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.     

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.     

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.     

Comparison of physical characteristics,body temperature and resting metabolic rate at 30‡C between subtropical and temperate natives

Anthropometric measurements, measurements of skin temperatures, rectal temperature, heart rate and metabolic rate at 30C were made on 25 young male residents of Okinawa who were born and raised in Okinawa (group O) and 25 young male residents of Okinawa who were born and raised on the Japan mainland but moved to Okinawa less than 2 years before the test (group M) in summer. Group O showed significantly shorter height, lighter body weight, and slender body shape than group M. Group O showed thinner skinfold thickness and smaller percentage of body fat content than group M. Skin temperatures for group O were higher than those for group M, and rectal temperature for group O was slightly lower than that for group M. Group O showed, less metabolic rate per body surface area and slower heart rate than group M. It is concluded that physical characteristics of subtropical natives is favorable for heat dissipation, and subtropical natives have superior capacity for non-evaporative heat dissipation than migrants of temperate natives to a subtropical zone.     

Cold-induced vasodilation and vasoconstriction in the finger of tropical and temperate indigenes

While heat acclimatization reflects the development of heat tolerance, it may weaken an ability to tolerate cold. The purpose of this study was to explore cold-induced vasodilation (CIVD) responses in the finger of tropical indigenes during finger cold immersion, along with temperate indigenes. Thirteen tropical male indigenes (subjects born and raised in the tropics) and 11 temperate male indigenes (subjects born and raised in Japan and China) participated. Subjects immersed their middle finger at 4.3±0.8 °C water for 30 min. Rectal temperature, skin temperatures, finger skin blood flow, blood pressure and subjective sensations were recorded during the test. The results showed that: (1) the tropical group demonstrated a lower minimum (T_min), maximum (T_max) and mean finger temperature (T_mean) compared to those of the temperate group (P<0.05); (2) seven tropical indigenes demonstrated a late-plateau type of CIVD pattern, which is characterized by a pronounced 1st vasoconstriction and a single CIVD with a faint and weak 2nd vasoconstriction, whereas no temperate indigene demonstrated the late-plateau type; and (3) the hand temperature at the end of finger immersion was 3 °C lower in the tropical than the temperate group (P<0.05). These results indicate that tropical indigenes have less active responses of arterio-venous anastomoses in the finger and weaker vasoconstrictions after the first CIVD response during finger cold immersion, which can be considered as being more vulnerable to cold injury of the periphery in severe cold.     

Effects of duration of stay in temperate area on thermoregulatory responses to passive heat exposure in tropical south-east Asian males residing in Japan

ABSTRACT: BACKGROUND: In this study, we investigated the effects of duration of stay in a temperate area on the thermoregulatory responses to passive heat exposure of residents from tropical areas, particularly to clarify whether they would lose their heat tolerance during passive heat exposure through residence in a temperate country, Japan. METHODS: We enrolled 12 males (mean +/- SE age 25.7 +/- 1.3 years) from south-east Asian countries who had resided in Japan for a mean of 24.5 +/- 5.04 months, and 12 Japanese males (age 24.1 +/- 0.9 years) . All subjects were university students who did not engage in vigorous physical or sport activities and were considered to have similar physical activity levels. Passive heat exposure was induced through leg immersion in hot water (42 [degree sign]C) for 60 minutes under conditions of 28 [degree sign]C air temperature and 50% relative humidity. RESULTS: Compared with the Japanese group, the tropical group displayed a higher pre-exposure rectal temperature (P < 0.01) and a smaller increase in rectal temperature during 60 minutes of leg immersion (P = 0.03). Additionally, the tropical group showed a tendency towards a lower total sweat rate (P = 0.06) and lower local sweat rate on the forehead (P = 0.07). The tropical group also had a significantly longer sweating onset time on the upper back (P = 0.04) compared with the Japanese groups. The tropical group who stayed in Japan for > 23 months sweated earlier on the forehead and upper back than those who stayed in Japan < 11 months (P < 0.01 and P = 0.03 for the forehead and upper back, respectively). There was a positive correlation between duration of stay in Japan and total sweat rate (r = 0.58, P <0.05), and negative correlations between duration of stay and sweating onset time on the forehead (r = -0.73, P = 0.01) and on the upper back (r = -0.66, P = 0.02). Other physiological indices measured in this study did not show any difference between the subjects in the tropical group who had lived in Japan for a shorter time and those who had lived there for a longer time. There were also no significant relationships between duration of stay and other physiological responses during 60 minutes of leg immersion (P > 0.05). CONCLUSIONS: We conclude that the nature of heat acclimatization of the sweating responses to passive heat exposure that are acquired from long-term heat acclimatization is decayed by a stay in a temperate area, as shown by the subjects in our tropical group. We did not find any evidence of a decay in the other physiological indices, indicating that heat tolerance acquired from long-term heat acclimatization is not completely diminished through residence in a temperate area for less than 4 years, although some aspects of this heat tolerance may be decayed.     

