Abstract
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Oxygen accumulated in Earth's atmosphere through the process of photosynthesis carried out by early cyanobacteria. These organisms released oxygen as a byproduct, gradually building up oxygen levels in the atmosphere over millions of years.
Oxygen began to accumulate in Earth's atmosphere around 2.4 billion years ago during the Great Oxidation Event. This was a gradual process that took hundreds of millions of years as photosynthetic bacteria started producing oxygen through photosynthesis.
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 did not accumulate in the atmosphere until approximately 1.5 billion years after life appeared on Earth because early organisms did not produce oxygen as a byproduct of photosynthesis. It took a few billion years for oxygen-producing cyanobacteria to evolve and become abundant, resulting in the significant accumulation of oxygen in the atmosphere known as the Great Oxidation Event.
Oxygen was least likely to have been a component of Earth's atmosphere before life began. It was initially scarce, and the atmosphere was primarily made up of gases such as methane, ammonia, water vapor, and carbon dioxide. Oxygen started to accumulate in the atmosphere following the emergence of photosynthetic organisms.
Billions of years ago, Earth's early atmosphere likely contained little to no oxygen. Oxygen began to accumulate in the atmosphere around 2.5 billion years ago due to the process of photosynthesis by early cyanobacteria and other organisms, which produced oxygen as a byproduct. This led to the gradual build-up of oxygen levels in the atmosphere over millions of years.