The Amazing Carbon Cycle
What It Is
How It Works
The cycle is divided into the fast (biological) cycle, involving photosynthesis and respiration, and the slow (geological) cycle, involving the movement of carbon through the lithosphere, mantle, and crust over millions of years.
Why It Matters
Human activity, specifically the combustion of fossil fuels and land-use changes, has increased atmospheric CO2 by nearly 52% since pre-industrial times, leading to global warming and ocean acidification.
Discovery & History
Early research by Antoine Lavoisier and Joseph Priestley laid the foundation for understanding carbon exchange, leading to the modern classification of carbon pools including the atmosphere, terrestrial biosphere, and deep ocean.
Real-World Examples
The Keeling curve demonstrates the seasonal and diurnal fluctuations of CO2 uptake in the northern hemisphere, highlighting the terrestrial biosphere's role in carbon sequestration.
Go deeper
Frequently Asked Questions
What is the carbon cycle?+
Why is the carbon cycle important?+
How does carbon move in the carbon cycle?+
Which parts of Earth are involved in the carbon cycle?+
How does the carbon cycle affect Earth's habitability?+
Based on content from Wikipedia ยท Licensed under CC BY-SA 4.0
