Characterization of methanotrophic bacterial populations in soils showing atmospheric methane uptake.

ABSTRACT: The global methane cycle includes both terrestrial and atmospheric processes and may contribute to feedback regulation of the climate. Most oxic soils are a net sink for methane, and these soils consume approximately 20 to 60 Tg of methane per year. The soil sink for atmospheric methane is microbially mediated and sensitive to disturbance. A decrease in the capacity of this sink may have contributed to the approximately 1%. year(-1) increase in the atmospheric methane level in this century. The organisms responsible for methane uptake by soils (the atmospheric methane sink) are not known, and factors that influence the activity of these organisms are poorly understood. In this study the soil methane-oxidizing population was characterized by both labelling soil microbiota with (14)CH(4) and

SUBMITTER: Holmes AJ 

PROVIDER: S-EPMC91497 | biostudies-literature | 1999 Aug

REPOSITORIES: biostudies-literature