{"refrec":{"BRefID":348153,"RR":"<b>Çagatay, M.N.; Eris, K.; Erdem, Z.</b> (2021). Morphology and late Pleistocene-Holocene sedimentation of the Strait of İstanbul (Bosphorus): A review. <i>Geol. Soc. Lond. Spec. publ. 523</i>: SP523-2021-48. <a href=\"https://dx.doi.org/10.1144/sp523-2021-48\" target=\"_blank\">https://dx.doi.org/10.1144/sp523-2021-48</a>","BEntID":344847,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Geol. Soc. Lond. Spec. publ. 523</i>: SP523-2021-48. <a href=\"https://dx.doi.org/10.1144/sp523-2021-48\" target=\"_blank\">https://dx.doi.org/10.1144/sp523-2021-48</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Çagatay, M.N.; Eris, K.; Erdem, Z.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Çagatay, M.N.; Eris, K.; Erdem, Z.","Englishabstract":"<p>    The Bosphorus (Istanbul Strait) is natural strait that connects the Black    Sea with the Aegean Sea via the Sea of Marmara and Dardanelles Strait. It    is a 31 km long and 3.5 km wide winding channel, with an irregular bottom    morphology. It has depressions up to -110 m deep, and two sills with depths    of -35 and -58 m in the south and north, respectively.</p><p>    Presently, a two-layer water exchange exists through the strait, with the    Mediterranean and Black Sea waters forming the lower and upper layers,    respectively. The Bosphorus channel extends as shelf valleys on the Black    Sea and Sea of Marmara shelves. However, it operated as a river valley or    an estuary during the stadial low-stand periods.</p><p>    The infill sedimentary succession of the Bosphorus channel is up to ∼100 m    thick above the Palaeozoic-Cretaceous basement with an irregular    topography. The oldest sediments are sandy to muddy fluvial-lacustrine    facies of late Pleistocene age, which are preserved only in up to -160    m-deep scoured depressions of the basement. They are overlain by mid-late    Holocene estuarine-marine shelly sandy to muddy sediments with patches of    bioherms and shelly lag deposits.</p><p>    The Bosphorus outlet areas of the Black Sea and Sea of Marmara are    characterized by a submarine fan and a shelf valley, respectively. The fan    system in the Black Sea started depositing ∼900 yr after the initial    vigorous marine water incursion at ∼8.4 <sup>14</sup>C kyr BP. On the    Marmara shelf, extension of the Bosphorus channel is a sinuous shelf valley    with a channel-leveé complex, which was deposited by the Black Sea outflow    during the 11-10 <sup>14</sup>C kyr BP. Catastrophic floodings of the Sea    of Marmara by torrential Black Sea outflows during the Greenland    Interstadial melt water pulses, as well as the strong Mediterranean current    towards the Black Sea during the interglacial periods, were responsible for    carving the Bosphorus channel and the shelf valleys, as well as removing    the sediments belonging to the earlier periods.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Morphology and late Pleistocene-Holocene sedimentation of the Strait of İstanbul (Bosphorus): A review","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-10 01:30:59.955013","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-12-14","DateCreate":"2021-12-14","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1144/sp523-2021-48"},"refs":null,"anarec":{"AnaID":348153,"PubliDate":2021,"Pagination":"SP523-2021-48","XtraPublOfAnaID":null,"ISBN":null,"Volume":"523","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":5898,"SerRR":"<b>Hartley, A.J. <i>et al.</i> (Ed.)</b> Geological Society Special Publication. Geological Society of London: Oxford; London; Edinburgh; Boston, Mass.; Carlton, Vic..  ISSN 0305-8719; e-ISSN 2041-4927","StandardTitleSer":"Geological Society Special Publication","ISSN":"0305-8719","AbbrevSer":"Geol. Soc. Lond. Spec. publ.","StandardTitleMon":null,"StartPage":null,"Pages":null,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Çagatay","Firstname":null,"Initials":"M.N.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":344847,"AutID":214790,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Eris","Firstname":"Kadir","Initials":"K.","Affiliation":"Geology & Mining, Technical University of Istanbul","Discriminator":null,"CorporateFlag":0,"BEntID":344847,"AutID":134650,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Erdem","Firstname":"Zeynep","Initials":"Z.","Affiliation":"MMB","Discriminator":null,"CorporateFlag":0,"BEntID":344847,"AutID":245916,"OrderNr":3,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":"MMB","InsFSN":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; Marine Microbiology and Biogeochemistry","ORCID":null,"PersID":33956,"InsID":13655}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":344847,"BEntPrivate":null,"availability":null,"litstyles":null,"thespers":null,"arch2discl":805,"SERpubls":[{"PublName":"Geological Society of London","City":"Oxford; London; Edinburgh; Boston, Mass.; Carlton, Vic."}],"MONpubls":null,"pictures":[],"thestermsPath":null,"thestermsASFA":null,"taxtermsASFA":null,"geotermsASFA":null,"collections":null,"conf":null,"proj":null,"Physdatasets":null,"spcols":{"805":{"SpName":"Koninklijk Nederlands Instituut voor Onderzoek der Zee","SpColID":805,"ParSpColID":null,"TopParID":null,"ShortName":"NIOZ","URLLocation":"https://www.vliz.be/imis/nioz/imis.php?refid=","LibID":2779,"OpenRepoFlag":1,"SpTypID":1,"TopParIDNotWebsite":null,"SpColPath":"NIOZ"}},"doi":null,"publs":null,"serparttypes":null,"monauthors":null,"MParts":null,"SParts":null,"hLibs":null,"langs":[{"BEntID":344847,"AbstractFlag":0,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"},{"BEntID":344847,"AbstractFlag":1,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"}],"urls":[{"URL":"https://dx.doi.org/10.1144/sp523-2021-48","externalID":"10.1144/sp523-2021-48","URLTypeCode":"DOI","URLID":98471,"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":"Leonne.van.der.Weegen@nioz.nl","newSesDate":{"date":"2021-12-14 12:57:00.720000","timezone_type":3,"timezone":"Europe/Brussels"},"updSesName":"Leonne.van.der.Weegen@nioz.nl","updSesDate":{"date":"2021-12-14 12:57:00.720000","timezone_type":3,"timezone":"Europe/Brussels"}}}
