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晚渐新世以来中国黄土高原风成红粘土序列的发现:亚洲内陆干旱化起源的新记录

, PP. 1469-1488

Keywords: 黄土高原,风成红粘土,磁性地层,晚渐新世,亚洲内陆干旱化

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Abstract:

?亚洲内陆荒漠的扩张影响了环境改善及经济社会发展,受到人们广泛关注.亚洲内陆干旱化成为古气候研究热点,其起始年代始终是这一研究的焦点问题.中国黄土高原晚新生代风成黄土和红粘土沉积作为研究亚洲内陆干旱化的理想载体,蕴含丰富的古气候信息.本文对黄土高原西部庄浪钻孔654m的岩芯进行了磁性地层学、沉积学和地球化学研究.结果表明,庄浪岩芯记录了25.6~4.8Ma的连续磁极性变化序列,主要由高分辨率的风成红粘土序列构成,最早的风成红粘土出现于25Ma,表明亚洲内陆干旱化至少在晚渐新世已经出现,这为研究晚渐新世以来亚洲内陆干旱化过程提供了不可多得的地质记录.

References

[1]  1 刘东生, 张宗祜. 中国的黄土. 地质学报, 1962, 42: 1—14
[2]  2 卢演俦, 安芷生. 约70万年以来黄土高原自然环境变化系列探讨. 科学通报, 1979, 24: 221—224
[3]  3 刘东生, 文启忠, 郑洪汉, 等. 中国黄土的古气候记录及其反映的古气候演化. 国际交流地质学术论文集(5): 水文地质 工程地质 第四纪地质 地貌. 北京: 地质出版社, 1980. 77—82
[4]  4 刘东生, 等. 黄土与环境. 北京: 科学出版社, 1985. 1—481
[5]  5 Kukla G, An Z S. Loess stratigraphy in central China. Paleogeogr Paleoclimatol Paleoecol, 1989, 72: 203—233
[6]  6 Kukla G, An Z S, Melice J L, et al. Magnetic susceptibility record of Chinese Loess. Trans Royal Soc Edinb-Earth Sci, 1990, 81: 263—288
[7]  7 丁仲礼, 刘东生. 中国黄土研究新进展(一) 黄土地层. 第四纪研究, 1989, 1: 24—25
[8]  8 Heller F, Liu T S. Magnetostratigraphical dating of loess deposits in China. Nature, 1982, 300: 431—433
[9]  9 安芷生, 卢演俦. 华北晚更新世马兰期气候地层划分. 科学通报, 1984, 29: 228—231
[10]  10 Sadao S, Wang Y Y. Magneto and chronostratigraphy revealed from the Luochuan loess sequence in China and its relevance to the Quaternary climatic change. In: Sadao S, Wang Y Y, eds. The Recent Research of Loess in China. Kyoto: Wako Printing, Ltd, 1984. 211—230
[11]  11 Kukla G, Heller F, Ming L X. Pleistocene climates in China dated by magnetic susceptibility. Geology, 1988, 16: 811—814
[12]  12 丁仲礼, 刘东生. 1.8 Ma 以来黄土-深海古气候记录对比. 科学通报, 1991, 18: 1401—1403
[13]  13 An Z S, Kukla G J, Porter S C, et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quat Res, 1991, 36: 29—36
[14]  14 An Z S, Kukla G J, Porter S C, et al. Late Quaternary dust flow on the Chinese Loess Plateau. Catena, 1991, 18: 125—132
[15]  15 Rutter N, Ding Z L, Evans M E, et al. Baoji-type pedostratigraphic section, Loess Plateau, north-central China. Quat Sci Rev, 1991, 10: 1—22
[16]  16 Rutter N W, Ding Z L, Evans M E, et al. Paleoclimates and monsoon variations interpreted from micromorphogenic features of Baoji paleosols, China. Quat Sci Rev, 1993, 12: 853—862
[17]  17 Ding Z L, Yu Z W, Rutter N W, et al. Towards an orbital time scale for Chinese loess deposits. Quat Sci Rev, 1994, 13: 39—70
[18]  18 An Z S, Liu T S, Lu H Y, et al. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China. Quat Int, 1990, 718: 91—95
[19]  19 安芷生, 吴锡浩, 汪品先, 等. 最近130 ka中国古季风—Ⅱ古季风变迁. 中国科学B辑, 1991, 11: 1209—1215
[20]  20 孙有斌, 鹿化煜, 安芷生. 黄土-古土壤中石英颗粒的粒度分布. 科学通报, 2000, 45: 2094—2097
[21]  21 Sun Y B, An Z S. Late Pliocene-Pleistocene changes in mass accumulation rates of eolian deposits on the central Chinese Loess Plateau. J Geophys Res, 2005, 110: D23101, doi: 10.1029/ 2005JD006064
