Phosphoserine Charge State Drives Ion Condensation and Spatial Polyamine Presentation in Multirepeat Silaffin
Aditya Sonpal1, Jim Pfaendtner1
1Department of Chemical and Biomolecular Engineering, North Carolina State University, Raleigh, North Carolina 27695, United States.
The Journal of Physical Chemistry. B
|July 6, 2026
Summary
Diatom silaffins
Area of Science:
- Biomineralization
- Materials Science
- Biochemistry
Background:
- Diatom silaffins guide silica formation via modified repeat domains.
- The impact of post-translational modifications (PTMs) on silaffin structure is not well understood.
Purpose of the Study:
- Investigate how PTMs influence the conformational ensemble of diatom silaffins.
- Elucidate the role of phosphate charge state and ionic strength in silaffin organization.
Main Methods:
- All-atom molecular dynamics (MD) simulations of a 195-residue silaffin construct (Sil1p R1-R7).
- Simulated native and deprotonated phosphate variants under varying NaCl concentrations.
- Analyzed ensemble compaction, ion organization, and polyamine accessibility.
Main Results:
- Silaffin structure disorders from AlphaFold 3 predictions.
- Phosphate charge state, not salt concentration, dictates ensemble compaction and ion organization.
- Doubly deprotonated phosphate forms extensive Na+ shells and bridging networks, leading to a compact state with surface-exposed polyamines.
Conclusions:
- Silaffin compaction is driven by phosphate charge and ion bridging, creating structured intermediates.
- Repeat-scale organization is crucial and not evident from single-peptide studies.
- Findings advance understanding for creating hierarchical biomimetic silica materials.
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