{"refrec":{"BRefID":144348,"RR":"<b>Bard, E.; Hamelin, B.; Delanghe-Sabatier, D.</b> (2010). Deglacial meltwater pulse 1B and Younger Dryas sea levels revisited with boreholes at Tahiti. <i>Science (Wash.) 327(5970)</i>: 1235-1237. <a href=\"https://dx.doi.org/10.1126/science.1180557\" target=\"_blank\">https://dx.doi.org/10.1126/science.1180557</a>","BEntID":137480,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 327(5970)</i>: 1235-1237. <a href=\"https://dx.doi.org/10.1126/science.1180557\" target=\"_blank\">https://dx.doi.org/10.1126/science.1180557</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bard, E.; Hamelin, B.; Delanghe-Sabatier, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bard, E. <i>et al.</i>","Englishabstract":"Reconstructing sea-level changes during the last deglaciation provides a way of understanding the ice dynamics that can perturb large continental ice sheets. The resolution of the few sea-level records covering the critical time interval between 14,000 and 9,000 calendar years before the present is still insufficient to draw conclusions about sea-level changes associated with the Younger Dryas cold event and the meltwater pulse 1B (MWP-1B). We used the uranium-thorium method to date shallow-living corals from three new cores drilled onshore in the Tahiti barrier reef. No significant discontinuity can be detected in the sea-level rise during the MWP-1B period. The new Tahiti sea-level record shows that the sea-level rise slowed down during the Younger Dryas before accelerating again during the Holocene.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Deglacial meltwater pulse 1B and Younger Dryas sea levels revisited with boreholes at Tahiti","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-10 01:31:39.630188","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2010,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2010-03-19","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000275162100033","VABBcode":null,"OpenAcc":0,"DOI":"10.1126/science.1180557"},"refs":null,"anarec":{"AnaID":144348,"PubliDate":2010,"Pagination":"1235-1237","XtraPublOfAnaID":null,"ISBN":null,"Volume":"327","Issue":"5970","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43776,"SerRR":"Science (Washington). 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