• There are many ways in which carbon can be stored for long periods of time on our planet. These are referred to as carbon sinks (ex: oceans, forests, trees…)
• Plants absorb CO2 from the atmosphere during photosynthesis, also called primary production, and release CO2 back in to the atmosphere during respiration
• Another major exchange of CO2 occurs between the oceans and the atmosphere. The dissolved CO2 in the oceans is used by marine biota in photosynthesis
• However, since the industrial revolution human activity has influenced the carbon cycle by changing land use and has released huge amounts of CO2 into the atmosphere
• Fossil fuel burning is increasing the atmosphere's store of carbon by 6.1 Giga tones each year
• Humans have created an imbalance in the carbon cycle significantly influencing the earths climate system
Source of Information : Climate Change: A Silent Threat by Sylvain Richer de Forges
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