地球科学进展 ›› 2019, Vol. 34 ›› Issue (1): 34 -47. doi: 10.11867/j.issn.1001-8166.2019.01.0034

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中亚干旱区第四系黄土和干旱环境研究进展
王鑫 1( ),张金辉 1,贾佳 1, 2,王蜜 1,王强 1,陈建徽 1,王飞 1,李再军 1,陈发虎 1, 3, *( )   
  1. 1. 兰州大学资源环境学院西部环境教育部重点实验室,甘肃 兰州 730000
    2. 浙江师范大学地理与环境科学学院,浙江 金华 321004
    3. 中国科学院青藏高原研究所,北京 100101
  • 收稿日期:2018-11-27 修回日期:2018-12-28 出版日期:2019-01-10
  • 通讯作者: 陈发虎 E-mail:xinw@lzu.edu.cn;fhchen@itpcas.ac.cn
  • 基金资助:
    国家自然科学基金项目“塔吉克盆地晚始新统—中新统风成沉积序列的年代学和古环境记录研究”(编号:41672158);国家重点研发计划项目“亚洲中部干旱区气候变化影响与丝路文明变迁研究”(编号:2018YFA0606404)

Pleistocene Loess-Paleosol Sequences in Arid Central Asia State of Art

Xin Wang 1( ),Jinhui Zhang 1,Jia Jia 1, 2,Mi Wang 1,Qiang Wang 1,Jianhui Chen 1,Fei Wang 1,Zaijun Li 1,Fahu Chen 1, 3, *( )   

  1. 1. Key Laboratory of Western China's Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
    2. College of Geography and Environmental Sciences, Zhejiang Normal University, Zhejiang 321004, China
    3. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2018-11-27 Revised:2018-12-28 Online:2019-01-10 Published:2019-03-05
  • Contact: Fahu Chen E-mail:xinw@lzu.edu.cn;fhchen@itpcas.ac.cn
  • About author:Wang Xin (1983-), male, Wuzhi County, He'nan Province, Associate professor. Research areas include quaternary geology and global change. E-mail: xinw@lzu.edu.cn |Chen Fahu (1962-), male, Danfeng County, Shaanxi Province, Professor, Academician of Chinese Academy of Sciences. Research areas include environmental change and the evolution of human civilization.E-mail: fhchen@itpcas.ac.cn
  • Supported by:
    National Natural Science Foundation of China “Chronological and paleoenvironmental study on the late Eocene to Miocene aeoilan sequences in the Tajik Basin”(No. 41672158);The National Key R&D Program of China “Research on the impact of environmental changes in central Asia and the change of the Silk Road civilization”(No. 2018YFA0606404)

中亚黄土位于连接欧洲黄土和中国黄土的咽喉地带,黄土地层的古气候记录研究对完整认识地质时期欧亚大陆古气候的演化历史、空间差异和不同时间尺度上的主控因素,深入理解欧亚大陆西风—季风系统的相互作用机制有重要意义。然而,中亚黄土的研究程度与欧洲和中国黄土相比明显偏弱,尤其与中国黄土的对比研究亟待加强。综述了近些年中亚第四系黄土研究的主要进展,基于代表性剖面和中国黄土古气候记录粗框架的对比,讨论了中亚干旱区第四纪以来构造尺度上的干旱化过程,轨道尺度上的干湿变化历史和亚轨道尺度上的干湿变化及其与东亚季风区古气候变化的相位关系。

Loess of central Asia is located in a linkage zone between the European and Chinese loess depositional belts. Paleoclimate signatures from loess-paleosol sequences here is a key for completely understanding the spatial-tempo paleoclimate changes of Euro-Asia and for understanding the interactions between westerlies and Asia monsoon system during geological time. However, paleoclimate investigations of loess-paleosol sequences in arid central Asia is relatively weak than those from Europe and Chinese Loess Plateau. Specific, correlations of paleoclimate records with Chinese loess is required for better understanding “westerly regimes” in central Asia and its phase relationship with monsoon Asia on various time scale. In this work, we reviewed new advantages of loess study in central Asia during the last decades. Based on the stratigraphic and paleoclimatic correlations of loess-paleosol sequences between central Asia and the Chinese Loess Plateau, we discussed aridification history of Asia on tectonic time scale, the hydroclimate changes in arid central Asia and its phase relationship with Monsoonal Asia on orbital and millennial time scale during the Pleistocene.

中图分类号: 

图1 亚洲内陆气候格局和本文涉及的黄土剖面位置
Fig. 1 Major climate regimes over Central Asia and locations of typical loess sections
图2 中亚干旱区典型黄土—古土壤剖面照片
Fig. 2 Photograph showing lithology of representative loess-paleosol sequences from Central Asia
图3 中亚黄土释放—搬运—沉积过程示意图[ 58 ]
Fig. 3 Schematic map showing emission, transportation, and deposition processes of loess deposits in Central Asia [ 58 ]
图4 伊朗北部晚第四系黄土粒度组成及组分分离结果[ 64 ]
Fig. 4 Grain-size distribution of upper Pleistocene loess in north Iran [ 64 ]
图5 中亚第四系黄土—古土壤序列及其与中国黄土高原的对比框架[ 27 , 35 , 42 , 43 ]
Fig. 5 Pleistocene loess-paleosol sequences in Central Asia and its correlation with the Chinese Loess Plateau [ 27 , 35 , 42 , 43 ]
图6 末次间冰期以来中亚代表性黄土—古土壤剖面的红度记录及其与中国黄土高原的对比[ 41 , 43 , 86 , 88 , 89 ]
Fig. 6 Correlations of redness records from loess-paleosol sequences in Central Asia and the Chinese Loess Plateau since last inter-glacial period [ 41 , 43 , 86 , 88 , 89 ]
图7 中亚干旱区第四系黄土剖面的红度记录及其与中国黄土高原、深海氧同位素记录的对比框架[ 42 , 43 , 88 , 89 ]
Fig. 7 Correlations of redness records from loess-paleosol sequences in Central Asia and the Chinese Loess Plateau since Pleistocene [ 42 , 43 , 88 , 89 ]
图8 中亚干旱区冰期(a)和间冰期(b)大气环流示意图[ 46 , 90 ]
Fig. 8 Schematic map showing major circulation patterns in central Asia during glacial (a) and interglacial (b) periods [ 46 , 90 ]
图9 鹿角湾剖面的湿度记录[ 8 ]及其与中国黄土[ 94 ]和公海湖泊记录[ 93 ]的对比
Fig. 9 Proxy indices of moisture changes from the Lujiaowan Section [ 8 ] and its correlation with those from the Chinese Loess [ 94 ] and Gonghai Lake [ 93 ]
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