Muscle accounts for glucose disposal but not blood lactate appearance during exercise after acclimatization to 4,300 m.

We hypothesized that the increased blood glucose disappearance (Rd) observed during exercise and after acclimatization to high altitude (4,300 m) could be attributed to net glucose uptake (G) by the legs and that the increased arterial lactate concentration and rate of appearance (Ra) on arrival at altitude and subsequent decrease with acclimatization were caused by changes in net muscle lactate release (L). To evaluate these hypotheses, seven healthy males [23 +/- 2 (SE) yr, 72.2 +/- 1.6 kg], on a controlled diet were studied in the postabsorptive condition at sea level, on acute exposure to 4,300 m, and after 3 wk of acclimatization to 4,300 m. Subjects received a primed-continuous infusion of [6,6-D2]glucose (Brooks et al., J. Appl. Physiol. 70: 919-927, 1991) and [3-13C]lactate (Brooks et al., J. Appl. Physiol. 71:333-341, 1991) and rested for a minimum of 90 min, followed immediately by 45 min of exercise at 101 +/- 3 W, which elicited 51.1 +/- 1% of the sea level peak O2 uptake (65 +/- 2% of both acute altitude and acclimatization peak O2 uptake). Glucose and lactate arteriovenous differences across the legs and arms and leg blood flow were measured. Leg G increased during exercise compared with rest, at altitude compared with sea level, and after acclimatization. Leg G accounted for 27-36% of Rd at rest and essentially all glucose Rd during exercise. A shunting of the blood glucose flux to active muscle during exercise at altitude is indicated. With acute altitude exposure, at 5 min of exercise L was elevated compared with sea level or after acclimatization, but from 15 to 45 min of exercise the pattern and magnitude of L from the legs varied and followed neither the pattern nor the magnitude of responses in arterial lactate concentration or Ra. Leg L accounted for 6-65% of lactate Ra at rest and 17-63% during exercise, but the percent Ra from L was not affected by altitude. Tracer-measured lactate extraction by legs accounted for 10-25% of lactate Rd at rest and 31-83% during exercise. Arms released lactate under all conditions except during exercise with acute exposure to high altitude, when the arms consumed lactate. Both active and inactive muscle beds demonstrated simultaneous lactate extraction and release. We conclude that active skeletal muscle is the predominant site of glucose disposal during exercise and at high altitude but not the sole source of blood lactate during exercise at sea level or high altitude.     

Decreased exercise muscle lactate release after high altitude acclimatization

Blood lactate concentration during exercise decreases after acclimatization to high altitude, but it is not clear whether there is decreased lactate release from the exercising muscle or if other mechanisms are involved. We measured iliac venous and femoral arterial lactate concentrations and iliac venous blood flow during cycle exercise before and after acclimatization to 4,300 m. During hypoxia, at a given O2 consumption the venous and arterial lactate concentrations, the venous and arterial concentration differences, and the net lactate release were lower after acclimatization than during acute altitude exposure. While breathing O2-enriched air after acclimatization at a given O2 consumption the venous and arterial lactate concentrations and the venous and arterial concentration differences were significantly lower, and the net lactate release tended to be lower than while breathing ambient air at sea level before acclimatization. We conclude that the lower lactate concentration in venous and arterial blood during exercise after altitude acclimatization reflected less net release of lactate by the exercising muscles, and that this likely resulted from the acclimatization process itself rather than the hypoxia per se.     

