Ventilation and oxygen consumption in rosy finches and house finches at sea level and high altitude

Summary Rosy finches (Leucosticte arctoa) breed at altitudes above 3500 m in eastern California. House finches (Carpodacus mexicanus) belong to the same subfamily (Carduelinae), but breed at much lower elevations. Oxygen consumption ( ) and ventilatory parameters of these two species were measured over a wide range of ambient temperatures (T _a) at low altitude (LA; 150 m) and at high altitude (HA; 3800 m).Minimal nighttime 's of rosy finches and house finches at LA (T _a=30°C) were close to allometrically predicted values for passerine birds. At both altitudes, increased linearly with decreasingT _a betweenT _a=20 and –10°C. Resting 's were slightly higher at HA than at LA on average.In both species, minute volume ( ) was inversely related toT _a.T _a-correlated increases in resulted from significant increases in both ventilatory frequency (f) and tidal volume (V T) at both altitudes. Oxygen extraction efficiency ( ) was independent ofT _a in rosy finches at LA, but declined significantly with decreasingT _a in rosy finches at HA and in house finches at both altitudes.At a givenT _a, both species had significantly greater (BTPS) at HA than at LA. Altitude-correlated increases in resulted primarly from increases inf with little change inV T. was significantly greater at HA than at LA in both species.In spite of the difference in altitudinal distributions of rosy finches and house finches, there were few conspicuous interspecific differences in metabolic or ventilatory adaptation to altitude or lowT _a over the range of conditions examined.Symbols and abbreviations BMR basal metabolic rate - BTPS at body temperature and pressure, saturated - oxygen extraction efficiency - f ventilation frequency - h mean coefficient of heat transfer - HA high altitude - instantaneous oxygen consumption - LA low altitude - RH relative humidity - SMR standard metabolic rate - STPD standard temperature and pressure, dry - T temperature - a ambient - b body - lc lower critical of thermoneutral zone - minute volume - V T tidal volume     

Alveolar PCO2 oscillations and ventilation at sea level and at high altitude.

This study examines the potential for a ventilatory drive, independent of mean PCO2, but depending instead on changes in PCO2 that occur during the respiratory cycle. This responsiveness is referred to here as "dynamic ventilatory sensitivity." The normal, spontaneous, respiratory oscillations in alveolar PCO2 have been modified with inspiratory pulses approximating alveolar PCO2 concentrations, both at sea level and at high altitude (5,000 m, 16,400 ft.). All tests were conducted with subjects exercising on a cycle ergometer at 60 W. The pulses last about half the inspiratory duration and are timed to arrive in the alveoli during early or late inspiration. Differences in ventilation, which then occur in the face of similar end-tidal PCO2 values, are taken to result from dynamic ventilatory sensitivity. Highly significant ventilatory responses (early pulse response greater than late) occurred in hypoxia and normoxia at sea level and after more than 4 days at 5,000 m. The response at high altitude was eliminated by normalizing PO2 and was reduced or eliminated with acetazolamide. No response was present soon after arrival (<4 days) at base camp, 5,000 m, on either of two high-altitude expeditions (BMEME, 1994, and Kanchenjunga, 1998). The largest responses at 5,000 m were obtained in subjects returning from very high altitude (7,100-8,848 m). The present study confirms and extends previous investigations that suggest that alveolar PCO2 oscillations provide a feedback signal for respiratory control, independent of changes in mean PCO2, suggesting that natural PCO2 oscillations drive breathing in exercise.     

Aldosterone dynamics during graded exercise at sea level and high altitude.

