{"refrec":{"BRefID":242048,"RR":"<b>Lampe, R.</b> (2005). Lateglacial and Holocene water-level variations along the NE German Baltic Sea coast: review and new results. <i>Quaternary International 133-134</i>: 121-136. <a href=\"http://dx.doi.org/10.1016/j.quaint.2004.10.005\" target=\"_blank\">http://dx.doi.org/10.1016/j.quaint.2004.10.005</a>","BEntID":233747,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Quaternary International 133-134</i>: 121-136. <a href=\"http://dx.doi.org/10.1016/j.quaint.2004.10.005\" target=\"_blank\">http://dx.doi.org/10.1016/j.quaint.2004.10.005</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lampe, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lampe, R.","Englishabstract":"A comprehensive overview is given of the current knowledge regarding the Lateglacial and Holocene water-table evolution along the West Pomeranian coast, which is related to the four evolutionary stages of the Baltic Sea: the Baltic Ice Lake, the Yoldia Sea, the Ancylus Lake and the Littorina Sea. The first three stages were characterized by intensive water-table fluctuations in the Baltic basin. The balance between glacio-isostatic uplift and water-table rise due to meltwater and river discharge produced either a temporary connection with the ocean or isolation from it. New findings are presented on the water levels reached during the different stages. Only at about 8 ky BP did the Baltic obtain a permanent connection with the ocean. The first marine sediments in the recent coastal zone, ca. 7.8 ky old, are found at -15 m and are related to the initial Littorina Sea. The maximum of the main Littorina-transgression was reached at -1.5 m to -2.0 m ca. 5.8 ky BP. The course of the sea level reveals that later only some minor oscillations took place, correlated with climatic fluctuations. These indicate a control by regional changes in the North Atlantic circulation rather than by global sea-level alterations. Isostatic movements were determined by comparing the reconstructed relative sea-level curve with curves assumed as nearly eustatic. The resulting isostatic curve shows uplift at 11.5 ky BP of about 55 m, which decreased until 7.8 ky BP to 6 m and ceased at ca. 3 ky BP. Currently, the coastal zone experiences a slight tilting with uplift in the northeastern part and inundation in the southwestern area.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Lateglacial and Holocene water-level variations along the NE German Baltic Sea coast: review and new results","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Baltic Sea;     West Pomerania;     Sea-level history;     Isostasy","OtherDescriptors":null,"Notes":null,"AnaPub":2005,"MonPub":null,"DateUpdate":"2014-10-14","DateCreate":"2014-10-14","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000227576900010","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.quaint.2004.10.005"},"refs":null,"anarec":{"AnaID":242048,"PubliDate":2005,"Pagination":"121-136","XtraPublOfAnaID":null,"ISBN":null,"Volume":"133-134","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45654,"SerRR":"Quaternary International. Elsevier: Oxford.  ISSN 1040-6182; e-ISSN 1873-4553","StandardTitleSer":"Quaternary International","ISSN":"1040-6182","AbbrevSer":"Quaternary International","StandardTitleMon":null,"StartPage":121,"Pages":16,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Lampe","Firstname":"Reinhard","Initials":"R.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":233747,"AutID":70858,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":null,"BEntPrivate":null,"availability":[{"BInstID":265329,"LibID":36,"BRefID":242048,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":1,"ShelfLocCode":"265329","RFID":null,"PaidValue":null,"Medium":"Server","Description":"Interne VLIZ documenten","Acronym":"VLIZ","Library":"Vlaams Instituut voor de Zee","DutchTerm":"Non-open access","URL":null,"ClassifID":228,"Classification":"Non-open access","ReqLink":1,"ClassifTypID":3,"URLLocation":"https://www.vliz.be/imisdocs/publications/","SubDir":1,"InternalReq":1,"LoggedInReq":1,"Disclaimer":"Disclaimer_VLIZ_Intern","DutchDisclaimer":"<p>Deze publicatie is enkel beschikbaar voor persoonlijk gebruik binnen de Innovocean site <br />en mag op geen enkele manier verder worden verspreid.</p>","FileFormat":".pdf","FileDescr":"pdf","InsPub":1,"InsID":36,"FileFormID":6,"LendableFlag":1,"PublicFlag":1,"orderLib":"A","Notes":null,"AccConID":null,"AccessConstraint":null,"LicURL":null}],"litstyles":null,"thespers":null,"arch2discl":null,"SERpubls":[{"PublName":"Elsevier","City":"Oxford"}],"MONpubls":null,"pictures":[],"thestermsPath":null,"thestermsASFA":null,"taxtermsASFA":null,"geotermsASFA":null,"collections":null,"conf":null,"proj":null,"Physdatasets":null,"spcols":null,"doi":null,"publs":null,"serparttypes":null,"monauthors":null,"MParts":null,"SParts":null,"hLibs":null,"langs":[{"BEntID":233747,"AbstractFlag":0,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"}],"urls":[{"URL":"http://dx.doi.org/10.1016/j.quaint.2004.10.005","externalID":"10.1016/j.quaint.2004.10.005","URLTypeCode":"DOI","URLID":36062,"URLTypID":13,"URLType":"DOI","URLPrefix":"http://dx.doi.org/"}],"thesterms":null,"taxterms":null,"geoterms":null,"othterms":null,"asfacodes":null,"asfa2codes":null,"thestermsFRIS":null,"taxtermsFRIS":null,"geotermsFRIS":null,"othtermsFRIS":null,"resmessage":"","complete":1,"sessions":{"newSesName":"Haspeslagh, Jan, J.","newSesDate":{"date":"2014-10-14 10:37:22.353000","timezone_type":3,"timezone":"Europe/Brussels"},"updSesName":"Haspeslagh, Jan, J.","updSesDate":{"date":"2014-10-14 10:37:22.353000","timezone_type":3,"timezone":"Europe/Brussels"}}}
