Shift of anaerobic to aerobic metabolism in the rats acclimatized to hypoxia

1. Metabolic acclimatization by repeated exposure to a simulated altitude of 4000, 5000 and 6000 m for 2 hr per day throughout 2 to 11 days was evaluated by the increased formation of ketone bodies as a marker of fatty acid oxidation and the decreased production of lactate and uric acid, the indicators of anaerobic metabolism in rats exposed to an altitude of 8000 m. 2. Pre-exposure of rats to an altitude of 5000 m and over caused an acclimatization to hypoxia. The rise of the altitude to which rats were pre-exposed reduced the period until the acquisition of metabolic acclimatization. 3. Acclimatized rats showed an increased activity of mitochondrial glutamate dehydrogenase without changes in glycolytic enzyme activity in skeletal muscle, heart and liver. 4. Acclimatization to high altitude hypoxia is concluded to involve a shift of the anaerobic glycolysis to aerobic metabolism by the increase in the oxidative enzymes.     

Effects of exercise on young and adult cattle at low and high altitude

Nine calves and nine oxen walked on a treadmill in a climatized low pressure chamber for one hour each day, 2 weeks at 400 m and 4 weeks at 3,500 m. The overall effects of walking were: increases in heart rate, pulmonary arterial pressure, rectal temperature, respiratory rate, blood-pH and lactate/pyruvate ratio. Haemoglobin, haematocrit, blood specific gravity and blood viscosity increased in the oxen but decreased in the calves. Blood lactate and blood pyruvate declined in both age groups, plasma viscosity only in the calves. The exercise effects were more pronounced at 3,500 m than at 400 m as exemplified by the following percentile differences (3,500-400 m): in heart rate 26%, mean pulmonary arterial pressure: 22%, respiratory rate: 11%, blood pH: 0.3%, blood lactate: 39%, blood pyruvate: 56%, haemoglobin: 4%, blood viscosity: 5%. Compared with the calves, the oxen experienced larger increases in heart rate and respiratory rate in response to exercise, suggesting a greater rise in metabolic rate: they also showed a more pronounced respiratory alkalosis. Thus, exercise seems to have strained the oxen more than the calves. In the oxen, there was a training effect as judged by reductions in exercising heart rate, respiratory rate and rectal temperature.     

Pulmonary hypertention,blood coagulation and aspirin treatment in high altitude exposed cattle

Six calves resident at 400 m altitude were exposed for 2 weeks to a simulated altitude of 4,500 m. This exposure produced the following changes: increases in heart rate (34 b/min), mean pulmonary arterial pressure (8 Torr), erythrocyte number (22%), haemoglobin (32%), haematocrit (34%), blood pH (0.037 units), leucocyte number (21%), blood clotting time (18%), and prothrombin time (7%). Decreases were found in thrombocyte number (8%) and clot retraction (22%). Orally administered acetylsalicylic acid (aspirin) over 14 days (90 mg/(kg.day)) had no effect on these responses to high altitude. The results provide further evidence against the involvement of prostaglandin as mediator in pulmonary hypertension.     

Effects of exposure to a simulated altitude of 3,500 m on calves and oxen

Nine calves and nine oxen were divided into 6 groups and exposed in a climatised low pressure chamber to the following conditions: 2 weeks at 400 m and 4 weeks at 3,500 m. High altitude produced the following changes: increases in heart rate and pulmonary artery pressure, both these changes being larger in the calves than in the oxen. During 4 weeks continuous exposure to 3,500 m, heart rate declined, whereas pulmonary arterial pressure rose. There were increments in respiratory rate, blood-pH, leucocyte number, rectal temperature, blood lactate and blood pyruvate, but no changes in the lactate/pyruvate ratio. Increases in erythrocyte number, haemoglobin, haematocrit, blood specific gravity and blood viscosity were more pronounced in the oxen than in the calves. Feed intake in all animals tended to be depressed in the first half of the high altitude periode. Water intake showed a fall during the first day at 3,500 m, but recovered thereafter. It is concluded that in response to high altitude the calves activated preferentially the circulatory, the oxen the erythropoetic system.     

