| 1,483 | 54 | 11 |
| Downloads | Citas | Reads |
浙江岸外东海内陆架MD06-3040柱状样完整保存有10.6cal.kaPB以来的全新世沉积记录,采取257个沉积物样品进行了有孔虫和介形虫定量分析。依据丰度上的优势成分和特征种的分布,识别出6个底栖有孔虫组合和4个介形虫组合。应用属种组合和不同生态(表生/内生、内陆架/中—内陆架、暖水)种的丰度,探讨了研究区全新世以来的古环境变迁。分析结果揭示了研究区全新世早期海面快速上升,沉积环境由滨岸内陆架(10.6—9.8cal.kaBP)、内陆架外缘(9.8—7.8cal.kaBP)转变至中陆架内侧并达全新世最高海面(7.8—3.4cal.kaBP)。台湾暖流在8.0cal.kaBP起开始发育,并在5.7—2.8和0.7—0cal.kaBP二个时期派生出明显的上升流。台湾暖流及其所派生的上升流是造成东海陆架泥质快速沉积的最主要原因。依据浮游有孔虫Globigerina bulloides的丰度变化,推测浙闽沿岸流在4.9—3.2cal.kaBP时期最为强盛。
Abstract：Core MD06-3040 was taken from the mud area off the Zhejiang-Fujian coast of the East China Sea(27°43.3663'N,121°46.8822'E,water depth 47 m,core length 19.36 m).A total of 257 samples were quantitatively analyzed for paleontological study of planktonic,benthic foramini-fera and ostracods as well as their paleoenvironmental implications.Holocene paleoenvironmental evolution since 10.6 cal.kaBP has been discussed by benthic foramini-feral and ostracod assemblages and some important ecological indicators(infaunal/epifaunal,inner-shelf/inner-middle shelf,warm-water species groups).Results show a rapid sea-level rise during the early Holocene from the inner inner-shelf(10.6—9.8 cal.kaBP),outer inner-shelf(9.8—7.8 cal.kaBP) to the middle shelf with the highest sea-level(7.8—3.4 cal.kaBP).The Taiwan Warm Current is suggested to be developed since 8.0 cal.kaBP and its derived upwelling appeared during the periods of 5.7—2.8 and 0.7—0 cal.kaBP respectively,resulting in the rapid mud depo-sition on the shelf of the East China Sea.The marked increase in abundance of planktonic foraminifera Globigerina bulloides is referred to the enhancement of the Zhejiang-Fujian Coast Current during 4.9—3.2 cal.kaBP.
王可,郑洪波,Prins M等,2008.东海内陆架泥质沉积反映的古环境演化.海洋地质与第四纪地质,28(4):1—10
王律江,1992.南海北部SO49-8KL柱状样底栖有孔虫及其古海洋学意义.业治铮,汪品先(主编),南海晚第四纪古海洋学研究.青岛:青岛海洋大学出版社.157—183
勾韵娴,郑淑英,黄宝仁,1983.广东雷琼地区上新世介形类动物群.中国古生物志,总号163册,新乙种第18号,1—134
肖尚斌,李安春,2005.东海内陆架泥区沉积物的环境敏感粒度组分.沉积学报,23(1):27—34
肖尚斌,李安春,蒋富清等,2004.近2ka来东海内陆架的泥质沉积记录及其气候意义.科学通报,49(21):2233—2238
肖尚斌,李安春,陈木宏等,2005.近8ka东亚冬季风变化的东海内陆架泥质沉积记录.地球科学,30(5):574—581
肖尚斌,李安春,蒋富清等,2005.近2ka闽浙沿岸泥质沉积物物源分析.沉积学报,23(2):265—274
何炎,胡兰英,王克良,1965.江苏东部第四纪有孔虫.中国科学院地质古生物研究所集刊,4:51—162
何炎,胡兰英,2001.广东雷州半岛上新世有孔虫.合肥:中国科学技术大学出版社.1—189
汪品先,章纪军,赵泉鸿等,1988.东海底质中的有孔虫和介形虫.北京:海洋出版社.1—438
郑守仪,1988.东海的胶结和瓷质有孔虫.北京:科学出版社.1—337
郑守仪,傅钊先,2001.中国动物志,粒网虫门,有孔虫纲,胶结有孔虫.北京:科学出版社.1—788
赵泉鸿,汪品先,1988.中国浅海现代介形虫的数量和属种分布.海洋与湖沼,19(6):553—561
赵泉鸿,瓦特立R,1988.对G.S.Brady(1869)香港介形虫的再研究.微体古生物学报,5(1):15—23
赵泉鸿,瓦特立R,1989.对J.T.Kingma(1948)印度尼西亚晚新生代介形虫新种的再研究,微体古生物学报,6(3):229—246
赵泉鸿,汪品先,1990.中国浅海现代介形虫的动物地理分区.海洋与湖沼,21(5):458—464
周保春,赵泉鸿,黄维等,1996.黄海西部介形虫分布再探.海洋学报,18(6):69—81
侯祐堂,陈德琼,杨恒仁等,1982.江苏地区白垩纪—第四纪介形虫动物群.北京:地质出版社.1—386
胡敦欣,杨作升,2001.东海海洋通量关键过程.北京:海洋出版社.3—13
胡敦欣,韩舞莺,章申等,2001.长江、珠江口及邻近海域陆海相互作用.北京:海洋出版社.137—153
秦蕴珊,郑铁民,1982.东海大陆架沉积物分布特征的初步探讨.中国科学院海洋研究所海洋地质研究室编,黄、东海地质.北京:科学出版社.39—51
秦蕴珊,赵一阳,陈丽蓉等,1987.东海地质.北京:科学出版社.1—290
