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dc.contributor.authorLewis, Simon G.-
dc.contributor.authorAshton, Nick-
dc.contributor.authorField, Michael H.-
dc.contributor.authorHoare, Peter G. ‎-
dc.contributor.authorKamermans, Hans-
dc.contributor.authorKnul, Monika V.-
dc.contributor.authorMücher, Herman Jozef‏-
dc.contributor.authorParfitt, Simon A.-
dc.contributor.authorRoebroeks, Wil-
dc.contributor.authorSier, Mark Jan-
dc.date.accessioned2019-03-21T14:17:24Z-
dc.date.issued2019-05-
dc.identifier.citationQuaternary Science Reviews, 2019, 211, 34-58es_ES
dc.identifier.issn0277-3791-
dc.identifier.issn1873-457X-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/1153-
dc.description.abstractThe timing, environmental setting and archaeological signatures of an early human presence in northern Europe have been longstanding themes of Palaeolithic research. In the space of 20 years, the earliest record of human occupation in Britain has been pushed back from 500 ka (Boxgrove) to 700 ka (Pakefield) and then to >800 ka (Happisburgh Site 3). Other sites also contribute to this record of human occupation; a second locality at Happisburgh, referred to as Site 1, attests to human presence at around 500 ka (MIS 13). This paper provides the first comprehensive account of research undertaken at Happisburgh Site 1 since 2000. The early human landscape and depositional environment was that of a river floodplain, where an active river channel, in which a grey sand was deposited, was abandoned, forming a floodplain lake, with marginal marsh/swamp environments, which was infilled with organic mud. This succession is sealed by Middle Pleistocene glacial deposits. An assemblage of 199 flint flakes, flake tools and cores was recovered from the grey sand and organic mud. The evidence from Happisburgh Site 1 is placed in the context of the wider British and European MIS 13 record. The growing evidence for a significant dispersal of humans into northern Europe around 500 ka raises critical questions concerning the environmental conditions under which this took place. We also consider the evolutionary and behavioural changes in human populations that might have enabled the more widespread and persistent period of human presence in northern Europe at this time.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/embargoedAccesses_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectPleistocenees_ES
dc.subjectEuropees_ES
dc.subjectLower Palaeolithices_ES
dc.subjectHandaxees_ES
dc.subjectMIS 13es_ES
dc.subjectCromer forest-bed formationes_ES
dc.titleHuman occupation of Northern Europe in MIS 13: Happisburgh Site 1 (Norfolk, UK) and its european contextes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quascirev.2019.02.028-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quascirev.2019.02.028es_ES
dc.date.available2019-03-21T14:17:24Z-
Aparece en las colecciones: Geocronología y Geología



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