{"refrec":{"BRefID":122434,"RR":"<b>Frank, N.; Paterne, M.; Ayliffe, L.; van Weering, T.; Henriet, J.P.; Blamart, D.</b> (2004). Eastern North Atlantic deep-sea corals: tracing upper intermediate water d<sup>14</sup>C during the Holocene. <i>Earth Planet. Sci. Lett. 219(3-4)</i>: 297-309. <a href=\"http://dx.doi.org/10.1016/S0012-821X(03)00721-0\" target=\"_blank\">dx.doi.org/10.1016/S0012-821X(03)00721-0</a>","BEntID":116504,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Earth Planet. Sci. Lett. 219(3-4)</i>: 297-309. <a href=\"https://dx.doi.org/10.1016/S0012-821X(03)00721-0\" target=\"_blank\">https://dx.doi.org/10.1016/S0012-821X(03)00721-0</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Frank, N.; Paterne, M.; Ayliffe, L.; van Weering, T.; Henriet, J.P.; Blamart, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Frank, N. <i>et al.</i>","Englishabstract":"Paired <sup>230</sup>Th/U and <sup>14</sup>C dating were performed on deep-sea corals (<i>Lophelia pertusa</i> and <i>Madrepora oculata</i>) from the northeastern North Atlantic at <img src=\"http://www.sciencedirect.com/scidirimg/entities/223c.gif\" alt=\"not, vert, similar\" title=\"not, vert, similar\" border=\"0\">730 m bsl to investigate past changes of the thermohaline circulation. These were estimated using the ?<sup>14</sup>C value of the upper intermediate waters, based on the <sup>14</sup>C ages of the top and base of each coral, where possible, and the <sup>230</sup>Th/U dating. The reliability of these estimates was checked by dating two very young corals of the species <i>L. pertusa</i>. One of these corals, collected alive in 1999 AD, gave a <sup>230</sup>Th/U age of 1995±4 AD after correction for non-radiogenic <sup>230</sup>Th. Another coral, the top of which dated to 1969±6 AD, recorded the atmospheric <sup>14</sup>C/<sup>12</sup>C increase due to the nuclear tests in the early 1960s. The calculated ?<sup>14</sup>C values from these two corals agree with those measured at GEOSECS Station 23 in 1972–1973 [Östlund et al., Earth Planet. Sci. Lett. 23 (1974) 69–86] and 1991–1992 [Nydal and Gisfelos, Radiocarbon 38 (1996) 389–406]. This, together with the 100% aragonite content and the d<sup>234</sup>U and <sup>230</sup>Th/<sup>232</sup>Th values of all the dated corals, indicates that none of the corals behaved as open systems with respect to their U-series nuclides and that they closely represent the water mass properties in which they lived. The pre-anthropogenic ?<sup>14</sup>C value of the North Atlantic intermediate waters was estimated at -69±4‰. The reservoir age varies from <img src=\"http://www.sciencedirect.com/scidirimg/entities/223c.gif\" alt=\"not, vert, similar\" title=\"not, vert, similar\" border=\"0\">400 years to <img src=\"http://www.sciencedirect.com/scidirimg/entities/223c.gif\" alt=\"not, vert, similar\" title=\"not, vert, similar\" border=\"0\">600 years, and this variation is due to atmospheric <sup>14</sup>C/<sup>12</sup>C changes. A reservoir age of 610±80 years, close to the pre-anthropogenic value, was determined from one coral dated at 10 430±120 cal yr BP, when the global sea level was approximately at -35 m [Bard et al., Nature 382 (1996) 241–244]. This suggests a modern-like pattern of the oceanic circulation prevailed in the Northeast Atlantic Ocean at this time although the deglaciation was not completely achieved.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Eastern North Atlantic deep-sea corals: tracing upper intermediate water d<sup>14</sup>C during the Holocene","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"deep-sea corals; Northeast Atlantic; <sup>230</sup>Th; U dating; radiocarbon dating; reservoir age","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2013-06-21","DateCreate":"2008-05-20","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000220146500010","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/S0012-821X(03)00721-0"},"refs":null,"anarec":{"AnaID":122434,"PubliDate":2004,"Pagination":"297-309","XtraPublOfAnaID":null,"ISBN":null,"Volume":"219","Issue":"3-4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42615,"SerRR":"Earth and Planetary Science Letters. Elsevier: Amsterdam.  ISSN 0012-821X; e-ISSN 1385-013X","StandardTitleSer":"Earth and Planetary Science Letters","ISSN":"0012-821X","AbbrevSer":"Earth Planet. Sci. 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