B A W H,1977.An economical,zoogeographic and taxonomic re-viewof recent planktonic foraminifera.Oceanic Micropaleonto-logy,1:1—100
CORLISS B H,CHENC,1988.Morphotype patterns of NorwegianSea deep-sea benthic foraminifera and ecological i mplications.Geology,16:716—719
GOODAY AJ,1994.The biology of deep-sea foraminifera:A re-viewof some advances and their applications in paleoceanogra-phy.Palaios,9:14—31
GOU Y,ZHENG S,HUANG B,1983.Pliocene ostracode fauna ofLeizhou Peninsula and northern Hainan Island,GuangdongProvince.Palaeontol.Sinica,162(B),18:1—134
HE Y,HUL,2001.Pliocene Foraminifers fromthe Leizhou Penin-sula of Guangdong Province,China.Hefei:Press Univ.Sci.&Techn.China,1—189
HE Y,HU L,WANG K,1965.Quaternary foraminifera of theeastern Jiangsu Province.Mem.Inst.Geol.&Palaeont.Acad.Sinica,4:51—162
HOU Y,CHEN T,YANG Het al.,1982.Cretaceous—Quaterna-ry Ostracode Fauna fromJiangsu.Beijing:Geol.Publ.House.1—386
HU D,1984.Upwelling and sedi mentation dynamics I:the role ofupwelling in sedi mentation in the Yellow Sea and East ChinaSea.Oceanol.Li mnol.,2(1):12—19
HU D,YANG Z,2001.The Key Process of Marine Fluxes in EastChina Sea.Beijing:Ocean Press.3—13
HU D,HAN W,ZHANG Set al.,2001.Land Ocean Interactionin the Estuary of Changjiang River,Zhujiang River andits Con-tiguity Sea Area.Beijing:China Ocean Press.137—153
KAI HO K,1994.Benthic foraminiferal dissolved-oxygen index anddissolved-oxygen levels in the modern ocean.Geology,22:719—722
KAI HO K,1999.Effect of organic carbon and dissolved oxygen onthe benthic foraminiferal oxygenindex(BFOI).Mar.Micropa-leont.,37:67—76
LI UJ P,XU K H,LI A Cet al.,2007.Flux and Fate of YangtzeRiver Sedi ment Delivered to the East China Sea.Geomorpholo-gy,85:208—224
LOEBLICH A RJR,TAPPAN H,1994.Foraminifera of the Sahulshelf and Ti mor Sea.Cushman Foundation for ForaminiferalResearch,Special Pub.,31:1—661
MURRAYJ,2006.Ecology Applications of Benthic Foraminifera.Cambridge,1—426
QI N Y,ZHAO Y,CHEN Let al.,1987.Geology of the East China Sea.Beijing:China Sci.Press.1—290
QI N Y,ZHENG T,1982.Preli minary Study on Sedi ments Distri-butionin the Inner Shelf of the East China Sea.In:Depart mentof the Marine Geology of Institute of Oceanology,ChineseAcademy of Sciences,Geology of the Yellow Sea and the EastChina Sea.Beijing:Science Press.39—51
SCOURSE J,AUSTI N W,LONG Bet al.,2002.Holocene evolu-tion of seasonal stratificationin the Celtic Sea:refined age mod-el,mixing depths and foraminiferal stratigraphy.Mar.Geo-logy,191:119—145
WANG K,ZHENG H,PRI NS Met al.,2008.High-resolution pa-leoenvironmental record of the mud sedi ments of the East ChinaSea inner shelf.Mar.Geol.&Quatern.,28(4):1—10
WANG L,1992.Late Quaternary deepsea benthic foraminifera inthe northern South China Sea andtheir paleoceanographici mpli-cations.In:YE Z,WANG P(eds.),Contributions to LateQuaternary Paleoceanography of the South China Sea.Qing-dao:Qingdao Ocean Univ.Press.157—183
