Minji Lee, Jin Ho Kim, Yun-Bae Kim, Chan Hong Park, Kyoungsoon Shin, Seung Ho Baek. Specific oceanographic characteristics and phytoplankton responses influencing the primary production around the Ulleung Basin area in spring[J]. Acta Oceanologica Sinica, 2020, 39(2): 107-122. doi: 10.1007/s13131-020-1545-9
Citation: Minji Lee, Jin Ho Kim, Yun-Bae Kim, Chan Hong Park, Kyoungsoon Shin, Seung Ho Baek. Specific oceanographic characteristics and phytoplankton responses influencing the primary production around the Ulleung Basin area in spring[J]. Acta Oceanologica Sinica, 2020, 39(2): 107-122. doi: 10.1007/s13131-020-1545-9

Specific oceanographic characteristics and phytoplankton responses influencing the primary production around the Ulleung Basin area in spring

doi: 10.1007/s13131-020-1545-9
Funds:  The Basic Core Technology Development Program for the Oceans and the Polar Regions of the National Research Foundation (NRF) funded by the Ministry of Science, ICT & Future Planning under contract No. NRF-2016 M1A5A1027456; the project of the Ministry of Ocean and Fisheries under contract No. PG51010.
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  • Corresponding author: E-mail: baeksh@kiost.ac.kr
  • Received Date: 2018-10-26
  • Accepted Date: 2018-12-12
  • Available Online: 2020-04-21
  • Publish Date: 2020-02-25
  • The East Sea (Sea of Japan) is a marginal, semi-closed sea in the northwestern Pacific. The Ulleung Basin area, which is located near the subpolar front of the East Sea, is known to have high primary production and good fisheries in spring season. After episodic wind-driven events during the spring of 2017, horizontal and vertical profiles of physical chemical biological factors were investigated at 29 stations located in the Ulleung Basin area. In addition, growth responses of phytoplankton communities to nutrient additions were evaluated by bioassay experiments to understand the fluctuation of phytoplankton biomass. Because of strong northwestern wind, phytoplankton biomass was scattered and upwelling phenomenon might be suppressed in this season. The phytoplankton abundances in the coastal stations were significantly higher than offshore and island stations. In contrast, the nutrient and chlorophyll a (Chl a) concentrations and the phytoplankton biomass were quite low in all locations. Bacillariophyceae was dominated group (>75.1% for coastal, 40.0% for offshore and 43.6% for island stations). In the algal bioassays, the phytoplankton production was stimulated by N availability. The in vivo Chl a values in the +N and +NP treatments were significantly higher than the values in the control and the +P treatments. Based on the field survey, the higher nutrients in coastal waters affected the growth of diatom assemblages, however, little prosperity of phytoplankton was observed in the offshore waters despite the injection of sufficient nutrients in bioassay experiments. The growth of phytoplankton depended on the initial cell density. All of results indicated that a dominant northwestern wind led to a limited nutrients condition at euphotic layers, and the low level of biomass supply from the coasts resulted in low primary production. Both supplying nutrients and introducing phytoplankton through the currents are critical to maintain the high productivity in the Ulleung Basin area of the East Sea.
