{"refrec":{"BRefID":238563,"RR":"<b>Lopez Correa, M.; Montagna, P.; Joseph, N.; Rüggeberg, A.; Fietzke, J.; Flogel, S.; Dorschel, B.; Goldstein, S.L.; Wheeler, A.; Freiwald, A.</b> (2012). Preboreal onset of cold-water coral growth beyond the Arctic Circle revealed by coupled radiocarbon and U-series dating and neodymium isotopes. <i>Quat. Sci. Rev. 34</i>: 24-43. <a href=\"http://dx.doi.org/10.1016/j.quascirev.2011.12.005\" target=\"_blank\">dx.doi.org/10.1016/j.quascirev.2011.12.005</a>","BEntID":230250,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Quat. Sci. Rev. 34</i>: 24-43. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2011.12.005\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2011.12.005</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lopez Correa, M.; Montagna, P.; Joseph, N.; Rüggeberg, A.; Fietzke, J.; Flogel, S.; Dorschel, B.; Goldstein, S.L.; Wheeler, A.; Freiwald, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lopez Correa, M. <i>et al.</i>","Englishabstract":"Cold-water coral mounds of <em>Lophelia pertusa</em> are widespread across the Scandinavian shelf, which was completely ice-covered during the Last Glacial Maximum between 22 to 18 ka BP. Rapid deglacial meltdown of the Fennoscandian inland ice and the retreat of its ice-streams freed most of the shelf of ice by ~15 ka BP. However, cold-water coral growth commenced only after the Pleistocene–Holocene transition at 11.65 ka BP, when modern-like climatic patterns and oceanographic conditions were established. A tight climatic coupling has been constrained with U-series ages. Coupled <sup>14</sup>C ages provide local reservoir ages from various gravity cores in a fjord-setting in Stjernsund at 70°N and on the open shelf in Trænadjupet at 66°N. Reinvestigation of earlier <sup>14</sup>C coral chronologies suggests that coral ecosystems widely established themselves across the entire 3000 km long Scandinavian shelf prior to ~10 ka BP. The earliest occurrence of <em>Madrepora oculata</em> at ~2.4 ka BP suggests a late Holocene colonization of the Norwegian shelf, which is linked to a prominent mound growth hiatus in Trænadjupet (64°N). Mound growth rates near the northern biogeographic boundary of <em>L. pertusa</em> with up to ~614 cm ka<sup>-1</sup> during certain growth periods are much higher than the previously reported fastest rates of ~220 cm ka<sup>-1</sup> from the Irish margin. Contemporaneous rapid fjordbasin sedimentation is slower with ~63 cm ka<sup>-1</sup>. Matrix <sup>14</sup>C ages overlap with coral <sup>14</sup>C ages from the same horizon. This indicates rapid framework construction and efficient trapping of background sediment. Hiatuses are frequent in on-mound sediments and only short periods of coral growth are recorded. Coupled ?<sup>14</sup>C and <em>e</em><sub>Nd</sub> values indicate a persistent Holocene inflow of the North Atlantic Current in Stjernsund, but also deglacial meltwater mixing during the early Holocene prior to ~9.5 ka BP. Reservoir ages are overall close to the surface marine reservoir age, but ?<em>R</em> is highly localized.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Preboreal onset of cold-water coral growth beyond the Arctic Circle revealed by coupled radiocarbon and U-series dating and neodymium isotopes","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":"Cold-water corals; Reservoir ages; Biogeography; Rapid climate change;Younger Dryas; Deglacial; Water mass mixing","OtherDescriptors":null,"Notes":null,"AnaPub":2012,"MonPub":null,"DateUpdate":"2015-10-29","DateCreate":"2014-05-18","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000301826100003","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.quascirev.2011.12.005"},"refs":null,"anarec":{"AnaID":238563,"PubliDate":2012,"Pagination":"24-43","XtraPublOfAnaID":null,"ISBN":null,"Volume":"34","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45667,"SerRR":"Quaternary Science Reviews. Pergamon Press: Oxford; New York.  ISSN 0277-3791; e-ISSN 1873-457X","StandardTitleSer":"Quaternary Science Reviews","ISSN":"0277-3791","AbbrevSer":"Quat. Sci. 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