Background: Isotopes can provide unique solutions to fundamental problems related to the ecology and evolution of migration and dispersal because prior movements of individuals can theoretically be tracked from tissues collected from a single capture. However, there is still remarkably little information available about how and why isotopes vary in wild animal tissues, especially over large spatial scales.
Methodology/principal findings: Here, we describe variation in both stable-hydrogen (deltaD(F)) and strontium ((87)Sr/(86)Sr(F)) isotopic compositions in the feathers of a migratory songbird, the Tree Swallow (Tachycineta bicolor), across 18 sampling sites in North America and then examine potential mechanisms driving this variation. We found that deltaD(F) was correlated with latitude of the sampling site, whereas (87)Sr/(86)Sr(F) was correlated with longitude. deltaD(F) was related to deltaD of meteoric waters where molting occurred and (87)Sr/(86)Sr(F) was influenced primarily by the geology in the area where feathers were grown. Using simulation models, we then assessed the utility of combining both markers to estimate the origin of individuals. Using 13 geographic regions, we found that the number of individuals correctly assigned to their site of origin increased from less than 40% using either deltaD or (87)Sr/(86)Sr alone to 74% using both isotopes.
Conclusions/significance: Our results suggest that these isotopes have the potential to provide predictable and complementary markers for estimating long-distance animal movements. Combining isotopes influenced by different global-scale processes may allow researchers to link the population dynamics of animals across large geographic ranges.