Physiological capacity for altering rates of heat exchange in the iguanid lizard, Dipsosaurus dorsalis, was determined by measuring the rate of temperature change as animals heated from 20? to 38? C and cooled from 40? to 22? C at wind velocities of 0, 90, 200 and 400 ft/min. Rates of heating exceeded rates of cooling by as much as 27% in live animals, while dead animals heated and cooled at the same rate. The percentage increase in the rate of heating was independent of body weight (range: 20-90 g) but was lower at the two highest wind velocities. Maximum rates of endogenous heat production during both heating and cooling could account for 44% of the difference in rate of temperature change at a body temperature of 30? C. The remainder of the difference was attributed to changes in the rate of blood flow between the core and the periphery.
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Wesley W. Weathers (1970) studied this question.
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