Maximal oxygen uptake and erythropoietic responses after training at moderate altitude

Six well-trained male cross-county skiers trained for 7 days at 2700 m above sea level, their accommodation being at 1695 m. Blood samples for haemoglobin concentration [Hb], erythropoietin concentration [EPO] and reticulocyte count were collected before, during and after altitude exposure. Packed cell volume (PCV), red blood cell count (RBC), transferrin-iron saturation, mean red cell volume (MCV), mean corpuscular haemoglobin concentration (MCHC), maximal oxygen uptake, maximal achieved ventilation and heart rate were determined pre- and postaltitude exposure. The [EPO] increased significantly from pre-altitude (mean 36 mU.ml-1, SD 5) to maximal altitude values (mean 47 mU.ml-1, SD 3). The [Hb] had increased significantly above pre-altitude values (mean 8.8 mmol.l-1, SD 0.5) on day 2 (mean 9.1 mmol.l-1, SD 0.4) and day 7 (mean 9.4 mmol.l-1, SD 0.4) at altitude and on day 4 postaltitutde (mean 9.2 mmol.l-1, SD 0.4). The reticulocyte counts had increased significantly above pre-altitude values (mean 6%, SD 3%) on day 3 at altitude (mean 12%, SD 8%) and day 4 postaltitude (mean 10%, SD 5%). The RBC counts had increased on the 4th postaltitude day. The transferrin-iron saturation had decreased below pre-altitude values (mean 23%, SD 4%) on day 4 postaltitude (mean 14%, SD 5%) and had increased on day 11 postaltitude (mean 22%, SD 7%). There were no significant changes in MCV, MCHC, PCV, maximal oxygen uptake and maximal achieved ventilation, and heart rate pre- to postaltitude. These observations demonstrated an erythropoietic response to the altitude training which was not sufficient to increase the postaltitude maximal oxygen uptake.     

Body water metabolism in high altitude natives during and after a stay at sea level

Body fluid compartments were studied in a group of high altitude natives after a stay of two months at sea level and during 12 days at an altitude of 3,500 m. Measurements of total body water and extracellular water were made on day 3 and 12 of reinduction to altitude, while plasma volume was measured on day 12 only. The intracellular water, blood volume and red cell mass were computed from the above parameters. Total body water and intracellular water decreased by 3.3% (P<0.001) and 5.0% (P<0.001) respectively by the 3rd day at altitude and did not change thereafter. Extracellular water increased progressively at altitude, but the increase was not significant. Blood volume and red cell mass increased significantly while plasma volume decreased at altitude. These data were compared with that of low landers. This study suggested body hypohydration on high altitude induction in low landers as well as in high altitude natives on reinduction.     

Comparative study of acetazolamide and spironolactone on body fluid compartments on induction to high altitude

Studies were conducted on 29 male healthy subjects having no previous experience of living at high altitude. These subjects were divided into three groups, i.e., subjects treated with placebo, acetazolamide and spironolactone. These subjects were first studied in Delhi. The drug schedule was started 24 hour prior to the airlift of these subjects to an altitude of 3,500 m and was continued for 48 hour after arrival at high altitude. Total body water, extra cellular water, plasma volume, blood electrolytes, pH, pO₂, pCO₂ and blood viscosity were determined on 3rd and 12th day of their stay at high altitude. Total body water, extra cellular water intracellular water and plasma volume decreased on high altitude exposure. There was a further slight decrease in these compartments with acetazolamide and spironolactone. It was also observed that spironolactone drives out more water from the extracellular compartment. Loss of plasma water was also confirmed by increased plasma osmolality. Increase in arterial blood pH was noticed on hypoxic exposure but the increase was found less in acetazolamide and spironolactone cases. This decrease in pH is expected to result in better oxygen delivery to the tissues at the low oxygen tension. It was also confirmed because blood pO₂ increased in both the groups. No significant change in plasma electrolytes was observed in subjects of various groups. Blood viscosity slightly increased on exposure to high altitude. The degree of rise was found less in the group treated with spironolactone. This study suggests that both the drugs are likely to be beneficial in ameliorating/prevention of AMS syndrome.     

慢性高原低氧对高原鼠兔和大鼠肝脏的作用

我们曾经发现,移入高原的实验大鼠子一代和高原鼠兔(Ochotona curzoniae)对高原低气压低氧有完全不同的适应能力和适应机理(杜继曾等,1982)。我们还观察到,在24小时急性高原低氧时,由低地移入2300米高原的大鼠后裔在5000米和8000米的高度上,出现了以转氨酶、肝溶酶体酸性磷酸酶活力升高、肝糖原和蛋白质含量下降的肝脏代谢异常和肝脏病理变化,而高原鼠兔只是在8000米高度时,才始出现部分指标的轻度变异(杜继曾等,1982),从而揭示了高原鼠兔的肝细胞代谢在细胞水平上对低氧的适应机制优越于移入高原的实验大鼠后代。慢性低氧又如何作用于大鼠和高原鼠兔的肝脏代谢?迄今尚无人研究。因此对这一作用规律的认识和阐明,在环境适应生理学领域、人类高原活动和畜牧业生产上都是十分重要的。     

