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E and physical
performance at altitude are not affected by menstrual cycle
phase
Thermal and Mountain Medicine Division, United States Army Research Institute of Environmental Medicine, Natick, Massachusetts 01760
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ABSTRACT |
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We hypothesized that progesterone-mediated
ventilatory stimulation during the midluteal phase of the menstrual
cycle would increase exercise minute ventilation
(
E; l/min) at sea level (SL) and with
acute altitude (AA) exposure but would only increase arterial
O2 saturation
(SaO2, %) with AA exposure. We further hypothesized that an increased exercise
SaO2 with AA exposure would enhance
O2 transport and improve both peak
O2 uptake
(
O2 peak; ml · kg
1 · min
1)
and submaximal exercise time to exhaustion (Exh; min) in the midluteal
phase. Eight female lowlanders [33 ± 3 (mean ± SD) yr, 58 ± 6 kg] completed a
O2 peak and
Exh test at 70% of their altitude-specific
O2 peak at SL and with
AA exposure to 4,300 m in a hypobaric chamber (446 mmHg) in their early
follicular and midluteal phases. Progesterone levels increased
(P < 0.05) ~20-fold from the early
follicular to midluteal phase at SL and AA. Peak
E (101 ± 17) and submaximal
E (55 ± 9) were not
affected by cycle phase or altitude. Submaximal
SaO2 did not differ between cycle
phases at SL, but it was 3% higher during the midluteal phase with
AA exposure. Neither
O2 peak nor Exh time
was affected by cycle phase at SL or AA. We conclude that, despite
significantly increased progesterone levels in the midluteal phase,
exercise
E is not increased
at SL or AA. Moreover, neither maximal nor submaximal exercise
performance is affected by menstrual cycle phase at SL or AA.
hypobaric hypoxia; ovarian hormones; submaximal exercise; peak oxygen uptake; ventilatory control
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INTRODUCTION |
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LOW LEVELS OF ESTRADIOL and progesterone are found in
the early follicular phase of the menstrual cycle, whereas high levels are found in the midluteal phase (26). The primary effects of estradiol
and progesterone are related to reproductive behavior, but a number of
reviews have addressed the role both progesterone and estradiol play in
stimulating minute ventilation (
E) (2, 28). There is ample evidence to suggest that progesterone is the major
reason for the observed increase in resting
E in the midluteal phase. First,
progesterone reaches peak values in the midluteal phase at the same
time that end-tidal PCO2 (PETCO2) reaches a nadir
(18). Second, there is a fivefold increase in progesterone in pregnant
women, which is accompanied by a 35-50% increase in resting
E (32, 35). Third, when synthetic
progesterone is administered to men, an increase in resting
E and chemosensitivity is observed (5,
42). However, estradiol may augment the stimulatory effects of
progesterone on resting
E (8, 39) by
increasing the number and affinity of progesterone receptors (8, 36).
Incremental increases in estradiol (10-55%) and progesterone
(18-80%) also occur during both maximal and submaximal exercise at sea level (SL), with more pronounced increases occurring in the
midluteal phase (6, 34). Given their stimulatory effects on resting
E, midluteal-phase increases in estradiol
and progesterone may increase exercise
E.
Several studies have reported an increase in maximal or submaximal
exercise
E in the midluteal phase (15, 24, 41, 52), whereas others have reported no differences (3, 13, 22,
27). Thus the effect of cyclic variations in ovarian hormones on
exercise
E at SL remains unclear.
Exercise
E plays a critical role in
providing O2 to exercising
muscles. However, exercise
E is not
considered to be a limiting factor during exercise at SL, given
that normal healthy individuals rarely approach mechanical or diffusion
limitations even at maximal exercise intensities (14). Regardless of
whether SL studies have reported an increased or similar exercise
E in the midluteal phase, the literature
is almost unanimous in reporting no differences in exercise performance
between phases of the menstrual cycle (9, 10, 13, 15, 22, 27, 31, 41).
In the two studies that reported an increase in submaximal exercise
performance in the midluteal phase (24, 34), both attributed
the increase to improvements in substrate utilization not submaximal
exercise
E. Thus cycle-phase differences
in exercise
E do not appear to be a
critical factor in limiting maximal or submaximal exercise performance
at SL.
