Radiocarbon to Calendar Date Conversion: Calendrical Bandwidths as a Function of Radiocarbon Precision
| dc.contributor.author | McCormac, F. G. | |
| dc.contributor.author | Baillie, M. G. L. | |
| dc.date.accessioned | 2021-02-11T20:33:44Z | |
| dc.date.available | 2021-02-11T20:33:44Z | |
| dc.date.issued | 1993-01-01 | |
| dc.identifier.citation | McCormac, F. G., & Baillie, M. G. L. (1993). Radiocarbon to calendar date conversion: Calendrical band widths as a function of radiocarbon precision. Radiocarbon, 35(2), 311-316. | |
| dc.identifier.issn | 0033-8222 | |
| dc.identifier.doi | 10.1017/S0033822200064997 | |
| dc.identifier.uri | http://hdl.handle.net/10150/653421 | |
| dc.description.abstract | Accurate high-precision 14C dating (i.e., +/- 20 yr precision or less on the 14C date) provides the narrowest calendrical band width and, hence, the best age range determination possible. However, because of the structure in the 14C calibration curve, the calendar age range for a given 14C precision is not constant throughout the calibration range. In this study, we quantify the calendar band widths for a range of 14C previsions throughout the calibration range. We show that an estimate of the likely calendar band width in years can be obtained from the expression: Band width (yr) = 2.12 x 14C precision (1 sigma) + 54.6. We also show that calendar band widths are widest around 4000 BP at the start of the Bronze Age, and become narrow through the later Bronze Age and Iron Age and back into the Neolithic. | |
| dc.language.iso | en | |
| dc.publisher | Department of Geosciences, The University of Arizona | |
| dc.relation.url | http://radiocarbon.webhost.uits.arizona.edu/ | |
| dc.rights | Copyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved. | |
| dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | |
| dc.subject | Neolithic | |
| dc.subject | Iron Age | |
| dc.subject | Stone Age | |
| dc.subject | computer programs | |
| dc.subject | precision | |
| dc.subject | calibration | |
| dc.subject | archaeology | |
| dc.subject | Bronze Age | |
| dc.subject | Holocene | |
| dc.subject | data processing | |
| dc.subject | Cenozoic | |
| dc.subject | Quaternary | |
| dc.subject | methods | |
| dc.subject | C 14 | |
| dc.subject | carbon | |
| dc.subject | isotopes | |
| dc.subject | radioactive isotopes | |
| dc.subject | absolute age | |
| dc.title | Radiocarbon to Calendar Date Conversion: Calendrical Bandwidths as a Function of Radiocarbon Precision | |
| dc.type | Article | |
| dc.type | text | |
| dc.identifier.journal | Radiocarbon | |
| dc.description.note | This material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries. | |
| dc.description.collectioninformation | The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information. | |
| dc.eprint.version | Final published version | |
| dc.description.admin-note | Migrated from OJS platform February 2021 | |
| dc.source.volume | 35 | |
| dc.source.issue | 2 | |
| dc.source.beginpage | 311 | |
| dc.source.endpage | 316 | |
| refterms.dateFOA | 2021-02-11T20:33:44Z |
