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Marine Radiocarbon Reservoir Effect in Late Pleistocene and Early Holocene Coastal Waters off Northern Iberia

Published online by Cambridge University Press:  30 August 2016

António M Monge Soares ,
Igor Gutiérrez-Zugasti ,
Manuel González-Morales ,
José M Matos Martins ,
David Cuenca-Solana  and
Geoffrey N Bailey
António M Monge Soares*
Affiliation:
Campus Tecnológico e Nuclear, Instituto Superior Técnico, Universidade de Lisboa, Estrada Nacional 10, 2695-066 Bobadela LRS, Portugal
Igor Gutiérrez-Zugasti
Affiliation:
Instituto Internacional de Investigaciones Prehistóricas de Cantabria, Universidad de Cantabria, Ed. Interfacultativo, Avda. de los Castros s/n, 39005 Santander, Cantabria, Spain
Manuel González-Morales
Affiliation:
Instituto Internacional de Investigaciones Prehistóricas de Cantabria, Universidad de Cantabria, Ed. Interfacultativo, Avda. de los Castros s/n, 39005 Santander, Cantabria, Spain
José M Matos Martins
Affiliation:
Campus Tecnológico e Nuclear, Instituto Superior Técnico, Universidade de Lisboa, Estrada Nacional 10, 2695-066 Bobadela LRS, Portugal
David Cuenca-Solana
Affiliation:
Instituto Internacional de Investigaciones Prehistóricas de Cantabria, Universidad de Cantabria, Ed. Interfacultativo, Avda. de los Castros s/n, 39005 Santander, Cantabria, Spain
Geoffrey N Bailey
Affiliation:
Department of Archaeology, University of York, King’s Manor YO1 7EP, York, UK
*
*Corresponding author. Email: amsoares@ctn.tecnico.ulisboa.pt.
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Abstract

Radiocarbon dating of closely associated marine mollusk shells and terrestrial material (mammal bones or charred wood) collected from archaeological contexts in northern Atlantic Iberian coastal areas is used to quantify the marine 14C reservoir effect (ΔR) for the coastal waters off the Cantabrian coast of northern Iberia. For the first time, ΔR values were reliably determined for these coastal waters and, also for the first time, a ΔR was calculated for the Late Pleistocene in Atlantic Iberia. Pairs of coeval samples of different carbon reservoirs selected from Upper Paleolithic (Late Pleistocene) and Mesolithic (Early Holocene) contexts yielded ΔR weighted mean values of –117±70 14C yr and –105±21 14C yr, respectively. These values show oceanographic conditions characterized by a reduced offset between atmospheric and surface water 14C contents, suggesting a nonexistent or very weak upwelling and some stratification of the water column. Similar oceanographic conditions have been recorded in other areas of Atlantic Iberia during the Holocene, such as off Andalusian and northwestern Galician coasts. Results not only provide useful information on environmental conditions but also a framework to obtain more precise and reliable absolute chronologies for the Late Pleistocene and Early Holocene in northern Iberia.

Keywords

marine 14C reservoir effectCantabrian coastLate PleistoceneEarly Holocene
Type
Research Article
Information
Radiocarbon , Volume 58 , Issue 4 , December 2016 , pp. 869 - 883
Copyright
© 2016 by the Arizona Board of Regents on behalf of the University of Arizona 

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