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Deposits and Soils of the Past 130,000 Years at the Desert–Loess Transition in Northern China

Published online by Cambridge University Press:  20 January 2017

Jimin Sun  and
Zhongli Ding
Jimin Sun*
Affiliation:
Institute of Geology, Chinese Academy of Sciences, P.O. Box 9825, Beijing, 100029, China
Zhongli Ding
Affiliation:
Institute of Geology, Chinese Academy of Sciences, P.O. Box 9825, Beijing, 100029, China
*
1E-mail: jmsun@igcas.igcas.ac.cn.
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Abstract

The desert–loess transitional zone in north-central China has long been thought sensitive to Quaternary climatic change. However, reconstruction of Quaternary climates in this area has been hindered by incompleteness of geological sections. Here we report the analytical results of two recently found sand–loess–soil sections. Both sections have thick eolian deposits from the last interglacial–glacial cycle and can be correlated with one another. Field observations, thermoluminescence dating, and other laboratory analyses show that the last interglacial period produced three paleosols and two intercalated loess layers. Loess from the last glacial period is interbedded with three sand horizons that represent desert extension. The expansion and contraction of desert in northern China may have been forced by the east Asia monsoon.

Type
Original Articles
Information
Quaternary Research , Volume 50 , Issue 2 , September 1998 , pp. 148 - 156
Copyright
University of Washington

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