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Multiple Choice
How do scientists explain the increase in oxygen in Earth's early atmosphere?
A
The direct release of oxygen from the breakdown of atmospheric nitrogen.
B
The evolution of photosynthetic organisms that released oxygen as a byproduct.
C
The accumulation of oxygen from volcanic eruptions.
D
The arrival of oxygen-rich meteorites from space.
Verified step by step guidance
1
Understand the context of Earth's early atmosphere: Initially, Earth's atmosphere was composed primarily of gases like carbon dioxide, methane, and nitrogen, with very little oxygen present.
Recognize the role of photosynthetic organisms: Scientists attribute the increase in oxygen to the evolution of early photosynthetic organisms, such as cyanobacteria, which used sunlight to convert carbon dioxide and water into glucose and oxygen through the process of photosynthesis.
Learn the chemical basis of photosynthesis: The general equation for photosynthesis is: . This process releases oxygen as a byproduct.
Understand the timeline of oxygen accumulation: Over millions of years, the oxygen released by photosynthetic organisms began to accumulate in the atmosphere, leading to the 'Great Oxygenation Event' approximately 2.5 billion years ago.
Eliminate incorrect explanations: The increase in oxygen was not due to the breakdown of atmospheric nitrogen, volcanic eruptions, or oxygen-rich meteorites. These processes do not produce significant amounts of oxygen in the atmosphere.