Seasonal patterns in grazing mortality of bacterioplankton in polar oceans: a bipolar comparison

Citation
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
Citations number
113
Categorie Soggetti
Aquatic Sciences
Journal title
AQUATIC MICROBIAL ECOLOGY
ISSN journal
09483055 → ACNP
Volume
25
Issue
2
Year of publication
2001
Pages
195 - 206
Database
ISI
SICI code
0948-3055(20010904)25:2<195:SPIGMO>2.0.ZU;2-Z
Abstract
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.