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Cagatay, M. N.; Eris, K.; Ryan, W. B. F.; Sancar, Ue; Polonia, A.; Akcer, S.; Biltekin, D.; Gasperini, L.; Gorur, N.; Lericolais, G.; Bard, E.
<?xml version='1.0' encoding='utf-8'?> <resource xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.1/metadata.xsd"> <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/39477</identifier> <creators> <creator> <creatorName>Cagatay, M. N.</creatorName> <givenName>M. N.</givenName> <familyName>Cagatay</familyName> <affiliation>ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey</affiliation> </creator> <creator> <creatorName>Eris, K.</creatorName> <givenName>K.</givenName> <familyName>Eris</familyName> <affiliation>ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey</affiliation> </creator> <creator> <creatorName>Ryan, W. B. F.</creatorName> <givenName>W. B. F.</givenName> <familyName>Ryan</familyName> <affiliation>Columbia Univ, Lamont Doherty Earth Observ, New York, NY 10027 USA</affiliation> </creator> <creator> <creatorName>Sancar, Ue</creatorName> <givenName>Ue</givenName> <familyName>Sancar</familyName> <affiliation>ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey</affiliation> </creator> <creator> <creatorName>Polonia, A.</creatorName> <givenName>A.</givenName> <familyName>Polonia</familyName> <affiliation>Inst Marine Geol, ISMAR CNR Bologna, Bologna, Italy</affiliation> </creator> <creator> <creatorName>Akcer, S.</creatorName> <givenName>S.</givenName> <familyName>Akcer</familyName> </creator> <creator> <creatorName>Biltekin, D.</creatorName> <givenName>D.</givenName> <familyName>Biltekin</familyName> <affiliation>ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey</affiliation> </creator> <creator> <creatorName>Gasperini, L.</creatorName> <givenName>L.</givenName> <familyName>Gasperini</familyName> <affiliation>Inst Marine Geol, ISMAR CNR Bologna, Bologna, Italy</affiliation> </creator> <creator> <creatorName>Gorur, N.</creatorName> <givenName>N.</givenName> <familyName>Gorur</familyName> <affiliation>ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey</affiliation> </creator> <creator> <creatorName>Lericolais, G.</creatorName> <givenName>G.</givenName> <familyName>Lericolais</familyName> <affiliation>IFREMER, Brest, France</affiliation> </creator> <creator> <creatorName>Bard, E.</creatorName> <givenName>E.</givenName> <familyName>Bard</familyName> <affiliation>CEREGE, Aix En Provence, France</affiliation> </creator> </creators> <titles> <title>Late Pleistocene-Holocene Evolution Of The Northern Shelf Of The Sea Of Marmara</title> </titles> <publisher>Aperta</publisher> <publicationYear>2009</publicationYear> <dates> <date dateType="Issued">2009-01-01</date> </dates> <resourceType resourceTypeGeneral="Text">Journal article</resourceType> <alternateIdentifiers> <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/39477</alternateIdentifier> </alternateIdentifiers> <relatedIdentifiers> <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.margeo.2009.06.011</relatedIdentifier> </relatedIdentifiers> <rightsList> <rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights> <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights> </rightsList> <descriptions> <description descriptionType="Abstract">Chirp sub-bottom profiling, multibeam bathymetric mapping and a combination of faunal and isotopic analysis of molluscs and foraminifera in sediment cores on the northern shelf of the Sea of Marmara (SoM) provide evidence of sea-level excursions, water exchanges between the adjacent Mediterranean and Black Seas, and oscillating salinity over the last 160 ka bp. During the marine isotope stages MIS-2, MIS-3, MIS-4 and MIS-6 the SoM disconnected from the Mediterranean Sea and evolved into a lake. During MIS-1, MIS-5 and MIS-7, the SoM reconnected and became salty once again. Sapropels formed shortly after each invasion of Mediterranean saltwater observed in our cores. Concurrent suboxic-dysoxic conditions prevailed over quite shallow substrates on the shelf.</description> </descriptions> </resource>
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