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In ice-covered southeastern Hudson Bay (northern Quebec, Canada) the production of suitable zooplankton prey for manne fish larvae was simdar withln and outside the area covered by the Great Whale h v e r plume Within the plume however, hght attenuahon by the turbld surface layer reduced the foraging efficiency of first-feeding Arctic cod Boreogadus s a ~ d a nd sand lance Ammodytes sp larvae In daytime, first-feeding larvae accumulated at the pycnocline where food availability (l e light X prey density) was maximum Below the pycnocline, the average number of prey lngested by indiv~dual arvae (foraging gain) decllned with depth At night, fish larvae and their prey redistnbuted more uniformly over the water column, suggesting a similar passive response to the turbulence field In the absence of a light gradient The observed Ideal free distributions (IFDs) were better explained by unequal foraging abilities of the larvae than by density-dependent interactions among the assemblage of planktonic predators

Vertical distribution and foraging of marine fish arvae under the ice cover of southeastern Hudson Bay