Gr(o)ger M,Henrich R,Bickert T et al.Glacial-interglacial variability in lower North Atlantic deep water:Inference from silt grain-size analysis and carbonate preservation in the western equatorial Atlantic.Marine Geology,2003,201(4):321~332
[2]
Wang Pinxian,Wang Lueliang,Bian Yunhua et al.Late Quaternary paleoceanography of the South China Sea:Surface circulation and carbonate cycles.Marine Geology,1995,127(1~4):145~165
[3]
Laj C,Wang P X,Balut Y et al.MD147-Marco Polo IMAGESⅫ Cruise Report.France:Institut Paul-Emile Victor(IPEV),2005
[4]
谢昕,郑洪波,陈国成等.古环境研究中深海沉积物粒度测试的预处理方法.沉积学报,2007,25(5):684~692 Xie Xin,Zheng Hongbo,Chen Guocheng et al.Pretreatment method of grain size measurement of marine sediment in paleoenvironment research.Acta Sedimentologica Sinica,2007,25(5):684~692
[5]
陈国成,郑洪波,李建如等.南海西部陆源沉积粒度组成的控制动力及其反映的东亚季风演化.科学通报,2007,52(23):2768~2776 Chen Guocheng,Zheng Hongbo,Li Jianru et al.Dynamic control on grain-size distribution of terrigenous sediments in the western South China Sea:Implication for East Asian monsoon evolution.Chinese Science Bulletin(in press)
[6]
Milliman J D.Meade R H.World-wide delivcry of fiver sediment to the oceans.Journal of Geology,1983,91:1~21
[7]
Porter S C,An Zhisheng.Correlation between climate events in the North Atlantic and China during the last glaciation.Nature,1995,375:305~308
[8]
Vandenberghe J,An Zhisheng,Nugteren G et al.New absolute time scale for the Quaternary climate in the Chinese loess region by grainsize analysis.Geology,1997,25(1):35~38
[9]
鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义.中国科学(D辑),1998,28(3):278~283 Lu Huayu,An Zhisheng.Paleoclimatic significance of grain size of loess-palaeosol deposit in Chinese Loess Plateau.Science in China(Series D),1998,28(6):626~631
[10]
Lu Huayu,Huissteden K V,An Zhisheng et al.East Asian winter monsoon variations on a millennial time-scale before the last glacial-interglacial cycle.Journul of Quaternary Sciences,1999,14(2):101~110
[11]
Fang Xiaomin,Li Jijun,van der Voo R.Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P.related to Tibetan uplift.Earth and Planetary Scienee Letters,1999,165(1):129~144
[12]
An Z S,Kutzbach J E,Prell W L et al.Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times.Nature,2001,411:62~66
[13]
Ding Z L,Yu Z W.Yang S L et al.Coeval changes in grain size and sedimentation rate of eolian loess,the Chinese Loess Plateau.Geophysical Research Letters,2001,28(10):2097~2100
[14]
Ding Z L,Derbyshire E,Yang S L et al.Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record.Paleoceanography,2002,17(3):1033,doi:1029/2001 PA000725
[15]
Lu H,Zhang F,Liu X.Patterns and frequencies of the East Asian winter monsoon variations during the past million years revealed by wavelet and spectral analyses.Global and Planetary Change,2003,35(1):67~74
[16]
安芷生,孙东怀,陈明扬等.黄土高原红粘土序列与晚第三纪的气候事件.第四纪研究,2000,20(5):435~446 An Zhisheng,Sun Donghuai,Chen Mingyang et al.Red clay in Chinese Loess Plateau and recorded paleoclimate events of the Late Tertiary.Quaternary Sciences,2000,20(5):435~446
[17]
孙继敏.中国黄土的物质来源及其粉尘的产生机制与搬运过程.第四纪研究,2004,24(2):175~183 Sun Jimin.Provenance,forming mechanism and transport of loess in China.Quaternary Sciences,2004,24(2):175~183
