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Earthen mounds in the Głubczyce Forest (SW Poland) – are they prehistoric long-barrows? Geoarchaeology of the Silesian soil record and human-environment interplay in the Holocene

Bibliographic Data

ID7535293
AuthorsMateusz Krupski (0000-0001-7992-967X, Wrocław University of Environmental and Life Sciences, corresponding author), Maksym Mackiewicz (0000-0003-2509-4739, Archeolodzy.org Foundation Bolesława Prusa 81/3i, 50-316 Wrocław, Poland; Polish Centre of Mediterranean Archaeology, University of Warsaw, Prosta 69, 00-838 Warszawa Warszawa Poland), Cezary Kabala (0000-0001-9796-3716, Institute of Soil Science and Environmental Protection Wrocław University of Environmental and Life Sciences, Grunwaldzka 53, 50-357 Wrocław Wrocław Poland), Maciej Ehlert (0000-0001-9690-6971, Archeolodzy.org Foundation Bolesława Prusa 81/3i, 50-316 Wrocław Wrocław Poland), Marzena Cendrowska (0000-0002-6140-555X, Archeolodzy.org Foundation Bolesława Prusa 81/3i, 50-316 Wrocław Wrocław Poland)
Year2021
Volume96
Issue2
Pages413-433
Publication date2021-02-05
Peer ReviewedYes
Open AccessNo
TypeARTICLE
VenuePraehistorische Zeitschrift (JOURNAL)
Journal identifiersISSN: 0079-4848 • E-ISSN: 1613-0804
PublisherDe Gruyter (PUBLISHER • DE)
DOI10.1515/pz-2021-0004
OpenAlexW3129752430
LanguageEN
Citations received4

Two earthen mounds, trapezoid in shape, oriented along the W-E/NW-SE axis and located in prominent landscape positions, were recently discovered in the Głubczyce Forest in the loess area of the Głubczyce Plateau (SW Poland). Their resemblance to long-barrows of the Funnel Beaker culture, as yet unknown in this part of Silesia prompted low-invasive research, involving ALS data analysis, magnetic prospection and a study of soil properties. The objective was to determine if these are indeed anthropogenic structures and if so, how and when were they built. The results indicate: 1) a transformation from chernozemic (Phaeozem) to clay-illuvial soil (Luvisol/Retisol) in the Głubczyce Forest area. Similar processes were identified in neighbouring Central European loess regions and linked with prehistoric climate/vegetation changes (the spread of dense, beech-dominant forests). Human management of the landscape (involving sustained deforestation), enabled the patchy preservation of chernozemic soils until the present-day, 2) both mounds are anthropogenic features, built on a Phaeozem using chernozemic soil. Their construction occurred before the soil transformation, i.e. most likely in prehistory. The development of the Głubczyce Forest may have taken place during the Migration period – a time of settlement decline in Silesia, and 3) the Głubczyce Forest bears further traces of anthropogenic activity: ancient agriculture (field systems), funerary practices, forest management and WWII combat

Archaeology · Beech · Deforestation (computer science · Geoarchaeology · Geography · Geomorphology · Holocene · Loess · Period (music · Physical geography · Prehistory · Vegetation (pathology · Ancient and Medieval Archaeology Studies · Forestry · Geology · Historical and Archaeological Studies · Marine and environmental studies

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Unique citing works4
Citations per year1,33
Citation span2023 - 2025 (3)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 4
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