Article ID Journal Published Year Pages File Type
4685510 Geomorphology 2011 16 Pages PDF
Abstract
► Holocene coastal foredunes (southern Baltic Sea) were dated by OSL. ► Change in foredune progradation dynamic occurred after 800 AD. ► Dating reveals six hiatuses within foredune progradation. ► The timing of hiatuses correlates with phases of enhanced aeolian activity. ► Four hiatuses probably correlate with general climatic shifts during the Holocene.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Reconstruction of Holocene coastal foredune progradation using luminescence dating - An example from the Świna barrier (southern Baltic Sea, NW Poland)
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