Diagnosis of Sulphur Nutrition

The Versatile Roles of Sulfur-Containing Biomolecules in Plant Defense-A Road to Disease Resistance

Sulfur (S) is an essential plant macronutrient and the pivotal role of sulfur compounds in plant disease resistance has become obvious in recent decades. This review attempts to recapitulate results on the various functions of sulfur-containing defense compounds (SDCs) in plant defense responses to pathogens. These compounds include sulfur containing amino acids such as cysteine and methionine, the tripeptide glutathione, thionins and defensins, glucosinolates and phytoalexins and, last but not least, reactive sulfur species and hydrogen sulfide. SDCs play versatile roles both in pathogen perception and initiating signal transduction pathways that are interconnected with various defense processes regulated by plant hormones (salicylic acid, jasmonic acid and ethylene) and reactive oxygen species (ROS). Importantly, ROS-mediated reversible oxidation of cysteine residues on plant proteins have profound effects on protein functions like signal transduction of plant defense responses during pathogen infections. Indeed, the multifaceted plant defense responses initiated by SDCs should provide novel tools for plant breeding to endow crops with efficient defense responses to invading pathogens.

Shifts in desulfonating bacterial communities along a soil chronosequence in the forefield of a receding glacier

Forefields of receding glaciers are unique and sensitive environments representing natural soil chronosequences, where sulfate availability is assumed to be a limiting factor. Bacterial mineralization of organosulfur is an important sulfate-providing process in soils. We analyzed the diversity of sulfonate-desulfurizing (desulfonating) bacteria in the Damma glacier forefield on the basis of the key gene asfA by terminal restriction fragment length polymorphism and clone libraries. The community structure and sequence diversity of desulfonating bacteria differed significantly between forefield soils deglaciated in the 1990s and the 1950s. Soil age had a strong effect on the desulfonating rhizosphere communities of Agrostis rupestris, but only a slight impact on the ones from Leucanthemopsis alpina. AsfA affiliated to Polaromonas sp. was predominantly found in the more recent ice-free soils and the corresponding rhizospheres of A. rupestris, while a group of unidentified sequences was found to be dominating the matured soils and the corresponding rhizospheres of A. rupestris. The desulfonating bacterial diversity was not affected by varying levels of sulfate concentrations. The level of asfA diversity in recently deglaciated soils suggests that desulfonating bacteria are a critical factor in sulfur cycling, with defined groups dominating at different stages of soil formation.