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海洋通报  2012 

东海陆架浙-闽沿岸泥质沉积研究进展

DOI: 10.11840/j.issn.1001-6392.2012.1.017, PP. 97-104

Keywords: 物源,泥质沉积物,东亚季风,东海,陆架,末次冰消期

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Abstract:

比较全面的回顾了关于东海浙-闽沿岸泥质体以及其形成前的沉积演化历史、泥质沉积的物质来源及其东亚季风/古气候记录等方面的研究进展。分析了目前关于浙-闽沿岸沉积研究中所存在的问题,即,泥质体的物质来源与形成,长江入海历史的陆架沉积物记录,8.2ka冷事件,年代框架调整及区域对比,代用指标指示意义等多方面问题。提出在东海浙-闽沿岸泥质区,我们需要更多高分辨率的钻孔进行综合研究,其中应该特别加强对泥质沉积物的研究,以期对海陆交界敏感地带的“源到汇”以及全球变化研究取得突破性进展。

References

[1]  Sun Y,Wu F,Clemens S C,Processes controlling the geochemical composition of the South China Sea sediments during the last climatic cycle,Chemical Geology,2008(3-4).
[2]  Wei GJ;Liu Y;Li XH,High-resolution elemental records from the South China Sea and their paleoproductivity implications,Paleoceanography? ,2003, 18(02).
[3]  Xiang R,Yang Z S,Saito Y,East Asia Winter Monsoon changes inferred from environmentally sensitive grain-size component records during the last 2300 years in mud area southwest off Cheju Island,ECS,Science in China(Series D),2006(6).
[4]  Xiao S B,Li A C,Jiang F Q..Recent 2000-year geological records of mud in the inner shelf of the East China Sea and their climatic implications[J].Chinese Science Bulletin,2005,(05):466-471.
[5]  Xiao S,Li A,Liu J P,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,Palaeogeography,Palaeoclimatology,Palaeoecology,2006(2-4).
[6]  Xiao S,Liu W,Li A,Pervasive autocorrelation of the chemical index of alteration in sedimentary profiles and its palaeoenvironmental implications,Sedimentology,2010(2).
[7]  Xu F,Li A,Li T..Rare earth element geochemistry in the inner shelf of the East China Sea and its implication to sediment provenances[J].Journal of Rare Earths,2011,(07):702-709.doi:10.1016/S1002-,0721(10)60526-1.
[8]  Xu F,Li A,Xu K,Cold event at 5500 a BP recorded in mud sediments on the inner shelf of the East China Sea,Chinese Journal of Oceanology and Limnology,2009(4).
[9]  Xu K,Milliman J D,Li A,Yangtze-and Taiwan-derived sediments on the inner shelf of East China Sea,Continental Shelf Research,2009(18).
[10]  Yancheva G,Nowaczyk N R,Mingram J,Influence of the intertropical convergence zone on the East Asian monsoon,Nature,2007.
[11]  Yang S Y,Jung H S,Lim D I,A review on the provenance discrimination of sediments in the Yellow Sea,Earth-Science Reviews,2003(1-2).
[12]  Yuan D,Zhu J,Li C,Cross-shelf circulation in the Yellow and East China Seas indicated by MODIS satellite observations,Journal of Marine Systems,2008(1-2).
[13]  Zhang CS. ;Wang LJ. ;Li GS. ;Dong SS. ;Yang JR. ;Wang XL.,Grain size effect on multi-element concentrations in sediments from the intertidal flats of Bohai Bay, China,Applied Geochemistry?,2002, 17(1).
[14]  Zheng Y,Kissel C,Zheng H B,Sedimentation on the inner shelf of the East China Sea:Magnetic properties,diagenesis and paleoclimate implications,Marine Geology,2010(1-4).
[15]  Zhou H,Guan H,Chi B,Record of winter monsoon strength,Nature,2007.
[16]  Zhou H,Wang B-S,Guan H,Constraints from strontium and neodymium isotopic ratios and trace elements on the sources of the sediments in Lake Huguang Maar,Quaternary Research,2009(2).
[17]  范德江,孙效功,杨作升..沉积物物源定量识别的非线性规划模型-以东海陆架北部表层沉积物物源识别为例[J].沉积学报,2002,(01):30-33.doi:10.3969/j.issn.1000-0550.2002.01.006.
[18]  李家彪,东海区域地质,北京:海洋出版社,2008.
[19]  刘健,朱日祥,李绍全..南黄海东南部冰后期泥质沉积物中磁性矿物的成岩变化及其对环境变化的响应[J].中国科学D辑,2003,(06):583-592.doi:10.3321/j.issn:1006-9267.2003.06.013.
[20]  秦蕴珊,赵一阳,陈丽蓉,东海地质,北京:科学出版社,1987.
[21]  孙晓燕,李广雪,刘勇..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,(04):11-17.
[22]  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,(06):581-587.doi:10.3321/j.issn:0029-814X.2000.06.001.
[23]  汪品先,穿凿地球系统的时间隧道,中国科学d辑,2009(10).
[24]  王可,郑洪波,Prins M..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,(04):1-10.
[25]  向荣,杨作升,郭志刚..济州岛西南泥质区粒度组分变化的古环境应用[J].地球科学-中国地质大学学报,2005,(05):582-588.doi:10.3321/j.issn:1000-2383.2005.05.010.
