Abstract

During the International Polar Year (IPY), large international research programs provided a unique opportunity for assessing the current state and trends in major components of arctic marine ecosystems at an exceptionally wide spatio-temporal scale: sampling covered most regions of the Canadian Arctic (IPY-Canada’s Three Oceans project), and the coastal and offshore areas of the southeastern Beaufort Sea were monitored over almost a full year (IPY-Circumpolar Flaw Lead project). The general goal of these projects was to improve our understanding of how the response of arctic marine ecosystems to climate warming will alter the productivity and structure of the food web and the ecosystem services it provides to Northerners. The present paper summarizes and discusses six key findings related to primary production (PP), which determines the amount of food available to consumers. (1) Offshore, the warming and freshening of the surface layer is leading to the displacement of large nanophytoplankton species by small picophytoplankton cells, with potentially profound bottom-up effects within the marine food web. (2) In coastal areas, PP increases as favourable winds and the deeper seaward retreat of ice promote upwelling. (3) Multiple upwelling events repeatedly provide food to herbivores throughout the growth season. (4) A substantial amount of pelagic PP occurs under thinning ice and cannot be detected by orbiting sensors. (5) Early PP in the spring does not imply a trophic mismatch with key herbivores. (6) The epipelagic ecosystem is very efficient at retaining carbon in surface waters and preventing its sedimentation to the benthos. While enhanced PP could result in increased fish and marine mammal harvests for Northerners, it will most likely be insufficient for sustainable large-scale commercial fisheries in the Canadian Arctic.

Highlights

  • Climate-driven changes in primary production (PP) will have consequences for biogeochemical cycling, the success of top predators and the yield of harvestable resources in the Arctic Ocean

  • The synthesis produced by Forest et al (2011) for Amundsen Gulf combined ship-based International Polar Year (IPY)-Circumpolar Flaw Lead System Study (CFL) data on bacterial production, zooplankton biomass and respiration, herbivory, bacterivory, vertical particle fluxes, pools of particulate and dissolved organic carbon (POC, DOC) and net community production (NCP)

  • Comprehensive annual (CFL) and quasi-synoptic (C3O) surveys of ecosystem data remain scarce in the Arctic Ocean

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Summary

Introduction

Climate-driven changes in primary production (PP) will have consequences for biogeochemical cycling, the success of top predators and the yield of harvestable resources in the Arctic Ocean. The general “classic” view summarized above must be considerably modified and enriched following two large IPY programs, the Circumpolar Flaw Lead System Study (CFL) and Canada’s Three Oceans (C3O) These projects documented sharp contrasts in the timing, magnitude and composition of primary production between shelf environments and the deep offshore waters of the Canada Basin. Latent heat fluxes driven by upwelling increase the upward flux of nutrients, especially at the ice edges of large polynyas (Dunbar 1981) The combination of these physical processes contributes to nutrient replenishment in the euphotic zone (i.e. surface layer where there is enough light to support photosynthesis), contrasting with the ice-covered surrounding waters where a strong stratification usually prevents such deep mixing (Tremblay et al 2008). 2 Results and discussion: primary production dynamics: a comparison between the deep basin and the continental shelves in the pan-Arctic

The Canadian Arctic in a global perspective
Size or species composition
Timing of ice-algal and pelagic production
Fate of primary production
Findings
Conclusion
Full Text
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