全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

末次盛冰期以来苏拉威西海区上层海水对快速气候变化的响应

, PP. 256-264

Keywords: 苏拉威西海区,上层海水,快速气候变化响应,11kaB.P.气候变化

Full-Text   Cite this paper   Add to My Lib

Abstract:

通过对苏拉威西海MD98-2178站位浮游有孔虫定量分析、表层浮游有孔虫Globigerinoidesruber壳体镁钙(Mg/Ca)比值反演海表温度(SST),并结合表层和次表层浮游有孔虫氧、碳同位素,探讨末次盛冰期以来,苏拉威西海区温度、盐度、生产力、温跃层深度变化及其对快速气候变化的响应。研究发现:末次盛冰期苏拉威西海区,海表温度存在明显降温,较现代海表温度下降了2.9℃,但缺乏对快速气候波动明显响应。MD98-2178站位盐度、生产力以及温跃层深度等记录,则明显响应快速气候波动,在H1,YD等变冷事件期间,盐度变高、生产力上升、温跃层深度变浅,指示东亚冬季风加强,热带辐合带(ITCZ)南移以及印度尼西亚穿越流(ITF)减弱。末次盛冰期以来,MD98-2178站位属种组合、生产力、盐度以及温跃层深度在11kaB.P.左右存在明显的突变,且在南海、印尼海区普遍存在,指示了该海域在11kaB.P.左右存在重要的气候变化过程。