Responses of native and migrant desert residents to arid heat

Four groups of Sonoran Desert residents were compared in three studies of heat tolerance. In the first two studies the task involved walking in arid heat at a moderate rate (5 km/hour) for two hours per day over a period of seven consecutive days. The first study compared seven Yaqui Indians with ten Mestizos, all lifelong residents of the same neighborhood in Hermosillo, Sonora. The groups showed no significant differences in physiological responses. The second study compared five Papago Indian students with five White students from Tucson, Arizona. The Papago showed significantly lower sweat rates and significantly lower rectal temperatures. None of the groups showed sequential changes which could be called acclimatization. The lower sweat rate of the Papago is partially the result of their smaller size, but their lower rectal temperatures may represent a more effective heat dissipating mechanism. The third study compared naturally acclimatized Yaquis and Mestizos in hot, humid conditions established by other investigators. These well acclimatized subjects responded in a manner intermediate between the unacclimatized and artificially acclimatized Caucasians reported in the literature. Thus desert acclimatization does not confer maximal acclimatization to humid heat.     

A study of nephron function in normal tropical residents using the creatinine and lithium clearances

 The kidney bears the brunt of the demands of a tropical climate for water and electrolyte homeostasis. We hypothesised that a tropical climate may cause adaptive changes in the entire organism leading to altered renal function in our subjects. Hence renal function data for residents of a temperate climate may not be applic- able to tropical residents. We therefore sought to elucidate renal function in subjects residing in a tropical climate. We used lithium clearance, C _Li, a non-invasive tool for assessing proximal tubular function in humans, and endogenous creatinine clearance, C _Cr, to estimate proximal tubular function and glomerular function, respectively, in our subjects. We did this in order to establish whether or not nephron function in our subjects differs from that for residents of a temperate climate. Nineteen male and 12 female Ghanaian subjects aged between 15 and 48 years were studied. The estimated G _Cr was 117.3±6.6 ml/min for male subjects and 97±6.4 ml/min for female subjects. C _Li was 20.3±1.6 ml/min for male and 19.1±0.4 ml/min for female subjects, respectively. The estimated absolute reabsorption rate of fluid of proximal tubules was 97.0±6.0 ml/min for males and 78.1±6.0 ml/min for females. The percentage proximal fluid reabsorption for male and female subjects was 81.2±1.4 and 79.5±1.6, respectively. The differences between male and female values (mean±SEM) were not statistically significant. The data suggest that the proximal tubule in residents of a tropical climate may reabsorb more fluid compared to that in residents of a temperate climate. Our values for proximal tubular reabsorption are higher than those reported for residents of a temperature climate. Our estimate of glomerular filtration, however, is similar to published data for Caucasians. The difference in proximal tubular function may reflect possible renal adaptation to a hot, humid climate. We conclude that renal function of tropical residents differs from that of residents of a temperate climate. This difference may be due to renal adaptation to the hot, tropical climate. Received: 1 July 1996 / Revised: 22 December 1996 / Accepted: 8 January 1997     

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 modafinil on heat thermoregulatory responses in humans at rest

The effects of modafinil on heat thermoregulatory responses were studied in 10 male subjects submitted to a sweating test after taking 200 mg of modafinil or placebo. Sweating tests were performed in a hot climatic chamber (45 degrees C, relative humidity <15%, wind speed = 0.8 m x s(-1), duration 1.5 h). Body temperatures (rectal (Tre) and 10 skin temperatures (Tsk)), sweat rate, and metabolic heat production (M) were studied as well as heart rate (HR). Results showed that modafinil induced at the end of the sweating test higher body temperatures increases (0.50 +/- 0.04 versus 0.24 +/- 0.05 degrees C (P < 0.01) for deltaTre and 3.64 +/- 0.16 versus 3.32 +/- 0.16 degrees C (P < 0.05) for deltaTsk (mean skin temperature)) and a decrease in sweating rate throughout the heat exposure (P < 0.05) without change in M, leading to a higher body heat storage (P < 0.05). AHR was also increased, especially at the end of the sweating test (17.95 +/- 1.49 versus 12.52 +/- 1.24 beats/min (P < 0.01)). In conclusion, modafinil induced a slight hyperthermic effect during passive dry heat exposure related to a lower sweat rate, probably by its action on the central nervous system, and this could impair heat tolerance.     

