Origin and Distribution of Suspended Organic Matter As Inferred From Carbon Isotope Composition in A Mediterranean Semi-Enclosed Marine System

• Published in: Chemistry and ecology 1999-06, Vol.16 (2-3), p.215-238
• Main Authors: Mazzola, A., Sarà, G., Venezia, F., Caruso, M., Catalano, D., Hauser, S.
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Biological and medical sciences; Fundamental and applied biological sciences. Psychology; Marine; Sea water ecosystems; Synecology
• ISSN: 0275-7540; 1029-0370
• DOI: 10.1080/02757549908037647

The origin and distribution of suspended organic matter, the trophic features and the stable carbon isotopic composition of particulate organic carbon (POC) were studied monthly in a Western Mediterranean semi-enclosed basin. Sampling stations were selected as a function of wind-exposure and the degree of vegetation cover and then compared with an adjacent unvegetated site. the predominant vegetation was seagrass (Posidonia oceanica and Cymodocea nodosa) and Caulerpa prolifera. Water samples were analyzed for total suspended matter (inorganic and organic fractions), photosynthetic pigments (chlorophyll-a and phaeopigments), dissolved organic carbon, particulate organic carbon and their isotopic composition. Temperature and salinity were also measured at the same sampling sites within range of Mediterranean limits. the suspended organic matter concentration was 1.77 ± 1.55 mg l −1 ; the chlorophyll-a concentration was low (0.35 ± 0.24 μg l −1 ); the disolved organic carbon concentration was 2,140 ± 2,010 μg l −1 ; the particulate organic carbon concentration was 212 ± 106 μg l −1 and the isotopic composition was 18.77 ± 2.51% ° . There were significant temporal differences except for phaeopigments, POC and its POC isotopic composition, and there were no spatial differences other than for δ 13 C. This picture highlighted a general seasonal trend and trophical features similar to adjacent sea. Spatial differences in δ 13 C showed that the source of suspended organic matter was different between stations as that between sources and wind-hydrodynamic constraints. In