• 제목/요약/키워드: Micro-phytoplankton

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Spatio-temporal Fluctuations of Size-structured Phytoplankton over an Annual Cycle in the Youngsan Lake

  • Song, Eun-Sook;Shin, Yong-Sik
    • 생태와환경
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    • 제41권4호
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    • pp.530-540
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    • 2008
  • The temporal and spatial variations of size-structured phytoplankton dynamics in Youngsan Lake were investigated to explore potential mechanims controlling the dynamics in the Youngsan Lake. Field data were collected monthly from February to October, 2003 at 6 stations along the axis of Youngsan Lake. In this study, phytoplankton (chlorophyll $\alpha$) were categorized into three size classes: micro-size ($>20{\mu}m$), nano-size ($2{\sim}20{\mu}m$) and pico-size ($<20{\mu}m$). Water temperature, light attenuation coefficients, PAR (photosynthetically active radiation) and suspended solids were measured to analyze relationship between physical-chemical properties and size structure of phytoplankton. Phytoplankton blooms developed during March, July and October in the upper region of the main stem whereas small-scaled spring bloom was observed in the lower region. The scales of phytoplankton blooms were higher in the upper regions than the lower region and blooms were predominated by micro-size class in upper region but predominated by nano-size class in lower region. Growth of size-structured phytoplankton appeared to be controlled by rather light availability than temperature-dependant metabolisms in the system. Phytoplankton growth may be also supported by ambient nutrients available in the water column from analyses of chlorophyll $\alpha$ vs. nutrient concentrations including nitrite+nitrate and orthophosphate. Growth of nano-sized phytoplankton alone appeared to be supported by orthophosphate as well as nitrite+nitrate indicating that response of phytoplankton to nutrient inputs may be size-dependent.

A Possible Explanation for the Dominance of Chlorophyll in Pico and Nano-size Fractions in the Waters Around the South Shetland Islands

  • Kawaguchi, So;Shiomoto, Akihiro;Imai, Keiri;Tsarina, Yoriko;Yamaguchi, Hitomi;Noiri, Yoshifumi;Iguchi, Naoki;Kameda, Takahiko
    • Ocean and Polar Research
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    • 제23권4호
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    • pp.379-388
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    • 2001
  • Ch1 a abundance, Ch1 a-specific productivity and phytoplankton growth rate in each size fraction (pico, $<2{\mu}m$; nano, $2-10{\mu}m$; micro, > $10{\mu}m$) in the waters around the South Shetland Islands (Ant-arctic Peninsula Area) were analysed. Although Ch1 a-specific productivity and growth rate were highest in micro-size fractions, ChI a abundance was highest in pico-size fractions. Selective removal of nano- and micro-size phytoplankton especially by krill and salp grazing, but not limitation of phytoplankton growth, seemed to be the major reason to explain this miss match between productivity and abundance of the phytoplankton community.

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담수성 식물플랑크톤의 크기별 동태에 대한 상향식, 하향식 조절간의 상대적 중요도 조사: I. 크기구조의 시 ${\cdot}$ 공간적 변동 (Relative Importance of Bottom- up vs. Top-down Controls on Size-structured Phytoplankton Dynamics in a Freshwater Ecosystem: I. Temporal and Spatial Variations of Size Structure)

