Nancy Serrano-Silva;Yohanna Sarria-Guzmán;Luc Dendooven;Marco Luna‐Guid

Laboratory of Soil Ecology, ABACUS, Cinvestav, Instituto Politecnico Nacional 2508, C.P. 07360 Mexico, D.F. (Mexico;Laboratory of Soil Ecology, ABACUS, Cinvestav, Instituto Politecnico Nacional 2508, C.P. 07360 Mexico, D.F. (Mexico)

anaerobic CH4 oxidation;biological production;global warming;methanogenic archaea;methanotrophic bacteri

Global warming, as a result of an increase in the mean temperature of the planet, might lead to catastrophic events for humanity. This temperature increase is mainly the result of an increase in the atmospheric greenhouse gases (GHG) concentration. Water vapor, carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) are the most important GHG, and human activities, such as industry, livestock and agriculture, contribute to the production of these gases. Methane, at an atmospheric concentration of 1.7 1.7 mu mol mol(-1) currently, is responsible for 16% of the global warming due to its relatively high global warming potential. Soils play an important role in the CH4 cycle as methanotrophy (oxidation of CH4) and methanogenesis (production of CH4) take place in them. Understanding methanogenesis and methanotrophy is essential to establish new agriculture techniques and industrial processes that contribute to a better balance of GHG. The current knowledge of methanogenesis and methanotrophy in soils, anaerobic CH4 oxidation and methanotrophy in extreme environments is also discussed.