期刊
FUNCTIONAL ECOLOGY
卷 24, 期 1, 页码 233-242出版社
WILEY
DOI: 10.1111/j.1365-2435.2009.01610.x
关键词
available N; C and N immobilization in microbial biomass; C and N mineralization; fertility islands; nitrification; Parkinsonia praecox; Prosopis laevigata; Tehuacan-Cuicatlan Region
类别
资金
- CONACyT
- CTIC-UNAM postdoctoral scholarship
P>1. Biological nitrogen (N) fixation by symbiotic and free-living organisms is considered the main pathway for N soil enrichment in desert and semi-desert ecosystems. This fact is more noticeable in tropical ecosystems where legume species have a high relative abundance. However, this biological fixation pathway does not guarantee the maintenance of soil N pools, and N conservation pathways are important in understanding controls over soil N cycling. 2. In dryland ecosystems, desert plants can form a 'fertility island' (FI) as soils beneath plants show higher concentrations of N and organic matter. 3. Here we assess how carbon (C) and N may interact to conserve soil N within the FI soil of two legume species (Prosopis laevigata and Parkinsonia praecox), one a known N-fixer and the other believed not to fix N, as well as within adjacent bare ground soil. In a semi-arid tropical ecosystem in central Mexico, we examined spatial patterns in C and N pools and transformation rates, and we investigated seasonal variations in these relationships. 4. Results show that FI soil C and N could be linked to total N storage through net C and N immobilization in microbial biomass and heterotrophic microbial activity. Soil under P. laevigata canopy had greater total N as well as N accumulated in microbial biomass than soil under P. praecox and bare ground soil. Nevertheless, inorganic N and potential net N mineralization rates were similar under soils of both species, although we expected higher inorganic N and N-mineralization values in N-fixer species to explain the greater total N. Higher total N concentrations under P. laevigata probably result from greater inputs of organic C and a higher potential net C mineralization rate in comparison to P. praecox and bare ground soil. 5. Even though N input and output values were not measured, the results highlight the importance of assessing the role of organic C, heterotrophic microbial activity, and N storage in microbial biomass in order to understand controls over N retention in soil N cycling. Thus, soil C-N interactions could be a control factor of N soil conservation in this tropical semi-arid ecosystem.
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