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中更新世以来西菲律宾海上层水体结构演化特征——来自钙质超微化石Florisphaeraprofunda的证据

, PP. 216-226

Keywords: 西菲律宾海,中更新世,温跃层变动,长周期,冰期-间冰期旋回,东亚季风

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Abstract:

MD06-3050岩芯位于西菲律宾海吕宋岛以东本哈姆高原,利用钙质超微化石下透光带种属Florisphaeraprofunda占总颗石的相对丰度,恢复了中更新世以来该海区的上层水体结构演化特征。结果显示,西菲律宾海区自1040ka以来,温跃层/营养跃层经历了由浅—深—浅—深的长周期变动,可能是由于全球碳库的长周期变化对气候系统的大规模调整所致;同时温跃层/营养跃层也具有明显的冰期-间冰期旋回性特征。温跃层变动的另一个重要特征是在中布容事件前后呈现出相反的冰期-间冰期变化趋势,认为可能是由东亚冬、夏季风强度变化引起。

References

[1]  15 Brand L E. Physiological ecology of marine coccolithophores.In: Winter A,Siesser W G eds.Coccolithophores.Cambridge: Cambridge University Press,1994.39~49
[2]  16 Young J R. Functions of coccoliths.In: Winter A,Siesser W G eds.Coccolithophores.Cambridge: Cambridge University Press,1994. 63~82
[3]  37 Groetsch J, Wu G,Berger W H.Carbonate saturation cycles in the Western Equatorial Pacific.In: Einsele G,Ricken W,Seilacher A et al.eds.Cycles and Events in Stratigraphy.New York: Springer Heidelberg,1991.110~125
[4]  38 Dollfus D, Beaufort L.Fat neural network for recognition of position-normalised objects. Neural Networks,1999, 12 (3):553~560
[5]  39 Beaufort L, Dollfus D.Automatic recognition of coccolith by dynamical neural network. Marine Micropaleontology,2004, 51 (1~2):57~73
[6]  40 Lisiecki L E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18 O records. Paleocenaography,2005, 20 (2):1~17,PA1003,doi: 10.1029/2004PA001071
[7]  41 Thierstein H R, Geitzenauer K R,Molfino B et al.Global synchroneity of Late Quaternary coccolith datum levels: Validation by oxygen isotopes. Geology,1977, 5 (7):400~404
[8]  42 Jansen J H F, Kuijpers A,Troelstra S R.A Mid-Brunhes climatic event: Long-term changes in global atmosphere and ocean circulation. Science,1986, 232 :619~622
[9]  43 Beaufort L, Lancelot Y,Camberlin P et al.Insolation cycles as a major control of equatorial Indian Ocean primary production. Science,1997, 278 :1451~1454
[10]  44 Bollmann J, Baumann K H,Thierstein H R.Global dominance of Gephyrocapsa coccoliths in the Late Pleistocene: Selective dissolution,evolution,or global environmental change?Paleo-ceanography,1998, 13 (5):517~529
[11]  45 Wang Pinxian, Tian Jun,Cheng Xinrong et al.Carbon reservoir changes preceded major ice-sheet expansion at the Mid-Brunhes event. Geology,2003, 31 (3):239~242
[12]  46 Rickaby R E M, Bard E,Sonzogni C et al.Coccolith chemistry reveals secular variations in the global ocean carbon cycle? Earth and Planetary Science Letters,2007, 253 (1~2):83~95
[13]  47 Mohtadi M, Hebbeln D,Ricardo S N et al. El Nio -like pattern in the Pacific during marine isotope stages(MIS)13 and 11?Paleoceanography,2006, 21 : PA1015,doi: 10.1029/2005PA001190
[14]  48 Rohling E J, Fenton M,Jorissen F J et al.Magnitudes of sea-level lowstands of the past 500000 years. Nature,1998, 394 :162~165
[15]  49 Bard E, Rickaby R E M.Migration of the subtropical front as a modulator of glacial climate. Nature,2009, 460 :380~383
[16]  50 Zhang Jiangyong, Wang Pinxian,Li Qianyu et al.Western equatorial Pacific productivity and carbonate dissolution over the last 550kyr: Foraminiferal and nannofossil evidence from ODP Hole 807A. Marine Micropaleontology,2007, 64 (3~4):121~140
