东海内陆架泥质区百年来黏土矿物组成变化及其环境意义

王亮; 范德江; 李巍然; 张喜林; 陈彬; 田元

doi:10.3969/j.issn.0253-4193.2015.05.009

东海内陆架泥质区百年来黏土矿物组成变化及其环境意义

doi: 10.3969/j.issn.0253-4193.2015.05.009

1.
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, 山东青岛 266100;国家海洋局第三海洋研究所, 福建厦门 361005
2.
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, 山东青岛 266100
3.
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, 山东青岛 266100;国土资源部青岛海洋地质研究所, 山东青岛 266071

基金项目: 国家自然科学基金项目(41376055,41030856);国家重大基础研究发展计划项目(2010CB951202)。

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出版历程
- 收稿日期: 2013-12-25
- 修回日期: 2014-06-05

The variation of clay minerals contents on the inner shelf of the East China Sea in the last one hundred years and its environmental implication

1.
Key Lab of Submarine Geosciences and Technology in the Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China
2.
Key Lab of Submarine Geosciences and Technology in the Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Key Lab of Submarine Geosciences and Technology in the Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;Qingdao Institute of Marine Geology, Ministry of Land and Resources, Qingdao 266071, China

摘要

摘要: 东海内陆架泥质区是东海现代沉积的"汇",其中黏土组分是泥质区沉积物的重要组成部分。沉积物中黏土矿物组合是反映沉积区物质来源和搬运动力状况的良好指标。本文利用XRD方法分析了东海内陆架泥质区两根沉积物岩心中黏土矿物组成和含量变化,结合放射性年代标定,揭示了近百年来黏土矿物组成的演变特征,探讨了黏土矿物的来源及其含量变化的制约因素。结果表明:东海内陆架泥质区沉积物以长江来源物质为主,受黄河及瓯江等河流物质的影响;近百年来内陆架泥质区黏土矿物组合发生显著阶段性变化,它们是东亚季风强弱波动和长江入海悬沙减少的共同作用的结果。
- 东海内陆架 /
- 黏土矿物 /
- 物源 /
- 东亚季风 /
- 长江输沙
Abstract: The modern depocenter in the East China Sea is the mud area on the inner shelf,and the clay fraction of the sediments in the area is the main component. In the study of sedimentology,the clay minerals assemblage was widely used as an indicator of provenance and transportation of particulates. In this study,we used the method of XRD to study the variation of clay mineral contents in two gravity cores collected from the mud area. The clay minerals,together with the analysis of grain size and radioactive dating on the samples,have been used to discuss their environmental implications. The result shows that sediments in the mud area of East China Sea are mainly derived from the supply of Changjiang River,and contain a little from the Huanghe River and Oujiang River. And,clay mineral records have exhibited significant changes in the last one hundred years,which may be influenced by the fluctuations of East Asian Monsoon and the decreasing of sediment discharge of the Changjiang River.
- inner shelf in the East China Sea /
- clay minerals /
- provenance /
- East Asian Monsoon /
- sediment discharge of the Changjiang River

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参考文献(49)

胡敦欣,杨作升,等.东海海洋通量关键过程[M].北京: 海洋出版社,2001: 72-81. Hu Dunxin,Yang Zuosheng,et al. Key Processes of the East China Sea Flux[M]. Beijing: China Ocean Press,2001:72-81.

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(17/18): 2141-2156.

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.

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. The analysis of provance of the sediment in the Min-Zhe mud areas[J]. Progress in Natural Science,2009,19(2): 185-191.

叶银灿,庄振业,刘杜娟,等.东海全新世沉积强度分区[J].青岛海洋大学学报(自然科学版),2002,36(6):941-948. Ye Yincan,Zhuang Zhenye,Liu Dujuan,et al. Holocene depositional strength zoning in the East China Sea[J]. Journal of Ocean University of Qingdao,2002,36(6): 941-948.

李军,胡邦琦,窦衍光,等.中国东部海域泥质沉积区现代沉积速率及其物源控制效应初探[J].地质论评,2012,58(4):745-756. Li Jun,Hu Bangqi,Dou Yanguang,et al. Modern sedimentation rate,budget and supply of the muddy deposits in the East China Sea[J]. Geological Review (in Chinese),2012,58(4): 745–756.

Xu K H,Li A C,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.

