For our work in Trinidad we are grateful to J. Rasweiler, III, S. (Patsy) Williams, R. Hernandez, H. Nelson, the Asa Wright Nature Center and the William Beebe Tropical Research Station (Simla). David Boodoo and B. Ramoutar, expedited our permits

in Trinidad, and A. Ramsey, in Tobago. Our colleague at UNL, S. Thomas, gave us important traveling, working and living tips at Simla. At Big Bend National Park, R. Skiles permitted our fieldwork and assisted in housing. Funding for Trinidad was obtained by Freeman from the Maude Hammond MK0683 ic50 Fling Fellowship awarded by the Research Council, University of Nebraska-Lincoln and a Putney Award from the University of Nebraska State Museum. Funding from University of Nebraska-Kearney to K. Geluso helped support our trip to Tobago. Further, general support came from the Museum, and additional travel support to Big Bend came from the School of Natural Resources and the University of Nebraska Agricultural Research Division. This project was conducted in accordance with and approved by the Institutional Animal Care and Use Committee at UNL. “
“Stable isotopes of oxygen have been widely used to reconstruct paleotemperatures and to investigate the thermal environment of fishes and mollusks, but they have

only occasionally been used as geographical markers in marine systems. As bone apatite grows at a constant temperature in marine mammals and food is the major source of water for these animals, particularly for pinnipeds, LDK378 price variations in the ratio

of stable isotopes of oxygen (δ18O) of bone apatite will likely reflect changes in the δ18O values of diet, and thus of the surrounding water mass, despite the potential confounding role of factors as the proximate composition of diet, sex and body size. Here, we used the δ18O values in bone apatite to investigate whether adult males of South American sea lion (Otaria byronia), from three regions in southwestern Atlantic Ocean (Brazil, Patagonia and Tierra del Fuego in Argentina), used the same water masses to forage and whether differences triclocarban exist in the water masses used by sea lions differing according to sex and developmental stage. Statistically significant differences were observed among the δ18O bone values of adult males from the three regions, with those from Patagonia more enriched in 18O, as expected from the δ18Oseawater values. These results revealed restricted dispersal movements of adult males between the three areas. On the other hand, adult males and females from Patagonia did not differ in average δ18Obone values, thus indicating the use of foraging grounds within the same water mass. Finally, the variability in the δ18Obone values of young of both sexes was much wider than the adults of the same sex from the same region, which suggests the existence of a juvenile dispersal phase in both sexes, although much shorter in females than in males.