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  • [1]
    Baek S H, Kim D, Son M, et al. 2015. Seasonal distribution of phytoplankton assemblages and nutrient-enriched bioassays as indicators of nutrient limitation of phytoplankton growth in Gwangyang Bay, Korea. Estuarine, Coastal and Shelf Science, 163: 265–278. doi: 10.1016/j.ecss.2014.12.035
    [2]
    Baek S H, Lee M, Kim Y B. 2016. Growth and community response of phytoplankton by N, P and Fe nutrient addition in around water of Ulleungdo and Dokdo in East Sea. Journal of the Korea Academia-Industrial cooperation Society, 11: 186–195
    [3]
    Baek S H, Lee M, Kim Y B. 2018. Spring phytoplankton community response to an episodic windstorm event in oligotrophic waters offshore from the Ulleungdo and Dokdo islands, Korea. Journal of Sea Research, 132: 1–14. doi: 10.1016/j.seares.2017.11.003
    [4]
    Chung C S, Shim J H, Park Y G, et al. 1989. Primary productivity and nitrogenous nutrient dynamics in the East Sea of Korea. Journal of the Korean Society of Oceanography, 24: 52–61
    [5]
    Fisher T R, Peele E R, Ammerman J W, et al. 1992. Nutrient limitation of phytoplankton in Chesapeake Bay. Marine Ecology Progress Series, 82(1): 51–63
    [6]
    Gilmartin M, Revelante N. 1974. The ‘island mass’ effect on the phytoplankton and primary production of the Hawaiian Islands. Journal of Experimental Marine Biology and Ecology, 16(2): 181–204. doi: 10.1016/0022-0981(74)90019-7
    [7]
    Gong Y, Park C K. 1969. On the oceanographical character of the low temperature region in the eastern sea of Korea. Bulletin of Fisheries Research Agency, 4: 69–91
    [8]
    Gong Y, Son S J. 1982. A study of oceanic thermal fronts in the southwestern Japan Sea. Bulletin of Fisheries Research Agency, 28: 25–54
    [9]
    Hernández-León S. 1991. Accumulation of mesozooplankton in a wake area as a causative mechanism of the “island-mass effect”. Marine Biology, 109(1): 141–147. doi: 10.1007/BF01320241
    [10]
    Hyun J H, Kim D, Shin C W, et al. 2009. Enhanced phytoplankton and bacterioplankton production coupled to coastal upwelling and an anticyclonic eddy in the Ulleung Basin, East Sea. Aquatic Microbial Ecology, 54: 45–54
    [11]
    Isobe A, Isoda Y. 1997. Circulation in the Japan Basin, the northern part of the Japan Sea. Journal of Oceanography, 53(4): 373–381
    [12]
    Isoda Y, Saitoh S. 1993. The northward intruding eddy along the east coast of Korea. Journal of Oceanography, 49(4): 443–458. doi: 10.1007/BF02234959
    [13]
    Kang Y S, Kim J Y, Kim H G, et al. 2002. Long-term changes in zooplankton and its relationship with squid, Todarodes pacificus, catch in Japan/East Sea. Fisheries Oceanography, 11(6): 337–346. doi: 10.1046/j.1365-2419.2002.00211.x
    [14]
    Kang Y S, Choi H C, Lim J H, et al. 2005. Dynamics of the phytoplankton community in the coastal waters of Chuksan harbor, East Sea. Algae, 20(4): 345–352. doi: 10.4490/ALGAE.2005.20.4.345
    [15]
    Kim K, Chung J Y. 1984. On the salinity-minimum and dissolved oxygen-maximum layer in the East Sea (Sea of Japan). In: Elsevier Oceanography Series. Amsterdam: Elsevier, 55–65
    [16]
    Kim D S, Kim K H, Shim J H, et al. 2007a. The effect of anticyclonic eddy on nutrients and chlorophyll during spring and summer in the Ulleung Basin, East Sea. The Sea, 12(4): 280–286
    [17]
    Kim J H, Wang P B, Park B S, et al. 2018. Revealing the distinct habitat ranges and hybrid zone of genetic sub-populations within Pseudo-nitzschia pungens (Bacillariophyceae) in the West Pacific area. Harmful Algae, 73: 72–83. doi: 10.1016/j.hal.2018.01.007