Hormonal responses to graded exercise of eight low altitude residents were examined at sea level (SL) and after 1 (acute) and 11 (chronic) days at 4,300 m (HA). Caloric, water, and electrolyte intakes were controlled, as were temperature and humidity. Blood was sampled at rest and during light and moderate upright bicycle exercise (20 min at 40% and 75% of maximal O2 uptake, respectively). Mean VO2 max at HA was 27% lower than at SL. Resting plasma levels of aldosterone (Aldo), renin, and angiotensin II (A II) were significantly lower (P smaller than 0.05) on day 1 at HA compared to SL, but returned to SL values by day 11. Plasma cortisol values at rest were similar at SL and HA and were not significantly altered by light or moderate exercise. Renin, A II, and Aldo rose progressively with increasing workload in each environment. With acute HA, renin and Aldo were lower than at either SL or chronic HA. The chronic HA levels tended to approximate SL findings, implying adaptation. The data suggest that aldosterone is predominantly under the control of the renin-angiotensin system during graded exercise at sea level and that the response of this system is altered on acute high-altitude exposure.     

The pressure tolerance of deep sea amphipods collected at their ambient high pressure

• 1.1. Deep sea benthic amphipods were collected at their normal ambient pressure of 394–442 atm from depths of approximately 4000 m (Parulicella caperesca, Orchomene sp. and other species).
• 2.2. Their activity at their normal pressure and temperature was observed and the responses to a standard pressure test were noted.
• 3.3. Contrary to a prediction derived from the responses of similar animals from lesser depths, the 4000 m amphipods did not convulse at high pressure although they exhibited mild hyperexcitability above 400 atm followed by a progressive inhibition of activity starting at approximately 700 atm.
• 4.4. In failing to convulse at high pressure the amphipods from 4000 m differ radically in their pressure tolerance from those which live at depths down to 2700 m.

     

Body water metabolism in high altitude natives during and after a stay at sea level

Body fluid compartments were studied in a group of high altitude natives after a stay of two months at sea level and during 12 days at an altitude of 3,500 m. Measurements of total body water and extracellular water were made on day 3 and 12 of reinduction to altitude, while plasma volume was measured on day 12 only. The intracellular water, blood volume and red cell mass were computed from the above parameters. Total body water and intracellular water decreased by 3.3% (P<0.001) and 5.0% (P<0.001) respectively by the 3rd day at altitude and did not change thereafter. Extracellular water increased progressively at altitude, but the increase was not significant. Blood volume and red cell mass increased significantly while plasma volume decreased at altitude. These data were compared with that of low landers. This study suggested body hypohydration on high altitude induction in low landers as well as in high altitude natives on reinduction.     

Comparison of the reproductive performance of rats at high altitude (3,800m) and at sea level

Estrous cycles and reproductive performance were compared among rats born at high altitude, rats of Berkeley stock transported to 3,800 m, and sea level controls. Disturbances of reproductive function observed in experimental groups were not due to reduced food intake. Estrous cycles of Berkeley stock at 3,800 m were normal, whereas cycles of high altitude native rats were irregular and fertility was impaired. Litter size was reduced in both groups at high altitude with fewer implantation sites than numbers of corpora lutea observed in the Berkeley stock rats at 3,800 m. In the high altitude native animals, numbers of corpora lutea correlated with implantation sites. Placentas from Berkeley stock rats (3,800 m) were heavier than those from the other groups, and fetal hematocrits from these animals were reduced.     

Reduced oxygen at high altitude limits maximum size

The trend towards large size in marine animals with latitude, and the existence of giant marine species in polar regions have long been recognized, but remained enigmatic until a recent study showed it to be an effect of increased oxygen availability in sea water of a low temperature. The effect was apparent in data from 12 sites worldwide because of variations in water oxygen content controlled by differences in temperature and salinity. Another major physical factor affecting oxygen content in aquatic environments is reduced pressure at high altitude. Suitable data from high-altitude sites are very scarce. However, an exceptionally rich crustacean collection, which remains largely undescribed, was obtained by the British 1937 expedition from Lake Titicaca on the border between Peru and Bolivia in the Andes at an altitude of 3809 m. We show that in Lake Titicaca the maximum length of amphipods is 2-4 times smaller than other low-salinity sites (Caspian Sea and Lake Baikal).