• ALGAE
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• 제22권4호
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• pp.261-271
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• 2007

The variations of species compositions, standing crops and seasonal succession of phytoplanktons including Cyanophyceae, Chlorophyceae and Bacillariophyceae were investigated with physico-chemical elements of water to clarify the causes of water bloom according to the water depth in the Lake Unmun. The increased amounts of turbidity, T-N, T-P and SS originated from heavy rain and typhoon in the middle of June provoked to produce phytoplanktons. In July and August, the dominant species was Peridinium sp., while the subdominant species was Microcystis aeruginosa. In October, Aulacoseira distans was dominant and Asterionella formosa was subdominant. During the period of water shortage, the concentrated pollutants caused the decrease of precipitation, the long stagnation time of water body and the mixed pollutants by upwelling as decreasing water temperature could accelerate the water bloom. The preventives to decrease microalgal generation should be controled by the stagnation time of water body by increasing outflow to intercept water bloom such as ulacoseira sp. in October as well as summer.

• Fisheries and Aquatic Sciences
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• 제2권2호
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• pp.210-217
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• 1999

Chemical oxygen demand (COD), phytoplankton cell number and chlorophyll-a concentration (Chl-a), sediment mean grain size and ignition loss were studied to determine their temporal trends in the study area. Historical data of COD, cell number and Chl-a were gathered from the late 1960s or early 1980s to 1997, and trends in temporal domain were obtained from a simple regression. Sediments for grain size and ignition loss (as organic contents in sediments) were sampled from the Chokchon macrotidal flat bimonthly from September 1990 to November 1996, and were analyzed using the decomposition method of time series analysis. In general, the first three data showed increasing trends based on regression analysis. The trends of sediment grain size fluctuated in a neutral pathway while those of ignition loss yielded no increasing pattern. In contrast with the suggestions from Ahn and Choi (1998) who reported a coarsening variation in sediment grain size to be a cause of the directional and remarkable changes of macrofaunal communities in this area, we could not find such a corresponding variation pattern from our samples. In diagnosing eutrophication, a paradoxical phenomenon was encountered between the trends in water column (COD, cell number and Chl-a) and sediment (ignition loss) data. In this paper, we inferred the possible processes that produce the discrepancy. Some explanations and biological responses to eutrophication were predicted and discussed.

• Fisheries and Aquatic Sciences
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• 제1권2호
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• pp.250-254
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• 1998

Harmful micro algae isolated from Korean coastal waters, were tested with FITC-conjugated lectins and observed by epifluorescent microscopy to distinguish each other. Strain-specific sugar composition at the cell surface was suggested by the affinity of lectins to different microalgae. The micro algae Cochlodinium polykrikoides (CP-1) and Gymnodinium $A_3\;(GA_{3-1}\;1)$, are morphologically similar, but exhibited different binding activity with the lectins ECA, HPA and WGA. In Peridiniales, the micro alga Alexandrium tamarense (AT) bound HPA and WGA, but Scrippsiella trochoidea (ST-1) did not bind those lectins. Three species of Prorocentrum also exhibited different binding specificity with HPA, PHA and SBA. A non­toxic Korean isolate of Heterosigma akashiwo (HA-2) bound ConA, PEA and UEA. These results suggest that lectins are useful in discriminating morphologically similar species, as well as different species or strains within the same genus.

• 한국지구과학회지
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• 제42권4호
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• pp.390-400
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• 2021

Ocean biogeochemistry plays a crucial role in sustaining the marine ecosystem and global carbon cycle. To investigate the oceanic biogeochemical responses to iron parameters in the tropical Pacific, we conducted sensitivity experiments using the Nucleus for European Modelling of the Ocean-Tracers of Ocean Phytoplankton with Allometric Zooplankton (NEMO-TOPAZ) model. Compared to observations, the NEMO-TOPAZ model overestimated the concentrations of chlorophyll and dissolved iron (DFe). The sensitivity tests showed that with increasing (+50%) iron scavenging rates, chlorophyll concentrations in the tropical Pacific were reduced by approximately 16%. The bias in DFe also decreased by approximately 7%; however, the sea surface temperature was not affected. As such, these results can facilitate the development of the model tuning strategy to improve ocean biogeochemical performance using the NEMO-TOPAZ model.