Although exercise performance may not be strongly influenced by
ventilatory cycle-phase differences at SL, the same may not be true
during an acute exposure to high altitude. Because arterial blood is
>96% saturated with O2 at SL
(20), a small increase (6-8%) (13) in exercise
E during the midluteal phase may not impart any exercise performance advantage at SL. At 4,300 m, however, arterial blood is ~84% saturated (20), and a small increase in
exercise
E during the midluteal phase
could raise the arterial PO2
(PaO2), increase arterial
O2 saturation
(SaO2), and thus increase arterial
O2 content. An increased arterial
O2 content would then create a
larger peripheral diffusion gradient for
O2, enhance
O2 transport during exercise, and
potentially improve both maximal and submaximal exercise performance
during the midluteal phase at 4,300 m.
The purpose of this study was to determine the effect of ovarian
hormone levels that are associated with the early follicular and
midluteal phases of the menstrual cycle on maximal and submaximal exercise performance at SL and acute altitude (AA). We hypothesized that increased estradiol and progesterone levels in the midluteal phase
would stimulate exercise
E during SL and
AA exposures, but such increased levels of exercise
E would improve
SaO2 only at AA, and thus would improve
maximal and submaximal exercise performance only at AA.
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METHODS |
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Volunteer test subjects. Ten nonsmoking women volunteers were originally enrolled in this study. Two of the 10 volunteers completed the study but were eliminated from further analysis because of inadequate menstrual cycle documentation. The remaining eight volunteers had an age, initial body weight, and height of 33 ± 3 (SD) yr, 58 ± 6 kg, and 163 ± 8 cm, respectively. Percent body fat, determined by hydrostatic underwater weighing, was 26 ± 3%. All had menstrual cycles of consistent length (25-35 days) and had not taken oral contraceptives or hormone therapy for at least 6 mo before entering the study. None was pregnant, and none had been pregnant for at least 2 yr before starting the study. All had normal hemoglobin and serum iron stores.
All volunteers were lifelong residents at low altitude and had no exposure to altitudes >1,000 m for at least 6 mo before the study. All were healthy, physically active women who participated in aerobic exercise (2-3 h/wk) before and during the study. All provided written acknowledgment of their voluntary consent, and they were made aware of their right to withdraw without prejudice at any time. Investigators adhered to Army Regulation 70-25 and US Army Research and Materiel Command Regulation 70-25 on the use of volunteers in research.Menstrual cycle documentation. Supportive evidence for normal ovulatory cycles was initially obtained by a menstrual cycle-history questionnaire. Evidence of ovulation was obtained by using the First Response Ovulation Predictor Test (Carter Wallace Products Division, New York, NY), which detected (within 24-36 h) the onset of the luteinizing hormone (LH) surge by using urine samples from the first morning void. Urine testing started 9-15 days after menses, depending on each woman's cycle length, and continued until the LH surge was detected. Volunteers kept a record of their first day of menses and ovulation test results for 1 mo before testing, during the 2-3 mo of testing, and for 1 mo after testing was completed.
Study protocol.
The study used an unblinded, balanced experimental design in which each
test volunteer's ovarian hormones, ventilatory parameters, and
exercise performances were evaluated at SL and AA during both the early
follicular (3-6 days after the beginning of menstruation) and
midluteal (6-9 days after the LH surge) phases of her menstrual cycle. The four test conditions were defined as sea level, follicular (SL/F); sea level, luteal (SL/L); acute altitude, follicular (AA/F); and acute altitude, luteal (AA/L). During each test condition, 3 days
were used to complete all exercise and ventilatory tests. On the first
day, volunteers completed pulmonary function tests (PFT) and a
treadmill peak O2 uptake
(
O2 peak) test. On the second day, during SL exposures only, volunteers completed hypoxic ventilatory response (HVR) and hypercapnic ventilatory response (HCVR)
tests. On the third day, they completed a treadmill submaximal exercise
to exhaustion (Exh) test conducted at 70% of altitude-specific
O2 peak. Each
exercise and ventilatory test was performed at the same time of day for
each volunteer in all four testing conditions. The order of menstrual
cycle phase and altitude combination in which testing was performed was randomized.
