Minerals in water fill the spaces inside organic tissue. The process gives a record of soft tissue as well as hard tissues. Fossils with permineralization are useful in studying internal structures, especially of plants.
Water from the ground, lakes, or oceans seeps into the pores of organic tissue and forms a crystal cast with deposited minerals. Crystals begin to form in the porous cell walls. This process continues on the inner surface of the walls until the central cavity of the cell, the lumen, is completely filled. The cell walls themselves remain intact surrounding the crystals. Permineralization is different from petrification in that the organic material is only filled with minerals and not completely replaced. Permineralization can occur in several ways:
Types[change | change source]
Silicification[change | change source]
Silicification is the most common type of permineralization.
Carbonate mineralization[change | change source]
Carbonate mineralization occurs as coal balls. Coal balls are fossilizations of plants and their tissues, usually made when there is seawater or acidic peat. This type of fossilization gives information about plant life in the Upper Carboniferous (325 to 280 million years ago).
Pyritization[change | change source]
References[change | change source]
- Mani K. 1996. Permineralization, in Fossils: a window to the past. 
- Babcock, Loren E. "Permineralization", in AccessScience@McGraw-Hill, http://www.accessscience.com, doi:10.1036/1097-8542.803250
- Oehler, John H & Schopf, J. William 1971. Artificial microfossils: experimental studies of permineralization of blue-green algae in silica. Science, New Series 174: 1229-1231.
- Scott, Andrew C. & Rex G. 1985. The formation and significance of Carboniferous coal balls. Philosophical Transactions of the Royal Society B 311 (1148): 123–137.
- Raiswell R. 1997. A geochemical framework for the application of stable sulfur isotopes to fossil pyritization. Journal of the Geological Society. 154, 343-356.