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dc.contributor.authorHeaton, Timothy J.
dc.contributor.authorKöhler, Peter
dc.contributor.authorButzin, Martin
dc.contributor.authorBard, Edouard
dc.contributor.authorReimer, Ron W.
dc.contributor.authorAustin, William
dc.contributor.authorRamsey, Christpher Bronk
dc.contributor.authorGrootes, Pieter M.
dc.contributor.authorHughen, Konrad A.
dc.contributor.authorKromer, Bernd
dc.contributor.authorAdkins, Jess
dc.contributor.authorBurke, Andrea
dc.contributor.authorCook, Mea S.
dc.contributor.authorOlsen, Jesper
dc.contributor.authorSkinner, Luke C.
dc.date.accessioned2020-08-14T08:30:02Z
dc.date.available2020-08-14T08:30:02Z
dc.date.issued2020-08-31
dc.identifier.citationHeaton , T J , Köhler , P , Butzin , M , Bard , E , Reimer , R W , Austin , W , Ramsey , C B , Grootes , P M , Hughen , K A , Kromer , B , Adkins , J , Burke , A , Cook , M S , Olsen , J & Skinner , L C 2020 , ' Marine20—the marine radiocarbon age calibration curve (0 – 55,000 cal BP) ' , Radiocarbon , vol. 62 , no. 4 , pp. 779-820 . https://doi.org/10.1017/RDC.2020.68en
dc.identifier.issn0033-8222
dc.identifier.otherPURE: 268761891
dc.identifier.otherPURE UUID: 0fa562ae-8918-471e-8383-868edf516a14
dc.identifier.otherRIS: urn:226E9255FB2E74974B1CF567A7BD5F1C
dc.identifier.otherORCID: /0000-0002-3754-1498/work/78891783
dc.identifier.otherScopus: 85088614410
dc.identifier.otherWOS: 000588638500003
dc.identifier.urihttp://hdl.handle.net/10023/20464
dc.descriptionT.J. Heaton is supported by a Leverhulme Trust Fellowship RF-2019-140\9, “Improving the Measurement of Time Using Radiocarbon”. M Butzin is supported by the German Federal Ministry of Education and Research (BMBF), as Research for Sustainability initiative (FONA); www.fona.de through the PalMod project (grant numbers: 01LP1505B, 01LP1919A). E. Bard is supported by EQUIPEX ASTER-CEREGE and ANR CARBOTRYDH. Meetings of the IntCal Marine Focus group have been supported by Collège de France.en
dc.description.abstractThe concentration of radiocarbon (14C) differs between ocean and atmosphere. Radiocarbon determinations from samples which obtained their 14C in the marine environment therefore need a marine-specific calibration curve and cannot be calibrated directly against the atmospheric-based IntCal20 curve. This paper presents Marine20, an update to the internationally agreed marine radiocarbon age calibration curve that provides a non-polar global-average marine record of radiocarbon from 0–55 cal kBP and serves as a baseline for regional oceanic variation. Marine20 is intended for calibration of marine radiocarbon samples from non-polar regions; it is not suitable for calibration in polar regions where variability in sea ice extent, ocean upwelling and air-sea gas exchange may have caused larger changes to concentrations of marine radiocarbon. The Marine20 curve is based upon 500 simulations with an ocean/atmosphere/biosphere box-model of the global carbon cycle that has been forced by posterior realizations of our Northern Hemispheric atmospheric IntCal20 14C curve and reconstructed changes in CO2 obtained from ice core data. These forcings enable us to incorporate carbon cycle dynamics and temporal changes in the atmospheric 14C level. The box-model simulations of the global-average marine radiocarbon reservoir age are similar to those of a more complex three-dimensional ocean general circulation model. However, simplicity and speed of the box model allow us to use a Monte Carlo approach to rigorously propagate the uncertainty in both the historic concentration of atmospheric 14C and other key parameters of the carbon cycle through to our final Marine20 calibration curve. This robust propagation of uncertainty is fundamental to providing reliable precision for the radiocarbon age calibration of marine based samples. We make a first step towards deconvolving the contributions of different processes to the total uncertainty; discuss the main differences of Marine20 from the previous age calibration curve Marine13; and identify the limitations of our approach together with key areas for further work. The updated values for ΔR, the regional marine radiocarbon reservoir age corrections required to calibrate against Marine20, can be found at the data base http://calib.org/marine/.
dc.format.extent42
dc.language.isoeng
dc.relation.ispartofRadiocarbonen
dc.rightsCopyright © 2020 by the Arizona Board of Regents on behalf of the University of Arizona. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.en
dc.subjectBayesian modelingen
dc.subjectCalibrationen
dc.subjectCarbon cycleen
dc.subjectComputer modelen
dc.subjectMarine environmenten
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subjectBDCen
dc.subjectR2Cen
dc.subject.lccGEen
dc.titleMarine20—the marine radiocarbon age calibration curve (0 – 55,000 cal BP)en
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.School of Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews.Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews.St Andrews Sustainability Instituteen
dc.contributor.institutionUniversity of St Andrews.Coastal Resources Management Groupen
dc.contributor.institutionUniversity of St Andrews.Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews.School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.St Andrews Isotope Geochemistryen
dc.identifier.doihttps://doi.org/10.1017/RDC.2020.68
dc.description.statusPeer revieweden
dc.date.embargoedUntil2020-08-12


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