and variability in Posidonia oceanica associated with seasonality and plant fraction
Introduction
Since the late 1970s, food web investigations in seagrass-dominated ecosystems have benefited from the use of carbon and nitrogen stable isotopic compositions (Fry et al., 1977, Fry et al., 1987, Dauby, 1989, Boon and Bunn, 1994, Jennings et al., 1997, Lepoint et al., 2000, Pinnegar and Polunin, 2000). Isotopic signatures are informative because their changes associated with the transition between two consecutive trophic levels can be predicted from the initial isotopic signal in the primary producer (Michener and Schell, 1994).
Despite its essential role in evaluating the potential diet of a particular consumer, little attention has been paid so far to the natural isotopic variability of marine macrophytes, the scarcity of information being specially noticeable in seagrasses. The stable isotopic composition of marine phanerogames is highly variable, owing to physiological and environmental factors that are usually linked to each other (Hemminga and Mateo, 1996). Specifically, the most important factors inducing variation in seagrass isotopic signatures appear to be, in order of decreasing importance, interspecific variability, the isotopic signal of the sources for synthesis (i.e. dissolved inorganic carbon and the various assimilable forms of nitrogen and sulphur), irradiance, and temperature, the last two being particularly determinant for carbon isotope ratios and strongly associated with seasonality. To our knowledge, this study represents the first attempt to assess the seasonal variability of and in different plant parts and compartments of the seagrass Posidonia oceanica (L.) Delile. Our ultimate goal is to contribute to increasing the accuracy of food web stable isotopic investigations in this key Mediterranean seagrass.
Section snippets
Materials and methods
Whole P. oceanica plants and plant detritus were collected in January, April, July and November 1998 in the Stagnone di Marsala coastal sound (37°52′N; 12°28′E), a semi-enclosed basin of approximately 2000 ha in western Sicily, Italy, with an average depth of 1.5 m. Two openings (in the northern and southern parts) allow water exchange. Water temperature and salinity present a wide annual range (11.8–28.6 °C; 33.1–45.5 PSU, respectively; Sarà et al., 1999). The basin is oligotrophic, with
Results and discussion
The mean carbon and nitrogen isotopic compositions obtained in this study (Table 1) were of the same order as those reported in previous studies (−16.4 to −8.3‰ for and 2.8 to 3.5‰ for ; McMillan et al., 1980, Cooper and De Niro, 1989, Dauby, 1989, Jennings et al., 1997, Lepoint et al., 2000, Pinnegar and Polunin, 2000). Substantial significant differences were found associated with both seasonality and plant fraction (Table 2).
Although differences in between intermediate and
Acknowledgements
This work was funded by the Ministero Politiche Agricole e Forestali (MiPAF, Italy) and Ministero dell’Istruzione, dell’Università e della Ricerca (MIUR, Italy). The authors thank Olga Invers and Linda Handley for stimulating the discussion on nitrogen dynamics.
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