The Oxygen Consumption of the Mountain White-Crowned Sparrow (Zonotrichia leucophrys oriantha) in Relation to Air Temperature

The Condor ◽  
1976 ◽  
Vol 78 (4) ◽  
pp. 569 ◽  
Author(s):  
Catherine S. Maxwell ◽  
James R. King
1997 ◽  
Vol 75 (3) ◽  
pp. 396-400 ◽  
Author(s):  
Paul C. Schieltz ◽  
Mary E. Murphy

To evaluate the contribution of changes in plumage insulation to the energy cost of molt, we measured oxygen consumption by wintering White-crowned Sparrows (Zonotrichia leucophrys gambelii) before and after plucking 12, 24, or 36% of their plumage, and when they were replacing these feathers. Measurements were made at 20 and 25 °C, two temperatures bracketing the lower critical temperature (ca. 23 °C) of wintering Z. l. gambelii, and at 10 °C, well below the birds' lower critical temperature. For comparison, oxygen consumption by naturally molting birds was measured at 25 °C during summer. In these sparrows, feather loss resulted in increased oxygen consumption only at 10 °C and when feather loss was moderate (24% plumage; 10% increase) to intensive (36% plumage; 24% increase). Regrowth of 24 and 36% of plumage resulted in increased oxygen consumption at 20 °C (10 and 8.5%, respectively) and 10 °C (16 and 28%, respectively). Oxygen consumption by birds was unaffected by loss or regrowth of 12% of the plumage regardless of temperature, and at 25 °C, oxygen consumption was unaffected by the intensity of plumage replacement (0–36%). Comparison of oxygen consumption at 25 °C between naturally molting summer birds and treated winter birds revealed that the energy cost of molt and the apparent energy inefficiency of molt result neither from added thermoregulatory costs nor from the costs of feather synthesis per se, but seemingly from metabolic changes entrained by molt.


The Condor ◽  
1972 ◽  
Vol 74 (4) ◽  
pp. 423-430 ◽  
Author(s):  
Martin L. Morton ◽  
Jorge E. Orejuela ◽  
Susan M. Budd

1993 ◽  
Vol 41 (1) ◽  
pp. 67 ◽  
Author(s):  
F Geiser

The pattern of torpor was examined in the eastern pygmy possum, Cercartetus nanus (21 g). Animals displayed torpor regularly in the laboratory, and the occurrence of torpor increased with decreasing air temperature (T(a)). At high T(a) (18-degrees-C) animals usually exhibited daily torpor, but torpor bouts of up to 2 days were observed occasionally. The duration of torpor bouts lengthened with a lowering of T(a) and the mean bout duration at T(a) = 5-degrees-C was 17.0 +/- 2.5 days. The minimum metabolic rate (measured as rate of oxygen consumption) of torpid individuals was 0.018 +/- 0.003 mL O2 g-1 h-1, which is less than 2% of the basal metabolic rate. The body temperature (T(b)) Of torpid animals fell to a minimum of 1.3 +/- 0.4-degrees-C. These results clearly demonstrate that Cercartetus nanus is a deep hibernator.


The Auk ◽  
2015 ◽  
Vol 132 (4) ◽  
pp. 893-902 ◽  
Author(s):  
Zachary M. Laubach ◽  
Wei Perng ◽  
Madeline Lombardo ◽  
Courtney Murdock ◽  
Johannes Foufopoulos

1971 ◽  
Vol 13 (4) ◽  
pp. 619-625 ◽  
Author(s):  
C. W. Holmes

SUMMARY1. Measurements of oxygen consumption and rectal temperature were made on young female calves at air temperatures of 9° and 20°C, before and after 4·5 kg milk was drunk at 23° and 39°C.2. When cool milk (23°C) was drunk at an air temperature of 9°C, vigorous shivering occurred, and during the 2-hr period after feeding, oxygen consumption was significantly higher than in the three other treatments.3. In all other treatments oxygen consumption increased considerably during the 30-min period which included drinking activity; the average increment, when no thermo-regulatory shivering occurred, was 1·9 ml O2 min−1kg−1.4. It was estimated that the 58 kcal ‘heat of warming’ required by milk at 23°C drunk at an air temperature of 9°C could be accounted for by the increment in heat production during the 2 hr after feeding and the fall in rectal temperature of 0-2-0-3°C which persisted after feeding in this treatment. These calculations suggested that the effect of a cool liquid on the energy balance of an animal would be less than that predicted from the ‘heat of warming’ required by the cool liquid.


The Auk ◽  
2004 ◽  
Vol 121 (4) ◽  
pp. 1269-1281 ◽  
Author(s):  
Thomas P. Hahn ◽  
Keith W. Sockman ◽  
Creagh W. Breuner ◽  
Martin L. Morton

Abstract Mountain White-crowned Sparrows (Zonotrichia leucophrys oriantha) winter in Mexico and often arrive in the vicinity of their breeding grounds in the Sierra Nevada well before nesting is possible. Arrival at Tioga Pass, California (elevation 3,030 m), usually occurs in early May, but residual winter snow and adverse weather can delay nesting for weeks. We used radiotelemetry to determine whether prebreeding Mountain White-crowned Sparrows engaged in weather-related altitudinal movements during the waiting period between the end of spring migration and onset of breeding during 1995–2001, with a range of residual winter snowpacks. Interannual variation in arrival date and onset of egg laying was 18 and 41 days, respectively. We tracked females for two years and males for all seven years. During spring snowstorms (which occurred in four years), radiomarked individuals moved to lower elevation sites, where they often remained for several days. Departing birds left Tioga Pass by early afternoon and returned early in the morning after storms. More frequent storms during tracking increased the likelihood of facultative altitudinal movements, but heavier residual winter snowpack did not. Warm days increased the likelihood of birds returning to Tioga Pass from low elevation. This study demonstrates that facultative altitudinal movement behavior can be a common feature of spring arrival biology in montane-breeding birds.


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