夏小明,谢钦春,李炎,等.东海沿岸海底沉积物中的¹³⁷Cs、²¹⁰Pb分布及其沉积环境解释[J].东海海洋,1999(01):21-28. Xia Xiaoming,Xie Qinchun,Li Yan,et al. ¹³⁷Cs and ²¹⁰Pb profiles of the seabed cores along the East China Sea coast and their implications to sedimentary environment[J]. Donghai Marine Science,1999(01): 21-28.

Huh C A,Su C C. Sedimentation dynamics in the East China Sea elucidated from ²¹⁰Pb,¹³⁷Cs and ²³⁹,²⁴⁰Pu[J]. Marine Geology,1999,160(1): 183-196.

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,2010,56(14):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 Science Bulletin,2010,56(14):1387-1396.

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,Zhao Yiyang,Chen Lirong,et al. Geology of the East China Sea[M]. Beijing: China Science Press,1987.

Milliman J D,Beardsley R C,Yang Z,et al. Modern Huanghe-derived muds on the outer shelf of the East China Sea: identification and potential transport mechanisms[J]. Continental Shelf Research,1985,4(1/2): 175-188.

杨作升,郭志刚,王兆祥,等. 黄东海陆架悬浮体及其向东部深海区输送的宏观格局[J]. 海洋学报,1992,14(2):81-90. Yang Zuosheng,Guo Zhigang,Wang Zhaoxiang,et al. Basic pattern of transport of suspended matter from the Yellow Sea and East China Sea to the eastern deep seas[J]. Haiyang Xuebao,1992,14(2): 81-90.

孙效功,方明,黄伟.黄东海陆架区悬浮体输运的时空变化规律[J]. 海洋与湖沼,2000,31(6):581-587. Sun Xiaogong,Fang Ming,Huang Wei. Spatial and temporal variations in suspended particulate matter transport on the Yellow and East China Sea shelf[J]. Oceanologia et Limnologia Sinica,2000,31(6): 581-587.

Xu K H,Milliman J D,Li A C,et al. Yangtze-and Taiwan-derived sediments on the inner shelf of East China Sea[J]. Continental Shelf Research,2009,29(18): 2240-2256.

Li F,Li P,Zhang X R,et al. Transport of suspended matter from the Changjiang River to the East China Sea shelf[J]. Chinese Journal of Oceanology and Limnology,1997,15(3): 264-270.

刘光华.黏土矿物特征与沉积环境关系的初步探讨[J].沉积学报,1987,5(1):50-54. Liu Guanghua. Preliminary Study on the relationship of clay mineral characteristics and Sedimentary environment[J]. Acta Sedimentologica Sinica,1987,5(1): 50-54.

朱凤冠,李秀珠,高水土.东海大陆架沉积物中黏土矿物的研究[J].东海海洋,1988,6(1):40-51. Zhu Fengguan,Li Xiuzhu,Gao Shuitu. Research of clay minerals of sediments on the continental shelf of the East China Sea[J]. Donghai Marine Science,1988,6(1): 40-51.

陈忠,颜文. 海洋沉积黏土矿物与古气候古环境演化响应的研究进展[J].海洋科学,2000,24(2):25-27. Chen Zhong,Yan Wen. Advances of the studies of clay minerals in marine sediments and its response to evolution of paleoclimate and paleoenvironment[J]. Marine Sciences,2000,24(2): 25-27.

李国刚.中国近海表层沉积物中黏土矿物的组成、分布及其地质意义[J].海洋学报,1990,12(4):470-479. Li Guogang. Composition,distribution of the clay minerals in surface sediments in the offshore China Seas and its geological significance[J]. Acta Oceanologica Sinica,1990,12(4): 470-479.

周晓静,李安春,万世明,等.东海陆架表层沉积物黏土矿物组成分布特征及来源[J].海洋与湖沼,2010,41(5):667-675. Zhou Xiaojing,Li Anchun,Wan Shiming,et al. Clay minerals in surface sediments of the East China Sea shelf: distribution and provenance[J]. Oceanologia Et Limnologia Sinica,2010,41(5): 667-675.

Yang S L,Zhang J,Zhu J,et al. Impact of dams on Yangtze River sediment supply to the sea and delta intertidal wetland response[J]. Journal of Geophysical Research: Earth Surface (2003-2012),2005,110: F03006,1-12.

