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  • 2000-2004  (2)
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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science, Ltd
    Aquaculture research 32 (2001), S. 0 
    ISSN: 1365-2109
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: In most vertebrates, the β-oxidation of long-chain fatty acids is stimulated by the presence of l-carnitine, which allows long-chain acyl-CoA-esters to cross the mitochondrial membrane. A study was undertaken to investigate the possible effects of supplemental dietary l-carnitine on the growth, tissue lipid content and activity of hepatic acetyl coenzyme-A carboxylase (ACoAC) in the European seabass (Dicentrarchus labrax). Four isoproteic (42% crude protein), isolipidic (19% crude fat) and isoenergetic (21.5 kJ g−1) diets were formulated to contain increasing levels of carnitine (0.3, 1.1, 2.0 and 3.0 g kg−1). Triplicate groups of 25 seabass (mean body weight: 250 g) were grown in seawater (temperature: 20 °C; salinity: 35 ppt) over 85 days. At the end of the growth study, whole body, liver, viscera, gonads, muscle and plasma samples were withdrawn for analyses. Dietary l-carnitine supplementation did not significantly affect weight gain, feed efficiency or protein utilisation. At the end of the experimental period, the whole body composition of fish did not differ significantly between experimental treatments. Similarly, neither total plasma triacylglycerols and cholesterol levels nor tissue lipid content were affected by the dietary l-carnitine supplementation. By contrast, fish fed the l-carnitine supplemented diets showed a three-fold increase in the activity of ACoAC, suggesting higher rates of lipogenesis in seabass liver. The overall results show that supplemental dietary l-carnitine is not suitable for reducing fat deposition in seabass fed high-fat diets.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A progradational sedimentary body, the infralittoral prograding wedge (IPW), has been developing from the mean fair-weather wave-base level to the storm wave-base level between the onshore (beach) and the offshore (inner continental shelf) depositional zones along the Spanish coast during the Late Holocene. The main sedimentary body is composed of large inclined master beds which prograde seawards parallel to the shoreline, formed by sediments swept offshore by waves from shallow-water littoral environments. The inclined beds downlap onto finer-grained offshore sediments and, in turn, are overlain by shoreface deposits. The IPW is generated by downwelling storm currents and associated seaward transport of sediment. It represents a new depositional model for clastic wave-dominated coasts, and its identification requires a new subdivision of the nearshore environment.
    Type of Medium: Electronic Resource
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