Environmental conditions.
All exercise testing was performed in a hypobaric chamber that was
maintained at a temperature and relative humidity of 22 ± 3°C
and 45 ± 5%, respectively. After the volunteers entered the
hypobaric chamber for the
O2 peak and Exh tests
during AA exposures, the chamber was decompressed to the barometric
equivalent of 4,300 m (446 mmHg) over a period of ~12 min. All
exercise tests in the hypobaric chamber were initiated within 30 min of
arriving at 4,300-m equivalent altitude and were completed within
1-3 h, depending on how long the volunteers exercised to reach exhaustion.
Ovarian hormone analysis.
Ovarian-hormone levels were measured to document menstrual cycle phase.
A resting blood sample was obtained before both the
O2 peak and Exh tests
for analyses of estradiol and progesterone levels. The mean from these
two testing occasions represents the resting estradiol and progesterone
levels, respectively. A serum progesterone value >5 ng/ml was
accepted as confirmation of the midluteal phase (26). Additional blood
samples for estradiol and progesterone were taken every 15 min and at
exhaustion during the Exh test. The mean value from these time periods
represents the exercise estradiol and progesterone levels,
respectively. Serum concentrations of estradiol and progesterone were
determined in duplicate by using a solid-phase
125I radioimmunoassay (Diagnostic
Products, Los Angeles, CA). The intra-assay variances for estradiol and
progesterone were 4.7 and 7.4%, respectively. All samples for one
volunteer were analyzed in the same assay to avoid interassay variations.
Ventilatory testing.
Resting pulmonary function measurements of forced vital capacity (FVC),
forced expired volume in 1 s
(FEV1), and maximal voluntary ventilation (MVV) were obtained
(BTPS) by standard protocols (21) with the use of a computerized dry-rolling seal spirometer (model PFT2450, SensorMedics, Yorba Linda, CA). Before the HVR test, the
PETCO2, a measure of resting
E, was measured by using a
CO2 analyzer (model LB-2, Beckman,
Anaheim, CA) for 2-3 min during resting breathing, and the mean
value from the last minute was used. Resting control of breathing was
assessed with the HVR and HCVR tests. The HVR was measured by inducing
progressive isocapnic hypoxia, over an 8- to 10-min period (50), by
using a rebreathing system containing an initial concentration of 21% O2. Continuous measurements were
made of PETCO2, which was
maintained within ±2 Torr of the resting level for that day by
manual adjustment of the air flow through a
CO2-absorber circuit. The
E was measured by using a dry-rolling
seal spirometer (model 762609 spirometer, SensorMedics), and
SaO2 was measured by finger pulse
oximetry (Oxyshuttle, SensorMedics). The measurement error of this
finger pulse oximeter is ±2% at >70%
SaO2 and ± 3% at <70%
SaO2. The HVR slope
(HVR-S), a measure of hypoxic chemosensitivity, was reported as

E/
SaO2,
calculated by using least squares regression. The HCVR test was
performed by inducing progressive hypercapnia and using a gas mixture
with an initial composition of 7%
CO2-93%
O2, following the protocol
described by Read (37). The
PETCO2 was allowed to rise
~15 Torr above resting levels for that day over a 5- to 7-min
period. The HCVR slope (HCVR-S), a measure of
hypercapnic chemosensitivity, was calculated, over the linear portion
of the

E/
PACO2
relationship, using least squares linear regression, and the
equation
E = S(PACO2
B), where
PACO2 is alveolar (end-tidal)
PCO2. The HCVR intercept, B, represents
an imaginary threshold of the
CO2-sensing system and was
reported as
PACO2.
Exercise-performance testing. Before all exercise tests, the volunteers were required to abstain from alcohol and caffeine for at least 24 h and to refrain from exercise on the testing day. The volunteers also maintained the same diet for 24 h before each of the four Exh tests. Twenty-four-hour dietary logs were analyzed for energy content and percent contribution of macronutrients by computer with the use of the Food Intake Analysis System (University of Texas Health Science Center, Houston, TX).
