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Late Pleistocene-Holocene evolution of the northern shelf of the Sea of Marmara

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.


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  <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>
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