• ALGAE
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• 제33권4호
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• pp.359-366
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• 2018

Mesocosm experiments conducted for ecological purposes have become increasingly popular because they can provide a holistic understanding of the biological complexities associated with natural systems. This paper describes a new outdoor mesocosm designed for $CO_2$ perturbation experiments of benthos. Manipulated the carbonate chemistry in a continuous flow-through system can be parallelized with diurnal changes, while irradiance, temperature, and nutrients can vary according to the local environment. A target hydrogen ion activity (pH) of seawater was sufficiently stabilized and maintained within 4 h after dilution, which was initiated by the ratio of $CO_2$-saturated seawater to ambient seawater. Specifically, pH and $CO_2$ partial pressure ($pCO_2$) levels gradually varied from 8.05-7.28 and $375-2,691{\mu}atm$, respectively, over a range of dilution ratios. This mesocosm can successfully manipulate the pH and $pCO_2$ of seawater, and it demonstrates suitability for ocean acidification experiments on benthic communities.

• 한국수산과학회지
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• 제47권2호
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• pp.154-159
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• 2014

The increasing of atmospheric $CO_2$ are changing the pH (ocean acidification) and temperature of the sea. Although the effects of ocean acidification on calcifying organisms have well-documented, only a few studies have examined the combined effects of ocean acidification and elevated temperature. This study investigated the effects of ocean acidification and elevated temperature for 2100 on survival and growth of juvenile abalone, Haliotis discus hannai. Ocean acidification was simulated by bubbling $CO_2$ into seawater at concentrations of 1,000 and 1,500 ppm, and temperature was set at room temperature $+2^{\circ}C$. Neither $CO_2$ nor temperature had a significant effect on survival of abalone, while both significantly affected growth. There was no significant interaction between the two factors. Shell length can be used as a growth index of abalone to access the impacts of ocean acidification and elevated temperature.

• 지질공학
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• 제32권4호
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• pp.559-569
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• 2022

이 연구는 포항시 흥해지역 지하수, 하천수, 저수지의 해수 혼합과 산성화, 그리고 포항지진(2017년 11월 15일)으로 인한 액상화 유출수의 기원에 대해서 알아보았다. 연구지역은 제3기 퇴적암층 지질로 구성된다. 지하수 6점, 저수지 5점, 하천수 4점, 액상화 유출수 2점, 해수 1점의 시료를 채취하여 화학성분과 산소 및 수소 동위원소를 분석하였다. 연구지역 중심을 동서로 관통하는 곡강천은 서쪽에서 동해쪽으로 흐른다. 하천 하부지역의 지하수와 저수지는 pH 4 이하의 산성수로 황산염이 부화된 Ca(Mg)-SO₄의 수질화학적 유형을 보인다. 제 3기 지층에서 확인되는 황철석의 산화에 의해 기원한 것으로 보이는 Al, Mn, Fe 성분이 특징적으로 높은 농도를 보인다. 하천 상부지역은 하천을 따라서 유입된 염수가 혼합되어 지하수는 Ca(Na)-HCO₃(Cl) 유형의 화학적 특성을 보인다. 𝛿D와 𝛿¹⁸O 동위원소 분석 결과 모든 물은 GMWL을 따라서 분포하며, 저수지는 증발작용으로 부화된 특성을 보인다. 화학성분과 동위원소 조성으로 볼 때 액상화 유출수 2점은 충적층으로 확산된 인접한 하천수, 그리고 염수화가 일부 진행된 심부와 천부 지하수가 용출된 것으로 보인다.

• 한국수산과학회지
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• 제50권2호
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• pp.153-159
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• 2017

We examined changes in the physiological responses of gray mullet Mugil cephalus exposed to acidic seawater (pH 6.0, 6.5, 7.0) and normal seawater (pH 8.0, control) for 15 days. As pH decreased, survival rate and body weight also decreased. Levels of aminotransferase, total protein and triglycerides also differed significantly with changes in pH, presumably due to stress caused by exposure to acidic water. The level of osmotic pressure was significantly higher in the pH 6.0 group than in other groups. Superoxide dismutase was significantly higher in the pH 6.5 and 7.0 groups than in the pH 8.0 group, and glutathione level was lowest in the pH 6.0 group. We conclude that decreasing the pH level of seawater induces a stress response in fish, damaging their ability to control their hematological and osmotic pressure. Antioxidant enzymes are generally sensitive to osmotic stress; in this study, antioxidant activity significantly changed with pH level. These results indicate that physiological stress induced by exposure to acidification reduces survival rates and inhibits growth in M. cephalus.

