黄海与东海泥质区高分辨率沉积记录研究新进展

王琳淼; 李广雪

doi:10.3724/SP.J.1140.2014.03167

黄海与东海泥质区高分辨率沉积记录研究新进展

王琳淼,
李广雪^,

中国海洋大学海洋地球科学学院, 海底科学与探测技术教育部重点实验室, 青岛 266100

基金项目:

国家自然科学重点基金项目(41030856)；山东省泰山学者建设工程专项

详细信息

作者简介:
王琳淼(1986-),女,博士生,从事海洋沉积记录与古环境研究,E-mail:wanglinmiao9@gmail.com

中图分类号: P512.2
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- 文章访问数: 2063
- HTML全文浏览量: 261
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出版历程
- 收稿日期: 2013-07-25
- 修回日期: 2014-04-24

HIGH-RESOLUTION SEDIMENTARY RECORDS OF THE MUDDY AREA IN THE SOUTH YELLOW SEA AND EAST CHINA SEA: A REVIEW OF NEW PROGRESS

WANG Linmiao,
LI Guangxue^,

College of Marine Geosciences, Key Laboratory of Submarine and Prospecting Techniques, Ocean University of China, Qingdao 266100

摘要

摘要: 陆架区沉积物季风代用指标在不同的地区可能具有不同意义，东海陆架泥质区的高分辨率古气候研究率先开始，有一大批成果通过提取敏感粒度指标进行东亚冬季风重建，并讨论了其与全球气候变化之间的驱动和响应关系；但有研究者指出，陆架沉积物的粒度指标更多的代表东亚夏季风信息，因此黄海地区更多的高分辨率沉积物古气候研究对此进行机制解释很有必要；古海洋学研究方面，最初依据有孔虫组合变化规律和AMS¹⁴C年代学结合进行古海洋环境重建，后来不断有学者提供高分辨率古海水温度记录，近期沉积记录中古生态系统信息的提取为古海洋环境演化的研究提供了新的参考；工业革命以来，有机污染物、重金属污染在陆架区泥质沉积记录中变化明显，反映出人类活动对海洋沉积记录的影响。
- 古气候 /
- 沉积记录 /
- 黄海 /
- 东海
Abstract: This paper gives a comprehensive overview of recent progress in the study of the mud area in the East China Sea and the Yellow Sea. The research progress in East Asian monsoon, paleoclimate, paleoceanology and the sedimentary records in response to human activities since the industrial revolution is discussed. It is found that the sensitive grain size, which was used as a proxy to Asian monsoon, may have different meanings in different areas. High-resolution paleoclimate studies in the Yellow Sea are important and should be carried out as soon as possible to explain the mechanism of the related process. Recently, the research of ancient ecosystem on the shelf has provided new references for climate change. Organic pollutants and heavy metals contamination on the shelf area could be used to reveal the environmental changes since the industrial revolution.
- climate change /
- sediment record /
- East China Sea /
- Yellow Sea

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参考文献(60)

