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  2. Abyssal zone - Wikipedia

    en.wikipedia.org/wiki/Abyssal_zone

    The biomass of the abyssal zone actually increases near the seafloor as most of the decomposing material and decomposers rest on the seabed. [9] The composition of the abyssal plain depends on the depth of the sea floor. Above 4000 meters the seafloor usually consists of calcareous shells of foraminifera, zooplankton, and phytoplankton.

  3. Decomposer - Wikipedia

    en.wikipedia.org/wiki/Decomposer

    The primary decomposer of litter in many ecosystems is fungi. [11] [12] Unlike bacteria, which are unicellular organisms and are decomposers as well, most saprotrophic fungi grow as a branching network of hyphae. Bacteria are restricted to growing and feeding on the exposed surfaces of organic matter, but fungi can use their hyphae to penetrate ...

  4. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water is the medium of the oceans, the medium which carries all the substances and elements involved in the marine biogeochemical cycles. Water as found in nature almost always includes dissolved substances, so water has been described as the "universal solvent" for its ability to dissolve so many substances.

  5. Deep sea - Wikipedia

    en.wikipedia.org/wiki/Deep_sea

    The deep sea is broadly defined as the ocean depth where light begins to fade, at an approximate depth of 200 m (660 ft) or the point of transition from continental shelves to continental slopes. [1] [2] Conditions within the deep sea are a combination of low temperatures, darkness, and high pressure. [3]

  6. Mesopelagic zone - Wikipedia

    en.wikipedia.org/wiki/Mesopelagic_zone

    It is uncommon to detect deep scattering layers below 1000m. Until recently, sonar has been the predominant method for studying the mesopelagic. [46] The Malaspina Circumnavigation Expedition was a Spanish-led scientific quest in 2011 to gain a better understanding of the state of the ocean and the diversity in the deep oceans. [49]

  7. Marine life - Wikipedia

    en.wikipedia.org/wiki/Marine_life

    The sea pig, a deep water sea cucumber, is the only echinoderm that uses legged locomotion. A benthopelagic and bioluminescent swimming sea cucumber , 3200 metres deep It is held by some scientists that the radiation of echinoderms was responsible for the Mesozoic Marine Revolution .

  8. Abyssal channel - Wikipedia

    en.wikipedia.org/wiki/Abyssal_channel

    Abyssal channels (also, deep-sea channels, underwater channels) are channels in Earth's sea floor. They are formed by fast-flowing floods of turbid water caused by avalanches near the channel's head, with the sediment carried by the water causing a build-up of the surrounding abyssal plains. Submarine channels and the turbidite systems which ...

  9. Deep-sea community - Wikipedia

    en.wikipedia.org/wiki/Deep-sea_community

    For the deep-sea ecosystem, the death of a whale is the most important event. A dead whale can bring hundreds of tons of organic matter to the bottom. Whale fall community progresses through three stages: [32] Mobile scavenger stage: Big and mobile deep-sea animals arrive at the site almost immediately after whales fall on the bottom.