Show simple item record

dc.contributor.authorWang, N.
dc.contributor.authorShen, C. D.
dc.contributor.authorDing, P.
dc.contributor.authorYi, W. X.
dc.contributor.authorSun, W. D.
dc.contributor.authorLiu, K. X.
dc.contributor.authorDing, X. F.
dc.contributor.authorFu, D. P.
dc.contributor.authorYuan, J.
dc.contributor.authorYang, X. Y.
dc.contributor.authorZhou, L. P.
dc.date.accessioned2021-02-11T21:22:56Z
dc.date.available2021-02-11T21:22:56Z
dc.date.issued2010-01-01
dc.identifier.citationWang, N., Shen, C. D., Ding, P., Yi, W. X., Sun, W. D., Liu, K. X., ... & Zhou, L. P. (2010). Improved application of bomb carbon in teeth for forensic investigation. Radiocarbon, 52(2), 706-716.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200045720
dc.identifier.urihttp://hdl.handle.net/10150/654245
dc.descriptionFrom the 20th International Radiocarbon Conference held in Kona, Hawaii, USA, May 31-June 3, 2009.
dc.description.abstractWhile radiocarbon is widely applied in dating ancient samples, recent studies reveal that 14C concentrations in modern samples can also yield precise ages due to the atmospheric testing of thermonuclear devices between 1950 and 1963. 14C concentrations in both enamel and organic matter of 13 teeth from 2 areas in China were examined to evaluate and improve this method of forensic investigation. Choosing enamel near the cervix of the tooth can reduce the error caused by the difference between the sample formation time and whole enamel formation time because tooth enamel formations take a long time to complete. A proper regional data set will be helpful to get an accurate result when calculating the age of the sample (T1) by the CALIBomb program. By subtracting the enamel formation time (t), the birth date of an individual (T2) can be confirmed by enamel F14C from 2 teeth formed at different ages. Calculated enamel formation dates by 14C concentration are basically consistent with corresponding actual values, with a mean error of 1.9 yr for all results and 0.2 yr for the samples formed after AD 1960. This method is more effective for dating samples completed after AD 1960. We also found that 14C concentrations in organic matter of tooth roots are much lower than atmospheric concentrations in root formation years, suggesting that the organic material keeps turning over even after tooth formation is complete. This might be a potential tool for identification of death age to extract a proper component for 14C dating. We also observed that delta-13C values between hydroxyapatite and organic matter indicate that isotopic fractionation during the biomineralization is 8-9‰ more positive in mineral fractions than in organic matter.
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.titleImproved Application of Bomb Carbon in Teeth for Forensic Investigation
dc.typeProceedings
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.volume52
dc.source.issue2
dc.source.beginpage706
dc.source.endpage716
refterms.dateFOA2021-02-11T21:22:56Z


Files in this item

Thumbnail
Name:
3704-4078-1-PB.pdf
Size:
556.5Kb
Format:
PDF

This item appears in the following Collection(s)

Show simple item record