کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6384901 1626647 2014 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Offshore-onshore linkages in the larval life history of sole in the Gulf of Lions (NW-Mediterranean)
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی
پیش نمایش صفحه اول مقاله
Offshore-onshore linkages in the larval life history of sole in the Gulf of Lions (NW-Mediterranean)
چکیده انگلیسی
Understanding individual dispersion from offshore natal areas to coastal nurseries during pelagic larval life is especially important for the sustainable management of exploited marine fish species. For several years, the hatching period, the larval life duration, the average growth rate and the otolith chemical composition (δ13C, δ18O, Sr:Ca and Ba:Ca) during the larval life were studied for young of the year (YOY) of sole collected in three main nurseries of the Gulf of Lions (GoL) (Thau, Mauguio and Berre). We investigated the spatial variation in the origin of the sole larvae which colonised the nurseries around the GoL, and whether temporal differences in environmental conditions during this life stage affected growth and larval life duration. The hatching period ranges from October to March, depending on year and site. Average ages at metamorphosis varied between 43 and 50 days, with the lowest and highest values consistently found for Mauguio and Berre, respectively. Otolith growth rates ranged between 2.7 and 3.2 μm d−1, with the lowest values in Thau and Mauguio and the highest in Berre. Otolith chemical composition during the larval life also varied, suggesting contrasted larval environmental histories in YOY among nurseries. In fishes from Berre and Mauguio, larval life was more influenced by the Rhône River, showing consistently higher larval Ba:Ca ratios (10/23 μmol mol−1) and lower δ13C (−6.5/−6.1‰) and δ18O values (−1.6/0.1‰) than for Thau (with Ba:Ca ratios < 8 μmol mol−1, δ13C ∼−2.3‰ and δ18O ∼1.5‰). Differences in larval otolith composition were observed for 2004, with higher Ba:Ca and lower δ13C and δ18O values than in the two other years. These differences were explained by changes in composition and chemical signatures of water masses after an exceptional flooding event of the Rhône River in late 2003.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Estuarine, Coastal and Shelf Science - Volume 149, 5 August 2014, Pages 194-202
نویسندگان
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