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

AbstractA 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 α-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, which was dominated by Firmicutes, Bacteroidetes, Deinococcus-Thermus, and Euryarchaeota (Methanomicrobia). Likewise, a temporary increase in the relative abundances of copiotrophic taxa (Firmicutes, Bacteroidetes, Thaumarchaeota) 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

Soil slope exposure affects physico-chemical and microbiological properties in soil aggregate size fractions

Slope exposure is known to affect soil biogeochemical processes in mountainous forest ecosystems, but little attention has yet been paid to its influence at a soil aggregate scale. Therefore, we evaluated the effects of slope exposure (north- vs south-facing slope) on the physico-chemical and microbiological properties of bulk soil and dry-sieved and water-stable aggregate size fractions in both organic (OF) and mineral (AE) horizons in an Italian alpine forest. The changes in organic carbon (OC) and nitrogen (ON) fractions were assessed together with a battery of thirteen enzyme activities involved in the main nutrient cycles. In addition, soil biological properties including microbial biomass (estimated as double-stranded DNA content), and microbial activity (assessed as the ratio between the extra-(exDNA) and intracellular (iDNA) fractions of the total soil DNA pool) were determined. The OF horizon at the north-facing slope was enriched in recalcitrant and insoluble OC and ON fractions and characterized by a lower microbial activity, as indicated by the higher exDNA/iDNA ratio with respect to the south-facing slope. On the contrary, exDNA and iDNA contents, microbial biomass, as well as most of the enzyme activities, reached higher levels at the southern exposure in the AE horizon. These exposure-effects were bulk soil- and aggregate size fraction-specific. Overall, lower values of the chemical and microbiological parameters were found in the water-stable fraction. Our findings indicate that slope exposure (and thus topography), soil horizon, and aggregate size distinctly influence soil OC dynamics in mountain ecosystems

Soil slope exposure affects physico-chemical and microbiological properties in soil aggregate size fractions

Slope exposure is known to affect soil biogeochemical processes in mountainous forest ecosystems, but little attention has yet been paid to its influence at a soil aggregate scale. Therefore, we evaluated the effects of slope exposure (north- vs south-facing slope) on the physico-chemical and microbiological properties of bulk soil and dry-sieved and water-stable aggregate size fractions in both organic (OF) and mineral (AE) horizons in an Italian alpine forest. The changes in organic carbon (OC) and nitrogen (ON) fractions were assessed together with a battery of thirteen enzyme activities involved in the main nutrient cycles. In addition, soil biological properties including microbial biomass (estimated as double-stranded DNA content), and microbial activity (assessed as the ratio between the extra-(exDNA) and intracellular (iDNA) fractions of the total soil DNA pool) were determined. The OF horizon at the north-facing slope was enriched in recalcitrant and insoluble OC and ON fractions and characterized by a lower microbial activity, as indicated by the higher exDNA/iDNA ratio with respect to the south-facing slope. On the contrary, exDNA and iDNA contents, microbial biomass, as well as most of the enzyme activities, reached higher levels at the southern exposure in the AE horizon. These exposure-effects were bulk soil- and aggregate size fraction-specific. Overall, lower values of the chemical and microbiological parameters were found in the water-stable fraction. Our findings indicate that slope exposure (and thus topography), soil horizon, and aggregate size distinctly influence soil OC dynamics in mountain ecosystems.Austrian Science Fund | Ref. I989-B16Ministerio de Economía, Industria y Competitividad | Ref. RYC-2016-2123