[22]  22 Liu T S. Loess in China. 2nd ed. Beijing: China Ocean Press; Berlin, Heidelberg: Springer-Verlag, 1988. 1—224
[23]  23 赵景波. 西安、山西保德第三纪晚期红土研究. 沉积学报, 1989, 7: 113—120
[24]  24 丁仲礼, 孙继敏, 朱日祥, 等. 黄土高原红粘土成因及上新世北方干旱化问题. 第四纪研究, 1997, 2: 147—157
[25]  32 Sun D H, Shaw J, An Z S, et al. Magnetostratigraphy and paleoclimatic interpretation of a continuous 7.2 Ma Late Cenozoic eolian sediments from the Chinese Loess Plateau. Geophys Res Lett, 1998, 25: 85—88
[26]  33 Sun D H, An Z S, Shaw J, et al. Magnetostratigraphy and paleoclimatic significance of late Tertiary aeolian sequences in the Chinese Loess Plateau. Geophys J Int, 1998, 134: 207—212
[27]  34 安芷生, 王苏民, 吴锡浩, 等. 中国黄土高原的风积证据: 晚新生代北半球大冰期开始及青藏高原的隆升驱动. 中国科学D辑: 地球科学, 1998, 28: 481—490
[28]  35 丁仲礼, 孙继敏, 杨石岭, 等. 灵台黄土-红粘土序列的磁性地层及其粒度记录. 第四纪研究, 1998, 1: 86—94
[29]  36 Ding Z L, Sun J M, Yang S L, et al. Preliminary magnetostratigraphy of a thick eolian red caly-loess sequence at Lingtai, the Chinese Loess Plateau. Geophys Res Lett, 1998, 25: 1225—1228
[30]  37 Ding Z L, Xiong S F, Sun J M, et al. Pedostratigraphy and paleomagnetism of a similar to 7.0 Ma eolian loess-red clay sequence at Lingtai, Loess Plateau, north-central China and the implications for paleomonsoon evolution. Palaeogeogr Palaeoclimatol Palaeoecol, 1999, 152: 49—66
[31]  38 宋友桂, 方小敏, 李吉均, 等. 六盘山东麓朝那剖面红粘土年代及其意义. 第四纪研究, 2000, 20: 2182—2185
[32]  39 Qiang X K, Li Z X, Powell C McA, et al. Magnetostratigraphic record of the Late Miocene onset of the East Asian monsoon, and Pliocene uplift of northern Tibet. Earth Planet Sci Lett, 2001, 187: 83—93
[33]  40 Xu Y, Yue L P, Li J X, et al. An 11-Ma-old red clay sequence on the Eastern Chinese Loess Plateau. Paleogeogr Paleoclimatol Paleoecol, 2009, 284: 383—391
[34]  41 Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 2002, 416: 159—163
[35]  42 Sun J M, Ye J, Wu W Y, et al. Late Oligocene-Miocene mid-latitude aridification and wind patterns in the Asian interior. Geology, 2010, 38: 515—518
[36]  43 Qiang X K, An Z S, Fu C F, et al. Magnetostratigraphy of Zhuanglang drilling core from western Loess Plateau. The 5th International Symposium on Tibetan Plateau & the 24th Himalaya-Karakorum-Tibet Workshop. 11—14 August 2009, Beijing, China, 2009. S2.7, 69
[37]  44 Zijderveld J D A. AC demagnetization of rocks: Analysis of results. In: Collinson D W, Runcorn S K, Creer K M, eds. Methods in Paleomagnetism. New York: Elsevier, 1967. 254—286
[38]  45 Kirschvink J L. The least-squares line and plane and the analysis of paleomagnetic data. Geophys J Royal Astron Soc, 1980, 62: 699—718
[39]  46 Cande S C, Kent D V. Revised calibration of the geomagnetic polarity timescale for the late Cretaceous and Cenozoic. J Geophys Res, 1995, 100: 6093—6095
[40]  47 刘进峰, 郭正堂, 乔彦松, 等. 秦安中新世黄土-古土壤序列石英颗粒形态特征、粒度分布及其对成因的指示意义. 科学通报, 2005, 50: 2806—2809
