PS 15-146
Impacts of global climate change on vulnerable ecosystems

Monday, August 10, 2015
Exhibit Hall, Baltimore Convention Center
Inyoung Jang, Department of Climate & Ecology, National Institute of Ecology, Chungcheongnam-Do, Korea, Republic of (South)
Hojeong Kang, School of Civil and Environmental Engineering, Ecological Engineering Lab, Seoul, Korea, Republic of (South)
Changwan Seo, Department of Climate & Ecology, National Institute of Ecology, Chungcheongnam-Do, Korea, Republic of (South)
Background/Question/Methods

Global climate change effects on various ecosystems in various way. Especially, wetland and arctic soils are vulnerable to global climate change and contain a large amount of undecomposed carbon. Responses of these vulnerable ecosystems to global climate change should be considered because the responses can further accelerate global climate change by adding extra carbon into the atmosphere in the form of CO2 or methane. In this study, we examined the effects of temperature increase on vulnerable ecosystems such as wetlands and arctic regions. We conducted temperature rising experiments in two different ways: in situ and incubation approach. We examined methane fluxes and microbial community structure at fourteen wetlands with 7 different latitudes from 30°N to 37°N in Mississippi basin for determining the effects of temperature on wetland ecosystems. The difference between the highest and the lowest latitude on a given day is about 4 ˚C during both the summer and winter for daily mean temperature. In addition, we also conducted the incubation experiments with the soils from arctic region and measured the greenhouse gas fluxes and microbial community structure as well.

Results/Conclusions

CH4 fluxes for wetland soils were large in middle latitude and positively correlated with soil organic matter level which can be affected by temperature increase. However, community composition and species richness of methane-related microorganisms did not show any differences among the latitudes. For the arctic incubation experiment, the largest emission rates of CO2 and N2O were found at 10°C, while the lowest values were demonstrated at 0°C and -20°C, respectively. However, the pattern of CH4 emission was different from the other gases. The difference was caused by diverse responses of CH4 production and oxidation processes at different temperature. The changes of CH4 related microorganisms were distinct as the temperature rise. Temperature increase impacts on vulnerable ecosystems in diverse way.