Increased dependence on blood glucose after acclimatization to 4,300 m

To evaluate the hypothesis that altitude exposure and acclimatization result in increased dependency on blood glucose as a fuel, seven healthy males (23 +/- 2 yr, 72.2 +/- 1.6 kg, mean +/- SE) on a controlled diet were studied in the postabsorptive condition at sea level (SL), on acute altitude exposure to 4,300 m (AA), and after 3 wk of chronic altitude exposure to 4,300 m (CA). Subjects received a primed continuous infusion of [6,6-2D]glucose and rested for a minimum of 90 min, followed immediately by 45 min of exercise at 101 +/- 3 W, which elicited 51.1 +/- 1% of the SL maximal O2 consumption (VO2 max; 65 +/- 2% of altitude VO2 max). At SL, resting arterial glucose concentration was 82.4 +/- 3.2 mg/dl and rose significantly to 91.2 +/- 3.2 mg/dl during exercise. Resting glucose appearance rate (Ra) was 1.79 +/- 0.02 mg.kg-1.min-1; this increased significantly during exercise at SL to 3.71 +/- 0.08 mg.kg-1.min-1. On AA, resting arterial glucose concentration (85.8 +/- 4.1 mg/dl) was not different from sea level, but Ra (2.11 +/- 0.14 mg.kg-1.min-1) rose significantly. During exercise on AA, glucose concentration rose to levels seen at SL (91.4 +/- 3.0 mg/dl), but Ra increased more than at SL (to 4.85 +/- 0.15 mg.kg-1.min-1; P less than 0.05). Resting arterial glucose was significantly depressed with CA (70.8 +/- 3.8 mg/dl), but resting Ra increased to 3.59 +/- 0.08 mg.kg-1.min-1, significantly exceeding SL and AA values.(ABSTRACT TRUNCATED AT 250 WORDS)     

Internal carotid flow velocity with exercise before and after acclimatization to 4,300 m.

Cerebral blood flow and O2 delivery during exercise are important for well-being at altitude but have not been studied. We expected flow to increase on arrival at altitude and then to fall as O2 saturation and hemoglobin increased, thereby maintaining cerebral O2 delivery. We used Doppler ultrasound to measure internal carotid artery flow velocity at sea level and on Pikes Peak, CO (4,300 m). In an initial study (1987, n = 7 men) done to determine the effect of brief (5-min) exercises of increasing intensity, we found at sea level that velocity [24.8 +/- 1.4 (SE) cm/s rest] increased by 15 +/- 7, 30 +/- 6, and 22 +/- 8% for cycle exercises at 33, 71, and 96% of maximal O2 uptake, respectively. During acute hypobaric hypoxia in a decompression chamber (inspired PO2 = 83 Torr), velocity (23.2 +/- 1.4 cm/s rest) increased by 33 +/- 6, 20 +/- 5, and 17 +/- 9% for exercises at 45, 72, and 98% of maximal O2 uptake, respectively. After 18 days on Pikes Peak (inspired PO2 = 87 Torr), velocity (26.6 +/- 1.5 cm/s rest) did not increase with exercise. A subsequent study (1988, n = 7 men) of the effect of prolonged exercise (45 min at approximately 100 W) found at sea level that velocity (24.8 +/- 1.7 cm/s rest) increased by 22 +/- 6, 13 +/- 5, 17 +/- 4, and 12 +/- 3% at 5, 15, 30, and 45 min.(ABSTRACT TRUNCATED AT 250 WORDS)     

Increased exercise SaO2 independent of ventilatory acclimatization at 4,300 m

Arterial O2 saturation (Sao2) decreases in hypoxia in the transition from rest to moderate exercise, but it is unknown whether other several weeks at high altitude SaO2 in submaximal exercise follows the same time course and pattern as that of ventilatory acclimatization in resting subjects. Ventilatory acclimatization is essentially complete after approximately 1 wk at 4,300 m, such that improvement in submaximal exercise SaO2 would then require other mechanisms. On days 2, 8, and 22 on Pikes Peak (4,300 m), 6 male subjects performed prolonged steady-state cycle exercise at 79% maximal O2 uptake (VO2 max). Resting SaO2 rose from day 1 (78.4 +/- 1.6%) to day 8 (87.5 +/- 1.4%) and then did not increase further by day 20 (86.4 +/- 0.6%). During exercise, SaO2 values (mean of 5-, 15-, and 30-min measurements) were 72.7% (day 2), 78.6% (day 8), and 82.3% (day 22), meaning that all of the increase in resting SaO2 occurred from day 1 to day 8, but exercise SaO2 increased from day 2 to day 8 (5.9%) and then increased further from day 8 to day 22 (3.7%). On day 22, the exercise SaO2 was higher than on day 8 despite an unchanged ventilation and O2 consumption. The increased exercise SaO2 was accompanied by decreased CO2 production. The mechanisms responsible for the increased exercise SaO2 require further investigation.     

