VARIATIONS IN PALEOPRODUCTIVITY RECORDED BY BENTHIC. FORAMINIFERA DURING MIS 3 FROM THE WESTERN SOUTH CHINA SEA
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摘要: 选取位于南海西部越南岸外上升流区的17954-2沉积柱状样为研究对象,通过对底栖有孔虫属种含量变化的分析,并与该站位已有的有孔虫研究结果对比,获得该海区MIS 3时期海洋古生产力的变化记录。结果表明,柱状样中的底栖有孔虫堆积速率和指示生产力的底栖有孔虫属种(Bulimina aculeata,Uvigerina peregrina,Cibicidoides wuellerstorfi等)与浮游有孔虫属种(Neogloboquadrina dutertrei,Globigerina bulloides)的含量变化有一致的对应关系。在6个温跃层变浅时期(S1~S6)中,S1~S5阶段出现了低SST、浅DOT、高生产力等现象,表明该区可能有较强的上升流的存在,其形成原因据推测可能是东亚夏季风在这些时期有所加强,而各指标的阶段性变化也表明MIS 3期后期可能出现"特强夏季风"事件。Abstract: Abundance of benthic foraminiferal species and benthic foraminifera accumulate rate(BFAR),as paleoproductivity proxies during MIS 3 from the core 17954-2,located in the modern summer upwelling area off the Vietnam coast in western South China Sea,was studied in this work.The results showed that changes in BFAR and the abundance of benthic foraminiferal species,which are related to productivity(such as Bulimina aculeata,Uvigerina peregrina,Cibicidoides wuellerstorfi),coincided with those of planktonic foraminiferal species(Neogloboquadrina dutertrei,Globigerina bulloides).Six distinct periods of shallower depth of thermocline(DOT)(referred to as S1~S6) were identified in this study.In S1~S5,the lower SST,shallower DOT and higher paleoproductivity indicated an enhanced upwelling,and the causes were supposed to be a strengthened East Asia summer monsoon during these periods.Changes in each proxy also supported a concept that an exceptionally strong summer monsoon could influence this region during the later stages of MIS 3.
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[1] Voelker A H L,Sarnthein M,Grootes P,et al.Correlation of marine 14C ages from the Nordic Seas with the GISP2 isotope record:implications for 14C calibration beyond 25kaBP[J].Radiocarbon,1998,40:517-534.
[2] van Kreveld S,Sarnthein M,Erlenkeuser,et al.Potential links between surging ice sheets,circulation changes,and the Dansgaard-Oeschger cycles in the Irminger Sea,60-18 kyr[J].Paleoceanography,2000,15:425-442.
[3] Berger A,Imbire J,Hays J D,et al.Milankovitch and climate[M].Dordrecht(Holland):Reidel Publish Company,1984:269-305.
[4] Heinrich H.Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130000 years[J].Quaternary Research,1988,29:142-152.
[5] Dansgaard W,Johnsen S J,Clausen H B,et al.Evidence for general instability of past climate from a 250 kyr ice-core record[J].Nature,1993,364:218-220.
[6] Kroon D,Steens T,Troelstra S R.Onset of monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminifera[C]//Proceedings of the Ocean Drilling Program Scientific Results,1991,117:257-265.
[7] 姚檀栋,Thompson L G,施雅风,等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科学,1997,27(5):447-452.
[YAO Tandong,Thompson L G,SHI Yafeng,et at.Climate variation since the Last Interglaciation recorded in the Guliya ice core[J].Science in China(Series D),1997,40(6):662-668.]
[8] 姚檀栋.古里雅冰芯氧同位素地层学[J].第四纪研究,2000,20(2):165-170.
[YAO Tandong.Oxygen isotope stratigraphy of the Guliya ice core[J].Quaternary Sciences,2000,20(2):165-170.]
[9] Shi Y F,Yu G,Liu X D,et al.Reconstruction of the 30-40 ka BP enhanced Indian monsoon climate based on geological records from the Tibetan Plateau[J].Palaeogeogr Palaeoclimatol Palaeoecol,2001,169:69-83.
[10] 施雅风,刘晓东,李炳元,等.距今40-30 ka青藏高原特强夏季风事件及其与岁差周期关系[J].科学通报,1999,44(14):1475-1480.
