ZOU Liang, DOU Yanguang, CHEN Xiaohui, HU Bangqi, LIN Xi. Provenance analysis for surface sediments in different depositional environments of the middle-south Okinawa Trough[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 115-124. DOI: 10.16562/j.cnki.0256-1492.2020082001
Citation: ZOU Liang, DOU Yanguang, CHEN Xiaohui, HU Bangqi, LIN Xi. Provenance analysis for surface sediments in different depositional environments of the middle-south Okinawa Trough[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 115-124. DOI: 10.16562/j.cnki.0256-1492.2020082001
shu

Provenance analysis for surface sediments in different depositional environments of the middle-south Okinawa Trough

  • 1.

    Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Natural Resources, China Geology Survey, Qingdao Institute of Marine Geology, Qingdao 266071,China

  • 2.

    Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China

More Information
  • Received Date: August 19, 2020
  • Revised Date: December 14, 2020
  • Available Online: February 28, 2021
    Graphical Abstract
    • Abstract
  • In this paper, surface sediments taken from three different depositional environments, i.e. the outer continental shelf, slope, and trough, of the middle-south Okinawa Trough were analyzed for rare earth elements (REE). The results suggest that the REE distribution patterns of the surface sediments from the continental slope and the Okinawa Trough are quite similar to those from Taiwan. The discrimination plot of La/Sm-Gd/Yb also shows that the surface sediments from continental slope and the Okinawa Trough are mainly located in the diagram close to the provenance end of Taiwan, further supporting the conclusion that the surface sediments of the continental slope and the Okinawa Trough are doubtlessly sourced from Taiwan. The obvious loss of heavy REE in the sediments of the outer continental shelf is consistent with the source of continental river sediments. In order to recognize the source of surface sediments in the outer shelf sedimentary area, the heavy mineral compositions of these sediments were analyzed. The results show that the heavy mineral assemblages of the outer continental shelf sediments are mainly composed of common hornblende, epidote, garnet, limonite, similar to the source composition of the Changjiang river. The outer continental shelf sediments are lack of zircon, mica, and magnetite, typical heavy minerals found in Taiwan, Huanghe river, and Minjiang river sediments respectively, which suggests that Taiwan, Yellow River, and the coast of Zhejiang and Fujian are not the main contributors to the outer continental shelf sediments. According to the results of previous dating data, the sediments of the outer shelf are relatively old, suggesting that the outer shelf sediments should be formed by the rework of the palaeo-Changjiang river materials by the modern circulation system of the East China Sea.
    • FullText(HTML)
    • References (47)
  • [1]
    Milliman J D, Shen H T, Yang Z S, et al. Transport and deposition of river sediment in the Changjiang estuary and adjacent continental shelf [J]. Continental Shelf Research, 1985, 4(1-2): 37-45. doi: 10.1016/0278-4343(85)90020-2
    [2]
    杨文达, 王振宇, 曾久岭. 冲绳海槽轴线地质特征[J]. 海洋地质与第四纪地质, 2001, 21(2):1-6. [YANG Wenda, WANG Zhenyu, ZENG Jiuling. Geologic features of the Okinawa trough Axis [J]. Marine Geology & Quaternary Geology, 2001, 21(2): 1-6.
    [3]
    赵月霞, 刘保华, 李西双, 等. 东海陆坡海底峡谷—扇体系沉积特征及物质搬运[J]. 古地理学报, 2011, 13(1):119-126. [ZHAO Yuexia, LIU Baohua, LI Xishuang, et al. Sedimentary characters and material transportation of submarine canyon-fan systems in slope of the East China Sea [J]. Journal of Palaeogeography, 2011, 13(1): 119-126. doi: 10.7605/gdlxb.2011.01.012
