• 제목/요약/키워드: Phytoplankton community structure

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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.

현미경, Flow Cytometer, HPLC 색소자료 및 원격탐사를 이용한 이어도 관측기지 주변수의 식물플랑크톤 연구 (Phytoplankton in the Waters of the Ieodo Ocean Research Station Determined by Microscopy, Flow Cytometry, HPLC Pigment Data and Remote Sensing)

  • 노재훈;유신재;이정아;김현철;이재학
    • Ocean and Polar Research
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    • 제27권4호
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    • pp.397-417
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    • 2005
  • Phytoplankton community structure and distribution pattern in the surface water around the Ieodo Ocean Research Station were investigated during seven cruises carried out from July, 2003 to October, 2004. Samples were analyzed using various tools including a microscope, flow cytometer, and HPLC. Satellite images were used to analyze spatio-temporal phytoplankton biomass distribution. SeaWiFS chlorophyll a (chl a) images showed that spring blooms occurred in April-May near the Ieodo Station, and these waters were under the influence of Changjiang Dilute Water during July-October. Also, during the July-October period, HPLC pigments data showed increasing zeaxanthin concentrations, a marker pigment of cyanobacteria whereas increasing concentrations of various other pigments such as fucoxanthin, peridinin, prasinoxanthia alloxanthin, 19'-hexanoyloxyfucoxanthin and chlorophyll b were noted during spring blooms. Such pigment marker data were consistent with picoplankton data analyzed by flow cytometer and nano-microplankton analyzed by microscope. The pigment-CHEMTAX method was used to drive the phytoplankton group apportioned chi a. Diatoms, chlorophytes, dinoflagellates, and cryptophytes comprised 25.8, 20.7, 15.9, and 14.1%, respectively, of the total chl a in May. Average cyanobacteria concentrations in July-October contributed 25.4% of the total concentration. This was the highest percent contribution and was followed by chlorophytes, diatoms, and prymnesiophytes. This study discusses results from various methods, similarities and differences in the results among those methods, and the application range of the results from different analytical methods. Also, the study reveals a detailed phytolpankton community structure in the waters around the Ieodo Station, and suggests future monitoring considerations in relation to cell morphology, ecology and diversity factors according to taxonomic groups.

의암호의 식물성 Plankton 군집의 구조와 동태 (Structure and Dynamics of Phytoplankton Commnities in Uiam Lake, Korea)

  • Yim, Yang-Jai;Kyu Song Cho;Chang Nam Sin
    • The Korean Journal of Ecology
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    • 제5권2_3호
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    • pp.132-135
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    • 1982
  • Structure and dynamics of the phytoplankton communities of Uiam lake, Korea, was investigated. In the Uiam lake four dominant species were found Oscillatoria limosa at Chuncheon City side, O. tenuis at Soyang river side, Melosira italica at south-east side and Asterionella gracillima at west side of the lake. By cluster analysis, based on the similarity index and dissimilarity index, the phytoplanktons in this lake were grouped into three communities; i.e. Oscillatoria, Melosira and Asterionella community. And also the same groups obtained by the cluster analysis were recognized by polar ordination technique along polluted degree gradient. It is clear that oscillatoria community occur in polluted site, Asterionella community in unpolluted site and Melosira community in less polluted site.

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HPLC를 이용한 광합성색소 분석과 CHEMTAX 프로그램을 이용한 식물플랑크톤 군집조성 연구 (Application of Photosynthetic Pigment Analysis Using a HPLC and CHEMTAX Program to Studies of Phytoplankton Community Composition)

