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Original Studies |
Department of Physiology (E.S., P.K., O.M.R.), Imperial College School of Medicine, St. Marys Campus, London W2 1PG, United Kingdom; and Department of Histochemistry (M.V.J.H., J.M.P.), Imperial College School of Medicine, Hammersmith Campus, London W12 0NN, United Kingdom
Address all correspondence and requests for reprints to: Dr. Olga M. Rutherford, Department of Physiology, Imperial College School of Medicine, Norfolk Place, London W2 1PG, United Kingdom.
| Abstract |
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Eleven amenorrheic athletes, 15 eumenorrheic athletes, and 10 sedentary controls were studied. Spine and hip bone mineral density was measured using dual-energy x-ray absorptiometry. Bone turnover was assessed by biochemical markers of formation (osteocalcin and bone-specific alkaline phosphatase) and resorption (deoxypyridinoline). NO metabolites were measured from 24-h urine samples using a chemiluminescence assay.
Spine, but not hip, bone mineral density was reduced in the amenorrheic group, compared with the eumenorrheic (P = 0.0001) and control (P = 0.04) groups. Osteocalcin, bone-specific alkaline phosphatase, and deoxypyridinoline were similar in all groups. NO metabolites were lower in the amenorrheic group, compared with controls (P = 0.035), despite a higher dietary intake of nitrates.
Unlike postmenopausal women, amenorrheic athletes do not have raised bone turnover but do have reduced NO metabolites and spinal osteopenia. The results show, however, that reduced NO production is a common denominator in both conditions and further support the importance of NO in estrogen-mediated protection of skeletal mass and strength.
| Introduction |
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Biochemical markers of bone turnover are being used increasingly as indicators of bone remodeling status. These markers have been extensively studied in bone disease states, in osteoporosis, and in some longitudinal studies of exercise intervention. In the first decade after the onset of the menopause, there is an increase in levels of osteocalcin, bone-specific alkaline phosphatase (bALP), and pyridinium cross-links, reflecting the increase in bone turnover (8). These levels can be reduced after treatment with hormone replacement therapy (HRT) (9).
Some studies have found higher levels of bone turnover in subjects who are more recreationally active (10, 11, 12). Few studies have specifically looked at bone turnover in amenorrheic athletes. Hetland et al. (13) assessed bone formation by osteocalcin and alkaline phosphatase, and bone resorption by urinary calcium and hydroxyproline, in female runners. They found no difference in bone turnover between amenorrheic and eumenorrheic runners, despite a lower spine bone mineral density (BMD) in the amenorrheic group. In their study, however, no comparisons with sedentary controls were made.
Recently, it has been suggested that the physiological effects of estrogen and mechanical stress on both cardiovascular function and bone turnover are exerted, at least in part, via elevation of nitric oxide (NO) synthesis. In young fertile women with normal menstrual cycles, the plasma nitrite and nitrate, the stable oxidation end products of NO, are at their highest at the midcycle, following closely those of estrogen levels (14). Postmenopausal women have reduced serum NO metabolite levels, and both short- and long-term HRTs elevate these levels in postmenopausal women (15, 16). There is clear evidence that estrogen can induce endothelial NO-synthase (eNOS) messenger RNA, protein, and enzymatic activity in a variety of cells, including those of bone (17, 18).
Recent evidence has established that NO generated from the eNOS isoform is one of the key mediators of mechanical stress-induced increase in bone formation (19, 20), providing for potential involvement in bone resorption associated with osteoporotic disease (21, 22). It is thought that low-level NO production by the eNOS isoform is an absolute requirement for bone cell function (21, 22, 23, 24). Support for the importance of NO on skeletal homeostasis derives from the study by Wimalawansa et al. (25) in rats, who showed that administration of nitroglycerin, an NO donor, in estrogen depletion-induced osteoporosis will suppress osteoporotic bone loss and, conversely, that inhibition of endogenous NO production will suppress the bone-conserving action of estradiol (25).
