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Does Atmospheric NO −3 Deposition Alter the Abundance and Activity of Ligninolytic Fungi in Forest Soils?

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Abstract

Although field studies have demonstrated an ecosystem-specific effect of experimental atmospheric nitrogen (N) deposition on litter decomposition, a mechanistic understanding of how ligninolytic microbial communities respond to atmospheric deposition is lacking. Because high levels of inorganic N suppress lignin decomposition by some basidiomycetes, it is plausible that the abundance and activity of these key microorganisms underlies differential ecosystem responses of decomposition to atmospheric N deposition. We hypothesize that: (a) atmospheric N deposition will cause an ecosystem-specific reduction in basidiomycete activity and abundance with greatest decreases in ecosystems with lignin-rich forest litter and (b) the abundance of lignin degrading basidiomycetes will be positively correlated with ligninolytic enzyme activity. To test these hypotheses, we measured the effects of experimental N deposition on the potential activity of phenol oxidase enzymes, and the abundance of basidiomycete genes encoding laccase, a primary phenol oxidase enzyme, in three hardwood forests spanning a range of leaf litter lignin content. The black oak-white oak (BOWO) contains high lignin litter, the sugar maple-basswood (SMBW) has low lignin litter, and the sugar maple-red oak (SMRO) is intermediate. An ecosystem by N deposition interaction significantly influenced phenol oxidase activity in the surface soil (P = 0.05), where phenol oxidase activity decreased with increasing experimental N deposition in the BOWO ecosystem. No consistent response to N deposition was evident for surface soil phenol oxidase activity within either the SMRO or SMBW ecosystem. This interaction did not influence laccase gene abundance. Instead, basidiomycete laccase gene abundance was reduced by experimental N deposition (main effect) in surface soil. There was only a weak correlation between basidiomycete laccase gene abundance and potential phenol oxidase enzyme activity, suggesting that the abundance of organisms possessing laccase genes may not control phenol oxidase activity in soil. Our results suggest that the regulation of laccase gene expression may mediate the decomposition response to atmospheric N deposition.

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ACKNOWLEDGEMENTS

Our work was supported by a grant from the Carbon Sequestration Program of the Office of Science (BER), U.S. Department of Energy. We would like to thank Rebecca Mau for field assistance and Liz Kruszewski, Jennifer Jenkins and Zach Wallace for laboratory assistance.

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Author notes

  1. Christopher B. Blackwood

    Present address: Department of Biological Sciences, Kent State University, Kent, Ohio, 44242, USA

Authors and Affiliations

  1. School of Natural Resources and Environment, University of Michigan, Dana Building, 440 Church St., Ann Arbor, Michigan, 48109-1041, USA

    Kirsten S. Hofmockel, Donald R. Zak & Christopher B. Blackwood

  2. Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, Michigan, 48109-1048, USA

    Donald R. Zak

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  1. Kirsten S. Hofmockel
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  2. Donald R. Zak
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  3. Christopher B. Blackwood
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Correspondence to Kirsten S. Hofmockel.

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Hofmockel, K.S., Zak, D.R. & Blackwood, C.B. Does Atmospheric NO −3 Deposition Alter the Abundance and Activity of Ligninolytic Fungi in Forest Soils?. Ecosystems 10, 1278–1286 (2007). https://doi.org/10.1007/s10021-007-9096-x

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  • DOI: https://doi.org/10.1007/s10021-007-9096-x

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