Plasma accumulation of hypoxanthine, uric acid and creatine kinase following exhausting runs of differing durations in man

During exhausting exercise adenylate kinase in the muscle cells is activated and a degradation of adenosine 5'-diphosphate occurs. Consequently, degradation products of adenosine 5'-monophosphate including hypoxanthine and uric acid, accumulate in plasma. The aim of this study was to compare the concentration changes of hypoxanthine and uric acid in plasma following running of varying duration and intensity. In addition, plasma creatine kinase activity was measured to assess the possible relationship between metabolic stress and protein release. Four groups of competitive male runners ran 100 m (n = 7), 800 m (n = 11), 5000 m (n = 7) and 42,000 m (n = 7), respectively, at an exhausting pace. Subsequent to the 100 m event (mean running time 11 s) plasma concentrations of hypoxanthine and uric acid increased by 364% and 36% respectively (P less than 0.05), indicating a very high rate of adenine nucleotide degradation during the event. Following the 800-m event (mean running time 125 s), hypoxanthine and uric acid concentrations had increased by 1598% and 66%, respectively (P less than 0.05). Both the events of longer duration, 5000 m and 42,000 m, also caused a significant increase in plasma concentration of hypoxanthine (742% and 237% respectively, P less than 0.05) and plasma uric acid (54% and 34% respectively, P less than 0.05). Plasma activities of creatine kinase were significantly increased at 24 h only following the 5000 m and 42,000 m events (64% and 1186% respectively, P less than 0.05). Changes in plasma creatine kinase activity showed no correlation with changes in plasma concentration of either hypoxanthine or uric acid for the 5000 m and 42,000 m events (r = 0.00-0.45, P greater than 0.05).     

Changes in the blood flow of the primary carotid and its branches during modifications of the O2 and CO2 composition of alveolar gas]

We measured common carotid blood flow using a range gated Doppler velocimeter, and internal and external blood velocities using a continuous Doppler in 20 lowlanders at sea level, under normal barometric pressure, in 10 subjects in an altitude chamber under a barometric pressure of 462 Torr (61.6 KPa) and then in 5 of them over a 3-weeks period at 3850 m of elevation (475 Torr = 63.3 KPa). The same measurements were also performed in 20 permanent residents at 3850 m. Common carotid blood flow was 15% higher in all subjects exposed to high altitude, due to a lowering in downstream resistances since systemic blood pressure did not change at high altitude. The increase in common carotid blood flow was the result of an immediate increase in internal carotid blood velocities observed in the altitude chamber as well as after the arrival at high altitude, but a few days later those velocities in the internal carotid artery declined to values similar to those observed at sea level. In the same time velocities in external carotid artery rose at high altitude, remained steadily elevated and the result is a permanent increase in common carotid blood flow at altitude. In all subjects we performed the same measurements, during an acute inhalation of gas mixtures to try to quantify the mechanisms controlling the changes in common carotid blood flow while changing gas inhalation. In the limits of the variations in PO2 (60 to 400 Torr) and in PCO2 (30 to 50 Torr) the stimulation by CO2 is twice more efficient than the O2 stimulation on vasomotion.     

江西官山常绿阔叶林土壤有机碳组分沿海拔的变化

对江西官山国家级自然保护区不同海拔(400、600、800、1000、1200 m)常绿阔叶林土壤总有机碳、惰性有机碳和活性有机碳进行分析,研究土壤有机碳的海拔分布特征。结果表明: 土壤总有机碳、惰性有机碳及活性有机碳含量在土壤表层最高,随土层加深而逐渐下降。随海拔升高,土壤总有机碳、惰性有机碳、易氧化有机碳、微生物生物量碳及0～20 cm土层土壤颗粒有机碳含量均出现先增后降的趋势, 且在海拔1000 m达到峰值,而土壤水溶性有机碳及20～40 cm土层土壤颗粒有机碳含量无明显变化。在0～10 cm土层,土壤惰性有机碳占总有机碳的比例在海拔800和1200 m显著高于海拔400和1000 m,而土壤活性有机碳占总有机碳的比例在海拔400 m最高;土壤惰性有机碳和活性有机碳占总有机碳的比例在10～40 cm土层随海拔的增加均呈先增加后降低的趋势,峰值分别在1000和600 m处。各组分有机碳与土壤湿度、微生物生物量氮、可溶性有机氮均呈显著正相关,而且活性有机碳与铵态氮呈显著正相关。海拔显著影响常绿阔叶林土壤有机碳组分的分布,惰性有机碳、易氧化有机碳和微生物生物量碳对海拔变化的响应更敏感。高海拔土壤惰性有机碳和活性有机碳在水分和氮素充足条件下易发生分解与转化,降低土壤碳库的稳定性。在全球气温持续升高背景下,要加强高海拔地区森林土壤有机碳的动态变化研究。     

