Take a seed! Revealing Neolithic landscape and agricultural development in the Carpathian Basin through multivariate statistics and environmental modelling
Titel: | Take a seed! Revealing Neolithic landscape and agricultural development in the Carpathian Basin through multivariate statistics and environmental modelling |
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Verfasser: | |
Veröffentlicht: | Freiburg : Universität, 2024 |
Umfang: | 1 Online-Ressource |
Format: | E-Book |
Sprache: | Englisch |
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Revealing Neolithic landscape and agricultural development in the Carpathian Basin through multivariate statistics and environmental modelling 028A $BVerfasser $4aut $8Kempf, Michael [Tp3] $9468457135 033A $pFreiburg $nUniversität 034D $a1 Online-Ressource 037A $aPLOS ONE. - 16, 10 (2021) , e0258206, ISSN: 1932-6203 037I $uhttp://vocabularies.coar-repositories.org/access_rights/c_abf2 $fUnrestricted online access 037J $aOpen Access $2star $uhttp://purl.org/coar/access_right/c_abf2 $fUnrestricted online access 045E $c930 046X $aArchivierung/Langzeitarchivierung gewährleistet $5DE-101 047I $aAbstract: The Carpathian Basin represents the cradle of human agricultural development during the Neolithic period, when large parts were transformed into ‘cultural landscapes’ by first farmers from the Balkans. It is assumed that an Early Neolithic subsistence economy established along the hydrologic systems and on Chernozem soil patches, which developed from loess deposits. However, recent results from soil chemistry and geoarchaeological analyses raised the hypothesis that extensive Chernozem coverage developed from increased land-use activity and that Early Neolithic ‘cultural’ groups were not restricted to loess-covered surfaces but rather preferred hydromorphic soils that formed in the floodplains. This article performs multivariable statistics from large datasets of Neolithic sites in Hungary and allows tracing Early to Late Neolithic site preferences from digital environmental data. Quantitative analyses reveal a strong preference for hydromorphic soils, a significant avoidance of loess-covered areas, and no preference for Chernozem soils throughout the Early Neolithic followed by a strong transformation of site preferences during the Late Neolithic period. 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