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首页> 外文期刊>Marine ecology progress series >Influence of tidal eddies and wind on the distribution of presettlement fishes around One Tree Island, Great Barrier Reef
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Influence of tidal eddies and wind on the distribution of presettlement fishes around One Tree Island, Great Barrier Reef

机译:潮汐涡流和风对大堡礁一树岛周围预设鱼类分布的影响

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Tidally generated eddies that form behind reefs are potentially important physical mechanisms of retention for coral reef fishes during their presettlement phase. The re-circulating properties of eddies may reduce the potential for dispersing fishes to be transported away from settlement habitat and influence patterns of connectivity among adult populations; however, empirical evidence is lacking. We identified the presence of eddies at One Tree Island (OTI) and sampled presettlement fishes in surface waters using a stratified sampling design based on the presence or absence of eddies as predicted from a calibrated hydrodynamic model of the Capricorn-Bunker region. Higher concentrations of presettlement fishes, mostly mullids (goatfishes), were found in the vicinity of the reef in locations where eddies were known to form rather than in locations without eddies, and this was consistent among days and tidal cycles. Locations where eddies were not predicted to form consistently had low concentrations of presettlement fishes. This pattern also occurred under a range of wind strengths and directions. There was evidence for an effect of the windward side of the reef, but areas with eddies maintained high concentrations even when on the leeward side. Higher concentrations were not necessarily found in the eddy itself; rather, they occurred at locations where eddies were predicted to form on the flood or ebb tide. Eddies increase the probability that presettlement fishes will stay near reefs through retention, in some cases their natal reef. Late-stage presettlement fishes are highly mobile and can respond to cues from the reef. Eddies may also increase behavioural interactions among fishes and assist in the detection of reefs that may elicit settlement behaviour.
机译:在珊瑚礁鱼的预设阶段,通过潮汐产生的涡流是珊瑚礁鱼滞留的潜在重要物理机制。涡流的再循环特性可能会降低将鱼类转移出定居点栖息地的可能性,并影响成年种群之间的连通性模式;但是,缺乏经验证据。我们根据摩ri座-邦克地区的校准水动力模型预测的涡流的存在或不存在,使用分层抽样设计,确定了一棵树在岛上(OTI)的涡流并在地表水中取样预设鱼类。在已知形成涡流的地方而不是没有涡流的地方,在珊瑚礁附近发现了较高浓度的预设鱼类,主要是鱼(go鱼),这在几天和潮汐周期中是一致的。预计不会持续形成涡流的位置的预定鱼类的浓度较低。这种模式也发生在一定范围的风强度和风向下。有证据表明,珊瑚礁的迎风面会产生影响,但涡流区域即使在背风面也保持较高的浓度。不一定会在涡流中发现更高的浓度。相反,它们发生在预计在洪水或退潮时会形成涡流的位置。涡流增加了预先定居的鱼类通过保留(在某些情况下是其本生礁)而停留在礁石附近的可能性。后期的预设鱼类移动性强,可以响应珊瑚礁的线索。涡流还可能增加鱼类之间的行为相互作用,并有助于发现可能引起定居行为的珊瑚礁。

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