Comparison Between the Formation of Peatlands and Paleosols of Sandy Land and the Changes of Ari4 Index During Holocene in Northeast China

被引：0
|
作者：
李取生
机构：
[1] Changchun Institute of Geography
[2] Changchun 130021
[3] PRC
[4] Academia Sinica
来源：
Chinese Science Bulletin | 1994年 / 15期
基金：
中国国家自然科学基金;
关键词：
Northeast China; peatlands and paleosols of sandy land; comparison study; change of aridity;
D O I：
暂无
中图分类号：
P531 [古地理学];
学科分类号：
070903 ;
摘要：
In Northeast China, peatlands and paleosols have developed very well in the eastern swamps and western sandy lands, respectively. They become an important object of studying the paleoenvironment in this region. Since both of them were formed under humid climate conditions, it is significant to compare their formation and ages for the unification of climatic change divisions and the reconstruction of the paleoclimate
引用
收藏
页码：1290 / 1294
页数：5
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