Permineralization is the process of fossilization where mainly water mineral deposits take the form of the organism. The minerals harden with time and pressure from over laying deposits turning into rock.
Petrification happens when silica binds with celulose of a plant and turns into stone often retaining the microstructure of the plant.
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Permineralized fossil are formed when dissolved minerals precipitate from a solution in the space occupied by the organism's remains.
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The fossilizing process that replaces organic matter with silica or calcite is called permineralization. In this process, minerals such as silica or calcite fill in the pore spaces of the original organic material, creating a fossil with fine details preserved.
Permineralization is one of the ways in which a plant or animal can be turned into a fossil.
An anthropolite is a petrifaction of the human body, or of any portion of it.
permineralization
permineralization
permineralization
You have what is known as permineralization preservation when tiny spaces inside a fossil are filled in with minerals. This process can result in the fossil being preserved in great detail, often retaining the original structure of the organism.
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Petrifaction, also known as mineralization, occurs when organic matter is gradually replaced by minerals to form a fossil. It requires a slow and steady deposition of minerals, typically from groundwater, to encase and replace the original organic material. The process can take millions of years to complete.
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The process is call petrification, via permineralization.