{"refrec":{"BRefID":437431,"RR":"<b>Kvorning, A.B.; Heikkila, M.; Pearce, C.; Seidenkrantz, M.-S.; Simpson, G.L.; Meire, L.; Kuijpers, A.; Larsen, N.K.; Ribeiro, S.</b> (2025). A Holocene fjord record from Greenland reveals exceptional Atlantic water influence during minimum ice-sheet extent. <i>Commun. Earth Environ. 6(1)</i>: 326. <a href=\"https://dx.doi.org/10.1038/s43247-025-02282-5\" target=\"_blank\">https://dx.doi.org/10.1038/s43247-025-02282-5</a>","BEntID":435262,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Commun. Earth Environ. 6(1)</i>: 326. <a href=\"https://dx.doi.org/10.1038/s43247-025-02282-5\" target=\"_blank\">https://dx.doi.org/10.1038/s43247-025-02282-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kvorning, A.B.; Heikkila, M.; Pearce, C.; Seidenkrantz, M.-S.; Simpson, G.L.; Meire, L.; Kuijpers, A.; Larsen, N.K.; Ribeiro, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kvorning, A.B. <i>et al.</i>","Englishabstract":"<span style=\"background-color:rgb(255,255,255);color:rgb(34,34,34);\">The Holocene Thermal Maximum has been considered an analog for near-future climate. Terrestrial records show that this period culminated in Southwest Greenland with the Greenland Ice Sheet retreating behind its present-day position. However, there is a paucity of Holocene coastal marine records proximal to the ice sheet from which to infer marine conditions. Here we present a multi-proxy record from Nuup Kangerlua covering the past ~10,500 years, supported by a one-year sediment trap time-series. We infer modern sea-surface conditions comparable to those following the fjord’s deglaciation from 10,000 to 8000 calibrated years before present. Warmer temperatures led to a period of pronounced meltwater discharge and peak marine productivity by 7500 calibrated years before present. We detect an exceptional oceanographic regime with no recent analog from ~7000 to 3000 calibrated years before present, when reduced ice-sheet extent was coeval with entrainment of subpolar mode water (of Atlantic origin) into the fjord.</span>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A Holocene fjord record from Greenland reveals exceptional Atlantic water influence during minimum ice-sheet extent","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-08 01:31:41.051948","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Palaeoceanography; Palaeoclimate","OtherDescriptors":null,"Notes":null,"AnaPub":2025,"MonPub":null,"DateUpdate":"2026-01-29","DateCreate":"2026-01-29","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s43247-025-02282-5"},"refs":null,"anarec":{"AnaID":437431,"PubliDate":2025,"Pagination":"326","XtraPublOfAnaID":null,"ISBN":null,"Volume":"6","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":337093,"SerRR":"Communications Earth & Environment. 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