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Terence J Wilkin Plymouth Postgraduate Medical School, University of
Plymouth, Plymouth PL4 8AA
twilkin{at}plymouth.ac.uk
A recent meta-analysis of 11 separate study populations and
over 2000 fractures concluded that bone mineral density "cannot identify individuals who will have a fracture."1 So why
do we measure it? The question is worth asking when the number of dual
energy x ray absorptiometry machines installed in the
United Kingdom exceeds 130 (National Osteoporosis Society, personal
communication), and the number of Medline citations incorporating the
term dual energy x ray absorptiometry has grown from 26 in 1988 to 464 in 1997. The concept of "fracture threshold" has led
to the recommendation that preventive treatment be given to women once
their bone density lies (arbitrarily) more than 1 SD below the mean for
premenopausal women
Bone comprises a matrix framework on which mineral is deposited.
Osteoporosis is caused by the disintegration of the matrix, and
osteomalacia by a failure to mineralise it. When mineralised matrix
disintegrates, calcium is inevitably lost. The negative calcium balance
observed with matrix loss gave rise to erroneous beliefs that the
calcium requirements of postmenopausal women were higher than those of
premenopausal women and that osteoporosis could be prevented by calcium
supplementation.2 Calcium is crucial during the
development of bone, but it cannot replace disintegrating matrix or
prevent its loss.3 As Heaney has pointed out, calcium is a
nutrient and not a drug, and the only disorder it can be expected to
alleviate is calcium deficiency.4 What is more, excess
calcium supplementation will suppress the secretion of parathyroid
hormone and slow the natural turnover of bone. "Fossilised" bone is
at risk from microfractures. Calcium intakes of between 1 g and 1.5 g
daily, commonly recommended in postmenopausal women, are associated
with an increased rather than decreased risk of fracture.5
Preventing osteoporosis does not depend on calcium, but rather on
preserving bone matrix, a living tissue whose structure, strength, and
integrity depend, in turn, on fine control of its turnover.
Bone turnover is maintained by two groups of cells The widespread view that treatment with antiresorptive drugs
restores lost bone, and that the increase in bone density observed is
responsible for the subsequent reduction in the fracture rate, needs
careful rethinking.6 There is no evidence that treatment for osteoporosis restores bone, although (unlike calcium supplements) antiresorptive drugs undoubtedly prevent its further loss. The small
increases in bone mineral density gained during the early years of
treatment with hormone replacement therapy or bisphosphonate drugs soon
level off,7 and probably reflect no more than the filling
by osteoblasts of the myriad pits dug before treatment by uncontrolled
osteoclasts.
7 8
The challenge to the view that there is a
causal relation between bone mineral density and risk of fracture lies
in the results of large, placebo controlled, double blind, multicentre
trials of bisphosphonate drugs (even those conducted in ageing women
with established osteoporosis). These show a reduction in the risk
of fracture at the hip and spine of more than 50%, but an increase in
bone mineral density at these sites of only 5-8%,9 and
even less in earlier studies of spinal fracture.7 It is
difficult to attribute such a spectacular clinical result to such a
small increase in bone mass.
Hui et al constructed a family of curves relating fracture risk to
bone density in different age groups. For the same bone density, the
risk of fracture rose eightfold to 10-fold from age <45 years to Apart from further undermining the validity of bone density as a
surrogate for individual fracture risk and its clinical use in
identifying those to whom treatment should be given, the observation calls for an explanation. One obvious mechanism is that ageing people
fall more frequently and, for a given bone density, sustain fracture
more often as a result. Fractures seldom occur without some impact,
however fragile the bone, but there may be an additional and more
subtle explanation to account for the differences in risk, one which
can reconcile the data from clinical trials on fracture risk, bone
density, and bone resorption.
