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dc.contributor.authorTurney, Chris M.
dc.contributor.authorHarkness, Douglas D.
dc.contributor.authorLowe, J. J.
dc.date.accessioned2021-02-11T21:32:04Z
dc.date.available2021-02-11T21:32:04Z
dc.date.issued1998-01-01
dc.identifier.citationTurney, C. S., Harkness, D. D., & Lowe, J. J. (1998). Carbon isotope variations and chronology of the last glacial-interglacial transition (14–9 ka BP). Radiocarbon, 40(2), 873-881.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200018841
dc.identifier.urihttp://hdl.handle.net/10150/654457
dc.descriptionFrom the 16th International Radiocarbon Conference held in Gronigen, Netherlands, June 16-20, 1997.
dc.description.abstractWe present delta-13C data from both bulk organic sediment samples and terrestrial plant macrofossils from five high-resolution sedimentary sequences from the United Kingdom from which extensive multiproxy data sets have been obtained. These span the last glacial-interglacial transition. Chronological control has been provided by radiocarbon dating and/or tephrochronology. The results demonstrate that significant shifts in bulk organic delta-13C can be identified at key climatic transitions in most of the sites. The data are affected by site-specific influences that restrict their use as chronological markers. However, terrestrial plant macrofossil records are more consistent and reveal shifts that appear to be synchronous and which therefore offer a basis for interregional correlation as well as significant paleoenvironmental information.
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.subjectinterglacial environment
dc.subjectBorrobol Basin
dc.subjectGransmoor England
dc.subjectLlanilid Wales
dc.subjectWhitrig Bog
dc.subjectWales
dc.subjecttephrochronology
dc.subjectpaleoenvironment
dc.subjectcarbon cycle
dc.subjectgeochemical cycle
dc.subjectaccelerator mass spectra
dc.subjectclimate change
dc.subjectcores
dc.subjectEngland
dc.subjectmass spectra
dc.subjectspectra
dc.subjectisotope ratios
dc.subjectGreat Britain
dc.subjectUnited Kingdom
dc.subjectScotland
dc.subjectHolocene
dc.subjectPlantae
dc.subjectigneous rocks
dc.subjectpyroclastics
dc.subjectvolcanic rocks
dc.subjectpaleoclimatology
dc.subjectPleistocene
dc.subjectorganic compounds
dc.subjectglaciation
dc.subjectEurope
dc.subjectWestern Europe
dc.subjectsediments
dc.subjectCenozoic
dc.subjectQuaternary
dc.subjectC 14
dc.subjectcarbon
dc.subjectdates
dc.subjectisotopes
dc.subjectradioactive isotopes
dc.subjectC 13 C 12
dc.subjectstable isotopes
dc.subjectabsolute age
dc.titleCarbon Isotope Variations and Chronology of the Last Glacial-Interglacial Transition (14-9 ka BP)
dc.typeProceedings
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.issue2
dc.source.beginpage873
dc.source.endpage881
refterms.dateFOA2021-02-11T21:32:04Z


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