Abstract
Lateglacial environments at Hijkermeer, northwest Netherlands, were reconstructed by means of chironomid, diatom and pollen analyses. Diatom assemblages indicate that Hijkermeer was a shallow, oligo- to mesotrophic lake during this period. Pollen assemblages reflect the typical northwest European Lateglacial vegetation development and provide an age assessment for the record from the beginning of the Older Dryas (ca 14 000 calibrated
Original language | English |
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Pages (from-to) | 2420-2437 |
Journal | Quaternary Science Reviews |
Volume | 26 |
Issue number | 19-21 |
DOIs | |
Publication status | Published - 2007 |