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On Thin Ice? - Climatic Influence on Energy Flow and Trophic
Structure in Arctic Marine Ecosystems
Website
Funding programme
- NFR: ARKTØK Programme (2003-2004)
Start date
Duration
Project leader
Partners
- Norwegian Polar Institute
- Univ. of Tromsø Norwegian College of Fisheries Science
- Bates College USA
- Univ. of Tasmania Australia
- Stirling Univ. Scotland
Description
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Idealized scheme describing two primary
production scenarios related to ice cover, and their trophic
implications.
Sea ice is a dominant feature of marine ecosystems in the Arctic. Its
presence directly or indirectly mediates many of the physical, chemical,
and biological processes of Arctic marine ecosystems, especially on the
shelves where benthic and pelagic systems are extensively coupled. Ice
is also one of the features of the Arctic seas that is most profoundly
affected by local, regional, and global climate, varying on scales
ranging from days to millennia. Therefore, sea ice can be seen as a
lever through which changes in climatic regimes can have far-reaching
consequences on the structure and function of Arctic marine ecosystems.
Using this rationale, we aim to test the hypothesis that changing ice
conditions associated with different climatic regimes drives primary
production on the northern Svalbard shelf through different dominant
sources (ice algae vs. phytoplankton). We propose that such variation in
the dominant source pathways of primary production has concomitant
effects on both the pelagic and benthic systems, as well as the trophic
pathways by which they are coupled. We will use field measurements and
laboratory analyses to test a series of working hypotheses related to
the primary producers, zooplankton, and benthic components northeast
Spitsbergen.
Ultimately, this study aims to provide some insight into the
energetic pathways and trophic structure of this ecosystem and its
stability versus sensitivity in the face of predicted future climate
changes.
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