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

COS 119-6 - The role of evolutionary history in a changing climate: Combined effects of phylogenetic dissimilarity, carbon dioxide, and nitrogen

Friday, August 9, 2013: 9:30 AM
101J, Minneapolis Convention Center
Mark Genung, Ecology and Evolutionary Biology, University of Tennessee - Knoxville, Knoxville, TN, Jennifer A. Schweitzer, University of Tennessee - Knoxville, Knoxville, TN and Joseph K. Bailey, Ecology and Evolutionary Biology, The University of Tennessee, Knoxville, Knoxville, TN
Background/Question/Methods

Biodiversity is fundamental to ecosystem services, and ecosystem function generally improves with increasing species richness. The most common explanations for the relationship between biodiversity and ecosystem function are driven by plant traits; this suggests that evolutionary history, which generates trait diversity, may influence ecosystem function. Unfortunately, biodiversity is declining across the globe, and climate change is a major driver of this decline. Climate change will alter CO2 and nitrogen (N) concentrations and also shift the composition of plant communities. However, the ecological importance of biotic environmental shifts relative to CO2 and N is not well known. We established an experiment that used 26 Tasmanian eucalypt species (from subgenera Eucalyptus and Symphyomyrtus), planted in species monocultures and mixtures. The mixtures manipulated both species richness (3 or 6 species) and phylogenetic diversity (1 or 2 subgenera). We also manipulated CO2 and N concentrations. We attempted to answer three broad questions: (1) Do different phylogenetic groups respond differently to increases in biodiversity (measured either at the species or subgenera level), (2) Do different phylogenetic groups respond differently to increases in CO2 and N, and (3) How important is phylogenetic dissimilarity relative to concentrations of CO2and N?

Results/Conclusions

We found that plants in pots that experienced elevated CO2 produced more belowground and aboveground biomass. The effect sizes of CO2 on aboveground biomass and belowground biomass were similar, suggesting that CO2 was not having a disproportionately large impact on belowground plant structures. CO2 and N appeared to be co-limiting, as manipulations of only CO2 or only N had no effect on productivity, but manipulating both CO2 and N simultaneously resulted in significant increases in total productivity, as well as aboveground and belowground productivity. We also found that the outcomes of species interactions were affected by the evolutionary relationships (i.e., phylogenetic similarity) between interacting plants, but the effects of evolutionary relationships were not dependent on manipulations of CO2 and N. Within a pot, more genetic similarity generally increased total mixture-level productivity. The effect size of phylogenetic similarity was roughly 40% of CO2 manipulation, and 35% of N manipulation. Determining the importance of phylogenetic similarity in light of these results is subjective and different researchers will likely arrive at different opinions. However, our results provide an initial example of how phylogenetic similarity can influence plant productivity to a degree that is comparable to manipulations of CO2 and N.