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.

Dublin Core

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  <dc:creator>Cagatay, M. N.</dc:creator>
  <dc:creator>Eris, K.</dc:creator>
  <dc:creator>Ryan, W. B. F.</dc:creator>
  <dc:creator>Sancar, Ue</dc:creator>
  <dc:creator>Polonia, A.</dc:creator>
  <dc:creator>Akcer, S.</dc:creator>
  <dc:creator>Biltekin, D.</dc:creator>
  <dc:creator>Gasperini, L.</dc:creator>
  <dc:creator>Gorur, N.</dc:creator>
  <dc:creator>Lericolais, G.</dc:creator>
  <dc:creator>Bard, E.</dc:creator>
  <dc:date>2009-01-01</dc:date>
  <dc: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.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/39477</dc:identifier>
  <dc:identifier>oai:zenodo.org:39477</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>MARINE GEOLOGY 265(3-4) 87-100</dc:source>
  <dc:title>Late Pleistocene-Holocene evolution of the northern shelf of the Sea of Marmara</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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