THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka

XU Taoyu; SHI Xuefa; LIU Shengfa; QIAO Shuqing; YANG Gang; WANG Guoqing; WANG Kunshan; WANG Xuchen

doi:10.3724/SP.J.1140.2012.06149

Marine Geology & Quaternary Geology > 2012 > 32(6): 149-158. > DOI: 10.3724/SP.J.1140.2012.06149

XU Taoyu, SHI Xuefa, LIU Shengfa, QIAO Shuqing, YANG Gang, WANG Guoqing, WANG Kunshan, WANG Xuchen. THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 149-158. DOI: 10.3724/SP.J.1140.2012.06149

Citation:

PDF (1040 KB)

THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka

1 Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
2 First Institute of Oceanography, State Oceanic Administration, Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology, Qingdao 266061, China;
3 China University of Geosciences(Wuhan), Wuhan 430074, China;
4 University of Massachusetts, Boston 02125, American

More Information

Received Date: August 11, 2012
Revised Date: October 05, 2012

Graphical Abstract

Abstract

Abstract

A climatic proxy system is constructed on the basis of the color reflectance data of the core MZ01 using first derivative and factors analysis method, and a high-resolution climatic sequence is established with the support of AMS¹⁴C dating data for the past 2 ka.900AD is the key turning-point in the course of climate evolution.Climate became significantly cold with high-frequency but low amplitude temperature fluctuation right after 900AD.In the past 2 ka,the climate in East China has experienced four stages including a cold stage before 580AD,a warm stage between 580 and 900AD,a temperature fluctuation stage between 900 and 1460AD and a cold stage between 1460 and 1880AD.Each stage includes some secondary regional or global temperature fluctuations.
- mud area,
- color reflectance,
- East Asia monsoon,
- climate,
- inner shelf of the East China Sea

FullText(HTML)

References (63)

