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Biophysical mechanisms of larval fish ingress into Chesapeake Bay

机译:幼鱼进入切萨皮克湾的生物物理机制

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Selective tidal stream transport is hypothesized as a dominant mechanism by which larvae of marine animals move through estuarine openings. For larvae moving from the shelf to estu-arine habitats, selective tidal stream transport proposes that larvae are higher in the water column during flood tide and lower in the water column during ebb tide. Although a number of studies conclude that selective tidal stream transport is the mechanism responsible for larval ingress, few studies consider alternative mechanisms or consider passive explanations for tidal patterns in larval distributions. We examined the biophysical mechanisms responsible for larval ingress into Chesapeake Bay using an Eulerian approach. We made flux calculations for 3 species and partitioned flux estimates among 3 different ingress mechanisms (wind forcing, residual bottom inflow and tidal). For the Atlantic croaker Micropogonias undulatus (Sciaenidae), all 3 mechanisms of ingress contributed to the net up-estuary flux of larvae, but tidal mechanisms become more important for larger sizes. Net up-estuary flux of the Atlantic menhaden Brevoortia tyrannus (Clupeidae) was dominated by residual bottom inflow and wind forcing. Ingress of the summer flounder Paralichthys dentatus (Para-lichthyidae) was dominated by tidal mechanisms, and the importance of tides increased with developmental stage. We found little evidence for the hypothesis that tidal patterns in larval distributions resulted from passive processes (water mass-specific distributions, buoyancy, vertical mixing), thereby supporting the hypothesis that tidal patterns resulted from active behaviors. However, our estimates of vertical mixing were not direct and additional work is needed to examine the role of vertical mixing in influencing vertical distributions in areas with strong tides. We conclude that a combination of wind forcing, residual bottom inflow, and selective tidal stream transport are responsible for the ingress of larval fishes into Chesapeake Bay, and that the relative importance of the 3 mechanisms differs among species and changes with larval development.
机译:选择性潮汐流被认为是海洋动物幼体通过河口开口的主要机制。对于从架子向河口栖息地移动的幼虫,选择性的潮汐流运输提出,在洪潮期间幼虫在水柱中较高,而在退潮期间在水柱中较低。尽管许多研究得出结论,选择性潮汐流运输是造成幼虫进入的机制,但很少有研究考虑替代机制或对幼虫分布中的潮汐模式做出被动解释。我们使用欧拉方法研究了导致幼虫进入切萨皮克湾的生物物理机制。我们对3种物种进行了通量计算,并在3种不同的进入机制(风强迫,残余底部入流和潮汐)之间分配了通量估计值。对于大西洋黄花鱼Micropogonias undulatus(Sciaenidae),所有三种进入机制均对幼虫的净河口净通量作出了贡献,但对于较大的种群,潮汐机制变得更为重要。残余的底部流入和强迫作用主要控制着大西洋捕捞的短尾小BreBrachortia tyrannus(Clupeidae)的河口净通量。夏季比目鱼的入侵是由潮汐机制主导的,潮汐的重要性随着发育阶段的增加而增加。对于这一假说,我们没有发现证据表明幼虫分布中的潮汐模式是由被动过程引起的(特定于水的质量分布,浮力,垂直混合),从而支持了潮汐模式是由主动行为引起的假说。但是,我们对垂直混合的估计不是直接的,需要做更多的工作来检验垂直混合在影响大潮地区垂直分布中的作用。我们得出的结论是,强迫风,残留底流和选择性潮汐流输送共同导致幼体鱼进入切萨皮克湾,并且这三种机制的相对重要性因物种而异,并随幼体发育而变化。

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