1. The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
- Author
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Ronny Friedrich, Christopher Bronk Ramsey, Konrad A Hughen, William E. N. Austin, Frederick Reinig, E. Marian Scott, Alex Bayliss, Lukas Wacker, Alexandra Fogtmann-Schulz, Jesper V. Olsen, Bernd Kromer, Timothy J Heaton, Pieter Meiert Grootes, Martin Butzin, Paul G. Blackwell, Charlotte Pearson, Peter Köhler, Hai Cheng, Christian Turney, Florian Adolphi, Sturt W. Manning, Ron W Reimer, David Richards, Michael Friedrich, R. Lawrence Edwards, Fusa Miyake, Jonathan G. Palmer, Alan G. Hogg, Thomas P. Guilderson, Paula J. Reimer, Johannes van der Plicht, Minoru Sakamoto, Ulf Büntgen, Manuela Capano, Irka Hajdas, Raimund Muscheler, Sabrina G K Kudsk, John Southon, Sahra Talamo, Simon Fahrni, Adam Sookdeo, Edouard Bard, Chaire Evolution du climat et de l'océan, Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD), National Natural Science Foundation of China (NSFC)NSFC 41888101NSFC 41731174Ministry of Education, China - 111 ProjectD19002National Science Foundation (NSF)1702816Malcolm H. Wiener Foundation - German Science foundation Swiss National Science Foundation (SNSF)200021L_157187College de France Swedish Research CouncilEuropean Commission Knut & Alice Wallenberg Foundation Federal Ministry of Education & Research (BMBF) PalMod project 01LP1505BEuropean Research Council (ERC)803147-RESOLUTIONAustralian Research CouncilFL100100195DP170104665UKRI Natural Environment Research Council NE/M004619/1Leverhulme TrustRF-2019-140\9, Isotope Research, Collège de France - Chaire Evolution du climat et de l'océan, Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), ANR-17-CE01-0001,CARBOTRYDH,Etude à haute résolution du radiocarbone des séries d'anneaux d'arbres des Alpes du Sud pour le Dryas Récent et l'Holocène: Une fenêtre sur le passé pour comprendre les variations rapides du cycle du carbone et de l'activité solaire(2017), Paula J Reimer, William E N Austin, Edouard Bard, Alex Bayli, Paul G Blackwell, Christopher Bronk Ramsey, Martin Butzin, Hai Cheng, R Lawrence Edward, Michael Friedrich, Pieter M Groote, Thomas P Guilderson, Irka Hajda, Timothy J Heaton, Alan G Hogg, Konrad A Hughen, Bernd Kromer, Sturt W Manning, Raimund Muscheler, Jonathan G Palmer, Charlotte Pearson, Johannes van der Plicht, Ron W Reimer, David A Richard, E Marian Scott, John R Southon, Christian S M Turney, Lukas Wacker, Florian Adolphi, Ulf Büntgen, Manuela Capano, Simon M Fahrni, Alexandra Fogtmann-Schulz, Ronny Friedrich, Peter Köhler, Sabrina Kudsk, Fusa Miyake, Jesper Olsen, Frederick Reinig, Minoru Sakamoto, Adam Sookdeo, Sahra Talamo, NERC, University of St Andrews. Coastal Resources Management Group, University of St Andrews. School of Geography & Sustainable Development, University of St Andrews. Marine Alliance for Science & Technology Scotland, University of St Andrews. Scottish Oceans Institute, and University of St Andrews. St Andrews Sustainability Institute
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010506 paleontology ,Archeology ,Calibration curve ,01 natural sciences ,calibration curve radiocarbon IntCal20 ,law.invention ,Atmosphere ,law ,[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry ,calibration curve ,0601 history and archaeology ,Radiocarbon dating ,R2C ,Ocean circulation model ,0105 earth and related environmental sciences ,GE ,Extinction ,IntCal20 ,060102 archaeology ,Northern Hemisphere ,Paleontology ,3rd-DAS ,06 humanities and the arts ,Radiocarbon ,Earth system science ,0402 Geochemistry, 0406 Physical Geography and Environmental Geoscience, 2101 Archaeology ,radiocarbon ,General Earth and Planetary Sciences ,Physical geography ,BDC ,Geology ,GE Environmental Sciences - Abstract
Authors thank the National Natural Science Foundation of China grants NSFC 41888101 and NSFC 41731174, the 111 program of China (D19002), U.S. NSF Grant 1702816, and the Malcolm H. Wiener Foundation for support for research that contributed to the IntCal20 curve. The work on the Swiss and German YD trees was funded by the German Science foundation and the Swiss National Foundation (grant number: 200021L_157187). The operation in Aix-en-Provence is funded by the EQUIPEX ASTER-CEREGE, the Collège de France and the ANR project CARBOTRYDH (to EB). The work on the correlation of tree ring 14C with ice core 10Be was partially supported by the Swedish Research Council and the Knut and Alice Wallenberg foundation. M. Butzin is supported by the German Federal Ministry of Education and Research (BMBF) through the PalMod project (grant number: 01LP1505B). S. Talamo and M. Friedrich. are funded by the European Research Council under the European Union’s Horizon 2020 Research and Innovation Programme (grant agreement No. 803147-RESOLUTION, awarded to ST). C. Turney would like to acknowledge support of the Australian Research Council (FL100100195 and DP170104665). P. Reimer and W. Austin acknowledge the support of the UKRI Natural Environment Research Council (Grant NE/M004619/1). Radiocarbon (14C) ages cannot provide absolutely dated chronologies for archaeological or paleoenvironmental studies directly but must be converted to calendar age equivalents using a calibration curve compensating for fluctuations in atmospheric 14C concentration. Although calibration curves are constructed from independently dated archives, they invariably require revision as new data become available and our understanding of the Earth system improves. In this volume the international 14C calibration curves for both the Northern and Southern Hemispheres, as well as for the ocean surface layer, have been updated to include a wealth of new data and extended to 55,000 cal BP. Based on tree rings, IntCal20 now extends as a fully atmospheric record to ca. 13,900 cal BP. For the older part of the timescale, IntCal20 comprises statistically integrated evidence from floating tree-ring chronologies, lacustrine and marine sediments, speleothems, and corals. We utilized improved evaluation of the timescales and location variable 14C offsets from the atmosphere (reservoir age, dead carbon fraction) for each dataset. New statistical methods have refined the structure of the calibration curves while maintaining a robust treatment of uncertainties in the 14C ages, the calendar ages and other corrections. The inclusion of modeled marine reservoir ages derived from a three-dimensional ocean circulation model has allowed us to apply more appropriate reservoir corrections to the marine 14C data rather than the previous use of constant regional offsets from the atmosphere. Here we provide an overview of the new and revised datasets and the associated methods used for the construction of the IntCal20 curve and explore potential regional offsets for tree-ring data. We discuss the main differences with respect to the previous calibration curve, IntCal13, and some of the implications for archaeology and geosciences ranging from the recent past to the time of the extinction of the Neanderthals. Publisher PDF
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- 2020
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