The project demonstrated that the soil fauna is highly sensitive to drought events occurring in forests. If forest soils become too dry, this inhibits the activity and the quantity of soil organisms and forests may absorb less carbon in the long term. This finding is significant in a climate change perspective, because through dead-litter feeding, soil organisms ultimately bind the carbon in the CO2 from the atmosphere into the soil humus, where it is stored over long periods of time.
The researchers additionally developed a novel approach to trace the origin of organic matter in soils. By analysis of hydrogen composition in the organic matter, researchers were able to disentangle the contribution from foliage, roots, and fungi to the build-up of organic matter in soils. Thus, this method has the potential to provide a faster and cost-effective way to analyze the sources of organic matter in soils, which still represent one of the key unknowns for the understanding of soil organic matter responses to climate change.
The results obtained in this project will improve the prediction of soil organic matter and soil carbon changes in response to increasing frequency of drought events, and thus will be highly relevant not only for scientists but also stakeholders and policy-makers to face pressing climate change challenges.