S.N. Winogradsky Institute of Microbiology, Russian Academy of Sciences, Moscow 117312, Russia.
Environ Microbiol. 2011 Jul;13(7):1800-14. doi: 10.1111/j.1462-2920.2011.02491.x. Epub 2011 May 12.
Northern peatlands represent a major global carbon store harbouring approximately one-third of the global reserves of soil organic carbon. A large proportion of these peatlands consists of acidic Sphagnum-dominated ombrotrophic bogs, which are characterized by extremely low rates of plant debris decomposition. The degradation of cellulose, the major component of Sphagnum-derived litter, was monitored in long-term incubation experiments with acidic (pH 4.0) peat extracts. This process was almost undetectable at 10°C and occurred at low rates at 20°C, while it was significantly accelerated at both temperature regimes by the addition of available nitrogen. Cellulose breakdown was only partially inhibited in the presence of cycloheximide, suggesting that bacteria participated in this process. We aimed to identify these bacteria by a combination of molecular and cultivation approaches and to determine the factors that limit their activity in situ. The indigenous bacterial community in peat was dominated by Alphaproteobacteria and Acidobacteria. The addition of cellulose induced a clear shift in the community structure towards an increase in the relative abundance of the Bacteroidetes. Increasing temperature and nitrogen availability resulted in a selective development of bacteria phylogenetically related to Cytophaga hutchinsonii (94-95% 16S rRNA gene sequence similarity), which densely colonized microfibrils of cellulose. Among isolates obtained from this community only some subdivision 1 Acidobacteria were capable of degrading cellulose, albeit at a very slow rate. These Acidobacteria represent indigenous cellulolytic members of the microbial community in acidic peat and are easily out-competed by Cytophaga-like bacteria under conditions of increased nitrogen availability. Members of the phylum Firmicutes, known to be key players in cellulose degradation in neutral habitats, were not detected in the cellulolytic community enriched at low pH.
北方泥炭地是全球主要的碳储存库之一,大约储存了全球土壤有机碳储量的三分之一。这些泥炭地中有很大一部分是由酸性的以泥炭藓为主的腐生沼泽组成,其植物残体分解的速度极慢。在含有酸性(pH4.0)泥炭提取物的长期培养实验中,监测了纤维素的降解情况,纤维素是泥炭藓衍生凋落物的主要成分。在 10°C 时,这个过程几乎无法检测到,在 20°C 时,其分解速度较低,而添加有效氮可显著加速这一过程。在存在环己酰亚胺的情况下,纤维素的分解仅部分受到抑制,这表明细菌参与了这一过程。我们旨在通过分子和培养相结合的方法来鉴定这些细菌,并确定限制其在原位活性的因素。泥炭中的土著细菌群落主要由α变形菌门和酸杆菌门组成。添加纤维素后,群落结构明显向细菌的相对丰度增加转变,而细菌的相对丰度增加与拟杆菌门有关。增加温度和氮的有效性导致与 Cytophaga hutchinsonii(16S rRNA 基因序列相似度为 94-95%)具有亲缘关系的细菌选择性地发展,它们密集地定殖于纤维素的微纤维上。从这个群落中获得的分离株中,只有一些酸杆菌门的亚类 1 能够降解纤维素,尽管速度非常缓慢。这些酸杆菌代表了酸性泥炭微生物群落中土著的纤维素降解成员,在氮有效性增加的条件下,它们很容易被 Cytophaga 样细菌所竞争。在中性生境中降解纤维素的关键成员厚壁菌门,在低 pH 值条件下富集的纤维素降解群落中并未检测到。