  • 이용우;박미옥;김윤숙;김성수;강창근
    • 한국해양학회지:바다
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    • 제16권3호
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    • pp.117-124
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    • 2011
  • High-Performance Liquid Chromatograph(HPLC)를 이용하여 식물플랑크톤의 광합성색소를 분석한 결과를 토대로 CHEMTAX 프로그램을 이용하여 식물플랑크톤 군집조성을 추정하는 방법이 많이 이용되고 있다. CHEMTAX 프로그램은 식물플랑크톤 군집별(class level)로 체내에 존재하는 주요색소의 chlorophyll a에 대한 상대적인 비 값을 기초로 분석을 한다 본 연구는 국내 해역에서 분리한 식물플랑크톤 군집별 주요 종들이 가지는 광합성색소의 상대적인 비 값을 파악하고 이 자료를 기초로 남해안에 위치한 여자만과 가막만에서 측정한 광합성색소 분석결과에 대해서 CHEMTAX 프로그램을 이용하여 식물플랑크톤의 군집조성을 파악하였다. 국내해역에 존재하는 같은 군집종들 사이에서도 주요색소의 상대적인 비 값은 차이를 보였으며, 국외의 다른 해역에서 제시된 상대적인 비 값과도 상당한 차이를 보였다. 본 연구에서 얻은 비 값을 기초로 식물플랑크톤 군집조성을 분석한 결과, 다른 해역에서 제시된 비 값을 이용하여 분석한 결과와 유의한 차이를 보였다. 우점하는 군집(bacillariophyceae와 dinophytes)에 대해서는 5% 이내에서 차이를 보였으며, 비록 chlorophyll a에 대해서 낮은 기여도를 보이지만 pico와 nano 크기의 군집들(cyanophytes와 prasinophytes)에서는 상당한 차이(2배 이상)를 보였다. 비록 HPLC-CHEMTAX 분석방법은 식물플랑크톤 군집조성 연구에 유용하게 이용되고 있지만, 보다 정확한 결과와 식물플랑크톤의 생리, 생태를 이해하기 위해서는 연구해역에 존재하는 식물플랑크톤 종들에 대한 주요색소의 상대적인 비 값에 대한 연구가 계속적으로 진행되어야 할 것으로 판단된다.

Ecological Studies on Togyo Reservoir in Chulwon, Korea VI. The List of Phytoplankton and Periphyton

  • Lee, Kyung;Yoon, Sook-Kyung
    • ALGAE
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    • 제18권4호
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    • pp.263-272
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    • 2003
  • The composition of phytoplankton and periphyton community in Togyo reservoir was investigated. A total of phytoplankton was composed of 150 taxa, belonging to 6 phyla, 8 classes, 15 orders, 5 suborders, 31 families, 71 genera, 106 species, 14 varieties, 1 form and 29 unidentified species. The observed number of diatoms and green algae were much higher than others. Within diatoms the pennate diatoms appeared more than centric diatoms and solitary forms or colonial forms appeared more than filamentous forms in green algae. A total of epipelic algae was composed of 125 taxa, belonging to 3 phyla, 3 classes, 6 orders, 3 suborders, 13 families, 30 genera, 87 species, 29 varieties, 2 forms and 7 unidentified species. The diatoms appeared much more than others. Among those, the pennate diatoms dominated the centric diatoms in species number observed. A total of epilithic algae was composed of 114 taxa, belonging to 4 phyla, 4 classes, 11 orders, 3 suborders, 22 families, 38 genera, 79 species, 8 varieties, 1 form and 26 unidentified species. The observed number of diatoms and green algae were much higher than others. Within diatoms the pennate diatoms dominated the centric diatoms in species number observed. The dominance of pennate diatoms of the diatom community in the epipelic algal community and the epilithic algal community could be assumed that was due to the presence of raphe structure of pennate diatoms.

장목만에서 여름철 영양염 특성 변화가 식물플랑크톤 군집구조에 미치는 영향 (Effects of Nutrient Property Changes on Summer Phytoplankton Community Structure of Jangmok Bay)

  • 장풍국;장민철;이우진;신경순
    • Ocean and Polar Research
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    • 제32권2호
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    • pp.97-111
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    • 2010
  • Phytoplankton production is affected by various physico-chemical factors of environment. However, one of the most critical factors generally accepted as controlling primary production of phytoplankton is nutrients. It has recently been found that the succession of phytoplankton groups and species are closely related to the chemical properties of ambient water including nutrient limitation and their ratios. In Jangmok Bay, silicate and nitrate are primarily supplied by rainfall, while phosphate and ammonia are supplied by wind stress. Typhoons are associated with rainfall and strong wind stress, and when typhoons pass through the South Sea, such events may induce phytoplankton blooms. When nutrients were supplied by heavy rainfalls during the rainy season and by summer typhoons in Jangmok Bay, the dominant taxa among the phytoplankton groups were found to change successively with time. The dominant taxon was changed from diatoms to flagellates immediately after the episodic seasonal events, but returned to diatoms within 3~10 days. Pseudo-nitzschia spp. were dominant mainly in the presence of low phosphate levels during the first of the survey which included the rainy season, while Skeletonema costatum was dominant when phosphate concentrations were high due to the strong wind stress during the latter half of the survey as a result of the typhoon. The competition between S. costatum and Chaetoceros spp. appeared to be regulated by the silicate concentration. S. costatum preferred high silicate and phosphate concentrations; however, Chaetoceros spp. were able to endure low silicate concentrations. These results implied that, in coastal ecosystems, the input patterns of each nutrient supplied by rainfall and/or wind stress appeared to contribute to the summer succession of phytoplankton groups and species.

