• 제목/요약/키워드: phytoplankton area

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서해(西海) 경기만(京幾灣) 식물(植物) 플랑크톤에 대(對)한 생태학적(生態學的) 연구(硏究) -IV. 식물(植物)플랑크톤의 군집구조(群集構造)와 계절적 천이 기작 (The Ecological Study of Phytoplankton in Kyeonggi Bay, Yellow Sea -IV. The Successional Mechanism and the Structure of the Phytoplankton Community)

  • 최중기;심재형
    • 한국해양학회지
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    • 제23권1호
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    • pp.1-12
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    • 1988
  • 경기만 식물 플랑크톤의 군집구조와 천이현상을 규명하기 위하여 군집의 다양성과 우정도, 군집사이의 유사도 및 종성분에 의한 주성분 분석등이 연구되었고 군집변화에 영향을 미치는 환경요인을 알기 위하여 주성분 분석이 이루어졌다. 다양성지수와 우정도 분석에 의하면 경기만내 식물 플랑크톤 군집은 큰 물리적 환경변화와 오염수의 유입으로 인하여 불안정한 환경하에 놓여있는 것으로 나타났다. 조사수역은 군집간의 유사도 분석에 의하면 강수유입에 영향을 받는 지역, 오염수의 영향을 받는 지역, 비교적 오염수의 영향을 덜 받으나 조석주기에 의해 변화가 큰 지역등으로 구분되었다. 전체 식물 플랑크톤 군집은 춘계형, 하계형, 추계형, 추 동계형의 4계절 양상으로 뚜렷하게 변화하며 천이하였다. 춘 하 추를 대표하는 하계군집들은 주로 일반적인 식물 플랑크톤들로 구성되었으며 온도와 광조건에 크게 영향을 받는 것으로 나타났고 늦가을 부터 초봄까지 많이 나타나는 동계군집들은 일시 부유성 저서 규조류로 주로 구성되어 있으며 부유퇴적물과 영양염의 높은 농도와 밀접한 관계를 보였다.

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초여름 韓國 西南海域 植物플랑크톤의 群集構造와 分布 (Community Structure and Spatial Distribution of Phytoplankton in the Southwestern Sea of Korea, in Early Summer)

  • 심재형;박용철
    • 한국해양학회지
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    • 제19권1호
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    • pp.68-81
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    • 1984
  • 한국 서남해역에 있어서 식물플랑크톤의 군집구조와 분포를 밝히기 위하여 1980년 여름에 수평적, 수직적으로 채집한 정량 자료를 분석하였다. 연구해역은 상이한 水塊를 대표하는 상이한 3개의 특징적인 군집을 이루고 있음을 보여준다. 제 1 군집은 대부분 연안성 및 내수성 硅藻類로 구성되어 서남해의 연안 수역을 대표하며, 제 2 군집은 외양성 및 연안성 구조류와 2-3종의 鞭毛藻類로 구성되어 黑潮의 지류로 생각되는 高鹽 水性인 제주 부근의 수역을 대표한다. 제 3 군집은 주로 소형인 鞭毛藻류와 微細藻類로 구성되고 底鹽 수성인 중간 수역을 대표하는 것으로 나타났다. 또한 식물플랑크톤과 환경요인의 수직분포에서 세포수, chlorophyll-a, 및 용존산소등이 특히 계절적인 pycnocline 부근의 수층에서 높은 농도를 보여준다. nanoplankton은 군집내에서 90% 이상에 이를 만큼 점유율을 보여 중요성이 높음을 나타낸다.

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경주시 연안해역의 식물플랑크톤 군집 장기 변동 (Long-term Variations of Phytoplankton Community in Coastal Waters of Kyoungju City Area)

  • 김현정;박재영;손민호;문창호
    • 수산해양교육연구
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    • 제28권5호
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    • pp.1417-1434
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    • 2016
  • Starting from the February 2008 till the end of November 2014, abundance of phytoplankton and their composition living in the coastal waters of Kyoungju city were investigated. Environmental and biological properties were also observed at 10 different stations on a seasonal basis. Due to the environmental variables, fluctuating pattern was appeared during the entire period of observation with different degree, as compared to those found in other costal waters in the East Sea. The concentration of phosphate was turned out to be very low which was even less than threshold level in the study area. Phytoplankton community structure was dominated by diatoms (both micro- and nanoplankton fractions) for several years and seasonal succession was also relied on the diatoms. The importance of dinoflagellates in the community was relatively low. Abundance of phytoplankton was heavily affected by physical factors in the surface water, however, affected more by chemical factors including nutrients in the deep water. For periods of this study, the phosphate concentrations was observed in an extremely low, which indicates that the main limiting factor affecting phytoplankton growth could be phosphate.

