Seasonal variations of physiological responses to heat of subtropical and temperate natives

In an attempt to compare the physiological responses of subtropical natives to heat with those of temperate natives, seasonal variations in physiological responses to heat were observed in young male residents of Okinawa who were born and raised in Okinawa, subtropical zone (group O) and young male residents of Okinawa who were born and raised on the Japan mainland, temperate zone, but moved to Okinawa in less than two years (group M). In both seasons, group O showed less sweat loss, lower Na concentration in sweat, lower rise in rectal temperature and less increase in heart rate during heat exposure than group M. In both groups, greater sweat loss, lower Na concentration in sweat and lower rise in rectal temperature in summer than in winter were observed. Seasonal differences in Na concentration in sweat, rise in rectal temperature and increase in heart rate for group O were smaller than those for group M. It was assumed the efficiency of sweat for cooling the body for group O was better than that for group M, and heat tolerance for group O was superior to that for group M.     

Studies on heat tolerance of subtropical natives after migration to a temperate zone

Anthropometric measurements and observations of physiological responses to heat were made in the autumn on 20 young male Japanese who were born and reared in the main islands of Japan (group M), 20 young male Japanese who were born and reared in Okinawa, subtropical zone, and who have lived in the main islands of Japan, temperate zone, for less than three years (group O). In winter the same tests were made on 25 subjects in group M and 17 subjects in group O. Group O showed lower skinfold thickness and less body fat content than group M. Both groups showed lower skinfold thickness and less body fat content in autumn than in winter. Group O was characterized by lower sweat rate and lower Na concentration in sweat for a given rise in body temperature. In both groups, greater sweat loss, lower Na concentration in sweat and smaller rise in body temperature were observed in autumn than in winter. Group O showed higher heat tolerance than group M when assessed by our numerical index for the assessment of heat tolerance. It was assumed that capacity of non-evaporative heat dissipatïon for group O was superior to that for group M, and the efficiency of sweat for cooling body in group O was better than that in group M. Differences in anthropometrical characteristics and physiological responses to heat between the two groups might reflect more advanced heat acclimatization of subjects in group O when compared with those in group M.     

Primate models to study eccrine sweating

The histochemistry and histology of the eccrine sweat gland in the rhesus monkey (Macaca mulatta) are described. The histochemical distribution and localization of enzymes and substrates are very similar to those found in the human; innervation is cholinergic. Active eccrine glands on the general body surface average 136 glands/cm². Above the thermal neutral zone (TNZ), sweating is the major avenue for heat loss and the role of panting in dissipating heat is relatively insignificant. The intrahypothalamic administration of prostaglandin E₁ (PGE₁) suppresses sweating and leads to an increase in core temperature. A linear relation is found between local sweat rates on the general body surface and clamped hypothalamic temperature. Studies also provide direct support for the concept that brain temperature and skin temperature interact additively in the control of sweating in higher primates. The functional characteristics of eccrine sweating in the patas monkey (Erythocebus) are qualitatively similar to those in the rhesus monkey. The patas monkey maintains a relatively constant rectal temperature (37.6–38.4°C) when equilibrated to a wide range of ambient temperaures of 15–40°C. Eccrine sweating is the main effector system for heat dissipation above the TNZ. We emphasize here that evaporative heat loss that is due to sweating is related to both mean skin and mean body temperature and at 40°C is 40% higher than that recorded from the rhesus monkey. These results indicate that the patas monkey, because of its high sweating capacity and other similarities with the human eccrine system, is a most appropriate animal model for comparative studies of eccrine sweat gland function in primates in general.     

Sex differences in thermoeffector responses during exercise at fixed requirements for heat loss

