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Clay minerals and geochemistry of the bottom sediments in the northwestern East China Sea

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Abstract

Clay minerals of 34 sediments collected from the northwestern continental shelf of the East China Sea have been determined by X-ray diffraction analysis. The clay mineral distribution is mainly controlled by the sediment source and the dominant circulation pattern. The predominant clay mineral in our study area is illite comprising more than 67% of the whole clay fraction. The highest concentration of illite (>68%) is found in the southeastern offshore parts beyond the reach of terrigenous input from the Jeju Island. It means that these illites are largely transported by the Kuroshio Current from the South China Sea (SCS). Smectite is highly concentrated in the northwest middle part and in the outer-shelf mud patch. It seems to be due to the high supply of smectite transported from China where fine-grained sediments are discharged from modern and ancient Huanghe (Yellow) River. The relatively high abundant kaolinite is likely derived from the Changjiang (Yangtze) River via the Taiwan Warm Current. In contrast, large amounts of chlorite and high chlorite/kaolinite ratios occur in the northwestern area, reflecting the transportation by the Yellow Sea Coastal Current from the southern Yellow Sea. The discrimination diagrams clearly show that the sediments in the northwestern East China Sea are ultimately sourced from Chinese rivers, especially from the Huanghe River, whereas the sediment in the northeast part might come from the Jeju Island. The muddy sediments of the Changjiang River’s submerged delta have much lower 87Sr/86Sr ratios (0.716 2–0.718 0) than those of the Shandong Peninsular mud wedge (0.721 6–0.724 9), which are supposed to be originated from the Huanghe River, suggesting the distribution pattern of 87Sr/86Sr ratios as a new tracer to discriminate the provenance of shelf sediments in the study area. The 87Sr/86Sr ratios of the outer-shelf muddy sediments ranged from 0.7169 to 0.7216 in a wide range and was between those of the Huanghe River and Changjiang River sediments, suggesting multiple sources of the sediment in the area.

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References

  • Aoki, S., K. Oinuma and K. Matsuike, 1983. Clay mineral composition in surface sediments and the concentration of suspended matter of the East China Sea. In: Sedimentation on the Continental Shelf with Special Reference to the East China Sea 2, China Ocean Press, Beijing, p. 440–449.

    Google Scholar 

  • Aoki, S. and K. Oinuma, 1988. The distribution of clay minerals in surface sediments of the Okhotsk Sea to the South China Sea along the Asiatic Continent. Clay Science 7: 73–82.

    Google Scholar 

  • Asahara, Y., T. Tanak, H. Kamioka, and A. Nishmura, 1995. Asian continental nature of 87Sr/86Sr ratios in north central Pacific sediments. Ear. Planet. Lett. 133: 105–116.

    Article  Google Scholar 

  • Beardsley, R. C., R. Limeburner, D. Hu, K. Le, G. A. Cannon and D. J. Pashinski, 1983. Structure of the Changjiang River plume in the East China Sea during June 1980. In: Sedimentation on the Continental Shelf with Special Reference to the East China Sea 2, China Ocean Press, Beijing, p. 243–260.

    Google Scholar 

  • Beardsley, R. C., R. Limeburner, H. Yu and G. A. Cannon, 1985. Discharge of the Changjiang (Yangtze River) into the East China Sea. Cont. Shelf Res. 4: 57–76.

    Article  Google Scholar 

  • Biscaye, P. E., 1965. Mineralogy and sedimentation of recent deep-sea clays in the Atlantic Ocean and adjacent seas and ocean. Geol. Soc. Am. Bull. 76: 803–832.

    Article  Google Scholar 

  • Brindley, G. W. and G. Brown (Ed), 1980. Crystal structures and clay minerals and their X-ray identification, London Mineralogical Society Monograph 5: 495p.

  • Butenko, J., J. D. Milliman, and J. C. Ye, 1985. Geomorphology, shallow structure and geological hazards in the East China Sea. Cont. Shelf Res. 4: 121–141.

    Article  Google Scholar 

  • Byers, S. C., E. L. Mills, and P.I. Stewart, 1978. A comparison of method for determining organic carbon in marine sediments with suggestions for a standard method. Hydrobiology 58: 73–82.

    Article  Google Scholar 

  • Choi, J. H., 1981. Recent clay minerals in the Kunsan estuary and the adjacent continental shelf. M. S. Thesis. Dept. of Oceanography, Seoul Nati. Univ., 52p.

