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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.
{ "DOI": "10.1016/j.margeo.2009.06.011", "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.", "author": [ { "family": "Cagatay", "given": " M. N." }, { "family": "Eris", "given": " K." }, { "family": "Ryan", "given": " W. B. F." }, { "family": "Sancar", "given": " Ue" }, { "family": "Polonia", "given": " A." }, { "family": "Akcer", "given": " S." }, { "family": "Biltekin", "given": " D." }, { "family": "Gasperini", "given": " L." }, { "family": "Gorur", "given": " N." }, { "family": "Lericolais", "given": " G." }, { "family": "Bard", "given": " E." } ], "container_title": "MARINE GEOLOGY", "id": "39477", "issue": "3-4", "issued": { "date-parts": [ [ 2009, 1, 1 ] ] }, "page": "87-100", "title": "Late Pleistocene-Holocene evolution of the northern shelf of the Sea of Marmara", "type": "article-journal", "volume": "265" }
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