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  2. 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.

  3. Mycoplankton - Wikipedia

    en.wikipedia.org/wiki/Mycoplankton

    Another process which mycoplankton take part in is known as the benthic shunt. This process takes place in the benthic zone, the sediments at the bottom of the water. The benthic shunt is typically referred to in relation to freshwater aquatic environments, but the concept is relevant and takes place in marine habitats as well.

  4. Upwelling - Wikipedia

    en.wikipedia.org/wiki/Upwelling

    Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water from deep water towards the ocean surface. It replaces the warmer and usually nutrient-depleted surface water.

  5. Gelatinous zooplankton - Wikipedia

    en.wikipedia.org/wiki/Gelatinous_zooplankton

    The global biomass of gelatinous zooplankton (sometimes referred to as jelly‐C) within the upper 200 m of the ocean amounts to 0.038 Pg C. [21] Calculations for mesozooplankton (200 μm to 2 cm) suggest about 0.20 Pg C. [22] The short life span of most gelatinous zooplankton, from weeks up to 2 to 12 months, [23] [24] suggests biomass ...

  6. Eddy pumping - Wikipedia

    en.wikipedia.org/wiki/Eddy_pumping

    On the contrary, this process creates downwelling when the cyclone decays and the pycnocline returns to its original state. Through such mechanism eddy pumping generates upwelling of cold, nutrient rich deep waters in cyclonic eddies and downwelling of warm, nutrient poor, surface water in anticyclonic eddies.

  7. Diel vertical migration - Wikipedia

    en.wikipedia.org/wiki/Diel_vertical_migration

    This is a major process in the ocean and without vertical migration it wouldn't be nearly as efficient. The deep ocean gets most of its nutrients from the higher water column when they sink down in the form of marine snow. This is made up of dead or dying animals and microbes, fecal matter, sand and other inorganic material.

  8. Gelatin - Wikipedia

    en.wikipedia.org/wiki/Gelatin

    Substances containing gelatin or functioning in a similar way are called gelatinous substances. Gelatin is an irreversibly hydrolyzed form of collagen, wherein the hydrolysis reduces protein fibrils into smaller peptides ; depending on the physical and chemical methods of denaturation, the molecular weight of the peptides falls within a broad ...

  9. Diatom - Wikipedia

    en.wikipedia.org/wiki/Diatom

    The surface mud of a pond, ditch, or lagoon will almost always yield some diatoms. Living diatoms are often found clinging in great numbers to filamentous algae, or forming gelatinous masses on various submerged plants. Cladophora is frequently covered with Cocconeis, an elliptically shaped diatom; Vaucheria is often covered with small forms.