Before each exercise test, the volunteer was weighed (wearing T-shirt, shorts, and socks) to the nearest 0.1 kg. During exercise, heart rate (HR) was determined from continuous electrocardiogram recordings (Cardiovit AT-6C; Schiller Canada, Nepean, ON, Canada). Respiratory gas measurements were made continuously during the
O2 peak test and
intermittently during the Exh test by using open-circuit calorimetry
(model 2900 metabolic cart; SensorMedics) calibrated with certified
gases and volume standard. The metabolic cart provided values
for
E,
O2 uptake
(
O2), and carbon dioxide output (
CO2). The
ventilatory equivalents for
O2
(
E/
CO2) and CO2
(
E/
CO2)
were calculated from individual
E,
O2, and
CO2 data to minimize
intrasubject variability in
E due to
different body sizes and metabolic rates. The
SaO2 and the rating of perceived
exertion (RPE), using the whole-body Borg scale (7), were obtained at
the end of peak exercise and every 15 min during submaximal exercise.
Peak-exercise testing.
The
O2 peak was
determined by a progressive-intensity, continuous, treadmill-running
test to exhaustion modified from Costill and Fox (12). After a 3-min
warm-up, the speed and grade were increased to 2.2-2.7 m/s and
2.0%, respectively, for the first 2 min. Thereafter, the speed was
kept constant and the grade was increased by 2% every 2 min. The
highest
O2 achieved for 1 min before exhaustion was recorded as
O2 peak.
Submaximal-exercise testing.
After a 3-min warm-up, each volunteer exercised, until exhaustion, at
70% of her altitude-specific
O2 peak. Treadmill
speed and/or grades were adjusted to reach the desired percentage of
O2 peak for each
volunteer. In all cases, the target
O2 was obtained within 10 min of the beginning of exercise. Cardiorespiratory measurements were
obtained during the last 5 min of every 15-min period of exercise, and
the mean value was calculated from the last 3 min. A 28-item validated
internal-state questionnaire (ISQ) (1) was given at
minute 45 during the Exh test, and a
respiratory distress symptom score (ISQ-R) and a fatigue symptom score
(ISQ-F) were calculated from the answers to this questionnaire to
determine the volunteer's level of perceived breathlessness and
fatigue during the Exh test. A typical question (i.e., "I cannot
easily exhale the air from my lungs") was rated by using a 6-point
rating scale, with 0 standing for "not at all" and 5 standing for
"extreme." The volunteers were not aware of their ongoing
exercise time during the Exh tests.
Statistical analyses.
Before the study was begun, sample-size estimations were performed by
using predicted mean phase differences and SD on
O2 peak and Exh time
from previous studies (9, 34). A sample size of 10 provided a 70%
probability of detecting a 2 ml · kg
1 · min
1
increase in
O2 peak
and a 15-min increase in Exh time at the P < 0.05 level (11). Two-way ANOVAs
with repeated measures on each factor were used to analyze the
differences between menstrual cycle phase (early follicular and
midluteal) and altitude (SL and AA) for all physiological parameters
measured during the
O2 peak and
Exh test. Three-way ANOVAs, with repeated measures on the additional
factor of time, were used for estradiol and progesterone analyses.
Significant main effects and interactions were analyzed by using
Tukey's least significant difference test. Dependent one-way
t-tests were used to analyze resting
E and ventilatory control at SL. Pearson
product-moment correlation coefficients were calculated for
relationships between levels of ovarian hormones, measures of
ventilation (both physiological and psychological), and measures of
exercise performance. Statistical significance was set at
P < 0.05. All data are
presented as means ± SD.
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RESULTS |
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Volunteer test subjects.
Body weights, energy intakes, and percent contributions of
macronutrients were not different between testing sessions. Mean length
of menstrual cycle was 28 ± 2 days during the 4 mo of testing, and
ovulation occurred 14 ± 6 days after the onset of menstruation. Among subjects in the early follicular phase, resting estradiol levels
ranged from 22 to 73 pg/ml while progesterone levels ranged from 0.2 to
1.1 ng/ml. Among subjects in the midluteal phase, resting estradiol
levels ranged from 62-200 pg/ml while progesterone levels ranged
from 5 to 27 ng/ml. Mean resting and exercise estradiol and
progesterone levels, presented in Table 1,
are within previously reported normal ranges for eumenorrheic women
(26).
