Plankton community response to physico-chemical forcing in the Ulleung Basin, east sea during summer 2008 SCOPUS KCI

Title
Plankton community response to physico-chemical forcing in the Ulleung Basin, east sea during summer 2008
Author(s)
Rho, T.; Kang, D.-J.; Kim, Y.-B.; Park, J.I.; Lee, Y.-W.; Im, D.H.; Lee, T.; Yoon, S.-T.; Kim, T.-H.; Kwak, J.-H.; Park, H.J.; Jeong, M.K.; Chang, K.-I.; Kang, C.-K.; Suh, H.-L.; Park, M.; Lee, H.; Kim, K.-R.
KIOST Author(s)
Kang, Dong Jin(강동진)
Publication Year
2010
Abstract
In Summer 2008, a multidisciplinary survey was conducted onboard R/V Haeyang 2000 to understand plankton response to the three distinct physico-chemical settings that developed in the Ulleung Basin of the East Sea. Baseline settings of hydrographic conditions included the presence of the thin (<20 m) Tsushima Surface Water (TSW) on top of the Tsushima Middle Water (TMW). It extends from the Korea Strait to 37°N along the 130°E and then turns offshore and encompasses the relatively saline (T>26°C, S>33.7) Ulleung Warm Eddy surface water centered at 36.5°N and 131°E. A relatively colder and saline water mass appeared off the southeastern coast of Korea. It was accompanied by higher nutrient and chlorophyll-α concentrations, suggesting a coastal upwelling. Most of the offshore surface waters support low phytoplankton biomass (0.3 mg chl-α m-3). A much denser phytoplankton biomass (1-2.3 mg m-3) accumulated at the subsurface layer between 20-50 m depth. The subsurface chlorophyll-a maximum (SCM) layer was closely related to the nutricline, suggesting an active growth of phytoplankton at depth. The SCM developed at shallow depth (20-30 m) near the coast and deepened offshore (50-60 m). A fucoxanthin/zeaxanthin ratio was high in coastal waters while it was low in offshore waters, which indicated that diatoms dominate coastal waters while cyanobacteria dominate offshore waters. The community structure and biomass of phytoplanktonare closely related to nitrogen availability. Zooplankton biomass was higher in the coastal region than in the offshore region while species richness showed an opposite trend. Zooplankton community structure retained a coastal/offshore contrast. These suggest that summer hydrography is a stable structure, lasting long enough to allow a hydrography-specific plankton community to evolve.
ISSN
1598-141X
URI
https://sciwatch.kiost.ac.kr/handle/2020.kiost/4153
DOI
10.4217/OPR.2010.32.3.269
Bibliographic Citation
Ocean and Polar Research, v.32, no.3, pp.269 - 289, 2010
Subject
chlorophyll a; coastal circulation; coastal water; community response; concentration (composition); cyanobacterium; ecological impact; hydrographic survey; nutrient cycling; physicochemical property; plankton; summer; upwelling; water mass; Pacific Ocean; Sea of Japan; Ulleung Basin; Bacillariophyta; Cyanobacteria
Keywords
Coastal upwelling; East sea; Physico-chemical forcing; Plankton community structure; Ulleung basin
Type
Article
Language
English
Document Type
Article
Related Researcher
Research Interests

Chemical Oceanography,Dissolved Gas in seawater,Development of Instruments,화학해양학,해수용존기체,관측장비개발

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