{"refrec":{"BRefID":353132,"RR":"<b>Scheder, J.; Bungenstock, F.; Haynert, K.; Pint, A.; Schlütz, F.; Frenzel, P.; Wehrmann, A.; Brückner, H.; Engel, M.</b> (2022). Insights into Holocene relative sea-level changes in the southern North Sea using an improved microfauna-based transfer function. <i>J. Quaternary Sci. 37(1)</i>: 71-85. <a href=\"https://dx.doi.org/10.1002/jqs.3380\" target=\"_blank\">https://dx.doi.org/10.1002/jqs.3380</a>","BEntID":350841,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Quaternary Sci. 37(1)</i>: 71-85. <a href=\"https://dx.doi.org/10.1002/jqs.3380\" target=\"_blank\">https://dx.doi.org/10.1002/jqs.3380</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Scheder, J.; Bungenstock, F.; Haynert, K.; Pint, A.; Schlütz, F.; Frenzel, P.; Wehrmann, A.; Brückner, H.; Engel, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Scheder, J. <i>et al.</i>","Englishabstract":"In light of global warming and rising relative sea level (RSL), detailed reconstructions of RSL histories and their controlling processes are essential in order to manage coastal-protection challenges. This study contributes to unravelling Holocene RSL change on the East Frisian North Sea coast in high resolution and with a new approach for the German Bight. For the first time, a transfer function (vertical error: 29.7 cm ≙ ~11% of the mean tidal range) for RSL change based on a combined training set of benthic foraminifers and ostracods from the back-barrier tidal basin of Spiekeroog is applied to the Holocene record of the back-barrier tidal basin of Norderney. The resulting RSL curve for the Norderney tidal basin is corrected for decompaction and shows a deceleration in RSL rise between 6000 and 5000 cal bp. The smallest possible error envelope (~1 m) results from the good suitability of salt-marsh layers between 5000 and 4000 cal bp. The RSL curve provides an approach towards the closure of the common data gap of peat-based curves for the southern North Sea related to a lack of basal peats in the youngest age range, and verifies regional differences in glacial isostatic adjustment.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Insights into Holocene relative sea-level changes in the southern North Sea using an improved microfauna-based transfer function","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-24 01:33:12.614816","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"coastal change; Foraminifera; multiproxy approach; northern Germany; Ostracoda","OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-10-06","DateCreate":"2022-06-28","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000705463600001","VABBcode":null,"OpenAcc":1,"DOI":"10.1002/jqs.3380"},"refs":null,"anarec":{"AnaID":353132,"PubliDate":2022,"Pagination":"71-85","XtraPublOfAnaID":null,"ISBN":null,"Volume":"37","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45705,"SerRR":"Journal of Quaternary Science. 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