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What is a fossil in biology?
What is a fossil and why is it important?
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What do fossils tell us about prehistoric animals and plants?
What are body fossils?
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Oct 27, 2020 · A fossil is the mineralized partial or complete form of an organism, or of an organism’s activity, that has been preserved as a cast, impression or mold. A fossil gives tangible, physical evidence of ancient life and has provided the basis of the theory of evolution in the absence of preserved soft tissues.
What is a fossil? A fossil is the preserved remains or traces of a dead organism close organism Any living thing, which includes insects, plants and animals, is an organism....
Feb 28, 2024 · Definition. A fossil is the preserved remains, impression, or trace of any once-living organism from a past geological age. These include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood, oil, coal, and DNA remnants.
Oct 22, 2024 · fossil, remnant, impression, or trace of an animal or plant of a past geologic age that has been preserved in Earth’s crust. The complex of data recorded in fossils worldwide—known as the fossil record —is the primary source of information about the history of life on Earth.
- The Editors of Encyclopaedia Britannica
Jul 24, 2022 · Fossils include shells, imprints, burrows, coprolites and organically-produced chemicals. The oldest fossils were bacteria that existed 3.8 billion years old. Fossils are once thought of to be all from extinct species until some were found to belong to species that are still living.
A fossil is the preserved evidence of an organism that lived in the distant past. Some fossils are formed from body parts, such as shells or bones. Others, such as preserved footprints, are from traces of an organism’s behaviors. Fossils are usually found in sedimentary rock.
Fossils are physical evidence of prehistoric animals and plants. They tell us about the history of our planet, from climate and evolution to diets and diseases. There may be more to these prehistoric remains than you ever realised. When an organism dies and is quickly covered by layers of mud, sand or silt, it has the potential to become a fossil.