TRANSMISSION // 2026.10.23.761470v1 AI ADAPTED
Rice may sense soil pH through changes in iron availability
A bioRxiv preprint proposes that rice responds to root-zone pH partly through iron availability and interactions between jasmonate and auxin signaling.

Changes in iron availability may help rice interpret the acidity or alkalinity of its root environment, according to a study described in a bioRxiv preprint.
What the study found
Singh and colleagues report that rice responses to rhizospheric pH—the pH of the soil environment around roots—are linked to changes in the relative availability of iron. The authors propose that plants interpret relatively greater iron toxicity under acidic conditions and iron deficiency under alkaline conditions through crosstalk between jasmonate (JA) and auxin, two plant hormone signaling systems.
The researchers used root-specific RNA sequencing, inductively coupled plasma mass spectrometry (ICP-MS), hormone measurements and physiological validation. Their abstract describes iron availability as a critical factor in the response, but does not provide numerical results or identify the specific genes involved.
Why it matters
Root-zone pH influences many aspects of plant physiology and development, yet how plants perceive it remains incompletely understood. The authors’ proposed mechanism offers a way to think about pH responses in terms of nutrient availability and hormone signaling rather than pH alone. It could help guide further research into how rice responds to different root environments.
Limits and unknowns
This account is based on the abstract of a bioRxiv preprint, not a full assessment of the paper. The abstract does not specify sample sizes, experimental conditions, effect sizes or the details of the physiological validation. It also does not establish whether the proposed mechanism applies to other plant species or field conditions.
- rice
- rhizosphere
- soil pH
- iron availability
- jasmonate
- auxin
- plant signaling