首页> 外文期刊>Annales de Limnologie: International journal of limnology >Hydrochemical and microbiological distinction and function of ombrotrophic peatland lagg as ecotone between Sphagnum peatland and forest catchment (Poleski National Park, eastern Poland)
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Hydrochemical and microbiological distinction and function of ombrotrophic peatland lagg as ecotone between Sphagnum peatland and forest catchment (Poleski National Park, eastern Poland)

机译:泥炭生泥炭地和森林集水区之间非营养共生泥炭地滞后作为过渡带的水化学和微生物学的区别(波兰东部Poleski国家公园)

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摘要

The testate amoeba, ciliate and rotifera communities living in interstitial waters in peatbog in eastern Poland were studied. Sampling was done on a monthly basis from April to November 2007-2008. Microbial communities were examined in a transect including three sites: (1) pine forest (site located 5 m from the lagg/forest contact zone), (2) lagg, (3) open peatbog (the centre of the peatbog). At each of the sites, interstitial water was sampled by means of piezometric wells placed to a depth of 1 m. The species richness and abundance of protozoa and rotifers significantly differed between the studied stations, with the lowest numbers in the pine forest and the highest in the lagg. These differences between macro-habitats may be due to differences in environmental conditions. The distribution of samples in ordination space led to conclude that studied habitats are distributed along the falling gradient of pH and rising gradient of total organic carbon, water table depth and nitrate nitrogen. Assemblages of all three groups showed a strong compositional gradient correlated with water-table depth, conductivity and total phosphorus. However, species composition of ciliates and rotifers was explained by nitrate nitrogen and/or phosphates concentrations. The results suggest that lagg zone of a raised bog can fulfil the function of an ecotone zone, distinguished by a significant increase in biodiversity, abundance and species specificity of micro-organisms. It can also be a place of very efficient matter and energy flow in a peat bog ecosystem.
机译:研究了波兰东部泥炭沼泽间质水域的睾丸变形虫,纤毛虫和轮虫群落。从2007年4月至2008年11月,每月进行一次抽样。在一个包括三个地点的样带中检查了微生物群落:(1)松树林(该地点距落后/森林接触区5 m),(2)落后,(3)开放的泥炭沼泽(泥炭沼泽的中心)。在每个位置,通过置于1 m深度的测压井对间隙水进行采样。在所研究的站之间,原生动物和轮虫的物种丰富度和丰度存在显着差异,其中松树林中的数量最少,而落后者中的数量最多。宏观栖息地之间的这些差异可能是由于环境条件的差异所致。样品在排序空间中的分布得出的结论是,所研究的栖息地沿pH值的下降梯度和总有机碳,地下水位深度和硝酸盐氮的上升梯度分布。所有三组的组合物均显示出与水位深度,电导率和总磷相关的强组成梯度。然而,纤毛虫和轮虫的物种组成由硝酸盐氮和/或磷酸盐的浓度来解释。结果表明,高沼地的滞后带可以实现生态过渡带的功能,其特征在于微生物的生物多样性,丰富度和物种特异性显着增加。它也可以是泥炭沼泽生态系统中非常高效的物质和能量流的地方。

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