[1]	Liu J P, Li A C, Xu K H, et al. Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea[J]. Continental Shelf Research, 2006, 26:21-41.
[2]	Saito Y, Katayama H, Ikehara K, et al. Transgressive and high-stand systems tracts and post-glacial transgression, the East China Sea[J]. Sedimentary Geology, 1998, 122:217.
[3]	Jin J, Chough S K. Partitioning of transgressive deposits in the southeastern Yellow Sea:a sequence strati-graphic interpretation[J]. Marine Geology, 1998, 149:79-92.
[4]	Xiao S H, Li A H, Liu J H, et al. Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 237:293-304.
[5]	Xiao S B, Li A C. A study on environmentally sensitive grain size population in inner shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1):27-34.
[6]	李广雪, 杨子赓, 刘勇. 中国东部海域海底沉积环境成因研究(附1:200万海底沉积物成因环境图说明书)[M]. 北京:科学出版社, 2005:23.[LI Guangxue, YANG Zigeng, LIU Yong. Origins of Seafloor Sedimentary Environments in Eastern China Sea Regions[M]. Beijing:Science Press, 2005:23.]
[7]	刘升发,石学法,刘焱光,等.中全新世以来东亚冬季风的东海内陆架泥质沉积记录[J].科学通报,2010, 55:1387-1396.[LIU Shengfa, SHI Xuefa, LIU Yanguang, et al. Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene[J]. Chinese Sci. Bull., 2010 , 55:1387-1396.]
[8]	秦蕴珊,赵一阳,陈丽蓉,等.东海地质[M].北京:科学出版社,1987.[QIN Yunshan, ZHAOYiyang, CHEN Lirong. The Geology of the East China Sea[M].Beijing:China Ocean Press, 1987.]
[9]	Xu K H, Li A H, Liu J P, et al. Provenance, structure, and formation of the mud wedge along inner continental shelf of the East China Sea:A synthesis of the Yangtze dispersal system[J]. Marine Geology, 2012, 291-294:176-191.
[10]	徐方健,李安春,万世明,等.东海内陆架陆源物质矿物组成对粒度和地球化学成分的制约[J].地球科学-中国地质大学学报,2009,34(4):613-622 [XU Fangjian, LI Anchun, WAN Shiming, et al. Terrigenous mineral constrains on the grain-size distribution and geochemical composition of sediments in the inner shelf of the East China Sea[J]. Acta Oceanologica Sinica, 2009, 31(3):95-102.]
[11]	肖尚斌,李安春,刘卫国,等. 闽浙沿岸泥质沉积的物源分析[J].自然科学进展, 2009, 19(2):185-191. [XIAO Shangbin, LI Anchun, LIU Weiguo, et al. Sediment provenance of the Zhejiang-Fujian coast mud[J]. Progress in Natural Science, 2009, 19(2):185-191.]
[12]	Youn J, Kim T. Geochemical composition and provenance of muddy shelf deposits in the East China Sea[J]. Quaternary International, 2011, 230:3-12.
[13]	Alexander C R, DeMaster D J, Nittrouer C A. Sediment accumulation in a modern epicontinental-shelf setting:the Yellow Sea[J]. Marine Geology, 1991, 98:51-72.
[14]	Liu J P, Milliman J D, Gao S. The Shandong mud wedge and post-glacial sediment accumulation in the Yellow Sea[J]. Geo-Marine Letters, 2002, 21:212-218.
[15]	Liu J, Saito Y, Kong X, et al. Geochemical characteristics of sediment as indicators of post-glacial environmental changes off the Shandong Peninsula in the Yellow Sea[J]. Continental Shelf Research, 2009,29:846-855.
[16]	Liu J P, Saito Y, Wang H J, et al. Sedimentary evolution of the Holocene subaqueous clinoform off the Shandong Peninsula in the Yellow Sea[J]. Marine Geology, 2007, 236:165-187.
[18]	Wang Y H, Dong H L, Li G X, et al. Magnetic properties of muddy sediments on the northeastern continental shelves of China:implication for provenance and transportation[J]. Marine Geology, 2010, 274:107-119.
[19]	Gao J, Pan H M, Wu L F, et al. Characterization of magnetotactic bacteria and magnetosomesin sediments from the Yellow Sea cold water mass[J]. Marine Science, 2006, 30:11-16.
[20]	Ding Z L, Yang S L, Sun J M, et al. Iron geochemistry of loess and red clay deposits in the Chinese Loess Plateau and implications for long-term Asian monsoon evolution in the last 7.0 Ma[J]. Earth and Planetary Science Letters, 2001, 185:99-109.
[21]	Sun Y, Wu F, Clemens S C, et al. Processes controlling the geochemical composition of the South China Sea sediments during the last climatic cycle[J]. Chemical Geology, 2008, 257:243-249.
[22]	Thompson L G, Thompson M E, Davis M E, et al. Holocene-late Pleistocene climatic ice core records from Qinghai-Tibetan Plateau[J]. Science, 1989, 246:474-477.
[23]	Yu K F, Zhao J X, Liu T S, et al. High-frequency winter cooling and reef coral mortality during the Holocene climatic optimum[J]. Earth and Planetary Science Letters, 2004, 224:143-155.
