{"refrec":{"BRefID":211548,"RR":"<b>Frank, N.; Freiwald, A.; López Correa, M.; Wienberg, C.; Eisele, M.; Hebbeln, D.; Van Rooij, D.; Henriet, J.-P.; Colin, C.; van Weering, T.; de Haas, H.; Buhl-Mortensen, P.; Murray Roberts, J.; De Mol, B.; Douville, E.; Blamart, D.; Hatté, C.</b> (2011). Northeastern Atlantic cold-water coral reefs and climate. <i>Geology (Boulder Colo.) 39(8)</i>: 743-746. <a href=\"http://dx.doi.org/10.1130/G31825.1\" target=\"_blank\">dx.doi.org/10.1130/G31825.1</a>","BEntID":203469,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geology (Boulder Colo.) 39(8)</i>: 743-746. <a href=\"https://dx.doi.org/10.1130/G31825.1\" target=\"_blank\">https://dx.doi.org/10.1130/G31825.1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Frank, N.; Freiwald, A.; López Correa, M.; Wienberg, C.; Eisele, M.; Hebbeln, D.; Van Rooij, D.; Henriet, J.-P.; Colin, C.; van Weering, T.; de Haas, H.; Buhl-Mortensen, P.; Murray Roberts, J.; De Mol, B.; Douville, E.; Blamart, D.; Hatté, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Frank, N. <i>et al.</i>","Englishabstract":"U-series age patterns obtained on reef framework–forming cold-water corals collected over a nearly 6000-km-long continental margin sector, extending from off Mauritania (17°N; northwest Africa) to the southwestern Barents Sea (70°N; northeastern Europe), reveal strong climate influences on the geographical distribution and sustained development of these ecosystems. Over the past three glacial-interglacial cycles, framework-forming cold-water corals (<i>Lophelia pertusa</i> and <i>Madrepora oculata</i>) seem to have predominantly populated reefs, canyons, and patches in the temperate East Atlantic and the Mediterranean Sea. Above 50°N corals colonize reefs in the northern East Atlantic primarily during warm climate periods with the biogeographic limit advancing from ~50°N to ~70°N. We propose that north-south oscillations of the biogeographic limit of reef developments are paced by ice ages and may occur synchronously with north-south displacement of cold nutrient-rich intermediate waters and surface productivity related to changes of the polar front.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Northeastern Atlantic cold-water coral reefs and climate","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2011,"MonPub":null,"DateUpdate":"2018-05-17","DateCreate":"2012-01-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000292824100011","VABBcode":null,"OpenAcc":0,"DOI":"10.1130/G31825.1"},"refs":null,"anarec":{"AnaID":211548,"PubliDate":2011,"Pagination":"743-746","XtraPublOfAnaID":null,"ISBN":null,"Volume":"39","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42917,"SerRR":"Geology. 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