WANG Pet al.,1985.Marine Micropaleontology of China.Bei-jing:China Ocean Press.1—370
WANG P,ZHANGJ,ZHAO Qet al.,1988.Foraminifera and Os-tracoda in Bottom Sedi ments of the East China Sea.Beijing:China Ocean Press.1—438
WHATLEY R,ZHAO Q,1987.Recent Ostracoda of the MalaccaStraits.Revista Espan ola de Micropaleontologia,19(3):327—366
WHATLEY R,ZHAO Q,1988.Recent Ostracoda of the MalaccaStraits.Revista Espan ola de Micropaleontologia,20(1):5—37
XI AO S,LI A,2005.A study on environmentally sensitive grainsize populationininner shelf of the East China Sea.Acta Sedi-mentol.Sinica,23(1):27—34
XI AO S,LI A,CHEN Met al.,2005.Recent8ka mud records ofthe East Asian winter monsoon fromthe inner shelf of the EastChina Sea.Earth Sci.——Journal of China Univ.of Geosci.,30(5):574—581
XI AO S,LI A,JI ANG Fet al.,2004.The2ka record and its cli-mate significance of the mud area of inner shelf of the East Chi-na Sea.Chinese Sci.Bull.,49(21):2233—2238
XI AO S,LI A,JI ANG Fet al.,2005.Provenance analysis of mudalong the Min-Zhe coast since2kaBP.Acta Sedi mentol.Sinica,23(2):265—274
XU X,ODA M,1999.Surface-water evolution of the eastern EastChina Sea during the last36,000years.Mar.Geology,156:285—304
YASSI NI L,JONES B,1995.Foraminifera and Ostracoda fromes-tuarine and shelf environments on the southeastern coast ofAustralia.Australia:The University of Wollongong Press.1—484
ZHAO Q,WANG P,1988.Modern Ostracodin sedi ments of shelfseas off China:Quantitative and qualitative distributions.Oceanol.Li mnol.Sinica,19(6):553—561
ZHAO Q,WHATLEY R,1988.The genusNeomonoceratina(Crustacea:Ostracoda)fromthe Cainozoic of the West Pacificmargins.Acta Oceanologica Sinica,7(4):562—577
ZHAO Q,WHATLEY R,1988.Arestudy of Brady’s1869Ostra-coda of Hongkong.Acta Micropalaeontologica Sinica,5(1):15—23
ZHAO Q,WHATLEY R,1989.Ataxonomic revision of the newspecies of Ostracoda described by J.T.Kingma(1948)fromthe Late Cainozoic of Indonesia.Acta Micropalaeontologica Sini-ca,6(3):229—246
ZHAO Q,WANG P,1990.Modern Ostracodain shelf seas off Chi-na:zoogeographical zonation.Oceanol.Li mnol.Sinica,21(5):458—464
ZHAO Q,WHATLEY R,ZHOUB,2000.The taxonomy and dis-tribution of recent species of the ostracod genusCytheropteronin the South China Sea.Revista Espan ola de Micropaleontolo-gia,32(2):259—281
ZHENG S,1988.The Agglutinated and Porcelaneous Foraminiferaof the East China Sea.Beijing:Sci.Press.1—337
ZHENG S,FU Z,2001.Fauna Sinica,Phylum Granuloreticulosa,Glass Foraminiferea,Agglutinated Foraminifera.Beijing:Sci.Press.1—788
ZHOU B,ZHAO Q,HUANG Wet al.,1996.Arestudy of ostra-cod distributionin the western YellowSea.Acta Oceanol.Sini-ca,18(6):69—81
Basic Information:
DOI：
China Classification Code:Q915
Citation Information:
[1]赵泉鸿,翦知湣,张在秀等.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[J].微体古生物学报,2009,26(02):117-128.
Fund Information:
上海科委科研计划项目(07DZ14003);; 国家973项目(2007CB815901);; 国家自然科学基金(40276017)资助