To assess potential mechanisms responsible for the lower sudomotor thermosensitivity in women during exercise, we examined sex differences in sudomotor function and skin blood flow (SkBF) during exercise performed at progressive increases in the requirement for heat loss. Eight men and eight women cycled at rates of metabolic heat production of 200, 250, and 300 W/m(2) of body surface area, with each rate being performed sequentially for 30 min. The protocol was performed in a direct calorimeter to measure evaporative heat loss (EHL) and in a thermal chamber to measure local sweat rate (LSR) (ventilated capsule), SkBF (laser-Doppler), sweat gland activation (modified iodine-paper technique), and sweat gland output (SGO) on the back, chest, and forearm. Despite a similar requirement for heat loss between the sexes, significantly lower increases in EHL and LSR were observed in women (P ≤ 0.001). Sex differences in EHL and LSR were not consistently observed during the first and second exercise periods, whereas EHL (348 ± 13 vs. 307 ± 9 W/m(2)) and LSR on the back (1.61 ± 0.07 vs. 1.20 ± 0.09 mg·min(-1)·cm(-2)), chest (1.33 ± 0.06 vs. 1.08 ± 0.09 mg·min(-1)·cm(-2)), and forearm (1.53 ± 0.07 vs. 1.20 ± 0.06 mg·min(-1)·cm(-2), men vs. women) became significantly greater in men during the last exercise period (P < 0.05). At each site, differences in LSR were solely due to a greater SGO in men, as opposed to differences in sweat gland activation. In contrast, no sex differences in SkBF were observed throughout the exercise period. The present study demonstrates that sex differences in sudomotor function are only evidenced beyond a certain requirement for heat loss, solely through differences in SGO. In contrast, the lower EHL and LSR in women are not paralleled by a lower SkBF response.     

Regional differences in the sweating responses of older and younger men.

Ten older (60-71 yr) and nine younger (20-25 yr) active healthy men were exposed to passive heating [by placing the lower legs and feet in a 43 degrees C water bath for 60 min while sitting in a warm (35 degrees C, 45% relative humidity) chamber] in summer and winter. The increase in rectal temperature (Tre) was significantly (P less than 0.05) greater, and mean skin temperature and forearm blood flow were lower, for the older men in both seasons. Total sweating rate was lower in the older men, but significantly (P less than 0.05) so only in the summer. The Tre threshold for sweating was unaffected by either age or site (back vs. thigh). The local sweating rate (msw) on the thigh was significantly lower (P less than 0.05) for the older men throughout the exposure, whereas there were no significant age-related differences for the average or peak values of back msw, although lesser sweating on the back occurred during the first 30 min of exposure. The decreased msw on the thigh was due to a lower sweat output per heat-activated sweat gland rather than from recruitment of fewer glands. It was concluded that regional differences exist in the age-related decrement in sweat gland function. Furthermore, these findings suggest that aging leads to a decreased ability to maintain body temperature with passive heating of the extremities, which may be attributed in part to decreased regional sweat gland function.     

Thermoregulation at rest and during exercise in prepubertal boys

Thermal balance was studied in 11 boys, aged 10-12 years, with various values for maximal oxygen uptake (VO2max), during two standardized sweating tests performed in a climatic chamber in randomized order. One of the tests consisted in a 90-min passive heat exposure [dry bulb temperature (Tdb) 45 degrees C] at rest. The second test was represented by a 60-min ergocycle exercise at 60% of individual VO2max (Tdb 20 degrees C). At rest, rectal temperature increased during heat exposure similar to observations made in adults, but the combined heat transfer coefficient reached higher values, reflecting greater radiative and convective heat gains in the children. Children also exhibited a greater increase in mean skin temperature, and a greater heat dissipation through sweating. Conversely, during the exercise sweating-test, although the increase in rectal temperature did not differ from that of adults for similar levels of exercise, evaporative heat loss was much lower in children, suggesting a greater radiative and convective heat loss due to the relatively greater body surface area. Thermophysiological reactions were not related to VO2max in children, in contrast to adults.     

Effect of long term residence in the temperate zone on the physique and sweating reaction of subtropical natives

Anthropometric measurements and observations of physiological responses to heat were made in the summer on 20 young male residents of the Japan mainland who were born in Okinawa but moved to the mainland within less than three years (group S) and 15 young male migrants of Japanese from Okinawa who had lived in the Japan mainland for more than 10 years (group L). Group L showed a thicker skinfold and greater body fat content than group S. Group L showed a greater sweat loss and higher rise in oral temperature than group S. Heat tolerance of group L was inferior to that of group S when assessed by our numerical index for evaluating human heat tolerance. The inferior heat tolerance of group L might reflect a lower efficiency of sweat for cooling the body and an inferior capacity for non-evaporative heat dissipation when compared with group S. The physiological responses of subtropical natives to heat were lost after longterm residence in the temperate zone.     

