Abstract
Sedimentation of fine-grained deposits on coastal zones and continental shelves are important because of the association with chemical pollutants, and the implication to the impact on biological processes, the stratigraphic correlations, and changes in sedimentary environments. The Yellow Sea continental shelf receives large quantities of sediment from the Huanghe (Yellow) River. Unfortunately, little attention has been yet paid to the sedimentation on the shallow shelf and its features, and the vertical sediment flux in the area is poorly understood. In this study, nine cores were collected in northern Yellow Sea by theR/V Science 1 in September, 1998 and 1999 to examine the sedimentation rate, sediment flux and the provenance with210Pb analysis. The210Pb activity profiles showed that the vertical sediment flux ranged from 0.06 to 1.18 g/cm2·a in the region. In central part of the area, there was a patch of fine-grained mud, with the flux below 0.33 g/cm2·a. Most profiles were featured in two-segment model. Differences in the profiles reflected spatial and temporal variations in hydrodynamic and sedimentary processes. In order to determine the provenance and sedimentary setting in the area, the geochemistry of Ca, Fe, Sr, Cu, Ti and Rb in 11 surficial sediment samples were studied, which showed that in the central northern Yellow Sea, the mud deposit was from multi-source but mainly from the Huanghe River.
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Reference
Alexander, C. R., D. J. Demaster and C. A. Nittrouer, 1991. Sediment accumulation in a modern epicontinental shelf setting: the Yellow Sea.Marine Geology 98: 51–72.
Demaster, D. J., 1985. Rates of sediment reworking at the Hebble site based on measurement of234Th,137Cs and210pb.Marine Geology 66: 133–148.
Gao, S., Y. A. Park, Y. Y. Zhao and Y. S. Qin, 1996. Transport and resuspension of fine-grained sediment over the Southeastern Yellow Sea.In: Lee, C. B. and Zhao, Y. Y., Proceeding of the Korea-China International Senibar on Holocence and Late Pleistocene Environments in the Yellow Sea Basin. Seoul National University, Seoul, 83–98.
Han, G. R., X. S. Xu and C. Y. Xin, 1998. Geochemical characteristics of the sediment in buried paleoriver channel area in the Huanghai Sea and Bohai Sea.Studia Marina Sinica 40: 79–87. (in Chinese)
Li, F. Y., 1993. Modern Sedimentation rates and sedimentation feature in the Huanghe River estuary based on210pb technique.Chinese Journal of Oceanology and Limnology 11: 333–342.
Li, F. Y., L. J. He and Y. L. Shi, 1996. Isotopic records of modern sedimentary environments in the Southern Yellow Sea. Proceedings of The Korea-China International Seminar on Holocene and late Pleistocene Environments in the Yellow Sea Basin11: 151–157.
Li, F. Y., Y. L. He and L. J. Shi, 1999. Discussion on sedimentation rates and material source in the east of the South Yellow Sea.Marine Sciences 5: 37–40. (in Chinese with English abstract)
Martin, J. M., J. Zhang, M. C. Shi and Q. Zhou, 1993. Actual flux of the Huanghe (Yellow River) sediment to the Western Pacific Ocean.Netherlands Journal of Sea Research 31(3): 243–254.
Milliman, J. D., and R. H. Meade, 1983. World wide delivery of river sediment to the oceans.The Journal of Geology 91: 1–21.
Milliman, J. D., F. Li and Y. Y. Zhao, 1986. Suspended matter regime in the Yellow Sea.Progress in Oceanography 17: 215–228.
Milliman, J. D., Y. Qin and Y. A. Park, 1989. Sediments and sedimentary processes in the Yellow and East China Seas.In: Taira A. and Masuda F., Proceedings of Sedimentary Facies in the Active Plate Margin, TER-RAPUB, Tokyo, pp. 233–249.
Park, S. C., H. H. Lee and H. S. Han, 2000. Evolution of late Quaternary mud deposits and recent sediment budget in the southeastern Yellow Sea.Marine Geology 170: 271–288.
Qin, Y. S, Y. Y. Zhao, L. R. Chen and S. L. Zhao, 1989. Geology of the Yellow Sea. China Ocean Press, 1–13. (in Chinese)
Schubel, J. R., H. T. Shen and M. J. Park, 1984. A comparison of some characteristic sedimentation processes of estuaries entering the Yellow sea.In: Park, Y. A. Pilkey, O. H. and Kim, S. W., Marine Geology and Physical Processes of the Yellow Sea, Korea Institute of Energy Resources, Seoul, 286–308.
Shen, H. T., 1990. Comparative studies of estuaries bordering the Yellow Sea.Chinese Journal of Oceanology and Limnology 21(5): 449–457.
Zhao, Y. Y., F. Y. Li, R. H. Jiang, Y. W. Chen, C. A. Nitrouer, D. J. Demaster and J. D. Milliman, 1990. On the source and genesis of the mud in the central area of the south Yellow Sea.Chinese Journal of Oceanology and Limnology 8: 66–73.
Zhao, Y. Y., F. Y. Li, D. J. Demaster, C. A. Nitrouer and J. D. Milliman, 1991. Preliminary studies on the sedimentation rate and sediment flux of the South Huanghai Sea.Oceanologia et Limnologia Sinica 22: 38–43. (in Chinese with English abstract)
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Supported by Qingdao Special Program for Outstanding Scientists (No.04-3-JJ-03), the “100 Talents Program” of the Chinese Academy of Sciences (CAS), the Knowledge Innovation Program of CAS (Nos. KZCX1-SW-01-08 and KZCX3-SW-214) and the NSF for Outstanding. Young Scientists (Nos. 49925614 and 49725612), and the NSF of Shandong Province (No. H74990247).
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Fengye, L., Xuegang, L., Jinming, S. et al. Sediment flux and source in northern Yellow Sea by210Pb technique. Chin. J. Ocean. Limnol. 24, 255–263 (2006). https://doi.org/10.1007/BF02842625
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DOI: https://doi.org/10.1007/BF02842625