ASSESSING THE RELIABILITY OF STABLE ISOTOPES IN FOSSIL BONE: A UNIQUE CASE STUDY OF PREHISTORIC LUNG PATHOLOGY
Our results show consistently lower δ18O values in pathologic bone, suggesting it may have formed at a higher body temperature. While the direction of offset between normal and pathologic bone (Δ18ON-P) is consistent, the magnitude of the offset is variable and sometimes larger than can be explained solely by elevated body temperature. A change in body water δ18O related to physiology and/or HPOA could be an additional factor influencing Δ18ON-P. For example, an increase in drinking water contribution to the body water reservoir could help to explain the observed δ18O offset for animals whose behavioral response to disease includes increased water consumption. This interpretation is supported by the high number of individuals concentrated in and around a shallow paleo-water body at Ashfall. Isotopic exchange during diagenesis may be another variable affecting the magnitude of Δ18ON-P, and can be examined further through intra-individual δ18O comparisons of different skeletal tissues (e.g., enamel and bone, phosphate and carbonate) or through δ18O comparisons between different members of the Ashfall fauna.