Tuesday, August 7, 2007: 4:00 PM
J2, San Jose McEnery Convention Center
Anthropogenic activities are increasing the concentration of atmospheric CO2. Some studies have reported an increase in nitrogen (N) fixation in systems exposed to elevated CO2, a response that would alleviate nutrient limitations to soil carbon storage. We report that N fixation and soil organic matter decline after long-term exposure to elevated CO2 in a Florida scrub-oak ecosystem. Increases in above-ground biomass may bind metal nutrients in forms unavailable to N fixing microbes and their plant symbionts, and constrain fixation and carbon storage. The most important of these nutrients for N fixation is molybdenum (Mo), a requisite cofactor of nitrogenase. Mo availability is also limited by the presence of oxides of iron, aluminum and manganese in soil. No study to date has examined the influence of elevated CO2 on these metal oxides and their impact on Mo availability. We present data suggesting that the decline in N fixation in the scrub-oak ecosystem is due to significantly lower Mo concentrations in symbiotic nitrogen fixing plants exposed to elevated CO2, which may be related to our observed differences in stand level oak [Mo]. We have also observed significant differences in the concentration of soil organic matter and metal oxides between the CO2 treatments and suggest that interactions between soil metal nutrients, their response to elevated CO2 and their impact on N fixation is critical to understand ecosystem response to elevated CO2.