Temperature-induced changes in the relevance of viral lysis and microzooplankton grazing of Antarctic phytoplankton indicates future alterations in seasonal carbon flow.

Even though differences in the size class of carbon were observed between the colder and warmer seasons, when total carbon produced was plotted against total carbon lost for all seasons combined, a highly significant relationship was observed with the slope of the linear regression line close to the 1:1 line (Fig. 10 ).

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