Geoderma (Jun 2024)
Antarctic rock and soil microbiomes: Shared taxa, selective pressures, and extracellular DNA effects
Abstract
Highly adapted and often endemic microbial taxa inhabit soils and rocks of extremely cold and dry Antarctic deserts. However, the source populations of these organisms have not yet been clarified. Local hotspots, rather than worldwide wind dispersion, have been described as the primary sources of microbial diversity. In particular, the endolithic niche offers a buffered environment, where layered microbial communities have been described, whose dispersion due to rock fragmentation may influence the diversity and nutrient availability of the surrounding soils. On the other hand, microorganisms thriving in soils could be transported to rock surfaces and colonise them. However, the bacterial taxa that are differentially selected and those exchanged between these two substrata have never been defined before. Additionally, the microorganisms detected in these substrata using DNA-based approaches may not be alive but may correspond to fragments of extracellular DNA originated from dead cells. To identify the taxa that are shared between the two substrata, the selective filters that drive their distributions, and the effects of relic DNA on subsequent interpretations of community structure, colonized rock samples were collected from sandstone outcrops in three localities, as well as soil samples at increasing distances from the outcrops. Homogeneous samples were divided into aliquots, and one of each aliquot was treated for extracellular DNA depletion. Both native and treated samples were screened for their bacterial composition through 16S rRNA gene metabarcoding. The results provide the first demonstration of the strong selection of bacterial communities in rocks and soils, reporting some taxa potentially exchanged between the two substrates. Specifically, genera differentially selected between the two habitats were identified, likely due to their different microenvironmental conditions, such as differences in their thermal regimes. Additionally, extracellular DNA depletion had few effects at the taxonomic level and on the identification of differentially selected genera between the two substrata, but it increased the number of significant correlations of physicochemical variables with the diversity and composition of the soil microbial communities. These findings lead us to the conclusion that, despite the strong selection of the two substrates, there is microbial propagule interchange between soils and rocks in this environment. Extracellular DNA should be carefully considered since it has a significant impact on microbial diversity estimations.
