Selected contribution: Peripheral chemoreflex function in high-altitude natives and patients with chronic mountain sickness.

Peripheral chemoreflex function was studied in high-altitude (HA) natives at HA, in patients with chronic mountain sickness (CMS) at HA, and in sea-level (SL) natives at SL. Results were as follows. 1) Acute ventilatory responses to hypoxia (AHVR) in the HA and CMS groups were approximately one-third of those of the SL group. 2) In CMS patients, some indexes of AHVR were modestly, but significantly, lower than in healthy HA natives. 3) Prior oxygenation increased AHVR in all subject groups. 4) Neither low-dose dopamine nor somatostatin suppressed any component of ventilation that could not be suppressed by acute hyperoxia. 5) In all subject groups, the ventilatory response to hyperoxia was biphasic. Initially, ventilation fell but subsequently rose so that, by 20 min, ventilation was higher in hyperoxia than hypoxia for both HA and CMS subjects. 6) Peripheral chemoreflex stimulation of ventilation was modestly greater in HA and CMS subjects at an end-tidal Po(2) = 52.5 Torr than in SL natives at an end-tidal Po(2) = 100 Torr. 7) For the HA and CMS subjects combined, there was a strong correlation between end-tidal Pco(2) and hematocrit, which persisted after controlling for AHVR.     

Selected contribution: Acute and sustained ventilatory responses to hypoxia in high-altitude natives living at sea level.

High-altitude (HA) natives have blunted ventilatory responses to hypoxia (HVR), but studies differ as to whether this blunting is lost when HA natives migrate to live at sea level (SL), possibly because HVR has been assessed with different durations of hypoxic exposure (acute vs. sustained). To investigate this, 50 HA natives (>3,500 m, for >20 yr) now resident at SL were compared with 50 SL natives as controls. Isocapnic HVR was assessed by using two protocols: protocol 1, progressive stepwise induction of hypoxia over 5-6 min; and protocol 2, sustained (20-min) hypoxia (end-tidal Po(2) = 50 Torr). Acute HVR was assessed from both protocols, and sustained HVR from protocol 2. For HA natives, acute HVR was 79% [95% confidence interval (CI): 52-106%, P = not significant] of SL controls for protocol 1 and 74% (95% CI: 52-96%, P < 0.05) for protocol 2. By contrast, sustained HVR after 20-min hypoxia was only 30% (95% CI: -7-67%, P < 0.001) of SL control values. The persistent blunting of HVR of HA natives resident at SL is substantially less to acute than to sustained hypoxia, when hypoxic ventilatory depression can develop.     

Selected contribution: Ventilatory response to CO2 in high-altitude natives and patients with chronic mountain sickness.

The ventilatory responses to CO(2) of high-altitude (HA) natives and patients with chronic mountain sickness (CMS) were studied and compared with sea-level (SL) natives living at SL. A multifrequency binary sequence (MFBS) in end-tidal Pco(2) was employed to separate the fast (peripheral) and slow (central) components of the chemoreflex response. MFBS was imposed against a background of both euoxia (end-tidal Po(2) of 100 Torr) and hypoxia (52.5 Torr). Both total and central chemoreflex sensitivity to CO(2) in euoxia were higher in HA and CMS subjects compared with SL subjects. Peripheral chemoreflex sensitivity to CO(2) in euoxia was higher in HA subjects than in SL subjects. Hypoxia induced a greater increase in total chemoreflex sensitivity to CO(2) in SL subjects than in HA and CMS subjects, but peripheral chemoreflex sensitivity to CO(2) in hypoxia was no greater in SL subjects than in HA and CMS subjects. Values for the slow (central) time constant were significantly greater for HA and CMS subjects than for SL subjects.     