[17]  51 Wiesner M G,Zheng L,Wong H et al.Fluxes of particulate matter in the South China Sea.In: Ittekkot V,Schfer P,Honjo S et al.eds.Particle Flux in the Ocean.London: John Wiley & Sons Ltd,1996.293~312
[18]  52 Houghton S D, Guptha M V S.Monsoonal and fertility controls on recent marginal sea and continental shelf coccolith assemblages from the Western Pacific and Northern Indian Oceans. Marine Geology,1991, 97 :251~259
[19]  53 Gregg W W, Casey N W.Modeling coccolithophores in the global oceans. Deep-Sea Research Ⅱ,2007, 54 (5~7):447~477
[20]  54 Shackleton N J. Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: Isotopic changes in the ocean during the last glacial.In: Les Méthodes Quantitatives d étude des. Viriations du Climat au Cours du Pleistocéne.Gif-sur-Yvette: Colloque international du CNRS,1974.203~209
[21]  55 Lear C H, Elderfield H,Wilson P A.Cenozoic deep-sea temperatures and global ice volumes from Mg/Ca in benthic foraminiferal calcite. Science,2000, 287 :269~272
[22]  56 de Garidel-Thoron T, Rosenthal Y,Bassinot F et al.Stable sea surface temperatures in the Western Pacific Warm Pool over the past 1.75 million years. Nature,2005, 433 :294~298
[23]  58 赵京涛,李铁刚,常凤鸣等.近190kaB.P.以来西太平洋暖池北缘上层海水结构和古生产力演化特征及其控制因素——来自钙质超微化石、有孔虫和同位素的证据.海洋与湖沼,2008, 39 (4):305~311
[24]  Zhao Jingtao,Li Tiegang,Chang Fengming et al.Evolution in upper water structure and paleoproductity in the northern margin of the Western Pacific Warm Pool and its forcing mechanism during the last 190kaB.P.evidence from nannofossil,foraminifera and their isotope composition. Oceanologia et Limnologia Sinica,2008, 39 (4):305~311
[25]  59 Ding Zhongli, Sun Jimin,Liu Dongsheng.Stepwise advance of the Mu Us Desert since Late Pliocene: Evidence from a red clay-loess record. Chinese Science Bulletin,1999, 44 (13):1211~1214
[26]  60 Xiao Jule, An Zhisheng.Three large shifts in East Asian monsoon circulation indicated by loess-paleosol sequences in China and Late Cenozoic deposits in Japan. Palaeogeography,Palaeoclimatology,Palaeoecology,1999, 154 (3):179~189
[27]  61 Hovan S A, Rea D K,Pisias N G et al.A direct link between the China loess and marine δ18 O records: Aeolian flux to the North Pacific. Nature,1989, 340 :296~298
[28]  62 Sun Xiangjun, Luo Yunli,Huang Fei et al.Deep-sea pollen from the South China Sea: Pleistocene indicators of East Asian monsoon. Marine Geology,2003, 201 (1~3):97~118
[29]  64 王汝建,翦知湣,肖文申等.南海第四纪的生源蛋白石记录: 与东亚季风、全球冰量和轨道驱动的联系.中国科学(D辑),2007, 37 (4):521~533
[30]  Wang Rujian,Jian Zhimin,Xiao Wenshen et al.Quaternary biogenic opal records in the South China Sea: Linkages to East Asian monsoon,global ice volume and orbital forcing. Science in China(Series D),2007, 50 (5):710~724
[31]  1 Yan Xiaohai, Ho Chungru,Zheng Quanan et al.Temperature and size variabilities of the Western Pacific Warm Pool. Science,1992, 258 :1643~1645
[32]  2 Trenberth K E, Branstator G W,Karoly D et al.Progress during TOGA in understanding and modeling global teleconnections associated with tropical sea surface temperatures. Journal of Geophysical Research,1998, 103 (C7):14291~14324
[33]  3 Koutavas A, Lynch-Stieglitz J,Marchitto T M et al. El Nio -like pattern in ice age tropical Pacific sea surface temperature. Science,2002, 297 :226~230
[34]  4 Lea D W.Paleoclimate: The glacial tropical Pacific——Not just a west side story. Science,2002, 297 :202~203
