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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Osteoporosis international 4 (1994), S. S47 
    ISSN: 1433-2965
    Keywords: Biochemical markers ; Bone loss ; Future risk ; Present risk ; Techniques of bone mass measurements
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract The two most important risk factors for long-term skeletal health are the peak bone mass and the subsequent rate of bone loss. The rate of bone loss after skeletal maturity is determined by both genetic factors and environmental factors. Furthermore, all factors that impair estrogen production will increase bone loss. The present risk of developing osteoporosis and fractures may be assessed by bone mass measurements in the total skeleton, or in local parts of the skeleton such as the spine, hip and forearm, by single-photon/X-ray absorptiometry (SPA or SXA), dual-photon/energy X-ray absorptiometry (DPA or DXA), or quantitative computed tomography (QCT). Furthermore, the rate of bone loss in postmenopausal women may be assessed by means of a number of biochemical markers. The fútúre risk of developing osteoporosis may thus be determined by combining the values for bone mineral content and bone loss.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1433-2965
    Keywords: Bone loss ; Dual-energy X-ray absorptiometry ; Lateral ; Postmenopausal
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Diminution of bone mineral density (BMD) in the spine and forearm was studied cross-sectionally in 363 women who were 6 months to 10 years postmenopausal. BMD was determined by dual-energy X-ray absorptiometry (DXA) (Hologic QDR-2000) in the lumbar spine, in both the supine lateral (LAT) and anteroposterior (AP) projections, and in the distal third of the forearm. The postmenopausal diminution of BMD was best described by an exponential fit. The initial rate of postmenopausal diminution of BMD was highest in the most trabecular sites (LAT〉AP〉 forearm), but 10-year diminution was similar at all sites (12%–13%, corresponding to about 1.0–1.5 SD), and extrapolation suggested reverse order of the rates of diminution thereafter (forearm〉AP〉LAT). When bone mineral content of the entire L3 vertebra (tBMC) was measured in vivo, AP tBMC could account for only 67% of the variation in LAT tBMC, compared withr 2=0.997 in vitro. This observation suggests an accuracy problem in vivo in one of the spine measurement methods. We conclude that the initial rate of BMD diminution after the menopause seems to be highest in the spine, especially when measured laterally, but that this rate levels off within the first decade. The lower precision error of a forearm measurement (0.8% v 1.6 for AP and 3.1 for LAT) therefore implies that this method may require a shorter observation period than spine measurements for the detection of bone loss 5–10 years after menopause. Long-term longitudinal spine and forearm measurements are, however, needed to confirm these conclusions.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Osteoporosis international 5 (1995), S. 276-280 
    ISSN: 1433-2965
    Keywords: Bone loss ; Bone markers ; Treatment follow-up
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Hormone replacement therapy (HRT) prevents postmenopausal bone loss, and is therefore increasingly prescribed to prevent the development of postmenopausal osteoporosis. Because of individual differences in the response to HRT as well as problems with compliance, it has been debated how the skeletal response to HRT should be monitored. When estrogen production decreases at the menopause, a number of biochemical markers of bone turnover increase considerably in the order of 50%–100% from baseline. When HRT is instituted, the markers decrease again within the following 3–6 months. In the present prospective study we investigated whether the determination of biochemical markers of bone turnover may be useful for monitoring the skeletal effect of HRT. Seventy-six early postmenopausal women received HRT and 43 received placebo. The treatment period was 24 months and the women were followed with repeated bone mass measurements (every 3 months) which allowed calculation of the bone loss. Serum and urine samples were collected at 3, 6, 12 and 24 months. The placebo group lost a significant amount of bone mineral density in both the forearm and the spine (p〈0.001), whereas the HRT group did not. There was, however, a relatively large overlap of values between the HRT and placebo groups, especially in the spine. After 3 months' treatment the correlation between the changes in the markers and the bone loss wasr=0.59, and this value increased tor=0.66 at 6 months andr=0.76 andr=0.77 at 12 and 24 months, respectively. The present study thus indicates that biochemical markers of bone turnover may be of value for monitoring the bone response to HRT.
    Type of Medium: Electronic Resource
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