Artículo

Long-term N-addition alters the community structure of functionally important N-cycling soil microorganisms across global grasslands

Frey, Beat ; Moser, Barbara ; Tytgat, Bjorn ; Zimmermann, Stephan ; Alberti, Juan Icon; Biederman, Lori A. ; Borer, Elizabeth Icon; Broadbent, Arthur A. D. ; Caldeira, Maria C. Icon; Davies, Kendi F. ; Eisenhauer, Nico Icon; Eskelinen, Anu Icon; Fay, Philip A. ; Hagedorn, Frank ; Hautier, Yann Icon; MacDougall, Andrew S. ; McCulley, Rebecca L. ; Moore, Joslin L ; Nepel, Maximilian ; Power, Sally A. ; Seabloom, Eric W. ; Vázquez, Eduardo ; Virtanen, Risto ; Yahdjian, María Laura Icon; Risch, Anita

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Fecha

01/2023

Editorial

Pergamon-Elsevier Science Ltd

Revista

Soil Biology And Biochemistry

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ISSN

0038-0717

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Inglés

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Resumen

Anthropogenic nitrogen (N) input is known to alter the soil microbiome, but how N enrichment influences the abundance, alpha-diversity and community structure of N-cycling functional microbial communities in grasslands remains poorly understood. Here, we collected soils from plant communities subjected to up to 9 years of annual N-addition (10 g N m−2 per year using urea as a N-source) and from unfertilized plots (control) in 30 grasslands worldwide spanning a large range of climatic and soil conditions. We focused on three key microbial groups responsible for two essential processes of the global N cycle: N2 fixation (soil diazotrophs) and nitrification (AOA: ammonia-oxidizing archaea and AOB: ammonia-oxidizing bacteria). We targeted soil diazotrophs, AOA and AOB using Illumina MiSeq sequencing and measured the abundance (gene copy numbers) using quantitative PCR. N-addition shifted the structure of the diazotrophic communities, although their alpha-diversity and abundance were not affected. AOA and AOB responded differently to N-addition. The abundance and alpha-diversity of AOB increased, and their community structure shifted with N-addition. In contrast, AOA were not affected by N-addition. AOA abundance outnumbered AOB in control plots under conditions of low N availability, whereas N-addition favoured copiotrophic AOB. Overall, N-addition showed a low impact on soil diazotrophs and AOA while effects for AOB communities were considerable. These results reveal that long-term N-addition has important ecological implications for key microbial groups involved in two critical soil N-cycling processes. Increased AOB abundance and community shifts following N-addition may change soil N-cycling, as larger population sizes may promote higher rates of ammonia oxidation and subsequently increase N loss via gaseous and soil N-leaching. These findings bring us a step closer to predicting the responses and feedbacks of microbial-mediated N-cycling processes to long-term anthropogenic N-addition in grasslands.

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