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首页> 外文期刊>Marine ecology progress series >Tidal settlement of the intertidal barnacles Chthamalus spp. in SW Portugal: interaction between diel and semi-lunar cycles
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Tidal settlement of the intertidal barnacles Chthamalus spp. in SW Portugal: interaction between diel and semi-lunar cycles

机译:潮间带Chthamalus spp的潮汐沉降。葡萄牙西南部:diel和半月周期之间的相互作用

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Patterns and processes of tidal settlement (within 1 tidal cycle) of Chthamalus spp. in SW Portugal were investigated during the summer of 2003. Settlement patterns in relation to different periods of the day (night and day) and semi-lunar tidal cycles (spring and neap tides) were assessed using artificial plates deployed in intertidal habitats dominated by C. montagui. Settlement of Chthamalus spp. varied at all temporal and spatial scales considered in this study. A strong interaction between diel and semi-lunar tidal cycles was detected. Settlement was higher during diurnal spring tides (afternoon) than during diurnal and nocturnal neap tides (morning and early night) and was lowest during nocturnal spring tides (late night). In order to investigate putative physical mechanisms of shoreward transport to explain our observations, the tidal variability of several physical variables (wind stress, seawater temperature and temperature stratification) was individually investigated and correlated with settlement. Onshore wind stress was positively correlated with settlement, and exhibited the same night/day and tfdal pattern. Onshore wind forcing could be acting as a mechanism promoting intensive larval delivery to the shore in the afternoon (sea breeze) and offshore retention late at night, leading to the high frequency variability patterns observed in barnacle settlement.
机译:Chthamalus spp潮汐沉降的模式和过程(在1个潮汐周期内)。在葡萄牙西南部,于2003年夏季进行了调查。使用部署在以C为主的潮间生境中的人造板,评估了与白天不同时段(夜间和白天)和半月潮周期(春季和午潮)有关的沉降模式。蒙塔吉Chthamalus spp的定居。在本研究中考虑的所有时空尺度上都存在差异。检测到狄尔和半月潮周期之间有很强的相互作用。在日春季潮(下午)期间的沉降高于在日春季和夜间小潮时期(早晨和深夜),而在夜间春季潮(夜间)最低。为了研究假定的上岸运输物理机制来解释我们的观察结果,单独研究了几个物理变量(风应力,海水温度和温度分层)的潮汐变化并将其与沉降相关联。陆上风应力与沉降呈正相关,并且表现出相同的昼夜和tfdal模式。陆上风的强迫作用可能是一种促进机制,促使密集的幼体在下午(海风)被运送到岸上,并在深夜被海上滞留,从而导致在藤壶定居中观察到高频变化模式。

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