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Marine particulate organic carbon (POC) POC includes components of living cells as well as dead material (detritus), and originates from both allochth
Marine particulate organic carbon (POC) POC includes components of living cells as well as dead material (detritus), and originates from both allochthonous and autochthonous sources. The POC pool can also exchange material with the dissolved OC (DOC) pool through aggregation and disaggregation of particles. This process and others may be involved in the formation of the molecularly uncharacterized component (MUC), which may incorporate both autochthonous and allochthonous OC.
Mean annual POC export at 100 m across the Southern Ocean
Mean annual POC export at 100 m across the Southern Ocean
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Zooplankton sample including several species of copepods (1–5), gastropod larva (6) doliolids (7), fish eggs (8), and decapod larva (9) (Photo by Iole
Zooplankton sample including several species of copepods (1–5), gastropod larva (6) doliolids (7), fish eggs (8), and decapod larva (9) (Photo by Iole Di Capua)
Upper left: Biogeochemical models Right: Ecosystem models Lower left: Size-spectra models These models also have temporal and spatial components.
Upper left: Biogeochemical models Right: Ecosystem models Lower left: Size-spectra models These models also have temporal and spatial components.
Like diatoms, radiolarians come in many shapes
Like diatoms, radiolarians come in many shapes
Also like diatoms, radiolarian shells are usually made of silicate
Also like diatoms, radiolarian shells are usually made of silicate