Wiki User
∙ 10y agoaddition of free oxygen
Wiki User
∙ 10y agoThe oxygenation of Earth's atmosphere was dependent on the development of photosynthetic life forms, like cyanobacteria. These organisms were able to convert sunlight into energy and release oxygen as a byproduct, which ultimately led to the increase in oxygen levels on Earth.
Fossils aren't but the life that made them is.
Changes in climate
how different parts of earths history compare to the whole world
fossil record geologic time scale
So you can understaned it much more better and think about it!
What are two ways that's scientists can study earths climates history
epoch
In sedimentary rock.
Historical geology.
Gravitational potential energy.
precambrian era
to die
because
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2/27/96 IS THE MOST IMPORTENT