Long-term N-addition alters the community structure of functionally important N-cycling soil microorganisms across global grasslands
; Biederman, Lori A. ; Borer, Elizabeth
; Broadbent, Arthur A. D. ; Caldeira, Maria C.
; Davies, Kendi F. ; Eisenhauer, Nico
; Eskelinen, Anu
; Fay, Philip A. ; Hagedorn, Frank ; Hautier, Yann
; MacDougall, Andrew S. ; McCulley, Rebecca L. ; Moore, Joslin L ; Nepel, Maximilian ; Power, Sally A. ; Seabloom, Eric W. ; Vázquez, Eduardo ; Virtanen, Risto ; Yahdjian, María Laura
; Risch, Anita Otros responsables
Fecha
01/2023
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Pergamon-Elsevier Science Ltd
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Soil Biology And Biochemistry
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0038-0717
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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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