References

[1]  1 Kerr R A. The tropics return to the climate system. Science,2001, 292 :660~661
[2]  2 Hoerling M P, Hurrell J W,Xu Taiyi.Tropical origins for recent North Atlantic climate change. Science,2001, 292 :90~92
[3]  3 Rasmusson E M, Michael H.El Nio and variations in climate. American Scientist,1985, 73 :168~177
[4]  4 Ropelewski C F, Halpert M S.Global and regional scale precipitation patterns associated with the El Nio/Southern Oscillation. Monthly Weather Review,1987, 115 :1606~1626
[5]  5 闻新宇,王绍武,朱锦红.古ENSO的研究进展.地球物理学报,2007, 50 (2):387~396
[6]  Wen Xinyu,Wang Shaowu,Zhu Jinhong. An overview of the paleo-ENSO. Chinese Journal of Geophysics,2007, 50 (2):387~396
[7]  6 汪品先,田 军,成鑫荣等.探索大洋碳储库的演变周期.科学通报,2003, 48 (21):2216~2227
[8]  Wang Pinxian,Tian Jun,Cheng Xinrong et al.Explore ocean carbon reservoir evolvement cycle. Chinese Science Bulletin,2003, 48 (21):2216~2227
[9]  7 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
[10]  8 Locarnini R A, Mishonov A V,Antonov J I et al.World Ocean Atlas 2005,Volume 1: Temperature.In: Levitus S ed.NOAA Atlas NESDIS 61,U.S.Washington,D.C.: Government Printing Office,2006.182
[11]  9 Gordon A L, Fine R A.Pathways of water between the Pacific and Indian oceans in the Indonesian seas. Nature,1996, 379 :146~149
[12]  10 Gordon A L, Susanto R D,Vranes K.Cool Indonesian throughflow as a consequence of restricted surface layer flow. Nature,2003, 425 :824~828
[13]  11 Gordon A L. Oceanography of the Indonesian Seas and their throughflow. Oceanography,2005, 18 (4):14~27
[14]  12 Schneider N. The Indonesian throughflow and the global climate system. Journal of Climate,1998, 11 :676~689
[15]  13 Gordon A L, Susanto R D,Ffield A et al.Makassar strait throughflow,2004 to 2006. Geophysical Research Letters,2008, 35 : L24605,doi: 10.1029/2008GL032372
[16]  14 Bé A W H. An ecological,zoogeographic and taxonomic review of recent planktonic foraminifera.In: Ramsay A T S ed.Oceanic Micropaleontology.London: Academic Press,1977.1~100
[17]  15 Saito T, Thompson P R,Breger D.Systematic Index of Recent and Pleistocene Planktonic Foraminifera.Tokyo: University of Tokyo Press,1981.190
[18]  16 Andreasen D J, Ravelo A C.Tropical Pacific Ocean thermocline depth reconstructions for the Last Glacial Maximum. Paleoceanography,1997, 12 :395~413
[19]  17 Cheng Xinrong, Wang Pinxian,Huang Baoqi et al.Carbon isotopic record of foraminifers in surface sediments from the South China Sea and its significance. Chinese Science Bulletin,2005, 50 (2):162~166
[20]  19 Lea D W, Mashiotta T A,Spero H J.Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing. Geochimica et Cosmochimica Acta,1999, 63 (16):2369~2379
[21]  20 Hastings D W, Kienast M,Steinke S et al.A comparison of three independent paleotemperature estimates from a high resolution record of deglacial SST records in the tropical South China Sea. EOS,2001, 82 : 12B-10
[22]  21 Dekens P S, Lea D W,Pak D K et al.Core top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation. Geochemistry Geophysics Geosystems,2002, 3 (4): doi: 10.1029/2001GC000200
[23]  22 Huang Kuofang, You Chengfeng,Lin Huiling et al.In situ calibration of Mg/Ca ratio in planktonic foraminiferal shell using time series sediment trap: A case study of intense dissolution artifact in the South China Sea. Geochemistry, Geophysics, Geosystems,2008, 9 : Q04016,doi: 10.1029/2007 GC001660
[24]  23 Steinke S, Chiu Hanyi,Yu Paisen et al.On the influence of sea level and monsoon climate on the Southern South China Sea freshwater budget over the last 22,000 years. Quaternary Science Reviews,2006, 25 :1475~1488
[25]  24 Bemis B E, Spero H J,Bijma J et al.Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations. Paleoceanography,1998, 13 :150~160
[26]  25 Waelbroeck C, Labeyrie L,Michel E et al.Sea-level and deep water temperature changes derived from benthic foraminifera isotopic record. Quaternary Science Reviews,2002, 21 :295~305
[27]  26 Fairbanks R G, Mortlock R,Chiu T et al.Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paired 230 Th/234 U/238 U and 14 C dates on pristine corals. Quaternary Science Reviews,2005, 24 :1781~1796
[28]  27 North Greenland Ice Core Project Members. High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature,2004, 431 :147~151
