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Peatland Microbial Communities and Decomposition Processes in the James Bay Lowlands Canada

机译:加拿大詹姆斯湾低地的泥炭地微生物群落和分解过程

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摘要

Northern peatlands are a large repository of atmospheric carbon due to an imbalance between primary production by plants and microbial decomposition. The James Bay Lowlands (JBL) of northern Ontario are a large peatland-complex but remain relatively unstudied. Climate change models predict the region will experience warmer and drier conditions, potentially altering plant community composition, and shifting the region from a long-term carbon sink to a source. We collected a peat core from two geographically separated (ca. 200 km) ombrotrophic peatlands (Victor and Kinoje Bogs) and one minerotrophic peatland (Victor Fen) located near Victor Bog within the JBL. We characterized (i) archaeal, bacterial, and fungal community structure with terminal restriction fragment length polymorphism of ribosomal DNA, (ii) estimated microbial activity using community level physiological profiling and extracellular enzymes activities, and (iii) the aeration and temperature dependence of carbon mineralization at three depths (0–10, 50–60, and 100–110 cm) from each site. Similar dominant microbial taxa were observed at all three peatlands despite differences in nutrient content and substrate quality. In contrast, we observed differences in basal respiration, enzyme activity, and the magnitude of substrate utilization, which were all generally higher at Victor Fen and similar between the two bogs. However, there was no preferential mineralization of carbon substrates between the bogs and fens. Microbial community composition did not correlate with measures of microbial activity but pH was a strong predictor of activity across all sites and depths. Increased peat temperature and aeration stimulated CO2 production but this did not correlate with a change in enzyme activities. Potential microbial activity in the JBL appears to be influenced by the quality of the peat substrate and the presence of microbial inhibitors, which suggests the existing peat substrate will have a large influence on future JBL carbon dynamics.
机译:由于植物的初级生产和微生物分解之间的不平衡,北部的泥炭地是大气碳的大型储存库。安大略省北部的詹姆士湾低地(JBL)是一个大型泥炭地,但仍未研究。气候变化模型预测,该地区将经历更加干燥的气候,可能会改变植物群落的组成,并将该地区从长期的碳汇转变为碳源。我们从JBL的Victor Bog附近的两个地理分离(约200千米)的非营养泥炭地(Victor和Kinoje Bogs)和一个中营养泥炭地(Victor Fen)收集了一个泥炭核心。我们表征(i)具有核糖体DNA的末端限制性片段长度多态性的古细菌,细菌和真菌群落结构,(ii)使用群落水平的生理谱和细胞外酶活性估算微生物活性,以及​​(iii)碳的通气和温度依赖性每个站点的三个深度(0-10、50-60和100-110–cm)的矿化作用。尽管养分含量和底物质量存在差异,但在所有三个泥炭地均观察到相似的优势微生物分类群。相反,我们观察到了基础呼吸,酶活性和底物利用率的差异,这些差异在维克多·芬(Victor Fen)处通常更高,在两个沼泽之间相似。但是,在沼泽和之间没有优先沉积碳底物的现象。微生物群落组成与微生物活性的测量值不相关,但pH值是所有位点和深度的活性的强烈预测指标。升高的泥炭温度和通气刺激了CO2的产生,但这与酶活性的变化无关。 JBL中潜在的微生物活性似乎受泥炭基质质量和微生物抑制剂的存在影响,这表明现有的泥炭基质将对未来的JBL碳动力学产生很大影响。

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