Slope aspect determines the abundance and composition of nitrogen‐cycling microbial communities in an alpine ecosystem

Abstract

Summary Slope aspect is an important topographic feature that can influence local environmental conditions. While strong effects of slope aspect on aboveground and belowground communities have been frequently elucidated, how slope aspect affects soil nitrogen (N) cycling microbes remains unclear. Here, we characterized the communities of soil N‐cycling microbes on south‐ and north‐facing slopes in an alpine ecosystem, by quantifying (qPCR) and high‐throughput sequencing six genes involved in N‐fixation ( nifH ), nitrification (archaeal and bacterial amoA ) and denitrification ( nirK , nirS and nosZ ). We found that the abundance, diversity and community composition of major N‐cycling microbes differed dramatically between the two slope aspects, and these variances could be well explained by the aspect‐driven differences in environmental conditions, especially soil temperature and moisture. The response patterns of different N‐cycling groups to slope aspect were much inconsistent, especially for those with similar functions (i.e. ammonia‐oxidizing archaea vs. bacteria, nirK ‐ vs. nirS ‐reducers), indicating strong niche differentiation between these counterparts. We also observed strong preferences and distinct co‐occurrence patterns of N‐cycling microbial taxa for the two slope aspects. These findings highlight the importance of slope aspect in determining the abundance, species distribution and community structure of N‐cycling microbes, and consequently influencing N‐cycling processes and ecosystem functioning.

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