  • 김종민;신용식
    • 생태와환경
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    • 제36권4호통권105호
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    • pp.403-412
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    • 2003
  • 전남 주암호에서의 식물플랑크톤 동태를 파악하기 위해 2003년 2월부터 10월까지 식물플랑크톤생체량 (클로로필 a)의 크기별 시 ${\cdot}$ 공간적 변동과 제반 환경요인에 대해 조사하였다. 본 논문에서는 주암호와 같은 담수호에서 식물플랑크톤의 크기 구조가 계절적, 공간적으로 어떻게 변화하고 그러한 변화 속에서 물리적 요인들이 어떤 영향을 미치는지 회귀분석을 통해 파악하고자 하였다. 식물플랑크톤 (클로로필 a)은 세 그룹 즉, 대형 (micro-size > 20 ${\mu}m$), 소형 (nano-size 3-20 ${\mu}m$) 마지막으로 초소형 (pico-size, < 3 ${\mu}m$)으로 구분했다. 물리적 특성 파악을 위해 수온, 광소멸계수, PAR (photosynthetically active radiation), 수중 탁도등도 동시에 측정하였다. 최대치의 클로로필 a 는 2003년 하류지역에서는 4월에 상류지역에서는 10월에 발생하였다. 식물플랑크톤의 대번성기에는 대부분 세포크기가 큰 대형 (micro-size)식물플랑크톤이 우세하였다. 주암호의 크기별 식물플랑크톤의 변동에 영향을 미칠 수 있는 물리적 특성들에 대해 논의하였다.

2002-2007년 통영바다목장해역에서 식물플랑크톤 현존량 및 생체량에 따른 우점종의 변동 및 관계 (Variation and Relationship between Standing Crops and Biomass of Phytoplankton Dominant Species in the Marine Ranching Ground of Tongyeong Coastal Waters from 2000 to 2007)

  • 정승원;권오윤;이진환
    • ALGAE
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    • 제23권1호
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    • pp.53-61
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    • 2008
  • In order to understand variation and relationship between standing crops and biomass of phytoplankton dominant species for the long term periods, this study was seasonally investigated in the marine ranching ground of Tongyeong coastal waters from 2000 to 2007. Total 268 taxa representing 217 Bacillariophyceae, 46 Dinophyceae, 4 Dictychophyceae, 1 Euglenophyceae were observed in phytoplankton communities. Dominant species consisted of 5 species as standard in standing crops: Chaetoceros curvisetus (18.01%), Chaetoceros socialis (12.95%), Skeletonema costatum (8.39%), Chaetoceros compressus (6.87%), Asterionellopsis glacialis (5.02%). However, to determine dominant species as biomass concept, Ditylum brightwellii, Guinardia striata, Rhizosolenia spp. and Skeletonema costatum were occupied with dominant species (19.67%). As determining for cell sizes, dominant species were divided with two groups such as micro- and nanophytoplankton (standing crops) and mesophytoplankton (biomass). However, Skeletonema costatum in anophytoplankton was associated to affect fluctuation between standing crops and biomass.

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.

Seasonal Variation of Phytoplankton Community Structure in NortheasternCoastal Waters off the Korean Peninsula

  • Kang, Yeon-Shik;Choi, Hyu-Chang;Noh, Jae-Hoon;Choi, Joong-Ki;Jeon, In-Seong
    • ALGAE
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    • 제21권1호
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    • pp.83-90
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    • 2006
  • Phytoplankton community in the coastal waters off the northeastern Korean Peninsula were characterized from May 2002 to August 2003. Taxonomic composition, abundance and biomass were determined at two water depths at 10 sample sites. A total of 153 phytoplankton species including 121 diatoms, 28 dinoflagellates, 7 green algae and 7 other species were identified. The mean abundance of phytoplankton varied from 15 to 430 cells mL–1 in the surface layer and from 11 to 545 cells mL–1 in the bottom layer, respectively. Phytoplankton was more abundant in coastal stations relative to those in more open ocean. The most dominant species were marine diatoms such as Thalassionema nitzschioides, Licmorphora abbreviata, Chaetoceros affinis and Chaetoceros socialis. In addition, a few limnotic diatoms including Fragilaria capucina v. rumpens, the green alga Scenedesmus dimorphus, some marine dinoflagellates and Cryptomonas sp. appeared as dominant species. Mean concentration of total chlorophyll-a varied from 0.22 to 7.87 μg chl-a L–1 and from 0.45 to 6.79 μg chl-a L–1 in the surface and bottom layers, respectively. The contribution of phytoplankton each size-fractionated varied highly with season. The contribution of microphytoplankton to total biomass of phytoplankton in the surface and bottom layer was high in February and August 2003, and that of nano-phytoplankton was high in May 2002 in both surface and bottom layers.

