Abstract
Understanding past climate events relies for a large part on correlations between various proxy records. For the last glacial cycle, these are mainly marine and ice core records. However, such tele-connections are often based on weak arguments. For terrestrial data the Hengelo interstadial is a key event, discovered more than 4 decades ago. Here we review the age of this event, in particular by its
Original language | English |
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Pages (from-to) | 21-28 |
Journal | Quaternary Geochronology |
Issue number | 32 |
DOIs | |
Publication status | Published - 2016 |