Temporal and spatial distribution characteristics of amino acids in the green tide outbreak area of Ulva prolifera in the South Yellow Sea
GAO Xin-peng1, JING Yu-ting1, SU Rong-guo1, SHI Xiao-yong1,2
1. Key Laboratory of Marine Chemistry Theory and Engineering Technology, Ministry of Education, School of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China; 2. Oceanography of the State Oceanic Administration Disaster Reduction Center, Beijing 100194, China
Abstract:According to the distinct growth phases of green tides, the green tides development area of Ulva prolifera was divided into two regions: south of 35°N and north of 35°N. The survey data of the South Yellow Sea in two cruises in the spring and summer of 2018 were used to analyze the spatial-temporal distribution characteristics of total dissolved amino acids (TDAA) and dissolved free amino acids (DFAA) in these two regions. The results revealed that concentrations of TDAA and DFAA showed a decreasing distribution from inshore (high) to offshore (low). In the area south of 35°N, the TDAA concentrations increased from spring to summer by 24.8% in the surface seawater and 60.6% in the middle layer seawater, respectively. However, in the area north of 35°N, the TDAA concentration was decreased by 8.7% overall, and decreased by 30.1% in the surface seawater. The uptake and utilization of DON by Ulva prolifera might be an important reason for the TDAA concentration decrease in the seawater with low DIN concentration in the area north of 35°N, which suggested that small molecular organic nitrogen, such as amino acids, played a key role in the late-stage green tide development of Ulva prolifera.
高新芃, 景玉婷, 苏荣国, 石晓勇. 南黄海浒苔绿潮暴发区氨基酸时空分布特征[J]. 中国环境科学, 2021, 41(6): 2902-2909.
GAO Xin-peng, JING Yu-ting, SU Rong-guo, SHI Xiao-yong. Temporal and spatial distribution characteristics of amino acids in the green tide outbreak area of Ulva prolifera in the South Yellow Sea. CHINA ENVIRONMENTAL SCIENCECE, 2021, 41(6): 2902-2909.
Cui J J, Shi J T, Zhang J H, et al. Rapid expansion of Ulva blooms in the Yellow Sea, China through sexual reproduction and vegetative growth[J]. Marine Pollution Bulletin, 2018,130:223-228.
[2]
Ricardo B, Svenja H, Michéal M M, et al. Spatial and temporal variability of biomass and composition of green tides in Ireland[J]. Harmful Algae, 2019,81:94-105.
[3]
Brian E L, Peter J B, Mark M L, et al. Macroalgal blooms on southeast Florida coral reefs[J]. Harmful Algae, 2005,4(6):1092-1105.
[4]
Thierry P, Nadège R, Alain M, et al. Modelling green macroalgal blooms on the coasts of Brittany, France to enhance water quality management[J]. Journal of Marine Systems, 2014,132:38-53.
[5]
修彬,梁生康,李小姣,等.浒苔绿潮对青岛近海溶解有机氮构成和生物可利用性影响[J]. 中国海洋大学学报(自然科学版), 2018, 48(10):37-46. Xiu B, Liang S k, LI X J, et al. The influence of Ulva Prolifera green tide on the composition and bioavailability of dissolved organic nitrogen in Qingdao offshore[J]. Periodical of Ocean University of China (Natural Science edition), 2008,48(10):37-46.
[6]
李鸿妹.营养盐与黄海浒苔绿潮暴发关系的探究[D]. 青岛:中国海洋大学, 2015. Li H M. Study on the relationship between nutrient salt and yellow sea margin green tide[D]. Qingdao:Ocean University of China, 2015.
[7]
张海波,刘珂,苏荣国,等.2018年南黄海浒苔绿潮迁移发展规律与营养盐相互关系探究[J]. 海洋学报, 2020,42(8):30-39. Zhang H B, Liu K, Su R G, et al. Research on the relationship between nutrient salt and migration development rules of Enteromorpha green Tide in the South Yellow Sea in 2018[J]. Acta Oceanologica Sinica, 2020,42(8):30-39.
[8]
Zhang H B, Su R G, Shi X Y, et al. Role of nutrients in the development of floating green tides in the Southern Yellow Sea, China, in 2017[J]. Marine Pollution Bulletin, 2020,156,111197.
[9]
Li H M, Zhang Y Y, Han X R, et al. Growth responses of Ulva prolifera to inorganic and organic nutrients:Implications for macroalgal blooms in the southern Yellow Sea, China[J]. Scientific Reports, 2016,6(1):1423-1432.
[10]
Liu F, Pang S J, Thierry C, et al. Understanding the recurrent large-scale green tide in the Yellow Sea:Temporal and spatial correlations between multiple geographical, aquacultural and biological factors[J]. Marine Environmental Research, 2013,83:38-47.
[11]
徐环,张桂成,李悦悦,等.近海溶解有机氮对浮游植物生物可利用性研究进展[J]. 海洋湖沼通报, 2016,(4):59-67. Xu H, Zhang G C, Li Y Y, et al. Advances in the study of dissolved organic nitrogen on phytoplankton bioavailability in coastal waters[J]. Bulletin of Marine Lakes, 2016,(4):59-67.
