Phytoplankton characteristics and hydrological conditions in the western part of the Sea of Okhotsk in the spring of 1999 and 2000 based on expeditionary and satellite data
Using the data obtained in 1999-2000 during the spring bloom of phytoplankton (late May-early June), the variability of the pigment concentrations, the phytoplankton biomass and species compositions, and the hydrological conditions on the eastern shelf of Sakhalin Island was studied. The study resul...
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Veröffentlicht in: | Oceanology (Washington. 1965) 2007-08, Vol.47 (4), p.519-530 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Using the data obtained in 1999-2000 during the spring bloom of phytoplankton (late May-early June), the variability of the pigment concentrations, the phytoplankton biomass and species compositions, and the hydrological conditions on the eastern shelf of Sakhalin Island was studied. The study resulted in revealing 135 microalgae species belonging to eight divisions. The most diversely presented were the Dinophyta dinoflagellates and Bacillariophyta diatoms (70 and 53 species, respectively). The concentration of chlorophyll a in the euphotic zone amounted, on average, to 3.8 mg/m^sup 3^ in 1999 and 2.4 mg/m^sup 3^ in 2000. It was shown that, in the northern and southern parts of the coastal zone, the concentration of chlorophyll a and the phytoplankton density in the spring were considerably different and depended on the hydrological conditions. In the north, their maximum values were found in the area of the depth break and were determined by the tidal mixing. The increased algae concentrations and temperature inversions at depths of 400-600 m confirm the downslope sliding of the near-bottom shelf waters. In the southern part, the high phytoplankton concentrations in the surface layer in 1999 confirmed by the monthly averaged estimates from the SeaWiFS satellite color scanner were caused by the abnormal northward propagation of the Soya Current waters and by intense tidal mixing.[PUBLICATION ABSTRACT] |
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ISSN: | 0001-4370 1531-8508 |
DOI: | 10.1134/S0001437007040091 |