Tissue-Specific Stable Isotope Fractionation in Subarctic Pinniped Species
Faculty Sponsors
Dr. Amy Hirons
Project Type
Event
Location
Alvin Sherman Library
Start Date
1-4-2026 12:00 AM
End Date
2-4-2026 12:00 AM
Tissue-Specific Stable Isotope Fractionation in Subarctic Pinniped Species
Alvin Sherman Library
Stable carbon (δ13C) and nitrogen (δ15N) isotope ratios are widely used to evaluate marine mammal diet, trophic position, and nutrient assimilation. However, interpretation is often confounded by tissue-specific isotopic discrimination, which alters isotope ratios during nutrient assimilation and tissue synthesis. Quantifying these offsets is essential for ensuring accurate trophic reconstructions across multiple tissues with different biochemical compositions. This study measured δ13 and δ15N values in muscle, blood, blubber, brain, collagen, kidney, liver, skin, fur, and vibrissae of Steller sea lions (Eumentopias jubatus), harbor seals (Phoca vitulina), and northern fur seals (Callorhinus ursinus). Samples from each species were collected from subsistence harvests in regions of the Bering and Gulf of Alaska between 1975 and 1997. Mean δ15N values varied less than 1% across all tissues and species, indicating minimal nitrogen fractionation and suggesting that δ15N values from most tissues provide comparable information for trophic-level estimates. In contrast, δ13C fractionation exhibited pronounced tissue and species-specific patterns. Lipid-rich tissues, particularly blubber, showed substantial δ13C depletion relative to muscle, consistent with the biochemical discrimination against 13C during lipid synthesis. Enrichment gradients from blubber toward keratinized tissues were evident in Steller sea lions, harbor seals, and northern fur seals. These results highlight the necessity of incorporating tissue-specific δ13C discrimination factors when interpreting isotope data. Accounting for these offsets will improve the reliability of trophic analyses, ecological reconstructions, and physiological assessments derived from stable isotope measurements.
