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dc.contributor.authorDe Jong, A. F. M.
dc.contributor.authorMook, W. G.
dc.date.accessioned2021-02-11T19:31:24Z
dc.date.available2021-02-11T19:31:24Z
dc.date.issued1980-01-01
dc.identifier.citationDe Jong, A. F. M., & Mook, W. G. (1980). Medium-term atmospheric 14C variations. Radiocarbon, 22(2), 267-272.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200009541
dc.identifier.urihttp://hdl.handle.net/10150/652411
dc.description.abstractHigh-precision 14C measurements are presented, carried out on single tree rings from a section of the floating South German Neolithic tree-ring chronology. They confirm the existence of pronounced medium-term variations in the order of 2 percent during the 33rd to 38th centuries BC. These variations turn out to be very regular while the precision of 1.5 per mil allows a comparison with a geochemical model calculation. Good agreement is acquired for an input function with a periodicity of about 150 years and an amplitude of approximately 30 percent in the 14C production rate.
dc.language.isoen
dc.publisherAmerican Journal of Science
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © The American Journal of Science
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.titleMedium-Term Atmospheric 14C Variations
dc.typeArticle
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.noteThis material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries.
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.volume22
dc.source.issue2
dc.source.beginpage267
dc.source.endpage272
refterms.dateFOA2021-02-11T19:31:24Z


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