[29]  28 Partin J W, Cobb K M,Adkins J F et al.Millennial-scale trends in West Pacific warm pool hydrology since the Last Glacial Maximum. Nature,2007, 449 :452~456
[30]  29 Labeyrie L D, Duplessy J C,Blanc P L.Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years. Nature,1987, 327 :477~482
[31]  30 Stott L, Poulsen C,Lund S et al.Super ENSO and global climate oscillations at millennial time scales. Science,2002, 297 :222~226
[32]  31 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
[33]  32 Xu Jian, Holbourn A,Kuhnt W et al.Changes in the thermocline structure of the Indonesian outflow during Terminations Ⅰ and Ⅱ. Earth and Planetary Science Letters,2008, 273 :152~162
[34]  33 Griffiths M L, Drysdale R N,Gagan M K et al.Increasing Australian-Indonesian monsoon rainfall linked to Early Holocene sea-level rise. Nature Geoscience,2009, 2 :636~639
[35]  34 Rosenthal Y, Oppo D W,Linsley B K.The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea,western equatorial Pacific. Geophysical Research Letters,2003, 30 (8): 1428,doi: 10.1029/2002GL016612
[36]  35 Wang Y J, Cheng H,Edwards R L et al.A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave,China. Science,2001, 294 :2345~2348
[37]  36 Herguera J C, Berger W H.Glacial to postglacial drop in productivity in the western equatorial Pacific: Mixing rate vs.nutrient concentrations. Geology,1994, 22 :629~632
[38]  37 Ravelo A C, Fairbanks R G,Philander S G H.Reconstructing tropical Atlantic hydrography using planktonic foraminifera and an ocean model. Paleoceangraphy,1990, 5 (3):409~431
[39]  38 Ravelo A C, Fairbanks R G.Oxygen isotopic composition of multiple species of planktonic foraminifera: Recorders of the modern photic zone temperature gradient. Paleoceangraphy,1992, 7 (6):815~831
[40]  39 叶黎明,翦知湣,金海燕等.末次盛冰期以来印度尼西亚穿越流对东印度洋上部水体结构的影响.第四纪研究,2008, 28 (3):458~464
[41]  Ye Liming,Jian Zhimin,Jin Haiyan et al.Influence of Indonesian throughflow on easternmost Indian upper ocean structure since last glacial maximum. Quaternary Sciences,2008, 28 (3):458~464
[42]  40 Spero H J, Lea D W.The cause of carbon isotope minimum events on glacial terminations. Science,2002, 296 :522~525
[43]  41 Kiefer T, Kienast M.Patterns of deglacial warming in the Pacific Ocean: A review with emphasis on the time interval of Heinrich event 1. Quaternary Science Reviews,2005, 24 :1063~1081
[44]  42 Yancheva G, Nowaczyk N R,Mingram J et al.Influence of the intertropical convergence zone on the East Asian monsoon. Nature,2007, 445 :74~77
[45]  43 de Garidel-Thoron T, Beaufort L,Linsley B K et al.Millennial-scale dynamics of the East Asian winter monsoon during the last 200,000 years. Paleoceanography,2001, 16 (5):491~502
[46]  18 Barker S, Greaves M,Elderfield H.A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry. Geochemistry,Geophysics,Geosystems,2003, 4 (9):8407,doi: 10.1029/2003GC000559
[47]  44 丁 旋, Guichard F,Bassinot F et al.末次冰消期印度尼西亚多岛海热传输通道之演变.科学通报,2003, 48 (2):199~204
[48]  Ding Xuan,Guichard F,Bassinot F et al.Evolution of heat transport pathways in the Indonesian Archipelago during last deglaciation. Chinese Science Bulletin,2002, 47 (22):1912~1917
[49]  45 丁 旋,方念乔,Guichard F et al.爪哇海末次冰盛期以来的季风与穿越流活动记录.第四纪研究,2008, 28 (3):465~471
[50]  Ding Xuan,Fang Nianqiao,Guichard F et al.Monsoon and throughflow activity records in the Java Sea during the Last Glacial Maximum. Quaternary Sciences,2008, 28 (3):465~471
[51]  46 Ding X, Bassinot F,Guichard F et al.Distribution and ecology of planktonic foraminifera from the seas around the Indonesian Archipelago. Marine Micropaleontology,2006, 58 :114~134
[52]  47 王 良,刘传联.末次冰期以来南海南部千年尺度的古海洋学.海洋地质与第四纪研究,2008, 28 (4):85~91
[53]  Wang Liang,Liu Chuanlian.Millennial scale paleoceanographic variations from the last glacial in the Southern South China Sea. Marine Geology & Quaternary Geology,2008, 28 (4):85~91
[54]  48 安 阳,翦知湣.末次冰消期南海南部的普林虫低值事件.科学通报,2009, 54 (17):2527~2532
[55]  An Yang,Jian Zhimin.Pulleniatina Minimum Event during the last deglaciation in the Southern South China Sea. Chinese Science Bulletin,2009, 54 (23):4514~4519
[56]  49 房殿勇,成鑫荣,吴国瑄等.南沙南部近30ka来的古海洋学记录.海洋地质与第四纪地质,2000, 20 (4):81~86
[57]  Fang Dianyong,Cheng Xinrong,Wu Guoxuan et al.Paleo-oceanograhic record of the past 30ka in the Southern Nansha area,South China Sea,Marine Geology & Quaternary Geology,2000, 20 (4):81~86.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133