진해만에서 물리화학적 환경요인이 식물플랑크톤 색소 및 군집조성의 시공간적 변화에 미치는 영향 (Effects of Physicochemical and Environmental Factors on Spatial and Temporal Variations in Phytoplankton Pigment and its Community Composition in Jinhae Bay)

  • 나수진;이지영;김정배;구준호;이가람;황현진
    • 해양환경안전학회지
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    • 제27권2호
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    • pp.340-354
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    • 2021
  • 본 연구에서는 ultra performance liquid chromatography(UPLC)를 이용하여 진해만의 식물플랑크톤 생체량 및 군집구조의 시공간적 분포에 미치는 환경요인의 영향을 조사하였다. 이를 위해 2019년 4월에서 12월까지 총 5회에 걸쳐 7개 정점에 대한 식물플랑크톤 색소분석과 수온, 염분, 용존산소(DO), 영양염(DIN, DIP, Si(OH)4) 등의 환경요인 분석을 행하였다. 조사기간 중 식물플랑크톤의 생체량(Chl-a)은 7월(평균 15.4±4.3 ㎍/L)에 가장 높았고, 12월(평균 3.5±0.6 ㎍/L)에 가장 낮았다. 보조색소의 경우 fucoxanthin이 가장 많이 검출되었고 그 다음으로 peridinin, Chl-b 순으로 나타났으며, 이들의 월 변동은 Chl-a와 유사한 경향을 보였다. 식물플랑크톤 군집분석결과, 규조류가 평균 70 %로 가장 우점하였으나, 일부 녹조류, 은편모조류, 와편모조류가 출현하기도 하였다. 우점종인 규조류는 특히 수온 및 N:P ratio와 밀접하게 연관되어 있어서 여름철 고온환경 및 육상으로부터의 영양염 유입에 민감하게 반응하는 것으로 추론되었다. 또한 식물플랑크톤 색소 및 종조성은 전반적으로 계절에 따른 물리화학적 환경요인의 변화 및 지형적 특성과 연관되어 있으며 강우로 인한 담수 및 영양염 공급에 큰 영향을 받는 것으로 추정되었다.

동중국해 식물플랑크톤 군집의 공간분포와 와편모조류 적조 (Spatial Distribution of Phytoplankton Community and Red Tide of Dinoflagellate, Prorocentrum donghaience in the East China Sea during Early Summer)

  • 윤양호;박종식;서호영;황두진
    • 환경생물
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    • 제21권2호
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    • pp.132-141
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    • 2003
  • We carried out a study on thermohaline structure and phytoplankton com munity in the East China Sea during early summer in 2005. As a result of marine environment and phytoplankton community, three characteristics of water type were identified. The former was characterized by the dominant species with diatoms, Chaetoceros lacinious, Ch. decipiens, Guninardia flaccida, Paralia sulcata, Pseudonitzschia pungens and Pseudosolenia calcar-avis in Chinese coastal waters, the secondary was done by lower water temperature, salinity and the dominant species with dinoflagellates, Prorocentrum donghaiense and Ceratium fusus, in over-all areas and the latter was done by the dominant species with coastal species of diatoms, Skeletonema costafum and Nitzschia longissima and silicoflagellate, Dictyocha speculum var. octopers in the transfer areas of Chinese continental coastal waters. Phytoplankton community in the surface layer identified a total of 66 species belonging to 36 genera. Dominant species was Prorocentrum donghaiense, Chaetoceros lacinious, Skeletonema costatum. Standing crops of phytoplankton in the surface layer flue tuated between $1.5 \times 10^4$cells $L^{-1}$ and $3.5\times 10^{5}$ cells $L^{-1}$. And the highest value appeared in the Changjiang estuaries with high dominance by diatoms and lowest one occurred in the southwestern area of Jeju Island with high dominance by dinoflagellates. Red tides with dinoflagellate, Prororcentrum donghaiense appeared in the frontal areas with mazimum cell density, $3.4\times 10^5$ cells $L^{-1}$. And outbreak environments was low water temperature under $20^{\circ}C$, and low salinity under 31.55 psu. The vertical distribution of red tide organisms went to about 30m depth from surface.