• 환경생물
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• 제22권
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• pp.86-92
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• 2004

광양만내 평균 해양 바이러스 양은 2.0${\times}$$10^{8}$ particles ml$^{-1}$로 매우 풍부했다. 각 계절별 바이러스의 밀도는 여름에 최대 9.0${\times}$$10^{8}$ particles ml$^{-1}$, 겨울에는 최소인 0.7${\times}$$10^{6}$ particles ml$^{-1}$을 기록했다. 광양만내의 바이러스, 박테리아, 식물플랑크톤 생물량의 공간적 분포는 외만 해역에 해당하는 정점 28, 38, 42, 46, 51에서 보다 내만 해역에 해당하는 정점 2, 5, 10, 12, 16, 20에서 많은 것으로 나타났다. 또한 내만 해역에 해당하는 정점 22, 26, 32, 34는 높은 바이러스 밀도를 보였지만 상대적으로 외만 해역에 비해서 낮은 박테리아와 식물플랑크톤의 생물량을 나타냈다. 몇몇 정점의 수심 깊이에서는 박테리아의 밀도가 바이러스의 밀도를 100배 정도 초과했다. 해양 바이러스와 그들의 숙주 생물의 밀도는 계절에 따라 변화했으며, 그들의 계절별 변화는 서로 밀접한 상호연관성을 가졌다. 여름에 바이러스와 박테리아의 밀도는 증가된 반면 식물플랑크톤의 엽록소 $\alpha$ 농도는 평균값을 유지하였다. 겨울에는 바이러스와 박테리아의 밀도가 급속하게 줄어들었고, 마찬가지로 엽록소 $\alpha$의 농도 역시 감소하다가, 곧 다시 증가했다. 바이러스의 밀도는 2001년 8월에 최고점에 도달했으며, 박테리아의 밀도는 2001년 8월과 2002년 6월에 최고값을 가졌다. 반면에 엽록소 $\alpha$의 농도는 2002년 4월에 최대치에 도달했다. 전체 숙주와 바이러스 밀도로 볼 때, 그들의 먹이사슬은 바이러스에 의한 사멸에 의해서 평형 상태로 유지되고, 바이러스의 밀도 또한 평형 상태를 유지하는 것으로 보였다. 이러한 시도는 우리나라 광양만 내에 존재하는 해양 바이러스의 생태적 분포 연구를 다루는 첫 번째 실험으로 사료된다.

• 한국해양환경ㆍ에너지학회지
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• 제9권4호
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• pp.203-215
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• 2006

'한국 남해 중앙부 해역의 표층퇴적물내 유기물의 시 공간적 분포특성을 파악하고자 2002년 4월부터 2003년 1월까지 15개 정점을 대상으로 격월간격으로 현장조사를 실시하였다. 저층해수(B-1m) 수온과 염분 그리고 표층퇴적물의 니질 함량과 함수율은 각각 $8.1{\sim}23.4^{\circ}C,\;29.2{\sim}34.5\;psu,\;71.2{\sim}99.9%$ 및 $38.7{\sim}68.9%$의 범위를 보였다. 강열감량(IL), 식물색소량(phaeopigment), 입자성 유기탄소(POC), 입자성 유기질소(PON) 및 화학적산소요구량(CODs)은 각각 $3.9{\sim}12.5%,\;1.58{\sim}29.51\;{\mu}g/g-dry,\;3.12{\sim}13.01\;mgC/g-dry,\;0.49{\sim}2.0\;mgN/g-dry$ 그리고 $9.6{\sim}44.05\;mgO_2/g-dry$의 범위를 보였다. 유기물의 공간적인 분포는 육지와 인접한 연안역보다 수심이 깊은 외양역에서 높은 유기물량을 나타내었다. 시간적으로는 저수온기보다 고수온기에 유기물량이 증가하였다. 유기물 기원은 C/N ratio가 평균 6.44(${\pm}0.51$)로 나타나 해양자체 생산에 의한 생물기원 유기물에 게 의존하고 있으나, 비교적 높은 POC/phaeopigment ratio로 부터 전체적으로 식물플랑크톤보다 쇄설성 유기물질에 의한 조성비가 높음을 알 수 있었다. 주성분분석 결과 누적 기여율 73.2%의 제 2주성분까지 도출되었다. 얻어진 인자부하량으로부터 제 1주성분은 '환경요인에 따른 표층퇴적물의 유기물 집적정도(57.3%)'를, 제 2주성분은 '해양의 생유기물에 의한 유기물 척도(15.9%)'로 판단되었다. 정점별 득점 분포로부터 남해 중앙부 해역의 표층퇴적물 환경은 유기물 함량과 퇴적물내 식물플랑크톤에 의한 유기물 조성 비율에 따라 4개의 해역으로 구분되었다.

