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  2. Benthic-pelagic coupling - Wikipedia

    en.wikipedia.org/wiki/Benthic-pelagic_coupling

    Benthic-pelagic coupling are processes that connect the benthic zone and the pelagic zone through the exchange of energy, mass, or nutrients. These processes play a prominent role in both freshwater and marine ecosystems and are influenced by a number of chemical, biological, and physical forces that are crucial to functions from nutrient cycling to energy transfer in food webs.

  3. Benthic boundary layer - Wikipedia

    en.wikipedia.org/wiki/Benthic_boundary_layer

    The benthic boundary layer (BBL) represents a few tens of meters of the water column directly above the sea floor [3] and constitutes an important zone of biological activity in the ocean. [4] It plays a vital role in the cycling of matter, and has been called the “endpoint” for sedimenting material, which fuels high metabolic rates for ...

  4. Benthos - Wikipedia

    en.wikipedia.org/wiki/Benthos

    These organisms can be used to indicate the presence, concentration, and effect of water pollutants in the aquatic environment. Some water contaminants—such as nutrients, chemicals from surface runoff, and metals [20] —settle in the sediment of river beds, where many benthos reside. Benthos are highly sensitive to contamination, so their ...

  5. Chemical bonding of water - Wikipedia

    en.wikipedia.org/wiki/Chemical_bonding_of_water

    For molecules containing lone pairs, the true hybridization of these molecules depends on the amount of s and p characters of the central atom which is related to its electronegativity. "According to Bent's rule , as the substituent electronegativies increase, orbitals of greater p character will be directed towards those groups.

  6. Macrobenthos - Wikipedia

    en.wikipedia.org/wiki/Macrobenthos

    Macrobenthos consists of the organisms that live at the bottom of a water column [1] and are visible to the naked eye. [2] In some classification schemes, these organisms are larger than 1 mm; [1] in another, the smallest dimension must be at least 0.5 mm. [3] They include polychaete worms, pelecypods, anthozoans, echinoderms, sponges, ascidians, crustaceans.

  7. Biogeochemical cycle - Wikipedia

    en.wikipedia.org/wiki/Biogeochemical_cycle

    Subterranean water can then seep into the ocean along with river discharges, rich with dissolved and particulate organic matter and other nutrients. There are biogeochemical cycles for many other elements, such as for oxygen, hydrogen, phosphorus, calcium, iron, sulfur, mercury and selenium. There are also cycles for molecules, such as water ...

  8. Demersal zone - Wikipedia

    en.wikipedia.org/wiki/Demersal_zone

    The demersal zone is the part of the sea or ocean (or deep lake) consisting of the part of the water column near to (and significantly affected by) the seabed and the benthos. [1] The demersal zone is just above the benthic zone and forms a layer of the larger profundal zone. [citation needed]

  9. Meroplankton - Wikipedia

    en.wikipedia.org/wiki/Meroplankton

    Water and benthos pollution from industrial sources has been demonstrated to have varying effects on biological diversity and survival potential of meroplankton. One study conducted in the Vostok Bay region in Russia , demonstrated that even in the presence of industrial pollutants, most species of meroplankton were able to proliferate almost ...