• 제목/요약/키워드: Phytoplankton Community

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통영 양식장 해역의 식물플랑크톤 군집의 연간변동 (Inter-annual Variation of Phytoplankton Community Structure in Aquacultural Areas of Tongyeong, SE Coastal Waters of Korea)

  • 임월애;이영식;강영실;김성수;김성연;최혜승;허영백;이태식;이재영
    • 한국해양학회지:바다
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    • 제15권4호
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    • pp.158-165
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    • 2010
  • 식물플랑크톤 군집은 그 해역의 환경특성을 잘 설명해 줄 수 있는 인자 중의 하나이다. 본 연구에서는 양식장 해역의 수질환경과 식물플랑크톤 군집의 년간 변동을 파악하고, 이를 기초로 해역별 환경 특성을 파악하고자 하였다. 2009년 1월에서 12월까지 매월 통영연안인 원문만, 한산만, 미륵도, 욕지도, 사량도 및 도산 평림해역의 30개 정점에서 식물플랑크톤 종조성과 수온, 염분, 영양염 및 chlorophyll a를 조사하였다. 수질환경 중 용존무기질소는 1, 2월과 12월, 용존무기인은 1, 2월, chl-a는 7월~10월이 가장 높았다. 식물플랑크톤 군집은 Chaetoceros spp.와 미동정된 소형 편모조류는 연중 우점하였고, 여름인 6~10월은 Pseudo-nitzschia spp., Dictyocha spp., Nitzschia longissima가 우점종으로 출현하였으며 그 밖의 계절은 Skeletonema costatum, Thalassiosira spp., Eucamphia zodiacus, Akashiwo sanguinea, Gymnodinium spp., Asterionella japonicus가 우점 출현하였다. 정점별로는 한산만, 사량도 북동쪽에서 외편모조 적조가 3회 발생하였으며, chl-a는 한산만에서 가장 높게 나타났다. 종다양성 지수는 원문만, 한산만과 도산평림해역에서 낮게 나타났고, 규조류와 외편모조류의 비율은 미륙도 서측해역에서 높았다. 우점식물플랑크톤의 출현은 각 해역의 시 공간적 특성을 나타내었으며, 최근 수온상승과 강우에 의한 식물플랑크톤 군집 변동도 예측되었다.

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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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.

다변량 통계분석을 이용한 북한강의 수질 및 식물플랑크톤 군집 특성 평가 (Evaluation of Water Quality and Phytoplankton Community Using a Multivariate Analysis in Bukhan River)

  • 김헌년;윤석제;변명섭;유순주;임종권
    • 한국물환경학회지
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    • 제35권1호
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    • pp.19-27
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    • 2019
  • The purpose of this study is to evaluate the water quality and phytoplankton community in Bukhan River which account for 44.4 % of the total inflow into Lake Paldang, using multivariate statistical techniques (i.e., correlation analysis, principal component analysis (PCA)/factor analysis (FA)). Water samples were collected from March to November 2015 and the following parameters measured; water temperature, pH, DO, EC, SS, BOD, Chl-a, COD, TN, $NO_3-N$, $NH_3-N$, TP, DTP, $PO_4-P$, and phytoplankton community. The water quality of the main stream and the tributaries were not significantly different apart from the relatively high concentration of BOD, COD and nutrients recorded in MH. The highest cell density of Stephanodiscus hantzschii and Merismopedia glauca dominated phytoplankton was observed in PD. Based on the correlation analysis, total phytoplankton and cyanophyceae were highly correlated with BOD, COD and nutrients. PCA/FA resulted in four main factors accounting for 82.240 % of the total variance in the water quality dataset. The group of component 1 (TN, DTN, DO, $NO_3-N$, water temperature) and component 2 ($PO_4-P$, T-P, DTP, SS) were classified as nutrient element factor whereas component 3 (Chl-a, COD, BOD, $NH_3-N$, pH) was related to organic substances. Hence, the identification of the main potential environmental pollution factors in Bukhan River will help policy makers make better and more informed decisions on how to improve the water quality.

