“…Compared with the hyporheic zone, pristine groundwater environments (in the absence of surface water impacts) are more stable and only experience little environmental changes (Griebler and Lueders, ), which may promote the effect of stochastic processes on community assembly compared with more dynamic environments (Ofiţeru et al ., ; Stegen et al ., ; Wang et al ., ; Zhou et al ., ). Moreover, in contrast to the typically studied biofilms in other environments like surface waters, which form dense, spatially coherent, heterogeneous structures that can reach a thickness in the range of several 100 micrometres (Battin et al ., ), sediment‐attached microbial communities in groundwater aquifers occur as small, patchily distributed microcolonies that consist of only a few cells (Schmidt et al ., ), which may be hypothesized to be more prone to stochastic effects than their biofilm counterparts in other environments.…”