• 한국환경과학회지
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• 제23권3호
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• pp.483-492
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• 2014

DNA damage such as genotoxicity was identified with comet assay, which blood cell of a marine parrot fish (Oplegnathus fasciatus) was exposed to an acidified seawater, lowered pH gradient making of $CO_2$ gas. The gradient of pH were 8.22, 8.03, 7.81, 7.55 with control as HBSS solution with pH 7.4. DNA tail moment of fish blood cell was $0.548{\pm}0.071$ exposed seawater of pH 8.22 condition, on the other hand, DNA tail moment $1.601{\pm}0.197$ exposed acidified seawater of pH 7.55 lowest condition. The approximate difference with level of DNA damage was 2.9 times between highest and lowest of pH. DNA damage with decreasing pH was significantly increased with DNA tail moment on blood cell of marine fish (ANOVA, p < 0.001). Ocean acidification, especially inducing the leakage of sequestered $CO_2$ in geological structure is a consequence from the burning of fossil fuels, and long term effects on marine habitats and organisms are not fully investigated. The physiological effects on adult fish species are even less known. This result shown that the potential of dissolved $CO_2$ in seawater was revealed to induce the toxic effect on genotoxicity such as DNA breakage.

• Ocean and Polar Research
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• 제34권2호
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• pp.197-199
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• 2012

According to the IPCC climate change scenario (A1B scenario), the surface seawater temperature of the South Sea of Korea by 2100 may be $2-3.5^{\circ}C$ higher than at present, and seawater pH may decrease from 8.1 to 7.8, due to the increase in atmospheric $CO_2$, which is predicted to increase in concentration from 380 to 750 ppm. These changes may not only intensify the strength of typhoons/storm surges but also affect the function and structure the marine ecosystem. In order to assess the impact of climate change on the marine ecosystem in Korean waters, the project named the 'Assessment of the impact of climate change on marine ecosystem in the South Sea of Korea' has been supported by the Ministry of Land, Transport and Maritime Affairs, from 2008. The goal of this project is to enhance our ability to adapt and prepare for the future environmental changes through the reliable predictions based on the knowledge obtained from projects like this. In this respect, this project is being conducted to investigate the effects of climate/marine environment changes (ocean warming and acidification), and to predict future changes of the structure and function of the ecosystem in the South Sea of Korea. This special issue contains 6 research articles, which are the highlights of the studies carried out through this project.

• Ocean and Polar Research
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• 제35권2호
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• pp.123-125
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• 2013

According to the Intergovernmental Panel on Climate Change (IPCC), ocean warming and acidification are accelerating as a result of the continuous increase in atmospheric $CO_2$. This may affect the function and structure of marine ecosystems. Recently, changes in marine environments/ecosystems have been observed (increase in SST, decrease in the pH of seawater, northward expansion of subtropical species, etc.) in Korean waters. However, we still don't understand well how climate change affects these changes and what can be expected in the future. In order to answer these questions with regard to Korean waters, the project named 'Assessment of the impact of climate change on marine ecosystems in the South Sea of Korea' has been supported for 5 years by the Ministry of Oceans and Fisheries and is scheduled to end in 2013. This project should provide valuable information on the current status of marine environments/ecosystems in the South Sea of Korea and help establish the methodology and observation/prediction systems to better understand and predict the impact of climate/marine environment changes on the structure and function of marine ecosystems. This special issue contains 5 research and a review articles that highlight the studies carried out during 2012-2013 through this project.

