{"refrec":{"BRefID":363021,"RR":"Cartelle, V.; García-Gil, S. (2019). From a river valley to a ria: evolution of an incised valley (Ria de Ferrol, north-west Spain) since the Last Glacial Maximum. Sedimentology 66(5): 1930-1966. https://dx.doi.org/10.1111/sed.12565","BEntID":360739,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". Sedimentology 66(5): 1930-1966. https://dx.doi.org/10.1111/sed.12565","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cartelle, V.; García-Gil, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cartelle, V.; García-Gil, S.","Englishabstract":"The evolution of incised valleys is an important area of research due to the invaluable data it provides on sea-level variations and depositional environments. In this article the sedimentary evolution of the Ría de Ferrol (north-west Spain) from the Last Glacial Maximum to the present is reconstructed using a multidisciplinary approach, combining seismic and sedimentary facies, and supported by radiocarbon data and geochemical proxies to distinguish the elements of sedimentary architecture within the ria infill. The main objectives are: (i) to analyse the ria environment as a type of incised valley to evaluate the response of the system to the different drivers; (ii) to investigate the major controlling factors; and (iii) to explore the differentiation between rias and estuaries. As a consequence of the sea-level rise subsequent to the Last Glacial Maximum (ca 20 kyr bp), an extensive basin, drained by a braided palaeoriver, evolved into a tide-dominated estuary and finally into a ria environment. Late Pleistocene and Holocene high-frequency sea-level variations were major factors that modulated the type of depositional environments and their evolution. Another major modulating factor was the antecedent morphology of the ria, with a rock-incised narrow channel in the middle of the basin (the Ferrol Strait), which influenced the evolution of the ria as it became flooded during Holocene transgression. The strait acted as a rock-bounded ‘tidal inlet’ enhancing the tidal erosion and deposition at both ends, i.e. with an ebb-tidal delta in the outer sector and tidal sandbanks in the inner sector. The final step in the evolution of the incised valley into the modern-defined ria system was driven by the last relative sea-level rise (after 4 kyr bp) when the river mouths retreated landward and a single palaeoriver was converted into minor rivers and streams with scattered mouths in an extensive coastal area.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"From a river valley to a ria: evolution of an incised valley (Ria de Ferrol, north-west Spain) since the Last Glacial Maximum","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":"Incised valley; ria; sea level; sedimentary environments; sedimentary facies; seismic facies; tide-dominated estuary","OtherDescriptors":null,"Notes":null,"AnaPub":2019,"MonPub":null,"DateUpdate":"2023-04-03","DateCreate":"2023-04-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000477915100017","VABBcode":null,"OpenAcc":0,"DOI":"10.1111/sed.12565"},"refs":null,"anarec":{"AnaID":363021,"PubliDate":2019,"Pagination":"1930-1966","XtraPublOfAnaID":null,"ISBN":null,"Volume":"66","Issue":"5","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43812,"SerRR":"Sedimentology. Wiley-Blackwell: Amsterdam. ISSN 0037-0746; e-ISSN 1365-3091","StandardTitleSer":"Sedimentology","ISSN":"0037-0746","AbbrevSer":"Sedimentology","StandardTitleMon":null,"StartPage":1930,"Pages":37,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Cartelle","Firstname":"Víctor","Initials":"V.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":360739,"AutID":502779,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":"0000-0002-8894-7172","PersID":40672,"InsID":null},{"AutName":"García-Gil","Firstname":"Soledad","Initials":"S.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":360739,"AutID":521533,"OrderNr":2,"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":388534,"LibID":36,"BRefID":363021,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":null,"ShelfLocCode":"388534","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":"
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