- 1University of Natural Resources and Life Sciences Vienna, Institute of Soil Research, Department of Ecosystem Management, Climate and Biodiversity, Groß-Enzersdorf, Austria (andreea.spiridon@boku.ac.at)
- 2Institute of Analytical Chemistry, Department of Natural Sciences and Sustainable Resources, University of Natural Resources and Life Sciences, Vienna, Austria
- 3Institute of Applied Synthetic Chemistry, Vienna University of Technology (TU Wien), Vienna, Austria
Micronutrient (MN) deficiencies, particularly iron (Fe), zinc (Zn), and copper (Cu), severely limit crop productivity and frequently coincide with regions of human micronutrient malnutrition ("hidden hunger"), a problem exacerbated by high‑pH, calcareous soils that restrict metal availability through the formation of insoluble metal pools. In these challenging environments, grasses (Poaceae) rely on root exudates, most notably phytosiderophores (PS), to mobilize micronutrients such as Fe through the release of specialized ligands that promote metal dissolution and uptake.
However, the ecological complexity surrounding PS-driven micronutrient acquisition remains largely understudied, primarily due to limited availability of these compounds. Our previous work showed that grass species exhibit distinct PS exudation patterns, varying in both quantity and quality, with exudation decreasing in the order Fe > Zn > Cu deficiency. Building on these findings, we conducted detailed PS–soil interaction studies using naturally Zn- and Fe-deficient soils to examine whether specific PS types differ in their micronutrient mobilizing efficiency. Our results show that metal mobilization is soil-specific and largely dependent on the inherent availability of the metals themselves, following trends similar to the DTPA-extractable metal pool, i.e., the more available the metal, the more effectively it can be mobilized by PS. While soil properties primarily dictated overall mobilization patterns, differences among PS themselves also emerged. Despite their structural similarities, the eight PS displayed distinct mobilization efficiencies that changed with time and PS concentration.
Mobilization occurred rapidly within the first few hours but plateaued after approximately six hours, consistent with rapid PS depletion in an active rhizosphere. Notably, only a small fraction of the applied PS contributed to metal mobilization; most remained inaccessible, likely due to strong sorption to soil particles even under sterile conditions. When real root exudates were supplied together with PS, mobilization increased synergistically, enhancing the release of several metals, including Zn and Mn, beyond the capacity of PS alone.
These results highlight that MN acquisition is not a one-dimensional process but relies on multiple, complex rhizosphere interactions. Understanding these dynamics brings us closer to optimizing crop breeding and management practices that harness root exudation and soil potential for improved micronutrient uptake.
How to cite: Spiridon, A., Causon, T., Hann, S., Kratena, N., Stanetty, C., and Oburger, E.: Wanted: Micronutrients – Exploring the efficiency of phytosiderophores and grass root exudates in mobilizing metals in soils. , EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-9461, https://doi.org/10.5194/egusphere-egu26-9461, 2026.