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Pulmonary function and resting
E and
control.
PFT results, presented in Table 2, are within previously
reported normal ranges (33). The FVC,
FEV1, and MVV were not affected by
cycle phase. The MVV was increased at AA compared with SL. Resting
PETCO2 was
decreased (P < 0.03) during SL/L
(36.3 ± 1.7 Torr) compared with during SL/F (38.9 ± 2.3 Torr).
Individual resting ventilatory responsiveness to the change in
progesterone from SL/F to SL/L is presented in Fig. 1.
The HVR-S during SL/F (0.50 ± 0.25) and SL/L (0.64 ± 0.33) were not different. Similarly, the HCVR-S values during SL/F
(1.93 ± 0.98) and SL/L (2.11 ± 1.35) were not different. The
HCVR-B was decreased (P = 0.08) during SL/L (38.9 ± 2.8) compared with during SL/F (41.3 ± 5.6). There were no correlations between estradiol, progesterone, or
progesterone/estradiol levels and respective
PETCO2, HVR-S, HCVR-S,
or HCVR-B during SL/F or SL/L. When results from SL/F and SL/L
were combined, there was a negative correlation
(r =
0.56;
P < 0.02) between progesterone and
PETCO2 but not
between any of the other previously mentioned parameters
(Fig. 1). There were positive correlations between HCVR-S and
mean submaximal
E/
CO2
during both SL/F (r = 0.57;
P = 0.08) and SL/L
(r = 0.63;
P = 0.09).
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Peak-exercise testing.
Cardiopulmonary measurements collected during the
O2 peak test are
presented in Table 3. There were no cycle-phase
differences in
O2 peak at SL
or AA, but
O2 peak was
decreased ~28% at AA compared with SL. The peak
E was not affected by
cycle phase or altitude, but
E/
O2 peak
was increased ~39% at AA compared with SL in both phases. Similarly,
E/peak
CO2 was increased ~40% at
AA compared with SL in both phases. The peak
SaO2 was not affected by cycle phase at
SL or AA, but it was decreased ~28% at AA compared with SL. Although
there were no cycle phase differences at SL or AA, peak HR was
decreased ~5% at AA compared with SL.
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E,
E/
O2 peak,
E/peak
CO2, or peak SaO2 in any of the four test conditions.
Furthermore, none of the ventilatory measurements during peak exercise
was correlated with respective
O2 peak measurements in
any of the four testing conditions. However,
O2 peak was positively
correlated with Exh time at SL/F (r = 0.75; P < 0.03), SL/L
(r = 0.77;
P < 0.02), AA/F
(r = 0.66;
P = 0.07), and AA/L
(r = 0.65;
P = 0.08).
Submaximal-exercise testing.
Submaximal cardiopulmonary responses collected during the Exh test
are presented in Table 4. The Exh time was
not affected by cycle phase or altitude. Submaximal
O2
(
O2 sub)
was not affected by cycle phase, but it was decreased ~28% at AA
compared with SL, because volunteers were exercising at 70% of their
altitude-specific
O2 peak
(i.e., a lower power output at AA). The submaximal
E (
Esub)
was not affected by cycle phase or altitude, but
E/
O2 sub
was increased ~33% during AA compared with SL. The
E/submaximal
CO2
(
CO2 sub)
did not differ between cycle phases, but it was increased ~40%
during AA compared with SL. The submaximal SaO2
(SaO2 sub)
was decreased ~22% in both phases during AA compared with SL and
showed a cycle-phase difference, being 2.4% higher during AA/L
compared with AA/F. Although there were no cycle-phase differences at
SL or AA, sumaximal HR (HRsub)
was decreased ~7% during AA compared with SL.
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E sub,
E/
O2 sub,
E ·
CO2 sub,
or SaO2 sub in any of
the four test conditions. Furthermore, none of the ventilatory
measurements during submaximal exercise was correlated with respective
Exh times in any of the four testing conditions.
