Respiratory Evaporative Water Loss Research Articles

Comparing the Contributions of Cutaneous and Respiratory Evaporative Water Loss to Cooling in Anna’s Hummingbirds (Calypte anna) Under Fasted and Fed Conditions

During high-temperature periods, endothermic animals evaporate water from the body surface to cool down. The two primary routes of evaporative water loss are: (1) evaporating water from the skin; and (2) evaporation from the respiratory surfaces during breathing and panting. In smaller avian species like Anna's hummingbirds ( Calypte anna), the higher cutaneous surface area to volume ratio presents an opportunity for the skin to become an important avenue for evaporative cooling, possibly becoming a major site. Additionally, hummingbirds feed on water-rich nectar. As a result, they eliminate surplus water through urination, but significant evaporation can also occur through their skin and respiratory system. Thus, total evaporative water loss could rise significantly for these animals when in a hydrated state. Here, this study investigates the relative importance of the two evaporative water loss routes (cutaneous and respiratory) of Anna's hummingbirds in fed and fasted states. We hypothesize that cutaneous evaporation has a high contribution to total evaporation. Moreover, we predict that evaporative water loss rates are higher under the fed (hydrated) condition relative to fasted states. Metabolic and evaporation rates from the head and the body were measured separately in a partitioned chamber at 30°C. Birds were fed immediately prior to entry into respirometry, and the transition from fed to fasted states was recorded over a two-hour period. Total evaporative water loss nearly doubled in the fed versus fasted condition (1.75 ± 0.85 mg H2O/min and 0.97 ± 0.28 mg H2O/min, respectively), with respiratory water loss being significantly higher in the fed compared to the fasted condition (0.87 ± 0.38 mg H2O/min versus 0.42 ± 0.12 mg H2O/min, respectively). On the other hand, the body had a large, but non-significant, difference in evaporative water loss rates between the fed and fasted conditions (0.88 ± 0.55 mg H2O/min and 0.57 ± 0.17 mg H2O/min, respectively). Importantly, cutaneous evaporative water loss made up half of the total evaporation in both the fed and fasted conditions. These results demonstrate that evaporative water loss is modulated by hydration status at both the respiratory and cutaneous surfaces. Furthermore, cutaneous evaporation makes up approximately the same proportion of total evaporation to other birds at thermoneutral temperatures. Future work manipulating ambient temperature in conjunction with hydration status will further our understanding of the relative importance of cutaneous evaporation for these small-bodied birds. Funded by the Genentech Foundations Scholarship, CSUPERB New Investigator Grant, and San Francisco State University. This is the full abstract presented at the American Physiology Summit 2024 meeting and is only available in HTML format. There are no additional versions or additional content available for this abstract. Physiology was not involved in the peer review process.

Similarity of Crocodilian and Avian Lungs Indicates Unidirectional Flow Is Ancestral for Archosaurs

Patterns of airflow and pulmonary anatomy were studied in the American alligator (Alligator mississippiensis), the black caiman (Melanosuchus niger), the spectacled caiman (Caiman crocodilus), the dwarf crocodile (Osteolaemus tetraspis), the saltwater crocodile (Crocodylus porosus), the Nile crocodile (Crocodylus niloticus), and Morelet's crocodile (Crocodylus moreletii). In addition, anatomy was studied in the Orinoco crocodile (Crocodylus intermedius). Airflow was measured using heated thermistor flow meters and visualized by endoscopy during insufflation of aerosolized propolene glycol and glycerol. Computed tomography and gross dissection were used to visualize the anatomy. In all species studied a bird-like pattern of unidirectional flow was present, in which air flowed caudad in the cervical ventral bronchus and its branches during both lung inflation and deflation and craniad in dorsobronchi and their branches. Tubular pathways connected the secondary bronchi to each other and allowed air to flow from the dorsobronchi into the ventrobronchi. No evidence for anatomical valves was found, suggesting that aerodynamic valves cause the unidirectional flow. In vivo data from the American alligator showed that unidirectional flow is present during periods of breath-holding (apnea) and is powered by the beating heart, suggesting that this pattern of flow harnesses the heart as a pump for air. Unidirectional flow may also facilitate washout of stale gases from the lung, reducing the cost of breathing, respiratory evaporative water loss, heat loss through the heat of vaporization, and facilitating crypsis. The similarity in structure and function of the bird lung with pulmonary anatomy of this broad range of crocodilian species indicates that a similar morphology and pattern of unidirectional flow were present in the lungs of the common ancestor of crocodilians and birds. These data suggest a paradigm shift is needed in our understanding of the evolution of this character. Although conventional wisdom is that unidirectional flow is important for the high activity and basal metabolic rates for which birds are renowned, the widespread occurrence of this pattern of flow in crocodilians indicates otherwise. Furthermore, these results show that air sacs are not requisite for unidirectional flow, and therefore raise questions about the function of avian air sacs.