These observations would offer an attractive explanation of why estrogen restores bone mass, given that NO is involved in the cascade of hormone receptor signaling mechanisms in bone cells. In the present study, we investigated bone turnover and BMD in amenorrheic and eumenorrheic athletes and sedentary controls and hypothesized that amenorrheic athletes with reduced BMD also have decreased NO metabolite levels, compared with the eumenorrheic and sedentary control groups.
| Materials and Methods |
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A total of 36 subjects were recruited, of which 11 were
amenorrheic athletes, 15 were eumenorrheic athletes, and 10 were
sedentary controls. Details of the 3 groups are given in Table 1
. The athletes were either club runners
or triathletes, and amenorrhea was defined as no menstruation in the
previous 6 months. The eumenorrheic athletes and sedentary controls all
had regular menstrual cycles (1013 cycles per year) between 25 and 35
days in length, and none of the subjects had any condition known to
affect bone metabolism. All subjects were healthy at the time of study.
Subjects gave written, informed consent, and the study was approved by
the local ethical committee.
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All subjects completed a detailed questionnaire on past medical and menstrual history, smoking and alcohol consumption, calcium intake, and physical activity levels. The calcium intake section has previously been validated against weighed intake (26). Dietary intake of nitrate was estimated from a food-frequency questionnaire (27). The questionnaire included dietary components rich in nitrates, as well as those eaten in quantity. Full details of training and competition schedules were obtained.
Anthropometry
Height and weight were measured with subjects in minimal clothing and bare feet. Skin-fold thicknesses were measured at 4 sites (suprailiac, subscapular, biceps, and triceps), and the percentage fat was calculated from the equation of Durnin and Womersley (28).
Bone density
BMD of the spine and hip was measured using dual-energy x-ray absorptiometry (Lunar DPX-L). The spine scan was analyzed to give BMD for lumbar 14 levels; and the hip scan was analyzed for greater trochanter, neck of femur, and Wards triangle. The coefficient of variation of repeat spine scans is less than 1%; and for all sites on the hip, it is less than 1.5% (29).
Bone turnover
Deoxypyridinoline (Dpd) was measured from 24-h urine samples from which a 50-ml aliquot was taken and frozen at -20 C until analyzed. Osteocalcin and bALP were measured from a blood sample taken the day of completion of the urine collection. Blood samples were collected in the afternoon, and assays were carried out in triplicate and in two batches. Samples were collected in either a heparanized tube with 100 µl Tresylol (for osteocalcin) or a plain tube (bALP). The tubes were immediately centrifuged at 1,500 rpm for 10 min, and aliquots of serum or plasma were frozen at -20 C until analyzed. All menstruating subjects had the samples collected within the first 4 days of the cycle, i.e. early follicular phase. Subjects were asked to refrain from training during the collection phase.
All bone marker assays were carried out using immunoassay kits from Metra Biosystems Inc. (CA). These were Pyrilinks-D, NovoCalcin, and Alalphase-B for Dpd, osteocalcin, and alkaline phosphatase respectively. The assays used a microtitre stripwell format using monoclonal antibodies and a b-nitrophenyl phosphate substrate. Dpd values were standardized for urinary creatinine.
Nitric oxide (NO)
NO was measured in 24-h urine samples by the chemiluminescence assay. Triplicate 50-µL samples were injected into a purge vessel, and urinary nitrate and nitrite were converted to NO in a reducing mixture of 0.1 mol/L vanadium(III) chloride in 1.0 mol/L HCl at 96.5 C. NO was detected by its chemiluminescence reaction with ozone, generated from pure oxygen using a Sievers NOA 270B NO analyzer (Sievers Instruments, Boulder, CO). Comparisons were made against standard curves generated by known concentrations of sodium nitrate.