회동수원지의 식물플랑크톤군집에 관하여 (On the phytoplankton community in Hoe-dong Reservoir)

  • 문성기;홍채규;정종문
    • 한국환경과학회지
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    • 제4권3호
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    • pp.167-176
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    • 1995
  • A study on phytoplankton community was carried out from June, 1992 to May, 1993 at selected stations in Hoedong Reservoir. The phytoplankton are identified as 176 taxa including 5 phylum, 67 genera. The important species in this reservoir were Asterionella formosa, C meneghiniana, Dictyosphaerium plilchellum, Fragilaria crotonensis, Melosira distans, M grantulata, M. granulata var. angustissima, M. granulate var. angntissima f. spirdis, Micractinium pussillum, Microcystis aeruginosa, Pundorina morn, Pediastrum boryanum, P. duplex, Peridinium sp., Scenedesmus quadriauda, Synedra acus, S. rumpens and S. ulna. The causative species of water bloom were identified as Microcystis aeruginsa, Trahellomonas hispida, Ceratium hirwdinella, Peridinium sp., Melosira italica, Staurastrum dorsidentiferum var. onatum in the area. During the study periods standing crcps of phytoplankton were maximum in August, 1992 and minimum in December 1992. The species dominance index and diversity index were ranged 24.7-99.9, 0.001-3.06, respectively. Key Words : phytoplankton community, causative species of water bloom, standing crops. dominance index, species diversity index.

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낙동강 하류에서 식물플랑크톤 생산력과 수질 변화와의 관계 (The Relationship between Phytoplankton Productivity and Water Quality Changes in Downstream of Nakdong River)

  • 박홍기;정종문;박재림;홍용기
    • 한국환경과학회지
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    • 제8권1호
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    • pp.101-106
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    • 1999
  • The relationship between primary productivity and changes in water quality was investigated at Mulgum station, a site downstream of the Nakdong River, Korea. Phytoplankton production was characterized by blooms of Microcystis aeruginosa during the summer and Stephanodiscus hantzschii during the winter. Primary production and secondary production by bacterioplankton ranged from 1.5~53.5 mg-C/ι day and 0.1~0.3 mg-C/ι day, respectively. Distribution of total organic carbon appeared to be highly correlated with phytoplankton biomass, especially during blooms of M. aeruginosa, when particulate organic carbon was 81% of total organic carbon and the main source of organic materials supplied into the water. The correlation coefficient between chlorophyll-a and BOD was 0.86. Thus it was concluded that autochthonous phytoplankton mostly affected the BOD level. Total bacterial numbers were also highly correlated with chlorophyll-a ($r^2$= 0.84) and the bacterial community appears to be regulated by phytoplankton biomass in this area.

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Comparison of Water Quality According to Seasonal Variation in Mokpo and Wando Costal Areas

  • Kim, Woo-Hang;Lee, Young-Sik
    • 한국환경과학회지
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    • 제17권3호
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    • pp.269-273
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    • 2008
  • The objective of this study was to evaluate the relationship between nutrients and phytoplankton. This study was done by the comparison to two costal areas Mokpo, which inflow fresh water, and Wando. In August, salinity of the sea water decreased by 3.5-4.5%o in Mokpo coastal area, but was not nearly decreased in Wando coastal area. This suggests a lot of fresh water inflow in Mokpo coastal area. DIN and DIP were decreased by water temperature increasing in Wando. However, in Mokpo, DIN and DIP were increased greatly during the summer season. Nitrogen was limited to a 10 NIP ratio especially during the summer season in Wando coastal area while phosphorus in Mokpo coastal area was limited with over 28 N/P ratio in all the seasons. Coefficient of determination$(r^2)$ between DIP and Chl.-a was 0.91 in Mokpo coastal area. On the other hand, Coefficient of determination$(r^2)$ between Chl.-a and DIN, DIP were 0.93 and 0.89, respectively, in Wando coastal area. These results suggest DIP in Mokpo and DIN and DIP in Wando might be limited at the increase of phytoplankton.

