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首页> 外文期刊>Global change biology >Effects of short- and long-term water-level drawdown on the populations and activity of aerobic decomposers in a boreal peatland
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Effects of short- and long-term water-level drawdown on the populations and activity of aerobic decomposers in a boreal peatland

机译:短期和长期水位下降对北方泥炭地种群和需氧分解物活性的影响

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摘要

We analysed the response of microbial communities, characterized by phospholipid fatty acids (PLFAs), to changing hydrological conditions at sites with different nutrient levels in a southern boreal peatland. Although PLFAs of Gram-negative bacteria were characteristic of the peatland complex, microbial communities differed among sites (ombrotrophic bog, oligotrophic fen, mesotrophic fen) and sampling depths (0-5, 5-10, 10-20, 20-30 cm). The microbial communities in each site changed significantly following water-level drawdown. The patterns of change varied among sites and sampling depths. The relative proportion of Gram-negative bacteria decreased in the upper 10 cm but increased in deeper layers of the fen sites. Fungi benefited from water-level drawdown in the upper 5 cm of the mesotrophic fen, but suffered in the drier surfaces of the ombrotrophic bog, especially in the 5-10 cm layer. In contrast, actinobacteria suffered from water-level drawdown in the mesotrophic fen, but benefited in the drier surfaces of the ombrotrophic bog. Basal respiration rate correlated positively with pH and fungal PLFA, and negatively with depth. We suggest that the changes in microbial community structure after persistent water-level drawdown follow not only the hydrological conditions but also the patterns of vegetation change. Our results imply that changes in structure and activity of the microbial community in response to climate change will be strongly dependent on the type of peatland.
机译:我们分析了以南方地区泥炭地不同养分水平为特征的,以磷脂脂肪酸(PLFAs)为特征的微生物群落对水文条件变化的响应。尽管革兰氏阴性菌的PLFA是泥炭地复合体的特征,但微生物群落在位点(营养缺陷型沼泽,贫营养型,中营养型)和采样深度(0-5、5-10、10-20、20-30 cm)之间有所不同。水位下降后,每个站点的微生物群落发生了显着变化。变化的模式因地点和采样深度而异。革兰氏阴性菌的相对比例在上部10 cm处降低,但在the部位的较深层增加。真菌得益于中营养上部5 cm的水位下降,但真菌在营养缺陷沼泽的较干燥表面受苦,特别是在5-10 cm的层中。相比之下,放线菌在中营养的芬中遭受水位下降,但在营养养护的较干燥表面受益。基础呼吸速率与pH和真菌PLFA呈正相关,与深度呈负相关。我们认为,持续水位下降后微生物群落结构的变化不仅遵循水文条件,而且还遵循植被变化的模式。我们的结果表明,响应气候变化的微生物群落结构和活性的变化将强烈取决于泥炭地的类型。

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