Mj. Kohn, PREDICTING ANIMAL DELTA-O-18 - ACCOUNTING FOR DIET AND PHYSIOLOGICAL ADAPTATION, Geochimica et cosmochimica acta, 60(23), 1996, pp. 4811-4829
Theoretical predictions and measured isotope variations indicate that
diet and physiological adaptation have a significant impact on animals
delta(18)O and cannot be ignored. A generalized model is therefore de
veloped for the prediction of animal body water and phosphate delta(18
)O to incorporate these factors quantitatively. Application of the mod
el reproduces most published compositions and compositional trends for
mammals and birds. A moderate dependence of animal delta(18)O on humi
dity is predicted for drought-tolerant animals, and the correlation be
tween humidity and North American deer bone composition as corrected f
or local meteoric water is predicted within the scatter of the data. I
n contrast to an observed strong correlation between kangaroo delta(18
)O and humidity (Delta delta(18)O/Delta h similar to 2.5 +/- 0.4 parts
per thousand/ 10% r.h.), the predicted humidity dependence is only 1.
3 - 1.7 parts per thousand/10% r.h., and it is inferred that drinking
water in hot dry areas of Australia is enriched in O-18 over rainwater
. Differences in physiology and water turnover readily explain the obs
erved differences in delta(18)O for several herbivore genera in East A
frica, excepting antelopes. Antelope models are more sensitive to biol
ogical fractionations, and adjustments to the flux of transcutaneous w
ater vapor within experimentally measured ranges allows their delta(18
)O values to be matched. Models of the seasonal changes of forage comp
osition for two regions with dissimilar climates show that significant
seasonal variations in animal isotope composition are expected, and t
hat animals with different physiologies and diets track climate differ
ently. Analysis of different genera with disparate sensitivities to su
rface water and humidity will allow the most accurate quantification o
f past climate changes.