[24]	Wang Y, Cheng H, Edwards R L, et al. The Holocene Asian monsoon:Links to solar changes and North Atlantic climate[J]. Science, 2005, 308:854-857.
[25]	Liu Z, Harrison S P, Kutzbach J, et al. Global monsoons in the mid-Holocene and oceanic feedback[J]. Climate Dynamics, 2004, 22:157-182.
[26]	肖尚斌, 李安春, 蒋富清, 等. 近2ka来东海内陆架的泥质沉积记录及其气候意义[J]. 科学通报, 2004, 49(21):2233-2238. [XIAO Shangbin, LI Anchun, JIANG Fuqing, et al. Sediment record and climatic significance of the inner shelf mud of the East China Sea for the past 2 ka[J]. Chinese Science Bulletin, 2004, 49(21):2233-2238.]
[27]	向荣,杨作升,Saito Y,等.济州岛西南泥质区近2300a环境敏感粒度组分记录的东亚冬季风变化[J]. 中国科学D辑, 2006, 36(7):654-662. [XIANG Rong, YANG Zuosheng, Saito Y, et al. Asia winter monsoon variation records of the sensitive grain size of the southwest mud of Jesu island during the recent 2300 years[J]. Science in China (Series D), 2006, 36(7):654-662.]
[28]	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.]
[29]	洪冰, 林庆华, 洪业汤. 全新世亚洲季风, ENSO及高北纬度气候间的关联[J]. 科学通报, 2006, 51(17):1977-1984. [HONG Bing, LIN Qinghua, HONG Yetang. Association among the Asian monsoon, ENSO and the climate of northern high latitude in Holocene[J]. Chinese Science Bulletin, 2006,51(17):1977-1984.
[30]	Xing L, Jiang Y Q, Yuan Z N, et al. Holocene temperature records from the East China Sea mud area southwest of the Cheju Island reconstructed by the and TEX86 paleothermometers[J]. Journal of Ocean University of China, 2013, 12(4), DOI: 10.1007/s11802-013-2202-0.
[31]	Liu Y, Zhou X, Huang W, et al. Responses of primary productivity to current and climate changes in the mud area to the southwest of Cheju Island during the past 800 years[J]. Journal of Ocean University of China, 2013, 12(4), DOI: 10.1007/s11802-013-2205-x.
[32]	Yuan Z N, Xing L, Zhang H L, et al. Biomarker records of phytoplankton productivity and community structure changes during the Last 14000 Years in the mud area southwest off Cheju Island. East China Sea[J]. Journal of Ocean University of China, 2013, 12(4), DOI: 10.1007/s11802-013-2230-9.
[33]	Guo Z G, Lin T, Zhang G, et al. High-resolution depositional record of polycyclic aromatic hydrocarbons in the central continental shelf mud of the East China Sea[J]. Environmental Science and Technology, 2006, 40(17):5304-5311.
[34]	Guo Z G, Lin T, Zhang G, et al. The sedimentary fluxes of polycyclic aromatic hydrocarbons in the Yangtze River Estuary coastal sea for the past century[J]. Science of the Total Environment, 2007, 386:33-41.
[35]	Hao Y C, Guo Z G, Yang Z S, et al. Tracking historical lead pollution in the coastal area adjacent to the Yangtze River Estuary using lead isotopic compositions[J]. Environmental Pollution, 2008, 156:1325-1331.
[36]	Guo Z G, Yang Z G, Fan D J, et al. Seasonal sedimentary effect on the Changjiang Estuary mud area[J]. Acta Geographica Sinica, 2003, 58(4):591-597.
[37]	徐方建, 李安春. 末次冰消期以来古气候演化研究进展及展望[J]. 科技导报, 2010, 28(9):102-106. [XU Fangjian, LI Anchun. Paleoclimatic evolution since the last deglaciation:a review and prospect view[J]. Science and Technology Review, 2010, 28(9):102-106.]
[38]	徐方建, 李安春, 黄敬利. 东海陆架浙-闽沿岸泥质沉积研究进展[J]. 海洋通报, 2012, 31(1):97-104. [XU Fangjian, LI Anchun, HUANG Jingli. Research progress in the mud deposits along the Zhe-Min coast of the East China Sea continental shelf[J]. Marine Science Bulletin, 2012, 31(1):97-104.]
[39]	徐方建, 李安春, 万世明,等. 东海内陆架泥质区中全新世环境敏感粒度组分的地质意义[J].海洋学报,2009,31(3):95-102. [XU Fangjian, LI Anchun, WAN Shiming, et al. The geological significance of environmental sensitive grain-size populations in the mud wedge of the East China Sea during the mid-Holocene[J]. Acta Oceanologica Sinica, 2009, 31(3):95-102.]
[40]	Hu Bangqi, Yang Zuosheng, Zhao Meixun, et al. Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area[J]. China Sci:China Earth Sci., 2012, 55:1656-1668.
[41]	张晓东,许淑梅,翟世奎,等.东海内陆架沉积气候信息的端元分析模型反演[J].海洋地质与第四纪地质,2006,26(2):25-32. [ZHANG Xiaodong, XU Shumei, ZHAI Shikui. The inversion of climate information from the sediment of inner shelf of East China Sea using end-member model[J]. Marine Geology and Quaternary Geology, 2006, 26(2):25-32.]
