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Biological Formation and Consumption of Methane

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Atmospheric Methane: Sources, Sinks, and Role in Global Change

Part of the book series: NATO ASI Series ((ASII,volume 13))

Abstract

Methane is an important product formed during the bacterial degradation of organic matter in environments such as flooded soils, wetlands, estuaries, marine and freshwater sediments, and the gastrointestinal tract of animals (Whitman et al., 1992). This chapter describes the conditions that lead to biogenic methane formation in natural environments, the metabolic pathways and interactions that lead to methanogenesis, and the implications of these factors on the biogeochemistry of methane.

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  1. Environmental Science and Engineering, Oregon Graduate Institute of Science and Technology, 20,000 N.W. Walker Road, Portland, Oregon, 97291-1000, USA

    David R. Boone

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  1. Global Change Research Center, Oregon Graduate Institute of Science and Technology, P. O. Box 91000, 97291-1000, Portland, Oregon, USA

    M. A. K. Khalil (Professor and Director) (Professor and Director)

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Boone, D.R. (1993). Biological Formation and Consumption of Methane. In: Khalil, M.A.K. (eds) Atmospheric Methane: Sources, Sinks, and Role in Global Change. NATO ASI Series, vol 13. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-84605-2_6

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  • DOI: https://doi.org/10.1007/978-3-642-84605-2_6

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