Search

Histomorphometric analysis of undecalcified sections was performed in transiliac biopsy cores taken from 29 patients (16 men, 13 women, aged 51 +/- 17 years) suffering from skeletal fluorosis due to chronic exposure to fluoride. The origin of the exposure, known in 20 patients, was either by water (endemic or sporadic), or industrial, or in a few cases iatrogenic. Measured on calcified bone using a specific ion electrode, bone fluoride content was significantly high in each specimen (mean +/- SD: 0.79 +/- 0.36% of bone ash) as compared to control values (less than 0.10%). The radiologically evident osteosclerosis observed in each patient was confirmed by the significant increase of cancellous bone volume (40.1 +/- 11.2 vs. 19.0 +/- 2.8% in controls, p less than 0.0001). There were significant increases in cortical width (1292 +/- 395 vs. 934 +/- 173 microns, p less than 0.0001) and porosity (14.4 +/- 6.4 vs. 6.5 +/- 1.7%, p less than 0.002), but without reduction of cortical bone mass. Osteoid parameters were significantly increased in fluorotic patients. The increase in cancellous osteoid perimeter was almost threefold greater than that noted in cancellous eroded perimeter. The fluorotic group had a greater number of osteoblasts than controls, with a very high proportion of flat osteoblasts. In 15 patients doubly labeled with tetracycline, the mineral apposition rate was significantly decreased, while mineralization lag time significantly increased. Bone formation rate and adjusted apposition rate were significantly decreased in skeletal fluorosis. Cancellous wall width was normal in fluorosis but the formation period and active formation period were significantly increased.(ABSTRACT TRUNCATED AT 250 WORDS)

Eighty one women with vertebral osteoporosis were treated for up to 2 years with fluoride administered either as monofluorophosphate (MFP, 200 mg/day, i.e., 26.4 mg fluoride-ion) or sodium fluoride (NaF, 50 mg/day, i.e., 22.6 mg fluoride-ion). All patients received calcium supplementation (1 g of Ca2+/day) taken apart from NaF and in the same tablet for MFP. Despite almost similar fluoride dosage of both regimens, the early increase in the bone mineral density (BMD) of the lumbar spine was higher with MFP than with NaF, reaching 11% and 4%, respectively, at 1 year (p = 0.007), and 21% and 6%, respectively, at 18 months (p less than 0.001). The incidence of lower extremity pain syndrome related to benign stress microfractures was also higher with MFP than with NaF (35% and 15%, respectively, p less than 0.01). Urinary fluoride levels were higher in the MFP than in the NaF group (9.6 +/- 3.5 vs. 6.8 +/- 3.4 at one year, p = 0.003), suggesting that this difference in efficacy and tolerance is related to a better bioavailability of fluoride provided by MFP than by NaF. The occurrence of a stress microfracture could not be predicted by any clinical, biochemical, or densitometric parameter before treatment, but patients presenting with a stress microfracture during the course of the treatment had a higher gain in bone mass than those without stress fractures (at 1 yr+11 vs. +5%, p = 0.03 and at 18 months +18 vs. +6.9%, p less than 0.02). In conclusion, there is a clear correlation between the efficacy and the occurrence of side effects of fluoride therapy in osteoporosis.(ABSTRACT TRUNCATED AT 250 WORDS)

We previously showed that circulating undercarboxylated osteocalcin (ucOC) is elevated in elderly women and is a powerful marker of the subsequent risk of hip fracture in elderly institutionalized women (J Clin Invest 1993; 91:1769). To investigate the relationship between bone mass and ucOC, we measured bone mineral density (BMD) of the hip with dual-energy x-ray absorptiometry in 98 elderly institutionalized women, 81.4 +/- 6.0 years old. ucOC was negatively correlated with BMD at all sites (r = -0.26 to -0.38, p0.001 to p0.0001), even after exclusion of the effect of age by partial correlation (for the femoral neck, r = -0.26, p0.01) and after controlling for serum parathyroid hormone. BMD was significantly lower at all sites of measurement in women with elevated ucOC (1.65 ng/ml, upper limit of the normal range in young women) than in those with normal ucOC (for the neck, 0.58 +/- 0.13 versus 0.43 +/- 0.13 g/cm2, p0.001). Similar results were obtained for ucOC expressed as the fraction of total OC (ucOC%). Multiple regression showed that ucOC has the highest predictive value for BMD when including age and body weight in the equation. In summary, our data indicate that serum ucOC is an independent determinant of BMD of the hip in elderly women. The mechanism by which serum ucOC is related to bone mass is unclear and should be addressed in further studies. However, our data suggest that ucOC level may be an interesting marker in the investigation of bone status in the elderly.

