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首页> 外文期刊>Estuarine Coastal and Shelf Science >Complex vertical migration of larvae of the ghost shrimp, Nihonotrypaea harmandi, in inner shelf waters of western Kyushu, Japan
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Complex vertical migration of larvae of the ghost shrimp, Nihonotrypaea harmandi, in inner shelf waters of western Kyushu, Japan

机译:在日本九州西部内陆水域中,鬼虾Nihonotrypaea harmandi的幼体复杂的垂直迁移

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The position of meroplanktonic larvae in the water column with depth-dependent current velocities determines horizontal transport trajectories. For those larvae occurring in inner shelf waters, little is known about how combined diel and tidally-synchronized vertical migration patterns shift ontogenet-ically. The vertical migration of larvae of Nihonotrypaea harmandi (Decapoda: Thalassinidea: Callia-nassidae) was investigated in mesotidal, inner shelf waters of western Kyushu, Japan in July-August 2006. The larval sampling at seven depth layers down to 60 m was conducted every 3 h for 36 h in a 68.5-m deep area 10 km off a major coastal adult habitat. Within a 61-65-m deep area 5-7.5 km off the adult habitat, water temperature, salinity, chlorophyll a concentration, and photon flux density were measured, and water currents there were characterized from harmonic analysis of current meter data collected in 2008. The water column was stratified, with pycnocline, chlorophyll a concentration maximum, and 2% of photon flux density at 2 m, recorded at around 22-24 m. The stratified residual currents were detected in their north component, directed offshore and onshore in the upper and lower mixed layers, respectively. More than 87% of larvae occurred between 20 m and 60 m, producing a net onshore transport of approximately 1.3 km d~(-1). At the sunset flooding tide, all zoeal-stage larvae ascended, which could further promote retention (1.4-km potential onshore transport in 3 h). The actual onshore transport of larvae was detected by observing their occurrence pattern in a shallow embayment area with the adult habitat for 24 h in October 1994. However, ontogenetic differences in the vertical migration pattern in inner shelf waters were also apparent, with the maximum mean positions of zoeae deepening with increasing stages. Zoeae I and II performed a reverse diel migration, with their minimum and maximum depths being reached around noon and midnight, respectively. Zoeae IV and V descended continuously. Zoeae III had behaviors that were intermediate to those of the earlier- and later-stage zoeae. Postlarvae underwent a normal diel migration (nocturnal ascent) regardless of tides, with the deepest position (below 60 m and/or on the bottom) during the day. These findings give a new perspective towards how complex vertical migration patterns in meroplanktonic larvae enable their retention in inner shelf waters before the final entry of postlarvae into their natal populations.
机译:浮游生物幼虫在水柱中的位置取决于深度,其流速取决于水流​​的水平。对于那些在内陆架水域中发生的幼虫,关于狄尔和潮汐同步组合的垂直迁移模式是如何从遗传学上转移的,鲜为人知。 2006年7月至8月,在日本九州西部的中生陆内侧陆架水域中调查了Nihonotrypaea harmandi(Decapoda:Thalassinidea:Callia-nassidae)幼虫的垂直迁移。每隔7层深至60 m的幼虫取样。在距离主要沿海成年栖息地10公里的68.5米深的区域中,进行3 h持续36 h。在距成年栖息地5-7.5公里的61-65米深区域内,测量了水温,盐度,叶绿素a浓度和光子通量密度,并根据2008年收集的电流表数据的谐波分析来表征水流水柱被分层,在2 m处有比可可啉,叶绿素的最大浓度和2%的光子通量密度,记录在22-24 m处。分层残余电流在其北部部分被检测到,分别在上,下混合层中定向到近海和陆上。超过87%的幼虫发生在20 m至60 m之间,产生约1.3 km d〜(-1)的净陆上运输。在日落洪水时,所有生长期的幼虫都上升,这可能进一步促进滞留(3小时内有1.4公里的潜在陆上运输)。 1994年10月,通过观察成虫在浅水区与成年栖息地之间的发生模式,可以检测到其在陆地上的实际陆上运输,持续了24 h。但是,在内层架水体中垂直迁移模式的个体发育差异也很明显,最大平均值zoeae的位置随着阶段的增加而加深。 Zoeae I和II进行了反向diel迁移,分别在中午和午夜达到了最小和最大深度。 Zoeae IV和V连续下降。 Zoeae III的行为介于早期和晚期zoeae的中间。幼虫不论潮汐如何都进行正常的di移动(夜间上升),白天的位置最深(60 m以下和/或在底部)。这些发现提供了一个新的观点,认为在浮游幼虫最终进入后代之前,其复杂的垂直迁移模式如何使它们保留在内层架水中。

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