addition of free oxygen
The Great Oxygenation Event, which occurred around 2.4 billion years ago, was heavily dependent on the development of photosynthetic cyanobacteria. These microorganisms produced oxygen as a byproduct of photosynthesis, significantly increasing atmospheric oxygen levels. This shift not only altered the planet's atmosphere but also paved the way for the evolution of aerobic organisms and complex life forms.
Changes in climate
Fossils aren't but the life that made them is.
how different parts of earths history compare to the whole world
fossil record geologic time scale
The Great Oxygenation Event, which occurred around 2.4 billion years ago, was heavily dependent on the development of photosynthetic cyanobacteria. These microorganisms produced oxygen as a byproduct of photosynthesis, significantly increasing atmospheric oxygen levels. This shift not only altered the planet's atmosphere but also paved the way for the evolution of aerobic organisms and complex life forms.
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
helller
helller
helller