Microbial communities,
which drive Earth’s geochemical cycles, can rapidly respond to change, but the proportion of this response that can be attributed to evolutionary processes, rather than species composition or gene expression shifts, remains an unresolved question. Most evolutionary rate estimates are available for nucleotide substitution rates and derive from laboratory measurements. It is difficult to know how relevant these rates are for geochemical environments, because studies on natural populations have been restricted to pathogens and endosymbionts.
We analyzed biofilms collected from a well-defined acid mine drainage system over 9 years to investigate the processes and determine rates of bacterial evolution directly in the environment. Population metagenomic analyses of the dominant primary producer yielded the nucleotide substitution rate, which we used to show that proliferation of a series of recombinant bacterial strains occurred over the past few decades. The ecological success of hybrid bacterial types highlights the role of evolutionary processes in rapid adaptation within natural microbial communities.