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Definition:
Fossils Organisms are the remains of plants and animals whose bodies were buried in the soil in the form of sand and mud at the bottom of old seas, lakes, and rivers. Organic life has any preserved traces that are usually more than 10,000 years old. The soft parts of the body burn out immediately after death, but hard parts like bones, shells, and teeth can be replaced by minerals that become harder. In very rare cases, soft parts of the body such as feathers, plant ferns, or other evidence of life such as footprints or dung can be preserved.
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Why we need Research over Fossils?
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Process of Fossil Formation:
Fossils are the process of transforming a plant or animal into a fossil. These small structures and a small part of the plants that existed six hundred years ago are still preserved as fossils. This may come as a surprise considering the millions of fossils collected over the years and the fact that they still contain billions of rocks. Plants and animals that normally turn into fossils and suffer and, with a few exceptions:-
Several Important Processes
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Each process usually follows the 6 previously mentioned steps: decay, removal, and burial. Consider using the same method to bake two cakes and use a different set of ingredients for each cake. In our case, cake cakes and fossilization are the way to go.
Fossils Invertebrates:
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Fossils Vertebrates:
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Modes of Preservation
There are Methods of care the eight vital categories are commonly known. Although these categories are well defined, a particular creature can fall into several categories or avoid them all. As a result, these categories should be considered as a way of care rather than a shoebox where all living things should be included. When thinking about organic varieties and methods of care, There is more important to consider the lack of biological information or the existence of more specific classifications than the organization. In addition to this consciousness, other creatures also have biological substances that protect ancient creatures (human bodies):-
1. Unaltered remains: The original fabric may be slightly deformed whole, dry, frozen, or preserved in amber.
2. Compression- impression: 2-dimensional flattened organic matter with or without film.
3. Mold−cast: 3-dimensional care where reality does not exist
4. Recrystallization: Aragonite returns to calcite or can be converted to dolomite.
5. Permineralization: Mineral fluid affects the cells of the body without losing real substances (except for the contents of the cells).
6. Dissolution−Replacement: The original substance dissolves and is replaced by another mineral. Organic body in which the body of an organism no longer exists, but some evidence of its existence remains.
7. Molecular fossils: The molecules that remain in the geographical record have no trace of other organisms. Some examples of biochemical degradation products of chlorophyll, flavonoids, collagen, DNA, lipids, and proteins.
8. Trace fossils: There are traces, pits, and other evidence that there were creatures.
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