Citations

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.

Abstract ABSTRACT: The cellular mechanisms for bone loss in type I (postmenopausal) osteoporosis are highly controversial. We attempted to resolve this by assessing rates of formation and resorption of iliac cancellous bone by a new histomorphometric method in 89 women with osteoporosis (mean age + SD, 66 + 6 years) and in 32 carefully selected normal postmenopausal women (64 + 6 years). In the osteoporotic women, bone resorption rate was increased by 39% (P <0.05) at the cellular level and by 67% (P <0.05) at the tissue level, whereas bone formation was unchanged at the tissue level but decreased by 14% (P <0.01) at the cellular (osteoblast) level. This pronounced remodeling imbalance (P <0.001) was probably exacerbated by a 45% increase (P < 0.1) in activation frequency of new remodeling foci. These abnormalities were associated with a high rate of cancellous bone loss (median, 5.8%/year versus 0.1%/year in controls). Thus, accelerated loss of cancellous bone in type I osteoporosis results from the combination of increased bone resorption and inadequate compensation by bone formation.

Abstract To determine whether Colles' fracture, generally considered a manifestation of postmenopausal osteoporosis, is associated with a decrease in bone density at the site of fracture, we measured bone mineral density of the ultradistal radius (UDR-BMD) by single-photon absorptiometry with computer-assisted image processing. In 119 normal women (ages 22–92 years), UDR-BMD decreased by 17% between ages 30 and 75 years. From UDR-BMD measurements in these normal women and in 40 women (ages 53–80 years) with Colles' fracture alone, a population-based analysis was made to estimate fracture risk at different values of UDR-BMD. Colles' fracture was uncommon at UDR-BMD > 0.40 g/cm2 (the “fracture threshold”). As bone density decreased below this level, fractures became more frequent (a “gradient of risk”).

Abstract True calcium absorption can only be measured by the time-consuming and expensive metabolic balance method and is not predicted well by measuring the fractional absorption (FA) of radiocalcium from a fixed calcium carrier. We describe here a 1 day method for measuring the actual fraction of calcium absorbed from the habitual diet (true fractional calcium absorption, TFCA) using stable isotopes of calcium. Oral and intravenous isotopes were administered with each of the three daily meals, and then the ratio of the two isotopes in the urine was measured by mass spectroscopy. In 12 subjects, TFCA determined from stable Ca correlated well with TFCA measured by the balance method (r = 0.71, P < 0.01), and the mean values were not different (0.26 and 0.26). In contrast, no significant correlation was found between FA and TFCA. The weak relationship between FA and TFCA underscores the importance of tracing dietary calcium rather than a fixed calcium carrier in tests of calcium absorption. Using the new method, TFCA was inversely related to dietary calcium (r = −0.45, P < 0.05), demonstrating that it could detect physiological changes in calcium absorption. Thus, this test has two important advantages: (1) it provides a simple way to measure TFCA and true fractional calcium absorption (the product of TFCA and dietary calcium), the physiologically relevant variables, and (2) because there is no radiation exposure, the test can be used in pregnant women and children, the isotopes can be prepared in advance, and several isotopes can be used simultaneously.

Abstract The concept that vertebral fractures are caused by excessive loss of cancellous bone has been challenged by a recent study (J Bone Min Res 2:221, 1987) suggesting that vertebral bodies are composed mainly of cortical bone rather than cancellous bone. To resolve disagreement we used two independent methods to quantify the proportions of cortical and cancellous bone in 400 μm thick sections of the bodies of the second lumbar vertebrae from six men (aged 21–58 years) and seven women (aged 25–58 years). Based on the ash weight of the manually dissected components, 80% of the total bone in men and 72% in women was cancellous bone. Based on computer-assisted scanning of sections with a microdensitometer, 81% of the total bone in men and 71% in women was cancellous bone. We conclude that the traditional concept is correct: the vertebral body is composed mainly of cancellous bone.

Abstract Although it is a cardinal feature of involutional osteoporosis, there is often disagreement on what constitutes a vertebral fracture. We measured vertebrae T4-L5 in 52 healthy women to develop a normal range (mean ± 3 SD) for vertebral shape and used these data to assess the prevalence of vertebral fractures. We classified vertebral fractures by type of deformity (wedge, biconcavity, or compression) and further by the degree of deformity (grades 1 and 2). In 195 postmenopausal women who were an age-stratified random sample of the Rochester population (ages 47–94), 40 (21%) had vertebral fractures (mean, 2 per person). There was a similar number of compression and wedge fractures, and grade 2 fractures were as common as grade 1. In a referral sample of 74 women with suspected osteoporosis, 62 (84%) had vertebral fractures (mean, 3.3 per person). Wedge fractures were most common, and grade 2 fractures were more common than grade 1. The distribution of type and grade of fractures differed between the two patient groups (P < 0.01). Bone mineral density of the lumbar spine was related to mean fracture grade (r = −0.33, P < 0.05) and to fracture number (r = −0.57, P < 0.001) but not to fracture type. We conclude that a comprehensive approach is required in describing vertebral fractures. Using this approach we found distortion in the fracture characteristics of women referred to an osteoporosis clinic compared to women in the community.

Abstract We studied the mechanism of impaired calcium absorption with aging in 51 healthy women whose ages ranged from 26 to 88 years. Serum concentrations of 1,25-dihydroxyvitamin D [1,25-(OH)2D, mean of four measurements per subject] increased with age by 22% (P < 0.05) but, by split-point analysis, plateaued or decreased slightly after age 65. In a subset of 20 subjects, [3H]1,25-(OH)2D3 kinetic analysis showed that this increase with age resulted from both increased production and decreased metabolic clearance of 1,25-(OH)2D. Despite the increase in serum 1,25-(OH)2D concentration, true calcium absorption did not change with age. The expected inverse correlation between true fractional calcium absorption and dietary calcium intake, however, was easily demonstrated (r = 0.66, P < 0.001). Serum intact parathyroid hormone (PTH) increased with age by 35% (P < 0.02) and serum bone gla protein (BGP, osteocalcin) increased by 47% (P < 0.001); the increases in serum PTH and serum BGP were directly correlated (r = 0.32, P < 0.05). The data are consistent with the following hypothetical model: (1) intestinal resistance to 1,25-(OH)2D action accounts for the increase in serum 1,25-(OH)2D concentrations with aging with no change in true calcium absorption; (2) this results in a compensatory increase in PTH secretion and in 1,25-(OH)2D production that prevents true calcium absorption from decreasing; (3) the previously described defect in 25-hydroxyvitamin D (25-OHD) 1α-hydroxylase activity in aging animals and humans acccounts for the leveling off in serum 1,25-(OH)2D concentration after age 65 years; and (4) the secondary hyperparathyroidism leads to increased bone turnover and thus contributes to age-related bone loss.