戴仕宝,杨世伦,郜昂,等.近50年来中国主要河流入海泥沙变化[J].泥沙研究,2007(2):49-58. Dai Shibao,Yang Shilun,Gao Ang,et al. Trend of Sediment flux of main rivers in China in the past 50 years [J]. Journal of Sediment Research,2007(2): 49-58.

Chu Z,Zhai S,Lu X,et al. A quantitative assessment of human impacts on decrease in sediment flux from major Chinese rivers entering the western Pacific Ocean[J]. Geophysical Research Letters,2009,36(19): L19603.

Liu J,Saito Y,Kong X,et al. Sedimentary record of environmental evolution off the Yangtze River estuary,East China Sea,during the last~13000 years,with special reference to the influence of the Yellow River on the Yangtze River delta during the last 600 years[J]. Quaternary Science Reviews,2010,29(17): 2424-2438.

周鹏.东海沉积物岩心中生物硅的测定及其地层学分析[D].厦门:厦门大学,2007. Zhou Peng. Measurement of biogenic silica (BSi) in marine sediment cores from East China Sea and their stratigraphical application[D].Xiamen:Xiamen University,2007.

朱凤冠.东海陆架区全新世地层中黏土矿物[J].东海海洋,1985,3(4):32-43. Zhu Fengguan. Clay minerals of the East China Sea shelf area in the recent Epoch stratum[J]. Donghai Marine Science,1985,3(4): 32-43.

何良彪,刘秦玉.黄河与长江沉积物中黏土矿物的化学特征[J].科学通报,1997,42(7): 730-734. He Liangbiao,Liu Qinyu. Chemical characteristics of clay minerals of Yangtze and Yellow Rivers[J]. Chinese Science Bulletin,1997,42(7): 730-734.

唐松,邵磊,赵泉鸿.南海渐新世以来黏土矿物的演变特征及意义[J].沉积学报,2004,22(2):337-341. Tang Song,Shao Lei,Zhao Quanhong. Characteristics of clay mineral in South China Sea since Oligocene and its significance[J]. Acta Sedimentologica Sinica,2004,22(2): 337-341.

刘志飞,Colin C,Trentesaux A,等.南海南部晚第四纪东亚季风演化的黏土矿物记录[J].中国科学D辑:地球科学,2004,34(3):272-279. Liu Zhifei,Colin C,Trentesaux A,et al. Clay mineral records of East Asian monsoon evolution during late Quaternary in the southern South China Sea[J]. Scientia Sinica Terrae,2004,34(3): 272-279.

范德江,杨作升,孙效功,等.东海陆架北部长江、黄河沉积物影响范围的定量估算[J].青岛海洋大学学报(自然科学版),2002,32(5):748-756. Fan Dejiang,Yang Zuosheng,Sun Xiaogong,et al. Quantitative evaluation of sediment provenance on the north area of the East China Sea shelf[J]. Journal of Ocean University of Qingdao,2002,32(5): 748-756.

蔡爱智.长江入海泥沙的扩散[J].海洋学报,1982,4(1):78-88. Cai Aizhi. Distribution of Yangtze sediment supply[J]. Haiyang Xuebao,1982,4(1): 78-88.

熊应乾,杨作升,刘振夏.长江、黄河沉积物物源研究综述[J].海洋科学进展,2003,21(3):355-362. Xiong Yingqian,Yang Zuosheng,Liu Zhenxia. A review of source study of the Changjiang and Yellow River sediments[J]. Advances in Marine Science,2003,21(3) : 355-362.

范德江,杨作升,毛登,等.长江与黄河沉积物中黏土矿物及地化成分的组成[J].海洋地质与第四纪地质,2001,21(4):7-12. Fan Dejiang,Yang Zuosheng,Mao Deng,et al. Clay minerals and geochemistry of sediments from the Yangtze and Yellow Rivers[J]. Marine Geology and Quaternary Geology,2001,21(4): 7-12.

周晓静,高抒,贾建军.长江黏土矿物示踪标记稳定性的初步研究[J].海洋与湖沼,2003,34(6):683-692. Zhou XiaoJing,Gao Shu,Jia Jianjun. Preliminary evaluation of the stability of Changjiang clay minerals as fingerprints for material source tracing [J]. Oceanologia Et Limnologia Sinica,2003,34(6): 683-692.

徐勇航,陈坚,王爱军,等.台湾海峡表层沉积物中黏土矿物特征及物质来源[J]. 沉积学报,2013,31(1):120-129. Xu Yonghang,Chen Jian,Wang Aijun,et al. Clay minerals in surface sediments of the Taiwan Strait and their provenance[J]. Acta Sedimentologica Sinica,2013,31(1): 120-129.

