XU Zhaokai, CUI Zhenyong, LIN Dongri, LI Tiegang, LI Anchun. PROVENANCE CHANGE OF HOLOCENE SEDIMENTS UNDER INFLUENCE OF THE TSUSHIMA WARM CURRENT ON THE SOUTHWESTERN SLOPE OF JAPAN SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 97-103. DOI: 10.3724/SP.J.1140.2011.04097
Citation: XU Zhaokai, CUI Zhenyong, LIN Dongri, LI Tiegang, LI Anchun. PROVENANCE CHANGE OF HOLOCENE SEDIMENTS UNDER INFLUENCE OF THE TSUSHIMA WARM CURRENT ON THE SOUTHWESTERN SLOPE OF JAPAN SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 97-103. DOI: 10.3724/SP.J.1140.2011.04097
shu

PROVENANCE CHANGE OF HOLOCENE SEDIMENTS UNDER INFLUENCE OF THE TSUSHIMA WARM CURRENT ON THE SOUTHWESTERN SLOPE OF JAPAN SEA

  • 1 Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;

  • 2 Department of Oceanography, Kunsan National University, Kunsan 573-701, Korea;

  • 3 South Sea Institute, Korea Ocean Research and Development Institute, Geoje 656-830, Korea

More Information
  • Received Date: March 09, 2011
  • Revised Date: April 01, 2011
    Graphical Abstract
    • Abstract
  • Synthetic analyses on typical element ratio and source discrimination function were carried out for a sediment core with high sedimentary rate collected along the Tsushima Warm Current (TWC) main stream on the southwestern slope of Japan Sea, in order to trace the sediment provenance change of the study area in the Holocene. Data suggest that the Nakdong River of Korea and Changjiang of China are the main source of the studied sediments. Affected by the TWC strength evolution and sea level rise, their contributions changed with time. There are five stages. In the early Holocene (9.6-6.5 kaBP), especially during the two Melt Water Pulse (MWP) stages including MWP-1C (9.4-8.7 kaBP) and MWP-1D (7.8-7.4 kaBP), the contribution of these rivers was high. Their contribution became lower during 6.5-3.0 kaBP and 2.0-0.7 kaBP, corresponding to the temporally weakening of TWC in the northern East China Sea and southwestern Japan Sea. In 3.0-2.0 kaBP and 0.7-0 kaBP, TWC was strengthened and more fluvial materials from the Nakdong River and Changjiang River were deposited in the study area.
    • FullText(HTML)
    • References (29)
  • [1]
    崔琰琳,吴德星,兰健.日本海环流研究综述[J].海洋科学进展,2006,24(4):577-592.

    [CUI Yanlin,WU Dexing,LAN Jian.Review of study on circulation in the Japan Sea[J].Advances in Marine Science,2006,24(4):577-592.]
    [2]
    Hsueh Y,Lie H J,Ichikawa H.On the branching of the Kuroshio west of Kyushu[J].Journal of Geophysical Research,1996,101(C2):3851-3857.
    [3]
    Liu J P,Xu K H,Li A C,et al.Flux and fate of Yangtze River sediment delivered to the East China Sea[J].Geomorphology,2007,85:208-224.[4 Park S C,Yoo D G,Lee K W,et al.Accumulation of recent muds associated with coastal circulations,southeastern Korea Sea (Korea Strait)[J].Continental Shelf Research,1999,19:589-608.
    [5]
    Bahk J J,Han S J,Khim B K.Variations of terrigenous sediment supply to the southern slope of the Ulleung Basin,East/Japan Sea since the Last Glacial Maximum[J].Geoscience Journal,2004,8:381-390.
    [6]
    Yang S Y,Jung H S,Lim D I,et al.A review on the provenance discrimination of sediments in the Yellow Sea[J].Earth-Science Reviews,2003,63:93-120.
    [7]
    Lim D I,Jung H S,Choi J Y,et al.Geochemical compositions of river and shelf sediments in the Yellow Sea:Grain-size normalization and sediment provenance[J].Continental Shelf Research,2006,26:15-24.
    [8]
    Cha H J,Choi M S,Lee C B,et al.Geochemistry of surface sediments in the southwestern East/Japan Sea[J].Journal of Asian Earth Sciences,2007,29:685-697.
    [9]
    Xu Z K,Lim D I,Choi J Y,et al.Rare earth elements in bottom sediments of major rivers around the Yellow Sea:implications for sediment provenance[J].Geo-Marine Letters,2009,29:291-300.
    [10]
    徐兆凯,崔镇勇,林东日,等.日本海西南陆坡全新世对马暖流演化的沉积学和地球化学记录[J].海洋地质与第四纪地质,2010,30(1):55-64.

    [XU Zhaokai,CHOI Jinyong,LIM Dhongil,et al.Evolution of the Tsushima Warm Current during the Holocene:Sedimentological and geochemical records on the southwestern slope of East/Japan Sea[J].Marine Geology and Quaternary Geology,2010,30(1):55-64.]
    [11]
    刘焱光,石学法,吕海龙.日本海、鄂霍次克海和白令海的古海洋学研究进展[J].海洋科学进展,2004,22(4):519-530.

