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The Sumatron rhino is considered a living fossil because it has changed very little over time. See link.

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13y ago

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What fish were examples of living fossils?

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What are non examples of fossils?

Some examples of non examples of fossils are as follows: knobby rocks, beautiful stones, bones. All fossils are rocks, and if bone fossils are found they will be much heavier than normal bone.


Are fossils examples of organic matter and why?

Yes, fossils are examples of organic matter because they are the preserved remains or traces of once-living organisms. Fossils can include bones, shells, teeth, and other organic materials that have undergone a process of mineralization or replacement with inorganic materials to become stone-like structures.


What are feeding breeding and living habits of rhinos?

feeding , breeding and living habits of rhino


How does the exaction of black rhinos effects other species?

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Living Large - 2011 Hippos and Rhinos 1-2 was released on: USA: 24 November 2011


What are examples of living fossils?

Examples of living fossils include the horseshoe crab, ginkgo tree, coelacanth fish, and nautilus. These are species that have remained relatively unchanged over millions of years and provide important insights into the Earth's evolutionary history.


What does living fossils mean?

An animal that lives on earth now but which has existed for such a long time that fossils of it are also known. Examples are:- The Coelacanth. The Horse Shoe Crab. The Ginkgo biloba The Elephant shrew The Trapdoor spider The Echidna The Crocodile (there are more)


What living things might you find in a very dry place?

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What are some non-examples of fossils?

Non-examples of fossils can include but not limited to:•A seashell found on the beach•A piece of driftwood•A footprint that your dog left yesterday


What is a rock formed from the remains of living things called?

A rock formed from the remains of living things is called a sedimentary rock. This type of rock is formed through a process known as lithification, where sediments such as dead plants or animals accumulate and become compacted over time. Examples include limestone, coal, and chalk.


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