Increased microbial activity contributes to phosphorus immobilization in the rhizosphere of wheat under elevated CO2

Understanding phosphorus (P) transformation in the rhizosphere affected by elevated CO2 (eCO(2)) needs to underpin the plant-derived C flow and P relationship in the plant-soil-microbe continuum. A pot experiment was conducted in CO2-controlled environmental cabinets. Wheat (Triticum aestivum) plants were grown in a P-sufficient Vertisol soil and exposed to 380 or 800 ppm CO2 for 6 weeks. Plants were labelled with (CO2)-C-13 under respective CO2 treatments. Elevated CO2 increased NaHCO3- and NaOH-extractable organic P (P-o) in the rhizosphere by 160% and 53%, respectively. Consistently, eCO(2) increased microbial C and respiration in the rhizosphere. Furthermore, the excess of C-13 atom in roots and rhizosphere soil, but not in shoots, were markedly higher under eCO(2) than aCO(2). Elevated CO2 increased the copy number of bacterial 16S rDNA from C-13-DNA and C-12-DNA fractions. Although the copy number of fungal 18S rDNA from C-13-DNA was higher under eCO(2), there was no difference on the copy number of total 18S rDNA between the CO2 treatments. It is concluded that the increased P-o in the rhizosphere under eCO(2) was mainly attributed to stimulating microbial biomass/activity which in turn immobilized more P and root-derived materials. The stimulation of microbes resulted from increased C efflux from root systems under eCO(2). (C) 2014 Elsevier Ltd. All rights reserved.