Acute mountain sickness is not related to cerebral blood flow: a decompression chamber study.

To evaluate the pathogenetic role of cerebral blood flow (CBF) changes occurring before and during the development of acute mountain sickness (AMS), peak mean middle cerebral artery flow velocities () were assessed by transcranial Doppler sonography in 10 subjects at 490-m altitude, and during three 12-min periods immediately (SA1), 3 (SA2), and 6 (SA3) h after decompression to a simulated altitude of 4,559 m. AMS cerebral scores increased from 0. 16 +/- 0.14 at baseline to 0.44 +/- 0.31 at SA1, 1.11 +/- 0.88 at SA2 (P < 0.05), and 1.43 +/- 1.03 at SA3 (P < 0.01); correspondingly, three, seven, and eight subjects had AMS. Absolute and relative at simulated altitude, expressed as percentages of low-altitude values (%), did not correlate with AMS cerebral scores. Average % remained unchanged, because % increased in three and remained unchanged or decreased in seven subjects at SA2 and SA3. These results suggest that CBF is not important in the pathogenesis of AMS and shows substantial interindividual differences during the first hours at simulated altitude.     

Influence of exposure to moderate altitude on the plasma concentraton of cortisol, aldosterone, renin, testosterone, and gonadotropins

The influence of 11 days at moderate altitude (2,000 m) combined with exercise on plasma concentration of testosterone, FSH (follicle-stimulating hormone), LH (luteinizing hormone), cortisol, aldosterone, and renin activity was studied in ten healthy subjects. Within 48 h of arrival at moderate altitude a significant increase in testosterone was found whereas FSH had decreased significantly and LH showed a tendency to decrease. Cortisol increased significantly at the beginning and reached a maximum at the end of altitude exposure. The plasma aldosterone level rose continuously and on the last day of altitude was significantly elevated. Plasma renin activity showed a tendency to decrease. On return to low land all measured parameters returned to base line values within 2 days. The findings of increases in plasma levels of aldosterone and testosterone (and serum T3 and T4, as reported by others) are in contrast to the previously found decrease of urinary excretion of all these hormones. This appears to be a distinct dissociation of serum levels of adrenal (and thyroid) hormones from their urinary excretion. The observed increase in plasma aldosterone is probably mediated through ACTH and the rise in plasma potassium, since plasma renin activity showed an opposite trend. The rise in plasma testosterone is probably of adrenal origin since plasma gonadotropins declined simultaneously. The increase of plasma levels of glucocorticoids, mineralocorticoids, and androgens after an ascent from 600 m to 2,000 m above sea level is compatible with an ACTH-mediated stimulation of the entire adrenal cortex and/or a diminished elimination of adrenal steroids: The concomitant fall of FSH, LH, and plasma renin would then be a consequence of a direct negative feedback inhibition of these hormones.     

Effects of high altitude and water deprivation on arginine vasopressin release in men

High-altitude exposure changes the distribution of body water and electrolytes. Arginine vasopressin (AVP) may influence these alterations. The purpose of this study was to examine the effect of a 24-h water deprivation trial (WDT) on AVP release after differing altitude exposures. Seven healthy males (age 22 +/- 1 yr, height 176 +/- 2 cm, mass 75.3 +/- 1.8 kg) completed three WDTs: at sea level (SL), after acute altitude exposure (2 days) to 4,300 m (AA), and after prolonged altitude exposure (20 days) to 4,300 m (PA). Body mass, standing and supine blood pressures, plasma osmolality (Posm), and plasma AVP (PAVP) were measured at 0, 12, 16, and 24 h of each WDT. Urine volume was measured at each void throughout testing. Baseline Posm increased from SL to altitude (SL 291.7 +/- 0.8 mosmol/kgH2O, AA 299.6 +/- 2.2 mosmol/kgH2O, PA 302.3 +/- 1.5 mosmol/kgH2O, P < 0.05); however, baseline PAVP measurements were similar. Despite similar Posm values, the maximal PAVP response during the WDT (at 16 h) was greater at altitude than at SL (SL 1.7 +/- 0.5 pg/ml, AA 6.4 +/- 0.7 pg/ml, PA 8.7 +/- 0.9 pg/ml, P < 0.05). In conclusion, hypoxia appeared to alter AVP regulation by raising the osmotic threshold and increasing AVP responsiveness above that threshold.     

