interactive effect of temperature and humidity on the oxygen isotope composition of kangaroos

• Published in: Functional ecology 2007-08, Vol.21 (4), p.757-766
• Main Authors: MURPHY, BRETT P, BOWMAN, DAVID M.J.S, GAGAN, MICHAEL K
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal Physiological Ecology; Animal, plant and microbial ecology; Australia; Autoecology; Biological and medical sciences; climate; climatic zones; Ecological modeling; Fundamental and applied biological sciences. Psychology; General aspects; herbivore; Herbivores; Human ecology; Kangaroos; Macropus; Mammalia; Oxygen isotopes; Precipitation; Relative humidity; Species; stable isotope; Teeth; Tooth enamel; Vertebrates: general zoology, morphology, phylogeny, systematics, cytogenetics, geographical distribution
• ISSN: 0269-8463; 1365-2435
• DOI: 10.1111/j.1365-2435.2007.01284.x

1. A strong relationship between the oxygen isotope composition (expressed as δ¹⁸O) of body water and relative humidity has been demonstrated for a number of mammalian herbivores with low drinking water requirements, including kangaroos. Consequently, it has been suggested that the oxygen isotope composition of preserved mammal remains may be used to reconstruct past relative humidity. Other physiological, environmental and ecological factors may also influence mammalian δ¹⁸O, thereby confounding the climatic signal, yet these factors have been rigorously examined in few taxa. 2. We examined sources of variation in the δ¹⁸O of tooth enamel, assumed to reflect δ¹⁸O of body water, of kangaroos (Macropus spp.) collected throughout Australia. 3. Relative humidity explained a large proportion of the variation in enamel δ¹⁸O, a finding that is consistent with previous studies. However, we also found a previously unreported interaction between mean annual temperature and relative humidity. At lower temperatures, the relationship between enamel δ¹⁸O and relative humidity was much steeper than at higher temperatures. 4. This may be a consequence of the Peclét effect in plant leaves, whereby high transpiration rates diminish the ¹⁸O enrichment of bulk leaf water. It is likely that this interaction is also present in other herbivores with low drinking water requirements. 5. We found little evidence that δ¹⁸O varied consistently between molars, suggesting that a 'weaning effect' is either absent or swamped by seasonal variation in precipitation δ¹⁸O. 6. We suggest that the oxygen isotope composition of preserved kangaroo remains cannot be used to reconstruct relative humidity unless ambient air temperature can be reliably estimated.