Anoxic Conditions and Fossilization
Discover how anoxic conditions and fossilization work together to preserve ancient wood. This hub article explains why the absence of oxygen (below 0.5 mg/L) stops aerobic decay and enables the silica-replacement process. Learn the difference between volcanic “hard seals” and lacustrine “soft seals,” and why anaerobic bacteria are critical for creating the molecular template required for high-fidelity petrification.
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