Preston Michael D, Smemo Kurt A, McLaughlin James W, Basiliko Nathan
Department of Geography, University of Toronto Mississauga Mississauga, ON, Canada.
Front Microbiol. 2012 Feb 29;3:70. doi: 10.3389/fmicb.2012.00070. eCollection 2012.
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 CO(2) 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.
由于植物的初级生产与微生物分解之间的不平衡,北方泥炭地是大气碳的一个大型储存库。安大略省北部的詹姆斯湾低地(JBL)是一个大型泥炭地复合体,但仍相对未被充分研究。气候变化模型预测该地区将经历更温暖和干燥的条件,这可能会改变植物群落组成,并使该地区从一个长期的碳汇转变为碳源。我们从位于JBL内靠近维克托沼泽的两个地理上分开(约200公里)的雨养泥炭地(维克托和基诺杰沼泽)以及一个矿质营养泥炭地(维克托泥炭沼)采集了泥炭芯。我们通过核糖体DNA的末端限制性片段长度多态性来表征(i)古菌、细菌和真菌群落结构,(ii)使用群落水平生理分析和细胞外酶活性来估计微生物活性,以及(iii)在每个地点的三个深度(0 - 10、50 - 60和100 - 110厘米)测定碳矿化的通气和温度依赖性。尽管营养成分和底物质量存在差异,但在所有三个泥炭地都观察到了相似的优势微生物类群。相比之下,我们观察到基础呼吸、酶活性和底物利用程度存在差异,这些在维克托泥炭沼通常更高,而在两个沼泽之间相似。然而,沼泽和泥炭沼之间碳底物没有优先矿化现象。微生物群落组成与微生物活性指标不相关,但pH是所有地点和深度活性的一个强有力的预测因子。泥炭温度和通气增加刺激了CO₂的产生,但这与酶活性的变化不相关。JBL中潜在的微生物活性似乎受泥炭底物质量和微生物抑制剂的存在影响,这表明现有的泥炭底物将对未来JBL的碳动态产生很大影响。