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carbon sequestration due to three processes
solubility/physical pump
Biological pump
Carbonate pump
DIC
dissolved inorganic carbon, sequestered with physical/solubility pump
POC
Particulate Organic Carbon, less prevalent than DOC and DIC
DOC
dissolved organic carbon
physical/solubility pump
CO2 (DIC) from atmosphere sequestered into ocean with diffusion and downwelling
% from physical/solubility pump
10%
% from biological pump
70%
% from Carbonate pump
20%
biological pump
process driven by pelagic food web, inorganic carbon is fixed by photosynthetic species that then die and fall to the sea floor (photosynthesis)
Carbonate pump
calcium carbonate formed into shells by organisms such as plankton and mollusks (calcification), fixes PIC but releases some CO2 therefore counter pump
Phytoplankton's role
efficiently fixes carbon with quick turnover and very low biomass. Generate large amounts of DOC to sustain food chain
components of biological carbon pump
organic carbon pump
carbonate pump
components of the organic carbon pump
gravitational pump (BGP)
particle injection pumps
Biological gravitational pump (BGP)
dominates open ocean uses algal aggregates, fecal pellets, carcasses
Eddy subduction pump (ESP)
10% of organic carbon pump - uses currents to pump carbon deep
Mixed layer pump (MLP)
15% of organic carbon pump - seasonal transitions
Mesopelagic Migration Pump (MMP)
20% of organic carbon pump - mesopelagic taxa vertical movement up and down water column
Seasonal lipid pump (SLP)
5% of organic carbon pump - high latitude productivity varies with phytoplankton stores varying (ex high latitude Krill)
Particle injection pumps (PIP)
eddy-subduction pump (ESP)
mixed layer pump (MLP)
mesopelagic migration pump (MMP)
seasonal lipid pump (SLP)
remineralization
The process by which organic matter is broken down by microbial activity, releasing nutrients back into the water column, contributing to the recycling of carbon in marine ecosystems.