Hsueh Y,Lie H J,Ichikawa H.On the branching of the Kuroshiowest of Kyushu.Journal of Geophysical Research,1996,101(C2):3851～3857
[2]
Fairbanks R G A.17,0002year glacio eustatic sea level record:Influence of glacial melting rates on the Younger Dryas event anddeep ocean circulation.N ature,1989,342:637～642
[3]
Ujiie H,Tanaka Y,Ono T.Late Quaternary paleoceanographicrecord from the middle Ryukyu Trench slope,Northwest Pacific.M arineM icropaleontology,1991,18:115～128
[4]
Ujiie H,Ujiie Y.Late Quaternary course changes of the KuroshioCurrent in the Ryukyu Arc region,Northwestern Pacific Ocean.M arineM icropaleontology,1999,37(1):23～40
[5]
Li T G,Liu Z X,Michael A et al.Heinrich event imp rints in theOkinawa Trough:Evidence from oxygen isotope and p lanktonicforaminifera.Palaeogeography,Palaeoclim atology,Palaeoecology,2001,176(1～4):133～146
[6]
杨永亮,刘振夏,沈承德等.南黄海、东海陆架及冲绳海槽北部沉积物10Be及9Be记录.第四纪研究,2007,27(4):529～538Yang Yongliang,Liu Zhenxia,Shen Chengde et a l.Be isotopes insurface sediments from the southern Yellow Sea,the East China Seacontinental shelf and in a sediment core from the northern OkinawaTrough.Qua terna ry S ciences,2007,27(4):529～538
[7]
李铁刚,孙荣涛,张德玉等.晚第四纪对马暖流的演化和变动:浮游有孔虫和氧碳同位素证据.中国科学(D 辑),2007,37(5):660～669Li Tiegang,Sun Rongtao,ZhangDeyu et al.Evolution and variationof the Tsushimawarm current during the LateQuaternary:Evidencesfrom p lanktonic foraminifera,oxygen and carbon isotopes.Science inChina(SeriesD),2007,50(5):725～735
[8]
Thunell R C,Reynolds L A.Sedimentation of p lanktic fora2minifera:Seasonal changes in species flux in the Panama Basin.M icropaleontology,1984,30:243～262
[9]
YamasakiM,Oda M.Sedimentation of p lanktonic foraminifera inthe East China Sea:Evidence from a sediment trap experiment.M arineM icropaleotology,2003,49(1):3～20
[10]
施雅风,孔昭宸主编.中国全新世大暖期气候与环境.北京:海洋出版社,199211～18Shi Yafeng,Kong Zhaochen eds.The Climates and Environments ofHolocene Megathermal in China.Beijing:China Ocean Press,1992.1～18
[11]
蓝淑芳,顾传晟,傅秉照.南黄海暖流水附近冷水块的分析研究.海洋科学集刊,1986,27:54～64Lan Shufang,Gu Chuansheng,Fu Bingzhao.A study of cold waterbody near the Southern Yellow Sea warm current water.S tudiaM arina S inica,1986,27:54～64
[12]
汪品先.西太平洋边缘海末次冰期古海洋学的比较研究.见: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,1992.308～321Wang Pinxian.West Pacific marginal seas in the last glaciation:Apaleoceanographic comparison.In:Ye Zhizheng,Wang Pinxianeds.Contributions to Late Quaternary Paleoceanography of the SouthChina Sea.Qingdao:Qingdao Ocean University Press,1992.308～321
[13]
Ujiie Y,Ujiie H,Taira A et al.Spatial and temporal variability ofsurface water in the Kuroshio source region,Pacific Ocean,over thepast 21000 years:Evidence from p lanktonic foraminifera.M arineM icropaleontology,2003,49(4):335～364
[14]
翦知湣,Saito Y,汪品先等.黑潮主流轴近两万年来的位移.科学通报,1998,43(5):532～536J ian Zhimin,Saito Y,Wang Pinxian et al.Shifts of the Kuroshioaxis over the last 20000 years.Chinese Science B ulletin,1998,43(12):1053～1056
[15]
李铁刚,阎 军,苍树溪.冲绳海槽北部Rd282和Rd286孔氧同位素记录及其古环境分析.海洋地质与第四纪地质,1996,16 6期李铁刚等:末次冰消期以来东黄海暖流系统的演化 953(2):57～64Li Tiegang,Yan Jun,Cang Shuxi.Oxygen isotope records andpaleoenvironment analysis in core Rd282 and core Rd286 in the northof the Okinawa Trough.M arine Geology & Quaternary Geology,1996,16(2):57～64
[16]
Xu X D,Motoyosh O.Surface2water evolution of the eastern EastChina Sea during the last 36000 years.M arine Geology,1999,156:285～304
[17]
Ijiri A,Wang L J,Oba T et al.Paleoenvironmental changes in thenorthern area of the East China Sea during the past 42,000 years.Palaeogeography,Palaeoclim atology,Palaeoecology,2005,219(3～4):239～261
[18]
Kawahata H,Ohshima H.Vegetation and environmental record inthe northern East China Sea during the Late Pleistocene.Global andPlanetary Change,2004,41(3～4):251～273
[19]
刘 健,李绍全,王圣洁等.末次冰消期以来南黄海海平面变化与黄海暖流的形成.海洋地质与第四纪地质,1999,19(1):13～24Liu J ian,Li Shaoquan,Wang Shengjie et al.Sea level changes ofthe Yellow Sea and formation of the Yellow sea warm current sincethe last deglaciation.M arine Geology & Quaternary Geology,1999,19(1):13～24
[20]
李铁刚,李绍全,苍树溪等.YSDP102钻孔有孔虫动物群与南黄海东南部古水文重建.海洋与湖沼,2000,31(6):588～595Li Tiegang,Li Shaoquan,Cang Shuxi et al.Paleo2hydrologicalreconstruction of the Southern Yellow Sea inferred from foraminiferalfauna in Core YSDP102.Oceanologia et L im nologia S inica,2001,31(6):588～595