References

[1]	向荣,杨作升,Y Saito,等.济州岛西南泥质区近2300 a来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.East Asia Winter Monsoon change of recent 2300a recorded by environmental sensitive grain-size population change in the mud area southwest off Cheju Island, ECS[J].Science in China (Series D), 2006, 36(7):654-662.]
[2]	向荣,杨作升,郭志刚,等.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,2005,30(5):582-588. [XIANG Rong, YANG Zuo sheng, GUO Zhigang, et al.Paleoenvironmental implications of grain-size component variations in the mud area Southwest off Cheju Island, ECS[J].Earth Science-Journal of China University of Geosciences, 2005, 30(5):582-588.]
[3]	Liu Xiaohong, Qin Dahe, Shao Xuemei,et al.Temperature variations recorded in tree-rings of Middle Qilian Mountains during the Last Millennium[J].Science in China (Series D), 2005, 8:521-529.
[4]	邵雪梅,黄磊,刘洪滨,等.树轮记录的青海德令哈地区千年降水变化[J].中国科学D辑,2004,34(2):145-153. [SHAO Xuemei, HUANG Lei, LIU Hongbin,et al.Reconstruction of precipitation variation from tree ring in recent 1000 years in Delingha, Qinghai[J].Science in China(Series D), 2004,34(2):145-153.]
[5]	杨保,康兴成,施雅风.近2000年都兰树轮10年尺度的气候变化及其与中国其它地区温度代用资料的比较[J].地理科学,2000,20(5):397-402. [YANG Bao, KANG Xingcheng, SHI Yafeng.Decadal climatic variations indicated by Dulan tree-ring and the comparison with temperature proxy data from other regions of China during the last 2000 years[J].Scientia Geographica Sinica, 2000, 20(5):397-402.]
[6]	姚檀栋,杨志红,皇翠兰,等.近2 ka来高分辨率的连续气候环境变化记录-古里雅冰心近2 ka记录初步研究[J].科学通报,1996,41(2):1103-1106. [YAO Tandong, YANG Zhihong, HUANG Cuilan, et al.Successive high-resolution climate and environment changes of the past about 2000 years recorded in Guliya ice core[J].Chinese Science Bulletin, 1996,41(12):1103-1106.]
[7]	洪业汤,姜洪波,陶发祥,等.近5 ka温度的金川泥炭δ¹⁸O记录[J].中国科学D辑,1997, 27(6):525-530. [HONG Yetang, JIANG Hongbo, TAO Faxiang, et al.δ¹⁸O records of temperature about 5 ka from peat in Jinchuan[J].Science in China (Series D), 1997,27(6):525-530.]
[8]	徐海,洪业汤,林庆华,等.红原泥炭纤维素氧同位素指示的距今6 ka温度变化[J].科学通报,2002,47(15):1181-1186. [XU Hai, HONG Yetang, LIN Qinghua, et al.Temperature variations in the past 6000 years inferred from δ¹⁸O of peat cellulose from Hongyuan, China[J].Chinese Science Bulletin, 2002, 47(18):1578-1584.]
[9]	卫克勤,林瑞芬.祁连山敦德冰心氧同位素剖面的古气候信息探究[J].地球化学,1994,23(4):311-320. [WEI Keqin, LIN Ruifen.An enquiry into paleoclimatic information from oxygen isotopic profile in Dunde ice core in Qilianshan[J].Geochimica, 1994, 23(4):311-320.]
[10]	马志邦,李红春,夏明,等.距今3 ka来京东地区的古温度变化:石笋Mg/Sr记录[J].科学通报,2002,47(23):1829-1834. [MA Zhibang, LI Hongchun, XIA Ming.et al.Paleotemperature changes over the past 3000 years in eastern Beijing, China:A reconstruction based on Mg/Sr records in a stalagmite[J].Chinese Science Bulletin, 2002, 48(4):395-400.]
[11]	竺可桢.中国近五千年来气候变迁的初步研究[J].中国科学,1973(2):168-189.[ZHU Kezhen.Study on the climate change of China during the last 5 ka[J].Science in China, 1973(2):168-189.]
[12]	葛全胜,郑景云,满志敏,等.过去2000年中国温度变化研究的几个问题[J].自然科学进展,2004,14(4):449-455. [GE Quansheng, ZHENG Jingyun, MAN Zhimin, et al.Key points on temperature change of the past 2000 years in China[J].Progress in Natural Science, 2004,14(4):449-455.]
[13]	刘健,李绍全,王圣洁,等.末次冰消期以来黄海海平面变化与黄海暖流的形成[J].海洋地质与第四纪地质,1999,19(1):13-24. [LIU Jian, LI Shaoquan, WANG Shengjie,et al.Sea level changes of the Yellow Sea and formation of the Yellow sea warm current since the last deglaciation[J].Marine Geology and Quaternary Geology,1999,19(1):13-24.]