Alveolar PCO2 and PO2 of high-altitude natives living at sea level

León-Velarde, Fabiola, Manuel Vargas, Carlos Monge-C.,Robert W. Torrance, and Peter A. Robbins. AlveolarPCO₂ andPO₂ of high-altitude natives livingat sea level. J. Appl.Physiol. 81(4): 1605-1609, 1996.Thisstudy was designed to determine whether subjects born at high altitude(HA; 2,000 m or above) who subsequently move to near sea level (SL)develop end-tidal PCO₂(PET_CO2) andPO₂(PET_O2) valuesthat equal those of SL natives living near SL. A total of 108 male HAnatives living near SL were identified by survey of a district in Lima,Peru, and a further 108 male SL natives from the same district wereidentified as control subjects. Of these subjects, satisfactory datafor inclusion in the study were obtained from 93 HA and 82 SL subjects.Mean PET_CO2 and PET_O2 values were 37.7 ± 2.5 (SD) and 104.7 ± 3.2 Torr, respectively, in HA subjects and37.7 ± 2.2 and 104.8 ± 3.0 Torr, respectively, in SL subjects.The average difference between SL natives and HA natives forPET_CO2 was 0.07 Torr(0.64 to 0.78; 95% confidence interval) and forPET_O2 was 0.05 Torr(0.89 to 0.99, 95% confidence interval). The average age andweight of the SL and HA subjects did not differ, but the HA subjectswere shorter and tended to have larger vital capacities, consistentwith their origin at HA. We conclude that thePET_CO2 andPET_O2 near SL of SL nativesand HA natives do not differ.

     

Changes in respiratory control in humans induced by 8 h of hyperoxia.

In humans, 8 h of isocapnic hypoxia causes a progressive rise in ventilation associated with increases in the acute ventilatory responses to hypoxia (AHVR) and hypercapnia (AHCVR). To determine whether 8 h of hyperoxia causes the converse of these effects, three 8-h protocols were compared in 14 subjects: 1) poikilocapnic hyperoxia, with end-tidal PO(2) (PET(O(2))) = 300 Torr and end-tidal PCO(2) (PET(CO(2))) uncontrolled; 2) isocapnic hyperoxia, with PET(O(2)) = 300 Torr and PET(CO(2)) maintained at the subject's normal air-breathing level; and 3) control. Ventilation was measured hourly. AHVR and AHCVR were determined before and 0.5 h after each exposure. During isocapnic hyperoxia, after an initial increase, ventilation progressively declined (P < 0.01, ANOVA). After exposure to hyperoxia, 1) AHVR declined (P < 0.05); 2) ventilation at fixed PET(CO(2)) decreased (P < 0.05); and 3) air-breathing PET(CO(2)) increased (P < 0.05); but 4) no significant changes in AHCVR or intercept were demonstrated. In conclusion, 8 h of hyperoxia have some effects opposite to those found with 8 h of hypoxia, indicating that there may be some "acclimatization to hypoxia" at normal sea-level values of PO(2).     

成人急性低氧通气压抑中的内啡肽作用

本工作设想,内啡肽参与了成人急性低氧通气压抑机制。受试者均为健康成年男子。6名受试者吸入中度低氧混合气(12.8％O_2)30min;7名吸入重度低氧混合气(10.8％O_2)20min,其中6名并在重度低氧下吸入三口纯氮气。吸入低氧气前先由静脉注入生理盐水(对照)或纳洛酮(中度低氧5mg,重度低氧10mg)。观察低氧时的通气反应、终末潮气二氧化碳分压(P_(ETCO2)、动脉血氧饱和度和外周低氧通气敏感性以及纳洛酮对上述测定的影响。结果表明,纳洛酮使重度低氧下的通气压抑明显减弱,低氧第3～15分钟的通气水平明显高于对照实验;而P_(ETCO2)明显低于对照值。但纳洛酮对中度低氧下的通气压抑无明显作用。此外,纳洛酮显著增强外周低氧敏感性。结果提示,在重度低氧下,内啡肽参与了成人低氧通气压抑机制,并对外周低氧敏感性有抑制作用。     

Effect of repeated normobaric hypoxia exposures during sleep on acute mountain sickness, exercise performance, and sleep during exposure to terrestrial altitude

