| 古气候与环境演变 |
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| Climate Fluctuations during Marine Isotope Stage 3 Suggested by Major Element Records in The Milanggouwan Stratigraphical Section in Salawusu River Valley, Inner Mongolia, China |
| WEN Xiao-hao1, LI Bao-sheng1,2, David Dian Zhang3, ZHENG Yan-ming4, NIU Dong-feng1, DU Shu-huan1 |
| 1.School of Geography, South China Normal University, Guangzhou 510631, China; 2.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710061, China; 3.Department of Geography, Hongkong University, Pokulam Road, Hongkong, China; 4.School of Geography and Planning Sun Yat-sen University, Guangzhou 510275, China |
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Abstract The Milanggouwan stratigraphical section in Salawusu river valley on the Ordos Plateau is an ideal site for reconstructing the paleoclimate of Mu Us Desert since the Late Pleistocene. Its MIS3 sequence contained four sedimentary types and were divided into nineteen units, and they constituted half nine sedimentary cycles for paleo-mobile dune sands alternating with fluvial-lacustrine facies and paleosols. The results of major elements analysis showed the contents of Al2O3, TOFE, CaO, MgO, K2O, Na2O and TiO2 in fluvial-lacustrine facies and paleosols were apparently higher than that in paleo-mobile dune sands; contrary is the contents of SiO2 for them; and thus these major elements constituted the similar half nine "element cycles". These "element cycles" showed that the megainterstadial climates of the Salawusu valley at least went through ten wet-warm events(W) and nine cold-dry events(C) and could be divided into five substages: MIS3e (58.90~49.50 kaBP), MIS3d (49.50~40.70 ka BP), MIS3c (40.70~36.90 ka BP), MIS3b (36.90~27.00 ka BP) and MIS3a (27.00~22.30 ka BP). Thereinto, the nineteen cold warm climatic fluctuations were roughly corresponded with the stadial interstadial of GRIP ice core; as well, the five substages were rather consistent with the Guliya ice core in the climatic fluctuating features and phase as well as the North Atlantic climate reflected by the N. pachydema(s.) numbers of V23-81 core.
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Received: 11 December 2008
Published: 07 September 2009
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Cite this article:
WEN Xiao-hao;LI Bao-sheng;David Dian Zhang;ZHENG Yan-ming;NIU Dong-feng;DU Shu-huan. Climate Fluctuations during Marine Isotope Stage 3 Suggested by Major Element Records in The Milanggouwan Stratigraphical Section in Salawusu River Valley, Inner Mongolia, China. JOURNAL OF DESERT RESEARCH, 2009, 29(5): 835-844.
URL:
http://www.desert.ac.cn/EN/ OR http://www.desert.ac.cn/EN/Y2009/V29/I5/835
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[1]Bocquet-Appel J P,Demars P Y.Neanderthal contraction and modern human colonization of Europe[J].Antiquity,2000,74:544-52.
[2]Antje H L.Voelker,workshop participants.Global distribution of centennial-scale records for Marine Isotope Stage (MIS) 3:A database[J].Quaternary Science Reviews,2002,21(10):1185-1212
[3]Van Andel T H.Reconstructing climate and landscape of the middle part of the last glaciation in Europe—The Stage 3 Project [J].Quaternary Research,2002,57:2-8.
[4]张慧,潘保田,徐树建,等.末次间冰期以来渭河上游气候演化的黄土记录研究[J].中国沙漠,2007,27(2):182-186.
[5]王涛.干旱区绿洲化、荒漠化研究的进展与趋势[J].中国沙漠,2009,29(1):1-9.
[6]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(20):1475-1480.
[7]李炳元.青藏高原大湖期[J].地理学报,2000,55(2):174-182.
[8]张虎才,马玉贞,彭金兰,等.距近42~18 ka腾格里沙漠古湖泊及古环境[J].科学通报,2002,47(24):1847-1857.
[9]陈一萌,饶志国,张家武,等.中国黄土高原西部马兰黄土记录的MIS3气候特征与全球气候记录的对比研究[J].第四纪研究,2004,24(3):355-365.
[10]夏正楷,刘德成,王幼平,等.郑州织机洞遗址MIS3阶段古人类活动的环境背景[J].第四纪研究,2008,28(1):96-102.
[11]隆浩,王乃昂,李育,等.毛乌素沙地北缘泊江海子剖面粒度特征及环境意义[J].中国沙漠,2007,27(2):187-193.
[12]鲁瑞洁,夏虹,强明瑞,等.近130 a来毛乌素沙地北部泊江海子湖泊沉积记录的气候环境变化[J].中国沙漠,2008,28(1):44-49.
[13]中国地质学会编辑委员会,中国科学院地质研究所.中国区域地层表(草案)[M].北京:科学出版社,1956:167-187.
