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Geol. 188(1-2)</i>: 79-108. <a href=\"https://dx.doi.org/10.1016/S0025-3227(02)00276-1\" target=\"_blank\">https://dx.doi.org/10.1016/S0025-3227(02)00276-1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Auffret, G.; Zaragosi, S.; Dennielou, B.; Cortijo, E.; Van Rooij, D.; Grousset, F.; Pujol, C.; Eynaud, F.; Siegert, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Auffret, G. <i>et al.</i>","Englishabstract":"The sedimentary sections of three cores from the Celtic margin provide high-resolution records of the terrigenous fluxes during the last glacial cycle. A total of 21 <sup>14</sup>C AMS dates allow us to define age models with a resolution better than 100 yr during critical periods such as Heinrich events 1 and 2. Maximum sedimentary fluxes occurred at the Meriadzek Terrace site during the Last Glacial Maximum (LGM). 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The high-resolution records of Heinrich events 1 and 2 show that in both cases the arrival of the Canadian icebergs was preceded by a European ice rafting precursor event, which took place about 1-1.5 kyr before. Two rafting episodes of European IRD also occurred immediately after Heinrich event 2 and just before Heinrich event 1. The terrigenous fluxes recorded in core MD95-2002 during the LGM are the highest reported at hemipelagic sites from the northwestern European margin. The magnitude of the Canadian IRD fluxes at Meriadzek Terrace is similar to those from oceanic sites. 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