Plants started to grow on the earth, plants breath in carbon dioxide (which is why it decreased so much) and they breath out oxygen. That is why the percentage of oxygen has increased so much.
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The increase in oxygen in Earth's atmosphere was primarily due to the process of photosynthesis by early plant life, which started around 2.5 billion years ago. This process involved plants using sunlight to convert carbon dioxide into oxygen as a byproduct, gradually increasing the proportion of oxygen in the atmosphere to its current levels.
The amount of oxygen in Earth's atmosphere increased gradually over millions of years due to the process of photosynthesis by early bacteria and later by plants. These organisms released oxygen as a byproduct, which accumulated in the atmosphere and changed its composition over time. This process, known as the Great Oxidation Event, occurred around 2.4 billion years ago and significantly increased the amount of oxygen in the atmosphere.
The increase in oxygen in Earth's atmosphere was attributed to the process of photosynthesis carried out by early cyanobacteria and plants. These organisms converted carbon dioxide into oxygen through photosynthesis, gradually increasing the oxygen levels in the atmosphere over millions of years.
Iron was the oxidized metal that caused substantial quantities of oxygen to accumulate in Earth's atmosphere, a process known as the Great Oxidation Event. This event occurred around 2.4 billion years ago as photosynthetic organisms began producing oxygen through photosynthesis, which reacted with iron in the oceans and rocks, leading to the buildup of oxygen in the atmosphere.
Oxygen was absent from Earth's early atmosphere because the planet's early life forms did not yet produce oxygen through photosynthesis. It wasn't until photosynthetic organisms like cyanobacteria evolved and began releasing oxygen as a byproduct that levels of oxygen in the atmosphere started to increase. This process took millions of years to significantly change the composition of Earth's atmosphere.
One major change in the composition of Earth's atmosphere was the Great Oxidation Event about 2.4 billion years ago. This event led to a significant increase in oxygen levels due to the emergence of photosynthetic organisms that released oxygen as a byproduct. This change had a profound impact on the evolution of life on Earth.