Abstract

Plankton succession was investigated in the subarctic Godthabsfjord, Western Greenland, from March to August 2010. The trophic role of protozooplankton (ciliates and hetero- trophic dinoflagellates) was evaluated with emphasis on their seasonal succession and as prey for the copepod community. The integrated protozooplankton biomass ranged between 0.1 and 4.0 g C m �2 , and was dominated by ciliates. Over the 6 mo study period, maximum potential ingestion rates of the protozooplankton ranged from 0.02 to 1.2 g C m �2 d �1 , corresponding to 30 to 194% of primary production d �1 or 0.5 to 37% of phytoplankton biomass d �1 . The highest copepod biomass (24 g C m �2 ) occurred in spring, with Metridia longa alone contributing up to 92% of the biomass. A grazing experiment with M. longa feeding on a natural plankton assemblage confirmed that this species cleared cells in the size range 10 to 60 µm with an average clearance rate of 2.4 ml µg C �1 d �1 . The copepod community, dominated by the genera Calanus, Metridia, Pseudocalanus, Oithona, Microsetella and Triconia/Oncaea, accounted for 72 to 93% of the copepod biomass in the spring. After the large calanoid copepod species left the surface layer, the protozooplankton increased numerically and were the most important grazers for some weeks until a late summer copepod community, dominated by cyclopoids Oithona spp., controlled the protist community. Our study indicated that protozooplankton succession is regulated by copepod grazing during most of the season, and that these protists provide an essential source of nutrition for the copepod populations.

Highlights

  • Greenlandic fjords support rich and diverse wildlife communities and are highly valuable ecosystems for commercial as well as cultural fishing (Hamilton et al 2000)

  • Our study indicated that protozooplankton succession is regulated by copepod grazing during most of the season, and that these protists provide an essential source of nutrition for the copepod populations

  • We investigated seasonal plankton dynamics in a side branch of the Godthåbsfjord, Kapisigdlit Fjord, with emphasis on the role of protozooplankton in the food web, and the interaction between the protozooplankton and the copepod community

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Summary

Introduction

Greenlandic fjords support rich and diverse wildlife communities and are highly valuable ecosystems for commercial as well as cultural fishing (Hamilton et al 2000). The Greenland fjords are major outlets of glacial runoff, and climate changes are likely to affect the hydrography, and possibly the food web structures, within these ecosystems (Mortensen et al 2011). Baseline studies of the key plankton components in these areas are essential to understand climate-mediated changes in pelagic food web structure and productivity. The Godthåbsfjord is a subarctic fjord system located next to Nuuk, the capital of Greenland. It is one of the largest fjord systems in Greenland, harbouring large populations of capelin and Atlantic cod (Smidt 1979, Storr-Paulsen et al 2004, Bergstrøm & Vilhjalmsson 2008). The copepod community is numerically dominated by Pseudocalanus spp., Mar Ecol Prog Ser 500: 67–82, 2014

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