동해에서 식물플랑크톤 군집 분포 분석을 위한 GOCI 활용 연구 (A Study on the Application of GOCI to Analyzing Phytoplankton Community Distribution in the East Sea)

  • 최종국;노재훈;;;이미진
    • 대한원격탐사학회지
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    • 제36권6_1호
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    • pp.1339-1348
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    • 2020
  • 식물성플랑크톤은 영양염, 광합성, 탄소순환 등의 측면에서 해양의 생태계를 제어하는데, 해양 환경에 미치는 영향의 정도는 식물성플랑크톤의 크기에 좌우된다. 원격탐사 기술을 기반으로 해양의 식물성플랑크톤 크기 별 생체량을 식별하려는 많은 연구가 있었으며, 그 중 가장 성공적인 접근법 중 하나는 식물성플랑크톤의 크기를 세 등급(micro-plankton;> 20 ㎛, nano-; 2-20 ㎛ 및 pico-; <2 ㎛)으로 구분하여 각 그룹별 엽록소 농도를 추정하는 삼성분 모델(three-component model)이다. 이 연구에서는 동해에서 식물성플랑크톤의 크기 별 생체량 분포를 추정하기 위한 GOCI 자료의 활용 가능성에 대해 검토하였다. 각 크기 별 엽록소 농도(CHL)를 도출하기 위해, 연구지역에서 수 년 동안 수집된 식물성플랑크톤 색소자료를 기반으로 회귀분석을 통해 삼성분 모델의 계수를 산출하였다. 새롭게 산출된 삼성분 모델을 시간 별 GOCI 기반 엽록소 농도 이미지에 적용하여, 전체 엽록소 농도 중 각 식물성플랑크톤 크기 별 생체량이 차지하는 비율을 산출하였다. 또한, 이 결과를 이용하여 동해에서 2013년 여름 대규모 적조가 발생한 시기의 크기 별 엽록소-a 농도 분포를 분석하였다.

동해 울산항에서 이화학적 환경요인 및 크기그룹별 식물플랑크톤 생체량의 계절적 변동 (Seasonal variation of physico-chemical factors and size-fractionated phytoplankton biomass at Ulsan seaport of East Sea in Korea)

  • 권오윤;강정훈
    • 한국산학기술학회논문지
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    • 제14권11호
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    • pp.6008-6014
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    • 2013
  • 울산항의 물리 및 이화학적 요인과 크기그룹별 식물플랑크톤 생체량의 계절변이 이해를 위해, 2007년 2월부터 2009년 11월까지 계절 조사를 수행하였다. 조사기간 중 수온과 염분은 각각 8.94-$24.26^{\circ}C$와 25.06-34.54 psu의 범위에서, 용존산소는 4.30-10.73 mg/L, 수소이온농도는 7.97-8.53, 화학적 산소요구량은 0.66-40.70 mg/L, 그리고 총 부유물질은 57.4-103.3 mg/L의 범위에서 변이를 나타냈다. 이 요인들은 무기영양염과 생체량을 지시하는 총 엽록소-a 농도 분포특성과 달리 뚜렷한 공간적 분포차이가 없었다. 무기영양염 중 인산염은 0.01-3.03 ${\mu}M$의 범위에서, 질산염은 0.05-21.62 ${\mu}M$, 그리고 규산염은 0.01-27.82 ${\mu}M$의 범위에서 변이를 나타냈는데, 특히 내측정점의 농도가 외측정점에 비해 약 2배 이상 높은 특징을 나타냈다. 총 엽록소-a 농도는 0.36-7.11 ${\mu}gL^{-1}$의 범위로, 내측정점 (평균 1.88 ${\mu}gL^{-1}$)에서 외측정점 (평균 0.90 ${\mu}gL^{-1}$)에 비해 높게 나타나 무기영양염의 분포특성과 유사하였다. 소형플랑크톤은 봄철 (34.0-81.2%), 여름철 (35.1-65.6%) 및 겨울철 (3.9-62.0%)에 전체 생체량의 높은 비율을 차지했고, 가을철에는 미소 및 초 미소플랑크톤이 각각 58.2-74.5%와 22.4-38.2%의 높은 비율을 나타냈다. 그러나 각 크기그룹별 생체량의 점유율의 내측 및 외측 정점 간의 공간분포는 뚜렷한 차이가 없었다. 따라서 동해 울산항의 식물플랑크톤은 계절적으로 가을철을 제외한 모든 시기에 소형플랑크톤 그룹 (평균 52.3%)에 의해 주도되었고, 이는 무기영양염의 농도와 밀접함을 지시하였다 (p<0.05).

