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In the environment of Alpine glacier forefields, bacteria represent the functional link between initial soil development and secondary colonization. An important question is whether soil bacteria are adapted to the poor nutrient availability in this environment and whether selection processes significantly limit their local expansion along the gradients of chemical and biological factors. To address these questions, we used a two-dimensional sampling strategy at our study site, the Damma glacier forefield, Switzerland, to characterize the soil environment by selected biogeochemical parameters. Our results revealed two contrasting sites that differed in time since deglaciation (‘young’ and ‘old’ soil, ≤ 13 years and > 53 years of ice-free conditions) and vegetation cover (threefold increase), but also showed significant differences in soil properties thought to be relevant for the successional development of glacier forefield soils, such as pH (0.5-fold decrease), ammonium (0.5-fold decrease) concentration, and the content of total organic carbon (10-fold increase). Isolated strains, affiliated to the genus Pseudomonas, according to their 16S rDNA profile, were tested experimentally for local adaptation by a reciprocal transfer experiment. The bacteria from both young and old soils showed a significant interaction with their local environment; the direction of the interaction, however, did not follow the expected pattern of local adaptation. The significant genoype-with-environment interaction indicates a limited local expansion of soil bacteria in the Damma glacier forefield over the range of only 110 m. The lack of local adaptation could be explained by environmental constraints such as exclusion of competition, different migration behaviour of bacteria from young and old soil, or the ability of early colonizing bacteria to survive under the glacier ice. [ABSTRACT FROM AUTHOR]