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The pelagic food web, showing the central involvement of marine microorganisms in how the ocean imports carbon and then exports it back to the atmosph
The pelagic food web, showing the central involvement of marine microorganisms in how the ocean imports carbon and then exports it back to the atmosphere and ocean floor
Pump processes vary with depthPhotic zone: 0–100 m; Mesopelagic: 100–1000 m; Bathypelagic: 1000 to abyssal depths. Below 1000 m depth carbon is consid
Pump processes vary with depthPhotic zone: 0–100 m; Mesopelagic: 100–1000 m; Bathypelagic: 1000 to abyssal depths. Below 1000 m depth carbon is considered removed from the atmosphere for at least 100 years. Scavenging: DOC incorporation within sinking particles.
Particulate inorganic carbon budget for Hudson Bay Black arrows represent DIC produced by PIC dissolution. Grey lines represent terrestrial PIC. Units
Particulate inorganic carbon budget for Hudson Bay Black arrows represent DIC produced by PIC dissolution. Grey lines represent terrestrial PIC. Units are Tg C y−1
The coccolithophore Emiliania huxleyi (µm = thousandth of one mm)
The coccolithophore Emiliania huxleyi (µm = thousandth of one mm)
Oceanic carbon cycle (IPCC)
Oceanic carbon cycle (IPCC)
Dissociation of carbon dioxide following Henry's Law
Dissociation of carbon dioxide following Henry's Law
Global air-sea CO2 flux – IPCC 2007
Global air-sea CO2 flux – IPCC 2007
Carbon cycle processes in high-latitude shelf seas
Carbon cycle processes in high-latitude shelf seas