Hori Tomoyuki, Aoyagi Tomo, Itoh Hideomi, Narihiro Takashi, Oikawa Azusa, Suzuki Kiyofumi, Ogata Atsushi, Friedrich Michael W, Conrad Ralf, Kamagata Yoichi
Environmental Management Research Institute, National Institute of Advanced Industrial Science and Technology Tsukuba, Japan.
Bioproduction Research Institute, National Institute of Advanced Industrial Science and Technology Sapporo, Japan.
Front Microbiol. 2015 May 5;6:386. doi: 10.3389/fmicb.2015.00386. eCollection 2015.
Reduction of crystalline Fe(III) oxides is one of the most important electron sinks for organic compound oxidation in natural environments. Yet the limited number of isolates makes it difficult to understand the physiology and ecological impact of the microorganisms involved. Here, two-stage cultivation was implemented to selectively enrich and isolate crystalline iron(III) oxide reducing microorganisms in soils and sediments. Firstly, iron reducers were enriched and other untargeted eutrophs were depleted by 2-years successive culture on a crystalline ferric iron oxide (i.e., goethite, lepidocrocite, hematite, or magnetite) as electron acceptor. Fifty-eight out of 136 incubation conditions allowed the continued existence of microorganisms as confirmed by PCR amplification. High-throughput Illumina sequencing and clone library analysis based on 16S rRNA genes revealed that the enrichment cultures on each of the ferric iron oxides contained bacteria belonging to the Deltaproteobacteria (mainly Geobacteraceae), followed by Firmicutes and Chloroflexi, which also comprised most of the operational taxonomic units (OTUs) identified. Venn diagrams indicated that the core OTUs enriched with all of the iron oxides were dominant in the Geobacteraceae while each type of iron oxides supplemented selectively enriched specific OTUs in the other phylogenetic groups. Secondly, 38 enrichment cultures including novel microorganisms were transferred to soluble-iron(III) containing media in order to stimulate the proliferation of the enriched iron reducers. Through extinction dilution-culture and single colony isolation, six strains within the Deltaproteobacteria were finally obtained; five strains belonged to the genus Geobacter and one strain to Pelobacter. The 16S rRNA genes of these isolates were 94.8-98.1% identical in sequence to cultured relatives. All the isolates were able to grow on acetate and ferric iron but their physiological characteristics differed considerably in terms of growth rate. Thus, the novel strategy allowed to enrich and isolate novel iron(III) reducers that were able to thrive by reducing crystalline ferric iron oxides.
结晶态铁(III)氧化物的还原是自然环境中有机化合物氧化最重要的电子汇之一。然而,分离菌株数量有限,使得难以了解相关微生物的生理学特性和生态影响。在此,实施两阶段培养以选择性富集和分离土壤及沉积物中可还原结晶态铁(III)氧化物的微生物。首先,以结晶态三价铁氧化物(即针铁矿、纤铁矿、赤铁矿或磁铁矿)作为电子受体,通过两年连续培养来富集铁还原菌,并去除其他非目标富营养菌。136个培养条件中有58个能使微生物持续存在,这通过PCR扩增得以证实。基于16S rRNA基因的高通量Illumina测序和克隆文库分析表明,每种三价铁氧化物上的富集培养物都含有属于δ-变形菌纲(主要是地杆菌科)的细菌,其次是厚壁菌门和绿弯菌门,这些细菌也构成了大多数已鉴定的操作分类单元(OTU)。维恩图表明,所有铁氧化物富集的核心OTU在地杆菌科中占主导地位,而每种类型的铁氧化物选择性地补充了其他系统发育组中特异性富集的OTU。其次,将包括新微生物在内的38种富集培养物转移到含可溶性铁(III)的培养基中,以刺激富集的铁还原菌增殖。通过灭绝稀释培养和单菌落分离,最终获得了δ-变形菌纲中的6个菌株;5个菌株属于地杆菌属,1个菌株属于泥杆菌属。这些分离菌株的16S rRNA基因序列与已培养的亲缘菌株的序列一致性为94.8 - 98.1%。所有分离菌株都能在乙酸盐和三价铁上生长,但它们的生理特性在生长速率方面有很大差异。因此,这种新策略能够富集和分离出能够通过还原结晶态三价铁氧化物而茁壮成长的新型铁(III)还原菌。