In order to evaluate the importance of mangrove leaf detritus as a food source for deca- pod crustacean larvae, stable isotopes (δ 13 C and δ 15 N) were measured in the tissue of these larvae and other selected organisms. Decapod crustacean larvae and planktonic adult decapods, Lucifer faxoni and Acetes americanus, were sampled in the Itamaraca estuarine system, Brazil. For comparison with stable isotope values in the estuary, plankton and POM samples were also taken on the adjacent con- tinental shelf. In the Itamaraca estuarine system, δ 13 C of decapod larvae and the holoplanktonic decapods L. faxoni and A. americanus ranged from about -17 to -23‰ (mean: -19.8 ± 1.5‰). This indicates that the contribution of mangrove carbon (δ 13 C: -26.8‰) to larval nutrition was generally negligible. Among decapod larvae, porcellanid zoeae showed relatively low δ 13 C values, while penaeid shrimp postlarvae showed the highest δ 13 C. Porcellanid zoeae were thus the only decapod larvae with a considerable percentage (13 to 40%) of mangrove carbon in their tissue. However, these low values may also be due to a negative isotope shift that occurs during embryogenesis. Feed- ing experiments with zoeae of Petrolisthes armatus (Anomura: Porcellanidae) and Sesarma rectum (Brachyura: Grapsidae) showed assimilatory shifts of up to 1.0 ± 0.2‰ for 13 C and up to 1.4 ± 0.6‰ for 15 N. Analysis of embryonic isotope fractionation for 5 decapod crustacean species, P. armatus, S. rectum, Aratus pisonii, Uca thayeri, and U. maracoani, showed that larval tissue was 13 C-depleted by up to 3.8‰ and 15 N-depleted by up to 2.3‰ in relation to parental tissue.
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