Temporal dynamics of total and active prokaryotic communities in two Mediterranean orchard soils treated with solid anaerobic digestate or managed under no-tillage

A field experiment was carried out to investigate the impact of two improved tillage systems (conventional tillage combined with the incorporation of solid anaerobic digestate, no-tillage) on the prokaryotic community composition in two tree orchard (olive, citrus) soils with contrasting texture, carbonate content and pH, located in Southern Italy. Soil samples were taken over a 5-month period to assess immediate (2 days) vs short-term (7 and 18 weeks) responses. Phylogenetic diversity and compositional shifts of both total and metabolically active soil prokaryotic communities were assessed by next-generation sequencing of 16S rRNA gene templates from soil-extracted DNA/RNA. In both digestate-treated soils, copiotrophic -Proteobacteria and oligotrophic Acidobacteria, Gemmatimonadetes, and Verrucomicrobia showed an immediate (2 days) but short-lived (7 weeks) shift in their relative abundance similar in persistence but not in magnitude. Whereas, selective soil-type dependent responses were observed for Actinobacteria, Chloroflexi, Firmicutes, and Planctomycetes. The autochthonous soil microbiota demonstrated resilience to the addition of the anaerobic digestate, and was dominated by Firmicutes, Bacteroidetes, Deinococcus-Thermus and Euryarchaeota (Methanomicrobia). Likewise, a temporary increase in the relative abundances of copiotrophic taxa (Firmicutes, Bacteroidetes, Thaumarcheota) was observed under conventional tillage, especially in the sandy loam (citrus) soil. Conversely, no-tillage favored the establishment of oligotrophic Chloroflexi and Verrucomicrobia in both soils. The active and the total prokaryotic communities differed from each other only in physically-disturbed soils. Soil management induced compositional shifts in the predominant microbial copiotrophic/oligotrophic community balance, whose persistence was linked to the tillage system, while magnitude depended on soil type.