[14]	肖尚斌,李安春,蒋富清,等.近2 ka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.Recent 2000 year geological records of mud in the inner shelf of the East China Sea and their climatic implications[J].Chinese Science Bulletin, 2004,49(21):2233-2238.]
[15]	王顺华,张国栋,张纪双, 等.东海内陆架泥质沉积Rb和Sr的地球化学及其古气候意义[J].科技导报,2007,25(3):22-27. [WANG Shunhua, ZHANG Guodong, ZHANG Jishuang, et al.Geochemical studies on Rb and Sr in the mud on the inner shelf of the East China Sea and their palaeoclimate significance[J].Science and Technology Review,2007, 25(3):22-27.]
[16]	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):26-32. [ZHANG Xiaodong,XU Shumei,ZHAI Shikui,et al.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):26-32.]
[17]	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,2010,55(21):2306-2314.
[18]	Barranco F T, Balsam W L, Deaton B C.Quantitative reassessment of brick red lutites:Evidence from reflectance spectrophotometry[J].Marine Geology,1989,89:299-314.
[19]	J I J F, Balsam W L, Chen J.Mineralogic and climatic interpretations of the Luochuan loess section (China) based on diffuse reflectance spectrophotometry[J].Quaternary Research, 2001,56:23-30.
[20]	黄维, 翦知湣, Bǘhring C.南海北部ODP 1144站颜色反射率揭示的千年尺度气候波动[J].海洋地质与第四纪地质,2003,23(3):5-10. [HUANG Wei, JIANG Zhimin, Bühring C.The Millennial-scale climate fluctuations revealed by the records of color reflectance from ODP site 1144 in the northern South China Sea[J].Marine Geology and Quaternary Geology,2003,23(3):5-10.]
[21]	刘连文,郑洪波,翦知湣.南海沉积物漫反射光谱反映的220 ka以来东亚夏季风变迁[J].地球科学-中国地质大学学报, 2009, 30(5):543-549. [LIU Lianwen, ZHENGg Hongbo, JIAN Zhimin.Visible reflectance record of South China Sea sediments during the past 220 ka and its implications for East Asian monsoon variation[J].Earth Science-Journal of China University of Geosciences, 2005, 30(5):543-549.]
[22]	王昆山,石学法,王国庆.南黄海陆架沉积物颜色反射率的初步研究[J].海洋科学进展,2006,24(1):30-38. [WANG Kunshan, SHI Xuefa, WANG Guoqing.A preliminary study on the sediment color reflectance in the Southern Yellow Sea shelf area[J].Advances in Marine Science, 2006, 24(1):30-38.]
[23]	王昆山,石学法,程振波,等.南黄海陆架中部沉积物反射率光谱的影响因素分析[J].海洋科学进展, 2007, 25(1):46-53. [WANG Kunshan, SHI Xuefa, CHENG Zhenbo, et al.Analysis of affecting factors for reflectance spectra of sediments from the central shelf area of the southern Yellow Sea[J].Advances in Marine Science, 2007, 25(1):46-53.]
[24]	Giosan L, Flood R D, Aller R C.Paleoceanographic significance of sediment color on western North Atlantic drifts:I.Origin of color[J].Marine Geology, 2002,189:25-41.
[25]	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.
[26]	杨作升,郭志刚,王兆祥,等.黄东海及其毗邻海域悬浮体与水团的对应关系及其影响因素[J].青岛海洋大学学报,1991,25(3):55-69. [YANG Zuosheng, GUO Zhigang, WANG Zhaoxiang, et al.Suspended matter in the Huanghai Sea and East China Sea:its contents, distribution, relation to the water masses and factors of influence[J].Journal of Ocean University of Qingdao,1991,25(3):55-69.]
[27]	杨作升,郭志刚,王兆祥,等.黄东海陆架悬浮体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.Macro-configuration of the suspended particulate matter transport on the Yellow and East China Sea shelf to its eastern sea area[J].Acta Oceanologica Sinica, 1992,14(2):81-90.]
[28]	Milliman J D, Bestdsley K C, Yang Z S, et al.Modern Huanghe derived on the outer shelf of the East China Sea:identification and potential mud-transport mechanisms[J].Cont Shelf Research,1985,4:175-188.