不同海拔地区藏族就诊人群血脂、血液黏度、HCY水平与心血管疾病的相关性研究

目的:探讨不同海拔地区藏族就诊人群血脂、血液黏度、HCY水平与心血管疾病的相关性。方法:采用回顾性分析的方法,将328例来自不同海拔地区的藏族就诊患者为三组,高海拔组(纳入99例),中海拔(纳入120例)和低海拔组(纳入109例),比较不同海拔高度组患者血压、血脂、血液黏度、HCY、疾病类型的差异,采用多元Logistic回归模型分析藏族就诊人群心血管疾病发病的影响因素。结果:不同海拔组收缩压、舒张压、血清HCY、TC、TG、HDL-C、LDL-C水平、全血黏度低切、中切、高切、血浆黏度和红细胞压积比较差异均有统计学意义(P0.05),随着海拔升高,收缩压、舒张压、血清HCY、TC、TG以及LDL-C、全血黏度低切、中切、高切、血浆黏度和红细胞压积水平显著升高(P0.05),而血清HDL-C水平显著下降。41.8%(137/328)的就诊者至少患有一种心血管疾病,和非心血管组比较,心血管疾病组年龄明显偏高,居住主要分布在中度及高度海拔地区,合并高血糖、高血脂、高HCY的比例均明显较高,差异均有统计学意义(P0.05)。年龄、海拔、高血糖、高血脂、高HCY均和心血管疾病相关(r=-0.230~0.334,P0.05)。多元Logistic回归分析显示年龄、居住地海拔、HCY水平、全血低切粘度、TG水平、LDL-C等因素是心血管疾病发生的危险因素,HDL-C是保护因素。结论:来自不同海拔地区的就诊人群在血压、血脂、血液黏度、HCY水平以及心血管疾病患者占比不同。年龄、居住地海拔、HCY水平、血液黏度、血脂水平等增加可能使高原藏族人群心血管疾病发生风险增加。     

Blood pressure and plasma catecholamines in acute and prolonged hypoxia: effects of local hypothermia.

This study measured the pressor and plasma catecholamine response to local hypothermia during adaptation to hypobaric hypoxia. Eight healthy men were studied at rest and after 10 and 45 min of local cooling of one hand and forearm as well as after 30 min of rewarming at sea level and again 24 h and 5 days after rapid, passive transport to high altitude (4,559 m). Acute mountain sickness scores ranged from 5 to 16 (maximal attainable score: 20) on the first day but were reduced to 0-8 by the fifth day. Systolic blood pressure, heart rate, and plasma epinephrine increased on day 1 at altitude compared with sea level but declined again on day 5, whereas diastolic and mean blood pressures continued to rise in parallel with plasma norepinephrine. With local cooling, an increased vasoactive response was seen on the fifth day at altitude. Very high pressures were obtained, and the pressure elevation was prolonged. Heart rate increased twice as much on day 5 compared with the other two occasions. Thoracic fluid index increased with cooling on day 5, suggesting an increase in pulmonary vascular resistance. In conclusion, prolonged hypoxia seems to elicit an augmented pressor response to local cooling in the systemic and most likely also the pulmonary circulation.     

Effects of a 12-day “live high, train low” camp on reticulocyte production and haemoglobin mass in elite female road cyclists

The aim of this study was to document the effect of "living high, training low" on the red blood cell production of elite female cyclists. Six members of the Australian National Women's road cycling squad slept for 12 nights at a simulated altitude of 2650 m in normobaric hypoxia (HIGH), while 6 team-mates slept at an altitude of 600 m (CONTROL). HIGH and CONTROL subjects trained and raced as a group throughout the 70-day study. Baseline levels of reticulocyte parameters sensitive to changes in erythropoeisis were measured 21 days and 1 day prior to sleeping in hypoxia (D1 and D20, respectively). These measures were repeated after 7 nights (D27) and 12 nights (D34) of simulated altitude exposure, and again 15 days (D48) and 33 days (D67) after leaving the altitude house. There was no increase in reticulocyte production, nor any change in reticulocyte parameters in either the HIGH or CONTROL groups. This lack of haematological response was substantiated by total haemoglobin mass measures (CO-rebreathing), which did not change when measured on D1, D20, D34 or D67. We conclude that in elite female road cyclists, 12 nights of exposure to normobaric hypoxia (2650 m) is not sufficient to either stimulate reticulocyte production or increase haemoglobin mass.     

