As the Arctic experiences unprecedented warming, previously frozen soils are beginning to thaw for extended periods. This phenomenon raises questions about the ecological impact of climate change.
A recent study conducted by an international research team, which includes scientists from Queen Mary University, has found that only half of the soil microbes are reactivated during this thawing process.
The findings suggest that while thawing soils may release some microbial activity, significant portions of the microbial community remain dormant, indicating a complex response to changing environmental conditions.