The rise of oxygen in the earth's atmosphere questions answer key 2025

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A smaller-scale glaciation, the Gaskiers, occurred later (about 580 million years ago). During these periods, temperatures plummeted and rose again, causing glacial melting and an influx of nutrients into the ocean, which researchers think caused oxygen levels to rise deep in the oceans.
O2 first accumulated in Earth's atmosphere at this time and has been present ever since. It's been thought that this happened sometime between 2.5 and 2.3 billion years ago.
This was a planet where bacteria reigned, and one kind of bacteria in particular \u2013 cyanobacteria \u2013 was slowly changing the world around it through photosynthesis. The atmosphere of the early Earth lacked oxygen. This began to change during what's known as the Great Oxidation Event, or GOE.
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Approximately 2.4 billion years ago the oxygen concentration in Earth's atmosphere increased suddenly from trace amounts to appreciable quantities, probably because of a combination of biological and geochemical processes.
Much of the CO2 dissolved into the oceans. Eventually, a simple form of bacteria developed that could live on energy from the Sun and carbon dioxide in the water, producing oxygen as a waste product. Thus, oxygen began to build up in the atmosphere, while the carbon dioxide levels continued to drop.
The rise in oxygen is attributed to photosynthesis by cyanobacteria, which are thought to have evolved as early as 3.5 billion years ago.
The rise in oxygen is attributed to photosynthesis by cyanobacteria, which are thought to have evolved as early as 3.5 billion years ago.
The history of Earth's oxygen For the first 2 billion years, most scientists believe very little oxygen was present in the atmosphere or ocean. But about 2.5-2.3 billion years ago, atmospheric oxygen levels first increased.

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