Grazing Rates of Rotifers and Their Contribution to Community Grazing in the Nakdong River

  • Kim, Hyun-Woo;Hwang, Soon-Jin;Joo, Gea-Jae
    • The Korean Journal of Ecology
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    • 제22권6호
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    • pp.337-342
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    • 1999
  • Rotifer grazing rates in both species and community levels on bacteria and phytoplankton were determined by using representative models (fluorescent beads: 0.75$\mu m$ for bacteria and 10 $\mu m$ for phytoplankton) at biweekly intervals. One-year study at the lower part of the Nakdong River (Mulgum) indicated that the seasonal pattern of rotifer biomass was similar to that of total zooplankton biomass. Total mean biomass of rotifers was significantly higher than that of other groups (rotifers, 148$\pm $327 $\mu g$C/l; cladoceran. 25$\pm 69$$\mu g$C/l; copepodids. 58$\pm 159$$\mu g$C/l). For laboratory grazing experiments. mean specific filtering rate (SFR: $ml\cdot \; l^{-1}\cdot \; day^{-1}$) for rotifers varied from 0.001 to 0.726, and > 90% individuals of rotifer species took up fluorescent microspheres. The high SFRs were achieved by Brachionus angularis, B. calyciflorus, and Filinia longiseta. Community filtering rates (CFRs, $ml\cdot \; l^{-1}\cdot \; day^{-1}$) varied in the range from 2 ~ 1,670. Rotifer filtering rates on phytoplankton were much higher than bacterial filtering rates, especially in the late growing season (May. June, and November). Rotifers appear to be important in transferring both bacterial and phytoplankton carbon to higher trophic levels at the lower Nakdong River.

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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.

회야강(울산)의 식물플랑크톤 군집구조 (The Structure of Phytoplankton Community in the Hoeya River (Ulsan))

  • 최철만;배진현
    • 한국환경과학회지
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    • 제11권3호
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    • pp.149-154
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    • 2002
  • This study was conducted to find the structure of phytoplankton community in the Hoeya river(Ulsan) from March 2000 to February 2001. The taxa of phytoplankton identified included 135 species, 5 divisions, 33 families and 82 genera. Among them, chrysophyta(diatoms) were 63 species(46.7%), chlorophyta(green algae) 47 species(34.8%), pyrrophyta(dinoflagellates) 13 species(9.6%), cyanophyta (cyanobacteria) 8 species(5.9%) and euglenophyta(euglenoids) 4 species(3.0%) respectively. Ecological important species is called frequently appearing species, red tide causative species, seawater species and pollution indicator. 22 species including Aulacoseira granulate were recorded frequently appearing species. 19 species including Ceratium furca were recorded as red tide causing species. And the pollution indicators were 33 species including Actinastrum hantzschii var. fluviatile. The highest standing crops were 3,103,441 cells/$\ell$ in August at the RW-1 and the lowest 1,245 cells/ $\ell$ in January at the RW-5. In the community analysis, the dominanance indices ranged from 0.34(October, RW-2) to 0.94(January, RW-1) and the diversity indices from 0.50(May, RW-2) to 2.57(September, RW-2). The saprobic indices were 2.43 in RW-1, 2.41 in RW-2, 2.375 in RW-3, 2.40 in RW-4, 2.43, in RW-5. Therefore, these areas were investigated "$\beta$-mesosaprobic". According to the similarity index among the stations, these areas were defined as residential district areas(RW-2 and RW-3), lower part of the dam (RW-1) and seawater areas(RW-4 and RW-5).

질산염 첨가에 따른 중형폐쇄생태계 내 플랑크톤 군집의 변화 (The Effect of Enhanced Nitrate Input on the Temporal Variation of the Plankton Community in a Mesocosm)

  • 강정훈;김웅서;신경순;장만;황근춘
    • Ocean and Polar Research
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    • 제27권3호
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    • pp.341-349
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    • 2005
  • Temporal variation of the natural planktonic community in the Southern Sea of Korea was investigated by using low floating enclosed bags (3.2m deep and 2,500 liter) in order to understand the effect of enriched nitrate on the planktonic community in the spring (March-April) of 2002. Prior to beginning the incubation, the bags were placed in two different concentrations of nitrate, which consisted of control (ambient water) and experimental mesocosms (final concentration of $12{\mu}M$). The nitrate concentration in the experimental mesocosms remained significantly higher than those in control mesocosms throughout the study period (ANOYA, p<0.001). Following the addition of nitrate, abundance and chi-a concentration of phytoplankton peaked on Day 1, when diatoms established the peak in the experimental mesocosms. Diatoms consisted mainly of Thalasxiosira decipiens, Pseudo-nitzschia pungem, Leptocylindrus danicu, Thalassionema nitzschioides, Chaetoceros pseudocrinitus and Actinoptychus senariu. However, the peak did not lead to the difference in abundance and composition of phytoplankton between control and experimental mesocosms during the study period. The dinoflagellates began to increase soon after the diatoms decreased in all mesocosms. Copepods, as a dominant group in the rnosozooplankton community, showed no immediate peak in relation to the nitrate addition, but only their own developmental process from the eggs to adult stage during the study period. The bottom-up control from enriched nitrate via phytoplankton to adult copepods was not distinguished in terms of the abundance of the planktonic community. This might stem from the relatively low nitrate availability of phytoplankton at no N-limited seawater and the weak coupling between rapidly sunken diatoms and copepods through the water column.