    [4]
    Milliman J D, Qin Y S, Park Y A. Sediments and sedimentary processes in the Yellow and East China Seas[M]//Taira A, Masuda F. Sedimentary Facies in the Active Plate Margin. Tokyo: Terra Scientific Publishing Company, 1989: 233-249.
    [5]
    Saito Y, Katayama H, Ikehara K, et al. Transgressive and highstand systems tracts and post-glacial transgression, the East China Sea [J]. Sedimentary Geology, 1998, 122(1-4): 217-232. doi: 10.1016/S0037-0738(98)00107-9
    [6]
    Yoo D G, Lee C W, Kim S P, et al. Late Quaternary transgressive and highstand systems tracts in the northern East China Sea mid-shelf [J]. Marine Geology, 2002, 187(3-4): 313-328. doi: 10.1016/S0025-3227(02)00384-5
    [7]
    Liu Z X, Berné S, Saito Y, et al. Internal architecture and mobility of tidal sand ridges in the East China Sea [J]. Continental Shelf Research, 2007, 27(13): 1820-1834. doi: 10.1016/j.csr.2007.03.002
    [8]
    Dou Y G, Yang S Y, Liu Z X, et al. Provenance discrimination of siliciclastic sediments in the middle Okinawa Trough since 30 ka: Constraints from rare earth element compositions [J]. Marine Geology, 2010, 275(1-4): 212-220. doi: 10.1016/j.margeo.2010.06.002
    [9]
    Jian Z M, Wang P X, Saito Y, et al. Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean [J]. Earth and Planetary Science Letters, 2000, 184(1): 305-319. doi: 10.1016/S0012-821X(00)00321-6
    [10]
    郭志刚, 杨作升, 雷坤, 等. 冲绳海槽中南部及其邻近陆架悬浮体的分布、组成和影响因子分析[J]. 海洋学报, 2001, 23(1):66-72. [GUO Zhigang, YANG Zuosheng, LEI Kun, et al. The distribution and composition of suspended matters and their influencing factors in the central-southern area of Okinawa Trough and its adjacent shelf sea [J]. Acta Oceanologica Sinica, 2001, 23(1): 66-72.
    [11]
    杨宝菊, 吴永华, 刘季花, 等. 冲绳海槽表层沉积物元素地球化学及其对物源和热液活动的指示[J]. 海洋地质与第四纪地质, 2018, 38(2):25-37. [YANG Baoju, WU Yonghua, LIU Jihua, et al. Elemental geochemistry of surface sediments in Okinawa Trough and its implications for provenance and hydrothermal activity [J]. Marine Geology & Quaternary Geology, 2018, 38(2): 25-37.
    [12]
    胡思谊, 曾志刚, 殷学博, 等. 冲绳海槽岩心沉积物稀土元素特征及物源指示[J]. 海洋地质与第四纪地质, 2018, 39(1):69-82. [HU Siyi, ZENG Zhigang, YIN Xuebo, et al. Characteristics of rare earth elements in the sediment cores from the Okinawa Trough and their implications for sediment provenance [J]. Marine Geology and Quaternary Geology, 2018, 39(1): 69-82.
    [13]
    窦衍光, 陈晓辉, 李军, 等. 东海外陆架-陆坡-冲绳海槽不同沉积单元底质沉积物成因及物源分析[J]. 海洋地质与第四纪地质, 2018, 38(4):21-31. [DOU Yanguang, CHEN Xiaohui, LI Jun, et al. Origin and provenance of the surficial sediments in the subenvironments of the East China Sea [J]. Marine Geology & Quaternary Geology, 2018, 38(4): 21-31.
    [14]
    McLennan S M. Rare earth elements in sedimentary rocks; influence of provenance and sedimentary processes [J]. Reviews in Mineralogy and Geochemistry, 1989, 21(1): 169-200.
    [15]
    Vital H, Stattegger K, Garbe-Schonberg C D. Composition and trace-element geochemistry of detrital clay and heavy-mineral suites of the lowermost Amazon River: a provenance study [J]. Journal of Sedimentary Research, 1999, 69(3): 563-575. doi: 10.2110/jsr.69.563
    [16]
    Xu Z K, Li T G, Chang F M, et al. Sediment provenance discrimination in northern Okinawa Trough during the last 24 ka and paleoenvironmental implication: rare earth elements evidence [J]. Journal of Rare Earths, 2012, 30(11): 1184-1190. doi: 10.1016/S1002-0721(12)60202-6
    [17]
    Machida H. The stratigraphy, chronology and distribution of distal marker-tephras in and around Japan [J]. Global and Planetary Change, 1999, 21(1-3): 71-94. doi: 10.1016/S0921-8181(99)00008-9
    [18]