There is an expectation that repeated daily exposures to normobaric hypoxia (NH) will induce ventilatory acclimatization and lessen acute mountain sickness (AMS) and the exercise performance decrement during subsequent hypobaric hypoxia (HH) exposure. However, this notion has not been tested objectively. Healthy, unacclimatized sea-level (SL) residents slept for 7.5 h each night for 7 consecutive nights in hypoxia rooms under NH [n = 14, 24 ± 5 (SD) yr] or "sham" (n = 9, 25 ± 6 yr) conditions. The ambient percent O(2) for the NH group was progressively reduced by 0.3% [150 m equivalent (equiv)] each night from 16.2% (2,200 m equiv) on night 1 to 14.4% (3,100 m equiv) on night 7, while that for the ventilatory- and exercise-matched sham group remained at 20.9%. Beginning at 25 h after sham or NH treatment, all subjects ascended and lived for 5 days at HH (4,300 m). End-tidal Pco(2), O(2) saturation (Sa(O(2))), AMS, and heart rate were measured repeatedly during daytime rest, sleep, or exercise (11.3-km treadmill time trial). From pre- to posttreatment at SL, resting end-tidal Pco(2) decreased (P < 0.01) for the NH (from 39 ± 3 to 35 ± 3 mmHg), but not for the sham (from 39 ± 2 to 38 ± 3 mmHg), group. Throughout HH, only sleep Sa(O(2)) was higher (80 ± 1 vs. 76 ± 1%, P < 0.05) and only AMS upon awakening was lower (0.34 ± 0.12 vs. 0.83 ± 0.14, P < 0.02) in the NH than the sham group; no other between-group rest, sleep, or exercise differences were observed at HH. These results indicate that the ventilatory acclimatization induced by NH sleep was primarily expressed during HH sleep. Under HH conditions, the higher sleep Sa(O(2)) may have contributed to a lessening of AMS upon awakening but had no impact on AMS or exercise performance for the remainder of each day.     

Ancestry explains the blunted ventilatory response to sustained hypoxia and lower exercise ventilation of Quechua altitude natives

Andean high-altitude (HA) natives have a low (blunted) hypoxic ventilatory response (HVR), lower effective alveolar ventilation, and lower ventilation (VE) at rest and during exercise compared with acclimatized newcomers to HA. Despite blunted chemosensitivity and hypoventilation, Andeans maintain comparable arterial O(2) saturation (Sa(O(2))). This study was designed to evaluate the influence of ancestry on these trait differences. At sea level, we measured the HVR in both acute (HVR-A) and sustained (HVR-S) hypoxia in a sample of 32 male Peruvians of mainly Quechua and Spanish origins who were born and raised at sea level. We also measured resting and exercise VE after 10-12 h of exposure to altitude at 4,338 m. Native American ancestry proportion (NAAP) was assessed for each individual using a panel of 80 ancestry-informative molecular markers (AIMs). NAAP was inversely related to HVR-S after 10 min of isocapnic hypoxia (r = -0.36, P = 0.04) but was not associated with HVR-A. In addition, NAAP was inversely related to exercise VE (r = -0.50, P = 0.005) and ventilatory equivalent (VE/Vo(2), r = -0.51, P = 0.004) measured at 4,338 m. Thus Quechua ancestry may partly explain the well-known blunted HVR (10, 35, 36, 57, 62) at least to sustained hypoxia, and the relative exercise hypoventilation at altitude of Andeans compared with European controls. Lower HVR-S and exercise VE could reflect improved gas exchange and/or attenuated chemoreflex sensitivity with increasing NAAP. On the basis of these ancestry associations and on the fact that developmental effects were completely controlled by study design, we suggest both a genetic basis and an evolutionary origin for these traits in Quechua.     

Hypoxic and hypercapnic drives to breathe generate equivalent levels of air hunger in humans.

