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Holocene aeolian sand mobilization, vegetation history and human impact on the stabilized sand dune area of the southern Nyírség, Hungary

Published online by Cambridge University Press:  02 August 2012

Tímea Kiss ,
György Sipos ,
Barbara Mauz  and
Gábor Mezősi
Tímea Kiss*
Affiliation:
Department of Physical Geography and Geoinformatics, University of Szeged, 6722 Szeged, Egyetem u. 2-6, Hungary
György Sipos
Affiliation:
Department of Physical Geography and Geoinformatics, University of Szeged, 6722 Szeged, Egyetem u. 2-6, Hungary
Barbara Mauz
Affiliation:
Department of Geography, University of Liverpool, Liverpool L697ZT, UK
Gábor Mezősi
Affiliation:
Department of Physical Geography and Geoinformatics, University of Szeged, 6722 Szeged, Egyetem u. 2-6, Hungary
*
⁎Corresponding author. Fax: + 36 62 4544158. Email Address:[email protected], [email protected], [email protected], [email protected]
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Abstract

Almost 20% of the territory of Hungary is covered by stabilized dunes formed during the Pleistocene. With the climate amelioration during the early Holocene the aeolian activity ceased. However, various environmental and anthropogenic factors could have reactivated the aeolian processes. Today, there is an increasing climatic stress on the dune fields of the Carpathian Basin, which is coupled with inadequate land use. It is therefore necessary to determine the timing and circumstances of sand mobilization during the Holocene. The site of the present study is located in a dune–interdune system on the southern part of the Nyírség alluvial fan, where periods of Holocene aeolian activity and environmental change were investigated using palynological and sedimentological methods, optically stimulated luminescence and radiocarbon dating. The data achieved show climate-driven Boreal aeolian activity at approximately 8.2 ka, and also demonstrate for the first time that during the Atlantic Phase (6.4 and 5.3 ka), in spite of the relatively humid climate and dense vegetation, aeolian activity has taken place, induced probably by agricultural practices. Following Subboreal morphological stability, aeolian activity occurred several times in the Subatlantic Phase (2.4–2.2, 1.2–0.8 and 0.4–0.1 ka) as a result of vegetation changes and human activity.

Keywords

HoloceneAeolian activityHuman impactOSL datingPalynology
Type
Articles
Information
Quaternary Research , Volume 78 , Issue 3 , November 2012 , pp. 492 - 501
Copyright
University of Washington

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