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Updated: Mar 24, 2026

A Colorimetric Method for Measuring Iron Content in Plants
Published on: September 7, 2018
Evolutionary analysis of iron (Fe) acquisition system in Marchantia polymorpha
Jing-Chi Lo1,2, Munkhtsetseg Tsednee1, Ying-Chu Lo1
1Agricultural Biotechnology Research Center, Academia Sinica, Taipei, 11529, Taiwan.
The liverwort Marchia polymorpha acquires iron using a reduction-based strategy, similar to non-graminaceous plants. This ancient iron uptake mechanism, involving specific ZIP proteins, may have originated in early land plant ancestors.
Area of Science:
- Plant Biology
- Biochemistry
- Evolutionary Biology
Background:
- Vascular plants utilize distinct strategies for iron (Fe) acquisition: strategy I (reduction-based) for Fe(2+) and strategy II (chelation-based) for Fe(3+).
- The iron uptake mechanisms in bryophytes, early land plants, remain poorly understood.
Purpose of the Study:
- To elucidate the iron acquisition strategy employed by the liverwort Marchia polymorpha.
- To investigate the molecular basis of iron uptake in a representative non-vascular land plant.
Main Methods:
- Iron isotope fractionation analysis to determine the Fe acquisition pathway.
- Enzyme activity assays for ferric chelate reductase and proton ATPase under varying Fe conditions.
- Gene expression analysis (knockdown and overexpression) of identified ZIP homologs.
Main Results:
- Marchia polymorpha employs a reduction-based iron acquisition strategy, confirmed by isotope fractionation.
- Increased ferric chelate reductase and proton ATPase activity were observed under iron deficiency.
- Knockdown of MpZIP3 impaired growth in low iron, while overexpression enhanced iron content in high iron conditions, indicating its role in iron uptake.
Conclusions:
- The non-vascular liverwort Marchia polymorpha utilizes strategy I for iron acquisition.
- This ancient iron uptake system may have been present in the common ancestor of all land plants.
- The mechanism was likely co-opted from the gametophyte to sporophyte generation during land plant evolution.
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