Methanol consumption drives the bacterial chloromethane sink in a forest soil.

ABSTRACT: Halogenated volatile organic compounds (VOCs) emitted by terrestrial ecosystems, such as chloromethane (CH₃Cl), have pronounced effects on troposphere and stratosphere chemistry and climate. The magnitude of the global CH₃Cl sink is uncertain since it involves a largely uncharacterized microbial sink. CH₃Cl represents a growth substrate for some specialized methylotrophs, while methanol (CH₃OH), formed in much larger amounts in terrestrial environments, may be more widely used by such microorganisms. Direct measurements of CH₃Cl degradation rates in two field campaigns and in microcosms allowed the identification of top soil horizons (i.e., organic plus mineral A horizon) as the major biotic sink in a deciduous forest. Metabolically ac

SUBMITTER: Chaignaud P 

PROVIDER: S-EPMC6194010 | biostudies-literature | 2018 Nov

REPOSITORIES: biostudies-literature