    [18]
    Kim D, Yang E J, Kim K H, et al. 2012. Impact of an anticyclonic eddy on the summer nutrient and chlorophyll a distributions in the Ulleung Basin, East Sea (Japan Sea). ICES Journal of Marine Science, 69(1): 23–29. doi: 10.1093/icesjms/fsr178
    [19]
    Kim H C, Yoo S J, Oh I S. 2007b. Relationship between phytoplankton bloom and wind stress in the sub-polar frontal area of the Japan/East Sea. Journal of Marine Systems, 67(3–4): 205–216. doi: 10.1016/j.jmarsys.2006.05.016
    [20]
    Kim C H, Yoon J H. 1999. A numerical modeling of the upper and the intermediate layer circulation in the East Sea. Journal of Oceanography, 55(2): 327–345. doi: 10.1023/A:1007837212219
    [21]
    Kwak J H, Hwang J, Choy E J, et al. 2013. High primary productivity and f-ratio in summer in the Ulleung basin of the East/Japan Sea. Deep Sea Research Part I: Oceanographic Research Papers, 79: 74–85. doi: 10.1016/j.dsr.2013.05.011
    [22]
    Kwon K Y, Moon C H, Kang C K, et al. 2002. Distribution of particulate organic matters along the salinity gradients in the Seomjin River estuary. Korean Journal of Fisheries and Aquatic Science, 35(1): 86–96. doi: 10.5657/kfas.2002.35.1.086
    [23]
    Lee J. 1983. Variations of sea level and sea surface temperature associated with wind-induced upwelling in the southeast coast of Korea in summer. Journal of the Korean Society of Oceanography, 18(2): 149–160
    [24]
    Lee J B, Han M S, Yang H S. 1998. The ecosystem of the southern coastal waters of the East Sea, Korea: I. Phytoplankton community structure and primary productivity in September, 1994. Korean Journal of Fisheries and Aquatic Science, 31(1): 45–55
    [25]
    Lee J Y, Kang D J, Kim I N, et al. 2009. Spatial and temporal variability in the pelagic ecosystem of the East Sea (Sea of Japan): a review. Journal of Marine Systems, 78(2): 288–300. doi: 10.1016/j.jmarsys.2009.02.013
    [26]
    Lee J C, Na J Y. 1985. Structure of upwelling off the southeast coast of Korea. Journal of the Korean Society of Oceanography, 20: 6–19
    [27]
    Lee M, Park B S, Baek S H. 2018. Tidal influences on biotic and abiotic factors in the Seomjin River Estuary and Gwangyang Bay, Korea. Estuaries and Coasts, 41(7): 1977–1993. doi: 10.1007/s12237-018-0404-9
    [28]
    Lee T, Rho T K. 2015. Seawater N/P ratio of the East Sea. The Sea, 20(4): 199–205. doi: 10.7850/jkso.2015.20.4.199
    [29]
    Liu G M, Chai F. 2009. Seasonal and interannual variation of physical and biological processes during 1994–2001 in the Sea of Japan/East Sea: a three-dimensional physical-biogeochemical modeling study. Journal of Marine Systems, 78(2): 265–277. doi: 10.1016/j.jmarsys.2009.02.011
    [30]
    Martin S, Kawase M. 1998. The southern flux of sea ice in the Tatarskiy Strait, Japan Sea and the generation of the Liman Current. Journal of Marine Research, 56(1): 141–155. doi: 10.1357/002224098321836145
    [31]
    Mooers C N K, Bang I, Sandoval F J. 2005. Comparisons between observations and numerical simulations of Japan (East) Sea flow and mass fields in 1999 through 2001. Deep Sea Research Part II: Topical Studies in Oceanography, 52(11–13): 1639–1661. doi: 10.1016/j.dsr2.2004.10.003
    [32]
    Moon C H, Yang S R, Yang H S, et al. 1998. Regeneration processes of nutrients in the polar front area of the last sea: IV. Chlorophyll a distribution, new production and the vertical diffusion of nitrate. Korean Journal of Fisheries and Aquatic Science, 31(2): 259–266
    [33]