  • Douglas, G. B., C. M. Gray, B. T. Hart and R. Beckett, 1995. A strontium isotopic investigation of the origin of suspended particulate matter (SPM) in the Murray-Darling River system, Australia. Geochim. Cosmochim. Acta. 59: 3 799–3 815.

    Article  Google Scholar 

  • Dasch, E. J., 1969. Isotope in weathering profiles, deep-sea sediments and sedimentary rock, Geochim. Cosmochim. Acta. 33: 1 521–1 552.

    Article  Google Scholar 

  • Datta, D. K. and V. Subramaniam, 1998. Distribution and fractionation of heavy metals in the surface sediments of the Gang-Brahmaputra-Meghna river system in the Bengal basin. Environ. Geol. 36: 93–101.

    Article  Google Scholar 

  • Gibbs, R. J., 1965. Error due to segregation in quantitative clay mineral X-ray diffraction mounting technique. American Mineralogist 50: 741–751.

    Google Scholar 

  • Goldstein, S. J. and S. B. Jacobsen, 1987. The Nd and Sr isotopic systematics of river-water dissolved material: Implications for sources of Nd and Sr in sea water. Chem. Geol. 66: 245–272.

    Google Scholar 

  • Gao, S., 2002. Shallow sedimentation and physical environment evolution as a part of global change: an example from the Bohai, Yellow and East China Sea region. Earth Sci. Frontier 9: 330–335.

    Google Scholar 

  • Hume, T. M., and C. S. Nelson, 1986. Distribution and origin of clay minerals in the surficial shelf sediments, western North Island, New Zealand. Mar. Geol. 69: 289–308.

    Article  Google Scholar 

  • Karlin, R., 1980. Sediment sources and clay mineral distribution off the Oregon coast. J. Sedi. Petr. 50: 543–560.

    Google Scholar 

  • Khim, B. K., 1988. Sedimentological study of the muddy deposits in the Yellow Sea. M. S. Thesis, Dept. of Oceanography, Seoul Nati. Univ., 106p.

  • Kim, D. C., 1980. Recent clay minerals of the Yeongsan Estuary and the adjacent continental shelf. M. S. Thesis, Dept. of Oceanography, Seoul Nati. Univ., 63p.

  • Krumbein, W. C. and F. J. Pettijohn, 1938. Manual of sedimentary petrography. Appleton Century Crofts, York, N. Y., 549p.

    Google Scholar 

  • Lee, H. J. and S. K. Chough, 1989. Sediment distribution, dispersal and budget in the Yellow Sea. Mar. Geol. 87: 195–205.

    Article  Google Scholar 

  • Loring, D. H. and G. Asmund, 1996. Geochemical factors controlling accumulation of major and trace elements in Greenland coastal fjord sediments. Environ. Geol. 28: 1–11.

    Article  Google Scholar 

  • Liu, J., R. X. Zhu and G. X. Li., 2003. Rock magnetic properties of the fine-grained sediment on the outer shelf of the East China Sea: implication for provenance. Mar. Geol. 193: 195–206.

    Article  Google Scholar 

  • Milliman, J. D. and R. H. Meade, 1983. World-wide delivery of river sediment to the oceans. J. Geol. 91: 1–21.

    Article  Google Scholar 

  • Milliman, J. D., R. C. Beardsley, J. S. Yang and R. Limebruner, 1985. Modern Huanghe River mud on the outer shelf of the East China Sea: identification and potential transport mechanisms. Cont. Shelf Res. 4: 175–188.

    Article  Google Scholar 

  • Naidu, A. S., J. S. Creager and T. C. Mowatt, 1982. Clay mineral dispersal in the north Bering and Chukchi Sea. Mar. Geol. 47: 1–15.

    Article  Google Scholar 

  • Naidu, A. S. and T. C. Mowatt, 1983. Sources and dispersal patterns of clay minerals in surface sediments from the continental shelf areas off Alaska. Geol. Soc. Am. Bull. 94: 841–854.

    Article  Google Scholar 

  • Park, B. K. and S. J. Han, 1985. The distribution of clay minerals in recent sediments of the Korea Strait. Sediment. Geology 41: 173–184.

    Google Scholar 

  • Park, Y. A. and B. K. Khim, 1992. Origin and dispersal of recent clay minerals in the Yellow Sea. Mar. Geol. 104: 205–213.

    Article  Google Scholar 

  • Park, J. B. and S. T. Kwon, 1993. Geochemical evolution of the Cheju volcanic island: Trace element chemistry of volcanic rocks from the northern part of Cheju Island. J. Geol. Soc. Korea 29: 477–492.

