Abstract
<p> <p id="x-x-sp0055"> The West Florida Shelf, located in the eastern Gulf of Mexico, transitions from a eutrophic ecosystem dominated by the Mississippi River plume to mesotrophic and oligotrophic ecosystems off the coast of peninsular Florida. Three extensive trawl surveys in this region were used to acquire samples of fish muscle, benthic algae from sea urchin stomach contents, and filtered particulate organic matter (POM) to create δ <sup> 13 </sup> C and δ <sup> 15 </sup> N isoscapes. Muscle δ <sup> 15 </sup> N from three widely distributed fish species, <em> Synodus foetens </em> (inshore lizardfish), <em> Calamus proridens </em> (littlehead porgy), and <em> Syacium papillosum </em> (dusky flounder), exhibited strong longitudinal correlations (Pearson′s <em> r </em> =−0.67 to −0.90, <em> p </em> <0.001) that coincided with the principal trophic gradient, whereas δ <sup> 13 </sup> C values of fish muscle and benthic algae were correlated with depth (Pearson′s <em> r </em> =−0.34 to −0.73, <em> p </em> <0.05). Correlations between isotopic values and surface concentrations of chlorophyll and particulate organic carbon (POC) imply linkages between the isotopic baseline and transitions from eutrophic to oligotrophic waters. The δ <sup> 13 </sup> C depth gradient and the δ <sup> 15 </sup> N longitudinal gradient were consistent between seasons and years, providing a foundation for future stable isotope studies of animal migration in the Gulf of Mexico. </p></p>
Original language | American English |
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Journal | Continental Shelf Research |
Volume | 68 |
DOIs | |
State | Published - Jan 1 2013 |
Keywords
- Stable isotope
- C and N pathways
- Isoscape
- Marine food web
- Animal migration
Disciplines
- Life Sciences