Permafrost as a source of mineral weathering bacteria: Implications of active layer thickening on James Ross Island, Antarctica
Micenková et al., CATENA 2025
Microbiological research in Antarctica provides a unique perspective on biodiversity and the influence of geochemistry on soil microbial composition. Samples from a 350 cm deep core were analyzed in the area of the J. G. Mendel Czech Antarctic Station on James Ross Island. Geological transitions, such as the interface between the active layer and permafrost or the change between Holocene marine sediments and Cretaceous rocks, had a key influence on microbial composition. Due to warming, the interaction between microbial communities in the active layer and permafrost is expected to deepen in the future.