the anthropometric measurements were generally highly intercorrelated. Univariate correlations among bone mass and density variables at the different sites were also high, especially in the female children. Model fitting procedures were employed to separate the effects of age, frame size, and fatness on the bone mass measures. Resulting models confirmed previous results which suggest that height is the best predictor of bone mass in children. As expected, models for bone mineral content and bone mineral density were similar. Models for hips and wrist sites were also similar in including an estimate of frame size, while in those for the spine hip circumference explained a greater percentage of the variance. It appears that there are several identifiable characteristics among the anthropometric variables which appear to exert differential effects on skeletal development in children.

Influences on skeletal mineralization in children and adolescents: evidence for varying effects of sexual maturation and physical activity.

OBJECTIVE: To establish rates of skeletal mineralization in children and adolescents, and to identify factors that influence these rates. DESIGN: Three-year observational study. SETTING: University hospital. SUBJECTS: Ninety white children, aged 6 to 14 years. MEASUREMENTS: Bone mineral density of the radius, spine, and hip was measured at baseline and 3 years later. Physical activity was assessed by questionnaires at 6-month intervals and dietary calcium intake by diet diary 1 day per month for 36 months. Sexual maturation (Tanner stage) was determined by an endocrinologist at 6-month intervals, as necessary to classify children as prepubertal, peripubertal, or postpubertal. RESULTS: Skeletal mineralization accelerated markedly at puberty in the spine (0.077 vs 0.027 gm/cm2 per year, peripubertal vs prepubertal) and greater trochanter (0.050 vs 0.027 gm/cm2 per year), less markedly in the femoral neck (0.047 vs 0.030 gm/cm2 per year), and only slightly in the radius. Nearly one third (15 gm) of the total skeletal mineral in the lumbar spine of adult women (approximately 52 gm) was accumulated in the 3 years around the onset of puberty. Increases in height and weight were the strongest correlates of skeletal mineralization: weight changes were more strongly correlated with trabecular bone sites and changes in height with cortical bone sites. Increases in calf muscle area were strongly associated with mineralization, particularly in peripubertal children, and physical activity was associated with more rapid mineralization in prepubertal children. CONCLUSIONS: Puberty has varying effects on skeletal mineralization depending on skeletal site; trabecular bone is apparently more sensitive to changing hormone concentrations. Physical activity and normal growth are also positively associated with skeletal mineralization, also depending on skeletal site and sexual maturation.

Calcium supplementation and increases in bone mineral density in children.

BACKGROUND: Increased dietary intake of calcium during childhood, usually as calcium in milk, is associated with increased bone mass in adulthood; the increase in mass is important in modifying the later risk of fracture. Whether the increase is due to the calcium content of milk, however, is not certain. METHODS: We conducted a three-year, double-blind, placebo-controlled trial of the effect of calcium supplementation (1000 mg of calcium citrate malate per day) on bone mineral density in 70 pairs of identical twins (mean [+/- SD] age, 10 +/- 2 years; range, 6 to 14). In each pair, one twin served as a control for the other; 45 pairs completed the study. Bone mineral density was measured by photon absorptiometry at two sites in the radius (at base line, six months, and one, two, and three years) and at three sites in the hip and in the spine (at base line and three years). RESULTS: The mean daily calcium intake of the twins given placebo was 908 mg, and that of the twins given calcium supplements was 1612 mg (894 mg from the diet and 718 mg from the supplement). Among the 22 twin pairs who were prepubertal throughout the study, the twins given supplements had significantly greater increases in bone mineral density at both radial sites (mean difference in the increase in bone mineral density: midshaft radius, 5.1 percent [95 percent confidence interval, 1.5 to 8.7 percent]; distal radius, 3.8 percent [95 percent confidence interval, 1.4 to 6.2 percent]) and in the lumbar spine (increase, 2.8 percent [95 percent confidence interval, 1.1 to 4.5 percent]) after three years; the differences in the increases at two of three femoral sites approached significance (Ward's triangle in the femoral neck, 2.9 percent; greater trochanter, 3.5 percent). Among the 23 pairs who went through puberty or were postpubertal, the twins given supplements received no benefit. CONCLUSIONS: In prepubertal children whose average dietary intake of calcium approximated the recommended dietary allowance, calcium supplementation increased the rate of increase in bone mineral density. If the gain persists, peak bone density should be increased and the risk of fracture reduced.