Skin biopsy specimens should be systematically collected in cases of encephalitis of unknown origin. These samples should be tested by RT-hnPCR immediately to confirm rabies; if the technique is not readily available locally, the samples should be tested retrospectively for epidemiological purposes.

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The hypothesis of a blunted chronotropic response of cardiac beta-adrenergic receptors in altitude hypoxia was tested in nine subjects at sea level (SL) by infusion of isoproterenol. Observations were made at SL, in acute hypoxia (2 days at 4,350 m, condition H1), in more prolonged hypoxia [13 days between 850 and 4,800 m, condition H2] and in chronic hypoxia [21 days at 4,800 m, condition H3]. Resting heart rate was higher in all hypoxic conditions. Resting norepinephrine concentrations were found to be significantly higher in conditions H2 (1.64 +/- 0.59) and H3 (1.74 +/- 0.76) than at SL (0.77 +/- 0.18 ng/ml). Isoproterenol, diluted in saline, was infused at increasing doses of 0.0, 0.02, 0.04, and 0.06 micrograms.kg-1.min-1. For the highest dose, there was a significantly smaller increase in heart rate in conditions H1 (35 +/- 9), H2 (33 +/- 11), and H3 (31 +/- 11) than at SL (45 +/- 8 min-1). The increase in pulse (systolic/diastolic) pressure, considered as the vascular response to isoproterenol infusion, was smaller in condition H3 (29 +/- 16) than at SL (51 +/- 24 mmHg). There was a significant increase in the dose of isoproterenol required to increase heart rate by 25 min-1 and decrease in slope of heart rate increase vs. log(dose) relationship in conditions H2 and H3. Thus an hypoxia-related attenuated response of beta-adrenergic receptors to exogenous stimulation was found in humans.(ABSTRACT TRUNCATED AT 250 WORDS)

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The variability in sensitivity to acute mountain sickness among individuals is a phenomenon well known to physicians and high altitude alpinists. The measurement of cardiac and respiratory responses to hypoxia (FIO2 = 0.115) at rest and during exercise (50% VO2max) allows the detection of those subjects who are more liable to suffer from high altitude diseases. In a retrospective study performed on 288 subjects evaluated with a hypoxic test during a Mountain medicine consultation, we found that the most clinically susceptible subjects had at least one abnormal response to the hypoxic tests, especially during exercise. The observation of one or several abnormal values in cardiac or respiratory responses to hypoxia leads us to advise a modification in the alpine or trekking objective, an increase in the acclimatization time and/or prevention by acetazolamide.

A decrease in heart rate response to isoproterenol (IP) infusion has been previously described in humans exposed to acute (2-3 days) or chronic (21 days) exposure to altitude hypoxia (J. Appl. Physiol. 65: 1957-1961, 1988). To evaluate this cardiac response in subacute (8 days) hypoxia and to explore its reversal with restoration of normoxia, six subjects received an IP infusion under normoxia (condition N), after 8 days in altitude (4,350 m, condition H8), on the same day in altitude after inhalation of O2 restoring normoxic arterial O2 saturation (SaO2, condition HO), and 6-11 h (condition RN) and 4-5 mo (condition ND) after the return to sea level. Cardiac chronotropic response to IP, evaluated by the mean increase in heart rate from base value (delta HR, min-1), was lower in condition H8 [mean 30 +/- 13 (SD)] than in condition N (50 +/- 14, P less than 0.03); it was slightly higher in condition HO (38 +/- 14) or condition RN (42 +/- 15) than condition H8 but still significantly different from condition N (P less than 0.03), despite normal values of SaO2. delta HR in condition ND (55 +/- 10) returned to base N value. These findings confirm the hypothesis of a hypoxia-induced decrease in cardiac chronotropic function. Two possible mechanisms are suggested: an O2-dependent one, rapidly reversible with recent restoration of normoxia, and a more slowly reversible mechanism, probably a downregulation of the cardiac beta-receptors.

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Effects of high altitude exposure on plasma lipids and lipoprotein cholesterol were studied in 8 mountaineers who spent 3 weeks at the Annapurna IV base camp (4800 m) after a 12 day trek. In spite of the moderate physical exertion at the camp, the loss of body weight was more pronounced during the stay at high altitude than during the trekking period. Compared with baseline values observed at sea level, marked reductions in plasma cholesterol (-27%) and phospholipids (-19%) were found 3 days after arrival at the camp and persisted during the next 17 days. A less marked fall in plasma triglycerides occurred, weakly significant at the end of the stay. Because there were no relevant changes in very low density lipoproteins or in high density lipoprotein (HDL)-cholesterol, the low plasma cholesterol levels at the high altitude resulted mainly from the reduction in low density lipoprotein (LDL)-cholesterol: the mean HDL/LDL cholesterol ratio changed from 0.39 at sea level to 0.63 at the end of the stay at 4800 m. Fluctuations in LDL-cholesterol were not concomitant with those in body weight and were independent of the exercise training during the expedition. This study shows moreover that the early drop in LDL-cholesterol was associated with an opposite change in plasma levels of catecholamines and thyroid hormones. Taking into account that such hormonal responses are classically observed at high altitude, the concomitant decrease in LDL-cholesterol might be interpreted as being a relevant adaptative response to hypoxic conditions at high altitude.