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  • Biochemical markers  (3)
  • (Squalus acanthias, Rectal gland)  (1)
  • 1
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    BBA - Enzymology 567 (1979), S. 410-420 
    ISSN: 0005-2744
    Keywords: (Na^+ + K^+)-ATPase ; (Squalus acanthias, Rectal gland) ; Molecular weight ; Solubilization
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-0827
    Keywords: Calcitonin ; Follow-up ; Osteoporosis ; Biochemical markers
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Abstract We reviewed data on 42 postmenopausal women with established osteoporosis (forearm fracture or a low bone mass0 who had been randomly treated for 1 year with either rectal salmon calcitonin (sCT), 100 IU daily (n=25) or nasal sCT, 200 IU daily (n=17) applying an estimation algorithm for bone loss rates. Both groups received a daily calcium supplement of 500 mg. A group of 18 age-matched women who received no treatment served as controls. The bone mineral content of the distal forearm (BMCarm) was measured every 3 months by single photon absorptiometry. The individual rates of change during the 1-year period were calculated by linear regression analysis (αBMCarm). Bone loss rates were estimated initially and after 1 year of therapy by measurements of serum alkaline phosphatase, plasma bone Gla protein, and fasting urinary hydroxyproline and calcium (both corrected for creatinine excretion) according to the estimation algorithm. Both administration forms revealed significant control group-corrected decreases in serum and urine markers of bone turnover of 15–40% (P〈0.05–0.01) and positive outcomes of 2% in αBMCarm (P〈0.01). The estimated effect on bone mass was expressed as the difference between the bone loss estimated after 1 year and initially (ΔESTBIO). A significant correlation was seen between αBMCarm and ΔESTBIO (r=0.5, P〈0.0001). We conclude that the effect of sCT on bone can be followed up by biochemical markers for bone turnover, i.e., by an annual blood and fasting urine sample, applying an estimation algorithm for the rate of bone loss.
    Type of Medium: Electronic Resource
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  • 3
    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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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Osteoporosis international 1 (1990), S. 35-40 
    ISSN: 1433-2965
    Keywords: Osteoporosis ; Prediction ; Biochemical markers
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract The present study includes 70 healthy, immediately postmenopausal women stratified according to future rate of bone loss. The stratification was performed by means of four parameters of bone turnover: serum alkaline phosphatase, fasting urinary calcium and hydroxyproline, and body weight, used in an equation developed in a previous study. After the stratification the women were followed without intervention for the next 24 months, with bone mass measurements every 3 months. The bone loss estimated at baseline by means of the equation correlated with the bone loss measured in the forearm (y=0.72x−1.52;r=0.61;P〈0.001). Plasma bone gla protein (BGP, osteocalcin), which is a new specific marker of bone formation, was now added to the model (replacing body weight). This increased the diagnostic validity (y=x;r=0.76;P〈0.001). From the present study we conclude that the postmenopausal bone loss can be predicted by means of four biochemical parameters determined in plasma and urine in women just after the menopause.
    Type of Medium: Electronic Resource
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