The change in peripheral sweating mechanisms of the tropical Malaysian who stays in Japan

Tropical subjects regulate core temperature with less amount of sweat against heat compared to temperate subjects through long-term heat-acclimatization. The purpose of the study is to determine whether acclimatization in tropical subjects decay during a stay in temperate area. The aim of this study, therefore, was to investigate the possible changes in the peripheral sweating mechanisms. Local sweating response activated by acetylcholine (ACh) applied iontophoretically among Malaysians with varying duration of stay in Japan and Japanese resident subjects. Directly activated (DIR) and axon reflex (AXR)-mediated sweating during ACh iontophoresis were measured by capacitance hygrometer (quantitative sudomotor axon reflex test, QSART) QSART was performed in a thermoneutral condition (24±0.5 °C, 40±3% rh). The sweat onset-time after the current loading was 1.05 min shorter in Malaysian with long-term stay in Japan (MLJ) than in Malaysian, and the AXR(1), AXR(2) and DIR sweating in MLJ were larger than Malaysian. From these results, suppressed neuroglandular response to ACh was confirmed in Malaysians. It is suggested that long-term heat-acclimatization acquired in tropical subjects may decay after immigration to temperate area.     

Tropical Malaysians and temperate Koreans exhibit significant differences in sweating sensitivity in response to iontophoretically administered acetylcholine

Natives of the tropics are able to tolerate high ambient temperatures. This results from their long-term residence in hot and often humid tropical climates. This study was designed to compare the peripheral mechanisms of thermal sweating in tropical natives with that of their temperate counterparts. Fifty-five healthy male subjects including 20 native Koreans who live in the temperate Korean climate (Temperate-N) and 35 native tropical Malaysian men that have lived all of their lives in Malaysia (Tropical-N) were enrolled in this study after providing written informed consent to participate. Quantitative sudomotor axon reflex testing after iontophoresis (2 mA for 5 min) with 10% acetylcholine (ACh) was used to determine directly activated (DIR) and axon reflex-mediated (AXR) sweating during ACh iontophoresis. The sweat rate, activated sweat gland density, sweat gland output per single gland activated, and oral and skin temperature changes were measured. The sweat onset time of AXR (nicotinic-receptor-mediated) was 56 s shorter in the Temperate-N than in the Tropical-N subjects (P < 0.0001). The nicotinic-receptor-mediated sweating activity AXR (1), and the muscarinic-receptor-mediated sweating activity DIR, in terms of sweat volume, were 103% and 59% higher in the Temperate-N compared to the Tropical-N subjects (P < 0.0001). The Temperate-N group also had a 17.8% (P < 0.0001) higher active sweat gland density, 35.4% higher sweat output per gland, 0.24°C higher resting oral temperature, and 0.62°C higher resting forearm skin temperature compared to the Tropical-N subjects (P < 0.01). ACh iontophoresis did not influence oral temperature, but increased skin temperature near where the ACh was administered, in both groups. These results suggest that suppressed thermal sweating in the Tropical-N subjects was, at least in part, due to suppressed sweat gland sensitivity to ACh through both recruitment of active sweat glands and the sweat gland output per each gland. This physiological trait guarantees a more economical use of body fluids, thus ensuring more efficient protection against heat stress.     

Effects of bromocriptine on sweat gland function during heat acclimatization

This study examined the involvement of the hormones aldosterone and prolactin in sweat gland function during heat acclimatization. Two groups of male subjects (n = 8) were tested - one receiving a placebo (control), the other receiving bromocriptine. Both groups performed cycle ergometer exercise at 50% of maximal oxygen uptake over 10 consecutive days in an environmental chamber maintained at 39 degrees C and 30% relative humidity. Duration of exercise was 90 min on days 2-4 and 6-9, and 45 min on test days 1, 5 and 10. Electrolyte concentrations were determined by total body washdown. Prolactin increased (p less than 0.001) during exercise on day 1 in the control group but not on days 5 and 10. In contrast, prolactin was suppressed by bromocriptine and did not rise in response to exercise or heat exposure. Plasma aldosterone increased during exercise in both groups, showing no differences between groups. The sodium concentration in sweat decreased significantly (p less than 0.05) in the control group from day 1 to 10 but was unchanged in the treatment group. These data suggest that acclimatization-related changes in sweat gland function may be attenuated by increases in central dopaminergic activity and implicate prolactin in control of sweat gland function.     

