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Patterns of Late Glacial vegetation in The Netherlands
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Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly...
Trace element distribution and implications in sediments across the Allerød-Younger Dryas boundary in the Netherlands and Belgium
Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands-northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly s...
Early Holocene environmental change and the presence of Mesolithic people in the Tungelroyse Beek valley near Mildert, the Netherlands
Unlocking the wealth of Dutch pollen data for future research and education
Vegetation changes in the Grote Nete valley (Campine region, Belgium) during the Boreal: a response to the 9.3 ka event?
Controls on late-Holocene drift-sand dynamics: The dominant role of human pressure in the Netherlands
Appendix_A_and_B – Supplemental material for Controls on late-Holocene drift-sand dynamics: The dominant role of human pressure in the Netherlands ...
Controls on late-Holocene drift-sand dynamics: The dominant role of human pressure in the Netherlands ...