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dc.contributor.authorGarcía Escárzaga, Asier
dc.contributor.authorGutiérrez Zugasti, Fernando Igor 
dc.contributor.authorCuenca Solana, David 
dc.contributor.authorGonzález Morales, Manuel R. 
dc.contributor.authorHamann, Christian
dc.contributor.authorRoberts, Patrick
dc.contributor.authorFernandes, Ricardo
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2023-03-07T13:31:56Z
dc.date.available2023-03-07T13:31:56Z
dc.date.issued2022
dc.identifier.issn1871-1014
dc.identifier.issn1878-0350
dc.identifier.otherHAR 2016-75605-Res_ES
dc.identifier.otherHAR 2017-86262-Pes_ES
dc.identifier.urihttps://hdl.handle.net/10902/28039
dc.description.abstractReconstructing the past variability of marine radiocarbon reservoir effects (MRE) is crucial for generating reliable chronologies for marine species and their consumers. We investigated the temporal MRE variability at the Early-to Mid-Holocene site of El Mazo (Asturias, northern Spain) by using a combination of new and previously published radiocarbon measurements on marine and terrestrial samples. The El Mazo site is characterized by overall well-defined archaeological layers of unknown occupation length with the predominant presence of two mollusc species (Patella vulgata Linnaeus, 1758 and topshell Phorcus lineatus [da Costa, 1778]) which were analysed for radiocarbon measurements. We employed the recently released IntCal20 calibration curve for the northern hemisphere and Bayesian modelling to reconstruct the site?s chronology and temporal variability in MREs according to mollusc species. Obtained radiocarbon modelling results, although the estimate precision is not high, reveal a temporal variability in MREs that can be interpreted in view of known past climatic and environmental events such as the 8.2 ka event. The results also revealed differences in MREs according to mollusc species, which need to be taken into account in future chronological modelling. Overall, our results provide reference MRE values for the study of chronologies in northern Iberia during the Early-to Mid-Holocene. In this respect, a non-conservative ?R reference for local marine samples dating earlier than c. 8.1 ka cal BP is - 238 ± 28 14C years.es_ES
dc.description.sponsorshipThis research was performed as part of the projects HAR 2016- 75605-R and HAR 2017-86262-P, funded by the Spanish Ministry of Economy and Competitiveness, MINECO. During the development of this research AGE was funded by the Basque Country Postdoctoral Programme through a postdoctoral grant (POS_2020_2_0032) and University of La Rioja (no code available). This study has also been supported by the Prehistoric Research Consolidated Group of the Basque Country University (IT-1223-19), funded by the Basque Country Government. PR and RF are funded by the Max Planck Society. We thank the Fishing Activity Service of the Cantabrian Government for the authorization to collect modern specimens. We also thank the Max Plank Society, University of La Rioja, Basque Country University (UPV/EHU), University of Cantabria (UC) and Instituto Internacional de Investigaciones Prehist´oricas de Cantabria (IIIPC) for providing support.es_ES
dc.format.extent13 p.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rights© 2021 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND licensees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceQuaternary Geochronology, 2022, 67, 101232es_ES
dc.subject.otherMesolithices_ES
dc.subject.otherShell middenses_ES
dc.subject.otherCantabrian regiones_ES
dc.subject.otherMarine radiocarbon reservoir effectes_ES
dc.subject.otherBayesian modellinges_ES
dc.subject.otherMarine environmentses_ES
dc.subject.other8.2 ka eventes_ES
dc.titleBayesian estimates of marine radiocarbon reservoir effect in northern Iberia during the Early and Middle Holocenees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1016/j.quageo.2021.101232es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1016/j.quageo.2021.101232
dc.type.versionpublishedVersiones_ES


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© 2021 The Authors. Published by Elsevier B.V.  This is an open access article under the CC BY-NC-ND licenseExcepto si se señala otra cosa, la licencia del ítem se describe como © 2021 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license