Spatial Distribution, Structure, Biomass, and Physiology of Microbial Assemblages across the Southern Ocean Frontal Zones during the Late Austral Winter

• Published in: Applied and Environmental Microbiology
• Main Authors: Hanson, Roger B., Lowery, H. Kenneth
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Society for Microbiology 1985
• Subjects: Ecology; Applied Microbiology and Biotechnology; Food Science; Biotechnology; Antarctic; Austral; Drake Passage; Narrow Passage; Pacific; Southern Ocean; The Antarctic; Antarc*; Antarctica; Sea ice
• Online Access: http://dx.doi.org/10.1128/aem.49.5.1029-1039.1985; https://journals.asm.org/doi/pdf/10.1128/aem.49.5.1029-1039.1985

We examined the spatial distributions of picoplankton, nanoplankton, and microplankton biomass and physiological state relative to the hydrography of the Southern Ocean along 90° W longitude and across the Drake Passage in the late austral winter. The eastern South Pacific Ocean showed some large-scale biogeographical differences and size class variability. Microbial ATP biomass was greatest in euphotic surface waters. The horizontal distributions of microbial biomass and physiological state (adenylate energy charge ratio) coincided with internal currents (fronts) of the Antarctic Circumpolar Current. In the Drake Passage, the biological scales in the euphotic and aphotic zones were complex, and ATP, total adenylate, and adenylate energy charge ratio isopleths were compressed due to the extension of the sea ice from Antarctica and constriction of the Circumpolar Current through the narrow passage. The physiological state of microbial assemblages and biomass were much higher in the Drake Passage than in the eastern South Pacific Ocean. The temperature of Antarctic waters, not dissolved organic carbon, was the major variable controlling picoplankton growth. Estimates of picoplankton production based on ATP increments with time suggest that production under reduced predation pressure was 1 to 10 μg of carbon per liter per day. Our results demonstrate the influence of large-scale hydrographic processes on the distribution and structure of microplankton, nanoplankton, and picoplankton across the Southern Ocean.