Hyperthermia modifies muscle metaboreceptor and baroreceptor modulation of heat loss in humans

The relative influence of muscle metabo- and baroreflex activity on heat loss responses during post-isometric handgrip (IHG) exercise ischemia remains unknown, particularly under heat stress. Therefore, we examined the separate and integrated influences of metabo- and baroreceptor-mediated reflex activity on sweat rate and cutaneous vascular conductance (CVC) under increasing levels of hyperthermia. Twelve men performed 1 min of IHG exercise at 60% of maximal voluntary contraction followed by 2 min of ischemia with simultaneous application of lower body positive pressure (LBPP, +40 mmHg), lower body negative pressure (LBNP, -20 mmHg), or no pressure (control) under no heat stress. On separate days, trials were repeated under heat stress conditions of 0.6°C (moderate heat stress) and 1.4°C (high heat stress) increase in esophageal temperature. For all conditions, mean arterial pressure was greater with LBPP and lower with LBNP than control during ischemia (all P ≤ 0.05). No differences in sweat rate were observed between pressure conditions, regardless of the level of hyperthermia (P > 0.05). Under moderate heat stress, no differences in CVC were observed between pressure conditions. However, under high heat stress, LBNP significantly reduced CVC by 21 ± 4% (P ≤ 0.05) and LBPP significantly elevated CVC by 14 ± 5% (P ≤ 0.05) relative to control. These results show that sweating during post-IHG exercise ischemia is activated by metaboreflex stimulation, and not by baroreflexes. In contrast, our results suggest that baroreflexes can influence the metaboreflex modulation of CVC, but only at greater levels of hyperthermia.     

Is cardiac filling pressure the limiting factor in adjusting to heat stress?

The concept that a specific level of central venous pressure (CVP) limits man's adjustment to heat stress has been debated. Evidence was presented that identifies a true limit of adjustment as being more related to factors affecting evaporative cooling, such as level of hydration, release of active vasodilation substance (AVS), and sweat gland fatigue. However, it was conceded that decreases in CVP and subsequent low-pressure baroreceptor activation modify cutaneous blood flow and subsequently reduce conductance of heat from the core to the periphery. It was suggested that CVP merely reflects a downstream pressure, which must be allowed to reach a pressure lower than that observed in the peripheral venous bed during active cutaneous vasodilation, to insure adequate venous return. However, a loss of evaporative cooling has been observed during prolonged progressive dehydration of subjects in the supine position, resulting in 3 to 4 percent loss of total body weight. This loss of evaporative cooling was not apparent when euhydration was maintained. As it was unlikely that CVP was reduced in these experiments in the supine position, it was concluded that CVP was not the limiting factor in man's adjustment to heat stress.     

Thermoregulatory adjustments during continuous heat exposure

Body temperature regulation was studied in 6 male subjects during an acclimation procedure involving uninterrupted heat exposure for 5 successive days and nights in a hot dry environment (ambient temperature = 35 degrees C, dew-point temperature = 7 degrees C; air velocity = 0.2 m.s-1). Data were obtained at rest and during exercise (relative mechanical workload = 35% VO2max). At rest, hourly measurements were made of oesophageal and 4 local skin temperatures, to allow the calculation of mean skin temperature, and of body motility and heart rate. During the working periods these measurements were made at 5 min intervals. Hourly whole-body weight loss was measured at rest on a sensitive platform scale while in the working condition just before starting and immediately after completing the bicycle exercise. The results show that, in both exercise and at rest, the successive heat exposures increased the sweat gland output during the first 3 days. Afterwards, sweat rate decreased without any corresponding change in body temperature. For the fixed workload, the sweat rate decline was associated with a decrease in circulatory strain. Adjustments in both sweating and circulatory mechanisms occur in the first 3 days of continuous heat exposure. The overall sweat rate decline could involve a redistribution of the regional sweating rates which enhances the sweat gland activities of skin areas with maximal evaporative efficiencies.     

Contribution of central versus sweat gland mechanisms to the seasonal change of sweating function in young sedentary males and females

In summer and winter, young, sedentary male (N = 5) and female (N = 7) subjects were exposed to heat in a climate chamber in which ambient temperature (Ta) was raised continuously from 30 to 42°C at a rate of 0.1°C min⁻¹ at a relative humidity of 40%. Sweat rates (SR) were measured continuously on forearm, chest and forehead together with tympanic temperature (Tty), mean skin temperature ( [`T] s ) \left( {\overline {\hbox{T}} {\hbox{s}}} \right) and mean body temperature ( [`T] b ) \left( {\overline {\hbox{T}} {\hbox{b}}} \right) . The rate of sweat expulsions (Fsw) was obtained as an indicator of central sudomotor activity. Tty and ( [`T] b ) \left( {\overline {\hbox{T}} {\hbox{b}}} \right) were significantly lower during summer compared with winter in males; SR was not significantly different between summer and winter in males, but was significantly higher during summer in females; SR during winter was higher in males compared with females. The regression line relating Fsw to ( [`T] b ) \left( {\overline {\hbox{T}} {\hbox{b}}} \right) shifted significantly from winter to summer in males and females, but the magnitude of the shift was not significantly different between the two subject groups. The regression line relating SR to Fsw was steepened significantly from winter to summer in males and females, and the change in the slope was significantly greater in females than in males. Females showed a lower slope in winter and a similar slope in summer compared to males. It was concluded that sweating function was improved during summer mediated by central sudomotor and sweat gland mechanisms in males and females, and, although the change of sweat gland function from winter to summer was greater in females as compared with males, the level of increased sweat gland function during summer was similar between the two subject groups.     

