Ocean and Polar Research

  • 제25권3호
  • /
  • Pages.315-329
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  • 2003
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  • 1598-141X(pISSN)
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  • 2234-7313(eISSN)
한국해양과학기술원 (Korea Institute of Ocean Science & Technology)
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제 1차 한-러 북극해 탐사(2000년 8월) 동안의 바렌츠해와 카라해의 식물플랑크톤 현존량 및 영양염 분포

Distribution of Phytoplankton Biomass and Nutrient Concentrations in the Barents and Kara Seas during the 1st Korea-Russia Arctic Expedition in August, 2000

  • 강성호 (한국해양연구원, 극지연구소, 극지환경특성연구본부) ;
  • 정경호 (한국해양연구원, 극지연구소, 극지환경특성연구본부) ;
  • 강재신 (한국해양연구원, 극지연구소, 극지환경특성연구본부) ;
  • 김예동 (한국해양연구원, 극지연구소, 극지환경특성연구본부)
  • 발행 : 2003.09.30
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초록

During the 1st Korea-Russia Arctic Expedition from 3 to 26 August, 2000 phytoplankton biomass and nutrient concentration were measured in the Barents and Kara Seas. Total of 57 surface samples were collected f3r the phytoplankton related measurements. Chlorophyll a (chi a) concentraitons were measured to investigate the relations between physico-chemical factors and phytoplankton biomass distribution. Chl a values ranged from 0.14 to $2.34mg\;m^{-3}$ (mean of $0.65{\pm}0.42mg\;m^{-3}$) over the surface stations. The elevated values of the chi a concentrations $(1.49{\sim}2.34mg\;m^{-3})$ were found in the southeastern Barents Sea near the Pechora River. Nanoplanktonic $(<20{\mu}m)$ phytoflagellates were the important contributors for the increase of the chi a. The nano-sized phytoflagellates accounted for more than 80% of the total chi a biomass in the study area. Mean chi a concentration in the Barents Sea $(0.72{\pm}0.57 mg\;m^{-3})$ was higher than in the Kan Sea $(0.52{\pm}0.45mg\;m^{-3})$, but there was no big difference between two areas. Surface temperatures and salinities ranged from 4.1 to $11.7^{\circ}C$ (mean of $8.8{\pm}1.9^{\circ}C$) and from 23.8 to 32.5psu (mean of $30.3{\pm}1.9^{\circ}C$ psu), respectively. The physical factors were not highly correlated with phytoplankton distribution. It is speculated that the insignificant correlation between phytoplankton biomass and physical factor was due to the same current which introduced similar water mass with higher water temperature and lower salinity into the study area. The mean values of major nutrients such as ammonia, nitrite, nitrate, phosphate, and silicate were $0.42{\pm}0.31{\mu}M,\;0.10{\pm}0.03{\mu}M,\;1.44{\pm}1.03{\mu}M,\;0.35{\pm}0.12{\mu}M,\;10.99{\pm}3.45{\pm}M$, respectively. The relations between phytoplankton biomass and nutrient concentration were not close, indicating that the surface nutrient concentrations during the study seem to be controlled by other physical factors such as input of fresh water (i.e. dilution effects).

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피인용 문헌

  1. Phytoplankton and Environmental Factors in the Southeastern Barents Sea during August 2003 vol.27, pp.3, 2005, https://doi.org/10.4217/OPR.2005.27.3.265