[18]
安芷生,张培震,王二七等.中新世以来我国季风-干旱环境演化与青藏高原的生长.第四纪研究,2006,26(5):678~693 An Zhisheng,Zhang Peizhen,Wang Erchie et al.Changes of the monsoon-arid environment in China and growth of the Tibetan Plateau since the Miocene.Quaternary Sciences,2006,26(5):678~693
[19]
孙东怀,鹿化煜.晚新生代黄土高原风尘序列的粒度和沉积速率与中国北方大气环流演变.第四纪研究,2007,27(2):251~262 Sun Donghuai,Lu Huayu.Grain-size and dust accumulation rate of Late Cenozoic aeolian deposits and the inferred atmospheric circulation evolutions.Quaternary Sciences,2007,27(2):251~262
[20]
孙有斌,刘青松.晚上新世-早更新世北太平洋和黄土高原的风尘沉积记录的初步对比.第四纪研究,2007,27(2):263~269 Sun Youbin,Liu Qingsong.Preliminary comparison of eolian depositions in the north Pacific and the Chinese Loess Plateau during the Late Pliocence-Early Pleistocene.Quaternary Sciences,2007,27(2):263~269
[21]
熊尚发.黄土-红粘土记录的构造尺度气候变化.第四纪研究,2007,27(2):242~250 Xiong Shangfa.Chinese loess-red clay bearing climate changes on tectonic time scales.Quaternary Sciences,2007,27(2):242~250
[22]
Rea D K,Hovan S A.Grain size distribution and depositional processes of the mineral component of abyssal sediments:Lessons from the North Pacific.Paleoceanography,1995,12:251~258
[23]
Prins M A,Postma G,Cleveringa J et al.Controls on terrigenous sediment supply to the Arabian Sea during the Late Quaternary:The Indus Fan.Marine Geology,2000,169(3~4):327~349
[24]
Prins M A,Postma G,Weltje G J.Controls on terrigenous sediment supply to the Arabian Sea during the Late Quaternary:The Makran continental slope.Marine Geology,2000,169(3~4):351~371
[25]
Stuut J B W,Prins M A.Schneider R R et al.A 300-kyr record of aridity and wind strength in southwestern Africa:Inferences from grain-size distributions of sediments on Walvis Ridge,SE Atlantic.Marine Geology,2002,180(1~4):221~233
[26]
Pichevin L,Cremer M,Giraudeau J et al.A 190 ky record of lithogenic grain-size on the Namibian slope:Forging a tight link between past wind-strength and coastal upwelling dynamics.Marine Geology,2005,218(1~4):81~96
[27]
Xiao Shangbin,Li Anchun,Liu J P et al.Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea.Palaeogeography,Palaeoclimatology,Palaeoecology,2006,237(2~4):293~304
[28]
Boulay S,Colin C,Trentesaux A et al.Mineralogy and sedimentology of Pleistocene sediment in the South China Sea(ODP Site 1144).Proceedings of the Ocean Drilling Program Scientific Results,2003,184:1~21
[29]
Sun Donghuai,Bloemendal J,Rea D K et al.Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments,and numerical partitioning of the sedimentary components.Sedimentary Geology,2002,152(3~4):263~277
[30]
Weltje G J,Prins M A.Muddled or mixed?Inferring palaeoclimate from size distributions of deep-sea clastics.Sedimentary Geology,2003,162(1~2):39~62
[31]
Prins M A,Vriend M,Nugteren G et al.Late Quaternary aeolian dust input variability on the Chinese Loess Plateau:Inferences from unmixing of loess grain-size records.Quaternary Science Reviews,2007,26(1~2):230~242
[32]
孙有斌,高抒,李军.边缘海陆源物质中环境敏感粒度组分的初步分析.科学通报,2003,48(1):83~86 Sun Youbin,Gao Shu,Li Jun.Preliminary analysis of grain-size populations with environmentally sensitive terrigenous in marginal sea setting.Chinese,Science Bulletin,2003,48(2):184~187
