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dc.contributor.authorTugrul, S
dc.contributor.authorYilmaz, A
dc.contributor.authorSalihoglu, I
dc.contributor.authorEdiger, Dilek
dc.contributor.authorPolat, CS
dc.date.accessioned2021-03-02T20:17:26Z
dc.date.available2021-03-02T20:17:26Z
dc.identifier.citationEdiger D., Tugrul S., Polat C., Yilmaz A., Salihoglu I., "Abundance and elemental composition of particulate matter tn the upper layer of northeastern Mediterranean", NATO Advanced Research Workshop on the Eastern Mediterranean as a Laboratory Basin for the Assessment of Contrasting Ecosystems, KIEV, Ukrayna, 23 - 27 Mart 1998, cilt.51, ss.241-266
dc.identifier.othervv_1032021
dc.identifier.otherav_012b7b7c-5277-4e3f-ac34-2ce9a4cefdf6
dc.identifier.urihttp://hdl.handle.net/20.500.12627/6764
dc.description.abstractSuspended particulate (POC: PON, PP) profiles obtained in 1991-1994 indicate the existence of characteristic subsurface maxima near the base of the euphotic zone in the cyclonic Rhodes gyre and its peripherial waters in the Northeastern Mediterranean. Interestingly the N:P of the bulk seston nas reasonable during stratification seasons when the surface water was relatively: poor in phosphate: but the ratio was unexpectedly low (N:P=6-12) in the late winter of 1992 when the surface layer of Rhodes gyre was occupied with nutrient rich deep waters.
dc.language.isoeng
dc.subjectEcology, Evolution, Behavior and Systematics
dc.subjectEcology
dc.subjectEcological Modeling
dc.subjectSmall Animals
dc.subjectPhysical Sciences
dc.subjectLife Sciences
dc.subjectHealth Sciences
dc.subjectEKOLOJİ
dc.subjectÇevre / Ekoloji
dc.subjectTarım ve Çevre Bilimleri (AGE)
dc.subjectDENİZ VE TATLISU BİYOLOJİSİ
dc.subjectBitki ve Hayvan Bilimleri
dc.subjectTarımsal Bilimler
dc.subjectZiraat
dc.subjectToprak ve Bitki Besleme
dc.subjectToprak ve Su Muhafazası ve Amenajmanı
dc.subjectSu Hasadı
dc.subjectÇevre Mühendisliği
dc.subjectÇevre Teknolojisi
dc.subjectEkoloji ve Kirlenme
dc.subjectMühendislik ve Teknoloji
dc.titleAbundance and elemental composition of particulate matter tn the upper layer of northeastern Mediterranean
dc.typeBildiri
dc.contributor.departmentİstanbul Üniversitesi , Deniz Bilimleri Ve İşletmeciliği Enstitüsü , Deniz Bilimleri Ve İşletmeciliği Bölümü
dc.identifier.volume51
dc.contributor.firstauthorID2472973


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