[41]  48 Ding Z L, Rutter N W, Sun J M, et al. Re-arrangement of atmospheric circulation at about 2.6 Ma over northern China: Evidence from grain size records of loess-palaeosol and red clay sequences. Quat Sci Rev, 2000, 19: 547—558
[42]  49 Sun J M. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau. Earth Planet Sci Lett, 2002, 203: 845—859
[43]  50 Guo Z T, Sun B, Zhang Z S, et al. A major reorganization of Asian climate by the early Miocene. Clim Past, 2008, 4: 153—174
[44]  57 Harrison T M, Copeland P, Kidd W S F, et al. Raising Tibet. Science, 1992, 255: 1663—1670
[45]  58 Kutzbach J E, Prell W L, Ruddimman W F. Sensitivity of Eurasian climate to surface uplift of the Tibetan Plateau. J Geol, 1993, 101: 177—190
[46]  25 Ding Z L, Sun J M, Liu T S, et al. Wind-blown origin of the Pliocene red clay formation in the central Loess Plateau, China. Earth Planet Sci Lett, 1998, 161: 135—143
[47]  26 Lu H Y, Vandenberghe J, An Z S. Aeolian origin and paleoclimatic implications of the ‘Red Clay’ (North China) as evidenced by grain-size distribution. J Quat Sci, 2001, 16: 89—97
[48]  27 Yang S L, Ding Z L. Comparison of particle size characteristics of the Tertiary ‘red clay’ and Pleistocene loess in the Chinese Loess Plateau: Implications for origin and sources of the ‘red clay’. Sedimentology, 2004, 51: 77—93
[49]  28 刘进峰, 郭正堂, 郝青正, 等. 秦安中新世黄土-古土壤序列石英颗粒形态特征、粒度分布及其对成因的指示意义. 科学通报, 2005, 50: 2806—2809
[50]  29 乔彦松, 郭正堂, 郝青正, 等. 中新世黄土-古土壤序列的粒度特征及其对成因的指示意义. 中国科学D辑: 地球科学, 2006, 36: 646—653
[51]  30 Li F J, Wu N Q, Pei Y P, et al. Wind-blow origin of Dongwan late Miocene-Pleiocene dust sequence documented by land snail record in western Chinese Loess Plateau. Geology, 2006, 34: 405—408
[52]  31 孙东怀, 刘东生, 陈明扬, 等. 中国黄土高原红粘土序列的磁性地层与气候变化. 中国科学D辑: 地球科学, 1997, 27: 265—270
[53]  51 Rea D K, Leinen M, Janecek T R. Geologic approach to the long-term history of atmospheric circulation. Science, 1985, 227: 721—725
[54]  52 Garzione C N, Ikari M J, Basu A R. Source of Oligocene to Pliocene sedimentary rocks in the Linxia Basin in northeastern Tibet from Nd isotopes: Implications for tectonic forcing of climate. Geol Soc Am Bull, 2006, 117: 1156—1166
[55]  53 Ruddimman W F, Kutzbach J K. Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and American West. J Geophys Res, 1989, 94: 18409—18427
[56]  54 Manabe S, Broccoli A J. Mountains and arid climates of middle latitudes. Science, 1990, 247: 192—195
[57]  55 An Z S, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and phased uplift of the Himalayan Tibetan Plateau since Late Miocene times. Nature, 2001, 411: 62—66
[58]  56 Kutzbach J E, Guetter P J, Ruddimman W F, et al. Senseitivity of climate to Late Cenozoic uplift in southern Asia and the American West: Numerical experiments. J Geophys Res, 1989, 94: 18393—18407
[59]  59 Ramstein G, Fluteau F, Besse J, et al. Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years. Nature, 1997, 386: 788—795

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