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• W2240608923 startingPage "2173" @default.
• W2240608923 abstract "Abstract:Arctic permafrost affected wetlands and tundra are known to be sources of the greenhouse gas methane (Christensen et al., , ; Kutzbach et al., ; Sachs et al., ; Wagner et al., ; Wille et al., ). As a consequence of the rising surface temperatures and the degradation of permafrost, methane emissions from these Arctic habitats are predicted to increase in the future. Evolution of methane fluxes across the subsurface/atmosphere boundary will thereby strongly depend on the activity of obligately aerobic methane oxidizing Proteobacteria which are known to be abundant and to significantly reduce methane emissions in permafrost affected soils despite seasonal freezing and thawing and extreme temperature gradients. Based on their function as the major (known) sink for methane, research is needed to quantify in situ activities of aerobic methane oxidizing Proteobacteria and understand their potential to adapt to the currently changing environment. Also, possible unknown sinks for methane in these regions like marine methane rich habitats need to be explored." @default.
• W2240608923 created "2016-06-24" @default.
• W2240608923 creator A5087589833 @default.
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• W2240608923 date "2010-01-01" @default.
• W2240608923 modified "2023-09-23" @default.
• W2240608923 title "Permafrost – Current and Future Challenges to Study Methanotrophy in Permafrost Affected Tundra and Wetlands" @default.
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• W2240608923 doi "https://doi.org/10.1007/978-3-540-77587-4_157" @default.
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