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Publikováno v:
Applied and Environmental Microbiology, 83 (18)
Glacier forefield soils can provide a substantial sink for atmospheric CH4, facilitated by aerobic methane-oxidizing bacteria (MOB). However, MOB activity, abundance, and community structure may be affected by soil age, MOB location in different fore
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::114a0800f2c7bafdd9d1cdd1506039c3
https://doi.org/10.1128/aem.01139-17
https://doi.org/10.1128/aem.01139-17