Similar carbohydrate but enhanced lactate utilization during exercise after 9 wk of acclimatization to 5,620 m

We hypothesized that reliance on lactate as a means of energy distribution is higher after a prolonged period of acclimatization (9 wk) than it is at sea level due to a higher lactate Ra and disposal from active skeletal muscle. To evaluate this hypothesis, six Danish lowlanders (25 +/- 2 yr) were studied at rest and during 20 min of bicycle exercise at 146 W at sea level (SL) and after 9 wk of acclimatization to 5,260 m (Alt). Whole body glucose Ra was similar at SL and Alt at rest and during exercise. Lactate Ra was also similar for the two conditions at rest; however, during exercise, lactate Ra was substantially lower at SL (65 micro mol. min(-1). kg body wt(-1)) than it was at Alt (150 micro mol. min(-1). kg body wt(-1)) at the same exercise intensity. During exercise, net lactate release was approximately 6-fold at Alt compared with SL, and related to this, tracer-calculated leg lactate uptake and release were both 3- or 4-fold higher at Alt compared with SL. The contribution of the two legs to glucose disposal was similar at SL and Alt; however, the contribution of the two legs to lactate Ra was significantly lower at rest and during exercise at SL (27 and 81%) than it was at Alt (45 and 123%). In conclusion, at rest and during exercise at the same absolute workload, CHO and blood glucose utilization were similar at SL and at Alt. Leg net lactate release was severalfold higher, and the contribution of leg lactate release to whole body lactate Ra was higher at Alt compared with SL. During exercise, the relative contribution of lactate oxidation to whole body CHO oxidation was substantially higher at Alt compared with SL as a result of increased uptake and subsequent oxidation of lactate by the active skeletal muscles.     

Women at altitude: ventilatory acclimatization at 4,300 m.

Women living at low altitudes or acclimatized to high altitudes have greater effective ventilation in the luteal (L) compared with follicular (F) menstrual cycle phase and compared with men. We hypothesized that ventilatory acclimatization to high altitude would occur more quickly and to a greater degree in 1) women in their L compared with women in their F menstrual cycle phase, and 2) in women compared with men. Studies were conducted on 22 eumenorrheic, unacclimatized, sea-level (SL) residents. Indexes of ventilatory acclimatization [resting ventilatory parameters, hypoxic ventilatory response, hypercapnic ventilatory response (HCVR)] were measured in 14 women in the F phase and in 8 other women in the L phase of their menstrual cycle, both at SL and again during a 12-day residence at 4,300 m. At SL only, ventilatory studies were also completed in both menstrual cycle phases in 12 subjects (i.e., within-subject comparison). In these subjects, SL alveolar ventilation (expressed as end-tidal PCO(2)) was greater in the L vs. F phase. Yet the comparison between L- and F-phase groups found similar levels of resting end-tidal PCO(2), hypoxic ventilatory response parameter A, HCVR slope, and HCVR parameter B, both at SL and 4,300 m. Moreover, these indexes of ventilatory acclimatization were not significantly different from those previously measured in men. Thus female lowlanders rapidly ascending to 4,300 m in either the L or F menstrual cycle phase have similar levels of alveolar ventilation and a time course for ventilatory acclimatization that is nearly identical to that reported in male lowlanders.     

Alterations in the serum electrolyte levels of women during high altitude (4,300 m) acclimatization

Eight, University of Missouri (230 m) college women were exposed for a period of 65 days to an elevation of 4,300 m on Pikes Peak. During the first week of altitude exposure marked increases in the serum levels of chloride, phosphate, proteinate and calcium and marked decreases in the serum levels of sodium, potassium, magnesium and estimated bicarbonate were observed. During the remainder of the altitude sojourn chloride, phosphate, potassium and magnesium reverted toward the initial low altitude value. Serum calcium levels, however, remained elevated during this latter period while sodium levels continued to decrease and proteinate levels continued to increase. There was little or no recovery of the estimated bicarbonate decrement as the period of exposure was prolonged. Two weeks after the subjects returned to Missouri some but not all of the electrolytes returned to their initial levels. Those not recovering completely included calcium, chloride, proteinate and estimated bicarbonate.

---

Zusammenfassung Bei acht Studentinnen der Universität von Missouri (230 m) wurden 65 Tage in der Station Pikes Peak (4.300 m) die Elektrolyte im Serum untersucht. Während der 1. Höhenwoche wurde ein deutlicher Anstieg des Chlorids, Phosphats, Proteinats und Calciums und ein deutlicher Abfall des Natriums, Kaliums, Magnesiums und berechneten Bikarbonats im Serum gefunden. In den folgenden Wochen kehrten die Werte des Chlorids, Phosphats, Kalium und Magnesium zu den Werten vor dem Übergang in die Höhe zurück. Der Calciumspiegel blieb dauernd erhöht, der Natriumspiegel fiel weiter ab, und der Proteinatspiegel stieg weiter an. Eine Verbesserung des Bikarbonatspiegels fand nicht statt. Zwei Wochen nach Rückkehr von der Höhe waren fast alle Elektrolytwerte wieder normal ausser Calcium Chlorid, Proteinat und Bikarbonat im Serum.

