Abstract

In extreme environments, the relationships between species are often exclusive and based on complex mechanisms. This review aims to give an overview of the microbial ecology of saline soils, but in particular of what is known about the interaction between plants and their soil microbiome, and the mechanisms linked to higher resistance of some plants to harsh saline soil conditions. Agricultural soils affected by salinity is a matter of concern in many countries. Soil salinization is caused by readily soluble salts containing anions like chloride, sulphate and nitrate, as well as sodium and potassium cations. Salinity harms plants because it affects their photosynthesis, respiration, distribution of assimilates and causes wilting, drying, and death of entire organs. Despite these life-unfavorable conditions, saline soils are unique ecological niches inhabited by extremophilic microorganisms that have specific adaptation strategies. Important traits related to the resistance to salinity are also associated with the rhizosphere-microbiota and the endophytic compartments of plants. For some years now, there have been studies dedicated to the isolation and characterization of species of plants’ endophytes living in extreme environments. The metabolic and biotechnological potential of some of these microorganisms is promising. However, the selection of microorganisms capable of living in association with host plants and promoting their survival under stressful conditions is only just beginning. Understanding the mechanisms of these processes and the specificity of such interactions will allow us to focus our efforts on species that can potentially be used as beneficial bioinoculants for crops.

Highlights

  • Soil salinization is a process of localised accumulation of soluble salts

  • It has been estimated that 33% of the irrigated agricultural land and over 20% of the total cultivated land of the world is saline

  • If the current trend of salinization is maintained, by 2050 we will see an approximately 30% increase in the cultivated land salinity. This means that agricultural productivity will be reduced due to the decline in cultivable land, with a consequent increase in the number of people suffering from hunger

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Summary

Introduction

Soil salinization is a process of localised accumulation of soluble salts. This phenomenon today is unanimously considered a severe threat to agricultural lands as it directly undermines the value and quality of soil (Ammari et al, 2013; Daliakopoulos et al, 2016). Soil salinity affects (directly or indirectly) both growth and reproduction of plants as a consequence of complex interactions between physicochemical properties of soil (salt content, poor aeration, an increase of crusting, hard setting, reduced infiltration, reduction of water uptake, and difficult root penetration) and plants’ morphological and physiological features (Rogers et al, 2005; Akbarimoghaddam et al, 2011).

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