So far, Earth is the only planet known to support life. The mere presence of life forms on Earth sets it aside from the other known planets in the universe.
Scientists started to formulate a series of theories regarding the emergence of life forms on the planet and relate it to the physical changes on Earth's environment.
The Cenozoic era is also known as the 'age of mammals', the Mesozoic era is also known as the 'age of reptiles', and the Paleozoic era is also known as the 'age of invertebrates'.
Epochs are the shortest subdivision unit in the Earth's geologic time scale that is characterized by the changes in life forms and may vary from continent to continent.
One of the earliest known evidence of life on Earth includes the stromatolite fossils collected from various samples of metasedimentary rocks in western Greenland and were aged 3.7 billion years old.
In 2015, fossils of the microbial mat (primitive microbial colony) that may represent potential biotic life dated 4.1 billion-year-old were collected in Western Australia.