Convergence of Microbial Assimilations of Soil Carbon, Nitrogen, Phosphorus, and Sulfur in Terrestrial Ecosystems

Convergence of Microbial Assimilations of Soil Carbon, Nitrogen, Phosphorus, and Sulfur in Terrestrial Ecosystems
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Download or read book Convergence of Microbial Assimilations of Soil Carbon, Nitrogen, Phosphorus, and Sulfur in Terrestrial Ecosystems written by and published by . This book was released on 2015 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: How soil microbes assimilate carbon-C, nitrogen-N, phosphorus-P, and sulfur-S is fundamental for understanding nutrient cycling in terrestrial ecosystems. We compiled a global database of C, N, P, and S concentrations in soils and microbes and developed relationships between them by using a power function model. The C:N:P:S was estimated to be 287:17:1:0.8 for soils, and 42:6:1:0.4 for microbes. We found a convergence of the relationships between elements in soils and in soil microbial biomass across C, N, P, and S. The element concentrations in soil microbial biomass follow a homeostatic regulation curve with soil element concentrations across C, N, P and S, implying a unifying mechanism of microbial assimilating soil elements. This correlation explains the well-constrained C:N:P:S stoichiometry with a slightly larger variation in soils than in microbial biomass. Meanwhile, it is estimated that the minimum requirements of soil elements for soil microbes are 0.8 mmol C Kg-1 dry soil, 0.1 mmol N Kg-1 dry soil, 0.1 mmol P Kg-1 dry soil, and 0.1 mmol S Kg-1 dry soil, respectively. Lastly, these findings provide a mathematical explanation of element imbalance in soils and soil microbial biomass, and offer insights for incorporating microbial contribution to nutrient cycling into Earth system models.


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