Fundamental Structure in Simultaneous Removal for Phytoplankton and Nutrient Salt in Lakes

  • SEKI, Tatsuhiro;ISHII, Yuuichi;ISHII, Toshio;TAKI, Kazuo
    • Environmental Engineering Research
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    • 제14권4호
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    • pp.220-225
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    • 2009
  • The water quality in eutrophic lakes is affected by serious problems, such as abnormal increasing of Cyanobacteria. The purpose of this study was to investigate the possibility of a modified flotation system using a hybrid technique formed by chemical compounds and an electrostatic bridge. Therefore, experiments using the hybrid technique were performed to measure the zeta potential value on the phytoplankton surface and the removal efficiencies of phytoplankton, ammonia nitrogen, nitrate nitrogen and phosphoric acid. The results were as follows: Firstly, the zeta potential of M.aeruginosa was observed to approach charge neutralization due to adhesion of magnesium hydroxide precipitate on the phytoplankton surface in the pH range 10.5 to 11. Secondly, the concentration of chlorophyll-a decreased from about 150 to 20${\mu}g$g/L, with a maximum removal efficiency of 84% due to coagulation with pH values higher than 10. Thirdly, the N$H_4$-N concentration was observed to decrease from 0.62 to 0.54mg-N/L (13%), and the P$O_4$-P concentration, which is a limiting factor to the formation of algae blooms, decreased from 0.27 to 0.02mg-P/L (92%). These findings suggest that the modified flotation system can be applied for the purification of the raw water of numerous lakes containing high phytoplankton populations and elevated pH.

Relative Microalgal Concentration in Prydz Bay, East Antarctica during Late Austral Summer, 2006

  • Mohan, Rahul;Shukla, Sunil Kumar;Anilkumar, N.;Sudhakar, M.;Prakash, Satya;Ramesh, R.
    • ALGAE
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    • 제24권3호
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    • pp.139-147
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    • 2009
  • Microalgae using a submersible fluorescence probe in water column (up to 100 m) were measured during the austral summer of 2006 (February) in Prydz Bay, East Antarctica (triangular-shaped embayment in the Indian sector of Southern Ocean). Concurrently, environmental parameters such as temperature, salinity and nitrogen (nitrate, ammonium, urea) uptake rates were measured. The concentration of phytoplankton is relatively high due to availability of high nutrients and low sea surface temperature. Phytoplankton community is dominated by diatoms whereas cryptophytes are in low concentration. The maximum concentration of total chlorophyll is 14.87 ${\mu}g\;L^{-1}$ and is attributed to upwelled subsurface winter water due to local wind forcing, availability of micro-nutrients and increased attenuation of photosynthetically available radiation (PAR). Concentration of blue-green algae is low compared to that of green algae because of low temperature. Comparatively high concentration of yellow substances is due to the influence of Antarctic melt-water whereas cryptophytes are low due to high salinity and mixed water column. Varied concentrations of phytoplankton at different times of Fluoroprobe measurements suggest that the coastal waters of Prydz Bay are influenced by changing sub-surface water temperature and salinity due to subsurface upwelling induced by local winds as also melting/freezing processes in late summer. The productivity is high in coastal water due to the input of macro as well as micro-nutrients.