Explainer: How a fossil forms | Science News for Students

Explainer: How a fossil forms

Jun 18, 2014 — 8:30 am EST

A collection of nearly 200-million-year-old fossils that the author retrieved from the beach on England’s “Jurassic Coast” during a recent vacation. 

Sarah Zielinski

Most times, when a living thing dies, it just rots. It leaves no trace that it was ever there. But when the conditions are just right, a fossil may form.

For this to happen, the organism typically must first become quickly buried in sediment on the floor of the sea or some other body of water. Sometimes it may even land in something like a sand dune. Over time, more and more sediments will pile atop it. Eventually compressed under its own weight, this growing accumulation of sediment will transform into hard rock.

Most organisms buried in that rock will eventually dissolve. Minerals may replace any bone, shell or once-living tissue. Minerals also may fill in the spaces between these hard parts. And so a fossil is born.

Some of these fossils contain important information about how an animal lived or died. Or they might even provide clues to ancient climate.

Fossils come in other forms, too. They can be any trace of an ancient living thing. For instance, scientists consider ancient, preserved footprints and burrows to be fossils. For these trace fossils to form, the impression they make on sediment has to quickly harden or get buried in sediment and remain undisturbed until it can be transformed into rock. Even animal poop can form trace fossils, called coprolites.

Most people associate fossils with animals. But plants and other types of organisms also can leave preserved traces. And they tend to form in much the same way as animal fossils. A special type of fossil is called petrified wood. It forms in the same way as do fossils of dinosaurs or other creatures. They often look similar to real wood, though. In this case, colorful minerals have moved in and replaced tree tissue.


Power Words

coprolite    Fossilized feces. The word coprolite, in Greek, means “dung stones.” Coprolites are very important because they can provide direct evidence of what ancient creatures ate.

fossil    Any preserved remains or traces of ancient life. There are many different types of fossils: The bones and other body parts of dinosaurs are called “body fossils.” Things like footprints are called “trace fossils.” Even specimens of dinosaur poop are fossils.

mineral    A chemical compound that is solid and stable at room temperatures and has a specific formula, or recipe (with atoms occurring in certain proportions) and a specific crystalline structure (meaning that its atoms are organized in certain regular three-dimensional patterns).

petrify    To turn once-living tissue into stone, usually over many millennia or longer. Petrified trees are a prime example.

sediment    Material (such as stones and sand) deposited by water, wind or glaciers.


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Further Reading

S. Zielinski. "Fossil hunting can start as child’s play." Science News for Students. June 18, 2014.

D. Fox. “Surprise! Fossils in a flash.” Science News for Students. May 16, 2014.

S. Perkins. “Reviving dinosaurs.” Science News for Students. March 4, 2014.

S. Perkins. “Tar pit bones yield climate clues.” Science News for Students. July 23, 2013.

S. Perkins. “Dino-sized poop.” Science News for Students. Jan. 31, 2013.

E. Sohn. “Fossil forests.” Science News for Students. Jan. 2, 2007.

E. Sohn. “Fingerprinting fossils.” Science News for Students. June 21, 2004.