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      Direct dating reveals the early history of opium poppy in western Europe

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          Abstract

          This paper aims to define the first chrono-cultural framework on the domestication and early diffusion of the opium poppy using small-sized botanical remains from archaeological sites, opening the way to directly date minute short-lived botanical samples. We produced the initial set of radiocarbon dates directly from the opium poppy remains of eleven Neolithic sites (5900–3500 cal BCE) in the central and western Mediterranean, northwestern temperate Europe, and the western Alps. When possible, we also dated the macrobotanical remains originating from the same sediment sample. In total, 22 samples were taken into account, including 12 dates directly obtained from opium poppy remains. The radiocarbon chronology ranges from 5622 to 4050 cal BCE. The results show that opium poppy is present from at least the middle of the sixth millennium in the Mediterranean, where it possibly grew naturally and was cultivated by pioneer Neolithic communities. Its dispersal outside of its native area was early, being found west of the Rhine in 5300–5200 cal BCE. It was introduced to the western Alps around 5000–4800 cal BCE, becoming widespread from the second half of the fifth millennium. This research evidences different rhythms in the introduction of opium poppy in western Europe.

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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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              Recent and Planned Developments of the Program OxCal

              OxCal is a widely used software package for the calibration of radiocarbon dates and the statistical analysis of 14C and other chronological information. The program aims to make statistical methods easily available to researchers and students working in a range of different disciplines. This paper will look at the recent and planned developments of the package. The recent additions to the statistical methods are primarily aimed at providing more robust models, in particular through model averaging for deposition models and through different multiphase models. The paper will look at how these new models have been implemented and explore the implications for researchers who might benefit from their use. In addition, a new approach to the evaluation of marine reservoir offsets will be presented. As the quantity and complexity of chronological data increase, it is also important to have efficient methods for the visualization of such extensive data sets and methods for the presentation of spatial and geographical data embedded within planned future versions of OxCal will also be discussed.
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                Author and article information

                Contributors
                salavert@mnhn.fr
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                20 November 2020
                20 November 2020
                2020
                : 10
                : 20263
                Affiliations
                [1 ]GRID grid.462844.8, ISNI 0000 0001 2308 1657, Unité Mixte de Recherche (UMR) Archéozoologie, Archéobotanique: Sociétés, Pratiques et Environnements, Muséum National d’Histoire Naturelle (MNHN), Centre National de Recherche Scientifique (CNRS), , Alliance Sorbonne Université, ; Paris, France
                [2 ]GRID grid.8591.5, ISNI 0000 0001 2322 4988, Laboratory of Prehistoric Archaeology and Anthropology, , University of Geneva, ; Geneva, Switzerland
                [3 ]GRID grid.5388.6, UMR EDYTEM, CNRS, Université Grenoble Alpes, , Université Savoie Mont-Blanc, ; Chambéry, France
                [4 ]GRID grid.6612.3, ISNI 0000 0004 1937 0642, Integrative Prehistory and Archaeological Science (IPAS), , Universität Basel, ; Basel, Switzerland
                [5 ]GRID grid.12832.3a, ISNI 0000 0001 2323 0229, Laboratoire des Sciences du Climat et de l’Environnement (LSCE), CNRS, Commissariat à l’Energie Atomique (CEA), , Université de Versailles Saint-Quentin, Paris-Saclay, ; Paris, France
                [6 ]GRID grid.503191.f, ISNI 0000 0001 0143 5055, UMR Histoire Naturelle de L’Homme Préhistorique, Musée de L’Homme, MNHN, ; Paris, France
                [7 ]GRID grid.462058.d, ISNI 0000 0001 2188 7059, ISEM, Univ Montpellier, CNRS, EPHE, IRD, ; Montpellier, France
                [8 ]GRID grid.508721.9, UMR TRACES, CNRS, , Université Toulouse Jean Jaurès, ; Toulouse, France
                [9 ]Museo delle Civiltà - Museo Preistorico Etnografico “Luigi Pigorini”, Rome, Italy
                [10 ]GRID grid.413454.3, ISNI 0000 0001 1958 0162, W. Szafer Institute of Botany, , Polish Academy of Sciences, ; Kraków, Poland
                [11 ]GRID grid.7080.f, Departament de Prehistòria, , Universitat Autònoma de Barcelona, ; Bellaterra, Spain
                [12 ]GRID grid.11696.39, ISNI 0000 0004 1937 0351, Laboratorio Di Archeobiologia Dei Musei Civici Di Como, Department of Humanities, , Università Degli Studi Di Trento, ; Trento, Italy
                [13 ]GRID grid.440910.8, ISNI 0000 0001 2196 152X, UMR Archéologie Des Sociétés Méditerranéennes, , Université Paul-Valéry Montpellier 3, CNRS, Ministère de La Culture Et de La Communication, Inrap/LabEx Archimède, ; Montpellier, France
                [14 ]GRID grid.10979.36, ISNI 0000 0001 1245 3953, Faculty of Arts, , Palacký University Olomouc, ; Olomouc, Czech Republic
                Article
                76924
                10.1038/s41598-020-76924-3
                7679390
                33219318
                ceed03b5-63ac-4f97-8bca-1d0436c747cc
                © The Author(s) 2020

                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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 11 August 2020
                : 2 November 2020
                Funding
                Funded by: FundRef http://dx.doi.org/10.13039/501100003135, Fondation Fyssen;
                Funded by: FundRef http://dx.doi.org/10.13039/501100001711, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung;
                Award ID: PP00P1_170515
                Award Recipient :
                Categories
                Article
                Custom metadata
                © The Author(s) 2020

                Uncategorized
                plant domestication,biogeochemistry
                Uncategorized
                plant domestication, biogeochemistry

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