[26]  肖尚斌,黄朋,万世明..末次盛冰期以来长江入海历史的回顾与展望[J].中国石油大学学报(自然科学版),2003,(06):125-130.doi:10.3321/j.issn:1000-5870.2003.06.035.
[27]  肖尚斌,李安春,陈木宏,近8 ka东亚冬季风变化的东海内陆架泥质沉积记录,地球科学-中国地质大学学报,2005(5).
[28]  肖尚斌,李安春,蒋富清,近2 ka闽浙沿岸泥质沉积物物源分析,沉积学报,2005(2).
[29]  肖尚斌,李安春,刘卫国..闽浙沿岸泥质沉积的物源分析[J].自然科学进展,2009,(02):185-191.doi:10.3321/j.issn:1002-008X.2009.02.009.
[30]  徐方建,李安春,李铁刚..末次冰消期以来东海内陆架沉积物地球化学特征及其古环境意义[J].地球化学,2010,(03):240-250.
[31]  徐方建,李安春,李铁刚,末次冰消期以来东海内陆架沉积物磁化率的环境意义,海洋学报,2011(1).
[32]  徐方建,李安春,李铁刚,末次冰消期以来东海内陆架沉积速率及其气候环境响应,地层学杂志,2011(1).
[33]  徐方建,李安春,李铁刚,中全新世以来东海内陆架泥质沉积物来源,中国石油大学学报(自然科学版),2011(1).
[34]  徐方建,李安春,万世明,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,海洋学报,2009(3).
[35]  徐方建,李安春,万世明,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,地球科学-中国地质大学学报,2009(4).
[36]  徐方建,李安春,肖尚斌,末次冰消期以来东海内陆架古环境演化,沉积学报,2009(1).
[37]  An Z,Kukla G J,Porter S C,Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years,Quaternary Research,1991(1).
[38]  Chen, J ;Chen, Y ;Liu, LW ;Ji, JF ;Balsam, W ;Sun, YB ;Lu, HY,Zr/Rb ratio in the Chinese loess sequences and its implication for changes in the East Asian winter monsoon strength,Geochimica et Cosmochimica Acta?,2006, 70(6).
[39]  Jian Z,Wang P,Saito Y,Holocene variability of the Kuroshio Current in the Okinawa Trough,northwestern Pacific Ocean,Earth and Planetary Science Letters,2000(1).
[40]  Li C X,Zhang J Q,Fan D D,Holocene regression and the tidal radial sand ridge system formation in the Jiangsu coastal zone,east China,Marine Geology,2001(1-4).
[41]  Li C,Wang P,Sun H,Late Quaternary incised-valley fill of the Yangtze delta (China):its stratigraphic framework and evolution,Sedimentary Geology,2002(1-2).
[42]  Liu J P;Li A C;Xu K H;Velozzi D M Yang Z S Milliman J D DeMaster D J,Sedimentary features of the Yangtze Riverderived along-shelf clinoform deposit in the East China Sea,Continental Shelf Research? ,2006, 26(17-18).
[43]  Liu J P,Xu K H,Li A C,Flux and fate of Yangtze River sediment delivered to the East China Sea,Geomorphology,2007(3-4).
[44]  Liu J P,Xue Z,Ross K,Fate of sediments delivered to the sea by Asian large rivers:Long-distance transport and formation of remote alongshore clinothems,SEPM-The Sedimentary Record,2009(4).
[45]  Liu J,Li A,Chen M,Sedimentary changes during the Holocene in the Bohai Sea and its paleoenvironmental implication,Continental Shelf Research,2008(10-11).
[46]  Liu J;Saito Y;Wang H;Yang Z G,Nakashima R,Sedimentary evolution of the Holocene subaqueous clinoform off the Shandong Peninsula in the Yellow Sea,Marine Geology? ,2007, 236(3-4).
[47]  Liu J;Zhu R X;Roberts A P,High-resolution analysis of early diagenetic effects on magnetic minerals in post-middle-Holocene continental shelf sediments from the Korea Strait,Journal of Geophysical Research? ,2004, 109.
[48]  Liu S,Shi X,Liu Y,Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene,Chinese Science Bulletin,2010(21).
[49]  Qiao S,Yang Z,Liu J,Records of late-Holocene East Asian winter monsoon in the East China Sea:Key grain-size component of quartz versus bulk sediments,Quaternary International,2011(1-2).
[50]  Su C C,Huh C A,210Pb,137Cs and 239,240Pu in East china Sea sediments:Sources,pathways and budgets of sediments and radionuclides,Marine Geology,2002(1-4).
[51]  徐方建,李安春,徐兆凯,东海内陆架沉积物稀土元素地球化学特征及物源意义,中国稀土学报,2009(4).
[52]  徐方建,万世明,李安春..中国边缘海陆源沉积物粒度与矿物组成的关系[J].自然科学进展,2008,(11):1271-1278.doi:10.3321/j.issn:1002-008X.2008.11.009.
[53]  张晓东,许淑梅,翟世奎..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,(02):25-32.
[54]  赵泉鸿,翦知湣,张在秀,东海内陆架泥质沉积区全新世古环境变迁:有孔虫证据,海洋地质与第四纪地质,2009(2).
[55]  赵泉鸿,翦知湣,张在秀,东海陆架泥质沉积区全新世有孔虫和介形虫及其古环境应用,微体古生物学报,2009(2).
[56]  赵一阳,鄢明才,中国浅海沉积物地球化学,北京:科学出版社,1994.
[57]  郑妍,郑洪波,王可..末次冰期以来东海内陆架沉积反映的海平面变化[J].同济大学学报(自然科学版),2010,(09):1381-1386.doi:10.3969/j.issn.0253-374x.2010.09.025.

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