    翟世奎, 于增慧, 杜同军. 冲绳海槽中部现代海底热液活动在沉积物中的元素地球化学记录[J]. 海洋学报, 2007, 29(1):58-65. [ZHAI Shikui, YU Zenghui, DU Tongjun. Elemental geochemical records of modern seafloor hydrothermal activities in sediments from the central Okinawa Trough [J]. Acta Oceanologica Sinica, 2007, 29(1): 58-65.
    [19]
    Iseki K, Okamura K, Kiyomoto Y. Seasonality and composition of downward particulate fluxes at the continental shelf and Okinawa Trough in the East China Sea [J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2003, 50(2): 457-473. doi: 10.1016/S0967-0645(02)00468-X
    [20]
    Katayama H, Watanabe Y. The Huanghe and Changjiang contribution to seasonal variability in terrigenous particulate load to the Okinawa Trough [J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2003, 50(2): 475-485. doi: 10.1016/S0967-0645(02)00469-1
    [21]
    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(3-4): 208-224. doi: 10.1016/j.geomorph.2006.03.023
    [22]
    Yang S Y, Wang Z B, Dou Y G, et al. A review of sedimentation since the last glacial maximum on the continental shelf of Eastern China [J]. Geological Society, London, Memoirs, 2014, 41(1): 293-303. doi: 10.1144/M41.21
    [23]
    张丹丹, 曾志刚, 殷学博. 冲绳海槽中部沉积物物质来源和沉积环境分析[J]. 海洋学报, 2017, 39(7):92-101. [ZHANG Dandan, ZENG Zhigang, YIN Xuebo. Analysis on sediment provenance and environmental changes in the middle Okinawa Trough [J]. Acta Oceanologica Sinica, 2017, 39(7): 92-101.
    [24]
    Taylor S R, McClennan S M. The Continental Crust: Its Composition and Evolution[M]. Blackwell, Oxford: Blackwell Scientific Publications, 1985: 1-190.
    [25]
    Sholkovitz E R, Elderfield H, Szymczak R, et al. Island weathering: river sources of rare earth elements to the Western Pacific Ocean [J]. Marine Chemistry, 1999, 68(1-2): 39-57. doi: 10.1016/S0304-4203(99)00064-X
    [26]
    Piper D Z, Bau M. Normalized rare earth elements in water, sediments, and wine: identifying sources and environmental redox conditions [J]. American Journal of Analytical Chemistry, 2013, 4(10A): 69-83.
    [27]
    Yang S Y, Jung H S, Choi M S, et al. The rare earth element compositions of the Changjiang (Yangtze) and Huanghe (Yellow) river sediments [J]. Earth and Planetary Science Letters, 2002, 201(2): 407-419. doi: 10.1016/S0012-821X(02)00715-X
    [28]
    Chen J C, Lo C Y, Lee Y T, et al. Mineralogy and chemistry of cored sediments from active margin off southwestern Taiwan [J]. Geochemical Journal, 2007, 41(5): 303-321. doi: 10.2343/geochemj.41.303
    [29]
    尚鲁宁, 陈磊, 张训华, 等. 冲绳海槽南部海底热液活动区地形地貌特征及成因分析[J]. 海洋地质与第四纪地质, 2017, 39(4):12-22. [SHANG Luning, CHEN Lei, ZHANG Xunhua, et al. Topographic features of the hydrothermal field and their genetic mechanisms in southern Okinawa Trough [J]. Marine Geology & Quaternary Geology, 2017, 39(4): 12-22.
    [30]
    蔡宗伟, 翟世奎, 于增慧, 等. 冲绳海槽中、南部热液活动区金属硫化物的地球化学特征[J]. 海洋科学, 2018, 42(11):73-82. [CAI Zongwei, ZHAI Shikui, YU Zenghui, et al. Geochemical characteristics of hydrothermal sulfide from the middle and southern hydrothermal fields in the Okinawa Trough [J]. Marine Sciences, 2018, 42(11): 73-82. doi: 10.11759/hykx20161215001
    [31]
    金贵娥, 洪小燕, 汪厦霞, 等. 九龙江河口区稀土元素地球化学特征[J]. 台湾海峡, 2010, 29(3):304-313. [JIN Guie, HONG Xiaoyan, WANG Xiaxia, et al. Geochemical characteristics of rare earth elements in Jiulongjiang Estuary [J]. Journal of Oceanography in Taiwan Strait, 2010, 29(3): 304-313.
    [32]
    Shinjo R, Kato Y. Geochemical constraints on the origin of bimodal magmatism at the Okinawa Trough, an incipient back-arc basin [J]. Lithos, 2000, 54(3-4): 118-137.
    [33]
    Dou Y G, Yang S Y, Shi X F, et al. Provenance weathering and erosion records in southern Okinawa Trough sediments since 28 ka: Geochemical and Sr–Nd–Pb isotopic evidences [J]. Chemical Geology, 2016, 425: 93-109. doi: 10.1016/j.chemgeo.2016.01.029
    [34]
