They can be preserved, e.g. in rocks, by the process of petrification, during which the tissues of organisms are replaced with minerals
The fossil record is small in relation to the number of organisms that have ever lived, due to the conditions for fossilisation being so rare
We can tell from fossils that organisms have changed significantly over millions of years
Fossils, as well as the rocks they are found in, can be dated, allowing us to accurately put fossil organisms into a sequence from oldest to youngest, and therefore see how organisms have changed through evolutionary time
The fossil record shows the kind of progression that the theory of evolution would lead us to expect, with older fossils showing simpler life forms and complexity increasing with time
The sequence of fossils aligns with ecology groups: plant fossils appear earlier in the fossil record than animals, and plants with the ability to be pollinated by insects appear before insect pollinators
Fossils can show evidence for transitional species, showing how one species could evolve into another e.g. Ambulocetus is a fossil that links amphibians with early whale-like organisms, and Archaeopteryx appears to link reptiles with birds