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Urbanization is becoming increasingly important in terms of climate change and ecosystem functionality worldwide. We are only beginning to understand how the processes of urbanization influence ecosystem dynamics and how peri-urban environments contribute to climate change. Brisbane in South East Queensland (SEQ) currently has the most extensive urban sprawl of all Australian cities. This leads to substantial land use changes in urban and peri-urban environments and the subsequent gaseous emissions from soils are to date neglected for IPCC climate change estimations. This research examines how land use change effects methane (CHâ) and nitrous oxide (NâO) fluxes from peri-urban soils and consequently influences the Global Warming Potential (GWP) of rural ecosystems in agricultural use undergoing urbanization. Therefore, manual and fully automated static chamber measurements determined soil gas fluxes over a full year and an intensive sampling campaign of 80 days after land use change. Turf grass, as the major peri-urban land cover, increased the GWP by 415 kg COâ-e haâ»Â¹ over the first 80 days after conversion from a well-established pasture. This results principally from increased daily average NâO emissions of 0.5 g NâO haâ»Â¹ dâ»Â¹ from the pasture to 18.3 g NâO haâ»Â¹ dâ»Â¹ from the turf grass due to fertilizer application during conversion. Compared to the native dry sclerophyll eucalypt forest, turf grass establishment increases the GWP by another 30 kg COâ-e haâ»Â¹. The results presented in this study clearly indicate the substantial impact of urbanization on soil-atmosphere gas exchange in form of non-COâ greenhouse gas emissions particularly after turf grass establishment.