Cerebrovascular responses to hypoxia and hypocapnia in high-altitude dwellers.

Cerebral blood flow is known to increase in response to hypoxia and to decrease with hypocapnia. It is not known, however, whether these responses are altered in high-altitude dwellers who are not only chronically hypoxic and hypocapnic, but also polycythaemic. Here we examined cerebral blood flow responses to hypoxia and hypocapnia, separately and together, in Andean high-altitude dwellers, including some with chronic mountain sickness (CMS), which is characterized by excessive polycythaemia. Studies were carried out at high altitude (Cerro de Pasco (CP), Peru; barometric pressure (P(B)) 450 mmHg) and repeated, following relief of the hypoxia, on the day following arrival at sea level (Lima, Peru; P(B) 755 mmHg). We compared these results with those from eight sea-level residents studied at sea level. In nine high-altitude normal subjects (HA) and nine CMS patients, we recorded middle cerebral artery mean blood flow velocity (MCAVm) using transcranial Doppler ultrasonography, and expressed responses as changes from baseline. MCAVm responses to hypoxia were determined by changing end-tidal partial pressure of oxygen (P(ET,O2)) from 100 to 50 mmHg, with end-tidal partial pressure of carbon dioxide clamped. MCAVm responses to hypocapnia were studied by voluntary hyperventilation with (P(ET,O2)) clamped at 100 and 50 mmHg. There were no significant differences between the cerebrovascular responses of the two groups to any of the interventions at either location. In both groups, the MCAVm responses to hypoxia were significantly greater at Lima than at CP (HA, 12.1 +/- 1.3 and 6.1 +/- 1.0%; CMS, 12.5 +/- 0.8 and 5.6 +/- 1.2%; P < 0.01 both groups). The responses at Lima were similar to those in the sea-level subjects (13.6 +/- 2.3%). The responses to normoxic hypocapnia in the altitude subjects were also similar at both locations and greater than those in sea-level residents. During hypoxia, both high-altitude groups showed responses to hypocapnia that were significantly smaller at Lima than at CP (HA, 2.17 +/- 0.23 and 3.29 +/- 0.34% mmHg(-1), P < 0.05; CMS, 1.87 +/- 0.16 and 3.23 +/- 0.24% mmHg(-1); P < 0.01). The similarity of the results from the two groups of altitude dwellers suggests that haematocrit is unlikely to greatly affect cerebrovascular reactivity to hypoxia and hypocapnia. The smaller vasodilatation to hypoxia and larger vasoconstriction to hypoxic hypocapnia at high altitude suggest that cerebrovascular responses may be impaired at the high altitude, i.e. a maladaptation. The changes in the responses within less than 24 h at sea level indicate that this impairment is rapidly reversible.

Orthostatic tolerance and blood volumes in Andean high altitude dwellers.

Orthostatic tolerance is a measure of the ability to prevent hypotension during gravitational stress. It is known to be dependent on the degree of vasoconstriction and the magnitude of plasma volume, but the possible influence of packed cell volume (PCV) is unknown. High altitude residents have high haematocrits and probably high packed cell volumes. However, it is not known whether plasma volume and blood volume are affected, or whether their orthostatic tolerance is different from low altitude residents. In this study we determined plasma volume, PCV and orthostatic tolerance in a group of high altitude dwellers (HA), including a subgroup of highland dwellers with chronic mountain sickness (CMS) and extreme polycythaemia. Plasma volume and PCV were determined using Evans Blue dye dilution and peripheral haematocrit. Orthostatic tolerance was assessed as the time to presyncope in a test of head-up tilting and lower body suction. All studies were performed at 4338 m. Results showed that plasma volumes were not significantly different between CMS and HA, or in highland dwellers compared to those seen previously in lowlanders. PCV and haematocrit were greater in CMS than in HA. Orthostatic tolerance was high in both CMS and HA, although the heart rate responses to orthostasis were smaller in CMS than HA. Orthostatic tolerance was correlated with haematocrit (r= 0.57, P < 0.01) and PCV (r= 0.54, P < 0.01). This investigation has shown that although high altitude residents have large PCV, their plasma volumes were similar to lowland dwellers. The group with CMS have a particularly large PCV and also have a very high orthostatic tolerance, despite smaller heart rate responses. These results are compatible with the view that PCV is of importance in determining orthostatic tolerance.

Ventilatory and cardiovascular responses to hypoxia and exercise in Andean natives living at sea level.