Anecdotal observations suggest that hypoxia does not elicit dyspnea. An opposing view is that any stimulus to medullary respiratory centers generates dyspnea via "corollary discharge" to higher centers; absence of dyspnea during low inspired Po(2) may result from increased ventilation and hypocapnia. We hypothesized that, with fixed ventilation, hypoxia and hypercapnia generate equal dyspnea when matched by ventilatory drive. Steady-state levels of hypoxic normocapnia (end-tidal Po(2) = 60-40 Torr) and hypercapnic hyperoxia (end-tidal Pco(2) = 40-50 Torr) were induced in naive subjects when they were free breathing and during fixed mechanical ventilation. In a separate experiment, normocapnic hypoxia and normoxic hypercapnia, "matched" by ventilation in free-breathing trials, were presented to experienced subjects breathing with constrained rate and tidal volume. "Air hunger" was rated every 30 s on a visual analog scale. Air hunger-Pet(O(2)) curves rose sharply at Pet(O(2)) <50 Torr. Air hunger was not different between matched stimuli (P > 0.05). Hypercapnia had unpleasant nonrespiratory effects but was otherwise perceptually indistinguishable from hypoxia. We conclude that hypoxia and hypercapnia have equal potency for air hunger when matched by ventilatory drive. Air hunger may, therefore, arise via brain stem respiratory drive.     

Ventilatory acclimatization in response to very small changes in PO2 in humans.

Ventilatory acclimatization to hypoxia (VAH) consists of a progressive increase in ventilation and decrease in end-tidal Pco(2) (Pet(CO(2))). Underlying VAH, there are also increases in the acute ventilatory sensitivities to hypoxia and hypercapnia. To investigate whether these changes could be induced with very mild alterations in end-tidal Po(2) (Pet(O(2))), two 5-day exposures were compared: 1) mild hypoxia, with Pet(O(2)) held at 10 Torr below the subject's normal value; and 2) mild hyperoxia, with Pet(O(2)) held at 10 Torr above the subject's normal value. During both exposures, Pet(CO(2)) was uncontrolled. For each exposure, the entire protocol required measurements on 13 consecutive mornings: 3 mornings before the hypoxic or hyperoxic exposure, 5 mornings during the exposure, and 5 mornings postexposure. After the subjects breathed room air for at least 30 min, measurements were made of Pet(CO(2)), Pet(O(2)), and the acute ventilatory sensitivities to hypoxia and hypercapnia. Ten subjects completed both protocols. There was a significant increase in the acute ventilatory sensitivity to hypoxia (Gp) after exposure to mild hypoxia, and a significant decrease in Gp after exposure to mild hyperoxia (P < 0.05, repeated-measures ANOVA). No other variables were affected by mild hypoxia or hyperoxia. The results, when combined with those from other studies, suggest that Gp varies linearly with Pet(O(2)), with a sensitivity of 3.5%/Torr (SE 1.0). This sensitivity is sufficient to suggest that Gp is continuously varying in response to normal physiological fluctuations in Pet(O(2)). We conclude that at least some of the mechanisms underlying VAH may have a physiological role at sea level.     

Regulation of breathing in newborns at high altitude

Resting respiratory parameters and respiratory responses to acute changes in end-tidal O2 and CO2 pressure (PETO2 and PETCO2) were investigated in Peru in 23 newborn and 4 older infants at 3.850 m and in 13 newborns at 800 m. The study was done with the subjects asleep in a thermoneutral environment. The transient increase in ventilation in both high- and low-altitude newborns was followed by a decrease in response to acute hypoxia. During hyperoxia the two groups showed a slight but not clearly significant decrease in ventilation, whereas older high-altitude infants showed a sustained decrease. All subjects showed a prompt and clear response to CO2 inhalation during hyperoxia. We conclude that ventilatory peripheral chemoreflex is not fully developed in newborns regardless of altitude. The weak link in the reflex arc may reside in the afferent component because CO2 response was not impaired. Since hypoxic response became persistent in older infants its blunting in adult high-altitude natives is not a legacy of newborns.     

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.     

