Overall and regional lung function in Andean natives after descent to low altitude.

Overall lung volumes, regional residual volume to total lung capacity ratio (RVr/TLCr), regional ventilation (V/V) and perfusion (Q/V) were measured at 670 m in six Quechua Indians on days 2 and 37 after leaving their high-altitude homes (3500-4500 m). On day 2 the lung volumes averaged between 124 and 137% of those predicted for low-altitude residents (LAR) and there were no significant changes on day 37. Although overall RV/TLC was not different from the predicted value for LAR, RVr/TLCr on day 2 was higher at the top and lower at the bottom of the lungs compared to LAR. Regional Q/V and V/V were not different from LAR on day 2, or on day 37. However, the ratio of Q/V at the bottom to Q/V at the top was 2.36 on day 2 and 2.84 on day 37 (P less than 0.05). On day 2 hemoglobin- and volume-corrected diffusing capacity was 145% of the value predicted for LAR and this fell to 135% predicted on day 37 (P less than 0.05). Natives of high altitude reportedly have more alveoli that LAR and this could explain the greater vital capacity toward the bottom of the lung if the alveolar proliferation is concentrated there. This might also lower pulmonary vascular resistance at the bottom which would explain the normal Q/V distribution, even though pulmonary artery pressure may be increased.

Cardiovascular adaptations in Andean natives after 6 wk of exposure to sea level.

Six male Quechua Indians (34.0 +/- 1.1 yr, 159.5 +/- 2.1 cm, 60.5 +/- 1.6 kg), life-long residents of La Raya, Peru (4,350-m altitude with an average barometric pressure of 460 Torr), were studied using noninvasive methods to determine the structural and functional changes in the cardiovascular system in response to a 6-wk deacclimation period at sea level. Cardiac output, stroke volume, and left ventricular ejection fractions were determined using radionuclide angiographic techniques at rest and during exercise on a cycle ergometer at 40, 60, and 90% of a previously determined maximal O2 consumption. Subjects at rest were subjected to two-dimensional and M-mode echocardiograms and a standard 12-lead electrocardiogram. Hemoglobin and hematocrit were measured on arrival at sea level by use of a Coulter Stacker S+ analyzer. After a 6-wk deacclimation period, all variables were remeasured using the identical methodology. Hemoglobin values decreased significantly over the deacclimation period (15.7 +/- 1.1 to 13.5 +/- 1.2 g/dl; P less than 0.01). The results indicate that the removal of these high-altitude-adapted natives from 4,300 m to sea level for 6 wk results in only minor changes to the cardiac structure and function as measured by these noninvasive techniques.

Skeletal muscle metabolism and work capacity: a 31P-NMR study of Andean natives and lowlanders.

Two metabolic features of altitude-adapted humans are the maximal O2 consumption (VO2max) paradox (higher work rates following acclimatization without increases in VO2max) and the lactate paradox (progressive reductions in muscle and blood lactate with exercise at increasing altitude). To assess underlying mechanisms, we studied six Andean Quechua Indians in La Raya, Peru (4,200 m) and at low altitude (less than 700 m) immediately upon arrival in Canada. The experimental strategy compared whole-body performance tests and single (calf) muscle work capacities in the Andeans with those in groups of sedentary, power-trained, and endurance-trained lowlanders. We used 31P nuclear magnetic resonance spectroscopy to monitor noninvasively changes in concentrations of phosphocreatine [( PCr]), [Pi], [ATP], [PCr]/[PCr] + creatine ([Cr]), [Pi]/[PCr] + [Cr], and pH in the gastrocnemius muscle of subjects exercising to fatigue. Our results indicate that the Andeans 1) are phenotypically unique with respect to measures of anaerobic and aerobic work capacity, 2) despite significantly lower anaerobic capacities, are capable of calf muscle work rates equal to those of highly trained power- and endurance-trained athletes, and 3) compared with endurance-trained athletes with significantly higher VO2max values and power-trained athletes with similar VO2max values, display, respectively, similar and reduced perturbation of all parameters related to the phosphorylation potential and to measurements of [Pi], [PCr], [ATP], and muscle pH derivable from nuclear magnetic resonance. Because the lactate paradox may be explained on the basis of tighter ATP demand-supplying coupling, we postulate that a similar mechanism may explain 1) the high calf muscle work capacities in the Andeans relative to measures of whole-body work capacity, 2) the VO2max paradox, and 3) anecdotal reports of exceptional work capacities in indigenous altitude natives.