    Wang J Z, Li A C, Xu K H, et al. Clay mineral and grain size studies of sediment provenances and paleoenvironment evolution in the middle Okinawa Trough since 17 ka [J]. Marine Geology, 2015, 366: 49-61. doi: 10.1016/j.margeo.2015.04.007
    [35]
    Chen C T A, Kandasamy S, Chang Y P, et al. Geochemical evidence of the indirect pathway of terrestrial particulate material transport to the Okinawa Trough [J]. Quaternary International, 2016, 441: 51-61.
    [36]
    陈静, 王哲, 王张华, 等. 长江三角洲东西部晚新生代地层中的重矿物差异及其物源意义[J]. 第四纪研究, 2007, 27(5):700-708. [CHEN Jing, WANG Zhe, WANG Zhanghua, et al. Heavy mineral distribution and its provenance implication in late Cenozoic sediments in western and eastern area of the Changjiang river delta [J]. Quaternary Sciences, 2007, 27(5): 700-708. doi: 10.3321/j.issn:1001-7410.2007.05.011
    [37]
    张凯棣, 李安春, 董江, 等. 东海表层沉积物碎屑矿物组合分布特征及其物源环境指示[J]. 沉积学报, 2016, 34(5):902-911. [ZHANG Kaili, LI Anchun, DONG Jiang, et al. Detrital mineral distributions in surface sediments of the East China Sea: implications for sediment provenance and sedimentary environment [J]. Acta Sedimentologica Sinica, 2016, 34(5): 902-911.
    [38]
    Garzanti E, Andò S. Plate tectonics and heavy mineral suites of modern sands [J]. Developments in Sedimentology, 2007, 58: 741-763. doi: 10.1016/S0070-4571(07)58029-5
    [39]
    Heroy D C, Kuehl S A, Goodbred S L Jr. Mineralogy of the Ganges and Brahmaputra Rivers: implications for river switching and Late Quaternary climate change [J]. Sedimentary Geology, 2003, 155(3-4): 343-359. doi: 10.1016/S0037-0738(02)00186-0
    [40]
    王中波, 杨守业, 李萍, 等. 长江水系沉积物碎屑矿物组成及其示踪意义[J]. 沉积学报, 2006, 24(4):570-578. [WANG Zhongbo, YANG Shouye, LI Ping, et al. Detrital mineral compositions of the Changjiang River sediments and their tracing implications [J]. Acta Sedimentologica Sinica, 2006, 24(4): 570-578. doi: 10.3969/j.issn.1000-0550.2006.04.015
    [41]
    窦衍光, 王昆山, 王国庆, 等. 长江水下三角洲沉积物碎屑矿物研究[J]. 海洋科学, 2007, 31(4):22-26, 31. [DOU Yanguang, WANG Kunshan, WANG Guoqing, et al. Research of detrital minerals in the sediment of sub-aqueous Yangtze Delta [J]. Marine Sciences, 2007, 31(4): 22-26, 31. doi: 10.3969/j.issn.1000-3096.2007.04.006
    [42]
    Yang S Y, Wang Z B, Guo Y, et al. Heavy mineral compositions of the Changjiang (Yangtze River) sediments and their provenance-tracing implication [J]. Journal of Asian Earth Sciences, 2009, 35(1): 56-65. doi: 10.1016/j.jseaes.2008.12.002
    [43]
    林晓彤, 李巍然, 时振波. 黄河物源碎屑沉积物的重矿物特征[J]. 海洋地质与第四纪地质, 2003, 23(3):17-21. [LIN Xiaotong, LI Weiran, SHI Zhenbo. Characteristics of mineralogy in the clastic sediments from the Yellow River Provenance, China [J]. Marine Geology & Quaternary Geology, 2003, 23(3): 17-21.
    [44]
    陈心怡, 黄奇瑜, 邵磊. 福建闽江和九龙江现代沉积物重矿物特征及其物源意义[J]. 古地理学报, 2018, 20(4):637-650. [CHEN Xinyi, HUANG Qiyu, SHAO Lei. Characteristics of heavy minerals in modern sediments of Minjiang and Jiulongjiang Rivers, Fujian Province and their provenance implication [J]. Journal of Palaeogeography, 2018, 20(4): 637-650. doi: 10.7605/gdlxb.2018.04.046
    [45]
    邓凯, 杨守业, 王中波, 等. 台湾山溪性小河流碎屑重矿物组成及其示踪意义[J]. 沉积学报, 2016, 34(3):531-542. [DENG Kai, YANG Shouye, WANG Zhongbo, et al. Detrital heavy mineral assemblages in the river sediments from Taiwan and its implications for sediment provenance [J]. Acta Sedimentologica Sinica, 2016, 34(3): 531-542.
    [46]
    王中波, 杨守业, 张志珣, 等. 东海陆架中北部沉积物粒度特征及其沉积环境[J]. 海洋与湖沼, 2012, 43(6):1039-1049. [WANG Zhongbo, YANG Shouye, ZHANG Zhixun, et al. The grain size compositions of the surface sediments in the East China Sea: Indication for sedimentary environments [J]. Oceanologia et Limnologia Sinica, 2012, 43(6): 1039-1049. doi: 10.11693/hyhz201206003003
    [47]
    陈丽蓉. 中国海沉积矿物学[M]. 北京: 海洋出版社, 2008: 121-155.

