Riggs, B. Lawrence

A case of idiopathic osteoporosis in a 12-year-old girl has been reported. Quantitative microradiographic studies of a biopsy specimen of iliac crest showed normal bone formation and an almost threefold increase in the level of bone resorption. The patient was observed without treatment, and a spontaneous clinical remission with roentgenographic improvement occurred. A second iliac crest biopsy specimen, obtained 15 months after the initial biopsy at a time when roentgenographic improvement was apparent, showed a return toward normal of the level of bone resorption. Metabolic balance studies conducted at this time showed that the patient was approximately in calcium balance. Because the majority of the previously reported cases have also exhibited spontaneous improvement, it is suggested that initially observation alone is indicated.

AbstractBackground: Osteocalcin (Oc), a serum marker of bone turnover, circulates in several forms. We developed an assay for intact human Oc and investigated its clinical features.Methods: We generated goat antibodies and N- and C-terminal Oc. The former was used on solid phase (polystyrene beads), and the latter was used as the tracer in an IRMA.Results: The assay was linear with no cross-reactivity to Oc(1–43), total imprecision (CV) of <10%, and recovery of 100% ± 10%. Assay values for intact Oc in EDTA plasma samples were unchanged at 18–25 °C for 6 h. Values for intact Oc in serum, EDTA plasma, and heparin plasma samples did not change after storage on ice for 8 h. Serum samples from patients with various conditions were stored at −70 or −135 °C for up to 5 years and yielded z-scores comparable to an Oc(1-43) IRMA for all conditions except for renal failure. In renal failure, the Oc(1–43) assay values were increased, whereas the intact assay values were in the reference interval.Conclusion: Decreases in Oc assay values are inhibited by calcium chelation, and slowed by reduced temperatures. The described assay for intact Oc allows improved specificity for bone compared with an assay for Oc(1–43).

Abstract We developed a competitive chemiluminoimmunoassay of osteocalcin that is similar to radioimmunoassay but uses acridinium-ester-labeled antigen instead of 125I-labeled osteocalcin; a second antibody immobilized on plastic beads is used to separate free and bound fractions. There was good correlation of the new chemiluminoimmunoassay (y) with a polyclonal antiserum (R102) radioimmunoassay (x) used in many previous clinical studies (r = 0.96, y = 0.968x + 2.69, Sy/x = 0.029, n = 86). The new assay recognized both the intact and the small fragment of osteocalcin in plasma and detected decreases of them (total, approximately 47%) after a 24-h infusion of parathyroid hormone. Patients with primary hyperparathyroidism had increased concentrations of intact osteocalcin. Children had higher concentrations of osteocalcin than adults did. Healthy women had greater osteocalcin concentrations at ages 50-70 years than earlier. Inverse correlations of bone mineral density and osteocalcin were found in healthy women and in women with osteoporosis.

1. To investigate whether there is a nyctohemeral rhythm in bone turnover, we measured serum bone Gla-protein (osteocalcin, an index of osteoblast activity) concentration every 2 h and urinary deoxypyridinoline (a marker of bone collagen resorption) excretion for 8 h periods in 10 pubertal girls (aged 10–14 years), 15 premenopausal women (aged 20–49 years) and 17 postmenopausal women (aged 50–75 years). 2. The serum concentration of bone Gla-protein and the urinary excretion of deoxypyridinoline were five times higher in the pubertal girls than in the premenopausal women. The urinary excretion of deoxypyridinoline in the postmenopausal women was twice that in the premenopausal women. 3. There was a nyctohemeral pattern in all age groups with mean night-time increases of 28% (P<0.001) in the urinary excretion of deoxypyridinoline and of 5% (P<0.001) in the serum bone Gla-protein concentration. 4. There also were nyctohemeral patterns in the urinary excretion of calcium (P<0.02), sodium (P<0.001) and potassium (P<0.001), with decreases at night. There was a negative correlation between the night-time changes in the urinary excretion of deoxypyridinoline and calcium, especially in adult women (P<0.01). 5. The serum level of parathyroid hormone increased with age, but this effect was only observed at night (01.00 to 07.00 hours). There was a nyctohemeral rhythm of the serum intact parathyroid hormone level at all ages, with a peak in the afternoon and night. 6. Thus, at night, there is a large increase in bone resorption and a small increase in osteoblastic activity, representing a nyctohemeral rhythm of bone turnover. Although the amplitudes of bone formation and bone resorption are greater during growth, the pattern of nyctohemeral changes present during growth continues up to the age of 75 years.

1. If gastric acid is necessary for the absorption of dietary calcium, the total absence of gastric acid secretion that occurs in pernicious anaemia could result in bone loss. To investigate this, we measured calcium absorption and bone density in 21 postmenopausal women (ages 51–76 years) with pernicious anaemia and in 24 normal postmenopausal women (ages 51–79 years). 2. Relative to the normal women, in the women with pernicious anaemia the bone mineral density of the lumbar spine was decreased by 16% (P < 0.001). 3. After adjustment for age and body weight, lumbar spine bone mineral density correlated with the serum concentration of group 1 pepsinogens (a group of proteins produced by the gastric fundus) (r= 0.61, P < 0.01). 4. Despite achlorhydria, the women with pernicious anaemia had normal true fractional calcium absorption and normal serum levels of parathyroid hormone and 1,25-dihydroxyvitamin D. 5. We conclude that gastric acid is not required for the absorption of dietary calcium. Thus, the loss of cancellous bone must be caused by some mechanism yet to be identified.

Estrogen (E) deficiency associated with the menopause is the major cause of bone loss in aging women. However, men also lose significant amounts of bone with age, but they do not have the equivalent of menopause, and serum total testosterone (T) and E levels decline only marginally with age in men. Thus, it has been difficult to attribute bone loss in aging men to either T or E deficiency. Here, we show in a population-based, age-stratified sample of 346 men, aged 23–90 yr, that serum total T and E (estradiol plus estrone) levels decreased over the life span by 30% and 12%, respectively, but bioavailable (or nonsex hormone-binding globulin-bound) T and E levels decreased by 64% and 47%, respectively. In these men and in a parallel cohort of 304 women, aged 21–94 yr, serum PTH increased 84% and 64% over the life span, and urinary N-telopeptide of type I collagen (NTx) excretion, a bone resorption marker, increased 77% and 80% between age 50–85 yr in the men and women, respectively. By univariate analyses, serum bioavailable T and E levels correlated positively with bone mineral density (BMD) at the total body, spine, proximal femur, and distal radius and negatively with urinary NTx excretion in men and women. Urinary NTx excretion was also negatively associated with BMD in both sexes. By multivariate analyses, however, serum bioavailable E level was the consistent independent predictor of BMD in both men and postmenopausal women. Thus, bioavailable E levels decline significantly with age and are important predictors of BMD in men as well as women. These studies suggest that in contrast to traditional belief, age-related bone loss may be the result of E deficiency not just in postmenopausal women, but also in men.