[Thermogenic responses of high-altitude adapted rats on low temperatures and low pressures]

The male rats were raised in two groups, one at Mt. Yatsugatake (2,100 m above sea level, the average ambient temperature 12.5 degrees C) for 30 days, and the other at a laboratory of Matsumoto (610 m above sea level, the average temperature 20 degrees C). The steady-state oxygen consumptions (VO2) and the rectal temperatures (TR) were measured under exposure conditions of various temperatures combined with different simulated altitudes. The values of VO2 and TR for a control group at 610 m-20 degrees C were regarded as 100% and the relative changes to the control values were obtained at various temperatures in the respective low-pressure condition. When measured at a simulated altitude of 2,000 m on the 2nd day after the rats raised at Mt. Yatsugatake were translocated to Matsumoto, the values at 0 degrees C and 10 degrees C room temperatures, VO2 and TR, were still significantly increased as compared with those of rats raised at Matsumoto. On the 40th day after the translocation from Mt. Yatsugatake, however, the values turned out to exhibit no significant difference in both groups. These results indicated that the greater thermogenesis of high-altitude adapted rats had been established by combined stimuli of low temperatures and low pressures as compared with those of Matsumoto-level adapted rats, but the responses returned to the control level by deadaptation process at 40 days after the translocation.