Partitioning of evaporative water loss into respiratory and cutaneous pathways in Wahlberg's epauletted fruit bats (Epomophorus wahlbergi).

The relative contributions of respiratory and cutaneous evaporation to total evaporative water loss (TEWL) and how the partitioning of these two avenues varies with environmental temperature has received little attention in bats. We trained Wahlberg's epauletted fruit bats (Epomophorus wahlbergi) captured in Pretoria, South Africa, to wear latex masks while hanging in respirometry chambers, and we measured respiratory evaporative water loss (REWL) and cutaneous evaporative water loss (CEWL) over air temperatures (Ta) from 10° to 40°C. The bats' normothermic body temperature (Tb) was approximately 36°C, which increased at higher Ta to 40.5° ± 1.0°C at Ta ≈ 40°C. Both TEWL and resting metabolic rate (RMR) increased sharply at Ta >35°C, with a mean TEWL at 40°C equivalent to 411% of that at 30°C. The increase in TEWL was driven by large increases in both CEWL and REWL. CEWL comprised more than 50% of TEWL over the entire Ta range, with the exception of Ta ≈ 40°C, where REWL accounted for 58% of evaporative water loss. Surface area-specific CEWL increased approximately sixfold with increasing Ta. Thermoregulation at Ta approaching or exceeding Tb involved a considerable energetic cost, with RMR at Ta ≈ 40°C exceeding by 24% that measured at Ta ≈ 10°C. Our data do not support recent arguments that respiratory gas exchange across the wing membranes represents 5%-10% of the total in E. wahlbergi.

Climate influences thermal balance and water use in African and Asian elephants: physiology can predict drivers of elephant distribution

Elephant movement patterns in relation to surface water demonstrate that they are a water-dependent species. Thus, there has been interest in using surface water management to mitigate problems associated with localized elephant overabundance. However, the physiological mechanisms underlying the elephant's water dependence remain unclear. Although thermoregulation is likely an important driver, the relationship between thermoregulation, water use and climate has not been quantified. We measured skin surface temperature of and cutaneous water loss from 13 elephants (seven African, 3768±642 kg; six Asian, 3834±498 kg) and determined the contribution of evaporative cooling to their thermal and water budgets across a range of air temperatures (8-33°C). We also measured respiratory evaporative water loss and resting metabolic heat production on a subset of elephants (N=7). The rate of cutaneous evaporative water loss ranged between 0.31 and 8.9 g min(-1) m(-2) for Asian elephants and 0.26 and 6.5 g min(-1) m(-2) for African elephants. Simulated thermal and water budgets using climate data from Port Elizabeth, South Africa, and Okaukuejo, Namibia, suggested that the 24-h evaporative cooling water debt incurred in warm climates can be more than 4.5 times that incurred in mesic climates. This study confirms elephants are obligate evaporative coolers but suggests that classification of elephants as water dependent is insufficient given the importance of climate in determining the magnitude of this dependence. These data highlight the potential for a physiological modeling approach to predicting the utility of surface water management for specific populations.

