Abstract
Stable isotopes are being increasingly used in wildlife forensics as means of determining the origin and movement of animals. The heavy isotope content of precipitated water and snow (δDp, δ18Op) varies widely and systematically across the globe, providing a label that is incorporated through diet into animal tissue. As a result, these isotopes are potentially ideal tracers of geographic origin. The hydrogen and oxygen isotope tracer method has excellent potential where (1) spatial variation of precipitation isotopes exist, and (2) strong, mechanistic relationships link precipitation and isotope ratios in biological tissue. Here, we present a method for interpolation of precipitation isotope values and use it to create global basemaps of growing-season (GS) and mean annual (MA) δDp and δ18Op. The use of these maps for forensic application is demonstrated using previously published isotope data for bird feathers (δDf) in North America and Europe. The precipitation maps show that the greatest potential for applying hydrogen and oxygen isotope forensics exists in mid- to high-latitude continental regions, where strong spatial isotope gradients exist. We demonstrate that δDf/δDp relationships have significant predictive power both in North America and Europe, and show how zones of confidence for the assignment of origin can be described using these predictive relationships. Our analysis focuses on wildlife forensics, but the maps and approaches presented here will be equally applicable to criminal forensic studies involving biological materials. These maps are available in GIS format at http://www.waterisotopes.org.
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Acknowledgements
This work was supported in part by Contract IS-FO-2029 from the Technical Science Working Group to TE Cerling and JR Ehleringer. Additional funding was provided by operating grants from Environment Canada to KAH and LIW.
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Bowen, G.J., Wassenaar, L.I. & Hobson, K.A. Global application of stable hydrogen and oxygen isotopes to wildlife forensics. Oecologia 143, 337–348 (2005). https://doi.org/10.1007/s00442-004-1813-y
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DOI: https://doi.org/10.1007/s00442-004-1813-y