COS 80-10
Ecosystem-specific responses of soil microbial communities to elevated carbon dioxide

Wednesday, August 7, 2013: 4:20 PM
M100GD, Minneapolis Convention Center
Zhili He, Institute for Environmental Genomics and Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK
Background/Question/Methods

The global atmospheric concentration of CO2 has been increasing for the last 150 years and is predicted to increase to 550 ppm by the middle of this century.  Some previous studies showed that elevated CO2 (eCO2) significantly affected the diversity, composition, structure, and function of soil microbial communities. However, those studies are largely based on a single experimental site or ecosystem. Whether the observed responses are site- or ecosystem-dependent remains unclear. In this study, we examined the response of soil microbial communities under eCO2 at six different experimental sites or/and ecosystems (BioCON, Duke, ORNL, MaizeFACE, SoyFACE and PHACE).  A total of 110 soil samples with 55 from ambient CO2 (aCO2) and 55 from eCO2 were examined by a comprehensive functional gene array (GeoChip 3.0).  Various statistical methods were applied to detect the effect of eCO2 and ecosystems on soil microbial communities and their linkages with soil properties.  

Results/Conclusions

Site/ecosystems, CO2 and their combination significantly (p < 0.05) affected the functional structure and metabolic potential of soil microbial communities with site/ecosystems having much stronger influence (~47%), followed by site/ecosystem and CO2 (~4.1%), and then CO2 (~1.3%). The abundance of most key functional genes involved in carbon (C), nitrogen (N), phosphorus (P) and sulfur (S) cycling differed significantly among different sites/ecosystems. However, the overall abundance of genes involved in C fixation (Pcc/Acc), C degradation (e.g., pulA, vanA, vdh, mnp, and phenol oxidase genes),  N fixation (nifH), denitrification (e.g., narG, nirS), N reduction (e.g., nasA, nrfA), phosphorus utilization (e.g., phytase genes), and sulfur metabolism (e.g., dsrA/B, sox) generally increased at eCO2. In addition, such changes in the soil microbial community were closely correlated with soil C and N. This study provides insights into our understanding of soil microbial communities and their feedbacks to terrestrial ecosystems in response to eCO2.