GC050-04
Interacting Effects of Elevated CO2 and Warming on Coastal Wetland Carbon Dynamics
Abstract:
Over the past five years, +5.1 °C of warming doubled CH4 emissions, but warming crossed with eCO2 caused emissions to decrease. eCO2 + warming also reduced the average nominal oxidation state of carbon (NOSC) in the DOC pool and increased heterogeneity in the soil surface, compared to plots with just warming. We hypothesized that these opposing responses were due to the stimulation of plant-mediated transport of O2 into otherwise anaerobic soils under eCO2 conditions, but not under warming alone. To test this hypothesis, we installed an automated redox system in March 2020 that collects replicated measurements every 30 minutes. Redox potential was highly variable in early summer, but by early July eCO2 + warming plots had consistently higher redox potential than warming only plots, indicating a more oxidizing environment. These real-time trends in redox potential also tracked the continuously measured water level and weekly plant phenology assessments over the year, illustrating the strong links between vegetation, biogeochemistry, and hydrology as drivers of carbon cycling in these ecosystems, especially under global change conditions.