Thermoregulatory defenses are characterized by thresholds, the core te
mperatures triggering each response. Core body temperature is normally
maintained within the interthreshold range, temperatures between the
sweating and vasoconstriction thresholds that do not trigger autonomic
defenses. This range usually spans only some 0.2 degrees C, but it re
mains unknown whether similar precision is maintained during the circa
dian core temperature cycle of about 0.8 degrees C. Accordingly, we ev
aluated the interthreshold range at four times of the day. We studied
ten male volunteers, each at 3 a.m., 8 a.m., 3 p.m.. and 8 p.m. At lea
st 12 h elapsed between tests, and the order was randomly assigned. At
each study time, volunteers were warmed peripherally until sweating w
as observed. Skin temperature was subsequently kept constant while cor
e temperature was decreased by central-venous infusion of ice-cold flu
id until peripheral vasoconstriction was detected. The volunteers were
not permitted to sleep during threshold determinations, although slee
p was not otherwise controlled. The core temperature triggering an eva
porative water loss of 40 g.m(-2).h(-1) identified the su eating thres
hold. Similarly, the vasoconstriction threshold was defined by the cor
e temperature triggering the initial decreases in plethysmographic fin
ger tip blood flow. The interthreshold range at 3 a.m. was tu ice that
observed at the other study times (P < 0.05). Our data suggest that a
utonomic control of body temperature is reduced at 3 a.m.. even when s
leep is denied. This result contradicts the general perception that ci
rcadian variation alters the thermoregulatory target temperature, but
not precision of body temperature control.