Thermoregulatory responses of middle-aged and young men during dry-heat acclimation

Thermoregulatory responses during heat acclimation were compared between nine young (mean age 21.2 yr) and nine middle-aged men (mean age 46.4 yr) who were matched (P greater than 0.05) for body weight, surface area, surface area-to-weight ratio, percent body fat, and maximal aerobic power. After evaluation in a comfortable environment (22 degrees C, 50% relative humidity), the men were heat acclimated by treadmill walking (1.56 m/s, 5% grade) for two 50-min exercise bouts separated by 10 min of rest for 10 consecutive days in a hot dry (49 degrees C ambient temperature, 20% relative humidity) environment. During the first day of heat exposure performance time was 27 min longer (P less than 0.05) for the middle-aged men, whereas final rectal and skin temperatures and heart rate were lower, and final total body sweat loss was higher (P less than 0.05) compared with the young men. These thermoregulatory advantages for the middle-aged men persisted for the first few days of exercise-heat acclimation (P less than 0.05). After acclimation no thermoregulatory or performance time differences were observed between groups (P greater than 0.05). Sweating sensitivity, esophageal temperature at sweating onset, and the sweating onset time did not differ (P greater than 0.05) between groups either pre- or postacclimatization. Plasma osmolality and sodium concentration were slightly lower for the young men both pre- and postacclimatization; however, both groups had a similar percent change in plasma volume from rest to exercise during these tests.(ABSTRACT TRUNCATED AT 250 WORDS)     

Latent heat loss and sweat gland histology of male goats in an equatorial semi-arid environment

The objective of this work was to quantify the heat loss by cutaneous evaporation of goats in an equatorial semi-arid environment. The latent heat loss from the body surfaces of these ten undefined breed goats was measured using a ventilated capsule in sun and shade and in the three body regions (neck, flank and hindquarters). Skin samples from these three regions were histologically analyzed to relate the quantity of sweat glands, the area of sweat glands and the epithelium thickness of each of these regions to the heat loss by cutaneous evaporation of the examined goats. The epithelium thickness that was measured varied significantly for body regions with different quantities and areas of sweat glands (P?<?0.01). Among the body regions that were examined, the samples from the neck demonstrated the highest epithelium thickness (16.23?±?0.13 μm). However, the samples of sweat glands from the flank had the biggest area (43330.51?±?778.71 μm²) and quantity per square centimeter (390?±?9 cm^?2). After the animals were exposed to sun, the flanks lost the greatest amount of heat by cutaneous evaporation (73.03?±?1.75 W?m^?2) and possessed the highest surface temperatures (39.47?±?0.18 °C). The histological characteristics may have influenced the heat loss by cutaneous evaporation that was observed in the flank region after the animals were exposed to sun.     

Limb vs trunk sweat gland recruitment patterns during exercise in humans

The purpose of this study was to examine the sweat gland recruitment pattern, on multiple trunk and limb sites, during exercise. Nineteen male volunteers performed 30 min of exercise on a cycle ergometer at approx. 25, 50 and 75% of their maximal oxygen uptake. The number of active sweat glands (per cm(2)) was determined immediately following each exercise bout at the following six sites: left triceps, chest, back, forearm, thigh and calf. The data showed that increases in rectal temperature during exercise resulted in a linear increase in the absolute number of active sweat glands recruited at all six sites (r=0.60-0.80). However, on a percentage basis, the limb sites increased proportionally more (300-600% increase) than the trunk sites (100-200% increase) with increases in rectal temperature. These data suggest that the absolute number of sweat glands recruited, on both the trunk and the limbs, increases in a linear manner with increases in rectal temperature during exercise. However, on a proportional basis, sweat gland recruitment on the limbs is greater than that found on the trunk during progressive exercise.     