가압부상 후 잔류 응집제가 플랑크톤 군집에 미치는 영향 (The Effects of Residual Al on Plankton Community after Dissolved Air Flotation (DAF) Application)

  • 김호섭;공동수;이형진;신종규;강태구
    • 한국물환경학회지
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    • 제23권6호
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    • pp.837-842
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    • 2007
  • This study was conducted to test the effect of residual Al on plankton community after dissolved air flotation (DAF) application. Growth rate of phytoplankton after DAF application ($0.37day^{-1}$) was about 2 times lower than that before DAF application ($0.70day^{-1}$). Under the condition of addition of nitrogen and phosphorus without light, growth rate phytoplankton in treatment without residual Al increased in difference with showing the negative growth rate in treatment with residual Al. Under the condition of light without addition of nutrient, growth rate of phytoplankton was no noticeable difference between the before and after DAF application. The relatively high settling rate (0.47 m/day) was observed in treatment after DAF application. Although the abundance of rotifer decreased, the abundance of copepod and cladoceran such as Daphnia galeata, Diaphanosoma sp. and Bosmina longirostris with relative higher grazing was no noticeable difference between the before and after DAF application. In the treatments before and after DAF application with zooplankton, growth rate of phytoplankton was $0.41{\pm}0.08day^{-1}$, $0.20{\pm}0.03day^{-1}$, respectively. This difference was in treatment after DAF application similar with those in treatments before and after DAF application without zooplankton. Those indicate that the filter-feeding effect of zooplankton on phytoplankton community may be not changed by residual Al after the DAF application. These results suggest that residual Al after DAF application be to improve water quality by inhibition of growth rate as well as increasing settling rate of phytoplankton.

서해 남부, 고창연안해역의 해양환경 및 식물플랑크톤 군집의 시·공간 변동특성 (Spatio-temporal Variations of Marine Environments and Phytoplankton Community in the Gochang Coastal Waters (GCW) of Southern West Sea in Korea)

  • 윤양호
    • 한국산학기술학회논문지
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    • 제21권11호
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    • pp.477-493
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    • 2020
  • 고창 연안해역의 해양환경 및 식물플랑크톤 군집의 시·공간적 변동 특성을 파악하기 위해 2016년 여름에서 2017년 봄까지 4계절 16개 정점을 조사하였다. 분석 결과, 수온은 표층에서 2.1℃에서 34.5℃의 범위로 큰 계절 변화를 보였지만, 염분은 표층에서 31.14 psu에서 32.64 psu의 범위로, 계절 변화가 크지 않아, 연안해역 수형은 수온에 지배되었다. Chl-a 역시 봄 최솟값 0.58 ㎍ L-1에서 여름 최댓값 10.5 ㎍L-1의 범위로 겨울에 높고, 가을과 봄에 낮았고, 큰 계절 변화를 보였다. 식물플랑크톤 군집은 53속 86종으로 단순하였다. 표층 현존량은 가을 최솟값 2.2 cells mL-1에서 여름 최댓값 689.2 cells mL-1의 변화 폭으로 여름에 높고, 가을에 낮았으나, 가을은 다른 계절보다 한 자릿수가 이상 낮았다. 우점종은 연중 규조류에 지배되어, 표층은 여름이 Leptocylindrus danicus, Chaetoceros curvisetus Skeletonema costatum-ls, 가을은 Paralia sulcata, Eucampia zodiacus, 겨울은 S. costatum-ls, Thalasiosira nordenskioeldii, 그리고 봄은 S. costatum-ls, Asterionella glacialis가 우점하였다. 즉 고창 연안해역의 식물플랑크톤 군집은 다양성이 높지만, 연중 특정 종에 크게 지배되는 군집구조를 나타내었다. 주성분 분석 결과 고창 연안해역은 낮은 수심으로 복사열에 의해 쉽게 가열 및 냉각되며, 조석혼합 등 해수 혼합 특성으로 표층퇴적물의 재부유에 의한 영양염 공급으로 식물플랑크톤 시·공간 분포가 결정되었다.