Schadt, C. W. | bioRxiv Science

bioRxiv2018

Phylogenomics reveals dynamic evolution of fungal nitric oxide reductases and their relationship to secondary metabolism

Fungi expressing P450nor, an unconventional nitric oxide (NO) reducing cytochrome P450, are thought to be significant contributors to soil nitrous oxide (N2O) emissions. However, fungal contributions to N2O emissions remain uncertain due to inconsistencies in measurements of N2O formation by fungi. Much of the N2O emitted from antibiotic-amended soil microcosms is attributed to fungal activity, yet fungal isolates examined in pure culture are poor N2O producers. To assist in reconciling these conflicting observations and produce a benchmark genomic analysis of fungal denitrifiers, genes underlying fungal denitrification were examined in >700 fungal genomes. Of 167 p450nor-containing genomes identified, 0, 30, and 48 also harbored the denitrification genes narG, napA or nirK, respectively. Compared to napA and nirK, p450nor was twice as abundant and exhibited two to five-fold more gene duplications, losses, and transfers, indicating a disconnect between p450nor presence and denitrification potential. Furthermore, co-occurrence of p450nor with genes encoding NO-detoxifying flavohemoglobins (Spearman r = 0.87, p = 1.6e-10) confounds hypotheses regarding P450nors primary role in NO detoxification. Instead, ancestral state reconstruction united P450nor with actinobacterial cytochrome P450s (CYP105) involved in secondary metabolism (SM) and 19 (11 %) p450nor-containing genomic regions were predicted to be SM clusters. Another 40 (24 %) genomes harbored genes nearby p450nor predicted to encode hallmark SM functions, providing additional contextual evidence linking p450nor to SM. These findings underscore the potential physiological implications of widespread p450nor gene transfer, support the novel affiliation of p450nor with fungal SM, and challenge the hypothesis of p450nors primary role in denitrification.

microbiology↗

bioRxiv2017

Alphaproteobacteria fix nitrogen in a Sphagnum-dominated peat bog using molybdenum-dependent nitrogenase

Microbial N2 fixation (diazotrophy) represents an important nitrogen source to oligotrophic peatland ecosystems, which are important sinks for atmospheric CO2 and susceptible to changing climate. The objectives of this study were: (i) to determine the active microbial group and type of nitrogenase mediating diazotrophy in a ombrotrophic Sphagnum-dominated peat bog (the S1 peat bog, Marcell Experimental Forest, Minnesota, USA); and (ii) to determine the effect of environmental parameters (light, O2, CO2, CH4) on potential rates of diazotrophy measured by acetylene (C2H2) reduction and 15N2 incorporation. Molecular analysis of metabolically active microbial communities suggested that diazotrophy in surface peat was primarily mediated by Alphaproteobacteria (Bradyrhizobiaceae and Beijerinckiaceae). Despite higher dissolved vanadium (V; 11 nM) than molybdenum (Mo; 3 nM) in surface peat, a combination of metagenomic, amplicon sequencing and activity measurements indicated that Mo-containing nitrogenases dominate over the V-containing form. Acetylene reduction was only detected in surface peat exposed to light, with the highest rates observed in peat collected from hollows with the highest water content. Incorporation of15N2 was suppressed 90% by O2 and 55% by C2H2, and was unaffected by CH4 and CO2 amendments. These results suggest that peatland diazotrophy is mediated by a combination of C2H2 - sensitive and C2H2 - insensitive microbes that are more active at low O2 and show similar activity at high and low CH4.\n\nImportancePrevious studies indicate that diazotrophy provides an important nitrogen source and is linked to methanotrophy in Sphagnum-dominated peatlands. However, the environmental controls and enzymatic pathways of peatland diazotrophy, as well as the metabolically active microbial populations that catalyze this process remain in question. Our findings indicate that oxygen levels and photosynthetic activity override low nutrient availability in limiting diazotrophy, and that members of the Alphaproteobacteria (Rhizobiales) catalyze this process at the bog surface using the molybdenum - based form of the nitrogenase enzyme.

microbiology↗