中国黄土区东亚古季风气候与冰期气候对比研究

A Comparative Study between the East Asia Paleomonsoon Climate and Glacial Climate in Chinese Loess Area

研究了中国黄土区冰期气候与季风气候记录；进行了黄土磁化率与大洋δ１８Ｏ曲线对比，并且将黄土组合—古土壤组合与冰期－间冰期气候进行了比较。结果表明：黄土组合与古土壤组合记录了冰期气候与间冰期气候；中国黄土—古土壤堆积是全球冰期—间冰期气候变化与东亚古季风气候变化共同作用的结果。

The records of Paleomonsoon and glacial climate in Chinese Loess Areas have been studied on the base of comparison between magnetic susceptibility curve and oceanic δ 18 O curve. It was explored the relationship between Loess Paleosol sequence and glacial interglacial climate, which led to such a conclusion that the Loess Paleosol sequence was the outcome of changeable glacial interglacial climate. Chinese Loess Paleosol sediments were just controlled by both the factors of glacial interglacial and paleomonsoon climate.