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Yakın Doğu Bulvarı, Lefkoşa, KKTC
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Proline Accumulation in Some Coastal Zone Plants of the Aegean Region of Turkey. M. Ozturk, B. Turkyilmaz, S. Gucel, A. Güvensen.

Yazar: Materyal türü: MakaleMakaleDil: İngilizce Yayın ayrıntıları:2011.Konu(lar): LOC sınıflandırması:
  • QK47
İçindekiler: The European Journal of Plant Science and Biotechnology 2011, Vol 5, p 54-56 Özet: In this study, the proline contents of ecophysiologically different plants were determined on a seasonal basis. The plant species investigated were Cakile maritima, Medicago marina, Pancratium maritimum and Suaeda prostrata (psammophyte-from sand dunes); Arthrocnemum fruticosum, Halimione portulacoides, Halocnemum strobilaceum, Limonium bellidifolium and Salicornia europaea (halophytes-from saline habitats). The results showed that proline content in all taxa was highest in autumn and lowest in spring. The accummulation in general was higher in halophytes (0.104 ± 0.004 ?mol g -1 (f.m.) to 55.138 ± 6.138 ?mol g -1 (f.m.)), as compared to psammophytes (0.242 ± 0.118 ?mol g -1 (f.m.) to 38.307 ± 1.455 ?mol g -1 (f.m.)). This can be attributed to both salinity and water stress in the halophytes, and water stress alone in the psammophytes.
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Online Electronic Document NEU Grand Library Online electronic QK47 .P76 2011 (Rafa gözat(Aşağıda açılır)) Ödünç verilmez EOL-1137

In this study, the proline contents of ecophysiologically different plants were determined on a seasonal basis. The plant species
investigated were Cakile maritima, Medicago marina, Pancratium maritimum and Suaeda prostrata (psammophyte-from sand dunes);
Arthrocnemum fruticosum, Halimione portulacoides, Halocnemum strobilaceum, Limonium bellidifolium and Salicornia europaea
(halophytes-from saline habitats). The results showed that proline content in all taxa was highest in autumn and lowest in spring. The
accummulation in general was higher in halophytes (0.104 ± 0.004 ?mol g -1 (f.m.) to 55.138 ± 6.138 ?mol g -1 (f.m.)), as compared to
psammophytes (0.242 ± 0.118 ?mol g -1 (f.m.) to 38.307 ± 1.455 ?mol g -1 (f.m.)). This can be attributed to both salinity and water stress in
the halophytes, and water stress alone in the psammophytes.

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