The biomass of Calanus spp. in the Norwegian Atlantic Current and the West Spitsbergen Current (2001–2009) was statistically related to a combination of salinity, temperature, water depth and sea ice concentration. The aim of this study was to identify the significance of these environmental factors for controlling the species-specific biomass distribution and the nature of such relationships. Calanus finmarchicus dominated the entire area and its biomass was mainly related to salinity. Calanus glacialis was mainly found along the northwest shelf of the Barents Sea, but its biomass was also related to the sea ice concentration and temperature with a critical threshold ∼6°C, above which the presence and biomass of C. glacialis decreased. The Calanus hyperboreus biomass was related to all environmental factors, which characterized by a confined spatial distribution to water associated with the Greenland Sea Gyre. We conclude that C. hyperboreus is an expatriate to the study area. The Calanus biomass distribution will not change greatly in the study area with an expected increase of water temperature by 2°C, whereas the critical temperature threshold for C. glacialis will be exceeded with temperature increases of ∼4°C with a likely disappearance of this cold water species from the north-west shelf of the Barents Sea.

Seasonal mesozooplankton community composition was studied monthly from March to October 2007 in the high Arctic, Rijpfjorden (Svalbard), and related to abiotic (hydrography, sea ice) and biotic (ice algae and phytoplankton biomass) environmental conditions. The community was numerically dominated by the cosmopolitan Oithona similis, whereas Arctic Calanus glacialis was the dominant taxon in terms of biomass. Seasonal mesozooplankton community development was largely influenced by the sea ice and hydrographic conditions, which impacted the primary production regime in the fjord. Three distinct periods could be identified based on species and life stages composition: (i) winter–spring transition (March–June), with high ice algal biomass in April–June, characterized by peak abundances of Pseudocalanus minutus, Calanus glacialis females and Clione limacina; (ii) sea ice break-up and phytoplankton bloom (July), with high numbers of Calanus nauplii and young copepodids, as well as larvae of benthic crustaceans such as Cirripedia and Decapoda; and (iii) ice-free post-bloom period (August–October), when the pulse of warm waters into the fjord resulted in development of a community with Atlantic characteristics and peak abundances of Oithona similis, Oithona atlantica, Limacina helicina and Echinodermata larvae within the upper 50 m. At the same time, older copepodids of Calanus glacialis and Calanus finmarchicus had already descended to overwintering depths (>100 m). Despite the 2–3 months delay in the phytoplankton bloom compared with ice-free Svalbard fjords, the Rijpfjorden mesozooplankton managed to fulfill their life cycles in a similar time, likely due to the utilization of the ice algal bloom, and warmer water enhancing species growth and development in late summer.