[29]	肖尚斌,李安春,蒋富清,等.近2ka闽浙沿岸泥质沉积物物源分析[J].沉积学报,2005,23(2):268-274. [XIAO Shangbin, LI Anchun, JIANG Fuqing, et al.Provenance analysis of mud along the Min-zhe coast since 2 kaBP[J].Acta Sedimentologica Sinica, 2005, 23(2):268-274.]
[30]	金元欢.我国入海河口的基本特点[J].东海海洋,1988,6(3):1-11. [JIN Yuanhuan.The characteristics of estuarine in China[J] Donghai Marine Science, 1988, 6(3):1-11.]
[31]	秦蕴珊,赵一阳,陈丽蓉,等.东海地质[M].北京:科学出版社,1987:7.[QIN Yunshan, ZHAO Yiyang, CHEN Lirong,et al.Geology of the East China Sea[M].Beijing:Science Press, 1987:7.]
[32]	胡敦欣,杨作升.东海海洋通量关键过程[M].北京:海洋出版社,2001:3-13.[HU Dunxin,YANG Zuosheng.Margin Flux in the East China Sea[M].Beijing:Ocean Press,2001:3 -13.]
[33]	Su J L.A review of circulation dynamics of the coastal oceans near China[J].Acta Oceanonlogica Sinica,2001,23(4):1-16
[34]	Yoneda M, Uno H, Shibata Y, et al.Radiocarbon marine reservoir ages in the western Pacific estimated by pre-bomb molluscan shells[J].Nuclear Instruments and Methods in Physics Research B,2007,259:432-437.
[35]	季峻峰,陈骏,W Balsam,等.黄土剖面中赤铁矿和针铁矿的定量分析与气候干湿变化研究[J].第四纪研究,2007,27(2):221-229. [JI Junfeng, CHEN Jun, W Balsam,et al.Quantitative analysis of hematite and goethite in the Chinese loess-paleosol sequences and its implication for dry and humid variability[J].Quaternary Sciences,2007,27(2):221-229].
[36]	沈振兴,张小曳,季峻峰,等.大气粉尘气溶胶中铁氧化物的光谱分析[J].海洋地质与第四纪地质, 2003,23(1):103-107. [SHEN Zhenxing, ZHANG Xiaoye, JI Junfeng, et al.Spectroscopy analysis of iron oxide in mineral aerosols[J].Marine Geology and Quaternary Geology, 2003, 23(1):103-107.]
[37]	黄维,刘志飞,陈晓良,等.寻求深海碳酸盐沉积含量的物理标志[J].地球科学-中国地质大学学报,2003,28(2):157-162. [HUANG Wei, LIU Zhifei, CHENG Xiaoliang, et al, Searching physical indicators of carbonate contents of deep sea sediments[J].Earth Science-Journal of China University of Geosciences, 2003, 28(2):157-162.]
[38]	谢巧勤,陈天虎,徐晓春,等.中国黄土中磁性矿物赋存形式研究[J].中国科学D辑,2008, 38(11):1404-1412. [XIE Qiaoqin, CHEN Tianhu, XU Xiaochun, et al.Transformation relationship among different magnetic minerals within loess paleosol sediments of the Chinese Loess Plateau[J].Science in China(Series D), 2009,52(3):313-322.]
[39]	葛全胜, 郑景云, 满志敏,等.过去2000年中国东部冬半年温度变化序列重建及初步分析[J].地学前缘,2002,9(2):169-181. [GE Quansheng, ZHENG Jingyun, MAN Zhimin, et al.Reconstruction and analysis on the series of winter-half-year temperature changes over the past 2000 years in eastern China[J].Earth Science Frontiers, 2002, 9(1):169-181.]
[40]	Stuiver M, Pieter M Grootes.GISP2 oxygen isotope ratios[J].Quaternary Research, 2000,53:277-284.
[41]	满志敏.唐代气候冷暖分期及各期气候冷暖特征的研究[J].历史地理,1990(8):1215.[MAN Zhimin.Study on the cold/warm stages of Tang Dynasty and the characteristics of each cold/warm stage[J].Historical Geography, 1990(8 ):1215.]
[42]	满志敏.关于唐代气候冷暖问题的讨论[J].第四纪研究,1998,18(1):20-30. [MAN Zhimin.Climate in Tang Dynasty of China discussion for its evidence[J].Quaternary Sciences,1998,18(1):20-30.]
[43]	吴宏岐,党安荣.隋唐时期气候冷暖特征与气候波动[J].第四纪研究,1998, 18(1):31-36. [WU Hongqi, DANG Anrong.Fluctuation and characteristics of climate change in temperature of Sui-Tang times in China[J].Quaternary Sciences, 1998,18(1):31-36.]
[44]	Shi Yafeng, Yao Tandong, Yang Bao.Decadal climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years[J].Science in China (Series D), 1999(S1):93-102.
[45]	高建慧,刘健,王苏民.中国中世纪暖期气候研究综述[J].地理科学, 2006, 26(3):376-383. [GAO JianHui, LIU Jian, WANG Sumin.Overview on studies of Medieval Warm Period in China[J].Scientia Geographica Sinica, 2006, 26(3):376-383.]