Latitudinal pattern of mountain vegetation zonation in southern and eastern Asia

A new scheme of altitudinal and latitudinal vegetation zonation is proposed for eastern Asia. The latitudinal patterns of mountain vegetation zonation show a clear boundary at ca. 20°–30° N. For the tropical mountains south of 20° N, the altitudinal series includes tropical lowland, tropical lower montane, and tropical upper montane zones. For the temperate mountains north of 30° N, the series includes temperate lowland, temperate lower montane, and temperate upper montane zones. The mountains located between 20° and 30° N show a transitional zonation pattern; the lower two zones are comparable to the lower two of the tropical zonation (tropical lowland and tropical lower montane), and the upper two zones are comparable to those of the temperate zonation (temperate lower montane and temperate upper montane). The tropical upper montane zone is not found north of 20°–30° N, while the tropical lower montane zone reaches down to sea level and constitutes the temperate lowland zone. Thus the zonation between 20° and 30° N includes tropical lowland, tropical lower montane/temperate lowland, temperate lower montane, and temperate upper montane zones. The latitudinal series of lowland rain forests follows the scheme of climatic division into tropical, subtropical/warm-temperate, cool-temperate and cold-temperate, with a shift of the respective life forms, evergreen, evergreen notophyllous, deciduous, and evergreen needle-leaved. The tropical lower montane forest can be correlated to the horizontal subtropical/ warm-temperate zone. The temperate altitudinal and latitudinal zonations above 30° N are correlated and show an inclined parallel pattern from high altitudes in the south to low altitudes down to sea level in the north.     

Influence of season on plasma antidiuretic hormone, angiotensin II, aldosterone and plasma renin activity in young volunteers

We investigated seasonal changes in hormonal and thermoregulatory responses. Eight volunteers were subjected to the experiment at four times of the year: around the vernal and autumnal equinoxes, and at the summer and winter solstices at latitude 35° N. Plasma antidiuretic hormone (ADH), angiotensin II (ANG II), aldosterone (ALD) and plasma renin activity (PRA) were analyzed before and after water immersion. Seasonal changes in thermoregulatory responses were assessed by measuring core temperature and sweat rate during immersion of the leg in hot water (at 42°C) for 30 min in a room maintained at 26°C. The concentration of plasma ADH and ALD before water immersion was significantly higher in summer than in other seasons. The concentrations of ANG II and PRA did not show seasonal variations. Changes in tympanic temperature during water immersion showed significant differences between seasons, and were higher in winter than in other seasons. The sweat rate was significantly higher in summer than in other seasons. In summary, ADH and ALD concentrations displayed a seasonal rhythm with marked elevation in summer; this may be a compensative mechanism to prevent dehydration from increased sweat loss during summer due to heat acclimatization.     

Studies on heat tolerance at rest and orthostatic heat tolerance in a hot environment

Twelve young male Japanese were exposed to a hot environment in summer, and changes in systolic blood pressure induced by changing the position from recumbent to sitting were observed. Sweating was induced in a climatic chamber at 30 degree C with 70% relative humidity by immersing both legs up to the knees into a water bath of 42 degree C for 90 min after sitting on a chair at rest for 30 min in the chamber. The mean values of rise in rectal temperature, body weight loss and mean sodium concentration in sweat were 0.62 degree C, 0.67 kg and 46 mEq/l, respectively. The mean values of fall in systolic blood pressure associated with changing posture and its recovery time were 13.7 mm Hg and 77.5 sec, respectively. Heat tolerance at rest was assessed by a numerical heat tolerance index involving relative water loss, relative rise in rectal temperature, and relative salt loss. Values of relative water loss, relative rise in rectal temperature, and the numerical heat tolerance index correlated closely to those of fall in systolic blood pressure and its recovery time.     

Photoperiodic response in the subtropical and warm‐temperate zone populations of the southern green stink bug Nezara viridula: why does it not fit the common latitudinal trend?

