“Soils are Earth’s largest reservoir of organic carbon,” states Andreas Richter, lead author of the study and professor at the Centre for Microbiology and Environmental Systems Science. Microorganisms silently dictate the global carbon cycle, breaking down this organic matter thereby releasing carbon dioxide. As temperatures rise – a guaranteed scenario under climate change–microbial communities are thought to emit more carbon dioxide, further accelerating climate change in a process known as soil carbon-climate feedback.
“We saw that more than 50 years of consistent soil warming increased microbial growth at the community level,” says Dennis Metze, PhD student and primary author of the study. “But remarkably, the growth rates of microbes in warmer soils were indistinguishable to those at normal temperatures.” The pivotal difference lay in the bacterial diversity: Warmer soils harboured a more varied array of active microbial taxa.
Predicting soil microbial activities in a future climate
“Understanding the complexities of the soil microbiome’s reaction to climate change has been a considerable challenge, often rendering it a ‘black box’ in climate modeling,” adds Christina Kaiser, associate professor at the Centre. This new finding transcends the traditional focus on community-aggregated growth, setting the stage for more accurate predictions of microbial behavior and its consequent effects on carbon cycling in the evolving climate scenario. The insights gained from this study illuminate the diverse microbial responses to warming and are vital for forecasting the soil microbiome’s impact on future carbon dynamics.