영광 안마군도 주변 해역 식물플랑크톤 군집의 계절 동태 (Seasonal dynamics of phytoplankton community in the Anma Islands of Yeonggwang(AIY), West Sea, Korea)

  • 주하연;송아영;박지혜;윤양호
    • 환경생물
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    • 제40권1호
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    • pp.70-86
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    • 2022
  • 서해 남부 안마군도 주변 해역 식물플랑크톤 군집의 계절 동태를 파악하기 위하여 2020년 봄부터 2021년 겨울까지 소형 해양조사선 에드오션호를 이용하여 21개 정점의 표층과 저층 해수를 대상으로 현장조사를 하였다. 결과, 출현한 식물플랑크톤 종은 52속 87종으로, 규조류가 67.8%, 와편모조류가 26.5%, 규질편모조류가 3.5%, 그리고 은편모조류 및 유글레나조류가 각 1.1%를 차지하였다. 계절별로 출현 종은 봄에 단순하였고, 겨울에 상대적으로 다양하였다. 표층 현존량은 여름 28.8±30.1 cells mL-1로 낮았고, 봄 87.0±65.1 cells mL-1로 높았다. 식물플랑크톤 군집은 연중 규조류가 80% 이상 높은 점유율을 나타내었고, 우점종은 Skeletonema costatum-ls가 봄과 겨울에 60% 이상 극우점을 보였고, 여름과 가을 각 34.6%와 24.2%로 최우점하였다. 군집구조 특성을 나타내는 다양도 지수는 현존량과 다르게 가을에 2.79±0.45로 높았고, 봄에 1.82±0.18로 낮았다. 그러나 우점도 지수는 봄에 0.86±0.08로 높았고, 가을에 0.44±0.13로 낮았다. 환경인자 및 식물플랑크톤 군집 관련 인자를 이용한 주성분 분석 결과, 식물플랑크톤 군집을 통해 본 안마군도 주변 해역의 생물해양학적 환경 특성은 상대적 개방해역 및 조석 혼합 등 해수 혼합에 의한 해저 퇴적층에서 공급되는 영양염 등에 의해 지배되는 것으로 추정되었다.

영산강 수계의 수질과 식물플랑크톤의 계절적 변화 (Seasonal Change of Phytoplankton Community and Water Quality in Yeongsan River Watershed)

  • 손미선;박종환;임채홍;김세경;임병진
    • 환경생물
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    • 제31권2호
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    • pp.105-112
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    • 2013
  • 본 연구는 2010년 4월부터 2011년 12월까지 영산강수계의 4개의 지점을 선정하여 수질과 일차생산량을 나타내는 식물플랑크톤의 현존량과의 관계를 규명하기 위하여 물리 화학적 환경요인 (수온, 용존산소량, pH, 총질소, 총인, 부유물질), 식물플랑크톤의 현존량, Chlorophylla의 농도를 조사하였다. 조사기간 동안 식물플랑크톤의 종 조성은 규조강 43종, 녹조강 93종, 남조강 16종, 기타 강 22종으로 총 174종으로 조사되었다. 식물플랑크톤의 개체군 밀도는 $275cells{\cdot}mL^{-1}{\sim}58,600cells{\cdot}mL^{-1}$으로 조사되었다. 봄철과 가을철에는 Cyclotella sp., Stephanodiscus sp.와 같은 규조강, 여름철에는 Scenedesmus quadricauda, Pediastrum biwae 및 Coelastrum sp.와 같은 녹조강과 Aulacoseira granulata와 같은 규조강이 우점하였으며, 가을과 겨울에는 Cyclotella sp., Stephanodiscus sp.와 같은 규조강과 Aphanizomenon sp., Oscillatoria sp.와 같은 남조강이 우점하는 것으로 조사되었다. Chlorophyll-a의 농도는 식물플랑크톤 현존량의 월별 변동과 대부분 같은 경향으로 변화하였다.