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Structure of the zooplankton communities in the region of the Ob River’s estuarine frontal zone

  • Marine Biology
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Oceanology Aims and scope

Abstract

The studies were carried out on September 27–30, 2007, in the area of the Ob estuarine frontal zone and over the adjacent inner Kara Sea shelf. Based upon the latitudinal changes in the salinity, the 100 nautical mile wide estuarine frontal zone was marked out. The frontal zone was inhabited by a specific zooplankton community dominated by species that occurred outside the frontal zone in only minor amounts. The biomass of the mesozooplankton averaging 984 mg/m3 in the frontal zone exceeded by 1.5 and 6 times the corresponding values in the inner desalinated area of the estuary and the adjacent areas of the Kara Sea shelf. At the inner southern periphery of the frontal zone, at maximal latitudinal salinity gradients (>2 psu per mile), the maximal development of the mesoplankton with the mean biomass for the water column of 3.1 g/m3 (37 g/m2) and up to 5.8 g/m3 in the subpycnocline layer was observed. The latitudinal extension of the biomass in the maximum zone did not exceed 10 miles. More than 90% of the maximum was composed of herbivorous zooplankton with the strong domination of the copepod Limnocalanus macrurus. The daily consumption within the zooplankton maximum area was estimated at 820 mgC/m2 per day. This value exceeds by two orders of magnitude the local primary production. At that level of consumption, the available phytoplankton biomass was consumed by grazers in less than 8 hours (!). A zooplankton aggregation at the southern periphery of the estuarine front exists due to the advection of phytoplankton from the adjacent river zone. The aggregation forms a natural pelagic biofilter where new allochthonous organic matter delivered by the river flow is accumulated and high secondary production is formed on its basis. An anomalously high concentration of planktic predatory Parasagitta elegans with biomass of over 1 g/m3 (46% of the total zooplankton biomass) was associated with the outer northern periphery of the estuarine frontal zone.

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Authors and Affiliations

  1. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia

    M. V. Flint, T. N. Semenova, E. G. Arashkevich, I. N. Sukhanova, V. I. Gagarin, V. V. Kremenetskiy, M. A. Pivovarov & K. A. Soloviev

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  1. M. V. Flint
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  2. T. N. Semenova
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  3. E. G. Arashkevich
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  4. I. N. Sukhanova
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  5. V. I. Gagarin
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  6. V. V. Kremenetskiy
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  7. M. A. Pivovarov
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  8. K. A. Soloviev
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Correspondence to M. V. Flint.

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Original Russian Text © M.V. Flint, T.N. Semenova, E.G. Arashkevich, I.N. Sukhanova, V.I. Gagarin, V.V. Kremenetskiy, M.A. Pivovarov, K.A. Soloviev, 2010, published in Okeanologiya, 2010, Vol. 50, No. 5, pp. 809–822.

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Flint, M.V., Semenova, T.N., Arashkevich, E.G. et al. Structure of the zooplankton communities in the region of the Ob River’s estuarine frontal zone. Oceanology 50, 766–779 (2010). https://doi.org/10.1134/S0001437010050139

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  • DOI: https://doi.org/10.1134/S0001437010050139

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