Poster
Milena Malisic
PhD student
Max Planck Institute for Plant Breeding Research, Cologne, Germany
Köln, Nordrhein-Westfalen, Germany
Charles Copeland (he/him/his)
Max Planck Institute for Plant Breeding Research
Köln, GERMANY
Anton Amrhein
Master student
Max Planck Institute for Plant Breeding Research, Cologne, Germany
Cologne, Nordrhein-Westfalen, Germany
Pengfan Zhang
Postdoc
Innovative Genomics Institute, University of California, Berkeley
Berkeley, California, United States
Stanislav Kopriva
Group Leader/Prof. Dr.
Botanical Institute, Cluster of Excellence on Plant Sciences (CEPLAS), University of Cologne, Cologne, Germany
Köln, Nordrhein-Westfalen, Germany
Sabine Metzger
Group leader
Cologne Biocenter, Cluster of Excellence on Plant Sciences, Mass Spectrometry Platform, University of Cologne, Cologne, Germany
Cologne, Nordrhein-Westfalen, Germany
Ruben Garrido-Oter
Max Planck Institute for Plant Breeding Research
Cologne, GERMANY
Nicolaus von Wirén
Director
Leibniz-Institute of Plant Genetics & Crop Plant Research
Gatersleben, Sachsen-Anhalt, Germany
Ricardo F.H. Giehl
Group leader
Leibniz-Institute of Plant Genetics & Crop Plant Research
Gatersleben, Sachsen-Anhalt, Germany
Paul Schulze-Lefert
Professor
Max Planck Institute for Plant Breeding Research
Köln, Nordrhein-Westfalen, Germany
Coumarins are a structurally and functionally diverse class of specialized metabolites in flowering plants that are secreted by roots in response to iron deprivation and play a key role in iron mobilization from soil. Environmental signals such as soil pH result in distinct coumarin secretion profiles and integration of this signal is important for effective iron uptake by roots. Although it is known that at circumneutral pH coumarins exuded by roots are essential for root microbiota-mediated mobilization of unavailable iron (Fe3+) in Arabidopsis thaliana, it remains unclear whether the bacterial root microbiota also contributes to plant iron nutrition at acidic pH. We show here that at circumneutral or acidic environmental pH, different coumarin structure types cooperatively interact with the root-associated bacterial microbiota, leading to increased iron mobilization either by Fe3+ chelation or Fe3+ reduction. Microbiota-mediated Fe3+ reduction at acidic pH eliminates the need for A. thaliana ferric chelate reductase, which is essential for the reduction of iron at the root surface of axenic plants. Collectively, our work indicates a ubiquitous role of the microbiota in iron mobilization from soil that becomes integrated in the adaptive response of the host to prevailing edaphic conditions.