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dc.contributor.authorScherer, Sascha
dc.contributor.authorHöpfer, Benjamin
dc.contributor.authorDeckers, Katleen
dc.contributor.authorFischer, Elske
dc.contributor.authorFuchs, Markus
dc.contributor.authorKandeler, Ellen
dc.contributor.authorLechterbeck, Jutta
dc.contributor.authorLehndorff, Eva
dc.contributor.authorLomax, Johanna
dc.contributor.authorMarhan, Sven
dc.contributor.authorMarinova, Elena
dc.contributor.authorMeister, Julia
dc.contributor.authorPoll, Christian
dc.contributor.authorRahimova, Humay
dc.contributor.authorRösch, Manfred
dc.contributor.authorWroth, Kirsten
dc.contributor.authorZastrow, Julia
dc.contributor.authorKnopf, Thomas
dc.contributor.authorScholten, Thomas
dc.contributor.authorKühn, Peter
dc.coverage.spatialTysklanden_US
dc.date.accessioned2021-07-06T14:26:32Z
dc.date.available2021-07-06T14:26:32Z
dc.date.created2021-01-11T09:37:02Z
dc.date.issued2021-06
dc.identifier.citationScherer, S., Höpfer, B., Deckers, K. et al. (2021) Middle Bronze Age land use practices in the northwestern Alpine foreland – A multi-proxy study of colluvial deposits, archaeological features and peat bogs. Soil, 7, 269-304.en_US
dc.identifier.issn2199-3971
dc.identifier.urihttps://hdl.handle.net/11250/2763621
dc.description.abstractThis paper aims to reconstruct Middle Bronze Age (MBA; 1600–1250 BCE) land use practices in the northwestern Alpine foreland (SW Germany, Hegau). We used a multi-proxy approach including the analysis of biogeochemical proxies from colluvial deposits and buried topsoils in the surroundings of the well-documented settlement site of Anselfingen and off-site pollen data from two peat bogs. This approach allowed for in-depth insights into the MBA subsistence economy and shows that the MBA in the northwestern Alpine foreland was a period of establishing settlements with sophisticated land management and land use practices. The reconstruction of phases of colluvial deposition was based on ages from optically stimulated luminescence (OSL) and radiocarbon (AMS14C) dating from multi-layered colluvial deposits and supports the local archaeological record with the first phase of major colluvial deposition occurring during the MBA followed by phases of colluvial deposition during the Iron Age, the Medieval period and modern times. The on-site deposition of charred archaeobotanical remains and animal bones from archaeological features, as well as polycyclic aromatic hydrocarbons (PAHs), charcoal spectra, phytoliths, soil microstructure, urease enzymatic activity, microbial biomass carbon (Cmic) and heavy metal contents from colluvial deposits, were used as proxies for on-site and near-site land use practices. The charcoal spectra indicate MBA forest management which favored the dominance of Quercus in the woodland vegetation in the surrounding area north of the settlement site. Increased levels of 5β stanols (up to 40 %) and the occurrence of pig bones (up to 14 %) support the presence of a forest pasture mainly used for pig farming. In the surrounding area south of the settlement, an arable field with a buried MBA plow horizon (2Apb) could be verified by soil micromorphological investigations and high concentrations of grass phytoliths from leaves and stems. Agricultural practices (e.g., plowing) focussed on five staple crops (Hordeum distichon/vulgare, Triticum dicoccum, Triticum monococcum, Triticum spelta, Triticum aestivum/turgidum), while the presence of stilted pantries as storage facilities and of heat stones indicate post-harvest processing of cereal crops and other agrarian products within the settlement. In the area surrounding the settlement, increased levels of urease activity, compared to microbial biomass carbon (up to 2.1 µg N µg C−1mic), and input of herbivorous and omnivorous animal faeces indicate livestock husbandry on fallow land. The PAH suites and their spatial distribution support the use of fire for various purposes, e.g., for opening and maintaining the landscape, for domestic burning and for technical applications. The off-site palynological data support the observed change in on-site and near-site vegetation as well as the occurrence of related land use practices. During the Early and Middle Bronze Age, fire played a major role in shaping the landscape (peak of micro-charcoal during the MBA), and anthropogenic activities promoted Quercus-dominated forest ecosystems at the expense of natural beech forests. This indicates a broader regional human influence in the northwestern Alpine foreland at low- and mid-altitude inland sites during the Middle Bronze Age.en_US
dc.language.isoengen_US
dc.publisherCopernicus Publicationsen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectarkeologien_US
dc.subjectbronsealderenen_US
dc.subjecttorvmyren_US
dc.titleMiddle Bronze Age land use practices in the northwestern Alpine foreland – A multi-proxy study of colluvial deposits, archaeological features and peat bogsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© Author(s) 2021.en_US
dc.subject.nsiVDP::Humaniora: 000::Arkeologi: 090en_US
dc.source.pagenumber269-304en_US
dc.source.volume7en_US
dc.source.journalSOILen_US
dc.identifier.doi10.5194/soil-7-269-2021
dc.identifier.cristin1868587
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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