Effect of biocrusts on bacterial community composition at different soil depths in Mediterranean semi-arid ecosystems

This study analyzed the influence of biocrusts on the chemical properties and bacterial diversity and community composition in the underlying soils along a depth gradient (the biocrust (C1), middle (S2) and deep (S3) soil layers) in two semi-arid Mediterranean ecosystems. Organic carbon, pH, electric conductivity and calcium carbonate content were estimated by wet oxidation, potentiometrically (pHmeter), with a conductivity-meter and volumetrically with a Bernard calcimeter, respectively. Bacterial diversity and community composition were estimated by 16S rRNA gene high-throughput amplicon sequencing. Chemical properties in C1 were significantly different from the other soil layers, showing higher organic carbon content and lower pH (p < 0.05). The relative abundance of several bacterial taxa, such as Bryocella, Methylobacterium, Segitebacter and Actinomycetospora showed significant positive correlations with organic carbon (r = 0.53 to 0.75) and negative with pH (r = -0.72 to -0.84), and were also highly correlated with each other (p < 0.01), suggesting a bacterial co-occurrence pattern associated with the biocrust. On the contrary, other bacterial taxa, such as Euzebyaceae, Truepera, Alphaproteobacteria and Caldinilaceae, showed positive correlations with electrical conductivity and calcium carbonate and were also correlated with each other (p < 0.01), in a second type of co-occurrence pattern associated with bare soil. The C1 and S2 layers had several taxa in common, while S3 layers had taxa common to bare soil, suggesting that the effect of biocrusts was limited to the first centimeters of soil and progressively decreased in depth. Bacterial diversity was lower in C1 than in the underlying layers and increased progressively from biocrust to deeper soil layers. The results suggest that the diversity and composition of soil microbial communities in biologically crusted sites in Mediterranean semi-arid environments are mainly controlled by chemical properties which in turn are modified by the biocrust along a depth gradient.