• 해양환경안전학회지
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• 제24권6호
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• pp.750-763
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• 2018

본 연구는 울진 바다목장해역에 서식하는 생물을 대상으로 바다목장 관리를 위한 해양생태계의 영양구조와 에너지흐름을 파악하기 위한 목적으로 2013년 3월부터 10월까지 총 4회 현장조사를 실시하였다. 본 연구에서 개별 생물종들의 생태학적 특징에 따라 유사도에 근거한 비계량형다차원척도법을 사용하여 최고포식자, 바다새, 대형 및 소형유영어류, 볼락류, 가자미류, 저서어류, 반저서어류, 두족류, 저서섭이자, 표서동물, 이매패류, 전복, 자포동물, 동물플랑크톤, 부착성해조류, 미소해조류, 식물플랑크톤, 유기쇄설물 등 총 19가지로 생물그룹핑되었다. Ecopath 모델의 입력변수인 각 생물군들의 생체량, 생산량/생체량의 비, 섭식량/생체량의 비, 피식-포식관계 자료를 사용하여 울진 바다목장해역의 영양구조와 에너지 흐름을 추정하였다. 연구해역에서 각 생물군들의 영양단계는 1 ~ 5.687 범위로 파악되었다. 울진 바다목장 해역에 서식하는 모든 생물그룹들의 전체 소비량의 합은 $229.7t/km^2/yr$, 생물그룹들의 전체 이출량은 $3,432.4t/km^2/yr$이었다. 모든 생물그룹들의 총 에너지량은 $6,796.2t/km^2/yr$, 전체 생산량은 $3,613.1t/km^2/yr$로 추정되었다. 울진 바다목장 해역에서의 순 생태계 생산량은 $3,490.3t/km^2/yr$, 전체 생물군의 생체량은 $167.3t/km^2/yr$으로 추정되었다.

• 수산해양교육연구
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• 제27권2호
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• pp.319-344
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• 2015

A seasonal characteristic of marine environment and fish assemblages in the coastal waters of Jeju Island were determined using samples collected by a trammel net in from 2012 to 2013. Annual mean temperature and salinity were $18.8^{\circ}C$, 33.7psu (2012) and $18.8^{\circ}C$, 33.8psu (2013) which shows stable water mass. nutrient concentrations represent that dissolved inorganic nitrogen (DIN) ranged from 0.030 to 0.217mg/L, dissolved inorganic phosphorus (DIP) from 0.002 to 0.010mg/L, and silicate ($SiO_2$) from 0.096 to 0.292mg/L. Chlorophyll a concentrations of phytoplankton ranged from 0.905 to $1.125{\mu}g/L$ were appeared the highest in summer and the lowest in winter. Suspended Solid(SS) concentrations ranged from 1.200 to 2.100mg/L (mean, 1.634mg/L) were appeared the highest in autumn and the lowest in spring. During the survey period, a total of 83 species (48 families and 12 orders) of fishes were identified, Perciformes and Scorpaeniformes accounted for 63.9% of the total number. The number of species was higher in summer than in winter, showing a peak in summer at 57 species and a low in winter at 47 species. The number of individuals and the biomass peaked in summer at 694 individuals and 151.9kg, and were the lowest in autumn at 466 individuals and 106.5kg. The diversity index, evenness index and richness index were appeared 2.92~3.14, 0.75~0.83 and 7.06~8.56 at each stations. the dominance index were appeared highest in spring and summer, were appeared the lowest in winter and autumn. The Filefish (Stephanolepis cirrhifer), Bluestriped angelfish (Chaetodontoplus septentrionalis), Marbled rockfish (Sebastiscus marmoratus), Rabbit fish (Siganus fuscescens), Blackfin sweeper (Pempheris japonica) were dominant species, which occurred abundantly during the entire survey period. The subtropical fishes were identified total of 41 species (49.4%) and the number of species was higher in summer at 29 (50.9%) species and a low in winter at 20 (42.6%) species. The dominant species of subtropical fishes were appeared Bluestriped angelfish, Blackfin sweeper, Rabbit fish, Scarbreast tuskfish (Choerodon azurio), Ballonfish (Diodon holocanthus), Flagfish (Goniistius zonatus), Blue-spotted boxfish (Ostracion immaculatus) in study sites. The subtropical fishes of species, individual and biomass showed significant correlation with environmental factors (Chlorophyll a, DIN, DIP, $SiO_2$) in almost all sampling sites.

