Pelagic microbial activity in the Northeast Water polynya, summer 1992

Heterotrophic activity and related measures of pelagic microorganisms in the Northeast Water (NEW) polynya, the largest and northernmost summer polynya in the Arctic, were studied during the Polar Sea cruise of July/August 1992 at stations spanning a range of ice conditions. Utilization (incorporation and respiration) of C-14-labelled amino acids was measured at in situ temperature as a proxy for microheterotrophic activity in samples from the chlorophyll maxima, intermediate water depths, and the benthic boundary layer. Total activity and bacterial abundance (measured by epifluorescence microscopy) were highest in the sub-zero surface water layer that dominates the northeast Greenland shelf, and particularly in areas most influenced by ice-edge processes and lateral advection. In this cold-water layer activity correlated strongly with particulate organic carbon (POC), to a lesser degree with phytoplankton-derived pigments and bacterial abundance, but not with median bacterial cell size. No significant correlations were detected in the warmer, Atlantic-influenced deep waters of the regional trough system where POC concentrations and other parameters were low. In comparison with temperate environments, pelagic heterotrophic activity in the NEW polynya appears to be low, a finding that bears upon the fate of dissolved organic matter and the efficient supply of particulate food to the benthos in this unique polar setting.