Respiratory evaporative water loss during hovering and forward flight in hummingbirds

Hummingbirds represent an end point for small body size and water flux in vertebrates. We explored the role evaporative water loss (EWL) plays in management of their large water pool and its use in dissipating metabolic heat. We measured respiratory evaporative water loss (REWL) in hovering hummingbirds in the field (6 species) and over a range of speeds in a wind tunnel (1 species) using an open-circuit mask respirometry system. Hovering REWL during the active period was positively correlated with operative temperature (T e) likely due to some combination of an increase in the vapor-pressure deficit, increase in lung ventilation rate, and reduced importance of dry heat transfer at higher T e. In rufous hummingbirds ( Selasphorus rufus; 3.3 g) REWL during forward flight at 6 and 10 m/s was less than half the value for hovering. The proportion of total dissipated heat (TDH) accounted for by REWL during hovering at T e > 40 °C was < 40% in most species. During forward flight in S. rufus the proportion of TDH accounted for by REWL was ~ 35% less than for hovering. REWL in hummingbirds is a relatively small component of the water budget compared with other bird species (< 20%) so cutaneous evaporative water loss and dry heat transfer must contribute significantly to thermal balance in hummingbirds.

Comparative physiology of Australian quolls (Dasyurus; Marsupialia)

Quolls (Dasyurus) are medium-sized carnivorous dasyurid marsupials. Tiger (3,840 g) and eastern quolls (780 g) are mesic zone species, northern quolls (516 g) are tropical zone, and chuditch (1,385 g) were once widespread through the Australian arid zone. We found that standard physiological variables of these quolls are consistent with allometric expectations for marsupials. Nevertheless, inter-specific patterns amongst the quolls are consistent with their different environments. The lower T (b) of northern quolls (34 degrees C) may provide scope for adaptive hyperthermia in the tropics, and they use torpor for energy/water conservation, whereas the larger mesic species (eastern and tiger quolls) do not appear to. Thermolability varied from little in eastern (0.035 degrees C degrees C(-1)) and tiger quolls (0.051 degrees C degrees C(-1)) to substantial in northern quolls (0.100 degrees C degrees C(-1)) and chuditch (0.146 degrees C degrees C(-1)), reflecting body mass and environment. Basal metabolic rate was higher for eastern quolls (0.662 +/- 0.033 ml O(2) g(-1) h(-1)), presumably reflecting their naturally cool environment. Respiratory ventilation closely matched metabolic demand, except at high ambient temperatures where quolls hyperventilated to facilitate evaporative heat loss; tiger and eastern quolls also salivated. A higher evaporative water loss for eastern quolls (1.43 +/- 0.212 mg H(2)O g(-1) h(-1)) presumably reflects their more mesic distribution. The point of relative water economy was low for tiger (-1.3 degrees C), eastern (-12.5 degrees C) and northern (+3.3) quolls, and highest for the chuditch (+22.6 degrees C). We suggest that these differences in water economy reflect lower expired air temperatures and hence lower respiratory evaporative water loss for the arid-zone chuditch relative to tropical and mesic quolls.

Thermoregulation in ratites: a review

Laboratory and free-ranging studies on the emu, ostrich and kiwi show ratites to be competent homeotherms. While body temperature and basal metabolic rate are lower in ratites than other birds, all of the thermoregulatory adaptations present in other birds are well established in ratites. The thermoneutral zone has been established for the emu and kiwi, and extends to 10°C. Below that zone, homeothermy is achieved via the efficient use of insulation and elevated metabolic heat production. In the heat, emus and ostriches increase respiratory evaporative water loss and use some cutaneous water loss. Respiratory alkalosis is avoided by reducing tidal volume. In severe heat, tidal volume increases, but the emu becomes hypoxic and hypocapnic, probably by altering blood flow to the parabronchi, resulting in ventilation/perfusion inhomogeneities. Ostriches are capable of uncoupling brain temperature from arterial blood temperature, a phenomenon termed selective brain cooling. This mechanism may modulate evaporative effector responses by manipulating hypothalamic temperature, as in mammals. The implications of thermal physiology for ratite production systems include elevated metabolic costs for homeothermy at low ambient temperature. However, the emu and ostrich are well adapted to high environmental temperatures.

Water turnover and the northern range of the koala (Phascolarctos cinereus).

Water turnover for koalas is positively correlated with the moisture content of selected trees suggesting that browse choice was driven by water requirements in summer but energy demands in winter. We compared the distribution of the koala to relative humidity and found that the bioregional delineation of the koala?s range corresponds closely to regions experiencing an average 9am relative humidity of less than 80% in February. This indicates that the northern coastal distribution of the koala may be limited by respiratory evaporative water loss as a cooling mechanism.