李传顺,石学法,高树基,等. 台湾河流沉积物的黏土矿物组成特征与物质来源[J].科学通报,2012,57(2/3):169-177. Li Chuanshun,Shi Xuefa,Gao Shuji,et al. Clay mineral composition and their sources for the fluvial sediments of Taiwanese rivers[J]. Chinese Science Bulletin,2012,57(2/3): 169-177.

陈静,马春燕,周园军.中国沿海河口黏土矿物组合特征及物源判别指标[OL]. [2010-10-11].中国科技论文在线,http://www2.paper.edu.cn/releasepaper/content/201010-118. Chen Jing,Ma Chunyan,Zhou Yuanjun. Clay minerals in the major Chinese coastal estuaries and their provenance implications[OL][2010-10-11]. Sciencepaper Online,http://www2.paper.edu.cn/releasepaper/content/201010-118.

金翔龙.东海海洋地质[M].北京:海洋出版社,1992. Jin Xianglong. Marine Geology of the East China Sea[M]. Beijing: China Ocean Press,1992.

Boulay S,Colin C,Trentesaux A,et al. Sediment sources and East Asian monsoon intensity over the last 450 ky: mineralogical and geochemical investigations on South China Sea sediments[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,2005,228: 260-277.

万世明,李安春,胥可辉,等. 南海北部中新世以来黏土矿物特征及东亚古季风记录[J].地球科学(中国地质大学学报),2008,34(3):289-300. Wan Shiming,Li Anchun,Xu Kehui,et al. Characteristics of Clay Minerals in the Northern South China Sea and Its Implications for Evolution of East Asian Monsoon since Miocene[J]. Earth Science—Journal of China University of Geosciences,2008,34(3): 289-300.

肖尚斌,李安春.东海内陆架泥区沉积物的环境敏感粒度组分[J].沉积学报,2005,23(1):122-129. Xiao Shangbin,Li Anchun. A study on environmentally sensitive grain-size population in inner shelf of the East China Sea[J]. Acta Sedimentologica Sinica,2005,23(1): 122-129.

徐建军,朱乾根,周铁汉.近百年东亚冬季风的突变性和周期性[J].应用气象学报,1999,10(1):1-8. Xu Jianjun,Zhu Qiangen,Zhou Tiehan. Sudden and periodic changes of East Asian winter monsoon in the past century[J]. Quarterly Journal of Applied Meteorology,1999,10(1): 1-8.

贺圣平,王会军.东亚冬季风综合指数及其表达的东亚冬季风年际变化特征[J].大气科学,2012,36(3):523-538. He Shengping,Wang Huijun. An integrated East Asian winter monsoon index and its inter-annual variability[J]. Chinese Journal of Atmospheric Sciences,2012,36(3):523-538.

李建平,曾庆存.一个新的季风指数及其年际变化和与雨量的关系[J].气候与环境研究,2005,10(3):73-87. Li JianPing,Zeng QingCun. A new Monsoon index,its interannual variability and relation with Monsoon precipitation[J]. Climatic and Environmental Research,2005,10(3): 73-87.

Wang H,Yang Z,Wang Y,et al. Reconstruction of sediment flux from the Changjiang (Yangtze River) to the sea since the 1860s[J]. Journal of Hydrology,2008,349(3): 318-332.

何梦颖,郑洪波,黄湘通,等.长江流域沉积物黏土矿物组合特征及物源指示意义[J].沉积学报,2011,29(3):544-551. He Mengying,Zheng Hongbo,Huang Xiangtong,et al. Clay mineral assemblages in the Yangtze drainage and provenance implications[J]. Acta Sedimentologica Sinica,2011,29(3): 544-551.

施能,杨永胜. 1873-1996年东亚冬、夏季风强度指数及其主要特征[J].南京气象学院学报,1998,21(2):47-53. Shi Neng,Yang Yongsheng. Main characteristics of East Asian summer/winter monsoon index for 1873-1996 [J]. Journal of Nanjing Institute of Meteorology,1998,21(2): 47-53.

Mao C,Chen J,Yuan X,et al. Seasonal variation in the mineralogy of the suspended particulate matter of the lower Changjiang River at Nanjing,China[J]. Clays and Clay Minerals,2010,58(5): 691-706.

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