Monday, 7 November 2005 - 1:00 PM
87-4

Impacts of Elevated Atmospheric CO2 on Grassland Biogeochemistry.

Jennifer Y. King, University of Minnesota, Dept of Soil, Water, and Climate and Dept of Ecology, Evolution, and Behavior, 439 Borlaug Hall; 1991 Upper Buford Circle, St. Paul, MN 55108-6028

Understanding interactions between carbon (C) and nitrogen (N) cycling has been central to past progress and ongoing work in climate change research. Arvin Mosier has been a leader in investigating the coupled biogeochemical cycles of C and N in agroecosystems. His research and integrated approach have significantly increased our understanding of the responses of these systems to global change.

Rising atmospheric carbon dioxide (CO2) levels can have direct effects on plant productivity and also important indirect effects on ecosystem biogeochemical cycles. An open-top chamber elevated atmospheric CO2 study was initiated in 1997 in the shortgrass steppe of northeastern Colorado to examine the responses of ecosystem dynamics to elevated CO2 and the potential impacts of elevated CO2 on ecosystem sustainability. This large, collaborative effort focused on changes in ecosystem cycling of water, carbon, and nitrogen with exposure to elevated CO2.

Elevated atmospheric CO2 conditions resulted in significantly higher aboveground plant biomass production and significantly lower plant tissue nitrogen concentrations. The combination of these responses resulted in higher net removal of N from experimental plots treated with elevated CO2. Such changes in N cycling are expected to limit the stimulation of ecosystem productivity under elevated CO2 by slowing decomposition rates and by reducing soil N availability. However, no changes in decomposition rates of aboveground plant tissue or in trace gas fluxes in response to elevated CO2 treatment were observed. Measurements of soil carbon cycling may help to elucidate changes in nitrogen cycling under elevated CO2 conditions.


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