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dc.contributor.authorZaitseva, G. I.
dc.contributor.authorvan Geel, B.
dc.contributor.authorBokovenko, N. A.
dc.contributor.authorChugunov, K. V.
dc.contributor.authorDergahev, V. A.
dc.contributor.authorDirksen, V. G.
dc.contributor.authorKoulkova, M. A.
dc.contributor.authorNagler, A.
dc.contributor.authorParzinger, G.
dc.contributor.authorvan der Plicht, J.
dc.contributor.authorBourova, N. D.
dc.contributor.authorLebedeva, L. M.
dc.date.accessioned2021-02-11T21:45:26Z
dc.date.available2021-02-11T21:45:26Z
dc.date.issued2004-01-01
dc.identifier.citationZaitseva, G. I., van Geel, B., Bokovenko, N. A., Chugunov, K. V., Dergachev, V. A., Dirksen, V. G., ... & Lebedeva, L. M. (2004). Chronology and possible links between climatic and cultural change during the first millennium BC in southern Siberia and Central Asia. Radiocarbon, 46(1), 259-276.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200039576
dc.identifier.urihttp://hdl.handle.net/10150/654756
dc.descriptionFrom the 18th International Radiocarbon Conference held in Wellington, New Zealand, September 1-5, 2003.
dc.description.abstractWe reconstructed climate change during the second half of the Holocene for the Minusinsk (southern Siberia) and the Uyuk (Central Asia) valleys in the Eurasian steppe zone. Sediment cores from 2 lakes and a soil profile from the Arzhan-2 burial mount were investigated. We combined pollen and geochemical analyses and radiocarbon dating with the archaeological record. A sharp increase of human population density occurred at the transition from the Bronze Age to Iron Age (about 2700 cal BP). The most representative Scythian culture started in the Uyuk and the Minusinsk valleys after increased humidity and occupation capacity of the steppe zone during the 9th century BC.
dc.language.isoen
dc.publisherDepartment of Geosciences, The University of Arizona
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectabsolute age
dc.subjectarchaeology
dc.subjectArzhan 2 burial mound
dc.subjectAsia
dc.subjectBronze Age
dc.subjectC 14
dc.subjectcarbon
dc.subjectCenozoic
dc.subjectCentral Asia
dc.subjectclimate change
dc.subjectcores
dc.subjectgeochemistry
dc.subjectHolocene
dc.subjecthuman activity
dc.subjecthumidity
dc.subjectIron Age
dc.subjectisotopes
dc.subjectKutuzhekovo Lake
dc.subjectlacustrine environment
dc.subjectlake sediments
dc.subjectmicrofossils
dc.subjectMinusinsk Valley
dc.subjectmiospores
dc.subjectNeolithic
dc.subjectpalynomorphs
dc.subjectpollen
dc.subjectpollen diagrams
dc.subjectQuaternary
dc.subjectradioactive isotopes
dc.subjectsediments
dc.subjectSiberia
dc.subjectsoil profiles
dc.subjectsouthern Siberia
dc.subjectsteppes
dc.subjectStone Age
dc.subjectUyuk Valley
dc.titleChronology and Possible Links between Climatic and Cultural Change During the First Millennium BC in Southern Siberia and Central Asia
dc.typeProceedings
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume46
dc.source.issue1
dc.source.beginpage259
dc.source.endpage276
refterms.dateFOA2021-02-11T21:45:26Z


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