Fungal organic acid uptake of mineral derived K is dependent on distance from carbon hotspot

Abstract

Fungal mineral weathering processes regulate the bioavailability of inorganic nutrients from mineral surfaces to organic matter and increase the bioavailable fraction of nutrients. Fungal mineral weathering strategies can be classified as biomechanical (direct) or biochemical (indirect). In the case of fungal uptake of mineral nutrients through indirect weathering, it is widely hypothesized that uptake of mineral derived nutrients occurs through organic acid chelation, but such processes have not been directly visualized. This is in part due to challenges in probing the complex and heterogeneous soil environment. Here, using an epoxy-based mineral doped soil micromodel platform that we developed, which mimics soil mineralogy and structure, it permitted us to visualize and spatially probe the molecular mechanisms of mineral weathering. Mass spectrometry imaging revealed differences in the distribution of fungal exudates, citric acid and tartaric acid, on the soil micromodels in presence of minerals. Citric acid was detected closer to the nutrient rich inoculation point, whereas tartaric acid was highly abundant away from inoculation point. This suggested that the organic acid exuded by the fungi depended on the proximity from the carbon rich organic substrate at the point of inoculation. Using a combination of X-ray fluorescence and X-ray near edge structure analysis, we identified citric acid- and tartaric acid-bound K within fungal hyphae networks grown in the presence of minerals. Combined our results provide direct evidence that fungi uptake and transport mineral derived nutrient organic acid chelation. The results of this study provided unprecedented visualization of fungal weathering of soil minerals and hyphal K+ transport, while resolving the indirect weathering mechanism of fungal K uptake from mineral interfaces.