Statistics
Data is expressed as mean ± SE, unless otherwise stated. Between-group comparisons were carried out using ANOVA with post hoc analysis by Students t test. Relationships between parameters were investigated using Spearmans rank correlation.
| Results |
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The amenorrheic athletes were significantly lighter than the other
two groups (P = 0.0025) and had the lowest body fat
percentage (P = 0.001; Table 1
). There was no
difference in the age of menarche or calcium intake among the groups.
The average length of amenorrhea was 42.2 months (range, 6120).
Bone density
Table 2
shows the group mean data
for BMD at each site. BMD of the spine, neck of femur, and greater
trochanter has also been expressed as a percentage of age- and
weight-matched controls taken from the large Lunar reference database.
Spine BMD was significantly lower in the amenorrheic athletes, compared
with both eumenorrheic athletes (P = 0.0001) and
sedentary controls (P = 0.04) and were also
significantly lower than predicted from the database (P
= 0.01; Fig. 1
). There was no
relationship between the length of amenorrhea and BMD of the spine.
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Bone turnover
There was no significant difference between levels of osteocalcin,
bALP, or Dpd among the three groups. Individual values are shown in
Fig. 2
. Most of the values in each group
fell within the normal ranges for premenopausal women, as supplied by
the manufacturers of the assay kits. One amenorrheic subject had an
extremely high bALP, but this was not associated with a high
osteocalcin or Dpd, although this subject did have one of the lowest
body fat levels (8.5%) and spine BMD (75% of age-matched).
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Nitric oxide metabolites and nitrate intake
Group mean NO levels and nitrate intakes are shown in Table 3
. The amenorrheic athletes had the
lowest urinary NO, and the sedentary controls had the highest, the
difference between these two groups being significant
(P = 0.035; Fig. 3
).
Because urinary levels of NO could be affected by dietary nitrate
intake, we assessed intake, to investigate any group differences.
Nitrate intake was highest in the amenorrheic athletes and lowest in
the sedentary controls, the difference again being significant
(P = 0.0329; Fig. 3
). There was a significant negative
correlation between nitrate intake and urinary NO levels
(r2 = -0.62; P = 0.042).
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| Discussion |
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Load-bearing exercise is known to be beneficial for bone density (32), and this is illustrated by the eumenorrheic athletes, who had the highest bone densities at all sites measured. When compared with the Lunar database, this group had significantly higher BMD at the greater trochanter and neck of femur. Despite their equally high level of activity, these sites were not increased in the amenorrheic group but were similar to the controls. That BMD was not low at the hip in the amenorrheic group suggests that the pattern of loading imparted by the athletic activities may be having a protective effect on the hip but not the spine. Some forms of exercise are able to give a protective effect to the spine in amenorrheic athletes; for example, amenorrheic rowers have higher spine bone densities than amenorrheic runners (33). The skeletal effects of athletic amenorrhea therefore depend, to a certain extent, on the types of activity performed.
Despite the spinal osteopenia in the amenorrheic group, there was no
difference in markers of bone formation or resorption between the
groups. We originally hypothesized that the amenorrheic athletes might
have an increased bone turnover, particularly resorption, similar to
that seen in postmenopausal women. Inspection of Fig. 2
clearly shows
that resorption, as indicated by Dpd excretion, is not increased in the
amenorrheic athletes, compared with the other two groups. There was no
relationship between the length of amenorrhea and any of the markers,
although the numbers may have been too small to detect such a
relationship. Therefore, despite apparently normal bone formation and
resorption, bone loss from the spine is occurring in amenorrheic
athletes. This agrees with the findings of Hetland et al.
(13), who also found normal formation and resorption in amenorrheic
athletes. Because the amenorrhea seems to particularly affect the
spine, the bone turnover status of the rest of the skeleton may mask
any localized imbalance. Systemic markers of bone turnover should
reflect total body BMD, which we have previously shown to be normal in
the amenorrheic athletes (2).
