J. Reeve et al., EVOLUTION OF SPINAL BONE LOSS AND BIOCHEMICAL MARKERS OF BONE REMODELING AFTER MENOPAUSE IN NORMAL WOMEN, Calcified tissue international, 57(2), 1995, pp. 105-110
The main objective of this study was to describe longitudinal patterns
of spinal bone loss in normal women who undergo a natural menopause.
The second objective was to determine if a proportion of women suffer
excessively rapid postmenopausal bone loss from the spine. If this was
the case it was the aim to devise a means of predicting the woman at
excess risk; but if all women lost bone at similar rates, the aim was
to document changing loss rates over the first 5-8 postmenopausal year
s. Responding women in six suburban general practices recalled for cer
vical smears who had their last menstrual period 9-36 months previousl
y were invited to participate in a longitudinal study of bone loss and
the biochemical markers plasma osteocalcin and urinary hydroxyproline
. Sixty-four subjects agreed to participate, a response rate of 80%. I
n the ensuing 5 years, six received hormone replacement therapy and ar
e not reported on. The main outcome measures were rates of spinal bone
loss over 5 years, measured by dual photon absorptiometry, and radial
bone loss over the first 2 years measured to quantitative computed to
mography. Spinal bone loss was similar between individuals, with 94% o
f the variability in the data being accounted for by a statistical mod
el that assumed parallel rates of bone loss. A less restrictive model
allowing women to have different rates of spinal bone loss accounted f
or 12% more of the remaining variance in the data than the previous mo
del. However, rates of radial bone loss were more dissimilar between w
omen than rates of spinal loss. The results of the biochemical data co
llected serially showed that the plasma osteocalcin rose slowly to a p
lateau at 5 years postmenopause; in contrast, the hydroxyproline fell
progressively with time over the whole period of study. These results
were interpreted as being consistent with diminishing rates of bone de
struction which gradually reequilibrated with bone formation as time p
assed after menopause.