Stocks and dynamics of bacterioplankton in the northwestern Sargasso Sea

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Abstract

We examined seasonal variations of bacterioplankton stocks and distributions in the upper 250 m in the Sargasso Sea near Hydrostation S and the U.S. JGOFS Bermuda Atlantic Time-series Study (BATS) site during 1987-1988 and 1991-1994. Mean vertical profiles of bacterial abundance, cell volume, and 3H-thymidine and 3H-leucine incorporation rates varied seasonally, and distribution patterns were correlated with physical mixing in the fall and winter. Conversion factors for 3H-thymidine and 3H-leucine incorporation were determined empirically to be 1.63 and 0.078 × 1018 cells mol-1, respectively. Integrated bacterial biomass and production within the euphotic zone were low compared to other oceanic sites and ranged between 241-411 mg C m-2 and 11-36 mg C m-2 day-1, respectively. Seasonal variation in bacterial biomass and production was observed; however, the range of variation was less than two-fold despite a five-fold range in primary production. Bacterial biomass (BB): phytoplankton biomass (PB) ratios remained high during the summer and fall, with bacterial biomass dominating the chl a-C estimates at times, and BB:PB ratios decreased in the winter and spring due to increased phytoplankton production. Low bacterial production (BP):phytoplankton production (PP) ratios were observed for all seasons. Although BP:PP ratios were low, growth efficiencies observed in this region indicate that carbon flux through seasonal BP could account for 17-> 100% of seasonal PP. The small response of bacterial production during and after a phytoplankton bloom may indicate that the majority of dissolved organic carbon (DOC) that accumulates in post bloom conditions is of semi-labile quality, resulting in slow bacterial oxidation of DOC. Copyright © 1996 Elsevier Science Ltd.

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APA

Carlson, C. A., Ducklow, H. W., & Sleeter, T. D. (1996). Stocks and dynamics of bacterioplankton in the northwestern Sargasso Sea. Deep-Sea Research Part II: Topical Studies in Oceanography, 43(2–3), 491–515. https://doi.org/10.1016/0967-0645(95)00101-8

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