    CHEN Lirong. Sedimentary Mineralogy of the China Sea[M]. Beijing: China Ocean Press, 2008: 121-155.
    • Related Articles

  • Related Articles

    [1]YE Fanfan, ZENG Zhigang. States of element occurrence of sediments in the southern Okinawa Trough and its hydrothermal activity[J]. Marine Geology & Quaternary Geology, 2023, 43(5): 160-172. DOI: 10.16562/j.cnki.0256-1492.2023022701
    [2]WU Nengyou, SUN Zhilei, LU Jianguo, CAI Feng, CAO Hong, GENG Wei, LUO Min, ZHANG Xilin, LI Qing, SHANG Luning, WANG Libo, ZHANG Xianrong, XU Cuiling, ZHAI Bin, LI Xin, GONG Jianming, HU Yu, LIN Genmei. Interaction between seafloor cold seeps and adjacent hydrothermal activities in the Okinawa Trough[J]. Marine Geology & Quaternary Geology, 2019, 39(5): 23-35. DOI: 10.16562/j.cnki.0256-1492.2019070102
    [3]HU Siyi, ZENG Zhigang, YIN Xuebo, ZHU Bowen, FANG Xue, QI Haiyan. Characteristics of rare earth elements in the sediment cores from the Okinawa Trough and their implications for sediment provenance[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 69-82. DOI: 10.16562/j.cnki.0256-1492.2017082301
    [4]YANG Baoju, WU Yonghua, LIU Jihua, LIU Yanguang, ZHANG Hui, WANG Xiaojing, LI Li. Elemental geochemistry of surface sediments in Okinawa Trough and its implications for provenance and hydrothermal activity[J]. Marine Geology & Quaternary Geology, 2018, 38(2): 25-37. DOI: 10.16562/j.cnki.0256-1492.2018.02.003
    [5]ZHU Aimei, SHI Xuefa, ZOU Jianjun, WU Yonghua, ZHANG Hui, BAI Yazhi. SEDIMENT PROVENANCE AND FLUXES IN THE NORTHERN OKINAWA TROUGH DURING THE LAST 88 KA[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 1-8. DOI: 10.16562/j.cnki.0256-1492.2015.05.001
    [6]WANG Jiaze, LI Anchun, HUANG Jie. SEDIMENT PROVENANCE AND PALEOENVIRONMENT RECORDS OF THE CENTRAL OKINAWA TROUGH FOR THE LAST 17 000 YEARS[J]. Marine Geology & Quaternary Geology, 2013, 33(6): 105-114. DOI: 10.3724/SP.J.1140.2013.06105
    [7]XU Zhaokai, CHANG Fengming, LI Tiegang, NAN Qingyun, JIANG Fuqing, LI Anchun. PROVENANCE OF SEDIMENTS IN THE NORTHERN OKINAWA TROUGH OVER THE LAST 24 KA: HIGH RESOLUTION RECORD FROM MAJOR ELEMENTS[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 73-82. DOI: 10.3724/SP.J.1140.2012.04073
    [8]LIU Fei-fei, YU Zeng-hui, GAO Yu-hua, ZHAI Shi-kui, ZHANG Ai-bin. SEQUENTIAL EXTRACTION PROCEDURE FOR MARINE SEDIMENTS AND APPLICATION TO THE MIDDLE OKINAWA TROUGH[J]. Marine Geology & Quaternary Geology, 2008, 28(5): 137-144.
    [9]ZENG Zhi-gang, CHEN Li-rong. PRELIMINARY STUDY ON VOLCANIC CRATER IN THE MIDDLE OKINAWA TROUGH[J]. Marine Geology & Quaternary Geology, 2008, 28(3): 31-34.
    [10]LI JUN. SPATIAL AND TEMPORAL VARIATION OF THE SEDIMENTATION RATES IN OKINAWA TROUGH SINCE THE LATE PLEISTOCENE AND THEIR CONTROLLING FACTORS[J]. Marine Geology & Quaternary Geology, 2007, 27(4): 37-43.

Catalog

    Get Citation
    PDF
    XML
    Article views (1734) PDF downloads (53) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

    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