Permineralization is one of the ways in which a plant or animal can be turned into a fossil.
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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.
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.
The process is call petrification, via permineralization.
freezing (refrigeration), drying (dessication), asphalt, amber, carbonization (distillation), permineralization
Some examples of permineralization include petrified wood, where organic matter is gradually replaced by minerals to create a fossilized version of the wood. Another example is fossilized bones, where minerals have replaced the organic material in the bone structure, preserving its shape and structure. In both cases, the process of permineralization involves minerals filling in the pores and voids of the organic material, essentially turning it into a rock-like structure.
Permineralized fossil are formed when dissolved minerals precipitate from a solution in the space occupied by the organism's remains.
The typical sequence or order of fossilization is when a plant or animal dies parts are preserved by freezing, mummification, distillation, or permineralization.
Permineralized or petrification wood is form when an organic material is converted into stone. This is accomplished by replacing the original material and filing with minerals. The finest petrified wood involves amorphous silica.
In geology, petrification or petrification is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals. So yeah the answer is petrification