Salt marshes gather a high diversity of prokaryotes across their environmental gradients. Most of this diversity and the factors determining their community assemblage are unknown. We massively sequenced a portion of the 16S gene to characterize the diversity of prokaryotes in soils from a salt marsh in Río Piedras, Southern Spain. We sampled in the four seasons, and in five plots dominated by a different halophyte (Spartina maritima, S. densiflora, Salicornia ramosissima, Arthrocaulon macrostachyum and Atriplex portulacoides) growing under different environmental conditions and representing different stages in the marsh ecological succession. Soil was sampled in their rhizosphere and adjacent bulk soil. We report the effects of different factors explaining prokaryotic beta diversity in the marsh: zonation (50 %), seasonality (14 %), and halophyte rhizosphere (7 %). Proteobacteria and Bacteroidota were the most abundant phyla. Firmicutes had a peak in winter and Desulfobacterota with other bacteria involved in sulfur cycling were abundant in the low marsh plots from S. maritima. Alpha diversity was highest in spring and decreased in winter. We detected a marked phylogenetic turnover between seasons and in rhizospheric soil respect to adjacent bulk soil for most pairwise comparisons. The effect of halophyte on its rhizosphere was species-specific, being S. maritima the species with more differentiated taxa between rhizosphere versus surrounding bulk soil. Our work highlights how the complex interaction between marsh zonation, seasonality and rhizosphere, onsets processes structuring bacterial community assemblage in salt marsh soils.
Keywords: Halophytes; Metabarcoding; Microbial ecology; Río Piedras; Salt marsh; bacteria.
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