    Oh H J, Suh Y S, Heo S. 2004. The relationship between phytoplankton distribution and environmental conditions of the upwelling cold water in the eastern coast of the Korean peninsula. Journal of the Korean Association of Geographic Information Studies, 7: 166–173
    [34]
    Ohshima K I. 1994. The flow system in the Japan Sea caused by a sea level difference through shallow straits. Journal of Geophysical Research, 99(C5): 9925–9940. doi: 10.1029/94JC00170
    [35]
    Park C K. 1979. On the distribution of dissolved oxygen off the east coast of Korea. Journal of the Korean Society of Oceanography, 14(2): 67–70
    [36]
    Park B S, Kim J H, Kim J H, et al. 2018. Intraspecific bloom succession in the harmful dinoflagellate Cochlodinium polykrikoides (Dinophyceae) extended the blooming period in Korean coastal waters in 2009. Harmful Algae, 71: 78–88. doi: 10.1016/j.hal.2017.12.004
    [37]
    Parsons T R. 2013. A Manual of Chemical & Biological Methods for Seawater Analysis. New York: Elsevier
    [38]
    Redfield A C. 1958. The biological control of chemical factors in the environment. American Scientist, 46: 205–221
    [39]
    Ryan J P, Polito P S, Strutton P G, et al. 2002. Unusual large-scale phytoplankton blooms in the equatorial Pacific. Progress in Oceanography, 55(3–4): 263–285. doi: 10.1016/S0079-6611(02)00137-4
    [40]
    Smith S M, Hitchcock G L. 1994. Nutrient enrichments and phytoplankton growth in the surface waters of the Louisiana Bight. Estuaries, 17(4): 740–753. doi: 10.2307/1352744
    [41]
    Smith V H, Tilman G D, Nekola J C. 1999. Eutrophication: impacts of excess nutrient inputs on freshwater, marine, and terrestrial ecosystems. Environmental Pollution, 100(1–3): 179–196. doi: 10.1016/S0269-7491(99)00091-3
    [42]
    Sournia A. 1978. Phytoplankton Manual: Monographs on Oceanographic Methodology. Vol 6. Paris: UNESCO
    [43]
    Tsuchiya K, Kuwahara V S, Yoshiki T, et al. 2014. Phytoplankton community response and succession in relation to typhoon passages in the coastal waters of Japan. Journal of Plankton Research, 36(2): 424–438. doi: 10.1093/plankt/fbt127
    [44]
    Wasmund N, Andrushaitis A, Łysiak-Pastuszak E, et al. 2001. Trophic status of the south-eastern Baltic Sea: a comparison of coastal and open areas. Estuarine, Coastal and Shelf Science, 53(6): 849–864. doi: 10.1006/ecss.2001.0828
    [45]
    Yang H S, Kim S S, Kang C G, et al. 1991. A study on sea water and ocean current in the sea adjacent to Korea Peninsula-III. Chemical characteristics of water masses in the polar front area of the central Korean East Sea. Korean Journal of Fisheries and Aquatic Science, 24(3): 185–192
    [46]
    Yoo S, Park J. 2009. Why is the southwest the most productive region of the East Sea/Sea of Japan?. Journal of Marine Systems, 78(2): 301–315. doi: 10.1016/j.jmarsys.2009.02.014
    [47]
    Zhang C I, Lee J B, Kim S, et al. 2000. Climatic regime shifts and their impacts on marine ecosystem and fisheries resources in Korean waters. Progress in Oceanography, 47(2–4): 171–190. doi: 10.1016/S0079-6611(00)00035-5
    [48]
    Zhang J, Liu S M, Ren J L, et al. 2007. Nutrient gradients from the eutrophic Changjiang (Yangtze River) Estuary to the oligotrophic Kuroshio waters and re-evaluation of budgets for the East China Sea Shelf. Progress in Oceanography, 74(4): 449–478. doi: 10.1016/j.pocean.2007.04.019
    [49]
    Zhao Hui, Tang Danling, Wang Yuqing. 2008. Comparison of phytoplankton blooms triggered by two typhoons with different intensities and translation speeds in the South China Sea. Marine Ecology Progress Series, 365: 57–65. doi: 10.3354/meps07488
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