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dc.contributor.authorBondevik, Stein
dc.contributor.authorLødøen, Trond
dc.contributor.authorTøssebro, Christine
dc.contributor.authorÅrskog, Hanne Bente
dc.contributor.authorHjelle, Kari Loe
dc.contributor.authorMehl, Ingvild Kristine
dc.coverage.spatialNorway, Western Norwaynb_NO
dc.date.accessioned2019-08-19T11:38:08Z
dc.date.available2019-08-19T11:38:08Z
dc.date.created2019-08-06T11:22:59Z
dc.date.issued2019
dc.identifier.citationBondevik, S., Lødøen, T. K., Tøssebro, C., Årskog, H., Hjelle, K. L., & Mehl, I. K. (2019). Between winter storm surges – Human occupation on a growing Mid-Holocene transgression maximum (Tapes) beach ridge at Longva, Western Norway. Quaternary Science Reviews, 215, 116-131.nb_NO
dc.identifier.issn0277-3791
dc.identifier.urihttp://hdl.handle.net/11250/2609079
dc.description.abstractSubstantial amounts of archaeological material have been found intermixed with beach pebbles and cobbles on the Tapes beach ridge at Longva on the island Flemsøya/Skuløya in Western Norway. The artefacts show that the beach ridge was settled in the Late Mesolithic. The most significant remains are fireplaces, birch bark from the floor of a tent/hut, fish sinkers and middens containing numerous waste flakes and lithic tools. Radiocarbon dating, mainly of burnt hazelnut shells, shows two periods of occupation. The older and longer period is dated to between 7600 and 6800 cal yr BP, and the younger phase to between 6200 and 5900 cal yr BP. Pollen analysis revealed open vegetation at the beach ridge during the occupation periods. Based on the beach ridge deposits and radiocarbon dates, we reconstructed the Tapes transgression maximum high tide sea level to 8.2–9.0 m between 7600 and 5600 cal yr BP. We conclude that the late Mesolithic inhabitants at Longva occupied the beach ridge while it was growing. During the largest storm surges – most likely to have been in the winter months – the sea would have washed over their settlements and deposited pebbles and cobbles on top of their remains. We suggest that the inhabitants abandoned the settlement before each stormy season, but returned and restored the site the following spring or summer.nb_NO
dc.language.isoengnb_NO
dc.publisherElseviernb_NO
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.subjectgeomorphologynb_NO
dc.subjectcoastalnb_NO
dc.subjectholocenenb_NO
dc.subjectlate mesolithic occupationnb_NO
dc.subjectmid-holocene transgressionnb_NO
dc.subjectScandinavianb_NO
dc.subjectstorm surgesnb_NO
dc.subjectsea level changesnb_NO
dc.subjectTapes transgressionnb_NO
dc.subjectWestern Norwaynb_NO
dc.titleBetween winter storm surges - Human occupation on a growing Mid-Holocene transgression maximum (Tapes) beach ridge at Longva, Western Norwaynb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionpublishedVersionnb_NO
dc.rights.holder© 2019 The Authors.nb_NO
dc.subject.nsiVDP::Humaniora: 000::Arkeologi: 090::Nordisk arkeologi: 091nb_NO
dc.source.pagenumber116-131nb_NO
dc.source.volume215nb_NO
dc.source.journalQuaternary Science Reviewsnb_NO
dc.identifier.doi10.1016/j.quascirev.2019.05.006
dc.identifier.cristin1714280
cristin.unitcode203,12,7,0
cristin.unitnameInstitutt for miljø- og naturvitskap
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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