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      Evidence for European presence in the Americas in ad 1021

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          Abstract

          Transatlantic exploration took place centuries before the crossing of Columbus. Physical evidence for early European presence in the Americas can be found in Newfoundland, Canada 1, 2 . However, it has thus far not been possible to determine when this activity took place 35 . Here we provide evidence that the Vikings were present in Newfoundland in ad 1021. We overcome the imprecision of previous age estimates by making use of the cosmic-ray-induced upsurge in atmospheric radiocarbon concentrations in ad 993 (ref.  6 ). Our new date lays down a marker for European cognisance of the Americas, and represents the first known point at which humans encircled the globe. It also provides a definitive tie point for future research into the initial consequences of transatlantic activity, such as the transference of knowledge, and the potential exchange of genetic information, biota and pathologies 7, 8 .

          Abstract

          Precise dating of wooden artefacts at a Norse settlement in Newfoundland establishes that the Norse were in the Americas in ad 1021.

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          THE INTCAL20 NORTHERN HEMISPHERE RADIOCARBON AGE CALIBRATION CURVE (0–55 CAL kBP)

          Radiocarbon ( 14 C) 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 14 C 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 14 C 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 14 C 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 14 C 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 14 C 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.
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            Bayesian Analysis of Radiocarbon Dates

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              Discussion Reporting of 14C Data

              Count rates, representing the rate of 14C decay, are the basic data obtained in a 14C laboratory. The conversion of this information into an age or geochemical parameters appears a simple matter at first. However, the path between counting and suitable 14C data reporting (table 1) causes headaches to many. Minor deflections in pathway, depending on personal interpretations, are possible and give end results that are not always useful for inter-laboratory comparisons. This discussion is an attempt to identify some of these problems and to recommend certain procedures by which reporting ambiguities can be avoided.
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                Author and article information

                Contributors
                m.kuitems@rug.nl
                m.w.dee@rug.nl
                Journal
                Nature
                Nature
                Nature
                Nature Publishing Group UK (London )
                0028-0836
                1476-4687
                20 October 2021
                20 October 2021
                2022
                : 601
                : 7893
                : 388-391
                Affiliations
                [1 ]GRID grid.4830.f, ISNI 0000 0004 0407 1981, Centre for Isotope Research, , University of Groningen, ; Groningen, the Netherlands
                [2 ]GRID grid.451254.3, ISNI 0000 0004 0377 1994, Parks Canada Agency, Government of Canada, ; Dartmouth, Nova Scotia Canada
                [3 ]Laboratory for Dendrochronology at BAAC, ’s-Hertogenbosch, the Netherlands
                [4 ]GRID grid.425697.b, ISNI 0000 0001 0701 3603, Cultural Heritage Agency of The Netherlands, ; Amersfoort, the Netherlands
                [5 ]Curt-Engelhorn-Center Archaeometry, Mannheim, Germany
                [6 ]GRID grid.25055.37, ISNI 0000 0000 9130 6822, Department of Archaeology, Queens College, , Memorial University of Newfoundland, ; St Johns, Newfoundland Canada
                [7 ]GRID grid.25055.37, ISNI 0000 0000 9130 6822, Department of Geography, , Memorial University of Newfoundland, ; St Johns, Newfoundland Canada
                [8 ]BIAX Consult, Zaandam, the Netherlands
                Author information
                http://orcid.org/0000-0002-8803-2650
                http://orcid.org/0000-0002-7174-3966
                http://orcid.org/0000-0002-8322-2068
                http://orcid.org/0000-0001-5363-2755
                http://orcid.org/0000-0001-7463-6034
                http://orcid.org/0000-0002-1302-7603
                http://orcid.org/0000-0001-5199-1957
                http://orcid.org/0000-0002-3116-453X
                Article
                3972
                10.1038/s41586-021-03972-8
                8770119
                34671168
                6c8efc9e-fda9-481a-9c91-b2d2b06bf791
                © The Author(s) 2021

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 21 May 2021
                : 31 August 2021
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                © The Author(s), under exclusive licence to Springer Nature Limited 2022

                Uncategorized
                archaeology,plant physiology,mass spectrometry
                Uncategorized
                archaeology, plant physiology, mass spectrometry

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