    [LIU Yanguang,SHI Xuefa,L Hailong.Advances in paleoceanographic studies on the Japan Sea,Okhotsk Sea and Bering Sea[J].Advances in Marine Science,2004,22(4):519-530.]
    [12]
    Khim B K,Park Y H,Bahk J J,et al.Spatial and temporal variation of geochemical properties and paleoceanographic implications in the South Korea Plateau (East Sea) during the late Quaternary[J].Quaternary International,2008,176-177:4661.
    [13]
    Li T G,Sun R T,Zhang D Y,et al.Evolution and variation of the Tsushima warm current during the late Quaternary:Evidence from planktonic foraminifera,oxygen and carbon isotopes[J].Science in China Series D:Earth Sciences,2007,50(5):725-735.
    [14]
    Lie H J,Cho C H.Recent advances in understanding the circulation and hydrography of the East China Sea[J].Fisheries Oceanography,2002,11:318-328.
    [15]
    Gaillardet J,Dupre'B,Alle`gre C J.Geochemistry of large river suspended sediments:silicate weathering or recycling tracer[J]Geochimica et Cosmochimica Acta,1999,63:4037-4051.
    [16]
    Choi M S,Cho Y G.Element geochemistry of suspended sediments in the Korean rivers:the Han,the Geum,the Mangyeong,the Yeongsan,the Seomjin and the Nakdong River[C]//Proceedings of the 5th International Symposium of Marine Sciences of the Yellow Sea (ISMY-V).Incheon,Korea,2001.
    [17]
    杨守业,李从先.长江与黄河沉积物REE地球化学及示踪作用[J].地球化学,1999,28(4):374-380.

    [YANG Shouye,LI Congxian.REE geochemistry and tracing application in the Yangtze River and the Yellow River sediments[J].Geochimica,1999,28(4):374-380.]
    [18]
    Lee J I,Lee Y I.Geochemistry and provenance of Lower Cretaceous Sindong and Hayang mudrocks,Gyeongsang Basin,Southeastern Korea[J].Geosciences Journal,2003,7(2):107-122.
    [19]
    李双林,李绍全,孟祥君.东海陆架晚第四纪沉积物化学成分及物源示踪[J].海洋地质与第四纪地质,2002,22(4):21-28.

    [LI Shunlin,LI Shaoquan,MENG Xianglin.Chemical composition and source tracing of late Quaternary sediments in the East China Sea shelf[J].Marine Geology and Quaternary Geology,2002,22(4):21-28.]
    [20]
    Shinjo R,Kato Y.Geochemical constraints on the origin of bimodal magmatism at the Okinawa Trough,an incipient backarc basin.Lithos,2000,54:118-137.
    [21]
    刘娜,孟宪伟.冲绳海槽中段表层沉积物中稀土元素组成及其物源指示意义[J].海洋地质与第四纪地质,2004,24(4):37-43.

    [LU Na,MENG Xianwei.Characteristics of rare earth elements in surface sediments from the middle Okinawa Trough:implications for provenance of mixed sediments[J].Marine Geology and Quaternary Geology,2004,24(4):37-43.]
    [22]
    杨守业,Jung H S,李从先,等.黄河、长江和韩国Keum、Yeongsan江沉积物常量元素地球化学特征[J].地球化学,2004,33(1):99-105.

    [YANG Shouye,JUNG Hoisoo,Li Congxian,el a1.Major element geochemistry of sediments from Chinese and Korean rivers[J].Geoehimica,2004,33(1):99-105.]
    [23]
    杨守业,李从先,Jung H S,等.中韩河流沉积物微量元素地球化学研究[J].海洋地质与第四纪地质,2003,23(2):19-24.

    [YANG Shouye,LI Congxian,JUNG Hoisoo,el al.Geochemistry of trace elements in Chinese and Korean river sediments[J].Marine Geology&Quaternary Geology,2003,23(2):19-24.]
    [24]
    Liu J P,Milliman J D,Gao S,et al.Holocene development of the Yellow River's subaqueous delta,North Yellow Sea[J].Marine Geology,2004,209:45-67.
    [25]
    Li C X,Chen Q Q,Zhang J Q,et al.Stratigraphy and paleoenvironmental changes in the Yangtze Delta during the Late Quaternary[J].Journal of Asian Earth Sciences,2000,18:453-469.
    [26]
    王可,郑洪波,Prins M,等.东海内陆架泥质沉积反映的古环境演化[J].海洋地质与第四纪地质,2008,28(4):1-10.

    [WANG Ke,ZHENG Hongbo,Prins M,et al.High-resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf[J].Marine Geology and Quaternary Geology,2008,28(4):1-10.]
    [27]
    Gorbarenko S A,Southon J R.Detailed Japan Sea paleoceanography during the last 25 kyr:constraints from AMS dating and δ18O of planktonic foraminifera[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2000,156:177-193.
    [28]
    Domitsu H,Oda M.Linkages between surface and deep circulations in the southern Japan Sea during the last 27000 years:Evidence from planktic foraminiferal assemblages and stable isotope records[J].Marine Micropaleontology,2006,61:155-170.
    [29]
    Fairbanks R G.A 17,000 year glacio eustatic sea level record:influence of glacial melting rates on the Younger Dryas event and deep ocean circulation[J].Nature,1989,342:637-642.
    [30]
    李铁刚,江波,孙荣涛,等.末次冰消期以来东黄海暖流系统的演化[J].第四纪研究,2007,27(6):945-954.