Water conservation in fasting northern elephant seals (Mirounga angustirostris).

Prolonged terrestrial fasting is a key element in the life history of elephant seals. While on land seals typically fast without access to fresh water, and thus must maintain positive water balance by reductions in water loss such that they can subsist primarily on metabolic water production (MWP). The terrestrial apnea demonstrated by seals may reduce respiratory evaporative water loss (REWL) to levels that allow seals to make a net gain of water from MWP. We empirically measured REWL in 13 fasting northern elephant seal pups and determined the effects on water conservation of a breathing mode that incorporates a regular pattern of apneas, of > or =1 min in duration, followed by eupneic recovery, compared with a breathing mode with no apneas longer than 20 s and resembling typical breathing patterns in other mammals (normative breathing). Overall REWL fell 41% from 0.075+/-0.013 g min(-1) (mean +/- s.d.) during normative breathing to 0.044+/-0.006 g min(-1) during apneic breathing. The decline in REWL is attributed to a decrease in overall ventilation rate, made possible by a decline in metabolic rate along with an increase in oxygen extraction that would occur during apneic breathing. Data on the range of ambient humidity conditions at the local breeding site were collected and used to bound the range of environmental conditions used in laboratory measurements. Our data showed that the observed variations in ambient humidity had no significant effect on REWL. A combination of apneic breathing and the complex nasal turbinates allows fasting elephant seals to reduce REWL well below the rate of MWP so that they can maintain water balance during the fast.

Operation Everest III: energy and water balance.

We hypothesized that hypoxia decreases energy intake and increases total energy requirement and, additionally, that decreased barometric pressure increases total water requirement. Energy and water balance was studied over 31 days in a hypobaric chamber at 452-253 Torr (corresponding to 4,500-8,848 m altitude), after 7 days acclimatization at 4,350 m. Subjects were eight men, age 27+/-4 years (mean+/-SD), body mass index 22.9+/-1.5 kg/m2. Food and water intake was measured with weighed dietary records, energy expenditure and water loss with labelled water. Insensible water loss was calculated as total water loss minus urinary and faecal water loss. Energy intake at normoxia was 13.6+/-1.8 MJ/d. Energy intake decreased from 10.4+/-2.1 to 8.3+/-1.9 MJ/d (P<0.001) and energy expenditure from 13.3+/-1.6 to 12.1+/-1.8 MJ/d (P<0.001) over the first and second 15-day intervals of progressive hypoxia. Absolute insensible water loss did not change (1.67+/-0.26 and 1.66+/-0.37 l/d), however, adjusted for energy expenditure it increased with ambient pressure reduction (P<0.05). In conclusion, hypoxia induced a negative energy balance, mainly by a reduction of energy intake. Overall insensible water loss was unchanged because the increase in respiratory evaporative water loss was counterbalanced by a decrease in metabolic rate that probably limited the hypoxia-induced increase in ventilation.

Pharmacological properties of traditional medicines. XXV. Effects of ephedrine, amygdalin, glycyrrhizin, gypsum and their combinations on body temperature and body fluid.

Effects of ephedrine, amygdalin, glycyrrhizin, gypsum and their combinations on body temperature and body fluid were studied in rats using the method developed in our previous reports. Ephedrine significantly increased respiratory evaporative water loss and heat loss in response to a marked elevation of body temperature. There was a small but significant increase in body temperature when amygdalin was orally given rats at a dose of 46.32 mg/kg. Glycyrrhizin and gypsum were unable to affect body temperature. However, gypsum was able to prevent the increased action of ephedrine on body temperature, amygdalin exhibited a preventive tendency to it, and glycyrrhizin did not affect it. The results are in good agreement with classical claims of Makyo-kanseki-to and the related crude drugs in traditional medicine. Moreover, a combination of the four components reproduced the effects of Makyo-kanseki-to on body temperature and body fluid. This report suggests that the co-administration of ephedrine and gypsum is physiologically more desirable than ephedrine alone for dry-type asthmatic patients with a fever. Also, it experimentally supports the clinical efficacy of Makyo-kanseki-to.

