A Novel Enrichment Culture Highlights Core Features of Microbial Networks Contributing to Autotrophic Fe(II) Oxidation Coupled to Nitrate Reduction.

Pub Date : 2021-01-01 Epub Date: 2021-07-02 DOI:10.1159/000517083
Yu-Ming Huang, Daniel Straub, Andreas Kappler, Nicole Smith, Nia Blackwell, Sara Kleindienst
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引用次数: 14

Abstract

Fe(II) oxidation coupled to nitrate reduction (NRFO) has been described for many environments. Yet very few autotrophic microorganisms catalysing NRFO have been cultivated and their diversity, as well as their mechanisms for NRFO in situ remain unclear. A novel autotrophic NRFO enrichment culture, named culture BP, was obtained from freshwater sediment. After more than 20 transfers, culture BP oxidized 8.22 mM of Fe(II) and reduced 2.42 mM of nitrate within 6.5 days under autotrophic conditions. We applied metagenomic, metatranscriptomic, and metaproteomic analyses to culture BP to identify the microorganisms involved in autotrophic NRFO and to unravel their metabolism. Overall, twelve metagenome-assembled genomes (MAGs) were constructed, including a dominant Gallionellaceae sp. MAG (≥71% relative abundance). Genes and transcripts associated with potential Fe(II) oxidizers in culture BP, identified as a Gallionellaceae sp., Noviherbaspirillum sp., and Thiobacillus sp., were likely involved in metal oxidation (e.g., cyc2, mtoA), denitrification (e.g., nirK/S, norBC), carbon fixation (e.g., rbcL), and oxidative phosphorylation. The putative Fe(II)-oxidizing protein Cyc2 was detected for the Gallionellaceae sp. Overall, a complex network of microbial interactions among several Fe(II) oxidizers and denitrifiers was deciphered in culture BP that might resemble NRFO mechanisms in situ. Furthermore, 16S rRNA gene amplicon sequencing from environmental samples revealed 36 distinct Gallionellaceae taxa, including the key player of NRFO from culture BP (approx. 0.13% relative abundance in situ). Since several of these in situ-detected Gallionellaceae taxa were closely related to the key player in culture BP, this suggests that the diversity of organisms contributing to NRFO might be higher than currently known.

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一种新的富集培养强调了促进自养铁(II)氧化和硝酸盐还原的微生物网络的核心特征。
铁(II)氧化耦合硝酸盐还原(NRFO)已经描述了许多环境。然而,很少有自养微生物催化NRFO被培养出来,它们的多样性以及它们对原位NRFO的机制仍然不清楚。从淡水沉积物中获得了一种新的自养型NRFO富集培养物,命名为BP培养物。在自养条件下,经过20多次转移,培养BP在6.5天内氧化了8.22 mM的铁(II),减少了2.42 mM的硝酸盐。我们应用元基因组学、元转录组学和元蛋白质组学分析培养BP,以鉴定参与自养NRFO的微生物并揭示其代谢。总体而言,共构建了12个宏基因组组装基因组(MAGs),其中Gallionellaceae sp. MAG具有优势(相对丰度≥71%)。BP培养基中与潜在的铁(II)氧化剂相关的基因和转录物,鉴定为Gallionellaceae sp., Noviherbaspirillum sp.和Thiobacillus sp.,可能涉及金属氧化(如cyc2, mtoA),反硝化(如nirK/S, norBC),碳固定(如rbcL)和氧化磷酸化。在Gallionellaceae sp.中检测到假定的铁(II)氧化蛋白Cyc2。总的来说,在培养BP中,几种铁(II)氧化剂和反硝化剂之间的复杂微生物相互作用网络被破解,可能类似于原位NRFO机制。此外,来自环境样品的16S rRNA基因扩增子测序显示了36个不同的Gallionellaceae分类群,其中包括来自培养BP的NRFO关键角色(约为1 / 4)。原位相对丰度0.13%)。由于这些原位检测到的Gallionellaceae分类群与培养BP的关键参与者密切相关,这表明参与NRFO的生物多样性可能比目前已知的要高。
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