Phosphate–Oxygen Isotopes from Marine Turtle Bones: Ecologic and Paleoclimatic Applications

Authors

Alan B. Coulson, University of South Carolina
Matthew J. Kohn, Boise State UniversityFollow
Matthew H. Shirley, University of Florida
Walter G. Joyce, Yale University
Reese E. Barrick, College of Eastern Utah

Document Type

Article

Publication Date

7-7-2008

Abstract

While certain freshwater turtle taxa possess a strong correlation between the δ¹⁸O_phosphate value of their bone mineral and that of their environmental water, it remains unclear whether the same correlation applies to marine turtles. Isotopic analysis of over 50 individuals representing three species (Chelonia mydas, Caretta caretta, Dermochelys coriacea) from Atlantic and Pacific waters demonstrates that the correlation is robust for the studied specimens, which include a wide range of growth stages for the loggerhead (C. caretta). In most cases, intra- and inter-bone isotopic variations are low (standard deviation < ± 0.34‰ and 0.44‰, respectively) which confirms that bone growth occurs, on average, over a narrow body temperature range (ca. ≤ ± 2.0°C) and that samples from any spot on any bone can be considered as representative of the entire skeleton. Applying the correlation between δ¹⁸O_w and δ¹⁸O_{bone PO4} to marine turtles may provide a new route for investigating extant marine turtle ecology and for reconstructing paleoceanic δ¹⁸O_w values.

Publication Information

Coulson, Alan B.; Kohn, Matthew J.; Shirley, Matthew H.; Joyce, Walter G.; and Barrick, Reese E.. (2008). "Phosphate–Oxygen Isotopes from Marine Turtle Bones: Ecologic and Paleoclimatic Applications". Palaeogeography, Palaeoclimatology, Palaeoecology, 264(1-2), 78-84. https://doi.org/10.1016/j.palaeo.2008.04.008