Evidence of early forms of life comes from fossils
Fossils are the “remains” of organisms from hundreds of thousands of years ago that are found in rocks
Formation
From parts of organisms that have not decayed because one or more of the conditions required for decay are absent
When parts of the organism are replaced by other materials as they decay
As preserved traces of organisms, such as footprints, burrows and rootlet traces
Many early forms of life were soft-bodied, which means that they have left few traces behind, which were mostly destroyed by geological activity; this is why scientists cannot be certain about how life began on Earth
Fossils show how much or how little different organisms have changed as life developed on Earth
Causes of extinction
Changes to the environment over geological time
New predators
New diseases
New, more-successful competitors
A single catastrophic event, such as massive volcanic eruptions or collisions with asteroids
New species
Isolation: two populations of a species become separated, such as by geographical isolation
Genetic variation: each population has a wide range of alleles that control their characteristics
Natural selection: in each population, the alleles that control the characteristics that help to organism to survive are selected
Speciation: the populations become so different that successful interbreeding is no longer possible