Organic Molecular Replacement Fossilization
Organic molecular replacement fossilization is the precise process where minerals substitute organic polymers at the atomic level, preserving cellular architecture for millions of years. This hub article explains the chemical transition from cellulose and lignin to silica or calcite, highlighting the role of molecular templates and the critical pH balance required for success. Learn the difference between permineralization and total replacement, and discover why volcanic ash provides the ideal conditions for high-fidelity preservation. Featuring technical comparisons of silica vs. calcite and case studies on xylem petrification, this guide provides the scientific framework for understanding how biological structures become stone.
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