It is intuitively likely that bone depends for strength more on its
architecture than on its mass. Bone in a younger person is structurally
normal, whereas in ageing people its architecture is compromised in two
ways. Firstly, the progressive erosion of trabeculas will leave them
weakened and, in some cases, disconnected.7 Microscopy
shows that trabecular erosions and disconnectivity cannot be reversed
by treatment.12 Secondly, and possibly more importantly,
the rate of bone turnover in women who are deficient in oestrogen
will inevitably be higher, mass for mass, than in women who are
oestrogen replete. If a bolt or two at a time were removed from a
cantilever bridge for replacement, architectural strength might not be
affected While measurements of bone density emphasise how little bone is
regained during antiresorptive treatment, measures of matrix loss show
a dramatic and immediate slowing of bone turnover. In postmenopausal
women, N-telopeptide type I collagen (a marker for osteoclast activity)
fell from 3 SD above the mean to the premenopausal mean within one
month of starting treatment, an effect which remained throughout the 15 month study.13 The bone specific alkaline phosphatase
value (a marker for osteoblastic activity) showed a similar pattern
within six months (the delay probably contributed to the 5% increase
in spinal bone mass observed over the study period). The fossa
intervention trial (FOSIT) observed over 1000 postmenopausal women with
low bone density in a placebo controlled trial of alendronate that
lasted more than 12 months. It showed an 80% reduction in the bone
resorption rate in relation to increases in bone density of 5% at the
lumbar spine and just 2% at the neck of the femur.14
Critics have pointed out that markers of bone turnover are "poorly
predictive of bone mineral density ... and cannot be
used to diagnose osteoporosis or to select patients for subsequent densitometry," but this is to miss the point.15 If the
modest gain in bone density seen with treatment is insufficient to
account for the substantial reduction in fracture risk, a state of high bone turnover, rather than its prevailing mass, may be the responsive element in fracture prevention, no matter at what age it is
encountered. The clinical implications are important, as there is no
evidence that bone density identifies those people who will sustain a
fracture, but abundant evidence that restoring bone turnover to normal
values universally reduces the risk. A switch in emphasis from bone
density, which declines irreversibly, to bone turnover, which rises,
but is fully reversible, makes reducing the risk of fracture a viable consideration at any age after the menopause.
A fall in bone mass, erosion of trabeculas, and ultimately their loss
of connectivity must, in themselves, render bone progressively more
fragile. However, the evidence cited suggests that fracture risk can be
reduced appreciably, even in older women who are already osteoporotic,
and without a noticeable restoration of bone mass. The widely held
notion that it is too late to treat women with established osteoporosis
because bone cannot be restored once it is lost is flawed because bone
density and fracture risk are poorly correlated and a high turnover of
bone can be normalised at any age or bone density. Bone
densitometry might arguably have only a limited role in strategies
to prevent osteoporotic fracture.
If high bone turnover rather than low bone density is the major
component of fracture risk, antiresorptive drugs should reduce the risk
of fracture to the same extent at any age after the menopause, independently of bone density, and when they are stopped their protective effect should be lost before bone density decreases. A
recent report by Michaelsson et al provides the first evidence that
bears out both these predictions.16 In a large, population based, case-control study, hormone replacement therapy reduced the risk
of hip fracture to the same extent, whether treatment began at the
menopause or decades later. After hormone replacement therapy was
stopped, protection against fracture fell rapidly in relation to the
interval since it was last used, and became statistically insignificant
after five years.
In 1995, it was claimed that "it is now possible to accurately
determine individuals' risk of osteoporosis, and to monitor their
response to treatment, by means of bone densitometry."7 In the light of current understanding, this is probably not the case.
People who will sustain a fracture cannot be identified by bone
densitometry, and if bone turnover is the key responsive element in
treatment, measures of bone resorption rather than of its density
should be the focus of technical developments in monitoring response to treatment.
How much, then, can we be certain of in formulating
programmes for the prevention of osteoporotic fracture? We know that
antiresorptive drugs taken at the time of the menopause will maintain
bone density for as long as they are continued. However, we also know
that without them few women sustain fractures before the age of 65 years, probably because they tend not to fall. So has anything been
gained in prescribing treatment during 15 years of low fracture risk?
Certainly, the NHS can afford neither to screen the perimenopausal population nor to treat blindly. We also know that antiresorptive drugs
reduce the risk of fracture equally at any age after the menopause, and
that this protection is lost rapidly when they are stopped. Finally,
bone density benefits little from antiresorptive agents, while bone
turnover returns to its premenopausal state.
If bone density determination cannot distinguish between those
who will and will not sustain osteoporotic fractures, it has no place
in selecting people for prophylaxis
I thank Debbie Hobbs for preparing this manuscript.
Competing interests: None declared.
(Accepted 24 November 1998)
Richard Eastell Section of Medicine, University
of Sheffield Division of Clinical Sciences, Northern General Hospital,
Sheffield S5 7AU
r.eastell{at}sheffield.ac.uk.
