fossil replacement is when you Suck MY MEAT ! ;D
it gives information about the past which to scientists is important to know
fossils found in tar
They are fossils and fossils are fossils er gars tyre true Joy God
Trace Fossils!
Fossils can be formed by:MummificationPetrificationDesiccationRelated question on Answers.com:How are fossils formed?
The terms are fossils.
They are known as fossils.
In simplest terms, fossils show what living things were like long ago.
The terms are fossils.
It is called replacement .
Well, not all scientists study fossils but some who participate in the art paleontology do. Anyway, here's the answer to your question: scientists study fossils to learn about the bone's past and who they might've belonged to to put it in layman's terms (simplified terms)
Residual structures and fossils.
Fossils can form from both soft parts and hard parts of organisms. Soft parts can become fossilized through processes like carbonization or preservation in amber, while hard parts like bones or shells can undergo mineralization or replacement to become fossils.
Petrified fossils occur when organic material, such as wood, transforms into stone through a process called permineralization, where minerals infiltrate the cells and replace the original organic material. In contrast, replacement fossils form when the original material is dissolved and replaced by minerals, resulting in a replica of the original structure. While both processes involve mineralization, petrified fossils maintain some original structure, whereas replacement fossils may be more complete replicas of the original organism.
Petrified feces is also called coprolite. It is body waste that has turned into stone. In terms of fossils, they are considered trace fossils, not body fossils. Paleofeces is the name for ancient human waste.
it gives information about the past which to scientists is important to know
Fossils created when minerals gradually replace the organic material of an organism, preserving its shape and structure, are called petrified fossils or replacement fossils. Over time, the original material is dissolved, and minerals fill the space, creating a fossilized replica of the organism.