| [1]An Z S,Liu T S,Lu Y C,et al.The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China[J].Quaternary International,1990,7/8:91-95.[2]An Z S,Kukla G,Porter S C,et al.Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130 000 years[J].Quaternary Research,1991,36:29-36.[3]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[J].Paleoceanography,2002,17(3):511-521.[4]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.[5]Sun Y B,Clemens S C,Morrill C,et al.Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon[J].Nature Geoscience,2012,5(1):46-49.[6]王丰年,李保生,牛东风,等.萨拉乌苏河流域MGS1层段粒度与CaCO3记录的全新世千年尺度的气候变化[J].中国沙漠,2012,32(2):331-339.[7]Prins M A,Postma G,Weltije G.Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary:The Makrancontinental slope[J].Marine Geology,2000,169:351-371.[8]王君兰,李晖,邓伟,等.内蒙古嘎顺诺尔湖泊沉积物磁化率与粒度的古环境意义[J].中国沙漠,2012,32(3):661-668.[9]孙东怀,安芷生,苏瑞侠,等.古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展,2001,11(3):269-276.[10]成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1978:1-147.[11]肖尚斌,李安春,蒋富清,等.近2 ka来东海内陆架的泥质沉积记录及其气候意义[J].科学通报,2004,49(21):2233-2238.[12]吴正,王为.华南沿海老红砂的成因与古地理环境[J].中国科学(D辑),1997,27(6):537-542.[13]陈居成,曾从盛,吴幼恭.闽东南沿海老红砂的分布与沉积地貌特征[J].台湾海峡,1998,17(1):50-54.[14]曾从盛,陈居成,吴幼恭.闽东南沿海老红砂研究[Ｍ].北京:地质出版社,1999:1-74.[15]李志文,李保生,孙俪,等.中国东南沿海老红砂的研究现状与展望.中国沙漠,2011,31(1):49-57.[16]吴正,王为.闽粤沿海老红砂多期沉积地层的发现及其意义[J].中国沙漠,2001,21(4):328-332.[17]吴正,黄山,金志敏,等.华南沿海老红砂的成因与红化作用[J].地理学报,1994,49(4):298-305.[18]陈方.海坛岛海岸风沙特征及其发育[J].海洋科学,1994,6:46-50.[19]吴正,王为,谭慧忠,等.闽南粤西沿海老红砂的沉积年代[J].科学通报,2000,45(3):533-537.[20]袁宝印,夏正楷,李保生,等.中国南方红土年代地层学与地层划分问题[J].第四纪研究,2008,28(1):1-13.[21]谭惠忠,吴正.闽粤沿海老红砂的热释光测年[J].中国沙漠,2001,21(4):393-396.[22] Grootes P M,Stuiver M,White J W C,et al.Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores[J].Nature,1993,366:552-554.[23] Wang Y J,Chen H,Edwards R L,et al.A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave,China[J].Science,2001,294:2345-2348.[24]金栋生,郑芬.福建省中部沿海地区十二万年来的古气候[J].福建地质,1993,12(3):218-227.[25]曾从盛.福建晚更新世海侵问题探讨[J].热带海洋,1993,12(1):39-45.[26]陆继军.福建沿海晚第四纪孢粉组合古植被和古气候[J].地理科学,1994,14(4):381-383.[27]赵侃,孔兴功,程海,等.MIS 3晚期东亚季风强度和DO事件年龄[J].第四纪研究,2008,28(1):177-183.[28]刘殿兵,汪永进,陈仕涛,等.东亚季风MIS 3早期DO事件的亚旋回及全球意义[J].第四纪研究,2008,28(1):169-176.[29]Yuan D X,Cheng H,Edwards R L,et al.Timing,duration,and transitions of the last interglacial Asian Monsoon[J].Science,2004,304:575-578.[30]杨达源,陈可锋,舒肖明.深海氧同位素第3阶段晚期长江三角洲古环境初步研究[J].第四纪研究,2004,24(5):525-530.[31]张茂恒,夏应菲,孟景闻,等.下蜀黄土中记录的氧同位素3阶段(MIS3)特殊暖湿现象[J].土壤学报,2008,45(1):9-15.[32]温小浩,李保生,郑琰明,等.岭南东江流域一级阶地网纹红土的时代及其粒度特征[J].地理与地理信息科学,2009,25(5):59-63.[33]朱永其,李承伊,曾成开.东海大陆架晚更新世最低海面[J].科学通报,1978,24(1):317-320.[34]王靖泰,汪品先.中国东部晚更新世以来海面升降与气候变化的关系[J].地理学报,1980,35(4):299-312.[35]张威,闫玲,崔之久,等.东亚沿海山地末次冰期冰川与环境[J].地理学报,2009,64(1):33-42.[36]任黎秀,和艳,杨达源.鄱阳湖湖滨十万年来沙山的演化[J].地理研究,2008,27(1):128-134.[37]Luo W,Li J J,Lu H Y,et al.The East Asian Winter Monsoon over the last 15 000 years:its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon[J].Quaternary Science Reviews,2012,32:131-142.[38]徐方建,李安春,万世明,等.东海内陆架泥质区中全新世环境敏感粒度组分的地质意义[J].海洋学报,2009,31(3):95-102.[39]李森,廖肖霞,王贵勇.近40 ka来海南岛海岸沙地气候与环境演变[J].地理研究,2009,28(5):1235-1242.[40]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.[41]Bond G,Broecker W,Johnsen S,et al.Correlations between climate records from North Atlantic sediments and Greenland ice[J].Nature,1993,365:143-147.[42]Thouveny N,de Beaulleu J L,Bonifay E,et al.Climate variations in Europe over the past 140 kyr deduced from rock magnetism[J].Nature,1994,371:503-506.[43]Thunell R C,Mortyn P G.Glacial climate instability in the Northeast Pacific-ocean[J].Nature,1995,376:504-506.[44]Sun Y B,Wang X L,Liu Q S,et al.Impacts of post-depositional processes on rapid monsoon signals recorded by the last glacial loess deposits of northern China[J].Earth and Planetary Science Letters,2010,29:171-179.[45]郭正堂,刘东生,吴乃琴,等.最近两个冰期黄土记录中的Heinrich型气候节拍[J].第四纪研究,1996,(1):31-40.[46]方小敏,潘保田,管东红,等.兰州约60 ka以来夏季风千年尺度不稳定性研究[J].科学通报,1999,44(4):436-439.[47]张美良,程海,袁道先,等.末次冰期贵州七星洞石笋高分辨率气候记录与Heinrich事件[J].地球学报,2004,25(3):337-344.[48]Wang L,Sarnthein M,Erlenkeuser H,et al.East Asian monsoon climate during the Pleistocene:high resolution sediment records from the South China Sea[J].Marine Geology,1999,156:245-284. |
2013, Vol. 33 
