{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,5]],"date-time":"2025-10-05T12:19:44Z","timestamp":1759666784903},"reference-count":37,"publisher":"Cambridge University Press (CUP)","issue":"3-4","license":[{"start":{"date-parts":[[2016,7,18]],"date-time":"2016-07-18T00:00:00Z","timestamp":1468800000000},"content-version":"unspecified","delay-in-days":1660,"URL":"https:\/\/www.cambridge.org\/core\/terms"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Radiocarbon"],"published-print":{"date-parts":[[2012]]},"abstract":"<jats:p>Radiocarbon dating of closely associated marine mollusk shells and terrestrial material (charred wood or bone) collected from archaeological contexts on Tenerife and Fuerteventura islands allowed us to quantify the marine <jats:sup>14<\/jats:sup>C reservoir effect (\u0394R) around the Canary Archipelago. Coastal Fuerteventura has a positive weighted mean \u0394R value of +185 \u00b1 30 <jats:sup>14<\/jats:sup>C yr, while for Tenerife a range of negative and positive values was obtained, resulting in a \u0394R weighted mean value of 0 \u00b1 35 <jats:sup>14<\/jats:sup>C yr. These values are in accordance with the hydrodynamic system present off the Canary Islands characterized by a coastal upwelling regime that affects the eastern islands (Fuerteventura and Lanzarote) but not the other islands of the archipelago, namely Tenerife. Because of this oceanographic pattern, we recommend the extrapolation of these results to the remaining islands of the archipelago, i.e. the first value must be used for the eastern islands, while for the central and western islands the acceptable \u0394R value is 0 \u00b1 35 <jats:sup>14<\/jats:sup>C yr.<\/jats:p>","DOI":"10.1017\/s0033822200047585","type":"journal-article","created":{"date-parts":[[2016,7,20]],"date-time":"2016-07-20T01:17:04Z","timestamp":1468977424000},"page":"943-952","source":"Crossref","is-referenced-by-count":4,"title":["Improving the <sup>14<\/sup>C Dating of Marine Shells from the Canary Islands for Constructing More Reliable and Accurate Chronologies"],"prefix":"10.1017","volume":"54","author":[{"given":"Jos\u00e9 M Matos","family":"Martins","sequence":"first","affiliation":[]},{"given":"Alfredo Mederos","family":"Mart\u00edn","sequence":"additional","affiliation":[]},{"given":"Paulo J Ces\u00e1rio","family":"Portela","sequence":"additional","affiliation":[]},{"given":"Ant\u00f3nio M Monge","family":"Soares","sequence":"additional","affiliation":[]}],"member":"56","published-online":{"date-parts":[[2016,7,18]]},"reference":[{"key":"S0033822200047585_ref35","doi-asserted-by":"publisher","DOI":"10.1017\/S0033822200003672"},{"key":"S0033822200047585_ref36","doi-asserted-by":"publisher","DOI":"10.1017\/S0033822200060264"},{"key":"S0033822200047585_ref25","doi-asserted-by":"crossref","DOI":"10.22498\/pages.14.3.12","article-title":"Marine reservoir corrections and the calibration curve","volume":"14","author":"Reimer","year":"2006","journal-title":"PAGES News"},{"key":"S0033822200047585_ref14","unstructured":"L\u00e1iz I , Sangr\u00e0 P , Pelegr\u00ed JL . 2000. Variabilidad estacional del borde oriental del Giro Subtropical del Atl\u00e1ntico Norte. 3\u00b0 Simp\u00f3sio sobre a Margem Ib\u00e9rica Atl\u00e2ntica:159\u201360."},{"key":"S0033822200047585_ref32","volume-title":"Actas del VIII Congreso Ib\u00e9rico de Arqueometr\u00eda","author":"Soares","year":"2010"},{"key":"S0033822200047585_ref12","unstructured":"Hern\u00e1ndez P\u00e9rez MS . 2002. El Julan (La Frontera, El Hierro, Islas Canarias). Direcci\u00f3n General de Patrimonio Hist\u00f3rico. Gobierno de Canarias. 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The variability of the marine radiocarbon reservoir effect in southern Iberian coast. 4th IGCP 526 meeting \u201cRisks, Resources, and Record of the Past on the Continental Shelves\u201d, Vigo, Spain, 28 September\u20131 October. 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Actas del V Congreso Panafricano de prehistoria y de Estudios del Cuarternario II (Santa Cruz de Tenerife) (6):43\u201352."},{"key":"S0033822200047585_ref29","doi-asserted-by":"publisher","DOI":"10.1017\/S0033822200035384"}],"container-title":["Radiocarbon"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/www.cambridge.org\/core\/services\/aop-cambridge-core\/content\/view\/S0033822200047585","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2019,4,26]],"date-time":"2019-04-26T15:31:26Z","timestamp":1556292686000},"score":1,"resource":{"primary":{"URL":"https:\/\/www.cambridge.org\/core\/product\/identifier\/S0033822200047585\/type\/journal_article"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2012]]},"references-count":37,"journal-issue":{"issue":"3-4","published-print":{"date-parts":[[2012]]}},"alternative-id":["S0033822200047585"],"URL":"https:\/\/doi.org\/10.1017\/s0033822200047585","relation":{},"ISSN":["0033-8222","1945-5755"],"issn-type":[{"value":"0033-8222","type":"print"},{"value":"1945-5755","type":"electronic"}],"subject":[],"published":{"date-parts":[[2012]]}}}