what is fossilization: The Tafonomia is the branch of paleontology that is dedicated to the study of fossils and the processes involved in their formation. This transformation from living organisms to fossils is what is known as fossilization and depends on certain circumstances for its success; so animals or plants do not always leave fossil records. Given the complexity of the phenomenon, doubts may arise about how a fossil is formed exactly or whether there are different types of fossilization and what their characteristics are. what is fossilization
What are fossils and how are they formed what is fossilization
Fossils are plant or animal remains that have been dead for a long time, which have not reached putrefaction and which, over the years, have become one more component of the earth’s crust. Its study, through the geological dating of rocks and phenomena at the planetary level, allows ordering the fossils in geological time , which is the time elapsed since the Earth was formed until today.
The process of fossil formation , called fossilization, is considered a complex natural cycle that depends on: the lack of oxygen, the rapid burial of organisms (generally in water sediment) and the paralysis of the decomposition process.
Obviously, there are fossilization processes in which the changes in the composition and structure of the organisms are minimal or scarce, which is why we speak of unaltered fossils (inclusion, mummification, freezing); however, there are also altered fossils (permineralization, carbonization, replacement) in which there is a drastic structural or chemical transformation. As indicated, fossils can be formed in a number of ways. Here is a brief explanation of how fossils are classified according to their formation .
These are the 3 types of fossilization according to the geological process :
Permineralization or petrification
It is the fossilization process by which the hard parts of an organism, made up of porous material and cavities, are covered by runoff water loaded with dissolved ions (silica, calcium carbonate, phosphates, sulfates, iron oxide) that occupies their interior, being able to cause the disappearance of the internal structure and the formation of crystals that preserve the surface structure of the organism. This type of mineralization, similar to the foundation process, is very common in dinosaur fossils . If these creatures are curious to you, here you can learn about herbivorous dinosaurs: names, types, characteristics and images and here about carnivorous dinosaurs: names, types, characteristics and images.
Printing or compression fossilization, very common in plants, occurs when the remains of organisms are subjected to high temperatures or high pressures exerted by rocks and other edaphic and subsoil materials.
Inclusion what is fossilization
This fossilization process occurs when organisms become trapped in conservative materials or environments. Depending on the conditions, 3 types of inclusion or embedding can be distinguished :
- Gelling or freezing: it is a fossilization more typical of glacial areas. The glaciations that have occurred on our planet have left numerous organisms preserved in whole (Siberian mammoth) or in part (mammoth hair in permafrost), buried under large layers of ice.
- Mummification: considered a pause in the disintegration process, without becoming a real fossilization, it originates after a massive loss of fluids in the organisms, which prevents the putrefaction of the organisms.
- Trapped in amber or pitch: Amber, which is a fossilized plant resin, preserves the external structure, but not the internal one, of organisms. Within the fossilization in amber it is common to find insects, spiders, frogs and lizards. With pitch, which is a very viscous hydrocarbon, the same thing happens. In general, Pleistocene fossils stand out, such as mammoths , mastodons, wolves, bison, saber-toothed lions , etc. what is fossilization
These are the 5 types of fossilization according to the physical process :
Disarticulation, which involves the separation of components from the remains of organisms, can occur during bioturbation processes, sediment compaction, or by phosyldiagenesis.
Fragmentation is a destructive process that is easy to identify in fossils, since it consists in their breaking, caused either by physical impacts or by the action of living beings.
This process is very common in marine fossils and consists of the removal or decomposition of materials from a hard substrate by the action of organisms. In these ecosystems, bioerosion is caused mainly by mollusks , sponges , crustaceans and fish , among others.
Abrasion what is fossilization
It consists of the erosion or wear of organic remains that end up being fossils through friction with water currents and also with air currents.
Corrosion is triggered by factors that promote chemical degradation and alter the surface of the fossil record.
These are the 5 types of fossilization according to the chemical process :
This type of fossilization is very common and consists of the replacement of hard organic remains by calcite, a mineral composed of calcium carbonate. Since the skeleton of corals is made up mostly of this material, fossilization through this process takes place rapidly.
This fossilization process, which consists of the substitution of organic components for carbon , characterizes the Carboniferous period, and is very common in plant remains and arthropods , due to its cellulose and chitin content, respectively. what is fossilization
Sometimes silica is derived from chemicals that allow fossilization, as is the case with chaldedonia. The most common fossils in this process are foraminifera, echinids, ammonites, gastropods, and brachiopods.
Pyritization what is fossilization
In pyritization, the organic parts of shells and skeletons are replaced by marcasite and pyrite, two types of iron sulfides, a product of the combination of sulfuric acid generated by the decomposition of marine organisms under anoxic conditions with the iron present in seawater. . what is fossilization
Phosphating what is fossilization
In this process, very common when there is a certain accumulation of vertebrate remains, the calcium phosphate present in bones and teeth, together with the calcium carbonate in the sediment, favors the formation of fossils.
Types of fossilization according to whether the organism is present
In addition to the types of fossils mentioned below, through the paleontological trace it is possible to obtain information about the organisms when they were alive. The ichnofossils (fossilized footprints or fossil footprints) can be found indoors, known as coprolites , or on the surface of the stratum, as is the case of dinosaur ichnites .
Corporal what is fossilization
In this type, the fossil preserves its skeleton to a greater extent. We have the example of the frozen mammoth and one closer to us, which we have surely seen at some time, the shells.
It is the impression or the filling of the fossils after dissolving their organic parts. If we see the shape printed, we speak of an external mold; On the contrary, if we observe that a tracing product of the internal filling of the organism has formed, we speak of an internal mold. what is fossilization
Fossil substances or chemical fossils
Fossil substances or chemical fossils can be found in geological materials, which turn out to be substances that were generated by the activity of extinct organisms and were trapped there. what is fossilization