• ALGAE
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• 제28권2호
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• pp.173-183
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• 2013

Sodium hypochlorite (NaOCl) is widely used to disinfect seawater in power plant cooling systems in order to reduce biofouling, and in ballast water treatment systems to prevent transport of exotic marine species. While the toxicity of NaOCl is expected to increase by ongoing ocean acidification, and many experimental studies have shown how algal calcification, photosynthesis and growth respond to ocean acidification, no studies have investigated the relationship between NaOCl toxicity and increased $CO_2$. Therefore, we investigated whether the impacts of NaOCl on survival, chlorophyll a (Chl-a), and effective quantum yield in three marine phytoplankton belonging to different taxonomic classes are increased under high $CO_2$ levels. Our results show that all biological parameters of the three species decreased under increasing NaOCl concentration, but increasing $CO_2$ concentration alone (from 450 to 715 ${\mu}atm$) had no effect on any of these parameters in the organisms. However, due to the synergistic effects between NaOCl and $CO_2$, the survival and Chl-a content in two of the species, Thalassiosira eccentrica and Heterosigma akashiwo, were significantly reduced under high $CO_2$ when NaOCl was also elevated. The results show that combined exposure to high $CO_2$ and NaOCl results in increasing toxicity of NaOCl in some marine phytoplankton. Consequently, greater caution with use of NaOCl will be required, as its use is widespread in coastal waters.

• 한국수산과학회지
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• 제46권6호
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• pp.862-867
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• 2013

Since the industrial revolution, seawater has increased in temperature and acidity due to the increase in anthropogenic carbon dioxide in the atmosphere. To understand the effect of elevated $CO_2$ on the early life stages of fish, we reared fertilized eggs of black sea bream Acanthopagrus schlegelii under three $CO_2$ concentrations (400, 850 and 1550 ppm) for 3 weeks. The standard length and wet weight of black sea bream larvae declined with enhanced $CO_2$ concentration in the rearing water (P<0.05). However, chemical analysis using ICP-OES on internal tissues of black sea bream larvae indicated that the whole-body calcium concentration increased with $CO_2$ concentration in the rearing water. These conflicting results suggest that future experiments should examine the acid-base balance to investigate the formation of bone and otolith during larval growth.

• 생명과학회지
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• 제27권7호
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• pp.826-833
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• 2017

대기의 이산화탄소의 농도 증가는 해양산성화와 지구온난화를 유발하는 것으로 알려져 있다. 해마는 해양생태계 및 수산자원생물로서 중요한 종으로 알려져 있지만, 최근 해양산성화로 인하여 개체수가 감소되고 있는 실정이다. 따라서 본 연구에서는 멸종 위기 종인 복해마(Hippocampus kuda)에 미치는 생리적 영향을 조사하기 위해서 사육수의 산성조건인 pH 6.0, 6.5, 7.0 및 자연해수(pH 8.0)의 환경에서 복해마(H. kuda)를 15일 동안 사육 후 체내 조성 변화 및 항산화 효소 활성 변화에 대하여 조사를 실시하였다. 복해마(H. kuda)의 크기 및 성장은 대조군인 pH 8.0을 제외한 실험군에서는 pH가 저하함에 따라 감소하는 경향을 나타내었다. 체내 조성성분인 회분, 조지방 및 조단백 또한 pH 저하에 따라 농도의존적으로 감소하는 것이 관찰되었다. SOD, CAT 및 GSH와 같은 항산화 효소의 분석 결과, SOD활성의 경우, pH 저하에 따라 농도의존적으로 감소하지만, 이와 상반되게 CAT 및 GSH에서는 pH저하에 따라 활성이 농도의존적으로 증가하는 결과가 나타내었다. 이것은 복해마(H. kuda)가 사육수의 pH 저하에 따른 체내 항상성을 유지하는 과정 중 스트레스가 야기되어 에너지 대사가 손상된 것으로 추정된다. 항산화효소는 일반적으로 산성화 스트레스에 민감하게 작용하는데 본 연구에서도 사육수의 pH 변화에 따라 항산화 효소작용이 유의하게 변화하였다. 이러한 결과로 복해마(H. kuda)에 있어서 산성화 노출을 통한 생리학적 스트레스가 항산화 반응 및 체내 성분과 성장을 저해하는 것으로 여겨진다.