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∙ 14y agoA trace fossil is formed by a footprint, trail, burrow, or other mark that an organism left in soft sediment.
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∙ 15y agoA trace fossil is evidence of an organism's activity (like footprints, burrows, or coprolites) but is not made of the organism itself. Trace fossils provide valuable information about the behavior and ecology of ancient organisms.
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∙ 14y agoA fossilized footprint or dung
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∙ 14y agotrace
This would be considered a trace fossil, specifically a "ichnofossil" which is a fossilized footprint, burrow, or other trace left by an organism rather than the remains of the organism itself.
Another kind of fossil is a mold or cast fossil, which forms when an organism's remains decay and leave an impression in the surrounding sediment that is later filled with minerals. Another type is a trace fossil, which is evidence of an organism's activity, like footprints or burrows, preserved in rock.
A prehistoric worm burrow is called a trace fossil. Trace fossils are preserved evidence of the activity of organisms, such as burrows, footprints, or feeding marks, rather than the remains of the organisms themselves.
You have what is known as permineralization preservation when tiny spaces inside a fossil are filled in with minerals. This process can result in the fossil being preserved in great detail, often retaining the original structure of the organism.
The fossil record supports the idea of evolution by showing a progression of life forms over time, with species changing and adapting to their environments. This evidence aligns with the theory that species have evolved from common ancestors.
This would be considered a trace fossil, specifically a "ichnofossil" which is a fossilized footprint, burrow, or other trace left by an organism rather than the remains of the organism itself.
Another kind of fossil is a mold or cast fossil, which forms when an organism's remains decay and leave an impression in the surrounding sediment that is later filled with minerals. Another type is a trace fossil, which is evidence of an organism's activity, like footprints or burrows, preserved in rock.
Personal beliefs and opinions are not a kind of evidence used to support evolutionary theory. Scientific evidence such as fossil records, DNA analysis, and observational data are the main sources of evidence.
A prehistoric worm burrow is called a trace fossil. Trace fossils are preserved evidence of the activity of organisms, such as burrows, footprints, or feeding marks, rather than the remains of the organisms themselves.
what kind of fossil is what!
foot prints and ammonites mainly, but any kind of organism if it had any contact with mud, under the right condition, it might just becomes a fossil
it was a dino and more things added to his list but he did'nt add it to the list.
Dinosaur footprints are called trace fossils because they show evidence of animal activity. Worm holes and burrows can also be fossilized, falling into the 'trace fossil' category.
AnswerThe fossil record is the primary source of evidence of past life forms.The fossil record is also an important source of evidence of evolution. However, Charles Darwin was able to develop his Theory of Evolution by Natural Selection largely without reference to fossil evidence. He saw evidence for evolution in present life forms. Another source of evidence for evolution is to be found in DNA.
The fossil record supports the idea of evolution by showing a progression of life forms over time, with species changing and adapting to their environments. This evidence aligns with the theory that species have evolved from common ancestors.
No, a cast fossil is not the same as a carbonized fossil. Cast fossils are formed when minerals fill in the cavity left by a previously existing organism, while carbonized fossils are formed when organic materials are compressed and heated, leaving a carbon residue of the original organism. Both types of fossils preserve the shape of the organism, but through different processes.
A fossil of this type is called an impression fossil. It forms when an organism's body creates an imprint in soft mud or sediment, which then hardens into rock and preserves the shape of the organism but not its actual remains. These fossils provide important information about ancient organisms and their environments.