A global analysis of soil microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems
Article first published online: 28 DEC 2012
Published 2012. This article is a US Government work and is in the public domain in the USA.
Global Ecology and Biogeography
Volume 22, Issue 6, pages 737–749, June 2013
How to Cite
Xu, X., Thornton, P. E. and Post, W. M. (2013), A global analysis of soil microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems. Global Ecology and Biogeography, 22: 737–749. doi: 10.1111/geb.12029
- Issue published online: 5 MAY 2013
- Article first published online: 28 DEC 2012
- US Department of Energy
- Office of Science
- Biological and Environmental Research (BER)
- soil microbial biomass;
- terrestrial ecosystems
To estimate the concentrations, stoichiometry and storage of soil microbial biomass carbon (C), nitrogen (N) and phosphorus (P) at biome and global scales.
We collected 3422 data points to summarize the concentrations and stoichiometry of C, N and P in soils, soil microbial biomass at global and biome levels, and to estimate the global storage of soil microbial biomass C and N.
The results show that concentrations of C, N and P in soils and soil microbial biomass vary substantially across biomes; the fractions of soil elements C, N and P in soil microbial biomass are 1.2, 2.6 and 8.0%, respectively. The best estimates of C:N:P stoichiometry for soil elements and soil microbial biomass are 287:17:1 and 42:6:1, respectively, at global scale, and they vary in a wide range among biomes. The vertical distribution of soil microbial biomass follows the distribution of roots up to 1 m depth.
The global storage of soil microbial biomass C and N were estimated to be 16.7 Pg C and 2.6 Pg N in the 0–30 cm soil profiles, and 23.2 Pg C and 3.7 Pg N in the 0–100 cm soil profiles. We did not estimate P in soil microbial biomass due to insufficient data and insignificant correlation between soil total P and climate variables used for spatial extrapolation. The spatial patterns of soil microbial biomass C and N were consistent with those of soil organic C and total N, i.e. high density in northern high latitude, and low density in low latitudes and the Southern Hemisphere.