2011
DOI: 10.1016/j.jmarsys.2010.08.002
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Adaptability and vulnerability of zooplankton species in the adjacent regions of the Black and Marmara Seas

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Cited by 20 publications
(20 citation statements)
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“…This may be explained by the aggregation of N. scintillans during the period of mass development in the cold layers of the Black Sea, which do not flow into the Bosphorus Strait (Bityukov 1969). In the Marmara Sea, the population of N. scintillans occupies the thin surface layer formed by the Black Sea water (Isinibilir et al 2011) due to the fact that body density of this dinoflagellate is close to the Black Sea water density (Bityukov 1969). During 2005-2009, the maximum abundance of N. scintillans reached 550,000 ind.…”
Section: Resultsmentioning
confidence: 99%
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“…This may be explained by the aggregation of N. scintillans during the period of mass development in the cold layers of the Black Sea, which do not flow into the Bosphorus Strait (Bityukov 1969). In the Marmara Sea, the population of N. scintillans occupies the thin surface layer formed by the Black Sea water (Isinibilir et al 2011) due to the fact that body density of this dinoflagellate is close to the Black Sea water density (Bityukov 1969). During 2005-2009, the maximum abundance of N. scintillans reached 550,000 ind.…”
Section: Resultsmentioning
confidence: 99%
“…In the Bosphorus Strait, the copepod A. clausi basically contributes to necrozooplankton. Isinibilir et al (2011) ). According to our refined estimation, the biomass of dead A. clausi during the same studied period amounted to 92.5 mg m −2 .…”
Section: Resultsmentioning
confidence: 99%
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