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Updated: Feb 1, 2026

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Cavity acidification limits ferritin iron biomineralization
Zhiheng Wang1, Yiwen Wang1, Ivan J Dmochowski1
1Department of Chemistry, University of Pennsylvania, 231 S. 34th Street, Philadelphia, PA 19104-6323, USA.
Journal of Inorganic Biochemistry
|January 30, 2026
Summary
This study reveals how ferritin stores iron by tracking proton release during iron oxidation. Ferritin accumulates protons internally, acting as a brake on iron biomineralization.
Area of Science:
- Biochemistry
- Biomineralization
- Protein Engineering
Background:
- Ferritin biomineralization studies focus on iron pathways and oxidation mechanisms.
- Spatiotemporal details of proton generation during iron hydrolysis are less understood.
Purpose of the Study:
- Investigate proton generation and release during ferroxidase reactions within Archaeoglobus fulgidus ferritin (AfFtn).
- Utilize site-specific labeling and fluorescence probes to monitor internal proton activity.
Main Methods:
- Engineered cysteines on AfFtn interior surface for covalent labeling with fluorescein-5-maleimide (F5M).
- Performed ferroxidase reactions and monitored F5M fluorescence quenching and bulk solution pH.
- Reassembled AfFtn 24mer cage from dimers at high ionic strength.
Main Results:
- F5M labeled at D61C (C61-F5M) effectively reported proton activity without Fe ion quenching.
- Internal cavity pH dropped to apparent 5.5 within 15s of Fe2+ addition.
- Ferritin released 1.6H+ per Fe2+ oxidized, retaining 0.4H+, indicating internal proton accumulation.
Conclusions:
- Ferritin accumulates protons within its cavity, acting as a regulatory brake on iron biomineralization.
- Internal proton buffering influences the kinetics of iron oxidation and release.
- The study provides novel insights into the spatiotemporal dynamics of proton activity in ferritin.
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