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.
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.
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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