Question
Compare the early Earth atmosphere to modern Earth atmosphere. (1 point)
Responses
There is now less carbon dioxide, less oxygen, and decreasing temperatures.
There is now less carbon dioxide, less oxygen, and decreasing temperatures.
The is now less oxygen, increasing carbon dioxide, and increasing temperatures.
The is now less oxygen, increasing carbon dioxide, and increasing temperatures.
There is more oxygen, decreasing carbon dioxide, and decreasing temperatures.
There is more oxygen, decreasing carbon dioxide, and decreasing temperatures.
There is now more oxygen, increasing temperatures, and increasing carbon dioxide.
There is now more oxygen, increasing temperatures, and increasing carbon dioxide.
Responses
There is now less carbon dioxide, less oxygen, and decreasing temperatures.
There is now less carbon dioxide, less oxygen, and decreasing temperatures.
The is now less oxygen, increasing carbon dioxide, and increasing temperatures.
The is now less oxygen, increasing carbon dioxide, and increasing temperatures.
There is more oxygen, decreasing carbon dioxide, and decreasing temperatures.
There is more oxygen, decreasing carbon dioxide, and decreasing temperatures.
There is now more oxygen, increasing temperatures, and increasing carbon dioxide.
There is now more oxygen, increasing temperatures, and increasing carbon dioxide.
Answers
GPT-4o mini
The correct comparison between the early Earth atmosphere and the modern Earth atmosphere is:
**There is more oxygen, decreasing carbon dioxide, and decreasing temperatures.**
In the early Earth atmosphere, there was significantly more carbon dioxide and much less oxygen. Over time, photosynthetic organisms contributed to the increase in atmospheric oxygen. The overall carbon dioxide levels have decreased, particularly due to the formation of carbonates and the sequestration of carbon in biomass. Modern temperatures have generally been stable, but geological and climatic changes have influenced temperature trends over time.
**There is more oxygen, decreasing carbon dioxide, and decreasing temperatures.**
In the early Earth atmosphere, there was significantly more carbon dioxide and much less oxygen. Over time, photosynthetic organisms contributed to the increase in atmospheric oxygen. The overall carbon dioxide levels have decreased, particularly due to the formation of carbonates and the sequestration of carbon in biomass. Modern temperatures have generally been stable, but geological and climatic changes have influenced temperature trends over time.