A comparison of hydration effect on body fluid and temperature regulation between Malaysian and Japanese males exercising at mild dehydration in humid heat

Background

This study investigated the effect of hydration differences on body fluid and temperature regulation between tropical and temperate indigenes exercising in the heat.

Methods

Ten Japanese and ten Malaysian males with matched physical characteristics (height, body weight, and peak oxygen consumption) participated in this study. Participants performed exercise for 60 min at 55% peak oxygen uptake followed by a 30-min recovery at 32°C and 70% relative air humidity with hydration (4 times each, 3 mL per kg body weight, 37°C) or without hydration. Rectal temperature, skin temperature, heart rate, skin blood flow, and blood pressure were measured continuously. The percentage of body weight loss and total sweat loss were calculated from body weight measurements. The percentage change in plasma volume was estimated from hemoglobin concentration and hematocrit.

Results

Malaysian participants had a significantly lower rectal temperature, a smaller reduction in plasma volume, and a lower heart rate in the hydrated condition than in the non-hydrated condition at the end of exercise (P <0.05), whereas Japanese participants showed no difference between the two hydration conditions. Hydration induced a greater total sweat loss in both groups (P <0.05), and the percentage of body weight loss in hydrated Malaysians was significantly less than in hydrated Japanese (P <0.05). A significant interaction between groups and hydration conditions was observed for the percentage of mean cutaneous vascular conductance during exercise relative to baseline (P <0.05).

Conclusions

The smaller reduction in plasma volume and percentage body weight loss in hydrated Malaysians indicated an advantage in body fluid regulation. This may enable Malaysians to reserve more blood for circulation and heat dissipation and thereby maintain lower rectal temperatures in a hydrated condition.     

Relationship of osmotic inhibition in thermoregulatory responses and sweat sodium concentration in humans

Heat acclimatization improves thermoregulatory responses to heat stress and decreases sweat sodium concentration ([Na(+)](sweat)). The reduced [Na(+)](sweat) results in a larger increase in plasma osmolality (P(osmol)) at a given amount of sweat output. The increase in P(osmol) inhibits thermoregulatory responses to increased body core temperature. Therefore, we hypothesized that the inhibitory effect of plasma hyperosmolality on the thermoregulatory responses to heat stress should be attenuated with the reduction of [Na(+)](sweat) due to heat acclimatization. Eleven subjects (9 male and 2 female) were passively heated by immersing their lower legs into water at 42 degrees C (room temperature 28 degrees C and relative humidity 30%) for 50 min following isotonic or hypertonic saline infusion. We determined the increase in the esophageal temperature (T(es)) required to elicit sweating and cutaneous vasodilation (CVD) (DeltaT(es) thresholds for sweating and CVD, respectively) in each condition and calculated the elevation of the T(es) thresholds per unit increase in P(osmol) as the osmotic inhibition of sweating and CVD. The osmotic shift in the DeltaT(es) thresholds for both sweating and CVD correlated linearly with [Na(+)](sweat) (r = 0.858 and r = 0.628, respectively). Thus subjects with a lower [Na(+)](sweat) showed a smaller osmotic elevation of the DeltaT(es) thresholds for sweating and CVD. These results suggest the possibility that heat acclimatization attenuates osmotic inhibition of thermoregulatory responses as well as reducing [Na(+)](sweat).     

Effects of menstrual cycle and physical training on heat loss responses during dynamic exercise at moderate intensity in a temperate environment

We evaluated the effects of the menstrual cycle and physical training on heat loss (sweating and cutaneous vasodilation) responses during moderate exercise in a temperate environment. Ten untrained (group U) and seven endurance-trained (group T) women (maximal O2 uptake of 36.7+/-1.1 vs. 49.4+/-1.7 ml.kg-1.min-1, respectively; P<0.05) performed a cycling exercise at 50% maximal O2 uptake for 30 min during both the midfollicular and midluteal menstrual phase in a temperate environment (ambient temperature of 25 degrees C, relative humidity of 45%). In group U, plasma levels of estrone, estradiol, and progesterone at rest and esophageal temperature (Tes) during exercise were significantly higher during the midluteal than during the midfollicular phase (P<0.05). Sweating rate and cutaneous blood flow (measured via laser-Doppler flowmetry) on the chest, back, forearm, and thigh were lower during the midluteal than during the midfollicular phase during exercise. Tes threshold for heat loss responses was significantly higher and sensitivity of the heat loss responses was significantly lower in the midluteal than in the midfollicular phase, regardless of body site. These effects of the menstrual cycle in group U were not observed in group T. The sweating rate and cutaneous blood flow were significantly higher in group T than in group U, regardless of menstrual phase or body site. Tes threshold for heat loss responses was significantly lower and sensitivity of heat loss responses was significantly greater in group T than in group U in the midluteal phase; however, sensitivity of the sweating response was significantly greater in the midfollicular phase. These results suggest that heat loss responses in group U were inhibited in the midluteal phase compared with in the midfollicular phase. Menstrual cycle had no remarkable effects in group T. Physical training improved heat loss responses, which was more marked in the midluteal than in the midfollicular phase.     

