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Article

Non-enzymatic methane formation by aerobic organisms

2021-03-01

Abstract excerpt

<title>Abstract</title> <p>Methane (CH4) is the most abundant organic compound in the atmosphere, largely originating from anthropogenic and natural biogenic sources1. Traditionally, biogenic CH4 has been regarded as the final product of the anoxic decomposition of organic matter by methanogenic Archaea. However, plants2–4, fungi5, algae6,7 and cyanobacteria8 have recently been shown to produce CH4 in the presenc...

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Literature Corpus work
49c15e74-c7e1-5d93-a909-79cd781555ea
DOI
10.21203/rs.3.rs-153741/v1
Open publication

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Non-enzymatic methane formation by aerobic organismsDOI 10.21203/rs.3.rs-153741/v1
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