The photoperiodic response of diapause induction is studied in females of five subtropical and warm‐temperate zone populations of Nezara viridula (L.) (Heteroptera: Pentatomidae) in Japan (26.4–34.7°N; 127.4–135.7°E). Laboratory tests at 25 °C demonstrate that both warm‐temperate and subtropical populations have pronounced photoperiodic responses of adult diapause induction. Under short‐day conditions (LD 10 : 14 h), 73–100% of females enter diapause, whereas, under long‐day conditions (LD 15 : 9 h), 87–100% of females are nondiapause and reproduce. When the critical photoperiod for diapause induction is plotted against the latitude of origin of each population, the data points do not show the expected tendency of increasing critical photoperiod northwards but, instead, vary between 12 h 15 min and 13 h 30 min. It is suggested that adults from different populations of such a highly migratory species move often among subtropical islands (by themselves or being assisted by typhoons), thus constantly destabilizing the photoperiodic responses. Although important for general synchronization of seasonal development in the tropics and subtropics, winter diapause might not be so critical for survival in mild winters in these zones. Such circumstances might make the selective pressure over the photoperiodic response less severe in the tropics and subtropics than in the temperate zone. It is suggested that the current climate warming might contribute to this situation as well by promoting polewards migrations and lessening the selective pressure of overwintering conditions.     

Effect of heat acclimation on anxiety-like behavior of rats in an open field

To mitigate the impacts of heat exposure, animals can take some actions to maintain their core body temperature, such as heat acclimation; however, the effect of heat acclimation on anxiety-like behavior in an open field is still not understood. The purpose of this study was to examine the anxiety-like behavior of heat acclimated rats in a temperate or heated open field. After being raised in a 23 °C environment for one week, male Wistar rats were exposed to a heated environment (32 °C) for 3 h (3H), 14 days (14D), or 28 days (28D), with free access to food and water, and compared with rats reared in a temperate environment (23 °C; Cont). After heat exposure, behavioral changes were monitored using an open field test (OFT) in a heated (32 °C) or temperate environment (23 °C). Compared with those in the Cont group, the body weights of rats in the 14D and 28D groups were lower. The OFT in the heated environment showed that grooming time was longer in 3H and 14D rats. In the temperate environment, grooming time was longer in all the heated groups. Rats from the 3H and 28D groups spent longer time in the center square when tested in the temperate environment. Rearing activity increased in 28D rats in the temperate environment, while the number of line crossings did not differ significantly between the heated groups and the two open fields. These results suggest that heat acclimation affected not only the physiological index such as core body temperature but also the anxiety-like behavior, mainly in the temperate open field. These changes might be beneficial when rats are faced with an open field.     

陕西种子植物区系地理初步研究

陕西约有种子植物３９０７种,隶属于１７７科１１１５属,其中热带属３２８属（２９４４％）,温带属６４５属（５８１１％）,中国特有属５３属（４７５％）。区系地理成分分析表明,北温带分布属是其植物区系的核心,反映出区系的温带性质。然而这些温带区系成分并非起源于北方,而是亚热带山区起源,是华夏植物区系的北向延伸,其与亚热带和热带植物区系成分有着共同的起源,是华夏植物区系的组成部分。由于特殊的地理位置,决定了其成为多种地理成分的汇集之地,并表现出由亚热带向温带过渡的区系特点。此外区系中单、少种科、属及古特有属相对丰富,体现出区系的古老性。     

Diapause and cold tolerance in Asian species of the parasitoid Leptopilina (Hymenoptera: Figitidae)

Diapause and cold tolerance are essential for temperate insects to pass the winter, with the mechanisms controlling these two traits varying considerably among insects. In the present study, diapause and cold tolerance are compared among three Leptopilina species: Leptopilina japonica Novkovi? & Kimura, Leptopilina victoriae Nordlander and Leptopilina ryukyuensis Novkovi? & Kimura, all larval parasitoids of frugivorous drosophilid flies, with the aim of understanding their climatic adaptations. The first species is divided into the temperate (Leptopilina japonica japonica) and subtropical subspecies (Leptopilina japonica formosana), and the latter two species are distributed in the tropical and subtropical regions. The temperate subspecies of L. japonica enters prepupal diapause at low temperatures (15 or 18 °C), irrespective of photoperiod, and some individuals enter diapause when exposed to 0 °C for 1 or 2 day(s) or when placed at low humidity. Leptopilina victoriae also shows signs of diapause initiation at 15 °C, although L. ryukyuensis and L. j. formosana from the subtropical regions do not. Preimaginal viability at low temperature (13, 14 or 15 °C) is usually lower in L. victoriae from the tropical regions compared with L. japonica or L. ryukyuensis from the temperate or subtropical regions. Diapausing prepupae of the temperate subspecies appear to be cold tolerant. However, the cold tolerance of nondiapausing prepupae, pupae and adult females varies little among the tropical, subtropical and temperate species or subspecies, and adult males of the temperate subspecies of L. japonica are less cold tolerant than those of the tropical or subtropical species or subspecies. Cold tolerance may be unnecessary, except for diapausing individuals of the temperate species, because nondiapausing individuals appear in warmer seasons.