Abstract

Although the biochemistry of bacterial and fungal siderophores has been intensively studied in laboratory cultures, their distribution and impacts on nutrient cycling and microbial communities in soils remain poorly understood. The detection of siderophores in soil is an analytical challenge because of the complexity of the soil matrix and their structural diversity. Liquid chromatography-mass spectrometry (LC-MS) is a suitable method for the sensitive analysis of siderophores in complex samples; however, siderophore extraction into liquid phases for analysis by LC-MS is problematic because of their adsorption to soil particles and organic matter. To determine extraction efficiencies of structurally diverse siderophores, spike-recovery experiments were set up with standards representing the three main siderophore classes: the hydroxamate desferrioxamine B (DFOB), the α-hydroxycarboxylate rhizoferrin, and the catecholate protochelin. Previously used solvent extractions with water or methanol recovered only a small fraction (< 35%) of siderophores, including < 5% for rhizoferrin and protochelin. We designed combinatorial chemical extractions (22 total solutions) to target siderophores associated with different soil components. A combination of calcium chloride and ascorbate achieved high and, for some soils, quantitative extraction of DFOB and rhizoferrin. Protochelin analysis was complicated by potential fast oxidation and interactions with colloidal soil components. Using the optimized extraction method, we detected α-hydroxycarboxylate type siderophores (viz. rhizoferrin, vibrioferrin, and aerobactin) in soil for the first time. Concentrations reached 461 pmol g–1, exceeding previously reported concentrations of siderophores in soil and suggesting a yet unrecognized importance of α-hydroxycarboxylate siderophores for biological interactions and biogeochemical processes in soil.

Highlights

  • Siderophores are produced by bacteria, fungi, and graminaceous plants to promote the chelation and uptake of the trace-nutrient iron (Fe)

  • Previous analyses of siderophores in soil showed the widespread presence of hydroxamate siderophores

  • water extracts from grassland soils revealed carboxylate phytosiderophores produced by graminaceous plants

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Summary

Introduction

Siderophores are produced by bacteria, fungi, and graminaceous plants to promote the chelation and uptake of the trace-nutrient iron (Fe). Siderophore Analysis in Soil by specific receptors, or by cell-surface reduction and uptake of Fe(II) Because they affect the availability of Fe, which can potentially limit microbial growth, siderophores play critical roles in host-microbe and microbiome interactions, including ‘tug-of-wars for iron’, ‘siderophore cheating’, and plant-growth promoting mechanisms (Haas et al, 2008; Swinburne, 2012; Butaiteet al., 2017). Siderophore production is induced by low intracellular iron concentrations, which are linked to iron bioavailability in the medium (Colombo et al, 2014) They provide a competitive growth advantage under conditions when the total iron concentration in the medium is replete, but the fraction of bio-available iron is low. Such conditions may be found in a biological host (Kramer et al, 2019) and in aerobic soil (Colombo et al, 2014)

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