Measurement of Whole-Body CO2 Production in Birds Using Real-Time Laser-Derived Measurements of Hydrogen (δ2H) and Oxygen (δ18O) Isotope Concentrations in Water Vapor from Breath

被引:14
|
作者
Mitchell, G. W. [1 ,2 ]
Guglielmo, C. G. [1 ]
Hobson, K. A. [3 ]
机构
[1] Univ Western Ontario, Dept Biol, Adv Facil Avian Res, London, ON, Canada
[2] Environm Canada, Wildlife Res Div, Natl Wildlife Res Ctr, Ottawa, ON K1A 0H3, Canada
[3] Environm Canada, Wildlife Res Div, Natl Hydrol Res Ctr, Saskatoon, SK, Canada
来源
PHYSIOLOGICAL AND BIOCHEMICAL ZOOLOGY | 2015年 / 88卷 / 06期
基金
加拿大自然科学与工程研究理事会;
关键词
breath; cavity ring-down spectrometry; doubly labeled water; isotopes; total body water; total energy expenditure; songbirds; RING-DOWN SPECTROSCOPY; DEUTERIUM-DILUTION; SPECTROMETRY; TECHNOLOGY; RATIOS;
D O I
10.1086/683013
中图分类号
Q4 [生理学];
学科分类号
071003 ;
摘要
The doubly labeled water (DLW) method is commonly used to measure energy expenditure in free-living wildlife and humans. However, DLW studies involving animals typically require three blood samples, which can affect behavior and wellbeing. Moreover, measurement of H (delta H-2) and O (delta O-18) isotope concentrations in H2O derived from blood using conventional isotope ratio mass spectrometry is technically demanding, time-consuming, and often expensive. A novel technique that would avoid these constraints is the real-time measurement of delta H-2 and delta O-18 in the H2O vapor of exhaled breath using cavity ring-down (CRD) spectrometry, provided that delta H-2 and delta O-18 from body H2O and breath were well correlated. Here, we conducted a validation study with CRD spectrometry involving five zebra finches (Taeniopygia gutiata), five brown-headed cowbirds (Molothrus ater), and five European starlings (Sturnus vulgaris), where we compared delta H-2, delta O-18, and rCO(2) (rate of CO2 production) estimates from breath with those from blood. Isotope concentrations from blood were validated by comparing dilution-space estimates with measurements of total body water (TBW) obtained from quantitative magnetic resonance. Isotope dilution-space estimates from delta H-2 and 6180 values in the blood were similar to and strongly correlated with TBW measurements (R-2 = 0.99). The H-2 and O-18 (ppm) in breath and blood were also highly correlated (R-2 = 0.99 and 0.98, respectively); however, isotope concentrations in breath were always less enriched than those in blood and slightly higher than expected, given assumed fractionation values between blood and breath. Overall, rCO(2) measurements from breath were strongly correlated with those from the blood (R-2 = 0.90). We suggest that this technique will find wide application in studies of animal and human energetics in the field and laboratory. We also provide suggestions for ways this technique could be further improved.
引用
收藏
页码:599 / 606
页数:8
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