Standard Evaporative Water Loss and Metabolism of Juvenile Varanus mertensi (Squamata: Varanidae)

Evaporative water loss (EWL) varies considerably both within and between reptile species (Dmi'el, 1985; Eynan and Dmi'el, 1993; Lahav and Dmi'el, 1996) and can also be affected by acclimation (Hillman et al., 1979; Kobayashi et al., 1983). EWL data are available for a wide variety of reptiles from various habitats (see review by Mautz, 1982) but are limited for goannas under controlled conditions (Warburg, 1965; Green, 1969; Thompson and Withers, 1997a). For lizards, such as goannas, body water is lost by evaporation from the skin (including the eyes) and the respiratory passages and as a mixture of urine and feces (and in some species from nasal salt glands; Green, 1969; Saint Girons et al., 1981). The rate of cutaneous evaporative water loss (CEWL) is largely determined by the exposed surface area of the skin and eyes, the resistance of these surfaces to evaporation, and the difference in water vapor concentrations across the surfaces. The respiratory evaporative water loss (REWL) is determined mainly by the lung ventilation rate and body temperature but may be reduced by nasal countercurrent heat and water exchange (Mautz, 1980). Environmental conditions such as ambient temperature, relative humidity, and wind velocity also affect EWL (Thorpe and Kontogiannis, 1977; Mautz, 1980, 1982). EWL is generally higher for mesic reptiles than arid species (Snyder, 1971; Dmi'el, 1972; Shoemaker and Nagy, 1977), and we would expect the EWL of a semiaquatic goanna to be higher than for comparable terrestrial species. However, there are no data for EWL of semiaquatic goannas under controlled conditions. The semiaquatic goanna Varanus mertensi has a much higher field water turnover (WTR) than predicted for lizards from arid and tropical zones (Christian et al., 1996), but it is not clear whether their high WTR is associated with a high cutaneous EWL, respiratory EWL, water excretion, or a combination thereof. This study examines the standard EWL (EWL,td) and standard metabolic rate (VO2std) for juvenile V mertensi. The primary objectives were to measure total evaporative water loss and calculate resistance to water evaporation under standardized laboratory conditions (TEWLtd, rstd), and to partition TEWLStd and rstd into its respiratory and cutaneous components. Thompson and Withers (1997a) report TEWL,td and resistance to total water loss (rtota) for a number of terrestrial and arboreal Western Australian

Selective brain cooling reduces respiratory water loss during heat stress

Terrestrial mammals developed sereral mechanisms to reduce water loss to counteract water shortage. One avenue of water loss is the evaporative heat loss by sweating and panting, which increasis with body temperature. Sweating and panting are activated by temperature signals of the body, whereby the brain is the most important site in generating temperature signals. Goats, like other artiodactyls, can cool their brains selectively below the temperature of the trunk core. The aim of the present study is to determine whether an inhibition of the selective brain cooling (SBC) mechanism will increase substantially the respiratory evaporative water loss during heat stress due to the higher brain temperature. The inhibition of SBC was performed by increasing brain temperature experimentally at the same rate as trunk temperature by means of extracorporeal heat exchangers. These experiments without SBC resulted in higher respiratory evaporative water loss compared to experiments with normal SBC. Eighteen experiments in two conscious goats had shown that at a trunk temperature of 40°C the respiratory water loss was reduced on average by 29 g/hr (0.7 l/day) due to the effect of SBC. This amount of water corresponds to about one third of the general water requirements. In conclusion, SBC substantially reduces the water loss in goats during heat stress and consequently improves survival chances during water shortage.

Central application of a nitric oxide donor activates heat defense in the rabbit

In chronically instrumented, conscious rabbits at moderately warm ambient thermal conditions, infusion of the NO-donor SIN-1 into the anterio-ventral 3rd cerebral ventricle (1–2 μg/min per kg BW, 2–4 μl/min, 30 min) initiated a co-ordinated activation of autonomic heat loss mechanisms, as indicated by the rise in ear skin temperature and by increases in panting frequency and respiratory evaporative water loss, while oxygen consumption decreased slightly. The heat loss responses were similar to those attributed to NO in studies employing systemic application of NO-donors. Different from NO acting peripherally, which causes arterial hypotension and tachycardia, centrally acting NO induced arterial hypertension and bradycardia. The observation of the same heat loss responses despite opposing circulatory actions suggests that NO is specifically involved in thermoregulation as a central activator of heat defense mechanisms.