Changes of bone turnover with aging are responsible for bone loss and play a major role in osteoporosis. Although an increase of bone turnover has been documented at the time of menopause, the subsequent abnormalities of bone resorption and formation and their potential role in determining bone mass in the elderly have not been investigated. To address this issue, we have measured a battery of new sensitive and specific markers of bone turnover in a population-based study of 653 healthy women analyzed cross-sectionally, including 432 women postmenopausal from 1 to 40 years, and the data were correlated with bone mineral density (BMD) measured by dual-energy X-ray absorptiometry (DXA) at different skeletal sites. Bone formation was assessed by serum osteocalcin (OC), serum bone-specific alkaline phosphatase (B-ALP), serum C-propeptide of type I collagen (PICP), and bone resorption by the urinary excretion of two pyridinoline cross-linked peptides (NTX and CTX). Bone turnover increased in perimenopausal women with both irregular menses and elevated serum follicle stimulating hormone (FSH). Menopause induced a 37-52% and 79-97% increase in the bone formation and bone resorption marker levels, respectively (p < 0.0001 except for PICP). In postmenopausal women, bone formation markers did not decrease with age. When resorption markers were corrected by whole body bone mineral content (BMC), the fraction of bone resorbed per day was not correlated with age in postmenopausal women and remained elevated for up to 40 years after menopause. In premenopausal women, the bone turnover rate accounted for only 0-10% of the variation in whole body BMC, total hip, distal radius, and lumbar spine BMD. With increasing time after menopause, the importance of the bone turnover rate as a determinant of bone mass increased at all sites and accounted for up to 52% of the BMD variance in elderly women. Thus, in women 20 years or more postmenopause, bone turnover was higher in those in the lowest quartile than in those in the highest quartile of BMD. In elderly women, 20 years since menopause and over, but not in younger ones, serum PTH was negatively correlated with serum 25-hydroxyvitamin D (r = -0.22, p < 0.05) and explained only 5-8% of the bone turnover variance (p < 0.01-0.001). These data indicate that the overall rates of both bone formation and bone resorption remain high in elderly women. The rate of bone turnover appears to play an increasing role as a determinant of bone mass with increasing time since menopause with a high bone turnover rate being associated with a low bone mass. Thus assessing bone marker levels may be useful in the evaluation of osteoporosis risk. In elderly women, secondary hyperparathyroidism caused in part by reduced serum 25-hydroxyvitamin D appears to be a marginal determinant of an increased bone turnover rate.

Increased bone turnover has been suggested as a potential risk factor for osteoporotic fractures. We investigated this hypothesis in a prospective cohort study performed on 7598 healthy women more than 75 years of age. One hundred and twenty-six women (mean years 82.5) who sustained a hip fracture during a mean 22-month follow-up were age-matched with three controls who did not fracture. Baseline samples were collected prior to fracture for the measurement of two markers of bone formation and three urinary markers of bone resorption: type I collagen cross-linked N- (NTX) or C-telopeptide (CTX) and free deoxypyridinoline (free D-Pyr). Elderly women had increased bone formation and resorption compared with healthy premenopausal women. Urinary excretion of CTX and free D-Pyr, but not other markers, was higher in patients with hip fracture than in age-matched controls (p = 0.02 and 0.005, respectively). CTX and free D-Pyr excretion above the upper limit of the premenopausal range was associated with an increased hip fracture risk with an odds ratio (95% confidence interval) of 2.2 (1.3-3.6) and 1.9 (1.1-3.2), respectively, while markers of formation were not. Increased bone resorption predicted hip fracture independently of bone mass, i.e., after adjustment for femoral neck bone mineral density (BMD) and independently of mobility status assessed by the gait speed. Women with both a femoral BMD value of 2.5 SD or more below the mean of young adults and either high CTX or high free D-Pyr levels were at greater risk of hip fracture, with an odds ratio of 4.8 and 4.1, respectively, than those with only low BMD or high bone resorption. Elderly women are characterized by increased bone turnover, and some markers of bone resorption predict the subsequent risk of hip fracture independently of hip BMD. Combining the measurement of BMD and bone resorption may be useful to improve the assessment of the risk of hip fracture in elderly women.

The major part of fluoride ingested is fixed on calcified tissues, mainly in bone tissue, and then is progressively but slowly recycled during bone remodeling. Thus, the measurement of bone fluoride content allows the determination of the extent of bone fluoride retention, and this parameter constitutes a useful complement to bone histology for the diagnosis of skeletal fluorosis and could also be used for the management of fluoride treatment of osteoporosis. A simple method is described to measure the fluoride content in calcined human iliac bone samples. Bone ashes were diluted in perchloric acid, and the measurement of the bone fluoride content was performed using a specific ion electrode combined with a reference electrode. Reference values are given for bone tissue from 76 control subjects (0.08 +/- 0.05% of bone ash), from two groups of 117 and 102 untreated osteoporotic patients (0.05 +/- 0.03% and 0.08 +/- 0.05%, respectively), from 166 sodium fluoride-treated osteoporotic patients (mean bone fluoride content varying from 0.24 to 0.67%, depending on the duration of therapy), and from 96 patients showing typical skeletal fluorosis (mean bone fluoride content varying from 0.56 to 1.33%, depending on the etiology of fluorosis and the relationship with the amount of fluoride ingested as well as with the duration of fluoride exposure). During a prolonged exposure of adult bone tissue to fluoride, the early bone fluoride uptake is variable and depends on the remodeling activity; then it increases rapidly before becoming more or less stable at a maximum level.

Transiliac undecalcified bone biopsy specimens were taken after tetracycline double labeling from 14 patients with radiologic evidence of osteosclerotic metastases from prostatic carcinoma. The histomorphometric analysis showed an increased trabecular bone volume in all patients, and in seven morphologic and dynamic evidence of osteomalacia (Group 1). The seven other patients demonstrated an extension of apposition surfaces without evidence of osteomalacia (Group 2). Group 1 was different from Group 2 in terms of a greater increase in serum alkaline phosphatase and a lower urinary calcium. In four Group 1 patients, a second bone sample taken after two to six months of treatment with vitamin D and calcium provided evidence of improving osteomalacia. The high incidence of osteomalacia in osteosclerotic metastases of prostatic origin appears to be the result of the increase in bone formation induced by prostatic cells, and the unability to satisfy the high calcium demand for new bone.