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dc.contributor.authorStuiver, Minze
dc.contributor.authorReimer, Paula J.
dc.contributor.authorBard, Edouard
dc.contributor.authorBeck, J. Warren
dc.contributor.authorBurr, G. S.
dc.contributor.authorHughen, Konrad A.
dc.contributor.authorKromer, Bernd
dc.contributor.authorMcCormac, Gerry
dc.contributor.authorvan der Plicht, Johannes
dc.contributor.authorSpurk, Marco
dc.date.accessioned2021-02-11T21:32:23Z
dc.date.available2021-02-11T21:32:23Z
dc.date.issued1998-01-01
dc.identifier.citationStuiver, M., Reimer, P. J., Bard, E., Beck, J. W., Burr, G. S., Hughen, K. A., ... & Spurk, M. (1998). INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon, 40(3), 1041-1083.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200019123
dc.identifier.urihttp://hdl.handle.net/10150/654515
dc.descriptionINTCAL 98: Calibration Issue.
dc.description.abstractThe focus of this paper is the conversion of radiocarbon ages to calibrated (cal) ages for the interval 24,000-0 cal BP (Before Present, 0 cal BP = AD 1950), based upon a sample set of dendrochronologically dated tree rings, uranium-thorium dated corals, and varve-counted marine sediment. The 14C age-cal age information, produced by many laboratories, is converted to 14C profiles and calibration curves, for the atmosphere as well as the oceans. We discuss offsets in measured 14C ages and the errors therein, regional 14C age differences, tree-coral 14C age comparisons and the time dependence of marine reservoir ages, and evaluate decadal vs. Single-year 14C results. Changes in oceanic deepwater circulation, especially for the 16,000-11,000 cal BP interval, are reflected in the Δ14C values of INTCAL98.
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.subjectINTCAL98 Program
dc.subjectprograms
dc.subjectocean circulation
dc.subjectTh U
dc.subjectAnthozoa
dc.subjectCoelenterata
dc.subjectcalibration
dc.subjectmarine sediments
dc.subjecterrors
dc.subjectatmosphere
dc.subjecttree rings
dc.subjectPleistocene
dc.subjectsediments
dc.subjectCenozoic
dc.subjectQuaternary
dc.subjectC 14
dc.subjectcarbon
dc.subjectdates
dc.subjectisotopes
dc.subjectradioactive isotopes
dc.subjectInvertebrata
dc.subjectabsolute age
dc.titleINTCAL98 Radiocarbon Age Calibration, 24,000-0 cal BP
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.volume40
dc.source.issue3
dc.source.beginpage1041
dc.source.endpage1083
refterms.dateFOA2021-02-11T21:32:23Z


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