IOCAS-IR  > 海洋地质与环境重点实验室
A Comprehensive Investigation of Coastal and Shelf Sediment Sources in the South Sea of Korea: A Marginal Sea of the Northwestern Pacific
Lim, Dhongil1; Cho, Yeong-Gil2; Jeong, Dohyun1; Kim, Jihun1; Xu, Zhaokai3; Chang, Taesoo4
2023-12-01
发表期刊OCEAN SCIENCE JOURNAL
ISSN1738-5261
卷号58期号:4页码:12
通讯作者Lim, Dhongil(oceanlim@kiost.ac.kr)
摘要To identify and quantify the sediment sources in the South Sea of Korea, a marginal sea of the northwestern Pacific, we analyzed a comprehensive aluminum-magnesium dataset comprising 121 surface sediment samples and two sediment cores. The findings demonstrate pronounced spatial variation in sediment sources, with Korean river sediments dominating in embayment bays and Chinese river sediments prevailing in the shelf area. In the coastal zone, Korean river sediments account for over 60-70%, but their proportion decreased to 10-20% in the shelf zone. This reveals that most of the sediments from Korean rivers are mainly confined to the coastal embayments, with limited transport to the shelf area. Notably, the central South Sea mud (CSSM) deposits are primarily govern by the sediment influx from Chinese rivers (CR), rather than the Seomjin River discharge. The prevalence of CR-sourced sediments in the shelf region is closely linked to the Tsushima Warm Current and Cheju Warm Current, transporting sediments from the East China Sea shelf northwards and the southwestern Korean coastal zone eastwards, respectively. This driving mechanism for the widespread deposition of CR sediments is further supported by an abrupt shift from KR to CR dominance in sediment sources around 8 kyr BP, coinciding with the establishment of the modern current systems in the northwestern Pacific marginal seas. Our study provides a new perspective on the source-to-sink pathways, particularly of Chinese river sediments, in the formation of the Korean coastal mud deposits.
关键词Sediment provenance Quantification Mud depositions Kuroshio Current South Sea of Korea
DOI10.1007/s12601-023-00121-2
收录类别SCI
语种英语
资助项目This work was supported by National Research Foundation of Korea (grant no. NRF-2022R1A2C1006208) and Korea Institute of Marine Science amp; Technology (KIMST) funded by the Ministry of Oceans and Fisheries (RS-2023-00256330, Development of risk managing[NRF-2022R1A2C1006208] ; National Research Foundation of Korea[RS-2023-00256330] ; Korea Institute of Marine Science amp; Technology (KIMST) - Ministry of Oceans and Fisheries ; Library of Marine Sample (LIMS), Korea Institute of Ocean Science and Technology (KIOST)
WOS研究方向Marine & Freshwater Biology ; Oceanography
WOS类目Marine & Freshwater Biology ; Oceanography
WOS记录号WOS:001076512000001
出版者KOREA INST OCEAN SCIENCE & TECHNOLOGY-KIOST
WOS关键词SOUTHEASTERN YELLOW SEA ; NORTHERN OKINAWA TROUGH ; EAST CHINA SEA ; CLAY MINERAL DISTRIBUTION ; LATE QUATERNARY DEPOSITS ; LAST GLACIAL MAXIMUM ; PALEO-SEOMJIN RIVER ; PROVENANCE DISCRIMINATION ; CONTINENTAL-SHELF ; SURFACE SEDIMENTS
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文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/181683
专题海洋地质与环境重点实验室
通讯作者Lim, Dhongil
作者单位1.Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 53201, South Korea
2.Mokpo Natl Univ, Dept Fisheries & Marine Resources, Mokpo 58554, South Korea
3.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
4.Chonnam Natl Univ, Dept Geol & Environm Sci, Gwangju 61186, South Korea
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Lim, Dhongil,Cho, Yeong-Gil,Jeong, Dohyun,et al. A Comprehensive Investigation of Coastal and Shelf Sediment Sources in the South Sea of Korea: A Marginal Sea of the Northwestern Pacific[J]. OCEAN SCIENCE JOURNAL,2023,58(4):12.
APA Lim, Dhongil,Cho, Yeong-Gil,Jeong, Dohyun,Kim, Jihun,Xu, Zhaokai,&Chang, Taesoo.(2023).A Comprehensive Investigation of Coastal and Shelf Sediment Sources in the South Sea of Korea: A Marginal Sea of the Northwestern Pacific.OCEAN SCIENCE JOURNAL,58(4),12.
MLA Lim, Dhongil,et al."A Comprehensive Investigation of Coastal and Shelf Sediment Sources in the South Sea of Korea: A Marginal Sea of the Northwestern Pacific".OCEAN SCIENCE JOURNAL 58.4(2023):12.
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