4.2 Article

Foraging site fidelity and stable isotope values of loggerhead turtles tracked in the Gulf of Mexico and northwest Caribbean

Journal

MARINE ECOLOGY PROGRESS SERIES
Volume 502, Issue -, Pages 267-279

Publisher

INTER-RESEARCH
DOI: 10.3354/meps10655

Keywords

Stable isotope; Carbon; Nitrogen; Sulfur; Premise testing; Satellite telemetry; Loggerhead turtle; Caretta caretta; delta C-13; delta N-15; delta S-34

Funding

  1. Florida Sea Turtle Grants Program
  2. US Fish and Wildlife Service in the NRDA Loggerhead Pre-assessment
  3. Florida Fish and Wildlife Conservation Commission through USFWS
  4. Florida Fish and Wildlife Conservation Commission through NMFS
  5. Disney Worldwide Conservation Fund
  6. Mote Scientific Foundation
  7. Norcross Wildlife Foundation
  8. New Canaan County School
  9. Wooster School
  10. Morrison Family Foundation
  11. Sarasota County Environmental Services
  12. Z. Srodes/Volvo Award
  13. NASA Signals of Spring
  14. Longboat Key Turtle Watch
  15. Coastal Wildlife Club
  16. Curtis School
  17. Community Foundation of Greater Lakeland
  18. Suntrust Bank
  19. Seaturtle.org
  20. West Marine of Sarasota

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We used stable isotope ( delta C-13, delta N-15, delta S-34) analysis in combination with satellite telemetry to evaluate the foraging areas chosen by 88 loggerhead turtles Caretta caretta nesting in southwestern Florida. Nine turtles were tracked and skin-sampled in more than one nesting season to evaluate within-individual consistency in foraging sites and stable isotope values. Turtles migrated to 5 regions: Caribbean, Florida Keys, West Florida Shelf, northern Gulf of Mexico, and Yucatan Peninsula. The stable isotope ratios across these foraging grounds ranged from -21.16 to -7.69 parts per thousand for delta C-13, 3.27 to 13.99 parts per thousand for delta N-15, and 1.91 to 20.64 parts per thousand for delta S-34. We compared bulk skin tissue stable isotope values for all turtles by bioregion, year, body size, depth of putative foraging area, and linear distance from the closest shore; among these factors, only bioregion showed a significant effect on isotope values. There were subtle regional differences in mean delta C-13, delta N-15, and delta S-34, and an apparent north-south isotopic shift aligning strongly with ocean currents adjacent to the Florida Keys. The influence of coastal topography and shifting biogeographic boundaries such as the Loop Current may cause strong ocean water mixing that results in the observed similarities in stable isotope values among regions. These results indicate that stable isotopes alone may be an inadequate tool for identifying fine-scale (< 100 km) residency of sea turtles within this ocean region.

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