[SHI Yafeng,LIU Xiaodong,LI Bingyuan,et al.A very strong summer monsoon event during 30-40 ka BP in the Qinghai-Xizang(Tibet) Plateau and its relation to precession[J].Chinese Science Bulletin,1999,44(18):1851-1856.]
[11] 黄宝琦,杨文瑜.南海北部氧同位3期时上部海水结构的变化[J].第四纪研究,2006,26(3):436-441.
[HUANG Baoqi,YANG Wenyu.Variations of upper water structure in MIS 3 from the northern South China Sea[J].Quaternary Sciences,2006,26(3):436-441.]
[12] 罗运利,孙湘君.南海深海沉积物花粉记录的快速气候波动事件[J].第四纪研究,1999,6:536-540.[LUO Yunli,SUN Xiangjun.Millennial-scale climatic fluctuations in pollen record of deep sea deposit from South China Sea[J].Quaternary Sciences,1999
,6:536-540.]
[13] Samthein M,Pflaumann U,Wang P,et al.eds.Preliminary report on SONNE-95 Cruise "Monitor Monsoon" to the South China Sea[R].1994.
[14] Chao S Y,Shaw P T,Wu S Y.Deep water ventilation in the south China Sea[J].Deep-sea Research(Part I),1996,43(4):445-466.
[15] Wiesner M G,Zheng L,Wong H K,et al.Fluxes of particulate matter in the South China[C]//Ittekkot V,Schafer P,Honjo S,et al.eds.Particle Flux in the Ocean.New York:John Wiley & Sons Ltd,1996:293-312.
[16] 汪品先.十五万年来的南海[M].上海:同济大学出版社,1995:74-82.[WANG Pinxian.South China Sea Since 150 Thousand Years[M].Shanghai:TONGJI UNIVERSITY PRESS,1995
:74-82.]
[17] 黄宝琦,翦知湣.越南岸外晚第四纪上升流与东亚夏季风变迁[J].第四纪研究,1999,6:518-525.[HUANG Baoqi,JIAN Zhimin.Late quaternary coastal upwelling and variations of the east Asian summer monsson off the Vietnam coast[J].Quaternary Sciences,1999
,6:518-525.]
[18] 黄宝琦,翦知湣,成鑫荣,等.南海晚第四纪上升流区海水上层水体结构的变化[J].科学通报,2001,46(11):948-952.
[HUANG Baoqi,JIAN Zhimin,CHENG Xinrong,et al.Late Quaternary upper-water column structure in upwelling areas of the South China Sea[J].Chinese Science Bulletin,2001,46(20):1741-1745.]
[19] 青子琪,刘连文,郑洪波.越南岸外夏季上升流区22万年来东亚季风的沉积与地球化学记录[J].海洋地质与第四纪地质,2005,25(2):67-72.
[QING Ziqi,LIU Lianwen,ZHENG Hongbo.Sedimentological and geochemical records of east Asian monsoon in summer upwelling region off the coast of Vietnam for the past 22000 years[J].Marine Geology and Quaternary Geology,2005,25(2):67-72.]
[20] 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,2005,30(5):543-549.
[LIU Lianwen,ZHENG 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 Geoscience,2005,30(5):543-549.]
[21] 向霏,王汝建,李建如,等.越南岸外上升流区48万年来高分辨率的生源组分记录及其古海洋学意义[J].海洋地质与第四纪地质,2006,26(6):81-89.
[XIANG Fei,WANG Rujian,LI Jianru,et al.High-resolution records of biogrnic components and their paleoceanographic implications in the upwelling area of the South China Sea off Eastern Vietnam over past 480 Ka[J].Marine Geology and Quaternary Geology,2006,26(6):81-89.]
[22] 苏翔,刘传联,李建如.越南岸外上升流区45万年来上层海水变化的颗石藻证据[J].海洋地质与第四纪地质,2007,27(2):71-76.
[SU Xiang,LIU Chuanlian,LI Jianru.Coccolith evidence for variation in upper ocean water in upwelling area off the coast of Vietnam for the past 450000 years[J].Marine Geology and Quaternary Geology,2007,27(2):71-76.]
