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dc.contributor.authorBruns, Michael
dc.contributor.authorMünnich, K. O.
dc.contributor.authorBecker, Bernd
dc.date.accessioned2021-02-11T19:31:27Z
dc.date.available2021-02-11T19:31:27Z
dc.date.issued1980-01-01
dc.identifier.citationBruns, M., Münnich, K. O., & Becker, B. (1980). Natural radiocarbon variations from AD 200 to 800. Radiocarbon, 22(2), 273-277.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200009553
dc.identifier.urihttp://hdl.handle.net/10150/652423
dc.description.abstractHigh precision radiocarbon measurements (+/- 2.5 per mil STD) were carried out on absolutely dated European oak material. These showed that significant shortterm atmospheric 14C variations of up to 2 percent occurred between AD 200 and 800. These changes, reflecting a 150-to 180-year periodicity, seem to correlate with the average sunspot activity around that time. In comparison with results obtained by other authors, a very regular pattern of natural atmospheric 14C variations is exhibited.
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.titleNatural Radiocarbon Variations from AD 200 to 800
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.beginpage273
dc.source.endpage277
refterms.dateFOA2021-02-11T19:31:27Z


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