Abstract
Our understanding of the continental climate development in East Asia is mainly based on loess-paleosol sequences and summer monsoon precipitation reconstructions based on oxygen isotopes (δ
Original language | English |
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Pages (from-to) | 256-264 |
Journal | Earth and Planetary Science Letters |
Volume | 301 |
Issue number | 1-2 |
DOIs | |
Publication status | Published - 2011 |