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dc.contributor.authorKulakovska, Larissa
dc.contributor.authorKononenko, Olesia
dc.contributor.authorHaesaerts, Paul
dc.contributor.authorPirson, Stéphane
dc.contributor.authorSpry-Marques, P.
dc.contributor.authorBosch, M.D.
dc.contributor.authorPopova, L.
dc.contributor.authorPopiuk, Yana
dc.contributor.authorDamblon, Freddy
dc.contributor.authorUsik, Vitaly
dc.contributor.authorNigst, Philip R
dc.date.accessioned2021-11-22T12:29:18Z
dc.date.available2021-11-22T12:29:18Z
dc.date.issued2021
dc.identifier.issn1040-6182
dc.identifier.urihttps://archer.chnu.edu.ua/xmlui/handle/123456789/2149
dc.description.abstractKorman’ 9 is a newly discovered Upper Palaeolithic site in the Middle Dniester valley (Ukraine). Here we present chronostratigraphic, palaeoenvironmental, chronological, lithic and faunal data. Within a ~4 m deep sequence we have identified four Archaeological Layers (AL 0 to III) and AL I can be attributed to the Epigravettian, AL II most probably to the Epigravettian (small sample size), and AL III most probably to the Gravettian. AL 0 is too small to allow a cultural attribution. Lithic analysis for AL I shows microblade technology and a toolkit dominated by microliths (backed and marginally retouched microblades and bladelets). Faunal analysis demonstrates that exploitation focuses on reindeer and horse. The archaeological results fit well into the regional Upper Palaeolithic record, and the correlations with sites like Molodova V, Korman’ IV, Cosautsi, and Dorochivsti III are well established. Our results allow us to conclude that humans were present at Korman’ 9 during the Last Glacial Maximum under arctic (AL II and AL III) and sub-arctic (AL I) conditions. We also discuss implications for our findings for the discussion of human presence/absence during cold and arid conditions around the Last Glacial Maximum.uk_UA
dc.description.sponsorshipThe feldwork and analysis were funded by the following grants to P.R. Nigst: EC FP7 Marie Curie Career Integration Grant no. 322261 (NEMO-ADAP Project), Leakey Foundation General Grant (spring 2012 granting cycle), D.M. McDonald Grants and Awards Fund grant, Isaac Newton Trust Small Grant, Isaac Newton Trust Matching Funding Grant, British Academy/ Leverhulme Trust Small Grant, and funds of the Max-Planck-Society. MDB was supported by an EC H2020 Marie Sklodovska Curie IntraEuropean Fellowship (grant no. 656325, EU-BEADS project)uk_UA
dc.language.isoenuk_UA
dc.publisherQuarternary Internationaluk_UA
dc.relation.ispartofseries587-588;230-250
dc.subjectUpper Palaeolithicuk_UA
dc.subjectLate Pleistoceneuk_UA
dc.subjectEpigravettianuk_UA
dc.subjectUkraineuk_UA
dc.subjectDniesteruk_UA
dc.subjectLast Glacial Maximumuk_UA
dc.titleKorman` 9: A new Upper Palaeolithic site in the Middle Dniester valley, Ukraineuk_UA
dc.typeArticleuk_UA


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