Seasonal δ13C and δ15N isoscapes of fish populations along a continental shelf trophic gradient

被引:64
作者
Radabaugh, Kara R. [1 ]
Hollander, David J. [1 ]
Peebles, Ernst B. [1 ]
机构
[1] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA
关键词
Stable isotope; C and N pathways; Isoscape; Marine food web; Animal migration; PARTICULATE ORGANIC-MATTER; CARBON ISOTOPIC COMPOSITION; LIZARDFISH SYNODUS-FOETENS; SCALE SPATIAL VARIATION; MISSISSIPPI RIVER; NITROGEN-FIXATION; STABLE-ISOTOPES; GULF; TURNOVER; HABITAT;
D O I
10.1016/j.csr.2013.08.010
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
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 delta C-13 and delta N-15 isoscapes. Muscle delta N-15 from three widely distributed fish species, Synodus foetens (inshore lizardfish), Calamus proridens (littlehead porgy), and Syacium papillosum (dusky flounder), exhibited strong longitudinal correlations (Pearson's r= -0.67 to -0.90, p <0.001) that coincided with the principal trophic gradient, whereas delta C-13 values of fish muscle and benthic algae were correlated with depth (Pearson's r=-0.34 to 0.73, p < 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 delta C-13 depth gradient and the delta N-15 longitudinal gradient were consistent between seasons and years, providing a foundation for future stable isotope studies of animal migration in the Gulf of Mexico. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:112 / 122
页数:11
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