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Understanding Methanogens, Methanotrophs, and Methane Emission in Rice Ecosystem

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Microbiomes and the Global Climate Change

Abstract

Rising concentration of methane (CH4), nitrous oxide, carbon dioxide, and chlorofluorocarbons in the atmosphere result in global warming. These greenhouse gases (GHGs) trap the infrared radiations remitted from the Earth. The global mean temperature is rising more rapidly than ever due to presence of higher concentration of GHGs in the atmosphere. Anthropogenic activities such as fossil fuel burning, biomass combustion, industrialization, modern agricultural system, etc., are the key factors responsible for rising GHGs concentration. After carbon dioxide, CH4 is the major GHG contributing to the global warming. CH4 is produced by methanogens by complex processes known as methanogenesis. Methanogens are strictly anaerobic bacteria and they can persist in extreme environmental conditions. Rice is the stable food for more than 50% of global population. Rice is generally cultivated in subtropical regions and it is reported that continuous flooded environment is better for higher production. Flooding condition of the rice creates favorable environment for methanogenic bacteria. Under anaerobic environment, methanogens consume soil organic matter as carbon source and emit CH4 gas to atmosphere. CH4 emission from rice soil is the net balances of two processes: production by methanogens and oxidation by methanotrophs. Methanotrophs are obligate aerobic bacteria which consume CH4 as the source of carbon and help oxidation of CH4 to carbon dioxide. In rice ecosystem, population of methanogenic and methanotrophic bacteria depends upon several biotic and abiotic factors which are discussed in this chapter.

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Malyan, S.K. et al. (2021). Understanding Methanogens, Methanotrophs, and Methane Emission in Rice Ecosystem. In: Lone, S.A., Malik, A. (eds) Microbiomes and the Global Climate Change. Springer, Singapore. https://doi.org/10.1007/978-981-33-4508-9_12

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