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首页> 外文期刊>Marine ecology progress series >Benthic foraminiferal community changes and their relationship to environmental dynamics in intertidal muddy sediments (Bay of Cádiz, SW Spain)
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Benthic foraminiferal community changes and their relationship to environmental dynamics in intertidal muddy sediments (Bay of Cádiz, SW Spain)

机译:潮间带泥质沉积物的底栖有孔虫群落变化及其与环境动力学的关系(西班牙西南加的斯湾)

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ABSTRACT: The temporal and vertical variability of live intertidal benthic foraminifera was studied in parallel to environmental variables such as porewater and overlying water nutrients, salinity, temperature, sedimentary pigments and organic carbon. About 80% of benthic foraminifera were concentrated in the upper 0-4 mm sediment layer, which was also the maximum oxygen penetration depth under light conditions as determined by oxygen microsensor measurements. Significant changes in the composition of the foraminiferal community over the course of the study were found in the surface layer (0-2 mm), whereas no differences were detected in the deepest sediment layers (10-30 mm). Univariate measures, such as abundance, species richness and diversity showed few differences over time and little relation to environmental variables. On the other hand, multivariate regression analysis for the whole community assemblage showed that the significant community composition changes over time in the surface layer could be related to fluctuations of several environmental variables, mainly those related to sediment food availability. The macroalgal bloom that occurred during the winter months had no detectable effect on benthic foraminiferal abundance or community patterns. Overall, the intertidal foraminiferal community in the Bay of Cádiz showed a highly dynamic character and a clear vertical distribution which could be effectively captured by studying the uppermost sediment layer at sub-centimetric vertical resolution.
机译:摘要:研究了潮间带底栖有孔虫的时间和垂直变化,并与环境变量(例如孔隙水和上层水养分,盐度,温度,沉积色素和有机碳)平行进行了研究。大约80%的底栖有孔虫集中在上部的0-4 mm沉积层中,这也是通过氧气微传感器测量确定的在光照条件下的最大氧气渗透深度。在研究过程中,有孔虫群落组成的显着变化在表层(0-2 mm)中发现,而在最深的沉积物层(10-30 mm)中没有发现差异。诸如丰度,物种丰富度和多样性之类的单变量测度显示,随着时间的推移几乎没有差异,并且与环境变量之间的关系也很小。另一方面,对整个群落组合的多元回归分析表明,表层的群落组成随时间的显着变化可能与几个环境变量的波动有关,主要是与沉积物食物的可获得性有关。冬季发生的大型藻华对底栖有孔虫的数量或群落格局没有可检测的影响。总体而言,加的斯湾的潮间带孔虫群落表现出高度的动态特征和清晰的垂直分布,可以通过研究亚厘米垂直分辨率下的最上层沉积物来有效地捕捉到。

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