[33]
汪品先.十五万年米的南海.上海:同济大学出版社,1995.1~184 Wang Pinxian.South China Sea since 150ka.Shanghai:Tongji University Press,1995.1~184
[34]
黄宝琦,成鑫荣,翦知湣等.晚上新世以来南海北部上部水体结构变化及东亚季风演化.第四纪研究,2004,24(1):110~115 Huang Baoqi,Cheng Xingrong,Jian Zhimin et al.Variations in upper ocean structure in the South China Sea and the evolution of the East Asian monsoon since Late Pliocene.Quaternary Sciences,2004,24(1):110~115
[35]
黄宝琦,杨文瑜.南海北部氧同位素3期时上部海水结构的变化.第四纪研究,2006,26(3):436~441 Huang Baoqi,Yang Wenyu.Variations of upper water structure in MIS 3 from the northem South China Sea.Quaternary Sciences,2006,26(3):436~441
[36]
丁旋,方念乔,陈萍等.孟加拉湾深海氧同位素2、3期上升流活动--北印度洋冬季风的实证.第四纪研究,2003,23(1):53~59 Ding Xuan,Fang Nianqiao,Chen Ping et al.Upwelling actions in the Bay of Bengal duringMarine Isotope Stages 2 and 3:Evidence for Indian winter monsoon.Quaternary Sciences,2003,23(1):53~59
[37]
郑洪波,杨文光,贺娟等.南海的氧同位素3期.第四纪研究,2008,28(1):68~78 Zheng Hongbo,Yang Wenguang,He Juan et al.Marine Isotope Stage 3(MIS 3)of South China Sea.Quaternary Sciences,2008,28(1):68~78
[38]
汪品先,赵泉鸿,翦知湣等.南海三千万年的深海记录.科学通报,2003,48(21):2206~2215 Wang Pinxian,Jian Zhimin,Zhao Quanhong et al.Thirty million year deep-sea records in the South China Sea.Chinese Science Bulletin,2003,48(23):2524~2534
[39]
汪品先,翦知湣,赵泉鸿等.南海演变与季风历史的深海证据.科学通报,2003,48(21):2228~2239 Wang Pinxian,Jian Zhimin,Zhao Quanhong et al.Evolution of the South China Sea and monsoon history revealed in deep-sea records.Chinese Science Bulletin,2003,48(23):2549~2561
[40]
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.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.Chinese Science Bulletin,2001,46(20):1741~1745
[41]
Jian Zhimin,Huang Baoqi,Kuhnt W et al.Late Quaternary upwelling intensity and East Asian monsoon forcing in the South China Sea.Quaternary Research,2001,55(3):363~370
[42]
Huang Baoqi,Jian Zhimin,Cheng Xinrong et al.Foraminiferal response to upwelling variations in the South China Sea over the last 220,000 years.Marine Micropaleontology,2002,47(1~2):1~15
[43]
Liu Zhifei,Trentesaux A,Clemens S C 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(1~3):133~146
[44]
Wiesner M G,Wang Yubo,Zheng Lianfu.Fallout of volcanic ash to the deep South China Sea induced by the 1991 eruption of Mount Pinatubo(Philippines).Geology,1995,23(10):885~888
[45]
Bühring C,Sarnthein M.Leg 184 Shipboard Scientific Party.Toba ash layers in the South China Sea:Evidence of contrasting wind directions during eruption ca.74ka.Geology,2000,28(3):275~278
[46]
黄维.渐新世以来南海沉积物分布格局及其演变.上海:同济大学博士学位论文,2004.1~112 Huang Wei.Sediment distributional patterns and evolution in the South China Sea since the Oligocene.Shanghai:Tongji University,2004.1~112
[47]
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.Marine Geology,1999,156(1~4):245~284
[48]
Sun Jimin.Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau.Earth and Planetary Science Letters,2002,203(3~4):845~859
[49]
Tamburini F,Adatte T,Follmi K et al.Investigating the history of East Asian monsoon and climate during the last glacial-interglacial period(0~140000 years):Mineralogy and geochemistry of ODP Sites 1143 and 1144,South China Sea.Marine Geology,2003,201(1~3):147~168
