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Plankton patchiness in the Polar Front region of the West Spitsbergen Shelf

机译:西斯匹次卑尔根大陆架极地锋区的浮游生物斑块

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ABSTRACT: Plankton patchiness, a widely known but poorly studied phenomenon, was investigated concurrently with measurements of environmental conditions in the Polar Front region west of Spitsbergen in summer (June-July) 2012. Continuous high-resolution observations were made using a laser optical plankton counter, a fluorometer and CTD along several sections in the surface 50 m of the sea with additional data from zooplankton net sampling and full-depth range hydrographical measurements at stations. The observed patches differed in terms of size, number and distribution patterns. They occupied only a minor portion of the studied ocean area (2-17%), but contained plankton concentrations that were 3-17 times higher than the concentrations in the background waters. The generation and existence of patches was associated with particular conditions created by increased primary production, optimal hydrography, discontinuities in the density field and/or the presence of meanders or eddies. The distribution of small size fraction patches, consisting of the phytoplankton, inorganic particles and detritus, was closely related to specific patterns in hydrography. The medium-size zooplankton and marine snow were concentrated mainly in conjunction with discontinuities in density field. The distribution of the large copepods was independent of any oceanographic feature detected in this study, which points towards biological cues as factors regulating zooplankton aggregation processes. Diverse mechanisms of patch formation as well as their ecological significance are discussed in the context of planktonic responses to the structured environment in the region of the Polar Front.
机译:摘要:2012年夏季(6月至7月),在斯匹次卑尔根以西的极地锋地区与浮游生物的斑块现象进行了调查,同时对环境条件进行了测量。使用激光光学浮游生物进行了连续的高分辨率观测。计数器,荧光计和CTD沿着海面50 m的多个部分,并具有浮游动物网采样和站点全深度水文测量的额外数据。观察到的斑块在大小,数量和分布方式方面有所不同。它们仅占研究海洋面积的一小部分(2-17%),但浮游生物的浓度比背景水的浓度高3-17倍。斑块的产生和存在与特定的条件有关,这些条件是由初级产量增加,最佳水文学,密度场的不连续性和/或曲折或涡流的存在而产生的。由浮游植物,无机颗粒和碎屑组成的小尺寸斑块的分布与水文学中的特定模式密切相关。中型浮游动物和海洋积雪主要集中在密度场的不连续性上。大型co足类的分布与本研究中检测到的任何海洋学特征均无关,这表明生物学线索是调节浮游动物聚集过程的因素。在极地地区对结构化环境的浮游反应中,讨论了斑块形成的各种机制及其生态意义。

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