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dc.contributor.authorScott, E. M.
dc.contributor.authorReimer, P. J.
dc.date.accessioned2021-02-11T21:22:35Z
dc.date.available2021-02-11T21:22:35Z
dc.date.issued2009-01-01
dc.identifier.citationScott, E. M., & Reimer, P. J. (2009). Calibration introduction. Radiocarbon, 51(1), 283-285.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200033816
dc.identifier.urihttp://hdl.handle.net/10150/654164
dc.description.abstractThere are 2 fundamental assumptions in radiocarbon dating, which were known early in the method development to be approximations, and which lead directly to the need to calibrate 14C dates: 1. The rate of formation of 14C in the upper atmosphere has been constant over the entire applied 14C dating timescale (approximately the last 65,000 yr). 2. The 14C activity of the atmosphere has been in equilibrium with the biosphere and ocean over the applied timescale.
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.titleCalibration Introduction
dc.typeArticle
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.volume51
dc.source.issue1
dc.source.beginpage283
dc.source.endpage285
refterms.dateFOA2021-02-11T21:22:35Z


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