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Bipolar seesaw control on last interglacial sea level. <i>Nature (Lond.) 522(7555)</i>: 197–201. <a href=\"http://dx.doi.org/10.1038/nature14499\" target=\"_blank\">http://dx.doi.org/10.1038/nature14499</a>","BEntID":239431,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 522(7555)</i>: 197–201. <a href=\"http://dx.doi.org/10.1038/nature14499\" target=\"_blank\">http://dx.doi.org/10.1038/nature14499</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Marino, G.; Rohling, E.J.; Rodríguez-Sanz, L.; Grant, K.M.; Heslop, D.; Roberts, A.P.; Stanford, J.D.; Yu, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Marino, G. <i>et al.</i>","Englishabstract":"A synthesis of new and existing data allows Heinrich Stadial 11 (HS11), a prominent Northern Hemisphere cold event, to be linked to the timing of peak sea-level rise during glacial termination T-II, whereas rapid sea-level rise in T-I is shown to clearly post-date Heinrich Stadial 1, so fundamentally different mechanisms seem to be at work during glacial terminations.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Bipolar seesaw control on last interglacial sea level","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-14 01:32:19.922092","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2015-06-12","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000356016700035","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/nature14499"},"refs":null,"anarec":{"AnaID":247730,"PubliDate":2015,"Pagination":"197–201","XtraPublOfAnaID":null,"ISBN":null,"Volume":"522","Issue":"7555","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43431,"SerRR":"Nature: International Weekly Journal of Science. 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