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Loess near Lanzhou in the late Pleistocene is very sensitive to climatic fluctuations. The Beiyuan terrace profile in Linxia City, of which the curve of susceptibility tallies with the trend of isotopic curves of Vostok 2083 m ice core in Antarctica, is 35m thick. There are five layers of paleosols under Malan loess(L_1). Upper three layers (S_(1-a),S(1-b)and S_(1-c) correspond to three warm stages in last interglaciation, Interstadial of Last Glacial (C stage in Antarctic ice core)was clearly recorded in the Beiyuan profile, in which three layers of paleosols and two of loess were formed. The lowest section of the profile belongs to penultimate glaciation, in which fossils of cold-drought-resistant mammal and mollusc have been discovered.  相似文献   
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末次冰期旋迴兰州黄土剖面与南极东方站冰岩芯的对比   总被引:1,自引:0,他引:1  
本文论述了临夏市北塬阶地剖面的磁化率曲线与南极东方站2083m冰岩芯的同位素曲线变化趋势十分吻合,剖面厚35m,马兰黄土之下出现5层古土壤,上部3层(S_(1-a),S_(1-b),S_(1-c))对应末次间冰期的3个温暖阶段,末次冰期的间冰段(南极冰岩芯的C阶段)在北塬黄土剖面中有清楚的反映,形成3层古土壤和两层黄土,剖面底剖已属于倒数笫二次冰期,发现有耐干冷的哺乳动物和软体动物化石。  相似文献   
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