Linked from

The 57 pages that link to Marine snow, each with the reason it gives.

• Benthic zoneRelated: It delivers food and carbon from surface waters to the deep benthos.

• PlanktonRelated: Planktonic remains and waste contribute to this food source for deep-ocean life.

• Pelagic zoneRelated: It transports energy and nutrients from productive surface waters into deep pelagic habitats.

• Diel vertical migrationRelated: Researchers distinguish migrant-driven carbon export from carbon sinking in particles.

• Mesopelagic zoneRelated: It carries surface-produced food into the mesopelagic zone.

• Deep-sea explorationRelated: Its variable supply shapes deep-sea food webs but is difficult to measure over time.

• AnglerfishRelated: This uneven food supply helps explain why waiting and luring can be advantageous at depth.

• Abyssal plainRelated: It supplies food to plain-dwelling organisms where sunlight-driven production is absent.

• Microbial ecologyRelated: Microbial activity on these particles influences carbon transport into the deep sea.

• Deep scattering layerRelated: Animals migrating through the layer transport carbon downward through feeding and waste production.

• CounterilluminationRelated: The dark, particle-filled background helps explain why silhouette concealment benefits deep-sea animals.

• Deep-sea ecologyRelated: It carries much of the surface ocean’s fixed carbon into deep-sea food webs.

• Biological carbon pumpRelated: Aggregates carry a portion of fixed carbon downward through the water column.

• Deep-sea fishRelated: This drifting material supplies food to many deep-sea ecosystems.

• Oxygen minimum zoneRelated: Its decomposition consumes oxygen as organic material sinks through the zone.

• Deep seaRelated: This drifting material supplies much of the deep sea’s food.

• Marine biologyRelated: Its production and sinking rates remain uncertain but shape deep-sea food supply.

• Bathypelagic zoneRelated: It delivers much of the food available to bathypelagic communities.

• Abyssal zoneRelated: It supplies much of the food reaching abyssal ecosystems.

• Carbonate compensation depthRelated: It transports carbonate particles from surface waters toward the seafloor.

• Hadal zoneRelated: This sinking material supplies food where sunlight cannot support local photosynthesis.

• LanternfishRelated: Lanternfish feed within the deep-ocean ecosystem sustained partly by sinking organic matter.

• Benthic ecologyRelated: Its delivery to the seabed often determines how much food reaches deep benthic communities.

• CopepodRelated: Copepod feeding and waste production contribute particles that become part of marine snow.

• Deep-sea biodiversityRelated: This falling material supplies much of the energy supporting communities far below productive surface waters.

• LeptocephalusRelated: Leptocephali feed largely on dissolved and particulate organic material associated with marine snow.

• Marine habitatRelated: Its supply helps determine how much life deep-sea habitats can support.

• Mesopelagic fishRelated: It supplies some food-web energy to mesopelagic communities.

• Bathyal zoneRelated: It supplies much of the food reaching bathyal communities.

• Deep-sea benthosRelated: It supplies much of the carbon consumed by deep-sea communities.

• Oceanic zoneRelated: It transports food and carbon from the oceanic surface toward its depths.

• RadiolariaRelated: Dead radiolarians and their skeletons can descend through the water within these aggregates.

• TunicateRelated: Tunicate filtering and waste contribute to the ocean's particle flux and food webs.

• Marine benthic zoneRelated: It transports surface-derived food to benthic organisms far below the sunlit ocean.

• Vampire squidRelated: The vampire squid gathers sinking particles as its main food source.

• FrogfishRelated: Deep-sea frogfish habitats are part of the food webs supported by this falling material.

• HalobatesRelated: Floating debris and small organisms associated with surface flotsam provide food for oceanic Halobates.

• Aphotic zoneRelated: It carries energy from sunlit waters into ecosystems without local photosynthesis.

• Black seadevilRelated: It supports deep-sea food webs in which black seadevils are predators.

• GonostomatidaeRelated: Bristlemouths consume organisms linked to sinking particles and help move carbon through the ocean.

• SalpRelated: Salp fecal pellets can become rapidly sinking particles within marine snow.

• Basket starRelated: Basket stars can intercept drifting organic material as well as living plankton.

• ChaetognathaRelated: Arrow worms feed within pelagic ecosystems shaped by this downward carbon flux.

• MyctophiformesRelated: Lanternfish feeding and waste contribute to the movement of organic matter through the water column.

• Pelagic sedimentRelated: These particles carry organic material from surface waters to deep-sea deposits.

• Praya dubiaRelated: It contributes to the deep-water food supply in the habitat where Praya dubia lives.

• Sea surface microlayerRelated: Some surface-derived organic particles join aggregates that sink out of the microlayer.

• Clione limacinaRelated: Clione and its prey participate in food webs that transfer carbon into deeper waters.

• Deep-sea communityRelated: This sinking material supplies much of the energy available to deep-sea organisms.

• FanfinRelated: Marine snow helps sustain the deep-sea food web in which fanfins prey.