Respiratory and cutaneous evaporative water loss at high environmental temperatures in a small bird

We measured rates of respiratory and cutaneous evaporative water loss as a function of air temperature in a small desert bird, the verdin Auriparus flaviceps. Birds were placed in a two-compartment metabolic chamber that separately collected water evaporated from the bird's head and body. Cutaneous and respiratory evaporative water loss, as well as CO2 production, were measured in resting birds at 2 &deg;C intervals between 30 and 50 &deg;C. Metabolic rate was lowest at 38 &deg;C (19 mW g-1) and increased to 28 mW g-1 at 50 &deg;C. At the lowest air temperature, 30 &deg;C, resting metabolic rate was 34 mW g-1. As air temperature increased from 30 to 50 &deg;C, cutaneous water loss increased from 3.3 to 10.3 mg g-1 h-1 and respiratory water loss increased from 2.1-64.1 mg g-1 h-1. At moderate air temperatures (30-36 &deg;C), water loss was divided almost evenly between respiratory and cutaneous components. As air temperature increased, however, verdins became heavily dependent on respiratory evaporation for heat dissipation. Evaporative water loss data for other species at high air temperatures suggest that partitioning of water loss may follow two different patterns. Evaporative heat dissipation may depend primarily on either cutaneous or respiratory modes of evaporative heat transfer. The physiological mechanisms and functional significance of these contrasting patterns of evaporative heat loss remain unknown.

Hypothalamic thermal stimulation modulates vasopressin release in hyperosmotically stimulated rabbits

Under thermoneutral conditions conscious rabbits received systemic infusions of NaCl as hypertonic solution (90 mueq.min-1.kg body wt-1), which raised their plasma osmolality from 283 to 312 mosmol/kgH2O. Rabbits receiving isotonic saline served as controls. Hypertonic stimulation induced a 60% reduction of both respiratory frequency and evaporative water loss. Rectal temperature rose by 0.4 degrees C despite enhanced peripheral vasodilation as indicated by increased ear skin temperature. Plasma vasopressin (AVP), aldosterone (ALDO), and corticosterone (COR) were significantly elevated from 6 to 16 pg/ml, 90 to 180 pg/ml, and 17 to 40 ng/ml, respectively. To elucidate the importance of central temperature for AVP and adrenal corticosteroid release, hypothalamic thermal stimulations (20 min) were superimposed during established iso- and hyperosmotic steady-state conditions. Different from isosmotic controls, hyperosmotic animals responded to hypothalamic cooling (37 degrees C) with a significant decrease in plasma AVP from 16 to 13 pg/ml and to hypothalamic warming (41 degrees C) with a significant rise from 16 to 19 pg/ml. A weak temperature effect on COR release was also disclosed, especially of hypothalamic cooling, which significantly lowered plasma COR from 42 to 34 ng/ml. These results provide evidence for positive local temperature coefficients of hypothalamic control of AVP release and suggest a similar property also for the control of COR release by the hypothalamo-adenohypophysial axis.

Respiratory Function in Exercising Fowl Following Occlusion of the Thoracic Air Sacs

ABSTRACT Oxygen consumption, respiratory evaporative water loss, respiratory rate and gas tensions in the clavicular and abdominal air sacs and in arterial blood were monitored after occluding either the cranial thoracic air sac only (CRT group) or the cranial and caudal thoracic air sacs together (CRT-CT group). Respiratory water loss was used to estimate minute ventilation. Both experimental groups were able to maintain control levels of ventilation at rest and during treadmill exercise at approximately three times the resting metabolic rate. The CRT group regulated blood and intrapulmonary and normally, but there was a slight hypoxaemia/hypercapnaemia in the CRT-CT group, apparently as a result of parabronchial hypoventilation. The differential distribution of gas tensions between the cranial and caudal groups of air sacs was the same in control and experimental birds, suggesting that a normal intrapulmonary airflow pattern was preserved in the absence of the thoracic air sacs. The findings are discussed in the light of current models of the control of intrapulmonary airflow in birds.

