Arctic Permafrost Thaw and Microbial Carbon Release
thecooldown.comNew research from Queen Mary University of London shows that Arctic soil microbes do not activate uniformly during thaw. While some organisms wake up quickly, others remain dormant for months, suggesting that carbon and methane release from permafrost is more complex than previous climate models assumed. Understanding these biological timelines is critical for forecasting greenhouse gas emissions. Because Arctic soils hold nearly one third of the world's soil carbon, these findings help refine how scientists predict climate risks and the speed of atmospheric warming.