    [LI Tiegang,JIANG Bo,SUN Rongtao,et al.Evolution pattern of warm current system of the East China Sea and the Yellow Sea since the last deglaciation[J].Quaternary Sciences,2007,27(6):945-954.]
    • Related Articles

  • Related Articles

    [1]FANG Liangcong, ZOU Jianjun, DOU Ruxi, WANG Qingchao, ZHU Aimei, Gorbarenko Sergey, Vasilenko Yuriy, Bosin Aleksandr, SHI Xuefa. Evolution of sedimentary arsenic in the western Sea of Japan over the last 3 0000 years and its paleoenvironmental significance[J]. Marine Geology & Quaternary Geology, 2025, 45(2): 1-11. DOI: 10.16562/j.cnki.0256-1492.2024121101
    [2]FANG Xiaorong, HU Ningjing, DOU Ruxi, ZHANG Ying, ZHANG Hui, LIU Jihua. Provenance evolution since Middle Holocene of the sediments on the East Siberian shelf: Evidence from elemental geochemistry[J]. Marine Geology & Quaternary Geology, 2021, 41(4): 60-73. DOI: 10.16562/j.cnki.0256-1492.2020122701
    [3]SHI Xuefa, ZOU Jianjun, YAO Zhengquan, DOU Ruxi, Gorbarenko Sergey. Sedimentation and environment evolution of the Sea of Japan since the Last Glaciation and its driving forces[J]. Marine Geology & Quaternary Geology, 2019, 39(3): 1-11. DOI: 10.16562/j.cnki.0256-1492.2019050801
    [4]GONG Jianming, LIAO Jing, HE Yongjun, YANG Chuansheng, SUN Zhilei, CHEN Zhiqiang, CHEN Qingsong. DISCUSSION ON GAS ORIGINS AND MAIN CONTROLLING FACTORS FOR GAS HYDRATES IN THE SEA OF JAPAN[J]. Marine Geology & Quaternary Geology, 2017, 37(5): 102-108. DOI: 10.16562/j.cnki.0256-1492.2017.05.010
    [5]ZHAO Xilin, YU Shengyao, LI Sanzhong, PENG Yinbiao, JIANG Yang, XING Guangfu, YU Minggang, LIU Kai. Differences in Mesozoic Magmatism Between Southeast China and Japan[J]. Marine Geology & Quaternary Geology, 2017, 37(4): 65-82. DOI: 10.16562/j.cnki.0256-1492.2017.04.004
    [6]SHEN Xingyan, WAN Shiming. RESEARCH PROGRESS OF QUATERNARY DEPOSITIONAL RECORDS OF THE JAPAN SEA AND ITS IMPLICATIONS FOR THE LINKAGES TO THE ASIAN CONTINENT[J]. Marine Geology & Quaternary Geology, 2015, 35(6): 139-151. DOI: 10.16562/j.cnki.0256-1492.2015.06.015
    [7]ZOU Jianjun, SHI Xuefa, LIU Yanguang, LIU Jihua. GEOCHEMICAL RECORD OF TERRIGENOUS SEDIMENTS FROM THE SEA OF JAPAN SINCE LAST GLACIAL AND ITS RESPONSE TO SEA LEVEL AND CLIMATE CHANGE[J]. Marine Geology & Quaternary Geology, 2010, 30(2): 75-86. DOI: 10.3724/SP.J.1140.2010.02075
    [8]XU Zhaokai, CHOI Jinyong, LIM Dhongil, LI Tiegang, LI Anchun. EVOLUTION OF THE TSUSHIMA WARM CURRENT DURING THE HOLOCENE: SEDIMENTOLOGICAL AND GEOCHEMICAL RECORDS ON THE SOUTHWESTERN SLOPE OF EAST/JAPAN SEA[J]. Marine Geology & Quaternary Geology, 2010, 30(1): 55-64. DOI: 10.3724/SP.J.1140.2010.01055
    [9]LIU Yanguang, ZOU Jianjun, LI Chaoxin, ZHANG Weibin, SHI Xuefa, Suk Bong-Chool. THE LAST GLACIATION MAXIMUM IN THE SEA OF JAPAN/EAST SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(4): 53-63. DOI: 10.3724/SP.J.1140.2009.04053
    [10]XU Zhaokai, CHOI Jinyong, LIM Dhongil, LI Tiegang, LI Anchun. CHARACTER AND ORIGIN OF AUTHIGENIC CARBONATES IN THE WESTERN CONTINENTAL SLOPE OF THE EAST JAPAN SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 41-47. DOI: 10.3724/SP.J.1140.2009.02041

Catalog

    Get Citation
    PDF
    XML
    Article views (2095) PDF downloads (19) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return