[12]
孙岩.南黄海和胶州湾海水中溶解氨基酸的分布与组成研究[D]. 青岛:中国海洋大学, 2012. Sun Y. Distribution and composition of dissolved amino acids in the South Yellow Sea and Jiaozhou Bay[D]. Qingdao:Ocean University of China, 2012.
[13]
孙岩,杨桂朋,陈岩,等.秋季南黄海表层海水中溶解氨基酸的分布与组成研究[J]. 中国海洋大学学报(自然科学版), 2012,42(10):81-87. Sun Y, Yang G P, Chen Y, et al. The distribution and composition of dissolved amino acids in the surface water of the South Yellow Sea in autumn[J]. Journal of Ocean University of China (Natural Science Edition), 2012,42(10):81-87.
[14]
刘莉,杨桂朋,陈岩.秋季中国东海海水中溶解氨基酸的分布与组成[J]. 海洋环境科学, 2013,32(4):510-517. Liu L, Yang G P, Chen Y. Distribution and composition of dissolved amino acids in the East China Sea in autumn[J]. Marine Environmental Science, 2013,32(4):510-517.
[15]
夏清艳.中国近海海水中溶解氨基酸的分布与组成研究[D]. 青岛:中国海洋大学, 2011. Xia Q Y. Research on the distribution and composition of dissolved amino acids in China's offshore waters[D]. Qingdao:Ocean University of China, 2011.
[16]
张桂成.长江口及其邻近海域溶解有机氮的生物可利用性及其在赤潮爆发过程中的作用研究[D]. 青岛:中国海洋大学, 2015. Zhang G C. Bioavailability of dissolved organic nitrogen and its role during outbreak of harmful algal blooms in Yangtze River Estuary and its adjacent sea[D]. Qingdao:Ocean University of China, 2015.
[17]
Xiu B, Liang S K, He X L, et al. Bioavailability of dissolved organic nitrogen and its uptake by Ulva prolifera:Implications in the outbreak of a green bloom off the coast of Qingdao, China[J]. Marine Pollution Bulletin, 2019,140:563-572.
[18]
白雨,赵亮,刘境舟.生态因子在黄海绿潮生消过程中的作用[J]. 海洋学报, 2019,41(8):97-105. Bai Y, Zhao L, Liu J Z. The role of ecological factors in the generation and disappearance of green tides in the Yellow Sea[J]. Acta Oceanologica Sinica, 2019,41(8):97-105.
[19]
Keesing J K, Liu D Y, Fearns P, et al. Inter- and intra-annual patterns of Ulva prolifera green tides in the Yellow Sea during 2007-2009, their origin and relationship to the expansion of coastal seaweed aquaculture in China.[J]. Marine pollution bulletin, 2011,62(6):1169-1182.
[20]
丁月旻.黄海浒苔绿潮中生源要素的迁移转化及对生态环境的影响[D]. 青岛:中国科学院研究生院(海洋研究所), 2014. Ding Y M. Impacts of Ulva proliferca in the green tide on the Yellow Sea ecological environmen-implications from migration and transformation of biogenic elements[D]. Qingdao:Graduate school of Chinese Academy of Sciences (Institute of Oceanography), 2014.
[21]
王朋,陈岩,杨桂朋,等.春季中国南黄海与东海海水中溶解氨基酸的分布和组成[J]. 海洋环境科学, 2015,34(2):217-224. Wang P, Chen Y, Yang G P, et al. Distribution and composition of dissolved amino acids in the East China Sea and the Yellow Sea during spring[J]. Marine Environmental Science, 2015,34(2):217-224.
[22]
Zhang P Y, Yang G P, Chen Y, et al. Temporal and spatial variations of particulate and dissolved amino acids in the East China Sea[J]. Marine Chemistry, 2016,186:113-144.
[23]
Susan M H, John W F. Amino acids in interstitial waters of marine sediments:a comparison of results from varied sedimentary environments[J]. Physics and Chemistry of the Earth, 1980,12:435-443.
[24]
王朋.南黄海与东海海水中氨基酸的组成和分布研究[D]. 青岛:中国海洋大学, 2014. Wang P. Study on the composition and distribution of amino acids in the South Yellow Sea and East China Sea[D]. Qingdao:Ocean University of China, 2014.
[25]
殷京玉,金春洁,石晓勇,等.2013年夏秋季黄海溶解无机氮的分布及季节变化特征[J]. 海洋通报, 2017,36(1):74-81. Yin J Y, Jin C J, Shi X Y, et al. Distribution and seasonal variation in dissolved inorganic nitrogen of the Yellow Sea in summer and autumn of 2013[J]. Marine Science Bulletin, 2017,36(1):74-81.
[26]
石学连.浒苔多糖的化学组分及生物学活性的初步研究[D]. 青岛:中国科学院研究生院(海洋研究所), 2009. Shi X L. A preliminary study on the chemical components and biological activities of Ulva prolifera[D]. Qingdao:Graduate University of the Chinese Academy of Sciences (Institute of Oceanology), 2009.