---

Resume Huit étudiantes de l'université du Missouri (230 m d'altitude) ont séjourné durant 65 jours à Pikes Peak (4.300 m d'altitude). Durant ce laps de temps, on a analysé régulièrement les électrolytes du sérum sanguin. Durant la première semaine de leur séjour en altitude, on a constaté une nette augmentation des chlorires, des phosphates, des protéinates et du calcium ainsi qu'une diminution marquée du sodium, de la potasse, du magnésium et de la valeur calculée du bicarbonate. Au cours des semaines suivantes, la valeur des chlorures, des phosphates, de la potasse et du magnésium s'est rétablie au niveau précédant la montée en altitude. Le taux de calcium est resté élevé alors que celui du sodium a continué de baisser et celui des protéinates à s'élever. On n'a pas constaté d'amélioration du taux de bicarbonate. Deux semaines après le retour en plaine, presque toutes les valeurs des électrolytes étaient redevenues normales dans le sérum, à l'exception de celles du chlorure de calcium, des proteinates et du bicarbonate.

     

Women at altitude: carbohydrate utilization during exercise at 4,300 m.

To evaluate the hypothesis that exposure to high altitude would reduce blood glucose and total carbohydrate utilization relative to sea level (SL), 16 young women were studied over four 12-day periods: at 50% of peak O(2) consumption in different menstrual cycle phases (SL-50), at 65% of peak O(2) consumption at SL (SL-65), and at 4,300 m (HA). After 10 days in each condition, blood glucose rate of disappearance (R(d)) and respiratory exchange ratio were measured at rest and during 45 min of exercise. Glucose R(d) during exercise at HA (4.71 +/- 0.30 mg. kg(-1). min(-1)) was not different from SL exercise at the same absolute intensity (SL-50 = 5.03 mg. kg(-1). min(-1)) but was lower at the same relative intensity (SL-65 = 6.22 mg. kg(-1). min(-1), P < 0.01). There were no differences, however, when glucose R(d) was corrected for energy expended (kcal/min) during exercise. Respiratory exchange ratios followed the same pattern, except carbohydrate oxidation remained lower (-23.2%, P < 0.01) at HA than at SL when corrected for energy expended. In women, unlike in men, carbohydrate utilization decreased at HA. Relative abundance of estrogen and progesterone in women may partially explain the sex differences in fuel utilization at HA, but subtle differences between menstrual cycle phases at SL had no physiologically relevant effects.     

Acclimatization to 4,300-m altitude decreases reliance on fat as a substrate

Roberts, A. C., G. E. Butterfield, A. Cymerman, J. T. Reeves, E. E. Wolfel, and G. A. Brooks. Acclimatization to 4,300-m altitude decreases reliance on fat as a substrate. J. Appl. Physiol. 81(4): 1762-1771, 1996.We testedthe hypothesis that exposure to altitude decreases reliance on freefatty acids (FFA) as substrates and increases dependency on bloodglucose. Therefore, the effects of exercise, hypobaric hypoxia, andaltitude acclimatization on FFA, glycerol and net glucose uptake andrelease [ = 2(leg blood flow)(arteriovenous concentration)]and on fatty acid (FA) consumption by the legs (= 3 × glycerolrelease + FFA uptake) were measured. Because sympathetic responses havebeen implicated, we utilized nonspecific -blockade and observedresponses to exercise, altitude, and altitude acclimatization. Westudied six healthy -blocked men () and five matched controls (C)during rest and cycle ergometry exercise (88 W) at 49% of sea-level(SL) peak O₂ uptake at the sameabsolute power output on acute altitude exposure (A1; barometric pressure = 430 Torr) and after 3 wk of chronic altitude exposure to4,300 m (A2). During exercise at SL, FA consumption rates increased (P < 0.05). On arrival at 4,300 m,resting leg FFA uptake and FA consumption rates were not significantlydifferent from those at SL. However, after acclimatization to altitude,at rest leg FA consumption decreased to essentially zero in both C and groups. During exercise at altitude after acclimatization, leg FAconsumption increased significantly, but values were less than at SL orA1 (P < 0.05), whereas glucoseuptake increased relative to SL values. Furthermore, -blockadesignificantly increased glucose uptake relative to control. We concludethat 1) chronic altitude exposure decreases leg FA consumption during rest and exercise;2) relative to SL, FFA uptakedecreases while glucose uptake increases during exercise at altitude;and 3) -blockade potentiatesthese effects.

