2007
DOI: 10.1134/s0097807807020091
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Characteristic of microalgae development in the Sea of Okhotsk in winter and modeling of their annual dynamics in Aniva Bay

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Cited by 6 publications
(4 citation statements)
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“…In particular, T. nordenskioeldii usually dominates the spring phytoplankton bloom in the shelf surface waters of the Sea of Okhotsk with water temperatures of 2-5 • C and salinities of 20-27 (Sorokin and Sorokin, 1999). There is evidence that Thalassiosira is abundant in the eastern coastal waters of Sakhalin Island along the moving path of the drift ice in winter and after ice retreat (Sorokin and Sorokin, 1999;Leonov et al, 2007;Zakharkov et al, 2007). We thus suggest that Thalassiosira could be a common component in the drift ice of the Sea of Okhotsk and they play important roles in the drift ice and seawater in the Sea of Okhotsk during the winter and the ice melt season.…”
Section: Discussionmentioning
confidence: 99%
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“…In particular, T. nordenskioeldii usually dominates the spring phytoplankton bloom in the shelf surface waters of the Sea of Okhotsk with water temperatures of 2-5 • C and salinities of 20-27 (Sorokin and Sorokin, 1999). There is evidence that Thalassiosira is abundant in the eastern coastal waters of Sakhalin Island along the moving path of the drift ice in winter and after ice retreat (Sorokin and Sorokin, 1999;Leonov et al, 2007;Zakharkov et al, 2007). We thus suggest that Thalassiosira could be a common component in the drift ice of the Sea of Okhotsk and they play important roles in the drift ice and seawater in the Sea of Okhotsk during the winter and the ice melt season.…”
Section: Discussionmentioning
confidence: 99%
“…There is a substantial standing stock of ice algae in the Okhotsk Sea ice. Dense ice algal communities have commonly been observed at the bottom of Okhotsk sea ice, especially in spring (Leonov et al, 2007). Chlorophyll a (Chl a) concentrations in the Okhotsk sea ice ranged between 0.2 to 3.5 mg m −2 , and was up to an order of magnitude higher than the under-ice seawater (Granskog et al, 2015).…”
Section: Introductionmentioning
confidence: 99%
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“…Phytoplankton biomass, including diatoms, is concentrated in summer over the Sakhalin Shelf at the upper boundary of a thermocline ranging from the surface to 10–15 m depths ( Sorokin & Sorokin, 1999 ; Rutenko & Sosnin, 2014 ; Prants et al, 2017 ). Vertical mixing and down-welling of Sakhalin Shelf waters is prevalent in winter ( Leonov et al, 2007 ). The 40-60 m depth ranges of the Offshore benthos are thus below the high surface concentrations of phytoplankton in summer.…”
Section: Discussionmentioning
confidence: 99%