Operation Everest II: elevated high-altitude pulmonary resistance unresponsive to oxygen

High altitude increases pulmonary arterial pressure (PAP), but no measurements have been made in humans above 4,500 m. Eight male athletic volunteers were decompressed in a hypobaric chamber for 40 days to a barometric pressure (PB) of 240 Torr, equivalent to the summit of Mt. Everest. Serial hemodynamic measurements were made at PB 760 (sea level), 347 (6,100 m), and 282/240 Torr (7,620/8,840 m). Resting PAP and pulmonary vascular resistance (PVR) increased from sea level to maximal values at PB 282 Torr from 15 +/- 0.9 to 34 +/- 3.0 mmHg and from 1.2 +/- 0.1 to 4.3 +/- 0.3 mmHg.l-1 X min, respectively. During near maximal exercise PAP increased from 33 +/- 1 mmHg at sea level to 54 +/- 2 mmHg at PB 282 Torr. Right atrial and wedge pressures were not increased with altitude. Acute 100% O2 breathing lowered cardiac output and PAP but not PVR. Systemic arterial pressure and resistance did not rise with altitude but did increase with O2 breathing, indicating systemic control differed from the lung circulation. We concluded that severe chronic hypoxia caused elevated pulmonary resistance not accompanied by right heart failure nor immediately reversed by O2 breathing.     

After effects of chronic hypoxia on cardiac output and muscle blood flow at rest and exercise

Cardiac output (Q, by N2-CO2 rebreathing) and limb muscle blood flow (qm, from 133Xe clearance) were determined in eight male subjects at rest and during cycloergometric loads immediately before and 12 days after return from the 1981 Swiss Lhotse Shar (8,398 m) Expedition. Compared to control conditions, after exposure to hypoxia: 1) Q was unchanged at rest and at 75 watts (W) but was 18% less (P less than 0.01) at 150 W with constant heart rate (approximately 140 beats X min-1); 2) qm in the vastus lateralis was identical at rest but 26% and 39% less (P less than 0.05 and P less than 0.001, respectively) at two submaximal leg work loads (75 and 125 W); 3) qm in the biceps at 50 W was 34% less (P less than 0.01); 4) hemoglobin flow (QHb and qmHb), similarly to blood flow (Q and qm), was significantly reduced; 5) the qm adjustment rate, measured from the time required to attain a new steady state upon a square wave change of work load starting from rest, was slower, particularly at the lower work loads. From the above results as well as from corresponding morphometric findings showing in the same subjects: 1) a decrease of the ratio between fiber section and number of capillaries and 2) a rise of the mitochondrial to fiber volume ratio, it is concluded that during altitude acclimatization peripheral O2 delivery becomes more efficient.     

Women at altitude: energy requirement at 4,300 m.

To test the hypotheses that prolonged exposure to moderately high altitude increases the energy requirement of adequately fed women and that the sole cause of the increase is an elevation in basal metabolic rate (BMR), we studied 16 healthy women [21.7 +/- 0.5 (SD) yr; 167.4 +/- 1.1 cm; 62.2 +/- 1.0 kg]. Studies were conducted over 12 days at sea level (SL) and at 4,300 m [high altitude (HA)]. To test that menstrual cycle phase has an effect on energetics at HA, we monitored menstrual cycle in all women, and most women (n = 11) were studied in the same phase at SL and HA. Daily energy intake at HA was increased to respond to increases in BMR and to maintain body weight and body composition. Mean BMR for the group rose 6.9% above SL by day 3 at HA and fell to SL values by day 6. Total energy requirement remained elevated 6% at HA [ approximately 670 kJ/day (160 kcal/day) above that at SL], but the small and transient increase in BMR could not explain all of this increase, giving rise to an apparent "energy requirement excess." The transient nature of the rise in BMR may have been due to the fitness level of the subjects. The response to altitude was not affected by menstrual cycle phase. The energy requirement excess is at present unexplained.