Journal of Plankton Research Vol.18 no.l p.1-16,1996 Density and distribution of bacterioplankton and planktonic dliates in the

Abstract. The total number of planktonic bacteria in the upper mixed layer of the Bering Sea during the late spring-early summer period ranged between 1 and ~4 x 106 ml"1 (biomass 10-40 mg C nr3). In the northern Pacific, along 47-52°N, the corresponding characteristics of the bacterioplankton...

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Main Authors: Bering Sea, North Pacific, Yu. I. Sorokin, P. Yu. Sorokin, T. I. Mamaeva
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.2901
http://plankt.oxfordjournals.org/content/18/1/1.full.pdf
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Summary:Abstract. The total number of planktonic bacteria in the upper mixed layer of the Bering Sea during the late spring-early summer period ranged between 1 and ~4 x 106 ml"1 (biomass 10-40 mg C nr3). In the northern Pacific, along 47-52°N, the corresponding characteristics of the bacterioplankton density in the upper mixed water layer were: total number 1-2 x 10s cells ml" ' and biomass 15-46 mg C nr3. Below the thermocline at 50-100 m, the density of bacterioplankton rapidly decreased. At 300 m depth, it stabilized at 0.1-0.2 x 10 * cells ml"'. The integrated biomass of bacterioplankton in the open Bering Sea ranged between 1.2 and 3.6 g C nr2 (wet biomass 6-18 g nr2). Its production per day varied from 2 to 23 mg C nr3 days ' in the upper 0-100 m. The numerical abundance of planktonic ciliates in this layer was estimated to be from 3 to 10 x 103 cells 1"', and in the northern Pacific from 0.4 to 4.5 x 1031"1. Their populations were dominated by naked forms of Strombidium, Strombilidium and Tontonia. In some shelf areas, up to 40 % of the total ciliate population was represented by the symbiotic ciliate Meso-dinium rubrum. The data on the integrated biomass of basic groups of planktonic micToheterotrophs are also presented, and their importance in the trophic relationships in pelagic communities of subarctic seas is discussed.