{"refrec":{"BRefID":363209,"RR":"<b>Wienberg, C.; Titschack, J.; Freiwald, A.; Frank, N.; Lundälv, T.; Taviani, M.; Beuck, L.; Schröder-Ritzrau, A.; Krengel, T.; Hebbeln, D.</b> (2018). The giant Mauritanian cold-water coral mound province: oxygen control on coral mound formation. <i>Quat. Sci. Rev. 185</i>: 135-152. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2018.02.012\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2018.02.012</a>","BEntID":360927,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Quat. Sci. Rev. 185</i>: 135-152. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2018.02.012\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2018.02.012</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wienberg, C.; Titschack, J.; Freiwald, A.; Frank, N.; Lundälv, T.; Taviani, M.; Beuck, L.; Schröder-Ritzrau, A.; Krengel, T.; Hebbeln, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wienberg, C. <i>et al.</i>","Englishabstract":"The largest coherent cold-water coral (CWC) mound province in the Atlantic Ocean exists along the Mauritanian margin, where up to 100 m high mounds extend over a distance of ∼400 km, arranged in two slope-parallel chains in 400–550 m water depth. Additionally, CWCs are present in the numerous submarine canyons with isolated coral mounds being developed on some canyon flanks. Seventy-seven Uranium-series coral ages were assessed to elucidate the timing of CWC colonisation and coral mound development along the Mauritanian margin for the last ∼120,000 years. Our results show that CWCs were present on the mounds during the Last Interglacial, though in low numbers corresponding to coral mound aggradation rates of 16 cm kyr<sup>−1</sup>. Most prolific periods for CWC growth are identified for the last glacial and deglaciation, resulting in enhanced mound aggradation (>1000 cm kyr<sup>−1</sup>), before mound formation stagnated along the entire margin with the onset of the Holocene. Until today, the Mauritanian mounds are in a dormant state with only scarce CWC growth. In the canyons, live CWCs are abundant since the Late Holocene at least. Thus, the canyons may serve as a refuge to CWCs potentially enabling the observed modest re-colonisation pulse on the mounds along the open slope. The timing and rate of the pre-Holocene coral mound aggradation, and the cessation of mound formation varied between the individual mounds, which was likely the consequence of vertical/lateral changes in water mass structure that placed the mounds near or out of oxygen-depleted waters, respectively.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The giant Mauritanian cold-water coral mound province: oxygen control on coral mound formation","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-28 01:33:03.921271","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Lophelia pertusa; Coral mound; Submarine canyon; Uranium-series dating; Mound aggradation rate; Last glacial; Dissolved oxygen concentration; South Atlantic Central Water; Mauritanian margin","OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2023-04-05","DateCreate":"2023-04-04","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000428830400010","VABBcode":null,"OpenAcc":1,"DOI":"10.1016/j.quascirev.2018.02.012"},"refs":null,"anarec":{"AnaID":363209,"PubliDate":2018,"Pagination":"135-152","XtraPublOfAnaID":null,"ISBN":null,"Volume":"185","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45667,"SerRR":"Quaternary Science Reviews. 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