Wilkin identifies two areas of weakness in the use of
bone mineral density measurements. Firstly, he argues that the risk of
fracture cannot be predicted from someone's bone mineral density as
the relation between the two described in cohort studies is too
weak.1 Secondly, he argues that bone mineral density
cannot be used as a surrogate for fracture risk in clinical trials as the relation between a change in density and a change in fracture risk
is not as predicted from these cohort studies.1
I believe that it is reasonable to use an individual's bone
mineral density to assess the risk of osteoporotic fracture and to make
decisions about treatment with antiresorptive drugs. The relation
between bone mineral density and fracture is analogous to that between
blood pressure and stroke, and it is just as strong. The problem with
bone mineral density has arisen when it has been used to diagnose
osteoporosis. This approach raises a risk factor for fracture to the
status of a diagnostic criterion, and ignores the importance of other
determinants of bone strength and of factors that increase the risk of
falls.2 Low bone mineral density is one of the strongest
risk factors for osteoporotic fracture. Nonetheless, it is preferable
to use this together with other predictive factors that are common and
easy to ascertain, such as low body weight (<58 kg), current smoking,
a first degree relative with low trauma fracture, and personal history
of low trauma fracture.3
An increase in bone mineral density of 5-10% is commonly reported for
antiresorptive treatments for osteoporosis, such as hormone replacement
therapy and bisphosphonate drugs. The relation between bone mineral
density and fracture risk provides a prediction that the reduction in
fracture should be about 25% The importance of a high rate of bone turnover as a risk factor
for fracture has been considered by others. Riggs et al, using data
from their clinical trial with hormone replacement therapy, concluded
that an increase in bone density and a decrease in bone turnover at the
spine had approximately equal effects in reducing the risk of spinal
fracture.4 Parfitt proposed that antiresorptive treatment
reduces the rates of bone remodelling, and since these remodelling
sites act as stress risers and promote microfractures, their reduction
lowers the risk of fracture.5 Wilkin is therefore correct
to say that the change in bone turnover resulting from antiresorptive
treatment may reduce the risk of fracture. The practical consequence of
this is that it is reasonable to use markers of bone turnover to
monitor treatment. However, in using these markers in clinical
practice, care needs to be taken to minimise their
variability.6
This marker hypothesis cannot be the entire explanation for the
unexpected relation between a change in bone mineral density and a
reduced risk of fracture. Treatment with alendronate results in the
hypermineralisation of bone tissue. This may change the biomechanical
properties of bone7 and explain the increase in bone
mineral density seen in the third year of alendronate treatment.8 Parathyroid hormone treatment increases bone
density and turnover, yet it reduces the risk of spine
fracture.9 We still have much to learn about the mechanism
by which treatments for osteoporosis reduce the risk of fracture.
a state of osteopenia, according to the WHO
definition. But should we be managing osteoporosis by numbers?
Summary points
Bone densitometry cannot identify people who will sustain
osteoporotic fracture
Bone density changes little with antiresorptive treatment (hormone
replacement therapy and bisphosphonate drugs), whereas bone turnover
falls dramatically
Bone turnover may be the responsive element in treatments to prevent
osteoporotic fracture
Antiresorptive treatments prevent fracture, regardless of whether they
are given at the menopause or decades later
Since frequency of impact, which rises exponentially with age, is the
main risk factor for fracture, treatment should be focused on infirm
older people, irrespective of their bone density
![]()
Osteoporosis and osteomalacia
osteoclasts, which
dig pits in mineralised matrix, and osteoblasts, which refill the pits.
Osteoclastic activity is constrained by the action of sex steroids, and
coordination with the osteoblasts is normally maintained such that
there is no net change in bone mass during early adult life. After the
menopause, circulating oestrogen concentrations fall rapidly and
osteoclastic activity accelerates, outstripping the attempts of
osteoblasts to keep pace. The net result is bone loss which, over a
period of years, may amount to 20% or more of the skeleton.
![]()
Effect of antiresorptive drugs
![]()
Factors in fracture risk
80
years.10 In a sample of 5800 Dutch men and women over 55 years of age, the risk of hip fracture rose 13-fold with age, to which
the decrease in bone density contributed only 1.9 in women and 1.6 in
men.11 These are important observations, because they
suggest that something very important in the ageing process influences
fracture risk independently of bone density.
Healthy, dense bone
but if a thousand were removed at one time (a high
turnover state), architectural strength could be compromised
critically, with little loss in mass. Fractures occur in situations in
which high bone turnover is combined with frequent impact. Bone density
does not contribute greatly to the individual's risk.
![]()
Programmes for preventing osteoporotic fracture
notwithstanding recent Department of Health guidelines.17 Current knowledge
indicates that prophylaxis should be targeted not at maintaining bone
density throughout menopausal life but at restoring normal bone
turnover in those who, for whatever reason, become infirm and at
greatest risk of impact. Such an approach to the prevention of
osteoporotic fracture would be evidence based, could be budgeted
for, and would rationalise management of the individual
patient
something that treatment by numbers does not.
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Acknowledgments
![]()
Footnotes
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References
results of 1000 patients from the FOSIT study.
Acta Obstet Gynecol Scand
1997;
76 (suppl 167):
61[Medline].
Commentary: Bone density can be used to assess
fracture risk
yet it is closer to 50%.2
Wilkin proposes that since the change in bone mineral density only
partly explains the change in fracture risk, these antiresorptive drugs
protect against fracture by reducing the turnover rate of
bone.
Osteoporotic bone
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References
© BMJ 1999
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