Perceptions of exertion and internal state during the Exh test are
presented in Table 5. The RPE during
submaximal exercise was similar in all four testing conditions.
Although there were no cycle phase differences, ISQ-R was increased
during AA compared with SL. The ISQ-F showed no cycle-phase or altitude
differences. There were no correlations between RPEs during submaximal
exercise and respective Exh times in any of the four conditions. Both
ISQ-R and ISQ-F were negatively correlated (range:
0.66 to
0.95; P < 0.05) with their
respective Exh times in each of the four testing conditions.
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DISCUSSION |
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The principal findings of this study are that, despite significantly
increased progesterone levels in the midluteal phase, exercise
E was not increased at SL or AA.
Furthermore, neither maximal nor submaximal exercise performance was
affected by menstrual cycle phase at SL or during an AA exposure. This
study also found that resting
E was
increased in the midluteal phase, but resting chemosensitivity was not
affected by cycle phase at SL.
A critical aspect of this study was confirmation of appropriate differences in ovarian hormone levels when the early follicular and midluteal phases of the menstrual cycle are compared. Urinary LH-surge-predictor kits and past, as well as current, data on menstrual history were used to predict the different phases of the menstrual cycle. Data were accepted only if the subjects had normal length (i.e., 25- to 35-day) consistent menstrual cycles, exhibited an LH surge every menstrual cycle, and had resting estradiol and progesterone levels within previously accepted normal ranges (26). These criteria resulted in appropriate differences in ovarian-hormone levels between cycle phases.
Resting SL measures of
E were used in
this study to establish the sensitivity of our instrumentation and to
provide evidence that our subjects were normal, healthy women. The
increase in resting
E (i.e., 2.7-Torr
lower PETCO2) in the
midluteal phase was expected and consistent with the mean phase
difference (i.e., 2.6- Torr lower
PETCO2) calculated from
seven previous studies (18, 38, 41, 44-46, 51). Thus, our
instrumentation was sensitive enough to detect small differences in
resting
E, and the results
confirm the magnitude of cycle-phase differences in resting
E reported in other studies.
In this study, resting measurements of ventilatory control were made to
provide potential explanations for any observed cycle phase differences
in exercise
E. Although progesterone
levels were significantly increased in the midluteal phase, resting
chemosensitivity was not altered by cycle phase at SL. Others have also
reported that HVR and HCVR are not increased in the midluteal phase,
despite increased resting
E (38, 45, 46).
However, several studies have reported an increased HVR and HCVR in the
midluteal phase (16, 17, 24, 41, 44, 52). In addition, one study
reported an increased HVR but similar HCVR (51), whereas another study found the opposite results (15). In evaluation of these studies, serum
measurements of estradiol and progesterone must be considered, because
anovulatory cycles can occur even with consistent, normal-length menstrual cycles (48). However, even when only studies providing hormonal documentation are considered (15, 17, 24, 38, 41, 51, 52), the
results remain equivocal.
Controversy regarding the effect of ovarian hormones on ventilatory chemosensitivity is probably due to 1) a wide range of estradiol and progesterone among subjects in the same study, as well as between studies, 2) individual responsiveness to a given ovarian hormone level, and 3) the relatively large within-subject, between-day variability inherent in measures of ventilatory chemosensitivity (40). There is a huge range, among subjects, in midluteal values (i.e., 6-9 days after LH surge) for estradiol (60-320 pg/ml) and progesterone (5-28 ng/ml) in a normal menstrual cycle (26). Thus it is difficult to compare the results from studies in which subjects had low mean values of estradiol and progesterone with results from studies in which subjects had high mean values of these ovarian hormones.
As shown in Fig. 1, there is also a large variation among women in
ventilatory responsiveness to any given level of progesterone. Data
from men and pregnant women also suggest a lack of correlation between
progesterone levels and resting ventilatory responsiveness (5, 32, 35).
