744-2 Rhizosphere Microorganisms as a Factor in Temperature Sensitivity of SOC Decomposition.

See more from this Division: S03 Soil Biology & Biochemistry
See more from this Session: Soil Carbon Dynamics

Wednesday, 8 October 2008: 8:30 AM
George R. Brown Convention Center, 370C

Jessica Gutknecht1, Biao Zhu1, Mary Firestone2 and Weixin Cheng1, (1)1156 High St., ISB rm 410, University of California Santa Cruz, Environmental Studies Department, Santa Cruz, CA
(2)Univ. of California, Berkeley, Berkeley, CA
Abstract:
Elevated temperature, caused by elevated atmospheric CO2, could cause an important positive feedback to global warming by increasing soil organic carbon (SOC) decomposition and an associated release of CO2 to the atmosphere. There are many potentially important factors involved in the temperature sensitivity of SOC decomposition such as plant species, rhizosphere processes, soil type, and especially the role of soil microbial communities. Soil microbial communities are the essential link between ecosystem function, plants, and soil, yet we lack a detailed understanding of microbial response to elevated temperature. In this study we simultaneously measured many aspects of the microbial community (biomass, composition, turnover, and activity) in a unique 13CO2 continuous labeling facility to elucidate the relationships between elevated temperature, plants, microorganisms, and SOC decomposition. Our treatments included elevated temperature (unheated or +5 °C using soil heating cables), two soil types (organic farm soil versus grassland soil), and three planting treatments (soybean, sunflower, and an unplanted control). After six and ten weeks of heating and plant growth, we destructively harvested pots to examine many aspects of microbial community dynamics including: activity (soil respiration, rhizosphere respiration, nitrogen mineralization and extra-cellular enzyme activity), community composition (13C lipid analysis), biomass (lipid biomass and chloroform fumigation), and turnover rates (using 15N pool dilution). A major finding of our study, from preliminary data, was that microbial community dynamics and treatment effects varied greatly between the two soil types.  Microbial biomass was higher, and enzyme activity lower, in grassland soil than organic farm soil. The effect of heating also appeared to be more significant in grassland soil than organic farm soil. In conclusion, we suggest that soil characteristics, and the associated microbial community, are important factors in the temperature sensitivity of SOC decomposition.

See more from this Division: S03 Soil Biology & Biochemistry
See more from this Session: Soil Carbon Dynamics