Illustrated · 2 min
How Do Scientists Study Evolution?
One way to learn more about how ancient species evolved is to use fossil evidence. Fossils are most often found in sedimentary rock. Sediments are sand or clay which settle at the bottom of a body of water. Over time, this layer of sediment is covered by new layers. As the layers get heavier, the sediment hardens into sedimentary rock.
Dead organisms can be buried under new layers of sediment and preserved in sedimentary rock. This process can create fossils.

Here are some examples of the types of fossils scientists can find. Insects, shells, bones, and plants can all be found as fossils.
Image source: By Gabi Slizewska
So how does all of this help us learn about evolution?
Fossils are often only parts of organisms, like bones or teeth, but they help us compare structures of extinct species to similar modern ones. This way, we can see how certain structures have changed over time.
Scientists can also use fossils and sedimentary layers in a process called relative dating. Relative dating puts the different sedimentary layers in chronological order. The lower layers are older than the layers closer to the surface. This also allows scientists to place the fossils in those layers in chronological order. Unfortunately, this technique does not give us an exact age of the fossils. Instead, it shows us relative age in comparison to the fossils in other layers.

Relative dating works by comparing the fossils found in different layers of sedimentary rock.
Image source: By Gabi Slizewska
Another really cool technique is called radiometric dating. This technique relies on radioactive isotopes to determine the age of a fossil in years. This is possible because radioactive isotopes present in the body decay, or break down, at a steady rate. A half-life is the amount of time it takes for half of the radioactive isotopes in a sample to convert to nonradioactive isotopes. Knowing the half-life of a specific radioactive isotope lets scientists make precise estimates of a fossil's age.
One form of this technique is called carbon dating. It is used with fossils of living organisms because they contain the radioactive carbon-14. However, carbon-14 has a short half-life on the evolutionary scale, so it is only useful for relatively "young" fossils (up to 60,000 years old).
Other radioactive isotopes such as potassium-40 can be used to date older fossils. However, these isotopes are found in rock, not in fossils. Using these isotopes allows scientists to date layers of sedimentary rock, which also dates the fossils within them.

An example of radiometric dating using radioactive uranium. The uranium decays into lead.
Image source: By Gabi Slizewska
Scientists used these methods to establish a geological time scale. This is a timeline of the Earth's history. It consists of eons, eras, and periods. These methods also let us determine the rate at which evolution takes place.
Below is an example of what the geological time scale looks like.

Image source: By United States Geological Survey [Public domain], via Wikimedia Commons

