Seasonal total methane depletion in limestone caves.

ABSTRACT: Methane concentration in caves is commonly much lower than the external atmosphere, yet the cave CH₄ depletion causal mechanism is contested and dynamic links to external diurnal and seasonal temperature cycles unknown. Here, we report a continuous 3-year record of cave methane and other trace gases in Jenolan Caves, Australia which shows a seasonal cycle of extreme CH₄ depletion, from ambient ~1,775 ppb to near zero during summer and to ~800 ppb in winter. Methanotrophic bacteria, some newly-discovered, rapidly consume methane on cave surfaces and in external karst soils with lifetimes in the cave of a few hours. Extreme bacterial selection due to the absence of alternate carbon sources for growth in the cave environment has resulted in an extremely high proportion 2

SUBMITTER: Waring CL 

PROVIDER: S-EPMC5559484 | biostudies-literature | 2017 Aug

REPOSITORIES: biostudies-literature