Furthermore, medroxyprogesterone acetate, a synthetic progesterone with
15 times the progestational activity of progesterone, stimulates
E to the same degree as does progesterone on a gram-for-gram basis (47). All of this evidence suggests that
perhaps target receptors for progesterone, rather than circulating progesterone levels, are critical for mediation of the resting ventilatory response. Because estradiol levels may be critical for
inducing progesterone receptors (8, 36), we considered whether the
level of estradiol or the progesterone-to-estradiol ratio was related
to chemosensitivity, and we found no correlations. Thus differing
results for HVR and HCVR between studies may have to do with whether
the women studied were responders or nonresponders to circulating
levels of estradiol and progesterone.
The large variability associated with measurements of HVR and HCVR (40) also makes comparisons between studies difficult. In our laboratory, the coefficients of variation for HCVR (42.7%) and HVR (62.9%) are large. Thus, if cycle-phase differences exist, large subject numbers are required to show significance. In the present study, there was no trend for either the HVR or HCVR slope to exhibit phase differences, but the lower HCVR intercept (P = 0.08) in the midluteal phase might have been significant if the numbers of subjects were increased. A definitive study employing a large number of subjects, accompanied by measurements made daily or every other day of both ovarian hormones and ventilatory control, is certainly warranted, given the current equivocal findings in the literature.
Although resting
E was increased in the
midluteal phase at SL, neither maximal nor submaximal exercise
E was increased at either SL or AA. This
finding agrees with the results of some studies (3, 13, 22, 27) but
disagrees with others (15, 41, 52). In one study, an increase in
maximal but not submaximal exercise
E was
reported in the midluteal phase (24). In a recent study that found an
increased exercise
E at both 55 and 85%
O2 max in the midluteal
phase, there was also a reported increase in
O2 (52). Thus the increase in
submaximal
E in their study
may have been secondary to the increased
O2 and not to
progesterone-mediated stimulation of
E.
Alternatively, the discrepancy between the study of Williams and
Krahenbul (52) and the present study could be due to the fact that our
mean progesterone values were comparable to their progesterone levels
in the early luteal and late luteal phases, in which they found no
increases in submaximal exercise
E. The
overall lack of a correlation between progesterone levels and
submaximal ventilatory measurements in any of our four test conditions
suggests that additional factors, such as changes in central motor
command and reflexes from the exercising limbs, may have a greater
influence on exercise
E than do endogenous
levels of progesterone (49).
In other studies on women that report an increased exercise
E in the midluteal phase an increased
resting HCVR has typically been reported (15, 24, 41, 52). Previous
studies in men have also shown that exercise
E is positively correlated with resting HCVR (29, 30). We also found a positive correlation between
HCVR-S and exercise
E in both cycle
phases. However, because there was no cycle-phase difference in HCVR-S
in the present study, it was not surprising that exercise
E was also not affected by cycle phase at
SL or AA.
The lack of a cycle-phase effect on exercise
E does not appear to be related to a
mechanical limitation to
E at SL
or AA in the midluteal phase. In the present study, consistent with a
previous report (10), there were no cycle-phase differences in the
mechanics of breathing at SL or AA. Furthermore, even though MVV was
increased at AA because of the reduced density of the air, the percent
utilization of MVV during both peak and submaximal exercise at SL and
AA was similar between phases of the menstrual cycle. Thus, in our
study, there did not seem to be a mechanical limitation to
E that would impair ovarian
hormone-mediated increases in exercise
E.
Because there was no improvement in exercise
E during submaximal exercise in the
midluteal phase at AA, the 3% increase in
SaO2 in the midluteal phase during the
Exh test at AA was surprising. The SaO2
may not always track changes in
E during
exercise at altitude, as reported by Bender et al. (4). In the present study, there was also no correlation between exercise
E and SaO2; this suggests that the
elevated exercise SaO2 may reflect an
improvement in pulmonary gas exchange. Alternatively, the 3% increase
in SaO2 in the midluteal phase could
reflect the ~2% measurement error inherent in the pulse oximeter.
However, any measurement error of the pulse oximeter should be randomly
distributed, making it unlikely that it was the main reason for the
observed difference in SaO2 between
phases of the menstrual cycle.
Although submaximal exercise SaO2 was increased in the midluteal phase at AA, Exh time was not affected by cycle phase during an AA exposure. We had hypothesized that the improvement in SaO2 during AA in the midluteal phase would result in an increased arterial O2 content, O2 transport, and exercise performance at AA. However, the small increase in exercise SaO2 that was observed in the midluteal phase obviously was not large enough to affect submaximal exercise performance.
