The ancient rocks that explain why iron turns deadly inside your cells
Why This Matters
Deep in Earth's crust, iron-rich rocks react with water in ways that scientists have studied for decades — but no one thought to compare those reactions to the chemistry of dying cells, until now. These hypotheses suggest that the same iron-and-oxygen dynamics churning through ancient geology could be the hidden blueprint for ferroptosis, a form of cell death increasingly linked to cancer, Alzheimer's, and Parkinson's disease. If the connection holds, tools built to map volcanic rock chemistry could one day help doctors predict when a cell is about to self-destruct — and whether that destruction could be weaponized against tumors or stopped to protect the brain.
Compare Hypotheses
Ferritin Protein Shell as Kinetic Barrier Controlling Ferrihydrite Fenton Activity
The protein cage surrounding your cells' iron stores may be a safety vault keeping a potent chemical reactor under lock and key.
Impact: If confirmed, this hypothesis could reshape how researchers approach diseases involving iron dysregulation — from neu...
Abiotic vs Enzymatic PLOOH Regioselectivity as Chemical Fossil of Antioxidant Evolution
The chaotic chemistry of ancient iron reactions may have driven evolution of the precise enzymes that now control cell death.
Impact: If confirmed, this hypothesis could reshape our understanding of why ferroptosis exists at all — reframing it not as ...
PHREEQC Iron Speciation Model Predicts GSH-Dependent Fenton Activity Amplification
A geology chemistry tool may reveal why iron becomes deadly only in the final stages of a cell's self-destruction.
Impact: If confirmed, this framework could help researchers pinpoint a precise biochemical tipping point — a GSH concentratio...
Pourbaix Stability Field Mapping of Ferrihydrite-Catalyzed PLOOH Production
Ancient rock chemistry could explain exactly where and why iron triggers cancer-linked cell death.
Impact: If confirmed, this hypothesis could give researchers a predictive, quantitative framework for identifying exactly whi...
All Hypotheses
Click any hypothesis to see the full mechanism, evidence, and test protocol.
Ferritin Protein Shell as Kinetic Barrier Controlling Ferrihydrite Fenton Activity
The protein cage surrounding your cells' iron stores may be a safety vault keeping a potent chemical reactor under lock and key.
Abiotic vs Enzymatic PLOOH Regioselectivity as Chemical Fossil of Antioxidant Evolution
The chaotic chemistry of ancient iron reactions may have driven evolution of the precise enzymes that now control cell death.
PHREEQC Iron Speciation Model Predicts GSH-Dependent Fenton Activity Amplification
A geology chemistry tool may reveal why iron becomes deadly only in the final stages of a cell's self-destruction.
Pourbaix Stability Field Mapping of Ferrihydrite-Catalyzed PLOOH Production
Ancient rock chemistry could explain exactly where and why iron triggers cancer-linked cell death.