Bec. Nordin et al., Biochemical variables in pre- and postmenopausal women: Reconciling the calcium and estrogen hypotheses, OSTEOPOR IN, 9(4), 1999, pp. 351-357
There is controversy as to whether the rise in urinary calcium at the menop
ause is the cause or the result of the rise in bone resorption at that time
. In an attempt to resolve this issue, we have compared the relevant bioche
mical variables in 102 premenopausal volunteers (mean age 37 years; range 2
1-52) and 86 apparently normal postmenopausal women (mean age 55 years; ran
ge 40-60). We measured the fasting serum calcium, creatinine, proteins, ele
ctrolytes and intact parathyroid hormone (PTH), and the urinary calcium and
creatinine both after an overnight fast and in a 24-h collection. We calcu
lated serum calcium fractions, creatinine clearance and the notional tubula
r maximum reabsorptive capacity for calcium. Creatinine excretion and clear
ance were lower in the post- than in the premenopausal women after correcti
on for surface area and age. Total serum calcium was higher in the post- th
an in the premenopausal women but this was accounted for by the higher liga
nd concentrations in the former. Fasting and 24-h urinary calcium were also
higher in the post- than in the premenopausal women due in part to the for
mer's higher filtered load of calcium (due to their higher serum complexed
calcium) but mainly to their reduced tubular reabsorption of calcium despit
e their slightly raised serum PTH. Our analysis resolves the rise in urinar
y calcium at the menopause into its two components: increased filtered load
and reduced tubular reabsorption. The changes in these two variables, neit
her of which can be attributed to increased bone resorption, produce an inc
rease in calcium requirement that is sufficient to account for postmenopaus
al bone loss. However, the translation of this menopausal increase in calci
um requirement into an increase in bone resorption at near-normal serum PTH
levels requires some menopause-dependent change in the responsiveness of t
he bone to calcium demand. We suggest that this change may occur at the lev
el of the osteoclasts and that estrogen may modify the calcium feedback set
point in these cells in a manner analogous to calcitonin. This model resolv
es the apparent conflict between the estrogen and calcium hypotheses and ex
plains the synergism between these two treatment modalities.