Changes in the characteristics of organic matter associated with hydrodynamics and phytoplankton size structure in the central-eastern Yellow Sea SCIE SCOPUS

DC Field Value Language
dc.contributor.author Lee, Yeon Jung -
dc.contributor.author Choi, Dong Han -
dc.contributor.author Lee, Ho Won -
dc.contributor.author Hyun, Myung Jin -
dc.contributor.author Kim, Gi Yeong -
dc.contributor.author Lee, Haeun -
dc.contributor.author Yang, Won Seok -
dc.contributor.author Kim, Ji Hoon -
dc.contributor.author Won, Jong Seok -
dc.contributor.author Ra, Kongtae -
dc.contributor.author Jeong, Hyeryeong -
dc.contributor.author Choi, Jin Young -
dc.contributor.author Lee, Seok -
dc.contributor.author Kim, Moon Koo -
dc.contributor.author Noh, Jae Hoon -
dc.date.accessioned 2021-11-22T03:30:13Z -
dc.date.available 2021-11-22T03:30:13Z -
dc.date.created 2021-11-22 -
dc.date.issued 2022-02 -
dc.identifier.issn 0048-9697 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/41766 -
dc.description.abstract The central-eastern Yellow Sea is an important region for transporting organic matter (OM) to the Pacific Ocean, however, there is limited information available regarding the characteristics and sources of OM in this area. The present study investigated the concentrations and stable isotopic compositions of carbon (δ13C) and nitrogen (δ15N) for particulate matter and sediment in the central-eastern Yellow Sea during April 2019. The physicochemical properties (i.e., salinity, temperature, fluorescence, and nutrients), size-fractionated phytoplankton biomass (Chl-a), and concentration and fluorescence characteristics of dissolved organic matter (DOM) were also determined. The satellite SST and Chl-a data indicated that mixing cold and warm water masses were observed. Phytoplankton blooms occurred a few days before our sampling campaign. Considering the high concentration of suspended solids in the bottom layer, resuspended sediment caused by tidal currents could be a major source of OM in coastal areas. The δ13C values of particulate organic matter (POM) in the coastal area were higher (−22 to −23‰) than those of OM from terrestrial sources (approximately −27 to −28‰). Instead, the lowest δ13C values were observed in the central part of our study area, where the relative abundance of picophytoplankton was high. These results indicated that phytoplankton-derived OM after phytoplankton spring blooms in the coastal area could be the primary source of OM rather than terrestrial origins. In addition, the source of OM that presented low δ13C values could be picophytoplankton-derived OM. The characteristics of DOM were related to biological processes (mediated by phytoplankton and bacteria) and resuspension of sedimentary organic matter. We did not detect an influx of large amounts of terrestrial OM in coastal sediments. Overall, the source and characteristics of OM appeared to be influenced by the hydrodynamics and the distribution properties of lower trophic-level organisms in the central-eastern Yellow Sea during the spring season. -
dc.description.uri 1 -
dc.language English -
dc.publisher Elsevier BV -
dc.title Changes in the characteristics of organic matter associated with hydrodynamics and phytoplankton size structure in the central-eastern Yellow Sea -
dc.type Article -
dc.citation.title Science of the Total Environment -
dc.citation.volume 807 -
dc.contributor.alternativeName 이연정 -
dc.contributor.alternativeName 최동한 -
dc.contributor.alternativeName 이호원 -
dc.contributor.alternativeName 현명진 -
dc.contributor.alternativeName 김기영 -
dc.contributor.alternativeName 이하은 -
dc.contributor.alternativeName 양원석 -
dc.contributor.alternativeName 김지훈 -
dc.contributor.alternativeName 원종석 -
dc.contributor.alternativeName 나공태 -
dc.contributor.alternativeName 정혜령 -
dc.contributor.alternativeName 최진영 -
dc.contributor.alternativeName 이석 -
dc.contributor.alternativeName 김문구 -
dc.contributor.alternativeName 노재훈 -
dc.identifier.bibliographicCitation Science of the Total Environment, v.807 -
dc.identifier.doi 10.1016/j.scitotenv.2021.151781 -
dc.identifier.scopusid 2-s2.0-85120037848 -
dc.identifier.wosid 000740225700015 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.subject.keywordPlus PARALLEL FACTOR-ANALYSIS -
dc.subject.keywordPlus TO-CHLOROPHYLL RATIO -
dc.subject.keywordPlus STABLE-ISOTOPE -
dc.subject.keywordPlus MARGINAL SEAS -
dc.subject.keywordPlus RIVER ESTUARY -
dc.subject.keywordPlus ARABIAN SEA -
dc.subject.keywordPlus CHINA-SEA -
dc.subject.keywordPlus CARBON -
dc.subject.keywordPlus NITROGEN -
dc.subject.keywordPlus MARINE -
dc.subject.keywordAuthor Yellow Sea -
dc.subject.keywordAuthor Physical-biogeochemical interactions -
dc.subject.keywordAuthor Hydrodynamics -
dc.subject.keywordAuthor Stable isotope ratio -
dc.subject.keywordAuthor PARAFAC -
dc.relation.journalWebOfScienceCategory Environmental Sciences -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Environmental Sciences & Ecology -
Appears in Collections:
Marine Environmental & Climate Research Division > Marine Ecosystem Research Center > 1. Journal Articles
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 1. Journal Articles
Marine Environmental & Climate Research Division > Marine Environmental Research Center > 1. Journal Articles
South Sea Research Institute > Risk Assessment Research Center > 1. Journal Articles
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