This study also confirms the findings of some that neither maximal (13,
15, 22, 31, 41) nor submaximal (9, 10, 13, 27, 31) exercise performance
is affected by the phase of the menstrual cycle at SL, but the study
also refutes the findings of others that have reported cycle-phase
differences in submaximal exercise performance (24, 34). Reasons for
discrepant findings between studies concerning submaximal exercise
performance may have to do with 1)
the fitness level of subjects (41),
2) the large variability associated
with the measurement of endurance-exercise performance (23), and
3) varying submaximal intensities
used to measure endurance-exercise performance (24, 34). In one study reporting an increased submaximal exercise
performance in the midluteal phase (34), the significance was
borderline (P = 0.06). with small
subject numbers. In the other study (24), a 90%
O2 max
exercise-until-exhaustion test was used, which may not be an
appropriate measurement of submaximal endurance capacity. In the
present study, the variability for Exh time was larger than was
anticipated on the basis of previous studies (9, 27, 34). Thus we
cannot discount the probability of a type II error in our significance
testing. However, there was absolutely no trend for Exh time to be
increased in the midluteal phase at SL, and, even if we had higher
numbers of subjects, the results likely would have been the same. Thus
our analysis suggests that menstrual cycle effects, if present, are
small and do not significantly affect submaximal exercise performance
at SL.
We also examined whether there was a relationship between the other
variables measured and submaximal exercise performance. The three
variables most correlated with Exh time in all four testing conditions
were ISQ-R, ISQ-F, and
O2 peak (Table 5). The
high negative correlation between ISQ-R and ISQ-F and Exh time suggests that perceptions of respiratory distress
and fatigue have a strong relationship with Exh time. Schoene et al.
(41) also suggested that a high degree of adverse respiratory
sensations, which were experienced in the luteal phase, limited
exercise performance in their low-altitude study. However, in our
study, perceptions of respiratory distress (i.e., ISQ-R) and fatigue
(i.e., ISQ-F) were not affected by cycle phase. Thus it was not
surprising that Exh time was also not affected by cycle phase.
Surprisingly, RPE was not correlated to Exh time in any of the four
testing conditions. This may be due to the fact that ISQ-F assesses
perception of future events (i.e., "I think I can continue this
exercise for 30 more min"), whereas the RPE assesses perception of
fatigue at that moment in time. Furthermore, the ISQ-R isolates respiratory sensations, whereas the RPE evaluates whole-body fatigue. The high correlation between
O2 peak and
Exh time corresponds with the research of others that have shown that
O2 max is highly positively correlated to middle- and long-distance running performance (19, 43).
In summary, the present study found that, despite significantly
increased progesterone levels in the midluteal phase, exercise
E was not increased at SL or AA. Moreover,
neither maximal nor submaximal exercise performance was affected by
cycle phase at SL or AA. This may have important implications for
individuals whose work, athletic competition, or recreation schedules
involve short-term exposures to altitude.
| |
ACKNOWLEDGEMENTS |
|---|
We would like to thank the test volunteers for their participation and cooperation in this study. The authors gratefully acknowledge the technical and logistical support provided by Jim Devine, James Bogart, Lindsay Gibson, Cpt. Timothy Lyons, Sgt. Sinclair Smith, and Pvt. Keesha Miller.
| |
FOOTNOTES |
|---|
The views, opinions and/or findings in this report are those of the authors, and should not be construed as an official Department of the Army position, policy or decision, unless so designated by other official documentation.
Citations of commercial organizations and trade names in this report do not constitute an official Department of the Army endorsement or approval of the products or services of these organizations.
The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked "advertisement" in accordance with 18 U.S.C. §1734 solely to indicate this fact.
Address for reprint requests and other correspondence: B. A. Beidleman, Thermal and Mountain Medicine Division, US Army Research Institute of Environmental Medicine, Natick, MA 01760 (E-mail: BBEIDLEMAN{at}NATICK-CCMAIL.ARMY.MIL).
Received 6 February 1998; accepted in final form 21 December 1998.
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