98th ESA Annual Meeting (August 4 -- 9, 2013)

COS 82-1 - Responses of ecosystem carbon cycle to experimental warming:a meta-analysis

Thursday, August 8, 2013: 8:00 AM
101G, Minneapolis Convention Center
Meng Lu, Smithsonian Environmental Research Center, Edgewater, MD, Xuhui Zhou, Institute of Biodiversity, Fudan University, Shanghai, China, Yiqi Luo, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK and Bo Li, Ministry of Education Key Lab for Biodiversity Science and Ecological Engineering, The Institute of Biodiversity Science, Fudan University, Shanghai, China
Background/Question/Methods Global warming potentially alters terrestrial ecosystem carbon (C) cycle, feeding back to further climate warming. However, how ecosystem C cycle responds and feed backs to warming remain unclear. We here used a meta-analysis to quantify response ratios of 18 variables of ecosystem C cycle to experimental warming.

Results/Conclusions Our results showed that warming stimulated gross ecosystem photosynthesis (GEP) by 15.7%, net primary production (NPP) by 4.4%, and above- and belowground plant C pools by 6.8% and 7.0%, respectively. The experimental warming also accelerated litter mass loss by 6.8%, soil respiration by 9.0%, and dissolved organic C leaching by 12.1%. In addition, the responses of some of those variables to experimental warming differed among the ecosystem types. The warming effects on C influx and efflux are roughly counterbalanced with each other, resulting in insignificant changes in litter and soil C contents, and net ecosystem exchange (NEE). The minor changes in soil C storage and NEE across ecosystems suggest that climate warming might not trigger strong carbon-climate feedback from terrestrial ecosystems. Our results are also potentially useful for parameterizing and benchmarking land surface models in terms of C cycle responses to climate warming.