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Inorganic carbon
Rocks (bicarbonate and carbonate)
Organic carbon
Plant materials
Carbon gases
CO2, CH4 and CO
Carbon reservoirs
Ocean, vegetation, permafrost, atmosphere
BLAG hypothesis
Past global temperature controlled by spreading rates
Slow seafloor spreading
Slow CO2 input, cold climate, decreased chemical weathering
Fast seafloor spreading
Rapid CO2 input, warm climate, increased weathering, increased CO2 removal
Biological ocean pump
Phytoplankton and cyanobacteria take in CO2
Iron fertilisation
Increase Fe in oceans to remove limiting factor for phytoplankton growth
Aerosols
Small liquid or solid particles suspended in the atmosphere