Magnified views of loose particles and a clump.
Mucus binds plankton debris and other particles together. © 2026 dive.explo360.fr — Contenus protégés par le droit d’auteur. Tous droits réservés.

How particles stick together

In sunlit water, microscopic algae in the phytoplankton grow using light and dissolved nutrients. Zooplankton feed on them, and in turn are eaten by other animals. Dead cells, droppings and scraps remain in the water.

Flakes change as they sink

Moving water can carry the clumps sideways or break them apart. Some collect more particles and sink faster. Small animals eat or tear up flakes, and bacteria break them down. As some of the material dissolves, less remains to sink.

A breaking flake with a small crustacean and a magnified view of bacteria.
An aggregate breaks apart, and small animals and bacteria make use of its material. © 2026 dive.explo360.fr — Contenus protégés par le droit d’auteur. Tous droits réservés.
An animal on the muddy seabed beneath a sparse fall of particles.
Particles from surface waters reach the dark seabed. © 2026 dive.explo360.fr — Contenus protégés par le droit d’auteur. Tous droits réservés.

The surface feeds the seabed

Far below the surface, there is too little light for photosynthesis. Marine snow brings food made near the surface. Some animals catch flakes in the water. Others eat what settles on the seabed, sometimes after microbes have broken it down. In some temperate seas, more food sinks after plankton blooms in spring.

The biological carbon pump

Phytoplankton use carbon dioxide dissolved in water to grow. When bits of plankton sink, they take some of that carbon along. This is part of the biological carbon pump. Feeding and decay release some carbon back into the water as carbon dioxide. How long it stays away from the air depends on where it’s released and where the water goes. Only a small share stays buried in the seabed.

A cross-section of the sea with downward arrows and a deep current.
Particles carry carbon into the deep. Currents move deep water and a little of the organic matter reaches the sediment. © 2026 dive.explo360.fr — Contenus protégés par le droit d’auteur. Tous droits réservés.
Particles drifting past animals attached to a Mediterranean rock wall.
Currents bring particles within reach of sponges and sea squirts. © 2026 dive.explo360.fr — Contenus protégés par le droit d’auteur. Tous droits réservés.

Spotting marine snow in the Mediterranean

Marine snow may be easier to see when there is more plankton or when mucus-rich clumps form. Sediment stirred up from the seabed can look much the same through a diving mask. Large masses of jelly-like mucilage form through different processes. Currents carry particles past rock walls, through open water and over seagrass beds. Sponges and sea squirts filter particles of sizes they can capture.

Interactive quiz

Marine snow quiz

5 question(s) to test your knowledge.

What happens to the flakes

A flake in your torch beam might contain bits of algae, droppings or mucus. It may have fed several organisms before reaching you. If part of it reaches the seabed, it links places that can be thousands of metres apart.

Scientific references

These sources document the main processes described in the article.