[42]	孙晓燕, 李广雪, 刘勇,等. 东海北部泥质区敏感粒度组分对东亚季风演变的响应[J]. 海洋地质与第四纪地质,2008,28(4):11-17. [SUN Xiaoyan, LI Guangxue, LIU Yong, et al. Response of environmental sensitive grain size group in core FJ04 from mud area in the north of East China Sea to East Asian winter monsoon evolvement[J]. Marine Geology and Quaternary Geology, 2008, 28(4):11-17.]
[43]	Zheng Y, Kissel C, Zheng H B, et al. Sedimentation on the inner shelf of the East China Sea:Magnetic properties, diagenesis and paleoclimate implications[J]. Marine Geology, 2010, 268:34-42.
[44]	杨作升,陈晓辉.百年来长江口泥质区高分辨率沉积粒度变化及影响因素探讨[J].第四纪研究,2007,27(5):690-699. [YANG, Zuosheng, CHENG, Xiaohui. Centurial high resolution records of sediment grain-size variation in the mud area off the Changjiang (the Yangtze River) estuary and its influential factors[J]. Quaternary Sciences, 2007, 27(5):690-699.]
[45]	Zhou X, Sun L G, Huang W, et al. Precipitation in the Yellow River drainage basin and East Asian monsoon strength on a decadal time scale[J]. Quaternary Research, 2012, 78:486-491.
[46]	Kim J M, Michal K. Benthic foraminifer record of environmental changes in the Yellow Sea (Hwanghae) during the last 15000 years[J]. Quaternary Science Reviews, 2000, 19:1067-1085.
[47]	Kong G S, Park S C. Late Quaternary paleoenvironmental changes in the southeastern Yellow Sea, Korea[J].Quaternary International, 2006, 144:38-52.
[48]	Xiang R, Yang Z S, Saito Y, et al. Paleoenvironmental changes during the last 8400 years in the southern Yellow Sea:Benthic foraminiferal and stable isotopic evidence[J]. Marine Micropaleontology, 2008, 67:104-119.
[49]	Wang L B, Yang Z S, Zhang R P, et al. Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current[J]. Chinese Sci. Bull., 2011, 56, doi: 10.1007/s11434-011-4442-y.
[50]	李广雪,孙晓燕,刘勇,等.中国东海北部晚全新世表层海水温度变化[J].科学通报,2009, 54:3374-3379.[LI Guangxue, SUN Xiaoyan, LIU Yong, et al. Sea surface temperature record from the north of the East China Sea since late Holocene[J]. Chinese Sci. Bull., doi: 10. 1007/s11434-009-0231-2.]
[51]	胡敦欣,丁宗信,熊庆成.东海北部一个气旋性涡旋的初步分析[J].科学通报,1980,25(1):29-31. [HU Dunxin, DING Zongxin, XIONG Qingcheng. Preliminary analysis of the northern part of the East China Sea a cyclonic vortex[J]. Chinese Sci.Bull., 1980, 25(1):29-31.]
[52]	Zhou X, Sun L G, Liu Y, et al. Potential applications of X-ray fluorescence core scanner in elemental analyses of the muddy sediments on the coastal shelves of China and in ecological study[J]. Journal of Ocean University of China, 2013, 12(4), DOI: 10.1007/s11802-013-2191-z.
[53]	Fang L, Xiang R, Zhao M X, et al. Phase evolution of Holocene paleoenvironmental changes in the Southern Yellow Sea:Benthic foraminiferal evidence from core CO₂[J]. Journal of Ocean University of China, 2013, 12(4), DOI: 10.1007/s11802-013-2214-9.
[54]	Zhao X C, Tao S Q, Zhang R P, et al. Biomarker records of phytoplankton productivity and community structure changes in the Central Yellow Sea mud area during the mid-late Holocene[J]. Journal of Ocean University of China, 2013, 12(4), DOI: 10.1007/s11802-013-2271-0.
[55]	Fan D J, Qi H Y. Annual lamination and its sedimentary implications in the Yangtze River delta inferred from High-resolution biogenic silica and sensitive grain-size records[J]. Continental Shelf Research, 2011, 31:129-137.
[56]	Guo Z G, Yang Z S, Fan D J, et al. Seasonal sedimentary effect on the Changjiang Estuary mud area[J]. Acta Geographica Sinica, 2003, 58(4):591-597.
[57]	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.
[58]	Dong A G, Zhai S K, Zabel M, et al. Heavy metals in Changjiang estuarine and offshore sediments:responding to human activities[J]. Acta Oceanologica Sinica, 2012, 31(2):88-101.
[59]	Audry S, Schöfer J Blanc. Fifty-year sedimentary record of heavy metal pollution (Cd, Zn, Cu, Pb) in the Lot River reservoirs (France)[J]. Environmental Pollution, 2004, 132:413-426.
[60]	Ligero R A, Barrera M, Casas-Ruiz M. Dating of marine sediments and time evolution of heavy metal concentrations in the Bay of Cadiz, Spain[J]. Environmental Pollution, 2002, 118:97-108.
[61]	Lima A, Eglinton T, Reddy C. High-resolution record of pyrogenic polycyclic aromatic hydrocarbon deposition during the 20th century[J]. Environ. Sci. Technol., 2003, 37:53-61.