[21]
Lie H J,Cho C H.Recent advantages in understanding thecirculation and hydrography of the East China Sea.FisheriesOceangraphy,2002,11(6):318～328
[22]
StuiverM,Reimer P J,Bard E et al.INTCAL98 Radiocarbon agecalibration 240000～0 cal.B.P.Radiocarbon,1998,40:1041～1083
[23]
Laj C,Mazaud A,Dup lessy J C.Geomagnetic intensity and 14Cabundance in the atmosphere and ocean during the past 50kyr.Geophysics Research Letters,1996,23(16):2045～2048
[24]
Li B H,J ian Z M,Wang P X.Pulleniatina obliqueloculata aspaleoceanographic indicator in the southern Okinawa Trough duringthe last 20000 years.MarineM icropaleontology,1997,32:59～69
[25]
OdaM,Takemoto A.Planktonic foraminifera and paleoceanographyin the Domain of the Kuroshio current around Japan during the last20000 years(in Japanese).The Quaternary Research(Tokyo),1992,31(5):341～357
[26]
孙荣涛,李铁刚,曹奇原等.冲绳海槽北部表层沉积物中浮游有孔虫的分布与海洋环境.海洋与湖沼,2003,34(5):511～518Sun Rongtao,Li Tiegang,Cao Qiyuan et al.Planktonic foraminiferadistributions in surface sediments of the northern Okinawa Troughand their marine environment interp retation.Oceanologia etL im nologia S inica,2003,34(5):511～518
[27]
Bond G C,Heinrich H,Broecker W et al.Evidence for massivedischarge of icebergs into the North Atlantic ocean during the lastglacial period.N ature,1992,360:245～249
[28]
李铁刚,刘振夏,HallM A等.冲绳海槽末次冰消期浮游有孔虫δ13C的宽幅低值事件.科学通报,2002,47(4):298～301Li Tiegang,Liu Zhenxia,HallM A et al.A broad deglacialδ13Cminimum event in p lanktonic foraminiferal records in the OkinawaTrough.Chinese Science B ulletin,2002,47(7):599～603
[29]
Manighetti B,Northcote L.Fabulous foraminifera:Examining pastclimates using microscop ic marine organisms.W ater & A tm osphereOnline,2000,8(3):24～26
[30]
汪品先,章纪军,赵泉鸿等.东海底质中的有孔虫和介形虫.北京:海洋出版社,1988.1～325Wang Pinxian,Zhang J ijun,Zhao Quanhong et al.Foraminifera andOstracodes in Surfacee Sediments of the East China Sea.Beijing:China Ocean Press,1988.1～325
[31]
Murry J W.Ecology and Palaeoecology of Benthic Foraminifera.New York:JohnWiley and Sons Inc,1991.1～397
[32]
Echols R J,Armentrout J M.Holocene foraminiferal distributionpatternson the shelf and slope,Yakataga2Yakutat area,NorthernGulf of Alaska.In:Field M E,Bouma A H,Colburn I P et al.eds.Quaternary Depositional Environments of the Pacific Coast,Pacific Coast Paleogeography Symposium Society of EconomicPaleontologists andMineralogists,1980.281～303
[33]
Green K E.Ecology of some Arctic foraminifera.M icro2paleontology,1960,6:57～78
[34]
Xiang Rong,Sun Youbin,Li Tiegang et al.Paleoenvironmentalchange in the middle Okinawa Trough since the last deglaciation:Evidence from the sedimentation rate and p lanktonic foraminiferalrecord.Palaeogeography,Palaeoclim atology,Palaeoecology,2007,243(3～4):378～393
[35]
Saito Y,Katahyama H,Ikehara K et al.Transgressive andhighstand systems tracts and post2glacial transgression,the EastChina Sea.Sedim entary Geology,1998,122(1～4):217～232
[36]
Liu J P,Milliman J D,Gao S et al.Holocene development of theYellow Riverps subaqueous delta,North Yellow Sea.M arineGeology,2004,209(1～4):45～67
[37]
Oba T,Kato M,Kitazato H et al.Paleoenvironmental changes inthe Japan Sea during the last 85000 years.Paleoceanography,1991,6(4):499～518
[38]
Lie H J,Cho C H.On the origin of the Tsushima Warm Current.Journal of Geophysical Research,1994,99(12):25081～25091
[39]
Lie H J,Cho C H,Lee J H.Separation of the Kuroshio water andits penetration onto the continental shelf west of Kyushu.Journal ofGeophysical Research,1998,103(C2):2963～2976
[40]
Lie H J,Cho C H.Recent advantages in understanding the circu2lation and hydrography of the East China Sea.FisheriesOceangraphy,2002,11(6):318～328
[41]
Park Y A,Khim B K.Origin and dispersal of recent clay mineralsin the Yellow Sea.M arine Geology,1992,104:205～213
[42]
Zhao Y Y,Qin Z Y,Li F Y et al.On the source and genesis of themud in the central area of the south Yellow Sea.Chinese Journal ofOceanology and L im nology,1990,8:66～73
[43]
J ian Z,Li B,Pflaumann U et al.Later Holocene cooling event inthe western Pacific.Science in China(Series D),1996,39(5):543～550
[44]
J ian ZM,Wang P X,Saito Y et al.Holocene variability of theKuroshio Current in the Okinawa Trough,Northwestern PacificOcean.Earth and Planetary Science Letters,2000,184:305～319