[46]	任国玉,张兰生.中世纪温暖期气候变化的花粉化石记录[J].气候与环境研究,1996,1(1):81-86. [REN Guoyu, ZHANG Lansheng.Climate of the Medieval warm period in Maili region as inferred from pollen record[J].Climmatic and Environmental Research, 1996,1(1):81-86.]
[47]	满志敏.中世纪温暖期我国华东沿海海平面上升与气候变化的关系[J].第四纪研究,1999(1):90.[MAN Zhimin.Relationship between the sea-level rising of East China and climate changing during the Medieval Warm Period[J].Quaternary Sciences, 1999(1 ):90.]
[48]	王绍武,谢志辉,蔡静宁,等.近千年全球平均气温变化的研究[J].自然科学进展,2002,12(11):1145-1149. [WANG Shaowu, XIE Zhihui, CAI Jingning, et al.Study on the change of global mean temperature during last millennium[J].Progress in Natural Science, 2002,12(11):1145-1149.]
[49]	Wang S, Gong D.Climate in China during the four special periods in Holocene[J].Prog.Nat.Sci.,2000, 10(5):379-386.
[50]	金章东,沈吉,王苏民,等.岱海的"中世纪暖期"[J].湖泊科学,2002,14(3):209-216. [JIN Zhangdong, SHEN Ji, WANG Sumin, et al.The Medieval Warm Period in the Daihai area[J].Journal of Lake Sciences, 2002,14(3):209-216.]
[51]	施雅风,孔昭宸,王苏民,等.中国全新世大暖期的气候波动与重要事件[J].中国科学B辑, 1992(12):1300-1308.[SHI Yafeng, KONG Zhaochen, WANG Sumin, et al.The climate fluctuate and important events of Holocene Optimum in China[J].Science in China (Series B),1992 , 22(12):1300-1308.]
[52]	张丕远.中国历史气候变化[M].济南:山东科学技术出版社,1996.[ZHANG Piyuan.Climate Change in China During Historical Times[M].Jinan:Shandong Science and Technology Press, 1996.]
[53]	满志敏,张修桂.中国东部中世纪温暖期的历史证据和基本特征的初步研究[C]//中国生存环境历史演变规律研究(一).北京:海洋出版社,1993:95-103.[MAN Zhimin, ZHANG Xiugui.Research on the documental evidence and the characteristics of MWP in the east part of China[C]//Research on the past life-supporting environmental change of China.Beijing:China Ocean Press, 1993:95 -103.]
[54]	葛全胜,郑景云,方修琦,等.过去2000年中国东部冬半年的温度变化幅度研究[J].第四纪研究,2002,22(2):166-173. [GE Quansheng, ZHENG Jingyun, FANG Xiuqi, et al.Temperature changes of winter-half-year in Eastern China during the past 2000 years[J].Quaternary Sciences, 2002, 22(2):166-173.]
[55]	郑景云,王绍武.中国过去2000年气候变化的评估[J].地理学报,2005,60(1):21-31. [ZHENG Jingyun, WANG Shaowu.Assessment on climate change in china for the last 2000 Years[J].Acta Geographica Sinica, 2005, 60(1):21-31.]
[56]	Lamb H H.Climate, Present, Past and Future[M].London:Methuen,1977:835.
[57]	王绍武.小冰期气候的研究[J].第四纪研究,1995,3:202-212.[WANG Shaowu.Studies on climate of the Little Ice Age[J].Quaternary Sciences, 1995 , 3:202-212.]
[58]	李明启,靳鹤龄,张洪.小冰期气候的研究进展[J].中国沙漠,2005,25(5):731-737. [LI Mingqi, JIN Heling, ZHANG Hong.Advances of climate research in the Little Ice Age[J].Journal of Desert Research, 2005, 25(5):731-737.]
[59]	王绍武,叶瑾琳,龚道溢.中国小冰期的气候[J].第四纪研究,1998,18(1):54-63. [WANG Shaowu, YE Jinlin, GONG Daoyi.Climate in china during the Little Ice Age[J].Quaternary Sciences, 1998, 18(1):54-63.]
[60]	何起祥.中国海洋沉积地质学[M].北京:海洋出版社, 2006:38-44.[HE Qixiang.Marine Sedimentary Geology of China[M].Beijing:Ocean Press,2006:38 -44.]
[61]	姜在兴.沉积学[M].北京:石油工业出版社,2003:36-43.[JIANGg Zaixing.Sedimentology[M].Beijing:Petroleum Industry Press, 2003:36 -43].
[62]	范代读,王扬扬,吴伊婧.长江沉积物源示踪研究进展[J].地球科学进展,2012,27(5):515-528. [FAN Daidu,WANG Yangyang, WU Yijing.Advances in provenance studies of Changjiang Riverine sediments[J].Advances in Earth Science, 2012, 27(5):515-528.]
[63]	孟庆勇,李安春,徐方建.东海泥质区EC2005孔的磁学记录及其还原成岩作用的影响[C]//中国地球物理(2009).2009:407.[MENG Qingyong, LI Anchun, XU Fangjian.Early diagenesis in the inner shelf of the East China Sea sediments characterized by rock-magnetic indices[C]//The Chinese Geophysics (2009).2009:407.]

