“…Our finding of a selective colonization of typical soil minerals encompassing species specific and predictable successional patterns has implications for the biogeochemical genesis, transformation and stability of the organo-mineral complexes. Clay minerals and iron oxyhydroxides affect biogeochemical processes through selective adsorption and protection of soil organic matter (Heckman et al, 2012), inactivation of extracellular enzymes, formation of organometal complexes (Finley et al, 2018) and provide opportunities for soil restoration and CO 2 mitigation (Baer et al, 2010;Babin et al, 2014). Moreover, physiological and biochemical differences between consecutive bacterial colonizers likely influence geochemical changes on mineral surfaces like weathering and aggregate formation (Lepleux et al, 2012;Ahmed and Holmström, 2015;Costa et al, 2018), the transformation and formation of organomineral complexes, and the accumulation of microbially derived soil organic matter (Kallenbach et al, 2016).…”