The deep ocean, often called the abyss, covers 66% of the planet. Schematically, it is the marine zone where there is not enough light to allow plants to grow. In fact, the lightened part of the ocean is shallow and does not exceed a few hundred meters; the rest of the ocean can reach much greater depths (11 km in the Mariana Trench) and is in complete darkness except for slight glows of bioluminescence. In the absence of local organic production, the organisms living at depth subsist due to organic matter produced in surface waters. This organic matter, in the form of decomposed matter, feces and molts, is clumped together by secretions from gelatinous organisms, sediments at depth and is degraded under the action of heterotrophic microbial communities, or is being recycled by pelagic organisms. Stratification of the water column, depth, surface production and seasonal variations as well as distance from continental shelves directly affect the flow of organic matter that reaches deep sediments. Generally speaking, the further we move away from the coast, the greater the depth, the lower the organic input and consequently, the lower the benthic biomass. Production in the abyssis approximately a hundredth of the primary production at the surface and benthic biomass expressed in fresh weight rarely exceeds 2 g/m 2. Only some populations of filter-feeding Chapter written by Jozée SARRAZIN and Daniel DESBRUYÈRES.