Nasal heat and water exchange in gray seals.

Metabolic rate (MR), expired air temperature (Tex), respiratory frequency (f), respiratory minute volume (V), and skin (Ts) and body (Tb) temperatures were recorded in three gray seals (Halichoerus grypus) at ambient air temperatures (Ta) between -40 and +20 degrees C. At Ta within the thermoneutral zone, MR averaged 3.7 W.kg-0.75, while mean V was 0.26 1.min-1.kg-0.75. At Ta below -11 degrees C [apparent lower critical temperature (Tlc)], both MR and V increased linearly with decreasing Ta. Average maximum MR (9.6 W.kg-0.75) and V (0.57 1.min-1.kg-0.75) were both recorded at Ta of -40 degrees C. Tex decreased with decreasing Ta to an average minimum value of 8 degrees C at Ta of -30 degrees C. The highest Tex recorded was 32 degrees C at Ta of +20 degrees C. At Ta of -20 degrees C, both total respiratory heat loss, with one exception, and respiratory evaporative water loss reached their lowest values. At this Ta, 66% of the heat and 80% of the water added to the inspired air were regained on expiration. We suggest that nasal heat exchange may be of considerable importance for thermal and water balance in many pinnipeds.

Respiratory and cardiovascular responses to spinal cord cooling at thermoneutral, low and high ambient temperatures in the chicken

1. Respiratory and cardiovascular responses of six chickens to spinal cord cooling (temperature of vertebral canal =34±0.8°C) were measured during thermoneutral (23°C), low (9°C) and high (34°C) ambient temperatures (Ta). 2. Spinal cord cooling at 23°CTa caused immediate increases compared to resting values in O2 consumption (128%), CO2 production (112%), minute volume (\(\dot V_E \); 125%), heart rate (HR; 113%) and cardiac output (CO; 127%). Similar responses, of greater magnitude, were found compared to resting values at 9°CTa when the spinal cord was cooled during thatTa: O2 consumption=139%; CO2 production=136%;\(\dot V_E \)=156%; HR=126%; and CO=157%. 3. In contrast, spinal cord cooling at 34°CTa caused no significant changes in O2 consumption or CO2 production compared to resting values, while\(\dot V_E \) and CO decreased. 4. There were no major changes in\(P_{O_2 } \),\(P_{CO_2 } \) or pH of the blood produced by spinal cord cooling, but a significant arterial hypocapnia and increased arterial and venous\(P_{O_2 } \) occurred at highTa. 5. Both CO and\(\dot V_E \) were linearly related to oxygen consumption among all the groups studied. However, some independence of respiration from O2 consumption, presumably because of thermoregulatory demand to increase respiratory evaporative water loss, was observed at the high ambient temperature.

Thermoregulation in Erythrocebus patas: a thermal balance study.

A thermal balance study over an ambient temperature (Ta) range of 15-40 degrees C was performed on six nonacclimated patas monkeys (Erythrocebus patas) weighing between 3.9 and 6.0 kg. O2 consumption, CO2 production, mean weighted skin temperature (Tsk), rectal temperature (Tre), respiratory evaporative water loss (Eresp), and total evaporative water loss (Etot) were measured continuously after equilibration at each Ta. Tsk increased as Ta increased, whereas Tre was maintained between 37.6 and 38.4 degrees C at Ta from 15 to 40 degrees C. Total evaporative heat losses increased with increasing Ta to a mean value of 76 W/m2 at 40 degrees C. Eresp was relatively constant and increased from 1.0 to 8.0 W/m2 at 15 and 40 degrees C, respectively. Whole-body conductance was similar to that previously reported for Macaca mulatta except at the highest Ta (40 degrees C), where the values for the patas monkey were significantly lower than those reported for the rhesus monkey (rhesus = 72 W/m2; patas = 33 W/m2). The data demonstrate that the patas monkey can maintain its core temperature within a narrow range over a wide range of Ta values. Additionally, Etot in the patas monkey is significantly higher than what has been reported in other nonhuman primates and approaches that reported in humans.