Sweating and skin blood flow during exercise: effects of age and maximal oxygen uptake

Individuals greater than or equal to 60 yr of age are more susceptible to hyperthermia than younger people. However, the mechanisms involved remain unclear. To gain further insight, we examined the heat loss responses of 7 young (24-30 yr) and 13 older (58-74 yr) men during 20 min of cycle exercise [67.5% maximal O2 uptake (VO2max)] in a warm environment (30 degrees C, 55% relative humidity). Forearm blood flow (FBF) and chest sweat rate (SR) were plotted as a function of the weighted average of mean skin and esophageal temperatures [Tes(w)] during exercise. The sensitivity and threshold for each response were defined as the slope and Tes(w) at the onset of the response, respectively. When the young sedentary men were compared with a subgroup (n = 7) of the older physically active men with similar VO2max, the SR and FBF responses of the two groups did not differ significantly. However, when the young men were compared with a subgroup of older sedentary men with a similar maximal O2 pulse, the SR and FBF sensitivities were significantly reduced by 62 and 40%, respectively. These findings suggest that during a short exercise bout either 1) there is no primary effect of aging on heat loss responses but, rather, changes are associated with the age-related decrease in VO2max or 2) the decline in heat loss responses due to aging may be masked by repeated exercise training.     

Methylcholine-activated eccrine sweat gland density and output as a function of age

The purpose of this investigation was to examine eccrine sweat gland responsiveness to intradermal injections of methylcholine (MCh) across three age groups of men [young (Y) = 22-24; middle (M) = 33-40; older (O) = 58-67 yr old, n = 5 per group]. Subjects were matched with respect to maximum O2 consumption, body size, and body composition, and were thoroughly heat acclimated before participation. Randomly ordered concentrations of acetyl-beta-methylcholine chloride ranging from 0% (saline) to 0.1% (5 x 10(-3) M) were injected into the skin of the dorsal thigh in a thermoneutral environment, and activated sweat glands were photographed at 30-s intervals for the next 8 min. Density of MCh-activated glands was independent of both age and [MCh] (e.g., 2 min after injection of 5 x 10(-3) M [MCh]: Y = 45 +/- 7, M = 46 +/- 12, O = 42 +/- 5 glands/cm2). However, sweat gland output (SGO) per active gland was significantly lower for the O group and failed to increase with increasing [MCh] above 5 x 10(-4) M. When MCh (5 x 10(-3) M) was injected after 1 h of exercise in the heat, higher SGO's were elicited in each group; however, the SGO of the O group was again significantly lower than that of the Y group (91 +/- 11 vs. 39 +/- 4 ng/gland, P less than 0.02) with the M group intermediate (69 +/- 11 nl/gland; 2 min postinjection data).(ABSTRACT TRUNCATED AT 250 WORDS)     

Sympathetic regulation of adrenal medullary function during aging

Our recent studies on changes in sympathoadrenal medullary function with age in anesthetized Wistar rats were reviewed. Although secretion rates of adrenaline and noradrenaline from the adrenal gland under resting conditions varied among animals, they gradually increased after 300 days and reached a level 2-4 times higher at 800-900 days compared with that of 100 days. Spontaneous activity of a single sympathetic nerve fiber under resting conditions also increased during aging in a manner similar to the catecholamine secretion rates. Reflex responses of mass activity of adrenal sympathetic nerve fibers to stimulation of baroreceptor and cutaneous mechanoreceptors were compared in young adult (4 months old) and aged (26 months old) Wistar rats under strictly controlled conditions for anesthesia, respiration and body temperature. Under these conditions the reflex depression in response to baroreceptor stimulation and cutaneous brushing as well as reflex excitation in response to cutaneous pinching were quite well maintained in the aged rats.