Swedish University of Agricultural Sciences, Department of Forest Mycology and Plant Pathology, Uppsala, Sweden.
Microbiol Spectr. 2023 Jun 15;11(3):e0006123. doi: 10.1128/spectrum.00061-23. Epub 2023 May 24.
The microbial process of denitrification is the primary source of the greenhouse gas nitrous oxide (NO) from terrestrial ecosystems. Fungal denitrifiers, unlike many bacteria, lack the NO reductase, and thereby are sources of NO. Still, their diversity, global distribution, and environmental determinants, as well as their relative importance, compared to bacterial and archaeal denitrifiers, remain unresolved. Employing a phylogenetically informed approach to analyze 1,980 global soil and rhizosphere metagenomes for the denitrification marker gene , which codes for the copper dependent nitrite reductase in denitrification, we show that fungal denitrifiers are sparse, yet cosmopolitan and that they are dominated by saprotrophs and pathogens. Few showed biome-specific distribution patterns, although members of the Fusarium oxysporum species complex, which are known to produce substantial amounts of NO, were proportionally more abundant and diverse in the rhizosphere than in other biomes. Fungal denitrifiers were most frequently detected in croplands, but they were most abundant in forest soils when normalized to metagenome size. Nevertheless, the overwhelming dominance of bacterial and archaeal denitrifiers suggests a much lower fungal contribution to NO emissions than was previously estimated. In relative terms, they could play a role in soils that are characterized by a high carbon to nitrogen ratio and a low pH, especially in the tundra as well as in boreal and temperate coniferous forests. Because global warming predicts the proliferation of fungal pathogens, the prevalence of potential plant pathogens among fungal denitrifiers and the cosmopolitan distribution of these organisms suggest that fungal denitrifier abundance may increase in terrestrial ecosystems. Fungal denitrifiers, in contrast to their bacterial counterparts, are a poorly studied functional group within the nitrogen cycle, even though they produce the greenhouse gas NO. To curb soil NO emissions, a better understanding of their ecology and distribution in soils from different ecosystems is needed. Here, we probed a massive amount of DNA sequences and corresponding soil data from a large number of samples that represented the major soil environments for a broad understanding of fungal denitrifier diversity at the global scale. We show that fungal denitrifiers are predominantly cosmopolitan saprotrophs and opportunistic pathogens. Fungal denitrifiers constituted, on average, 1% of the total denitrifier community. This suggests that earlier estimations of fungal denitrifier abundance, and, thereby, it is also likely that the contributions of fungal denitrifiers to NO emissions have been overestimated. Nevertheless, with many fungal denitrifiers being plant pathogens, they could become increasingly relevant, as soilborne pathogenic fungi are predicted to increase with ongoing climate change.
反硝化作用的微生物过程是陆地生态系统中温室气体氧化亚氮(NO)的主要来源。与许多细菌不同,真菌反硝化菌缺乏 NO 还原酶,因此是 NO 的来源。然而,它们的多样性、全球分布和环境决定因素,以及与细菌和古菌反硝化菌相比的相对重要性,仍然没有得到解决。本研究采用系统发育信息分析方法,对全球范围内 1980 个土壤和根际宏基因组中反硝化作用的标志基因 进行分析,该基因编码反硝化作用中的铜依赖亚硝酸盐还原酶,结果表明真菌反硝化菌虽然稀少,但分布广泛,主要由腐生菌和病原体组成。尽管已知某些尖孢镰刀菌物种复合体成员会产生大量的 NO,但它们在根际中的丰度和多样性与其他生物群相比并没有表现出特定的生物群落分布模式。真菌反硝化菌最常被检测到在农田中,但在森林土壤中的丰度最高,与宏基因组大小相比。然而,细菌和古菌反硝化菌的压倒性优势表明,真菌对 NO 排放的贡献比之前估计的要低得多。相对而言,它们可能在碳氮比高、pH 值低的土壤中发挥作用,尤其是在苔原以及北方和温带针叶林中。由于全球变暖预测真菌病原体的增加,真菌反硝化菌中潜在植物病原体的流行以及这些生物的世界性分布表明,陆地生态系统中真菌反硝化菌的丰度可能会增加。真菌反硝化菌与细菌反硝化菌不同,它们是氮循环中一个研究较少的功能群,尽管它们会产生温室气体 NO。为了抑制土壤中 NO 的排放,需要更好地了解它们在不同生态系统土壤中的生态和分布。在此,我们通过对来自大量样本的大量 DNA 序列和相应土壤数据进行探测,在全球范围内广泛了解真菌反硝化菌的多样性。结果表明,真菌反硝化菌主要是世界性的腐生菌和机会性病原体。真菌反硝化菌平均占总反硝化菌群落的 1%。这表明,以前对真菌反硝化菌丰度的估计,以及由此对真菌反硝化菌对 NO 排放的贡献的估计,可能过高。然而,由于许多真菌反硝化菌是植物病原体,它们可能会变得越来越重要,因为随着气候变化的持续,土壤传播的致病真菌预计会增加。