{"refrec":{"BRefID":334300,"RR":"<b>Gowan, E.J.; Zhang, X.; Khosravi, S.; Rovere, A.; Stocchi, P.; Hughes, A.L.C.; Gyllencreutz, R.; Mangerud, J.; Svendsen, J.-I.; Lohmann, G.</b> (2021). A new global ice sheet reconstruction for the past 80 000 years. <i>Nature Comm. 12</i>: 1199. <a href=\"https://doi.org/10.1038/s41467-021-21469-w\" target=\"_blank\">https://doi.org/10.1038/s41467-021-21469-w</a>","BEntID":330856,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Comm. 12</i>: 1199. <a href=\"https://doi.org/10.1038/s41467-021-21469-w\" target=\"_blank\">https://doi.org/10.1038/s41467-021-21469-w</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gowan, E.J.; Zhang, X.; Khosravi, S.; Rovere, A.; Stocchi, P.; Hughes, A.L.C.; Gyllencreutz, R.; Mangerud, J.; Svendsen, J.-I.; Lohmann, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gowan, E.J. <i>et al.</i>","Englishabstract":"<p>    The evolution of past global ice sheets is highly uncertain. One example is    the missing ice problem during the Last Glacial Maximum (LGM, 26 000-19 000    years before present) – an apparent 8-28 m discrepancy between far-field    sea level indicators and modelled sea level from ice sheet reconstructions.In the absence of ice sheet reconstructions, researchers often use marine    <em>δ</em><sup>18</sup>O proxy records to infer ice volume prior to the    LGM. We present a global ice sheet reconstruction for the past 80 000    years, called PaleoMIST 1.0, constructed independently of far-field sea    level and <em>δ</em><sup>18</sup>O proxy records. Our reconstruction is    compatible with LGM far-field sea-level records without requiring extra ice    volume, thus solving the missing ice problem. However, for Marine Isotope    Stage 3 (57 000-29 000 years before present) - a pre-LGM period - our    reconstruction does not match proxy-based sea level reconstructions,    indicating the relationship between marine <em>δ</em><sup>18</sup>O and sea    level may be more complex than assumed.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A new global ice sheet reconstruction for the past 80 000 years","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:32:21.474729","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-03-01","DateCreate":"2021-03-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000623786100001","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41467-021-21469-w"},"refs":null,"anarec":{"AnaID":334300,"PubliDate":2021,"Pagination":"1199","XtraPublOfAnaID":null,"ISBN":null,"Volume":"12","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":198717,"SerRR":"Nature Communications. 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