Journal
JOURNAL OF APPLIED PHYSIOLOGY
Volume 88, Issue 2, Pages 365-368Publisher
AMER PHYSIOLOGICAL SOC
DOI: 10.1152/jappl.2000.88.2.365
Keywords
biological rhythms; body temperature; chronic hypoxia; oxygen consumption
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Because the circadian rhythms of oxygen consumption ((V) over dotO(2)) and body temperature (T-b) could be contributed to by differences in thermogenesis and because hypoxia depresses thermogenesis in its various forms, we tested the hypothesis that hypoxia blunts the normal daily oscillations in (V) over dotO(2) and T-b. Adult rats were instrumented for measurements of T-b and activity by telemetry; (V) over dotO(2) was measured by an open-flow method. Animals were exposed to normoxia (21% O-2), hypoxia (10.5% O-2), and normoxia again, each 1 wk in duration, in either a 12:12-h light-dark cycle (synchronized) or constant light (free running). In this latter case, the period of the cycle was similar to 25 h. In synchronized conditions, hypoxia almost eliminated the T-b circadian oscillation, because of the blunting of the T-b rise during the dark phase. On return to normoxia, T-b rapidly increased toward the maximum normoxic values, and the normal cycle was then reestablished. In hypoxia, the amplitude of the activity and (V) over dotO(2) oscillations averaged, respectively, 37 and 56% of normoxia. In free-running conditions, on return to normoxia the rhythm was reestablished at the expected phase of the cycle. Hence, the action of hypoxia was not on the clock itself but probably at the hypothalamic centers of thermoregulation. Hyperoxia (40% O-2) or hypercapnia (3% CO2) had no significant effects on circadian oscillations, indicating that the effects of hypoxia did not reflect an undifferentiated response to changes in environmental gases. Modifications of the metabolism and T-b rhythms during hypoxia could be at the origin of sleep disturbances in cardiorespiratory patients and at high altitude.
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