Researchers compared five soils that suppressed C. paradoxa with five soils that allowed it to thrive. The suppressive soils had more culturable bacteria and were enriched in several bacterial groups, including Actinobacteria, Proteobacteria, Firmicutes and Acidobacteria. They also had higher pH, calcium content, cation exchange capacity, base saturation and sand content.

Adding calcium carbonate increased suppressiveness, especially when soil pH was 7.0. Transferring microbes from suppressive soils into soils that had been conducive to the pathogen, together with calcium carbonate, also induced suppressiveness. The findings point to a combined role for soil microbial communities and soil chemistry in limiting the fungus.