Low acute hypoxic ventilatory response and hypoxic depression in acute altitude sickness

Persons with acute altitude sickness hypoventilate at high altitude compared with persons without symptoms. We hypothesized that their hypoventilation was due to low initial hypoxic ventilatory responsiveness, combined with subsequent blunting of ventilation by hypocapnia and/or prolonged hypoxia. To test this hypothesis, we compared eight subjects with histories of acute altitude sickness with four subjects who had been asymptomatic during prior altitude exposure. At a simulated altitude of 4,800 m, the eight susceptible subjects developed symptoms of altitude sickness and had lower minute ventilations and higher end-tidal PCO2's than the four asymptomatic subjects. In measurements made prior to altitude exposure, ventilatory responsiveness to acute hypoxia was reduced in symptomatic compared to asymptomatic subjects, both when measured under isocapnic and poikolocapnic (no added CO2) conditions. Diminution of the poikilocapnic relative to the isocapnic hypoxic response was similar in the two groups. Ventilation fell, and end-tidal PCO2 rose in both groups during 30 min of steady-state hypoxia relative to values observed acutely. After 4.5 h at 4,800 m, ventilation was lower than values observed acutely at the same arterial O2 saturation. The reduction in ventilation in relation to the hypoxemia present was greater in symptomatic than in asymptomatic persons. Thus the hypoventilation in symptomatic compared to asymptomatic subjects was attributable both to a lower acute hypoxic response and a subsequent greater blunting of ventilation at high altitude.     

Time course of air hunger mirrors the biphasic ventilatory response to hypoxia.

Determining response dynamics of hypoxic air hunger may provide information of use in clinical practice and will improve understanding of basic dyspnea mechanisms. It is hypothesized that air hunger arises from projection of reflex brain stem ventilatory drive ("corollary discharge") to forebrain centers. If perceptual response dynamics are unmodified by events between brain stem and cortical awareness, this hypothesis predicts that air hunger will exactly track ventilatory response. Thus, during sustained hypoxia, initial increase in air hunger would be followed by a progressive decline reflecting biphasic reflex ventilatory drive. To test this prediction, we applied a sharp-onset 20-min step of normocapnic hypoxia and compared dynamic response characteristics of air hunger with that of ventilation in 10 healthy subjects. Air hunger was measured during mechanical ventilation (minute ventilation = 9 +/- 1.4 l/min; end-tidal Pco(2) = 37 +/- 2 Torr; end-tidal Po(2) = 45 +/- 7 Torr); ventilatory response was measured during separate free-breathing trials in the same subjects. Discomfort caused by "urge to breathe" was rated every 30 s on a visual analog scale. Both ventilatory and air hunger responses were modeled as delayed double exponentials corresponding to a simple linear first-order response but with a separate first-order adaptation. These models provided adequate fits to both ventilatory and air hunger data (r(2) = 0.88 and 0.66). Mean time constant and time-to-peak response for the average perceptual response (0.36 min(-1) and 3.3 min, respectively) closely matched corresponding values for the average ventilatory response (0.39 min(-1) and 3.1 min). Air hunger response to sustained hypoxia tracked ventilatory drive with a delay of approximately 30 s. Our data provide further support for the corollary discharge hypothesis for air hunger.     

Methodological and physiological variability within the ventilatory response to hypoxia in humans.

Measurement of the acute hypoxic ventilatory response (AHVR) requires careful choice of the hypoxic stimulus. If the stimulus is too brief, the response may be incomplete; if the stimulus is too long, hypoxic ventilatory depression may ensue. The purpose of this study was to compare three different techniques for assessing AHVR, using different hypoxic stimuli, and also to examine the between-day variability in AHVR. Ten subjects were studied, each on six different occasions, which were >/=1 wk apart. On each occasion, AHVR was assessed using three different protocols: 1) protocol SW, which uses square waves of hypoxia; 2) protocol IS, which uses incremental steps of hypoxia; and 3) protocol RB, which simulates an isocapnic rebreathing test. Mean values for hypoxic sensitivity were 1.02 +/- 0.48, 1.15 +/- 0.55, and 0.93 +/- 0.60 (SD) l. min(-1). %(-1) for protocols SW, IS, and RB, respectively. These differed significantly (P < 0.01). The coefficients of variation for measurement of AHVR were 20, 23, and 36% for the three protocols, respectively. These were not significantly different. There was a significant physiological variation in AHVR (F (50,100) = 3.9, P < 0. 001), with a coefficient of variation of 26%. We conclude that there was relatively little systematic variation between the three protocols but that AHVR varies physiologically over time.     