Nutrient Depletion and Primary Productivity in the Marginal Ice Zone of the Northwestern Weddell Sea During Austral Summer

  • Kang, Sung-Ho;Chung, Kyung-Ho;Kim, Dong-Yup;Park, Byong-Kwon;Kim, Dong-Seon
    • Journal of the korean society of oceanography
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    • 제35권1호
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    • pp.34-45
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    • 2000
  • Spatial distributions of phytoplankton biomass and nutrients were examined to investigate the magnitude of phytoplankton blooms along the marginal ice zone (MIZ) in the northwestern Weddell Sea during austral summer of 1995. High phytoplankton biomass was associated with the MIZ in the study area. Vertical stability induced by meltwater appears to be the most important factor controlling phytoplankton biomass distribution. Nitrate concentrations are significantly depleted within the upper water column at the phytoplankton biomass maximum. The time required to attain the observed nutrient depletion was calculated from phytoplankton biomass and nitrate depletion, which ranges from 27 to 68 days in transect 4 and from 33 to 145 days in transect 3. Phytoplankton production was also calculated from nitrate depletion and time-scales of nitrate depletion, which varies from 272 to 1752 mg C m$^{-2}$ day$^{-1}$ in transect 4 and from 327 to 2648 mg C m$^{-2}$ day$^{-1}$ in transect 3. In the Southern Ocean where primary productivity shows large temporal and spatial variations, the productivity measurement from nutrient depletion can provide an average rate of primary production during phytoplankton bloom.

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Phytoplankton Community in Adjacent Waters of Ulchin Nuclear Power Plant

  • Choi, Hyu Chang;Kang, Yeon Shik;Jeon, In Sung
    • 환경생물
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    • 제22권3호
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    • pp.426-437
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    • 2004
  • To understand the phytoplankton community in adjacent waters of Ulchin nuclear power plant (UNPP), abundance and the size fractionated $chl-\alpha$ concentrations were evaluated through seasonal interval sampling from April 2003 to February 2004. A total of 211 different phytoplankton species was observed and mean abundance of phytoplankton in each study period ranged from 244,286 to 1,221,779 cells $L^{-1}$. The contributions of microplankton $(>20\mu{m})$ to total phytoplankton abundance ranged from 42.5 to 83.6% (average 66.1%) and those of nanoplankton $(>20\mu{m})$ ranged from 16.4 to 57.5% (average 33.9%). Total chl-$\alpha$ concentrations of phytoplankton ranged from 0.52 to $2.26\mu{g}\;L^{-1}$. The contribution of chl-$\alpha$ concentrations of microplankton was higher than that of nano- and picoplankton through the study period with exception of July 2008. The results of abundances and $chl-\alpha$ concentrations suggest that microplankton has an important role in adjacent waters of UNPP. The diminution of abundances and $chl-\alpha$ concentrations of phytoplankton was observed after passage through the cooling water system, but it was gradually recovered by mixing with the ambient waters. Our results suggested that the influence of thermal discharges on phytoplankton should be restricted within narrow limits around outlet area of thermal effluents.

2016년 한국 수산자원보호해역에서 식물플랑크톤 군집의 계절 및 해역별 분포 (The Seasonal and Regional Distribution of Phytoplankton Communities in the Fisheries Resources Protection Area of Korea in 2016)

  • 유만호;박경우;오현주;구준호;권정노;윤석현
    • 해양환경안전학회지
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    • 제24권2호
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    • pp.288-293
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    • 2018
  • 수산자원보호해역의 계절 및 해역별 식물플랑크톤 군집특성을 파악하기 위해, 2016년 천수만, 통영(I, II), 한산만, 진동만에서 식물플랑크톤 군집조성, 현존량 및 우점종을 조사하였다. 조사결과, 대부분의 환경요인(수온, 염분, 영양염류)은 계절적인 변화가 뚜렷한 반면 부유물질은 해역별 차이를 보였다. 식물플랑크톤 현존량은 평균 $13{\sim}4,062cells{\cdot}ml^{-1}$의 범위로 조사시기 및 해역에 따라 큰 변동범위를 보였다. 특히 천수만은 4월과 10월에 식물플랑크톤 대량증식(>$10^3cells{\cdot}ml^{-1}$)이 발생하였고, 우점종인 Skeletonema spp.(4월)와 Chaetoceros socialis(10월)가 시기적인 차이를 보였다. 조사해역의 식물플랑크톤 우점종은 Pseudo-nitzschia spp., Skeletonema spp., Chaetoceros pseudocriniuts 등의 돌말류와 와편모류인 Scrippsiella trochoidea, Tripos furca 등이 출현하였다. 계절적으로는 돌말류가 동 추계에 우점하는 반면 와편모류가 춘 하계에 우점하는 일반적인 연안특성을 보였다. 단, 지역적으로는 고탁도 해역인 서해에 위치한 천수만이 남해 해역보다 돌말류가 차지하는 비율이 9 ~ 27 %가 높았다.