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高寒溪流中微生物有机质的利用:关键酶控机制。

Microbial Organic Matter Utilization in High-Arctic Streams: Key Enzymatic Controls.

机构信息

Department of Bioscience, Aarhus University, Ole Worms Allé 1, Aarhus, Denmark.

Catalan Institute for Water Research (ICRA), Girona, Spain.

出版信息

Microb Ecol. 2019 Oct;78(3):539-554. doi: 10.1007/s00248-019-01330-w. Epub 2019 Feb 10.

Abstract

In the Arctic, climate changes contribute to enhanced mobilization of organic matter in streams. Microbial extracellular enzymes are important mediators of stream organic matter processing, but limited information is available on enzyme processes in this remote area. Here, we studied the variability of microbial extracellular enzyme activity in high-Arctic fluvial biofilms. We evaluated 12 stream reaches in Northeast Greenland draining areas exhibiting different geomorphological features with contrasting contents of soil organic matter to cover a wide range of environmental conditions. We determined stream nitrogen, phosphorus, and dissolved organic carbon concentrations, quantified algal biomass and bacterial density, and characterized the extracellular enzyme activities involved in catalyzing the cleavage of a range of organic matter compounds (e.g., β-glucosidase, phosphatase, β-xylosidase, cellobiohydrolase, and phenol oxidase). We found significant differences in microbial organic matter utilization among the study streams draining contrasting geomorphological features, indicating a strong coupling between terrestrial and stream ecosystems. Phosphatase and phenol oxidase activities were higher in solifluction areas than in alluvial areas. Besides dissolved organic carbon, nitrogen availability was the main driver controlling enzyme activities in the high-Arctic, which suggests enhanced organic matter mineralization at increased nutrient availability. Overall, our study provides novel information on the controls of organic matter usage by high-Arctic stream biofilms, which is of high relevance due to the predicted increase of nutrient availability in high-Arctic streams in global climate change scenarios.

摘要

在北极地区,气候变化导致溪流中有机物质的迁移增强。微生物胞外酶是溪流有机物质处理的重要调节剂,但关于这个偏远地区酶过程的信息有限。在这里,我们研究了高北极河流生物膜中微生物胞外酶活性的可变性。我们评估了格陵兰东北部的 12 个溪流流域,这些流域具有不同的地貌特征,土壤有机物质含量不同,以覆盖广泛的环境条件。我们测定了溪流中的氮、磷和溶解有机碳浓度,量化了藻类生物量和细菌密度,并表征了参与催化一系列有机物质化合物(如β-葡萄糖苷酶、磷酸酶、β-木糖苷酶、纤维二糖水解酶和酚氧化酶)裂解的胞外酶活性。我们发现,具有不同地貌特征的研究溪流之间的微生物有机物质利用存在显著差异,这表明陆地和溪流生态系统之间存在强烈的耦合。在融雪区,磷酸酶和酚氧化酶的活性高于冲积扇区。除了溶解有机碳,氮的可利用性是控制北极地区酶活性的主要驱动因素,这表明在增加养分供应的情况下,有机物质的矿化作用增强。总的来说,我们的研究提供了关于高北极溪流生物膜对有机物质利用的控制的新信息,由于在全球气候变化情景中高北极溪流中养分供应的预测增加,这具有很高的相关性。

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