Changes in respiratory control during and after 48h of isocapnic and poikilocapnic hypoxia in humans

Ventilatory acclimatization tohypoxia is associated with an increase in ventilation under conditionsof acute hyperoxia(E_hyperoxia) and an increase in acute hypoxic ventilatory response (AHVR). Thisstudy compares 48-h exposures to isocapnic hypoxia( protocol I) with 48-hexposures to poikilocapnic hypoxia ( protocolP) in 10 subjects to assess the importance ofhypocapnic alkalosis in generating the changes observed in ventilatoryacclimatization to hypoxia. During both hypoxic exposures,end-tidal PO₂ was maintained at60 Torr, with end-tidal PCO₂ held at the subject's prehypoxic level( protocol I) or uncontrolled( protocol P).E_hyperoxiaand AHVR were assessed regularly throughout the exposures.E_hyperoxia(P < 0.001, ANOVA) and AHVR(P < 0.001) increased during thehypoxic exposures, with no significant differences betweenprotocols I andP. The increase inE_hyperoxiawas associated with an increase in slope of theventilation-end-tidal PCO₂ response(P < 0.001) with no significantchange in intercept. These results suggest that changes in respiratorycontrol early in ventilatory acclimatization to hypoxiaresult from the effects of hypoxia per se and not the alkalosisnormally accompanying hypoxia.

     

Gender differentiation of the chemoreflex during growth at high altitude: functional and neurochemical studies

The effect of chronic hypoxia on gender differences in physiology and neurochemistry of chemosensory pathways was studied in prepubertal and adult rats living at sea level (SL; Lyon, France) or at high altitude (HA; La Paz, Bolivia, 3,600 m). HA adult rats had higher hematocrit (Ht%), Hb concentration, resting ventilatory rate (Ve(100)), and higher tyrosine hydroxylase (TH) activity in carotid bodies (CB) than SL animals. At HA and SL, adult females had lower Ht% (46.0 +/- 0.8 vs. 50.4 +/- 0.6% at HA, P < 0.05 and 43.8 +/- 0.9 vs. 47.1 +/- 0.8% at SL, P < 0.05) and Hb (16.1 +/- 0.3 vs. 17.7 +/- 0.2 g/dl at HA, P < 0.05 and 14.5 +/- 0.3 vs. 15.6 +/- 0.1 g/dl at SL, P < 0.05) than males. Females had higher Ve(100) [170 +/- 19 vs. 109 +/- 7 ml. min(-1). 100 g(-1) at HA, P < 0.05 and 50 +/- 3 vs. 40 +/- 2 ml. min(-1). 100 g(-1) at SL, not significant (NS)] and lower CB-TH activity (1.40 +/- 0.2 vs. 3.87 +/- 0.6 pmol/20 min at HA, P < 0.05 and 0.52 +/- 0.1 vs. 0.68 +/- 0.1 pmol/20 min at SL; NS) than males at HA only. The onset of hypoxic ventilatory response during development was delayed at HA. Prepubertal HA females had higher Ve(100) than males (2 wk old, +47%) and higher CB-TH activity (3 wk old, +51%). Medullary noradrenergic groups were sex dimorphic during development at SL. Rats raised at HA had a drop of TH activity between the second and the third postnatal week in all medullary groups. In conclusion, our data support the hypothesis that the CB is the major site for sexual differentiation of the ventilatory control. Ventilatory differences appeared before puberty, and the animals bred at HA had profound alterations in the developmental process of the chemoreflex and its neural pathways. Some of these alterations are under dependence of the sex of the animal, and there is an important interaction between gender and the hypoxic environmental condition during the developmental period.     