[35]  5 Stott L, Poulsen C,Lund S et al.Super ENSO and global climate oscillations at millennial time scales. Science,2002, 297 :222~226
[36]  6 Philander S G, Fedorov A V.Role of tropics in changing the response to Milankovich forcing some three million years ago. Paleoceanography,2003, 18 (2): 1~11,doi: 10.1029/2002PA000837
[37]  7 Visser K, Thunell R,Stott L.Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature,2003, 421 :152~155
[38]  8 Rodgers K B, Lohmann G,Lorenz S et al.A tropical mechanism for Northern Hemisphere deglaciation. Geochemistry, Geophysics, Geosystems,2003, 4 (5): 1~10,doi: 10.1029/2003GC000508
[39]  9 Lea D W, Pak D K,Spero H J.Climate impact of Late Quaternary equatorial Pacific sea surface temperature variations. Science,2000, 289 :1719~1724
[40]  10 Beaufort L, de Garidel-Thoron T,Linsley B et al.Biomass burning and oceanic primary production estimates in the Sulu Sea area over the last 380kyr and the East Asian monsoon dynamics. Marine Geology,2003, 201 (1~3):53~65
[41]  11 Holbourn A, Kuhnt W,Kawamura H et al.Orbitally-paced paleoproductivity variations in the Timor Sea and Indonesian Throughflow variability during the last 460kyr. Palaeoceanography,2005, 20 (3): 1~18,doi: 10.1029/2004PA001094
[42]  12 Liu Chuanlian, Wang Pinxian,Tian Jun et al.Coccolith evidence for Quaternary nutricline variations in the Southern South China Sea. Marine Micropaleontology,2008, 69 (1):42~51
[43]  13 Li Tiegang, Zhao Jingtao,Sun Rongtao et al.The variation of upper ocean structure and paleoproductivity in the Kuroshio source region during the last 200kyr. Marine Micropaleontology,2010, 75 (1~4):50~61
[44]  14 Hibberd D J. The ultrastructure and taxonomy of the Chrysophyceae and Prymnesiophyceae(Haptophyceae): A survey with some new observations on the ultrastructure of the Chrysophyceae. Botanical Journal of the Linnean Society,1976, 72 (2):55~80
[45]  17 Winter A, Jordan R W,Roth P H.Biogeography of living coccolithophores in ocean waters.In: Winter A,Siesser W G eds.Coccolithophores.Cambridge: Cambridge University Press,1994. 161~178
[46]  18 Balestra B, Ziveri P,Baumann K H et al.Surface water dynamics in the Reykjanes Ridge area during the Holocene as revealed by coccolith assemblages. Marine Micropaleontology,2010, 76 (1~2):1~10
[47]  19 Stoll H M,Rosenthal Y,Falkowski P.Climate proxies from Sr/Ca of coccolith calcite: Calibrations from continuous culture of Emiliania huxleyi.Geochimica et Cosmochimica Acta,2002, 66 (6):927~936
[48]  20 López-Otlvaro G E, Flores J A,Sierro F J et al.Variations in coccolithophorid production in the Eastern Equatorial Pacific at ODP Site 1240 over the last seven glacial-interglacial cycle. Marine Micropaleontology,2008, 69 (1):52~69
[49]  21 Okada H, Honjo S.The distribution of oceanic coccolithophorids in Pacific. Deep-Sea Research and Oceanographis Abstracts,1973, 20 (4):365~374
[50]  22 Molfino B, McIntyre A.Nutricline variation in the equatorial Atlantic coincident with the Younger Dryas. Paleoceanography,1990, 5 (6):997~1008
[51]  23 Bassinot F C, Beaufort L,Vincent E et al.Changes in the dynamics of Western Equatorial Atlantic surface currents and biogenic productivity at the "Mid-Pleistocene Revolution"(930ka).In: Shackleton N J,Curry W B,Richter C eds. Proceedings of the Ocean Drilling Program Scientific Results, 154,1997. 269~284
