Department of Ecological Microbiology, University of Bayreuth, 95440 Bayreuth, Germany.
Environ Microbiol. 2010 Apr;12(4):845-61. doi: 10.1111/j.1462-2920.2009.02128.x. Epub 2009 Dec 27.
Cellulose is the most abundant biopolymer in terrestrial ecosystems and is degraded by microbial communities in soils. However, relatively little is known about the diversity and function of soil prokaryotes that might participate in the overall degradation of this biopolymer. The active cellulolytic and saccharolytic Bacteria in an agricultural soil were evaluated by 16S rRNA (13)C-based stable isotope probing. Cellulose, cellobiose and glucose were mineralized under oxic conditions in soil slurries to carbon dioxide. Under anoxic conditions, these substrates were converted primarily to acetate, butyrate, carbon dioxide, hydrogen and traces of propionate and iso-butyrate; the production of these fermentation end-products was concomitant with the apparent reduction of iron(III). [(13)C]-cellulose was mainly degraded under oxic conditions by novel family-level taxa of the Bacteroidetes and Chloroflexi, and a known family-level taxon of Planctomycetes, whereas degradation under anoxic conditions was facilitated by the Kineosporiaceae (Actinobacteria) and cluster III Clostridiaceae and novel clusters within Bacteroidetes. Active aerobic sub-communities in oxic [(13)C]-cellobiose and [(13)C]-glucose treatments were dominated by Intrasporangiaceae and Micrococcaceae (Actinobacteria) whereas active cluster I Clostridiaceae (Firmicutes) were prevalent in anoxic treatments. A very large number (i.e. 28) of the detected taxa did not closely affiliate with known families, and active Archaea were not detected in any of the treatments. These collective findings suggest that: (i) a large uncultured diversity of soil Bacteria was involved in the utilization of cellulose and products of its hydrolysis, (ii) the active saccharolytic community differed phylogenetically from the active cellulolytic community, (iii) oxygen availability impacted differentially on the activity of taxa and (iv) different redox guilds (e.g. fermenters and iron reducers) compete or interact during cellulose degradation in aerated soils.
纤维素是陆地生态系统中最丰富的生物聚合物,由土壤中的微生物群落降解。然而,对于可能参与这种生物聚合物整体降解的土壤原核生物的多样性和功能,人们知之甚少。通过基于 16S rRNA(13)C 的稳定同位素探测,评估了农业土壤中活跃的纤维素分解菌和糖化菌。在土壤悬浮液中,纤维素、纤维二糖和葡萄糖在好氧条件下矿化生成二氧化碳。在缺氧条件下,这些底物主要转化为乙酸盐、丁酸盐、二氧化碳、氢气和痕量的丙酸盐和异丁酸盐;这些发酵终产物的产生伴随着铁(III)的明显还原。[(13)C]-纤维素主要在好氧条件下被拟杆菌门和绿弯菌门的新型科级分类群以及已知的浮霉菌门的科级分类群降解,而在缺氧条件下,动胶菌科(放线菌)和簇 III 梭菌科以及拟杆菌门内的新簇有利于降解。在有氧[(13)C]-纤维二糖和[(13)C]-葡萄糖处理中,活跃的亚群落主要由 Intrasporangiaceae 和 Micrococcaceae(放线菌)主导,而活跃的簇 I 梭菌科(厚壁菌门)在缺氧处理中更为普遍。检测到的大量(即 28 个)分类群与已知科群没有密切关联,并且在任何处理中都没有检测到活跃的古菌。这些综合发现表明:(i)大量未培养的土壤细菌多样性参与了纤维素及其水解产物的利用;(ii)活跃的糖化群落在系统发育上与活跃的纤维素分解群落不同;(iii)氧气供应对不同分类群的活性有不同的影响;(iv)在通气土壤中,不同的氧化还原菌群(例如发酵菌和铁还原菌)在纤维素降解过程中竞争或相互作用。