[14]董光荣,李保生,高尚玉.由萨拉乌苏河地层看晚更新世以来毛乌素沙地的变迁[J].中国沙漠,1983,3(2):9-14.
[15]关有志,陈振英,贾惠兰.萨拉乌苏河地区第四纪地层中的元素分布与古气候[J].中国沙漠,1986,6(1):32-35.
[16]邵亚军.萨拉乌苏河地区晚更新世以来的孢粉组合及其反映的古植被和古气候[J].中国沙漠,1987,7(2):22-27.
[17]李保生,董光荣,吴正,等.鄂尔多斯萨拉乌苏河地区马兰黄土与萨拉乌苏组的关系及其地质时代问题[J].地质学报,1987,61(3):218-230.
[18]李保生,董光荣,吴正,等.我国北方上更新统城川组的建立[J].地质论评,1993,39(2):91-100.
[19]李保生,靳鹤龄,吕海燕,等.150 ka以来毛乌素沙地的堆积与变迁过程[J].中国科学(D辑),1998,28(1):85-90.
[20]Li Baosheng,David Dian Zhang,Jin Heling,et al.Palaeo-monsoon activities of Mu Us Desert,China since 150 ka—A study of the stratigraphic sequences of the Milanggouwan section,Salawusu River area[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2000,162:1-16.
[21]李保生,靳鹤龄,祝一志,等.“河套东南角理想剖面”的新近研究[J].中国沙漠,2001,21(4):346-353.
[22]李后信,李保生,祝一志,等.150 ka BP以来萨拉乌苏河流域主元素变动旋回[J].地球化学,2002,31(5):424-432.
[23]吕玉晓,李保生,靳鹤龄,等.萨拉乌苏河流域末次间冰期全球变化区域响应的主元素记录[J].中国沙漠,2004,24(2):136-143.
[24]李明启,靳鹤龄,董光荣,等.萨拉乌苏河流域微量元素揭示的气候变化[J].中国沙漠,2006,26(2):172-179.
[25]靳鹤龄,李明启,苏志珠,等.220 ka以来萨拉乌苏河流域地层磁化率与气候变化[J].中国沙漠,2006,26(5):680-686.
[26]靳鹤龄,董光荣,左昕昕.滴哨沟湾地层沉积特征记录的毛乌素沙地变迁[J].中国沙漠,2008,28(6):1064-1072.
[27]Martinson D G,Pisias N G,Hays J D,et al.Age dating and the orbital theory of the Ice ages:Development of a high-resolution 0~300 000-year chronostratigraphy[J].Quaternary Research,1987,27:1-29.
[28]Stuiver M,Reimer P J,Bard E,et al.INTCAL98 Radiocarbon age calibration 24 000~0 cal a BP[J].Radiocarbon,1998,40:1041-1083.
[29]Stuiver M,Reimer P J,Reimer R W.2005.CALIB 5.0.http://radiocarbon.pa.qub.ac.uk/calib/.
[30]Reimer P J,Baillie M G L,Bard E,et al.IntCal04 Terrestrial radiocarbon age calibration,0~26 cal kyr BP[J].Radiocarbon,2004,46(3):1029-1058.
[31]程序[EB/OL].http://www.calpal-online.de/index.html.
[32]高尚玉,董光荣,李保生,等.萨拉乌苏河第四纪地层中化学元素的迁移和聚集与古气候的关系[J].地球化学,1985(3):269-276.
[33]刘东生.黄土与环境[M].北京:科学出版社,1985:238-255.
[34]文启忠.中国黄土地球化学[M].北京:科学出版社,1989.
[35] Nesbitt H W,Young G M.Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations [J].Geochimica et Cosmochimica Acta,1984,48:1523-1534.
[36]陈骏,安芷生,刘连文,等.最近2.5 Ma以来黄土高原风尘化学组成的变化与亚洲内陆的化学风化[J].中国科学(D辑),2001,31(2):136-145.
[37]Honda M,Shimizu H.Geochemical,mineralogical and sedimentological studies on the Taklimakan Desert sands[J].Sedimentology,1998,45,1125-1143.
[38]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.
[39]Thompson L G,Yao T,Davis M E,et al.Tropical climate instability:The last glacial cycle from a Qinghai-Tibetan ice core[J].Science,1997,276:1821-1825.
[40]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.
[41]孙建中.黄土学[M].香港:香港考古学会出版社,2005.
[42]Bond G,Heinrich H,Broecker W,et al.Evidence for massive discharges of icebergs into the North Atlantic Ocean during the last glacial[J].Nature,1992,360:245-249.
[43]Heinrich H.Origin and consequences of cyclic ice-rafting in the Northeast Atlantic ocean during the past 130 000 years[J].Quaternary Research,1988,29:142-152. |
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2009, Vol. 29 