[52]  24 McIntyre A, Molfino B.Forcing of Atlantic equatorial and subpolar millennial cycles by precession. Science,1996, 274 :1867~1870
[53]  25 Baumann K H, epek M,Kinkel H.Coccolithophores as indicators of ocean water masses,surface-water temperature,and paleo-productivity—— Examples from the South Atlantic.In: Fischer G,Wefer G eds.Use of Proxies in Paleoceanography: Examples from the South Atlantic.New York: Springer-Verlag,1999.111~144
[54]  26 Kinkel H, Bumann K H, epek M.Coccolithophores in the equatorial Atlantic Ocean: Response to seasonal and Late Quaternary surface water variability. Marine Micropaleontology,2000, 39 (1~4):87~112
[55]  27 Flores J A, Brcena M A,Sierro F J.Ocean-surface and wind dynamics in the Atlantic Ocean off North West Africa during the last 140000 years. Palaeogeography,Palaeoclimatology,Palaeocology,2000, 161 (3~4):459~478
[56]  28 Ahagon N, Tanaka Y,Ujiie H. Florisphaera profunda,a possible nannoplankton indicator of Late Quaternary changes in seawater turbidity at the northwestern margin of the Pacific. Marine Micro-paleontology,1993, 22 (3):255~273
[57]  29 Okada H, Wells P.Late Quaternary nannofossil indicators of climate change in two deep-sea cores associated with the Leeuwin current off Western Australia.Palaeogeography,Palaeoclimatology,Palaeo-ecology,1997, 131 (3~4):413~432
[58]  30 Okada H, Matsuoka M.Lower-photic nannoflora as an indicator of the Late Quaternary monsoonal palaeorecord in the tropical Indian Ocean.In: Moguilevsky A,Whatley R eds.Microfossils and Oceanic Environments.Wales: Aberystwyth Press,University of Wales,1996. 231~245
[59]  31 Castradori D. Calcareous nannofossils and the origin of Eastern Mediterranean sapropels. Paleoceanography,1993, 8 (4):459~471
[60]  32 孙守勋,腾 军.菲律宾海的气候特征.海洋预报,2003, 20 (3):31~39
[61]  Sun Shouxun,Teng Jun.Climate character of the Philippine Sea. Marine Forecasts,2003, 20 (3):31~39
[62]  33 张 弦,俞慕耕,江 伟等.菲律宾海及其邻近海区的水文特征.海洋通报,2004, 23 (1):8~14
[63]  Zhang Xuan,Yu Mugeng,Jiang Wei et al.Hydrologic characteristic of the Philippine Sea and its nearby areas. Marine Science Bulletin,2004, 23 (1):8~14
[64]  34 吴文风.海军气象学.北京: 海潮出版社,1995.221~222
[65]  Wu Wenfeng.Marine Meteorology.Beijing: Ocean Press,1995. 221~222
[66]  35 Qiu Bo, Lukas R.Seasonal and interannual variability of the North Equatorial Current,the Mindanao Current,and the Kuroshio along the Pacific western boundary. Journal of Geophysical Research,1996, 101 (C5):12315~12330
[67]  36 孙荣涛.黑潮流系与暖池区晚更新世以来的古环境研究.青岛: 中国科学院海洋研究所博士学位论文,2006.25~26
[68]  Sun Rongtao.Research of the paleoenvironment of the Kuroshio current system and the Warm Pool during the Late Pleistocene.Qingdao: Doctoral Dissertation of Institute of Oceanology,Chinese Academy of Sciences,2006.25~26
[69]  57 黄宝琦,李保华,翦知湣.1.5Ma以来南海南北上部水体温度变化对比.海洋地质与第四纪地质,2004, 24 (1):79~83
[70]  Huang Baoqi,Li Baohua,Jian Zhimin.Comparison of variations in upper water temperatures between the northern and Southern South China Sea 1.5Ma BP. Marine Geology & Quaternary Geology,2004, 24 (1):79~83
[71]  63 Liu Z, Trentesaux A,Clemen S et al.Clay mineral assemblages in the Northern South China Sea: Implications for East Asian monsoon evolution over the past 2 million years. Marine Geology,2003, 201 :133~146

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