Effects of a 1-yr stay at altitude on ventilation, metabolism, and work capacity.

The hypoxic and hypercapnic ventilatory drive, gas exchange, blood lactate and pyruvate concentrations, acid-base balance, and physical working capacity were determined in three groups of healthy males: 17 residents examined at sea level (group I), 24 sea-level natives residing at 1,680-m altitude for 1 yr and examined there (group II), and 17 sea-level natives residing at 3,650-m altitude for 1 yr and examined there (group III). The piecewise linear approximation technique was used to study the ventilatory response curves, which allowed a separate analysis of slopes during the first phase of slow increase in ventilation and the second phase of sharp increase. The hypoxic ventilatory response for both isocapnic and poikilocapnic conditions was greater in group II and even greater in group III. The first signs of consciousness distortion in sea-level residents appeared at an end-tidal O2 pressure level (4.09 +/- 0.56 kPa) higher than that of temporary residents of middle (3.05 +/- 0.12) and high altitude (2.90 +/- 0.07). The hypercapnic response was also increased, although to a lesser degree. Subjects with the highest hypoxic respiratory sensitivity at high altitude demonstrated greater O2 consumption at rest, greater ventilatory response to exercise, higher physical capacity, and a less pronounced anaerobic glycolytic flux but a lower tolerance to extreme hypoxia. That is, end-tidal O2 pressure that caused a distortion of the consciousness was higher in these subjects than in those with lower hypoxic sensitivity. Two extreme types of adaptation strategy can be distinguished: active, with marked reactions of "struggle for oxygen," and passive, with reduced O2 metabolism, as well as several intermediate types.(ABSTRACT TRUNCATED AT 250 WORDS)     

Ventilation and hypoxic ventilatory response of Tibetan and Aymara high altitude natives

Newcomers acclimatizing to high altitude and adult male Tibetan high altitude natives have increased ventilation relative to sea level natives at sea level. However, Andean and Rocky Mountain high altitude natives have an intermediate level of ventilation lower than that of newcomers and Tibetan high altitude natives although generally higher than that of sea level natives at sea level. Because the reason for the relative hypoventilation of some high altitude native populations was unknown, a study was designed to describe ventilation from adolescence through old age in samples of Tibetan and Andean high altitude natives and to estimate the relative genetic and environmental influences. This paper compares resting ventilation and hypoxic ventilatory response (HVR) of 320 Tibetans 9–82 years of age and 542 Bolivian Aymara 13–94 years of age, native residents at 3,800–4,065 m. Tibetan resting ventilation was roughly 1.5 times higher and Tibetan HVR was roughly double that of Aymara. Greater duration of hypoxia (older age) was not an important source of variation in resting ventilation or HVR in either sample. That is, contrary to previous studies, neither sample acquired hypoventilation in the age ranges under study. Within populations, greater severity of hypoxia (lower percent of oxygen saturation of arterial hemoglobin) was associated with slightly higher resting ventilation among Tibetans and lower resting ventilation and HVR among Aymara women, although the associations accounted for just 2–7% of the variation. Between populations, the Tibetan sample was more hypoxic and had higher resting ventilation and HVR. Other systematic environmental contrasts did not appear to elevate Tibetan or depress Aymara ventilation. There was more intrapopulation genetic variation in these traits in the Tibetan than the Aymara sample. Thirty-five percent of the Tibetan, but none of the Aymara, resting ventilation variance was due to genetic differences among individuals. Thirty-one percent of the Tibetan HVR, but just 21% of the Aymara, HVR variance was due to genetic differences among individuals. Thus there is greater potential for evolutionary change in these traits in the Tibetans. Presently, there are two different ventilation phenotypes among high altitude natives as compared with sea level populations at sea level: lifelong sustained high resting ventilation and a moderate HVR among Tibetans in contrast with a slightly elevated resting ventilation and a low HVR among Aymara. Am J Phys Anthropol 104:427–447, 1997. © 1997 Wiley-Liss, Inc.