{"refrec":{"BRefID":285231,"RR":"<b>Gupta, S.; Collier, J.S.; Garcia-Moreno, D.; Oggioni, F.; Trentesaux, A.; Vanneste, K.; De Batist, M.; Camelbeeck, T.; Potter, G.; Van Vliet-Lanoë, B.; Arthur, J.C.R.</b> (2017). Two-stage opening of the Dover Strait and the origin of island Britain. <i>Nature Comm. 8</i>: 12 pp. <a href=\"https://dx.doi.org/10.1038/ncomms15101\" target=\"_blank\">https://dx.doi.org/10.1038/ncomms15101</a>","BEntID":277256,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Comm. 8</i>: 12 pp. <a href=\"https://dx.doi.org/10.1038/ncomms15101\" target=\"_blank\">https://dx.doi.org/10.1038/ncomms15101</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gupta, S.; Collier, J.S.; Garcia-Moreno, D.; Oggioni, F.; Trentesaux, A.; Vanneste, K.; De Batist, M.; Camelbeeck, T.; Potter, G.; Van Vliet-Lanoë, B.; Arthur, J.C.R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gupta, S. <i>et al.</i>","Englishabstract":"Late Quaternary separation of Britain from mainland Europe is considered to be a consequence of spillover of a large proglacial lake in the Southern North Sea basin. Lake spillover is inferred to have caused breaching of a rock ridge at the Dover Strait, although this hypothesis remains untested. Here we show that opening of the Strait involved at least two major episodes of erosion. Sub-bottom records reveal a remarkable set of sediment-infilled depressions that are deeply incised into bedrock that we interpret as giant plunge pools. These support a model of initial erosion of the Dover Strait by lake overspill, plunge pool erosion by waterfalls and subsequent dam breaching. Cross-cutting of these landforms by a prominent bedrock-eroded valley that is characterized by features associated with catastrophic flooding indicates final breaching of the Strait by high-magnitude flows. These events set-up conditions for island Britain during sea-level highstands and caused large-scale re-routing of NW European drainage.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Two-stage opening of the Dover Strait and the origin of island Britain","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-22 01:31:57.104280","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2017,"MonPub":null,"DateUpdate":"2017-05-31","DateCreate":"2017-05-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000398161100001","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/ncomms15101"},"refs":null,"anarec":{"AnaID":285231,"PubliDate":2017,"Pagination":"12 pp","XtraPublOfAnaID":null,"ISBN":null,"Volume":"8","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":198717,"SerRR":"Nature Communications. 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