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首页> 外文期刊>The ISME journal emultidisciplinary journal of microbial ecology >Nitrogen fixation in distinct microbial niches within a chemoautotrophy-driven cave ecosystem
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Nitrogen fixation in distinct microbial niches within a chemoautotrophy-driven cave ecosystem

机译:化学自养驱动的洞穴生态系统内不同微生物区域的固氮作用

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摘要

Microbial sulfur and carbon cycles in ecosystems driven by chemoautotrophy - present at deep-sea hydrothermal vents, cold seeps and sulfidic caves - have been studied to some extent, yet little is known about nitrogen fixation in these systems. Using a comprehensive approach comprising of 15 N 2 isotope labeling, acetylene reduction assay and nitrogenase gene expression analyses, we investigated nitrogen fixation in the sulfide-rich, chemoautotrophy-based Frasassi cave ecosystem (Italy). Nitrogen fixation was examined in three different microbial niches within the cave waters: (1) symbiotic bacterial community of Niphargus amphipods, (2) Beggiatoa-dominated biofilms, which occur at the sulfide-oxygen interface, and (3) sulfidic sediment. We found evidence for nitrogen fixation in all the three niches, and the nitrogenase gene (homologs of nifH) expression data clearly show niche differentiation of diazotrophic Proteobacteria within the water streams. the nifH transcript originated from the symbiotic community of Niphargus amphipods might belong to the thiothrix ectosymbionts. Two abundantly expressed nifH genes in the Beggiatoa-dominated biofilms are closely related to those from Beggiatoa- and Desulfovibrio-related bacteria. these two diazotrophs were consistently found in Beggiatoa-dominated biofilms collected at various time points, thus illustrating species-specific associations of the diazotrophs in biofilm formation, and micron-scale niche partitioning of sulfur-oxidizing and sulfate-reducing bacteria driven by steep redox gradients within the biofilm. Finally, putative heterotrophs (Geobacter, Azoarcus and Desulfovibrio related) were the active diazotrophs in the sulfidic sediment. Our study is the first to shed light on nitrogen fixation in permanently dark caves and suggests that diazotrophy may be widespread in chemosynthetic communities.
机译:在深海热液喷口,冷渗漏和硫化物洞穴中存在的由化学自养作用驱动的生态系统中的微生物硫和碳循环已得到一定程度的研究,但对这些系统中的固氮知之甚少。使用包括15 N 2同位素标记,乙炔还原测定和固氮酶基因表达分析的综合方法,我们研究了富硫,基于化学自养作用的Frasassi洞穴生态系统(意大利)中的固氮作用。在洞穴水域的三个不同的微生物生态位中检测了固氮作用:(1)食蟹纲双足动物的共生细菌群落;(2)生于乙藻的生物膜,该生物膜发生在硫化物-氧气的界面上;(3)硫化物沉积物。我们发现在所有三个生态位中都存在固氮的证据,而固氮酶基因(nifH的同源物)表达数据清楚地表明了水流中重氮营养菌的生态位分化。源自Niphargus amphipods的共生群落的nifH转录本可能属于thiothrix ectosymbionts。 Beggiatoa为主的生物膜中两个大量表达的nifH基因与Beggiatoa和Desulfovibrio相关细菌的基因密切相关。这两个重氮营养体在各个时间点收集的以贝格托亚为主的生物膜中始终存在,从而说明了重氮营养体在生物膜形成中的物种特异性关联,以及由陡峭的氧化还原梯度驱动的硫氧化细菌和硫酸盐还原细菌的微米级生态位分配。在生物膜中。最后,推定的异养生物(与土壤杆菌,固氮菌和脱硫弧菌有关)是硫化沉积物中的活性重氮营养菌。我们的研究首次揭示了永久性黑暗洞穴中的固氮作用,并表明重氮营养作用可能在化学合成群落中广泛分布。

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