The common factor between postmenopausal women and amenorrheic athletes is a lowering of estrogen levels. The mechanism of this reduction is, however, different. In amenorrheic athletes, the low estrogen levels are secondary to a reduction in pituitary LH production, because of an inhibition of GnRH release from the hypothalamus (34). In postmenopausal women, the decline in estrogen is caused by a depletion of ovarian follicles, and the lack of negative feedback of estrogen on the hypothalamic-pituitary axis results in raised LH production. The mechanism behind a lowering of GnRH in amenorrheic athletes is still unknown. There is some evidence for a raised cortisol production in this group (34, 35), and this may play a role in inhibiting hypothalamic GnRH release. Raised glucocorticoid levels are also associated with bone loss. The mechanism differs from that seen in postmenopausal women, with a depression of bone formation and an unaltered bone resorption (36, 37). Other endocrine changes have also been implicated in athletic amenorrhea, such as a raised endorphin release and altered thyroid status (38, 39). These additional hormonal changes may also be influencing bone turnover in a manner different from that of low estrogen.
This finding of no increase in bone turnover is important when considering treatment options for amenorrheic athletes with a low bone density. HRT is sometimes used when natural menses cannot be regained (40). HRT acts mainly by inhibiting bone resorption (41). Although successful in retarding bone loss in postmenopausal women, where resorption is increased, its effects in the amenorrheic athlete may be limited. If resorption is normal, and depressed by HRT, this may have the overall effect of depressing bone turnover and reducing the ability of the bone to repair microfractures. The incidence of stress fractures is much greater in amenorrheic (compared with eumenorrheic) athletes (42), and these often take a long time to heal. If bone remodeling is suppressed, then it is possible that this problem could be further exacerbated.
Despite the lack of similarity between bone turnover in amenorrheic athletes and postmenopausal women, concentrations of NO metabolites were affected as predicted, with the lowest being in the amenorrheic group. A confounding factor when measuring NO metabolites is the dietary intake of nitrates. These were assessed by questionnaire and found to be the reverse of the NO metabolite levels, i.e. amenorrheic athletes had the highest dietary intake of nitrates. It is therefore extremely unlikely that the low levels of nitrite/nitrate found in the amenorrheic group were caused by a low dietary intake. Exercise has been shown to increase NO synthesis (43, 44), and this is thought to play a role in arteriolar vasodilatation during exercise and the cardioprotective effect of chronic exercise. Levels of NO metabolites might then be expected to be high in athletes (43); this was not the case for the eumenorrheic group, who had a urinary NO metabolite level similar to that of the sedentary controls in the present study. The amenorrheic athletes, although also extremely active, had the lowest urinary NO levels. The low levels of NO metabolites in the amenorrheic athletes are most likely caused by chronic low estrogen levels. NO is generated in many estrogen-sensitive tissues, and the urinary levels will reflect the contribution from many of these sites. It is unlikely, however, that NO synthesis in bone would be unaffected by low estrogen if production in other tissues has been reduced. At a cellular level in bone, eNOS-derived NO is thought to mediate mechanical stress stimuli by osteocytes (19, 20), activate osteoblast function (45), and suppress osteoclast resorption activity (23, 24).
In conclusion, the results show that amenorrheic athletes do not resemble postmenopausal women in terms of bone turnover but do have reduced urinary concentrations of NO metabolites and spinal osteopenia. The question, therefore, arises as to the mechanism behind bone loss in these young women. Longitudinal studies of athletes who experience amenorrhea for part of the year, because of variations in training intensity, would enable more detailed study within an individual of the pattern of bone turnover and NO synthesis status with changing endocrine status. Subtle changes in bone formation and resorption, which may be obscured by group comparisons, might then become apparent. Further attention needs to be paid to treatment options for these women. Restoration of NO synthesis by dietary arginine supplementation could be one approach (46).
| Footnotes |
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Received November 7, 1997.
Revised March 13, 1998.
Accepted April 22, 1998.
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