1 Ocak 2009 Dergi makalesi Açık Erişim

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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        "affiliation": "ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey", 
        "name": "Cagatay, M. N."
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      {
        "affiliation": "ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey", 
        "name": "Eris, K."
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        "affiliation": "Columbia Univ, Lamont Doherty Earth Observ, New York, NY 10027 USA", 
        "name": "Ryan, W. B. F."
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      {
        "affiliation": "ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey", 
        "name": "Sancar, Ue"
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      {
        "affiliation": "Inst Marine Geol, ISMAR CNR Bologna, Bologna, Italy", 
        "name": "Polonia, A."
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      {
        "name": "Akcer, S."
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      {
        "affiliation": "ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey", 
        "name": "Biltekin, D."
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      {
        "affiliation": "Inst Marine Geol, ISMAR CNR Bologna, Bologna, Italy", 
        "name": "Gasperini, L."
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      {
        "affiliation": "ITU EMCOL, Fac Min, TR-34469 Istanbul, Turkey", 
        "name": "Gorur, N."
      }, 
      {
        "affiliation": "IFREMER, Brest, France", 
        "name": "Lericolais, G."
      }, 
      {
        "affiliation": "CEREGE, Aix En Provence, France", 
        "name": "Bard, E."
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    "description": "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.", 
    "doi": "10.1016/j.margeo.2009.06.011", 
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    "journal": {
      "issue": "3-4", 
      "pages": "87-100", 
      "title": "MARINE GEOLOGY", 
      "volume": "265"
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      "title": "Dergi makalesi", 
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    "title": "Late Pleistocene-Holocene evolution of the northern shelf of the Sea of Marmara"
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