{"refrec":{"BRefID":302861,"RR":"<b>Polyak, V.J.; Onac, B.P.; Fornós, J.J.; Hay, C.C.; Asmerom, Y.; Dorale, J.A.; Ginés, J.; Tuccimei, P.; Ginés, A.</b> (2018). A highly resolved record of relative sea level in the western Mediterranean Sea during the last interglacial period. <i>Nature Geoscience 11(11)</i>: 860-864. <a href=\"https://dx.doi.org/10.1038/s41561-018-0222-5\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-018-0222-5</a>","BEntID":295108,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 11(11)</i>: 860-864. <a href=\"https://dx.doi.org/10.1038/s41561-018-0222-5\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-018-0222-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Polyak, V.J.; Onac, B.P.; Fornós, J.J.; Hay, C.C.; Asmerom, Y.; Dorale, J.A.; Ginés, J.; Tuccimei, P.; Ginés, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Polyak, V.J. <i>et al.</i>","Englishabstract":"The magnitude and trajectory of sea-level change during marine isotope stage (MIS) 5e of the last interglacial period is uncertain. In general, sea level may have been 6–9 m above present sea level, with one or more oscillations of up to several metres superimposed. Here we present a well-dated relative sea-level record from the island of Mallorca in the western Mediterranean Sea for MIS-5e, based on the occurrence of phreatic overgrowths on speleothems forming near sea level. We find that relative sea-level in this region was within a range of 2.15 ± 0.75 m above present levels between 126,600 ± 400 and 116,000 ± 800 years ago, although centennial-scale excursions cannot be excluded due to some gaps in the speleothem record. We corrected our relative sea-level record for glacio-isostatic adjustment using nine different glacial isostatic models. Together, these models suggest that ice-equivalent sea-level in Mallorca peaked at the start of MIS-5e then gradually decreased and stabilized by 122,000 years ago, until the highstand termination 116,000 years ago. Our sea-level record does not support the hypothesis of rapid sea-level fluctuations within MIS-5e. Instead, we suggest that melting of the polar ice sheets occurred early in the interglacial period, followed by gradual ice-sheet growth.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A highly resolved record of relative sea level in the western Mediterranean Sea during the last interglacial period","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:01.897972","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2018-11-08","DateCreate":"2018-11-08","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000448672100013","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41561-018-0222-5"},"refs":null,"anarec":{"AnaID":302861,"PubliDate":2018,"Pagination":"860-864","XtraPublOfAnaID":null,"ISBN":null,"Volume":"11","Issue":"11","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123796,"SerRR":"Nature Geoscience. 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