© 2004 by ICES/CIEM International Council for the Exploration of the Sea/Conseil International pour l'Exploration de la Mer
Carbon cycling through the pelagic foodweb in the northern Humboldt Current off Chile (23°S)
a Universidad Austral de Chile, Instituto de Biología Marina Casilla 567, Valdivia, Chile
b Centro de Investigaciones Oceanográficas del Pacífico Sur-Oriental (COPAS) Concepción, Chile
c Universidad de Concepción, Departamento de Oceanografía Concepción, Chile
d Universidad Austral de Chile, Instituto de Acuicultura Puerto Montt, Chile
e Institut de Ciències del Mar (CSIC) Barcelona, Catalunya, Spain
*Correspondence to H. E. González: Universidad Austral de Chile, Instituto de Biología Marina, Casilla 567, Valdivia, Chile. e-mail: hgonzale{at}uach.cl.
The structure of the zooplankton foodweb and their dominant carbon fluxes were studied in the upwelling system off northern Chile (Mejillones Bay; 23°S) between October 2000 and December 2002. High primary production (PP) rates (1–8 gC m–2 d–1) were mostly due to the net-phytoplankton size fraction (>23 µm). High PP has been traditionally associated with the wind-driven upwelling fertilizing effect of equatorial subsurface waters, which favour development of a short food chain dominated by a few small clupeiform fish species. The objective of the present work was to study the trophic carbon flow through the first step of this "classical chain" (from phytoplankton to primary consumers such as copepods and euphausiids) and the carbon flow towards the gelatinous web composed of both filter-feeding and carnivorous zooplankton. To accomplish this objective, feeding experiments with copepods, appendicularians, ctenophores, and chaetognaths were conducted using naturally occurring plankton prey assemblages. Throughout the study, the total carbon ingestion rates showed that the dominant appendicularian species and small copepods consumed an average of 7 and 5 µgC ind–1 d–1, respectively. In addition, copepods ingested particles mainly in the size range of nano- and microplankton, whereas appendicularians ingested in the range of pico- and nanoplankton. Small copepods and appendicularians removed a small fraction of total daily PP (range 6–11%). However, when the pico- + nanoplankton fractions were the major contributors to total PP (oligotrophic conditions), grazing by small copepods increased markedly to 86% of total PP. Under these more oligotrophic conditions, the euphausiids grazing increased as well, but only reached values lower than 5% of total PP. During this study, chaetognaths and ctenophores ingested an average of 1 and 14 copepods ind–1 d–1, respectively. In terms of biomass consumed, the potential impact of carnivorous gelatinous zooplankton on the small-size copepod community (preferred prey) was important (2–12% of biomass removed daily). However, their impact produced more significant results on copepod abundance (up to 33%), which suggests that carnivorous gelatinous zooplankton may even modulate (control) the abundance of some species as well as the size structure of the copepod community.
Keywords: coastal foodweb, gelatinous zooplankton, Humboldt Current system, trophic carbon flow
accepted 23 March 2004.
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