Abstract

Soil pH is probably the most important variable explaining bacterial richness and community composition locally as well as globally. In contrast, pH effects on fungi appear to be less pronounced, but also less studied. Here we analyze the community responses of bacteria and fungi in parallel over a local extreme pH gradient ranging from 4 to 8. We established the pH gradient by applying strongly alkaline wood ash in dosages of 0, 3, 9, 15, 30, and 90 t ha–1to replicated plots in aPicea abiesplantation and assessed bacterial and fungal community composition using high throughput amplicon sequencing 1 year after ash application. At the same time, the experiment investigated if returning wood ash to plantation forests pose any immediate threats for the microbial communities. Among the measured environmental parameters, pH was by far the major driver of the microbial communities, however, bacterial and fungal communities responded differently to the pH increment. Whereas both bacterial and fungal communities showed directional changes correlated with the wood ash-induced increase in pH, the bacterial community displayed large changes at wood ash dosages of 9 and 15 t ha–1while only higher dosages (>30 t ha–1) significantly changed the fungal community. The results confirm that fungi are less sensitive to pH changes than bacteria but also that fertilizing plantation forests with wood ash, viewed through the lens of microbial community changes, is a safe management at standard dosages (typically 3 t ha–1).

Highlights

  • Soil microorganisms as bacteria and fungi provide important ecosystem services as primary decomposers of organic matter (Bardgett, 2005), and as symbionts assisting plants with nutrient uptake (Whitman et al, 1998; Smith and Read, 2008)

  • Wood ash addition to the forest soil increased soil pH significantly from 3.8 in control plots, to 7.7 in plots treated with 90 t ha−1 of wood ash

  • Wood ash amendment and soil pH significantly correlated with the increasing concentrations of NH4, NO3, PO4

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Summary

Introduction

Soil microorganisms as bacteria and fungi provide important ecosystem services as primary decomposers of organic matter (Bardgett, 2005), and as symbionts assisting plants with nutrient uptake (Whitman et al, 1998; Smith and Read, 2008). PH effects on fungi are less pronounced, and the responses of fungal communities appear weaker than those of bacterial communities. PH appears to be a significant determinant for fungal communities, but typically not as the most important driver (Tedersoo et al, 2014; Bahram et al, 2018). In a global-scale study (Tedersoo et al, 2014), soil pH was one of the most important predictors of fungal richness. Specific fungal strains typically have a wider pH optimum, often covering a range of 5–9 pH units without significant inhibition of growth (Rousk et al, 2010; Bahram et al, 2018)

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