The role of zooplankton in the transformation of the organic matter in the Ob estuary,on the shelf,and in the deep regions of the Kara Sea |
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| Authors: | E G Arashkevich M V Flint A B Nikishina A F Pasternak A G Timonin J V Vasilieva S A Mosharov K A Soloviev |
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| Institution: | (3) Russian Academy of Sciences, Vernadsky Inst. Geochemistry, Analytical Chemistry, Kosygina Str. 19, 119991 Moscow, Russia;(4) Russian Academy of Sciences, Inst. Geology, Pyzhevsky per. 7, 119017 Moscow, Russia |
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| Abstract: | The data for the present study were collected at 20 sampling stations in the Kara Sea along the transect from the Ob estuary
to the deep sea St. Anna Trough in September 2007. Based on the hydrophysical features, the distribution of the Chl a, and the primary production, we distinguished six habitats: the river, estuary, inner and outer shelf, continental slope,
and trough. The impact of the small-size (<0.5 mm) and large-size (>0.5 mm) fractions of the zooplankton on the phytoplankton’s
organic carbon in the different regions of the Kara Sea was estimated. The ingestion rate was assessed using the analysis
of the gut fluorescence content and the gut evacuation rate. The zooplankton grazed 1–2% of the phytoplankton biomass in the
river and estuary; 3.5% over the shelf; and 6 and 10% in the regions of the trough and slope, respectively. The grazing impact
of the small-sized zooplankton increased from the river zone to the deep regions (from 1 to 90%) along with their share in
the total zooplankton abundance (from 18 to 95%). From 72 to 86% of the primary production was grazed over the shelf and slope.
The primary production did not cover the feeding requirements of the zooplankton in the estuarine regions and St. Anna Trough
in the autumn. In the estuarine regions, the major portion of the organic matter settles on the bottom due to the strong inflow
of the allochthonous matter and the relatively low zooplankton grazing. |
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