     

Decreased exercise blood lactate concentrations after respiratory endurance training in humans

For many years, it was believed that ventilation does not limit performance in healthy humans. Recently, however, it has been shown that inspiratory muscles can become fatigued during intense endurance exercise and decrease their exercise performance. Therefore, it is not surprising that respiratory endurance training can prolong intense constant-intensity cycling exercise. To investigate the effects of respiratory endurance training on blood lactate concentration and oxygen consumption (VO2) during exercise and their relationship to performance, 20 healthy, active subjects underwent 30 min of voluntary, isocapnic hyperpnoea 5 days a week, for 4 weeks. Respiratory endurance tests, as well as incremental and constant-intensity exercise tests on a cycle ergometer, were performed before and after the 4-week period. Respiratory endurance increased from 4.6 (SD 2.5) to 29.1 (SD 4.0) min (P < 0.001) and cycling endurance time was prolonged from 20.9 (SD 5.5) to 26.6 (SD 11.8) min (P < 0.01) after respiratory training. The VO2 did not change at any exercise intensity whereas blood lactate concentration was lower at the end of the incremental [10.4 (SD 2.1) vs 8.8 (SD 1.9) mmol x l(-1), P < 0.001] as well as at the end of the endurance exercise [10.4 (SD 3.6) vs 9.6 (SD 2.7) mmol x l(-1), P < 0.01] test after respiratory training. We speculate that the reduction in blood lactate concentration was most likely caused by an improved lactate uptake by the trained respiratory muscles. However, reduced exercise blood lactate concentrations per se are unlikely to explain the improved cycling performance after respiratory endurance training.     

O2 extraction maintains O2 uptake during submaximal exercise with beta -adrenergic blockade at 4,300m

Wholebody O₂ uptake (O₂)during maximal and submaximal exercise has been shown to be preservedin the setting of -adrenergic blockade at high altitude, despitemarked reductions in heart rate during exercise. An increase in strokevolume at high altitude has been suggested as the mechanism thatpreserves systemic O₂ delivery (blood flow × arterialO₂ content) and thereby maintains O₂ at sea-level values. To test thishypothesis, we studied the effects of nonselective -adrenergicblockade on submaximal exercise performance in 11 normal men(26 ± 1 yr) at sea level and on arrival and after 21 days at 4,300 m. Six subjects received propranolol (240 mg/day), and five subjectsreceived placebo. At sea level, during submaximal exercise, cardiacoutput and O₂ delivery were significantly lower inpropranolol- than in placebo-treated subjects. Increases instroke volume and O₂ extraction were responsible for themaintenance of O₂. At 4,300 m,-adrenergic blockade had no significant effect onO₂, ventilation, alveolarPO₂, and arterial blood gases duringsubmaximal exercise. Despite increases in stroke volume, cardiac outputand thereby O₂ delivery were still reduced inpropranolol-treated subjects compared with subjects treated withplacebo. Further reductions in already low levels of mixed venousO₂ saturation were responsible for the maintenance ofO₂ on arrival and after 21 days at4,300 m in propranolol-treated subjects. Despite similarworkloads and O₂,propranolol-treated subjects exercised at greater perceived intensitythan subjects given placebo at 4,300 m. The values for mixed venousO₂ saturation during submaximal exercise inpropranolol-treated subjects at 4,300 m approached thosereported at simulated altitudes >8,000 m. Thus -adrenergicblockade at 4,300 m results in significant reduction in O₂delivery during submaximal exercise due to incomplete compensation bystroke volume for the reduction in exercise heart rate. Total bodyO₂ is maintained at a constant levelby an interaction between mixed venous O₂ saturation, thearterial O₂-carrying capacity, and hemodynamics duringexercise with acute and chronic hypoxia.

