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Option 1 : Petrification
The correct answer is Petrifaction.
Concept:
- Fossilization is defined as the physical, chemical and biological processes that lead to the preservation of plant and animal remains over time.
- Some common methods of fossilization are petrifaction, permineralization, compression, casts and molds.
- Petrifaction is the process by which biological material transforms into a fossil by replacing the original material and filling the original pore spaces with minerals.
- The fossils formed as a result of this process typically contain a significant amount of the original material of the specimen.
- Groundwater containing dissolved minerals fills the pore spaces and cavities of specimens, most notably bone, shell, or wood.
- When these minerals precipitate out of the water, they fill the pores of the organisms tissues.
- These are the best, but most rare, types of fossils because they preserve both the external forms and the internal structures.
- The cellular details are preserved due to the infiltration of minerals like MgCO3, CaCO3, SiO2, FeS, etc. into the tissue.
- Pseudofossils:
- Inorganic rocks that appear to be fossils are sometimes mineral deposition.
- Compression:
- Plant parts such as leaves, stems, and seeds are compressed by the sediments' vertical pressure.
- Flattened plant parts are retained as thin carbonaceous films and the outline of external features.
- Internal structures are generally not preserved.
- Incrustation:
- The deposition of carbonate minerals and iron occurs in the form of a hard cast or incrustation around the plant parts.
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