• 환경생물
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• 제28권4호
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• pp.202-211
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• 2010

The variations of physico-chemical factors and the species compositions of phytoplanktons were investigated to analyze the marine ecosystem at the depths during summer in the coast of Dokdo (stations DOK 1-3). The mean values of conductivity (48.9 mS $cm^{-1}$), salinity (32.9 psu) and total suspended solids (57.9 mg $L^{-1}$) were the highest in DOK 1. The biomass (Chl-a) of phytoplanktons was the highest in the surface of DOK 1 (2.61 ${\mu}gL^{-1}$). By the means of physicochemical factors (salinity, turbidity, Chl-a, TN, TP and Si), the water estimated in the coast of Dokdo was more eutrophicated than that in 2008. The phytoplanktons were a total of 42 species in Dokdo, which were composed of 33 species (78.6%) for Bacillariophyceae and 9 species (21.4%) for Dinophyceae. The standing crops of phytoplanktons were the highest ($18{\times}10^3$ cells $L^{-1}$) in the surface of DOK 2 and in the surface of DOK 3, while they were the lowest ($2{\times}10^3$ cells $L^{-1}$) at depth of 40 m of DOK1 and at depth of 30 m of DOK 3. The dominant species of phytoplanktons were Chaetoceros castracanei ($6{\times}10^3$ cells $L^{-1}$) in the surface, Rhizosolenia alata f. gracillima ($3{\times}10^3$ cells $L^{-1}$) at depth of 20 m and Protocentrum compressum ($4{\times}10^3$ cells $L^{-1}$) at the depth of 30 m of DOK 1. At the surface of DOK 2, the dominant species was Bacillaria paxillifer ($6{\times}10^3$ cells $L^{-1}$), while it was Hemiaulus indicus ($12{\times}10^3$ cells $L^{-1}$) at the surface of DOK 3. The DOK 1, which is affected by upwelling, whirlpool and circulation due to the East Korean Warm Current, was the most eutrophicated water body among three stations. The monitoring of marine ecosystem in the coast of Dokdo should be continued to propose the alternatives for water quality and species conservation and to purify the eutrophicated water body due to artificial pollutants as well as natural effectors by the global warming, the climatic change, etc.

• Ocean Science Journal
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• 제41권1호
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• pp.11-29
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• 2006

We investigated species composition and spatial distribution of the euphausiid community in the Yellow Sea and identified the relationship with environmental factors (temperature, salinity, chlorophyll $\alpha$, nitrate, phosphate, and silicate) using bimonthly data from June, 1997 to April, 1998. The environment varied during the sampling period. In warm seasons, thermocline was well developed rendering lower temperature and higher salinity and nutrient concentrations in the bottom layer. During cold seasons the water column was well mixed and no such vertical stratification was noted. Horizontal distribution of temperature, however, differed slightly between near-coast and offshore areas because of the shallow depth of the Yellow Sea, and between southern and northern areas because of the intrusion of water masses such as Yellow Sea Warm Current and Changjiang River Diluted Water. Four euphausiid species were identified: Euphausia pacifica, E. sanzoi, Pseudeuphausia sp. and Stylocheron affine. E. sanzoi and S. affine were collected, just one juvenile each, from the southern area in June and December, respectively. Pseudeuphausia sp. were collected in the eastern area all the year round except June. E. pacifica occurred at the whole study area and were the predominant species, representing at least 97.6% of the euphausiid abundance. Further, the distribution pattern of the species was varied in regards to developmental stages (adult, furcilia, calyptopis, egg). From spring to fall, E. pacifica adults were abundant in the central area where the Yellow Sea Bottom Cold Water prevailed. Furcilia and calyptopis extended their distribution into nearly all the study area during the same period. From late fall to winter, adults were found at the near-coastal are a with similar pattern for furcilia and calyptopis. The distribution pattern of E. pacifica was consistent regarding temperature, salinity, and three nutrients during the sampling period, whereas chlorophyll $\alpha$ showed a different pattern according to the developmental stages. The nutrients should indirectly affect via chlorophyll $\alpha$ and phytoplankton concentration. With respect to these results, we presented a scenario about how the environmental factors along with the water current affect the distribution of E. pacifica in the Yellow Sea.