4.8 Article

Global biogeography of microbial nitrogen-cycling traits in soil

Publisher

NATL ACAD SCIENCES
DOI: 10.1073/pnas.1601070113

Keywords

nitrification; nitrogen fixation; ammonia assimilation; metagenomics; dissimilatory nitrite reduction

Funding

  1. US Department of Education Graduate Assistance in Areas of National Need Fellowship
  2. US Department of Energy, Office of Science, Office of Biological and Environmental Research Grant [DE-PS02-09ER09-25]
  3. Direct For Biological Sciences [1457160] Funding Source: National Science Foundation
  4. Division Of Environmental Biology [1457160] Funding Source: National Science Foundation

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Microorganisms drive much of the Earth's nitrogen (N) cycle, but we still lack a global overview of the abundance and composition of the microorganisms carrying out soil N processes. To address this gap, we characterized the biogeography of microbial N traits, defined as eight N-cycling pathways, using publically available soil metagenomes. The relative frequency of N pathways varied consistently across soils, such that the frequencies of the individual N pathways were positively correlated across the soil samples. Habitat type, soil carbon, and soil N largely explained the total N pathway frequency in a sample. In contrast, we could not identify major drivers of the taxonomic composition of the N functional groups. Further, the dominant genera encoding a pathway were generally similar among habitat types. The soil samples also revealed an unexpectedly high frequency of bacteria carrying the pathways required for dissimilatory nitrate reduction to ammonium, a little-studied N process in soil. Finally, phylogenetic analysis showed that some microbial groups seem to be N-cycling specialists or generalists. For instance, taxa within the Deltaproteo bacteria encoded all eight N pathways, whereas those within the Cyanobacteria primarily encoded three pathways. Overall, this trait-based approach provides a baseline for investigating the relationship between microbial diversity and N cycling across global soils.

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