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dc.contributor.authorFraile, Igaratza-
dc.contributor.authorArrizabalaga, Haritz-
dc.contributor.authorRooker, Jay R.-
dc.date.accessioned2017-08-23T08:52:12Z-
dc.date.available2017-08-23T08:52:12Z-
dc.date.issued2015-
dc.identifierISI:000350154300028-
dc.identifier.citationICES JOURNAL OF MARINE SCIENCE, 2015, 72, 625-634-
dc.identifier.issn1054-3139-
dc.identifier.urihttp://dspace.azti.es/handle/24689/293-
dc.description.abstractWe used carbon and oxygen isotope ratios (delta C-13 and delta O-18) in otoliths as a tool for identifying the nursery origin of Atlantic bluefin tuna (Thunnus thynnus) caught in the eastern North Atlantic Ocean (Bay of Biscay). Juvenile and adult bluefin tuna were collected over three consecutive years (2009-2011) using the regional bait boat fleet. Otolith delta C-13 and delta O-18 values of bluefin tuna were measured by mass spectrometry, and values were compared with a reference sample of yearling bluefin tuna from eastern (Mediterranean Sea) and western (Gulf of Mexico) nurseries to determine nursery origin. Maximum likelihood estimates based on otolith delta C-13 and delta O-18 values indicated that the overall contribution of western migrants to the Bay of Biscay fishery was <1\% and varied over the years assessed. A small number of potential western migrants (2.7\%) was detected in 2009, and most of these fish appear members of the abundant 2002 and 2003 year classes. In contrast, the Bay of Biscay fishery was composed exclusively (100\%) of eastern origin bluefin tuna in 2010 and 2011, suggesting that this fishery is supported almost exclusively by the eastern spawning area but transatlantic western population may contribute to this fishery in a few years.-
dc.description.sponsorshipThe authors thank L. Naval and the staff from La Bacaladera for providing Atlantic bluefin tuna samples for this study. They are indebted to the crew from Attalaya Berria, Tukutuku, and Berriz Gure Naia vessels for their contribution on behalf of the bluefin tuna sampling programme. They thank the comments of two anonymous reviewers that improved the manuscript. This work was carried out under the provision of the ICCAT Atlantic Wide Research Program for Bluefin Tuna (GBYP), funded by the European Union, by several ICCAT CPCs, the ICCAT Secretariat and by other entities (see http://www.iccat.int/GBYP/en/Budget.htm). The contents of this paper do not necessarily reflect the point of view of ICCAT or of the other funders. This work was also supported by grant CTM2011-27505 by the Spanish Ministry of Economy and Competitiveness (MINECO), National Geographic Society (Grant W132-10), and the Basque Government (Grant 351BI20080022). This paper's contribution number is 666 from AZTI-Tecnalia (Marine Research).-
dc.language.isoeng-
dc.publisherOXFORD UNIV PRESS-
dc.subjectmixing rate-
dc.subjectotolith-
dc.subjectstable isotope-
dc.subjectThunnus thynnus-
dc.subjectCOD GADUS-MORHUA-
dc.subjectISOTOPIC COMPOSITION-
dc.subjectEASTERN ATLANTIC-
dc.subjectFISH OTOLITHS-
dc.subjectNATAL ORIGIN-
dc.subjectDELTA-C-13-
dc.subjectFRACTIONATION-
dc.subjectDELTA-O-18-
dc.subjectMOVEMENTS-
dc.subjectCHEMISTRY-
dc.titleOrigin of Atlantic bluefin tuna (Thunnus thynnus) in the Bay of Biscay-
dc.typeArticle-
dc.identifier.journalICES JOURNAL OF MARINE SCIENCE-
dc.format.page625-634-
dc.format.volume72-
dc.contributor.funderEuropean Union-
dc.contributor.funderICCAT CPC-
dc.contributor.funderICCAT Secretariat-
dc.contributor.funderSpanish Ministry of Economy and Competitiveness (MINECO) \[CTM2011-27505]-
dc.contributor.funderNational Geographic Society \[W132-10]-
dc.contributor.funderBasque Government \[351BI20080022]-
dc.identifier.e-issn1095-9289-
dc.identifier.doi10.1093/icesjms/fsu156-
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