This study was designed to determine in subjects born at high altitude who move to sea level (HA-SL: born at 3500 m or above; n = 25) whether their cardiorespiratory responses to hypoxia and exercise are similar to those of sea level natives (SL,n = 25). The average age (39 +/- 7.3 yr), weight (72 +/- 7.3 kg), and height (1.71 +/- 0.01 m) did not differ between the SL and HA-SL subjects. All subjects were studied at rest or during exercise (60 W on cycle ergometer) while breathing room air (F(IO2) = 0.21 and P(B) = 760) or hypoxia (F(IO2) = 0.115 and PB = 760) in the following order: (1) normoxia at rest (NX-Rs), (2) hypoxia at rest (HX-Rs, 11.5% O(2)), hypoxia at exercise (HX-Ex), and normoxia at exercise (NX-Ex). Each period lasted 5 min. In absolute values, HA-SL showed significantly higher ventilation (V(E), L/min) during exercise in both normoxia and hypoxia and higher oxygen saturation (Sa(O2), %) during hypoxia both at rest and in exercise. They also had lower end-tidal CO(2) values (P(ETCO2), torr) at rest in both normoxia and hypoxia, but a higher P(ETCO2) in hypoxic exercise. Heart rate (HR, beats/min) was lower at rest in both normoxia and hypoxia, but higher in exercise. With acute hypoxia, Sa(O2) decreased less in the HA-SL than in the SL at rest (HA-SL, 9.2 +/- 0.8; SL, 12.0 +/- 0.82) and during exercise (HA-SL, 18.3 +/- 1.1; SL, 21.2 +/- 1.2). In conclusion, this study shows that HA-SL natives have increased ventilation and heart rate during exercise once their lifelong hypoxia is relieved.

Sodium cyanate: from a promising therapeutic agent to a research tool in high altitude physiology.

Sodium cyanate (NaOCN) first appeared on the biomedical scene as a potential therapeutic agent for sickle-cell disease. Although it did not fulfill its early promise in the clinic, it proved to be useful as a pharmacological tool in physiological research, particularly in the physiology of oxygen transport. NaOCN has been especially valuable in the area of investigation which is reviewed here: the study of oxygen transport, both in normoxic and in hypoxic conditions, in experimental models in which NaOCN was used to induce a shift to the left of the oxygen dissociation curve. The classical idea is that a low Hb-O2 affinity is of adaptive value for life at high altitudes but it has been challenged by several pieces of evidence. One of them is the demonstration of increased survival in hypoxic hypoxia of animals with a high Hb-O2 affinity induced by NaOCN. We also discuss the advantages and potentially confounding factors which should be taken into consideration when interpreting results of studies in which the oxygen dissociation curve has been modified by administration of NaOCN.

Sodium cyanate: from a promising therapeutic agent to a research tool in high altitude physiology

Sodium cyanate (NaOCN) first appeared on the biomedical scene as a potential therapeutic agent for sickle-cell disease. Although it did not fulfill its early promise in the clinic, it proved to be useful as a pharmacological tool in physiological research, particularly in the physiology of oxygen transport. NaOCN has been especially valuable in the area of investigation which is reviewed here: the study of oxygen transport, both in normoxic and in hypoxic conditions, in experimental models in which NaOCN was used to induce a shift to the left of the oxygen dissociation curve. The classical idea is that a low Hb-O2 affinity is of adaptive value for life at high altitudes but it has been challenged by several pieces of evidence. One of them is the demonstration of increased survival in hypoxic hypoxia of animals with a high Hb-O2 affinity induced by NaOCN. We also discuss the advantages and potentially confounding factors which should be taken into consideration when interpreting results of studies in which the oxygen dissociation curve has been modified by administration of NaOCN

Time-course of the polycythemic response in normoxic and hypoxic mice with high blood oxygen affinity induced by cyanate administration.

The Hb-O2 affinity and the erythropoietic response as a function of time were studied in mice treated with sodium cyanate for up to 2 months. Cyanate increased the Hb-O2 affinity in normoxic mice more than in chronically hypoxic mice. The hemoglobin concentration rose as a function of time both in normoxic and hypoxic conditions but reached higher levels in hypoxia. After 42 days of study (21 days of hypoxia) hemoglobin reached maximum levels and thereafter showed a plateau in both cyanate and control animals. It is concluded that a chronic left-shifted oxygen dissociation curve does not avoid the development of hypoxic polycythemia in mice. Moreover, prolonged cyanate administration potentiates the erythropoietic response to chronic hypoxia. Since polycythemia is an index of tissue hypoxia, the results show that the high hemoglobin affinity did not prevent tissue hypoxia in low PO2 conditions. Results showing beneficial effects of high hemoglobin oxygen affinity induced by cyanate based on acute hypoxic expositions should be cautiously interpreted with regard to their adaptive value in animals chronically exposed to natural or simulated hypoxia.