    Google Scholar 

  • Piper, D. J. W. and R. M. Slatt, 1977. Late Quaternary clay mineral distribution on the estern continental margin of Canada. Geo. Soc. Am. Bull. 88: 267–272.

    Article  Google Scholar 

  • Qin, Y. S. and F. Li, 1983. Study of influence of sediment loads discharged from the Huanghe River on sedimentation in the Bohai Sea and the Huanghe Sea. In: Sedimentation on the Continental Shelf with Special Reference to the East China Sea 2, China Ocean Press, Beijing, p. 83–92.

    Google Scholar 

  • Revel, M., J. A. Sinko and F. E. Grousset, 1996. Sr and Nd isotopes as tracers of north Atlantic lithic particles: paleoclimatic implication. Paleoceanography 11: 95–113.

    Article  Google Scholar 

  • Stein, R., 1990. Organic carbonation/sedimentation rate relationship and its paleoenvironmental significance for marine sediment. Geo-Marine Letters 10: 37–44.

    Article  Google Scholar 

  • Taylor, S. R. and S. K. McLennan, 1985. The continental crust: its composition and evolution. Bleakwell, Oxford, 312p.

    Google Scholar 

  • Tutken, T., A. Eisenhauer, B. Wiegand and B. T. Hansen, 2002. Glacial-interglacial cycles in Sr and Nd isotope composition of Arctic marine sediments triggered by the Svalbard/Barents Sea ice sheet. Mar. Geol. 182: 315–372.

    Article  Google Scholar 

  • Walter, H. J., E. Hegner, B. Diekmann, G. Kuhn, V. D. Rurger and M. M. Loeff, 2000. Provenance and transport of terrigenous sediment in the south Atlantic Ocean and their relations to glacial and interglacial cycles: Nd and Sr isotopic evidence. Geocim. Cosmochin. Acta 64: 3 813–3 827.

    Google Scholar 

  • Xu, D., 1983. Mud sedimentation on the East China Sea shelf. In: Sedimentation on the Continental Shelf with Special Reference to the East China Sea, 2, China Ocean Press, Beijing, p. 506–516.

    Google Scholar 

  • Yang, Z. and J. D. Milliman, 1983. Fine-grained sediment sources of East China Sea. In: Sedimentation on the Continental Shelf with Special Reference to the East China Sea 2, China Ocean Press, Beijing, p. 405–415.

    Google Scholar 

  • Yang, S. Y., H. S. Jung, D. I. Lim and C. X. Li, 2003. A review on the provenance discrimination of sediments in the Yellow Sea. Earth-Science Reviews 63: 93–120.

    Article  Google Scholar 

  • Yang, S. Y., D. I. Lim, H. S. Jung, H. S. and B. C. Oh, 2004. Geochemical composition and provenance discrimination of coastal sediments around Cheju Island in the southeastern Yellow Sea. Mar. Geol. 206: 41–53.

    Article  Google Scholar 

  • Zhao, Y. Y., Z. Y. Qin, F. G. Li and Y. W. Chen, 1990. On the sources and genesis of the mud in the central area of the South Yellow Sea, Chinese Journal of Oceanology Limnology 8: 66–73.

    Article  Google Scholar 

  • Zhao, Y. Y., Y. A. Park, J. Y. Qin, S. Gao, Y. Y. Li, P. Chen and R. H. Jiang, 2001. Material source for the Eastern Yellow Sea Mud: evidence of mineralogy and geochemistry from China-Korea joint investigation. The Yellow Sea 7: 22–26.

    Google Scholar 

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Authors and Affiliations

  1. Department of Oceanography, College of Ocean Sciences, Cheju National University, Jeju-do, 690-756, Korea

    Jeungsu Youn

  2. State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China

    Shouye Yang

  3. Research Institute of Oceanography, Seoul National University, Seoul, 151-742, Korea

    Yong Ahn Park

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  1. Jeungsu Youn
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  2. Shouye Yang
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  3. Yong Ahn Park
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Correspondence to Jeungsu Youn.

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This work was supported by the research grant of the Cheju National University of Year 2006.

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Youn, J., Yang, S. & Park, Y.A. Clay minerals and geochemistry of the bottom sediments in the northwestern East China Sea. Chin. J. Ocean. Limnol. 25, 235–246 (2007). https://doi.org/10.1007/s00343-007-0235-1

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  • DOI: https://doi.org/10.1007/s00343-007-0235-1

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