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Temporal dynamics of allochthonous coarse particulate organic matter in a subtropical Atlantic rainforest Brazilian stream

机译:亚热带大西洋雨林巴西河流中异质粗颗粒有机物的时间动态

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Allochthonous organic matter is a major energy source for headwater stream ecosystems. Therefore, examinations of how energy flows throughout these streams requires knowledge of mechanisms driving leaf input, retention and export. In this study we quantified the major input pathways and retention dynamics of coarse particulate organic matter (CPOM) in an Atlantic Rainforest stream in southern Brazil. We hypothesised that much of the temporal variability in the CPOM budget would be driven by precipitation, and thus we focus especially on the importance of vertical v. lateral input pathways, precipitation-driven inputs v. stocks, and composition of CPOM throughout 1 year. Most leaf litter entered the stream by the lateral input pathway (70.5gm(-2)month(-1)+/- 108s.d.) compared with the vertical (32.4gm(-2) month(-1) +/- 17.5s.d.), and lateral input was correlated with precipitation and bank slope. In addition, torrential rainfall caused a net decrease in CPOM by reduction in the benthic stocks. Finally, six species represented 52.9% of total leaf input, where the most important (similar to 25% of total input) was Schizolobium parahyba. Overall, this research confirms our prediction that the CPOM budget of this Atlantic Rainforest stream is driven in large part by precipitation.
机译:异源有机质是上游水域生态系统的主要能源。因此,要检查能量如何在这些流中流动,需要了解驱动叶片输入,保留和输出的机制。在这项研究中,我们量化了巴西南部大西洋雨林溪流中粗颗粒有机物(CPOM)的主要输入途径和保留动态。我们假设CPOM预算中的大部分时间变化都是由降水驱动的,因此,我们特别关注垂直v。横向投入途径,降水驱动的投入v。库存和CPOM在整个1年中的重要性。与垂直输入(32.4gm(-2)month(-1)+/-相比,大多数叶子凋落物通过侧向输入途径(70.5gm(-2)month(-1)+/- 108s.d.)进入河流。 17.5sd),并且横向输入与降水和河岸坡度相关。此外,暴雨导致底栖动物种群减少,导致CPOM净减少。最后,六个物种占叶总输入量的52.9%,其中最重要的(约占叶总输入量的25%)是副气生双歧杆菌。总体而言,这项研究证实了我们的预测,即该大西洋雨林溪流的CPOM预算很大程度上是由降水驱动的。

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