Recolonization of midwestern North America by cougars (Puma concolor) provides an opportunity to study dispersal pathways from established western populations. Determining the migration routes of these top predators is of critical importance to implement efficient management plans. But, because of logistic problems linked to long-term monitoring of these secretive animals, dispersal corridors remain unknown. Recently, biologists have employed stable isotope analyses of specific animal tissues as a powerful approach to determine an animal's previous locations and hence, infer origin and long-distance dispersal. To determine the origin and migration route of a cougar road-killed in eastern Nebraska, we intersected hydrogen (dD) and carbon (d13C) isotopic values along one of its claw with base maps of D and 13C for
Results/Conclusions
Deer lymph nodes produced a west-east dD gradient that matches the known deuterium pattern in precipitation. The carbon isotopic gradient reveals higher d13C values in eastern Nebraska than in the Great Plains, a results of the higher importance of corn (C4 plant) than herbaceous plants (C3 plants) in white-tailed deer diet in eastern Nebraska. The variation in dD values within the claw suggests an initial period spent in South Dakota's Black Hills, followed by a recent long-distance migration. The multiple isotope analysis reveals that this cougar travelled east through southern South Dakota or northern