Abstract

AimsDespite little soil development and organic matter accumulation, lodgepole pine (Pinus contorta var. latifolia) consistently shows vigorous growth on bare gravel substrate of aggregate mining pits in parts of Canadian sub-boreal forests. This study aimed to investigate the bacterial microbiome of lodgepole pine trees growing at an unreclaimed gravel pit in central British Columbia and suggest their potential role in tree growth and survival following mining activity.MethodsWe characterized the diversity, taxonomic composition, and relative abundance of bacterial communities in rhizosphere and endosphere niches of pine trees regenerating at the gravel pit along with comparing them with a nearby undisturbed forested site using 16S rRNA high-throughput sequencing. Additionally, the soil and plant nutrient contents at both sites were also analyzed.ResultsAlthough soil N-content at the gravel pit was drastically lower than the forest site, pine tissue N-levels at both sites were identical. Beta-diversity was affected by site and niche-type, signifying that the diversity of bacterial communities harboured by pine trees was different between both sites and among various plant-niches. Bacterial alpha-diversity was comparable at both sites but differed significantly between belowground and aboveground plant-niches. In terms of composition, pine trees predominantly associated with taxa that appear plant-beneficial including phylotypes of Rhizobiaceae, Acetobacteraceae, and Beijerinckiaceae at the gravel pit and Xanthobacteraceae, Acetobacteraceae, Beijerinckiaceae and Acidobacteriaceae at the forest site.ConclusionsOur results suggest that, following mining activity, regenerating pine trees recruit bacterial communities that could be plant-beneficial and support pine growth in an otherwise severely N-limited disturbed environment.

Highlights

  • Forest landscapes around the world are subject to alteration by natural and anthropogenic disturbances, often leading to ecosystem degradation (Caviedes and Ibarra 2017)

  • No available P was detected in the soil samples from the gravel pit whereas undisturbed forest soils had a considerable amount of available P (Table S1)

  • We determined that the soil properties had no significant association with the bacterial operational taxonomic units (OTUs) (Fig. S1)

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Summary

Introduction

Forest landscapes around the world are subject to alteration by natural and anthropogenic disturbances, often leading to ecosystem degradation (Caviedes and Ibarra 2017). Disturbance regimes like resource extraction degrade forest soils through compaction and displacement of litter and soil, which affect the availability of nutrients in soils and inhibit root growth and obstruct the supply of oxygen and water to soil microbes and plant roots (Osman 2013) These impacts can alter the plant–soil–microbial dynamics and subsequently affect the normal ecosystem functioning (Bowd et al 2019). The establishment of pits and quarries for aggregate mining requires complete removal of natural vegetation and topsoil or in some cases even subsoil (Winfield and Taylor 2005), resulting in the loss of the existing biodiversity as plant and soil habitats are destroyed Artificial reclamation of such disturbed systems is one way to remediate ecosystem services, but it may involve costly procedures and the risk of introducing exotic floral and faunal species (Macdonald et al 2015). Our understanding is largely limited regarding how the assemblages of these pioneering aboveground and belowground biological communities have evolved to thrive in these disturbed ecosystems

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