[23] 杜江辉,黄宝琦.MIS 3期南海西部上层水体古海洋学变化[J].科学通报,2009,54(23):3753-3760.
[DU JiangHui,HUANG BaoQi.Variations in upper water structure during MIS 3 from the western South China Sea[J].Chinese Science Bulletin,2010,55(3):301-307.]
[24] Jian Z.M.,Huang B.Q.,Kuhnt W.,et al.Late Quaternary upwelling intensity and East Asian monsoon forcing in the South China Sea[J].Quaternary Sciences,2001,55:363-370.
[25] 杨文瑜,黄宝琦,肖洁,等.南海西部浮游有孔虫记录的MIS 3期表层海洋环境变化[J].第四纪研究,2008,8:437-446.[YANG Wenyu,HUANG Baoqi,XIAO Jie.Environmental changes of surface sea recorded in planktonic foraminifera during MIS 3
in the western South China Sea[J].Quaternary Sciences,2008,8:437-446.]
[26] Wang L,Sarnthein M,Erlenkeuser H,et al.East Asian monsoon climate during the Late Pleistocene:high-resolution sediment records from the South China Sea[J].Marine Geology,1999,156:245-284.
[27] Loeblich A R,Tapan J H.Foraminiferal genera and their classification[M].New York:Van nostrand Reinhold Company,1988:970.
[28] Ujiie H.Bathyal benthic foraminifera in a piston core east off the Miyako Islands,Ryukyu Island Arc[M].Ryukyus:Bull.Coll.Sci.Univ.,1990:1-60.
[29] Barker W H.Taxonomic notes on the species figured by H.B.Brady in his report on the foraminifera dredged by H.M.S.Challenger' during the years 1873-1876[M].Tulsa,Okla.:Society of Economic Paleontologists and Mineralogists,1960:238.
[30] Lutze G F.Depth distribution of benthic foraminifera on the continental margin of northwest Africa.Meteor' Forschungsergeb[J].Reihe C,1980,32:31-80.
[31] Altenbach A V.Short term processes and patterns in the foraminiferal response to organic flux rates[J].Marine Micropaleontology,1992,19(1):119-129.
[32] Corliss B H.The ecology of deep-sea benthic foraminifera[J].PaleoBios,1994,16(2) Supplements:28.
[33] Corliss B H,Chen C.Morphotype patterns of Norwegian Sea deep-sea benthic foraminifera and ecological implications[J].Geology,1988,16(8):716-719.
[34] de Stigter H C,Jorissen F J,van der Zwaann G J.Bathymetric distribution and microhabitat partitioning of live benthic foraminifera along a shelf to deep sea transect in the southern Adriatic Sea[J].Journal of Foraminifera Research,1998,28:40-65.
[35] Herguera J C,Berger W H.Paleoproductivity from benthic foraminifera abundance:Glacial to postglacial change in the west-equatorial Pacific[J].Geology,1991,19(12):1173-l176.
[36] Wollenburg J E,Knies J,Mackensen.High-resolution paleo-productivity fluctuations during the past 24 kyr as indicated by benthic foraminifera in marginal Arctic Ocean[J].Paleoceanography,Paleoclimatology,Paleoecology,2004,204:209-238.
[37] Carstens J,Wefer G.Recent distribution of planktonic foraminifera in the Nansen Basin,Arctic Ocean[J].Deep-Sea Research,1992,30:507-524.
[38] Wolienberg J E,Kuhnt W.The response of benthic foraminifers to carbon flux and primary production in the Arctic Ocean[J].Marine Micropaleontology,2000,40:189-231.
[39] Kaiho K.Benthic foraminiferal dissolved-oxygen index and dissolved-oxygen levels in the modern ocean[J].Geology,1994,22(8):719-722.
[40] Jian Z,Wang P,Kienast M,et al.Benthic foraminiferal paleoceanography of the South Sea over the last 40,000 years[J].Marine Geology,1999,156(1):159-186.
[41] Jian Zhimin,Chen Ronghua,Li Baohua.Deep-sea benthic foraminiferal record of the paleoceanography in the Southern Okiniwa Trough over the last 20000 years[J].Science in China(Series D),1996,39(5):551-560.
