Linked from

The 41 pages that link to Biological carbon pump, each with the reason it gives.

• Filter feedingRelated: Filter feeders can redirect captured carbon into sinking waste, tissues, or carcasses.

• Marine snowNarrower topic: Marine snow is a major vehicle in this ocean-scale carbon transfer.

• PlanktonRelated: Plankton incorporate carbon into particles that can sink below the sunlit surface.

• ZooplanktonRelated: Zooplankton package and transport carbon through fecal pellets, feeding, and daily migration.

• Antarctic Circumpolar CurrentRelated: Nutrient circulation around Antarctica supports productivity that helps export carbon to depth.

• Pelagic zoneRelated: Pelagic organisms drive carbon downward when particles and migrating animals carry it to depth.

• Diel vertical migrationRelated: Migrants carry surface-derived carbon downward through respiration, excretion, and mortality.

• PhytoplanktonRelated: Sinking phytoplankton and their remains carry captured carbon below the surface.

• Antarctic krillRelated: Krill fecal pellets and sinking carcasses transport carbon downward from surface feeding grounds.

• Primary productionRelated: Marine primary production feeds the export of organic carbon to deeper waters.

• Mesopelagic zoneRelated: Mesopelagic feeding and migration redistribute carbon below the sunlit ocean.

• KrillRelated: Krill feed, respire, and produce sinking waste that can carry carbon downward.

• DiatomRelated: Sinking diatom cells and aggregates carry photosynthetically fixed carbon downward.

• Deep scattering layerRelated: Vertical migrations by layer inhabitants help move carbon into deeper water.

• Deep-sea ecologyNarrower topic: It links surface production to deep-sea food supply and carbon storage.

• Marine biologyRelated: Marine organisms influence how much atmospheric carbon the ocean stores.

• StratificationRelated: Layering influences the nutrient supply and carbon exchange that sustain this process.

• Bathypelagic zoneRelated: How much carbon persists or is returned at these depths remains difficult to quantify.

• CoccolithophoreRelated: Coccoliths can ballast sinking particles and help export carbon from surface waters.

• Carbonate compensation depthNarrower topic: It carries shell material downward toward sediments where compensation occurs.

• LanternfishRelated: Their migrations and waste transport carbon downward from feeding grounds near the surface.

• AlgaeRelated: Algal production supplies much of the organic material that carries carbon into deep water.

• CopepodRelated: Copepods influence carbon export through fecal pellets, respiration, and daily vertical migration.

• Deep-sea biodiversityRelated: Deep-sea organisms help store carbon by consuming, transforming, and burying sinking material.

• Oyashio CurrentRelated: High productivity in Oyashio-influenced waters can increase the export of organic carbon downward.

• Mesopelagic fishRelated: The size of the fishes’ contribution through feeding and migration remains uncertain.

• AutotrophRelated: Marine autotrophs help draw atmospheric carbon into ocean food webs and deeper waters.

• Marine microbiologyRelated: Microbial activity shapes particle production, sinking, and carbon remineralization.

• NeustonRelated: Neustonic production and consumption can contribute to carbon transfer through marine food webs.

• RhizariaRelated: Rhizarians can contribute carbon-bearing particles and influence how material sinks through the ocean.

• HaptophyteRelated: Haptophyte production and sinking particles help move carbon into ocean depths.

• SalpRelated: Salp feeding and sinking waste can carry plankton-derived carbon downward.

• Biological carbon fixationRelated: Marine organisms fix dissolved carbon and some of it sinks, storing carbon away from the atmosphere.

• MyctophiformesRelated: Daily fish migrations can transport carbon downward through feeding and waste.

• Pelagic sedimentRelated: Pelagic deposits receive part of the carbon exported downward by marine life.

• StomiiformesRelated: Vertical migrations by midwater fishes can move carbon below the surface.

• Clione limacinaRelated: Clione belongs to planktonic food webs that help move carbon through the ocean.

• Deep-sea communityRelated: Sinking organic matter feeds deep communities while moving carbon away from the atmosphere.

• Marine chemistryRelated: It redistributes carbon and nutrients between surface waters and the deep ocean.

• Marine hatchetfishRelated: Migrating hatchetfishes can carry carbon downward through respiration and waste.

• Ocean surface ecosystemRelated: Surface production and particle sinking help determine how much carbon leaves the atmosphere-facing ocean.