[1]	DUAN Haoyi, MAO Judong, CHENG Peng, REN Xiaolin, FAN Dejiang. Clay minerals and detrital minerals in clay fraction from the Changjiang River estuary and inner continental shelf of the East China Sea and their provenance indication[J]. Marine Geology & Quaternary Geology, 2024, 44(5): 119-128. DOI: 10.16562/j.cnki.0256-1492.2023092102
[2]	CONG Shuai, WU Xiao, QI Fukang, BI Naishuang, LI Yunhai, LI Dongyi, WANG Houjie. Cross-shelf sediment transport and its regulatory mechanisms on the inner shelf of the East China Sea during typhoon events[J]. Marine Geology & Quaternary Geology, 2024, 44(5): 38-49. DOI: 10.16562/j.cnki.0256-1492.2024070202
[3]	ZHAO Song, CHANG Fengming, LI Tiegang, XU Ye. THE APPLICATION OF GRAIN-SIZE END MEMBER ALGORITHM TO PALEOENVIRONMENTAL RECONSTRUCTION ON INNER SHELF OF EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 187-196. DOI: 10.16562/j.cnki.0256-1492.2017.03.019
[4]	LI Xiaoyan, JIAN Zhimin, SHI Xuefa, LIU Shengfa. HOLOCENE FORAMINIFERA FROM THE MUD AREA OF THE INNER SHELF,EAST CHINA SEA AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 61-71. DOI: 10.3724/SP.J.1140.2012.04061
[5]	ZHU Aimei, LIU Jihua, ZHANG Hui, BAI Yazhi, CUI Jingjing, LIU Shengfa. DISTRIBUTION PATTERN OF REES IN THE INNER-SHELF MUD AREA OF EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 1-10. DOI: 10.3724/SP.J.1140.2012.01001
[6]	LIU Shengfa, SHI Xuefa, LIU Yanguang, ZHU Aimei, YANG Gang. SEDIMENTATION RATE OF MUD AREA IN THE EAST CHINA SEA INNER CONTINENTAL SHELF[J]. Marine Geology & Quaternary Geology, 2009, 29(6): 1-7. DOI: 10.3724/SP.J.1140.2009.06001
[7]	ZHAO Quanhong, JIAN Zhimin, ZHANG Zaixiu, CHENG Xinrong, WANG Ke, ZHENG Hongbo. HOLOCENE PALEOENVIRONMENTAL CHANGES OF THE INNER-SHELF MUD AREA OF THE EAST CHINA SEA: EVIDENCE FROM FORAMINIFERAL FAUNAS[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 75-82. DOI: 10.3724/SP.J.1140.2009.02075
[8]	LIU Shengfa, LIU Yanguang, ZHU Aimei, LI Chaoxin, SHI Xuefa. GRAIN SIZE TRENDS AND NET TRANSPORT PATTERNS OF SURFACE SEDIMENTS IN THE EAST CHINA SEA INNER CONTINENTAL SHELF[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 1-6. DOI: 10.3724/SP.J.1140.2009.01001
[9]	WANG Ke, ZHENG Hong-bo, Maarten Prins, ZHENG Yan. HIGH-RESOLUTION PALEOENVIRONMENTAL RECORD OF THE MUD SEDIMENTS OF THE EAST CHINA SEA INNER SHELF[J]. Marine Geology & Quaternary Geology, 2008, 28(4): 1-10. DOI: 10.3724/SP.J.1140.2008.03001
[10]	ZHANG Xiao-dong, XU Shu-mei, ZHAI Shi-kui, ZHANG Huai-jing. THE INVERSION OF CLIMATE INFORMATION FROM THE SEDIMENT OF INNER SHELF OF EAST CHINA SEA USING END-MEMBER MODEL[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 25-32.

Cited By

Get Citation

PDF

XML

Article views (2296) PDF downloads (81)

Turn off MathJax

Article Contents

Abstract

References

THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka

Abstract

References

Related Articles

Catalog

Links

About Journal

Contact Us

THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka

Abstract

References

Related Articles

Catalog

Links

About Journal

Contact Us

Export File

Citation

Format

Content