1. Petrification
  2. Pseudofossil
  3. Compression
  4. Incrustation
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1 Answers

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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