HERBIVORE TOOTH OXYGEN-ISOTOPE COMPOSITIONS - EFFECTS OF DIET AND PHYSIOLOGY

The applicability of rapid and precise laser probe analysis of tooth e namel for delta(18)O has been verified, and the method has been applie d to different modern herbivores in East Africa. Sampling and pretreat ment procedures involve initial bleaching and grinding of enamel to <7 5 mu m, and elimination of adsorbed water and organic compounds with B rF5. Typical analytical reproducibilities for 0.5-2 mg samples are +/- 0.08 parts per thousand (+/- 1 sigma). Chemical and spectroscopic cha racterization of pretreated but unanalyzed samples show no alteration compared to fresh enamel. Solid reaction products are nearly pure CaF2 with little evidence for residual O-2. Because laser probe fluorinati on extracts oxygen from all sites in the apatite structure (phosphate, structural carbonate, and hydroxyl), only unaltered tooth enamel (>95 % apatite) can be analyzed reliably. Different East African herbivores exhibit previously unsuspected compositional differences. Average ena mel delta(18)O values (V-SMOW) are approximately: 25 parts per thousan d (goat), 27 parts per thousand (oryx), 28 parts per thousand(dikdik a nd zebra), 29 parts per thousand(topi), 30 parts per thousand(gerenuk) , and 32 parts per thousand (gazelle). These compositions differ from generalized theoretical models, but are broadly consistent with expect ed isotope effects associated with differences in how much each animal (a) drinks, (b) eats C3 vs. C4 plants, and (c) pants vs. sweats. Cons ideration of diet, water turnover, and animal physiology will allow th e most accurate interpretation of ancient teeth and targeting of envir onmentally-sensitive animals in paleoclimate studies.