Skip to main page content
U.S. flag

An official website of the United States government

Dot gov

The .gov means it’s official.
Federal government websites often end in .gov or .mil. Before sharing sensitive information, make sure you’re on a federal government site.

Https

The site is secure.
The https:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

Access keys NCBI Homepage MyNCBI Homepage Main Content Main Navigation
. 2015 Apr 20:5:9697.
doi: 10.1038/srep09697.

N2O production, a widespread trait in fungi

Affiliations

N2O production, a widespread trait in fungi

Koki Maeda et al. Sci Rep. .

Abstract

N2O is a powerful greenhouse gas contributing both to global warming and ozone depletion. While fungi have been identified as a putative source of N2O, little is known about their production of this greenhouse gas. Here we investigated the N2O-producing ability of a collection of 207 fungal isolates. Seventy strains producing N2O in pure culture were identified. They were mostly species from the order Hypocreales order-particularly Fusarium oxysporum and Trichoderma spp.-and to a lesser extent species from the orders Eurotiales, Sordariales, and Chaetosphaeriales. The N2O (15)N site preference (SP) values of the fungal strains ranged from 15.8‰ to 36.7‰, and we observed a significant taxa effect, with Penicillium strains displaying lower SP values than the other fungal genera. Inoculation of 15 N2O-producing strains into pre-sterilized arable, forest and grassland soils confirmed the ability of the strains to produce N2O in soil with a significant strain-by-soil effect. The copper-containing nitrite reductase gene (nirK) was amplified from 45 N2O-producing strains, and its genetic variability showed a strong congruence with the ITS phylogeny, indicating vertical inheritance of this trait. Taken together, this comprehensive set of findings should enhance our knowledge of fungi as a source of N2O in the environment.

PubMed Disclaimer

Figures

Figure 1
Figure 1. N2O production by the positive fungi strains with (white) and without (black) 10% C2H2 in the headspace.
Error bars indicate the standard deviation (n = 3). Both strain names and MIAE numbers are indicated.
Figure 2
Figure 2. N2O production by 15 selected fungi strains inoculated in 3 different sterile soils.
NO2 was used as the electron acceptor. The strains were incubated for 7 days, and headspace N2O concentration were measured 3 times (2, 4 and 7 days after NO2 addition). Code for the soils: Black circle: Sweden (Slogaryd), forest soil; grey triangle: France, arable soil; black rectangle: The Netherlands, grassland soil. Code for the fungi: a: Trichoderma harzianum (MIAE00042); b: Fusarium verticillioides (MIAE00306); c: Penicillium adametzii (MIAE01008); d: F. oxysporum f. sp. lini (MIAE00347); e: F. dimerum (MIAE00598); f: Metarhizium anisopliae (MIAE00953); g: Chaetomium sp. (MIAE00985); h: T. harzianum (anamorph) (MIAE01011); i: Leptosphaeria sp. (MIAE01060); j: T. tomentosum (MIAE00031); k: Fusarium sp. (MIAE01519); l: Clonostachys candelabrum (MIAE00941); m: Phialocephala sp. (MIAE00968); n: Colletotrichum coccodes (MIAE01515); o: Aspergillus sp. (MIAE01518);); p: No fungi control. The error bar represents the standard deviation (n = 3).
Figure 3
Figure 3. Neighbour-joining phylogenetic tree of nirK amino acid sequences constructed by Clustal W with 1000 bootstrap samplings.
Strain names in bold indicate the sequences obtained in this study. The numbers in parentheses indicate the number of the strains. Bootstrap values greater than 75% are indicated as black circles.

References

    1. Davidson E. A., Rogers J. & Whitman W. Fluxes of nitrous oxide and nitric oxide from terrestrial ecosystems. In: Microbial production and consumption of greenhouse gases: methane, nitrogen oxides, and halomethanes. (eds. Rogers J. E., , Whitman W. B., eds. ) 219–235. (American Society for Microbiology, 1991).
    1. Davidson E. The contribution of manure and fertilizer nitrogen to atmospheric nitrous oxide since 1860. Nat. Geosci. 2, 659–662 (2009).
    1. Forster P. et al. Changes in Atmospheric Constituents and in Radiative Forcing. In: Climate Change 2007: The Physical Science Basis. (eds. Solomon S., et al.) Ch.2, 130–234. (Cambridge University Press, 2007).
    1. Ravishankara A., Daniel J. & Portmann R. Nitrous oxide (N2O): the dominant ozone-depleting substance emitted in the 21st century. Science 326, 123–125 (2009). - PubMed
    1. Hooper A. B. & Terry K. Hydroxylamine oxidoreductase of Nitrosomonas: Production of nitric oxide from hydroxylamine. BBA-Enzymol. 571, 12–20 (1979). - PubMed

Publication types

Associated data