Heterotrophic bacterial dynamics were assessed in the sea ice and surface waters on the Mackenzie Shelf (Beaufort Sea), from 5 March to 3 May 2004. On 11 occasions, heterotrophic protist bacterivory was assessed from the disappearance of fluorescently labeled bacteria (FLB) in sea-ice samples collected from areas of high and low snow cover. Concurrently, sea-ice and surface water samples were analyzed for dissolved organic carbon (DOC), exopolymeric substances (EPS) and chlorophyll a concentrations, and protist and bacterial abundances. Total bacterial abundances were significantly higher in the sea ice than in surface waters. However, DOC concentrations and abundances of large (≥ 0.7 µm) bacteria were not significantly higher in the sea ice as compared to surface waters. This suggests that DOC was being released from the sea ice, potentially supporting the growth of large-sized bacteria at the ice-water interface. Heterotrophic protist (HP) bacterivory averaged 57% d -1 of large-sized bacterial abundances in the sea ice with ingestion rates averaging 768 and 441 bacteria HP -1 d -1, under high and low snow cover, respectively. High concentrations of EPS during the sea-ice algal bloom may have interfered with the grazing activities of heterotrophic protists as indicated by the significant negative correlations between ingestion rates and EPS-carbon concentrations under high (τ = -0.57, p < 0.05) and low (τ = -0.56, p < 0.05) snow cover. Bacterivory satisfied heterotrophic protist carbon requirements prior to, but not during, the sea-ice algal bloom, under high and low snow cover. EPS may have been an additional carbon source for the heterotrophs, especially during the sea-ice algal bloom period. This study provides evidence of an active heterotrophic microbial food web in first-year sea ice, prior to and during the sea-ice algal bloom. This study also highlights the significance of DOC and EPS as integral components of the microbial food web within the sea ice and surface waters of Arctic shelves.
KEY WORDS: Bacteria · FLB · Grazing · DOC · EPS · Sea ice · Arctic
Resale or republication not permitted without written consent of the publisherAquat Microb Ecol 50: [25][26][27][28][29][30][31][32][33][34][35][36][37][38] 2007 production in landfast sea ice during the spring/summer period (Smith et al. 1989, Smith & Clement 1990. In Arctic pack ice or in landfast sea ice during winter, bacteria can be important contributors to total sea-ice carbon biomass, potentially surpassing algal or heterotrophic protist (HP) carbon biomass (Gradinger & Zhang 1997, Gradinger et al. 1999a, Kaartokallio 2004. In addition, bacterial secondary production can surpass primary production when sea-ice algae are light limited in thick pack ice (Grossmann & Dieckmann 1994).Bacteria in landfast Arctic sea ice can be much larger than those found in the surface water (Bunch & Harland 1990, Laurion et al. 1995. In addition, sea-ice bacteria in Arctic pack ice appear to be more active than pelagic bacteria (Junge et al. 2002) and ...