Vulnerability of copepod eggs in salinity and temperature gradients of the Marmara and Black Seas
Yazarlar (7)
Leonıd Svetlıchny
Elena Hubareva
Genuarıo Belmonte
Prof. Dr. Melek İşinibilir Okyar İstanbul Üniversitesi, Türkiye
Prof. Dr. Funda ÜSTÜN Sinop Üniversitesi, Türkiye
İzzet Noyan Yılmaz
Türkiye
Benin Toklu Alıçlı İstanbul Üniversitesi, Türkiye
Makale Türü Açık Erişim Özgün Makale (SSCI, AHCI, SCI, SCI-Exp dergilerinde yayınlanan tam makale)
Dergi Adı MARINE ECOLOGY PROGRESS SERIES (Q1)
Dergi ISSN 0171-8630 Dergi Bilgileri (2010)
Dergi Tarandığı Indeksler SCI-Expanded
Makale Dili İngilizce Basım Tarihi 01-2010
Kabul Tarihi Yayınlanma Tarihi 30-11-2010
Cilt / Sayı / Sayfa 419 / 0 / 109–120 DOI 10.3354/meps08837
Makale Linki https://www.int-res.com/abstracts/meps/v419/p109-120/
UAK Araştırma Alanları
Su Ürünleri Temel Bilimler
Özet
Mass density, sinking speed and hatching success of eggs in Calanus euxinus, Acartia clausi and A. tonsa have been examined in response to salinity and temperature of the Marmara and Black Seas. Eggs of C. euxinus from the Marmara and Black Sea populations (mean mass density of 1.036 to 1.040 g cm–3) laid in brackish (18 to 22 psu) upper layers of the Marmara Sea could sink to high-saline (~ 38.5 psu) deep layers during embryonic development. Gradual salinity increase from 22 to 38.5 psu in laboratory experiments reduced egg hatching success in C. euxinus from the Marmara Sea from 97±4 to 47±11%(means±SD) while all eggs of the Black Sea C. euxinus did not hatch. Mean mass density of eggs in A. tonsa and A. clausi amounted to 1.062 and 1.044 g cm–3, respectively. Eggs of A. tonsa with higher mass density and longer development time than those of A. clausi could descend to high salinity …
Anahtar Kelimeler
Calanus euxinus | Acartia clausi | Acartia tonsa | Egg mass density | Hatching success | Salinity and temperature tolerance | Black Sea | Marmara Sea
BM Sürdürülebilir Kalkınma Amaçları
Atıf Sayıları
Web of Science 8
Google Scholar 15
Vulnerability of copepod eggs in salinity and temperature gradients of the Marmara and Black Seas

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