[50]
Wehausen R.Brumsack H J.Astronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments.Earth and Planetary Science Letters,2002,201(3~4):621~636
[51]
刘志飞,赵玉龙,李建如等.南海西部越南岸外晚第四纪粘土矿物记录.中国科学(D辑),2007,37(9):1176~1184 Liu Zhifei,Zhao Yulong,Li Jianru et al.Late Quaternary clay minerals off Middle Vietnam in the western South China Sea:Implications for source analysis and East Asian monsoon evolution.Science in China(Series D),2007,50(11):1674~1684
[52]
Kennett J P.Marine tephrochronology.In:Emiliani C ed.The Sea (7).New York:Wiley,1981.1373~1436
[53]
陈国成,郑洪波,李建如等.48万年来南海及周边地区火山喷发作用的沉积学记录.海洋地质与第四纪地质,2007,27(4):69~76 Chen Guocheng,Zheng Hongbo,Li Jianru et al.Sedimentary records of volcanic activities in the South China Sea over the past 480ka.Marine Geology & Quaternary Geology,2007,27(4):69~76
[54]
Song S R,Chen C H,Lee M Y et al.Newly discovered eastern dispersal of the youngest Toba Tuff.Marine Geology,2000,167(3~4):303~312
[55]
Liang X,Wei G,Shao L et al.Records of Toba eruptions in the South China Sea-Chemical characteristics of the glass shards from ODP 1143A.Science in China(Series D),2001,31(10):871~878
[56]
Liu Zhifei,Colin C,Trentesaux A.Major element geochemistry of glass shards and minerals of the Youngest Toba Tephra in thesouthwestern South China Sea.Journal of Asian Earth Sciences,2006,27(1):99~107
[57]
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
[58]
罗运利,陈怀成,吴国瑄等.南海最近3个冰期旋回中的天然火与气候--ODP1114孔深海沉积中的炭屑记录.中国科学(D辑),2001,31(10):854~860 Luo Yunli,Chen Huaicheng,Wu Guoxuan et al.Records of natural fire and climate history during the last three glacial-interglacial cycles around the South China Sea-Charcoal record from the ODP 1144.Science in China(Series D),2001,31(10):897~904
[59]
Sun Xiangjun,Li Xu,Luo Yunli et al.The vegetation and climate at the last glaciation on the emerged continental shelf of the South China Sea.Palaeogeography,Palaeoclimatology,Palaeoecology,2000,160(3~4):301~316
[60]
李学杰.南海两部沉积特征及其从晚更新世以来的变化.上海:同济大学博士学位论文,2005.1~91 Li Xuejie.Sedimentary characteristics of the Western South China Sea and their variations since the Late Pleistocene.Dissertation for the Doctoral Degree.Shahghai:Tongji University,2005.1~91
[61]
Milliman J D.Syvitski J P M.Geomorphic/tectonic control of sediment discharge to the ocean:The importance of small mountainous rivers.Journal of Geology,1992,100(5):525~554
[62]
Selvaraj K,Chen C T A.Moderate chemical weathering of subtropical Taiwan:Constraints from solid-phase geochemistry of sediments and sedimentary rocks.Journal of Geology,2006,114:101~116
[63]
Lu Huayu,Zhang Fuqing,Liu Xiaodong et al.Patterns and frequencies of the East Asian winter monsoon variations during the past million years revealed by wavelet and spectral analyses.Global and Planetary Change,2002,35(1~2):67~74
[64]
Laskar J.The chaotic notion of the solar system:A numerical estimate of the size of the chaotic zoins.Icurus,1990,88:266~291
[65]
Paillard D,Labeyrie L,Yiou P.Analyseries 1.0:A macintosh software for the analysis of geographical time-series.EOS,1996,77:379