Paper No. 2
Presentation Time: 9:15 AM


TIPPLE, Brett J.1, VALENZUELA, Luciano O.2, CHESSON, Lesley A.3, BOWEN, Gabriel J.4 and EHLERINGER, James R.1, (1)Department of Biology, University of Utah, 247 South 1400 East, Salt Lake City, UT 84112, (2)Laboratorio de Ecología Evolutiva Humana, Unidad de Enseñanza Universitaria Quequén, Calle 508 No 881, Quequén, 7631, Argentina, (3)IsoForensics Inc, Salt Lake City, UT 84108, (4)Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112,

Understanding an individual’s travel-history can be an important piece of information in a forensic investigation. The analysis of stable oxygen (O) isotopes of human hair has assisted in the reconstruction of the geographic-movement histories of individuals in criminal investigations. While oxygen isotope values (δ18O) of human hair provide geographic origin information, the estimated regions can be spatially broad. Strontium (Sr) isotope ratios (87Sr/86Sr) of human hair can provide a complementary isotopic approach to measurement of 18O in hair for human provenancing as 87Sr/86Sr ratios record independent geographic information and thus further constrain the estimated regions predicted by δ18O values. To understand the linkages between the Sr and O isotope systems in keratinous tissues and an individual’s environment, human hair and tap waters were collected throughout the Salt Lake Valley of Utah and the 87Sr/86Sr ratios and δ18O values were measured on paired samples. We found that different communities were provided municipal water with distinct 87Sr/86Sr ratios. Hairs with higher 87Sr/86Sr ratios were from individuals that resided in neighborhoods that had higher tap water 87Sr/86Sr ratios. Furthermore, we observed the majority of paired tap water and hair 87Sr/86Sr ratios had a 1:1 relationship, indicating little to no fractionation between Sr isotope ratios in water and hair. We found the δ18O values of Salt Lake City water and hair samples had an average value of -16.2 ‰ and 9.8 ‰, respectively. We used the hair model of Ehleringer et al. (2008) to predict tap water δ18O values of an individual’s drinking water source and observed that the predicted tap water δ18O values agreed with the measured δ18O values of tap water available in the community. Our findings indicated that different municipalities within the Salt Lake Valley used different combinations of water resources and these combinations of water resources provided a unique isotopic marker for a municipality. In turn, these community-specific isotopic signals were reflected in the isotope ratios of the hair of individuals that resided within that particular neighborhood. We propose that the paired analyses of both O and Sr isotope ratios in hair may allow for greater refinement in reconstructing the travel-movement history of an individual.