     

Disposal of lactate during and after strenuous exercise in humans

Heavy dynamic exercise using both arm and leg muscles was performed to exhaustion by seven well-trained subjects. The aerobic and anaerobic energy utilization was determined and/or calculated. O2 uptake during exercise and during 1 h of recovery was measured as well as splanchnic and muscle metabolite exchange. Glycogen and lactate content in the quadriceps femoris was determined before exercise, immediately after exercise, and after a recovery period. In four male subjects the estimated mean lactate production during exercise was 830 mmol. The splanchnic uptake of lactate during recovery was 80 mmol, and the calculated maximum amount oxidized during the recovery period was 330 mmol. About 60 mmol were accounted for in the body water at the end of the rest period. The remaining 360 mmol of lactate were apparently resynthesized into glycogen in muscle via gluconeogenesis. It is concluded that approximately 50% of the lactate formed during heavy exercise is transformed to glycogen via glyconeogenesis in muscle during recovery and that lactate uptake by the liver is only 10%.     

Effects of altitude acclimatization on pulmonary gas exchange during exercise

Pulmonary gas exchange was studied in eight normal subjects both before and after 2 wk of altitude acclimatization at 3,800 m (12,470 ft, barometric pressure = 484 Torr). Respiratory and multiple inert gas tensions, ventilation, cardiac output (Q), and hemoglobin concentration were measured at rest and during three levels of constant-load cycle exercise during both normoxia [inspired PO2 (PIO2) = 148 Torr] and normobaric hypoxia (PIO2 = 91 Torr). After acclimatization, the measured alveolar-arterial PO2 difference (A-aPO2) for any given work rate decreased (P less than 0.02). The largest reductions were observed during the highest work rates and were 24.8 +/- 1.4 to 19.7 +/- 0.8 Torr (normoxia) and 22.0 +/- 1.1 to 19.4 +/- 0.7 Torr (hypoxia). This could not be explained by changes in ventilation-perfusion inequality or estimated O2 diffusing capacity, which were unaffected by acclimatization. However, Q for any given work rate was significantly decreased (P less than 0.001) after acclimatization. We suggest that the reduction in A-aPO2 after acclimatization is a result of more nearly complete alveolar/end-capillary diffusion equilibration on the basis of a longer pulmonary capillary transit time.     

Effects of exercise training on acclimatization to hypoxia: systemic O2 transport during maximal exercise.

Acclimatization to hypoxia has minimal effect on maximal O2 uptake (Vo2 max). Prolonged hypoxia shows reductions in cardiac output (Q), maximal heart rate (HR-max), myocardial beta-adrenoceptor (beta-AR) density, and chronotropic response to isoproterenol. This study tested the hypothesis that exercise training (ET), which attenuates beta-AR downregulation, would increase HRmax and Q of acclimatization and result in higher Vo2 max. After 3 wk of ET, rats lived at an inspired Po2 of 70 Torr for 10 days (acclimatized trained rats) or remained in normoxia, while both groups continued to train in normoxia. Controls were sedentary acclimatized and nonacclimatized rats. All rats exercised maximally in normoxia and hypoxia (inspired Po2 of 70 Torr). Myocardial beta-AR density and the chronotropic response to isoproterenol were reduced, and myocardial cholinergic receptor density was increased after acclimatization; all of these receptor changes were reversed by ET. Normoxic Vo2 max (in ml.min-1.kg-1) was 95.8 +/- 1.0 in acclimatized trained (n = 6), 87.7 +/- 1.7 in nonacclimatized trained (P < 0.05, n = 6), 74.2 +/- 1.4 in acclimatized sedentary (n = 6, P < 0.05), and 72.5 +/- 1.2 in nonacclimatized sedentary (n = 8; P > 0.05 acclimatized sedentary vs. nonacclimatized sedentary). A similar distribution of Vo2 max values occurred in hypoxic exercise. Q was highest in trained acclimatized and nonacclimatized, intermediate in nonacclimatized sedentary, and lowest in acclimatized sedentary groups. ET preserved Q in acclimatized rats thanks to maintenance of HRmax as well as of maximal stroke volume. Q preservation, coupled with a higher arterial O2 content, resulted in the acclimatized trained rats having the highest convective O2 transport and Vo2 max. These results show that ET attenuates beta-AR downregulation and preserves Q and Vo2 max after acclimatization, and support the idea that beta-AR downregulation partially contributes to the limitation of Vo2 max after acclimatization in rats.