[42] Jian Zhimin,Saito Y,Wang Pinxian.Shifts of the Kuroshio axis over the last 20000 years[J].Chinese Science Bulletin,1998,43(12):1053-1056.
[43] Li Tiegang,Xiang Rong,Sun Rongtao,et al.Benthic foraminifera and bottom water evolution in the middle-southern Okiniwa Trough during the last 18ka[J].Science in China(Series D),2005,48(6):805-814.
[44] Samthein M,Altenbach A V.Late Quaternary changes in surface water and deep water masses of the Nordic Seas and north-eastern North Atlantic:A review[J].Geologische Rundschau,1995,84(1):89-107.
[45] Altenbach A V.Short term processes and patterns in the foraminiforal responses to organic flux rates[J].Marine Micropaleontology,1992,19(1):119-129.
[46] Miao Q,Thunell R C.Late Pleistocene-Holocene distribution of deep-sea benthic foraminifera in the South China Sea and Sulu Sea:Paleoceanography implications[J].Journal of Foraminiferal Research,1996,26(1):9-23.
[47] Peterson L C,Prell W L.Carbonate preservation and rates of climatic change:an 800 kye record from the Indian Ocean[C]//The Carbon Cycle and Atmospheric CO2:Natural Variations Archean to Present.Washington D C:AGU Geophys Monogr 32,1985:251-269.
[48] Le J,Shackleton N J.Carbonate dissolution fluctuations in the western equatorial Pacific during the Late Quaternary[J].Paleoceanography,1992,7:21-42.
[49] 陈荣华,翦知湣,郑玉龙,等.南海中部浮游有孔虫通量的季节变化[J].同济大学学报,2000,28(1):73-77.
[CHEN Ronghua,JIAN Zhimin,ZHENG Yulong,et al.Seasonal Variations of the Planktonic Foraminiferal Flux in the Central South China Sea[J].Journal of Tongji University,2000,28(1):73-77.]
[50] Helleman S,Rosenstein M.Normal monthly wind stress over the world ocean with error estimates[J].Journal Physical Oceanogeography,1983,13:1093-1104.
[51] Wiesner M G,Zheng L,Wong H K.Fluxes of Particulate Matter in the South China Sea[C]//Particulate Flux in the Ocean.New York:John Wiley and Sons,1996:91-154.
[52] Suess E,Thiede J.Coastal upwelling:Its sediment record.Part A.Responses of the sedimentary regime to present coastal upwelling[M].New York,London:Plenum Press,1983:1-13.
[53] Huang B Q,Jian Z M,Cheng X R,et al.Foraminiferal responses to upwelling variations in the South China Sea over the last 220000[J].Marine Micropaleontology,2003,47(1-2):1-15.
[54] Wang Y J,Cheng H,Edwards R L,et al.A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave[J].China Science,2001,294:2345-2348.
[55] Knutti R,Fl ckiger J,Stocker T F,et al.Strong hemispheric coupling of glacial climate through freshwater discharge and ocean circulation[J].Nature,2004,430:851-856.
[56] Broecker W S.Thermohaline circulation,the Achilles heel of our climate system:Will man-made CO2 upset the current balance?[J].Science,1997,278:1582-1588.
[57] Porter S C,An Z S.Correlation between climate events in the North Atlantic and China during the last glaciation[J].Nature,1995,375:305-308.
[58] 施雅风,贾玉连,于革,等.40-30 kaBP青藏高原及邻区高温大降水事件的特征、影响及原因探讨[J].湖泊科学,2002,14(1):1-11.
[SHI Yafeng,JIA Yulian,YU Ge,et al.Features,Impacts and Causes of the High Temperature and Large Precipitation Event in the Tibetan Plateau and Its Adjacent Area During 40-30 ka BP[J].Journal of Lake Sciences,2002,14(1):1-11.]
[59] 施雅风,于革.40-30 kaBP中国暖湿气候和海侵的特征与成因探讨[J].第四纪研究,2003,23(1):1-11.
[SHI Yafeng,YU Ge.Warm-humid climate and transgressions during 40~30kaBP and their potential mechanisms[J].Quaternary Sciences,2003,23(1):1-11.]
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