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Processes controlling the benthic food web of a mesotrophic bight (KwaZulu-Natal, South Africa) revealed by stable isotope analysis
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2013
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EngineeringMarine ChemistryMarine SystemsOceanographyEarth ScienceMarine ParadeStable Isotope AnalysisSouth AfricaBiological OceanographyFood WebBenthic EcologyOceanic SystemsTrophic WebIsotope AnalysisBiogeochemistryMarine GeologyMarine BiotaBenthic Food WebBenthic CommunityBenthic-pelagic CouplingIsotope GeochemistryStable Isotope ProbingMarine BiologyPaleoecology
MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 484:97-114 (2013) - DOI: https://doi.org/10.3354/meps10311 Processes controlling the benthic food web of a mesotrophic bight (KwaZulu-Natal, South Africa) revealed by stable isotope analysis A. M. De Lecea1,*, S. T. Fennessy2, A. J. Smit3 1Geological Sciences, and 3Biological Sciences, School of Agricultural, Earth and Environmental Sciences, Westville Campus, University of KwaZulu-Natal, Durban 4001, South Africa 2Oceanographic Research Institute, PO Box 10712, Marine Parade, Durban 4056, South Africa *Email: a_lezea@yahoo.co.uk ABSTRACT: The KwaZulu-Natal Bight is considered oligotrophic/mesotrophic with distinct sources of nutrients entering the system by a series of oceanographic processes, including an upwelling cell and several estuaries, of which the Thukela River is the most important; the upwelling cell is suggested to be the main factor controlling the biology of the Bight. Our aim is to describe the main nutrient/organic matter (OM) source driving the benthic system of the Bight and to produce a food web to aid in understanding the trophic interactions occurring in the demersal ecosystem. For this, marine and riverine sediment samples, total suspended solids and marine demersal organisms were collected across the Bight, and δ13C and δ15N composition was analysed during 2 seasons. Our results, based on δ13C, δ15N, percent organic carbon, percent nitrogen and carbon:nitrogen ratios, suggest that the OM in the sediments is mainly dominated by riverine input and the benthic food web is controlled mainly by riverine total suspended solids input. Future studies should look at the role played by bacteria in the degradation of terrestrial OM and the overall effect in the food web of the Bight. Omnivory appears to be a widespread strategy for demersal organisms throughout the Bight, a finding supported by the lack of clear δ15N enrichment between prey and predators and the low variability of trophic positions across a wide array of organisms. KEY WORDS: Demersal · Food web · Stable isotope · Marine · Riverine · Organic matter · Sediment Full text in pdf format Supplementary material PreviousNextCite this article as: De Lecea AM, Fennessy ST, Smit AJ (2013) Processes controlling the benthic food web of a mesotrophic bight (KwaZulu-Natal, South Africa) revealed by stable isotope analysis. Mar Ecol Prog Ser 484:97-114. https://doi.org/10.3354/meps10311 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 484. Online publication date: June 12, 2013 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2013 Inter-Research.
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