Mr. Anderson et Rb. Rivkin, Seasonal patterns in grazing mortality of bacterioplankton in polar oceans: a bipolar comparison, AQUAT MIC E, 25(2), 2001, pp. 195-206
Despite the relevance of high latitude oceans to models and budgets of biog
enic carbon,and the central role of heterotrophic microbes in global biogeo
chemical cycles, the patterns of energy flow through the lower food web in
polar regions are poorly understood. To assess bacteria-based food webs in
polar regions, the distribution, growth, and respiration and grazing losses
of bacteria must be characterized. We report on the results of a seasonal
(late winter through late summer) study of protist grazing in both Resolute
Bay, Northwest Territories, Canadian Arctic and McMurdo Sound, Antarctica,
and summarize the literature on the relations between the growth and grazi
ng mortality of polar bacterioplankton. Bacterial abundance varied 5-fold i
n the Arctic and 25-fold in the Antarctic. Average bacterial growth rates r
anged from 0.1 to 1.1 d(-1). During comparable seasons, bacterial abundance
was 2- to 3-fold higher and growth rates were 2- to 3-fold lower in the An
tarctic than the Arctic. When grazing occurred, microzooplankton consumed n
early all of the local bacterial production. Grazing losses of bacteria wer
e negligible immediately before and after the phytoplankton bloom. We propo
se that at these times, bacterioplankton were nutrient limited and protists
were predominantly herbivorous. Protozoan grazers appear to alternate betw
een bacterivorous and herbivorous nutritional modes as prey fields change i
n response to the seasonal progression in submarine irradiance and concentr
ation of dissolved nutrients. The timing and magnitude of the phytoplankton
bloom and the duration of the post-bloom period exert a significant influe
nce on the flux of bacterioplankton carbon through microzooplankton and ult
imately the coupling of the microbial and metazoan food webs.