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dc.contributor.authorBrewster, Ciarán
dc.contributor.authorMeiklejohn, Christopher
dc.contributor.authorvon Cramon-Taubadel, Noreen
dc.contributor.authorPinhasi, Ron
dc.date.accessioned2018-02-21T15:21:11Z
dc.date.available2018-02-21T15:21:11Z
dc.date.issued2014-06-10
dc.identifier.citationBrewster, C., C. Meiklejohn, N. von Cramon-Taubadel & R. Pinhasi, 2014. Craniometric analysis of European Upper Palaeolithic and Mesolithic samples supports discontinuity at the Last Glacial Maximum. Nature Communications 5:4094. DOI: 10.1038/ncomms5094.en_US
dc.identifier.issn2041-1723
dc.identifier.urihttp://hdl.handle.net/10680/1359
dc.description.abstractThe Last Glacial Maximum (LGM) represents the most significant climatic event since the emergence of anatomically modern humans (AMH). In Europe, the LGM may have played a role in changing morphological features as a result of adaptive and stochastic processes. We use craniometric data to examine morphological diversity in pre- and post-LGM specimens. Craniometric variation is assessed across four periods—pre-LGM, late glacial, Early Holocene and Middle Holocene—using a large, well-dated, data set. Our results show significant differences across the four periods, using a MANOVA on size-adjusted cranial measurements. A discriminant function analysis shows separation between pre-LGM and later groups. Analyses repeated on a subsample, controlled for time and location, yield similar results. The results are largely influenced by facial measurements and are most consistent with neutral demographic processes. These findings suggest that the LGM had a major impact on AMH populations in Europe prior to the Neolithic.en_US
dc.description.urihttps://www.nature.com/articles/ncomms5094
dc.language.isoenen_US
dc.publisherMacmillan Publishers Limiteden_US
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleCraniometric analysis of European Upper Palaeolithic and Mesolithic samples supports discontinuity at the Last Glacial Maximumen_US
dc.typeArticleen_US
dc.identifier.doi10.1038/ncomms5094


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