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Although in all sequences the organic wet layer 2 is directly superimposed by coversands Table 4 , it cur- rently remains unclear whether eolian sedimentation started immediately after these dune slacks turned dry.
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The higher positioned dune slacks 2 to 5 m above actual sea level , on the other hand, remained dry. At present, it is not very well understood whether the eolian sedimentation process ceased or con- tinued in these higher slacks. The lack of mineral material in the peat of wet phase 3 at Verre- broek 1 in contrast to the sandy peat of wet phase 2 at the same location suggests a temporary interruption of eolian activity.
In this stage, the Great Ridge turned into a massive overall dry coversand dune. Human Occupation The combination of a growing massive dune complex, which was gradually becoming drier, and numerous intermediate dune slacks must have created an increasingly attractive environment for prehistoric hunter-gatherers during the Late Glacial.
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The environment offered opportunities for hunting and gathering a variety of edible and useful plant material. The frequent occurrence of ani- mal dung fungi Sordariaceae , some probably associated with European elk Alces alces Bos et al. This is also the time interval in which the dune slacks reached their highest water level, making them attractive for hunting water fowl and mammals, such as beaver, and collecting freshwater snails.
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It is rather unlikely that these dune slacks were used for fishing as no fish remains were present in the deepest dune slacks, while remains of water fleas, such as Daphnia, which are usually eaten by fish, were found Bos et al. Figure 6 Simplified map showing the maximum extent of the Moervaart paleolake and the distribution of Federmesser sites along the southern edge of the Great Ridge of Maldegem-Stekene. Sampled locations: 1.
Rieme; 2. Unfortunately, these sites cannot be detected easily by means of tra- ditional survey methods field walking, manual coring, etc. Possibly the area was too hostile for human occupation during this period due to the intensity of wind erosion and extreme cold conditions. Also, the final disappearance of all open water reservoirs may have had a dramatic impact on human occupation of the area as this source of freshwater was no longer available for drinking water for both humans and animals.
The Lateglacial and early P. Geoarchaeological research of the large Postglacial occupation of northern Belgium: the evi- palaeolake of the Moervaart municipalities of Wacht- dence from Sandy Flanders.
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Notae Praehis- the European Plain. Continued carbon 37 2 — Development of the radiocarbon lake area East Flanders, Belgium : preliminary re- calibration program. Radiocarbon 43 2A — Notae Praehistoricae — In press. Journal of Reports Ghent University 3.
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IntCal09 and Marine09 radiocarbon age calibration p — Haute P. Mesolithic cial aeolian sand deposition in NW Europe: optical territories and land-use systems in north-western dating of the dune complex at Opgrimbie NE Bel- Belgium. Used Circular shears for circles and rings made of sheet metal in Slupsk, Poland Manufacturer: Weingarten Rotary shears are used to cut out perfect circles or rings from sheet metal.
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