Detailed grain-size analyses, both in China and western Europe, indicate th
e occurrence of short climatic cycles during loess deposition of the last g
lacial. Cold episodes coincided with enhanced deposition of relatively coar
se loess and alternated with relatively warmer episodes with decreased depo
sition of finer loess and soil formation. In Europe, these oscillations may
coincide with alternations of permafrost development and degradation. The
short-term climatic events in the loess sections are similar to the Dansgaa
rd-Oeschger events in ice-core records. (C) 2001 Elsevier Science B.V. All
rights reserved.