Abundance, biomass, composition and grazing impact of the sea-ice meiofauna in the North Water, northern Baffin Bay

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Influence of environmental factors on the development of bottom ice protist communities during the winter-spring transition (2009, background): “…sites due to the higher algal biomass (Gosselin et al. 1990, Smith et al. 1997) or, alternatively, by less intense grazing pressure on the protist community by copepods and other metazoans (Nozais et al. 2001, Seuthe et al. 2007) under the high snow cover site due to the lower food availability.”
Enrichment of nutrients, exopolymeric substances and microorganisms in newly formed sea ice on the Mackenzie shelf (2007, background): “There was no evidence of large flagellates (e.g. >70 µm) or meiofauna (e.g. nematodes), which are conspicuous components of multi- and first-year Arctic sea ice (Nozais et al. 2001, Michel et al. 2002).”
Temporal and vertical variations of lipid biomarkers during a bottom ice diatom bloom in the Canadian Beaufort Sea: further evidence for the use of the IP25 biomarker as a proxy for spring Arctic sea ice (2011, unknown): “2008) or meiofauna (Fraser et al. 1989; Nozais et al. 2001; Peters et al. 2004).”
Significance of sedimentation and grazing by ice micro- and meiofauna for carbon cycling in annual sea ice (northern Baffin Bay) (2002, methodology): “Particulate ice-algae production was measured using the 14C-assimilation method described by Lee et al. (2001) and Nozais et al. (2001).”