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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. 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.

  4. Benthic zone - Wikipedia

    en.wikipedia.org/wiki/Benthic_zone

    As with oceans, the benthic zone is the floor of the lake, composed of accumulated sunken organic matter. The littoral zone is the zone bordering the shore; light penetrates easily and aquatic plants thrive. The pelagic zone represents the broad mass of water, down as far as the depth to which no light penetrates. [9]

  5. Benthic boundary layer - Wikipedia

    en.wikipedia.org/wiki/Benthic_boundary_layer

    The benthic boundary layer (BBL) plays a vital role in the cycling of matter and is commonly referred to as the “endpoint” or "sink" for sediment material, which fuels high metabolic rates for microbial populations. [7] The particles from the pelagic ecosystem sink to the BBL where they will be used by organisms. [2]

  6. Pelagic zone - Wikipedia

    en.wikipedia.org/wiki/Pelagic_zone

    Altogether, the pelagic zone occupies 1,330 million km 3 (320 million mi 3) with a mean depth of 3.68 km (2.29 mi) and maximum depth of 11 km (6.8 mi). [2] [3] [4] Pelagic life decreases as depth increases. The pelagic zone contrasts with the benthic and demersal zones at the bottom of the sea. The benthic zone is the ecological region at the ...

  7. Meroplankton - Wikipedia

    en.wikipedia.org/wiki/Meroplankton

    [2] Not all meroplankton are larvae or juvenile stages of larger organisms. Many dinoflagellates are meroplanktonic, undergoing a seasonal cycle of encystment and dormancy in the benthic zone followed by excystment and reproduction in the pelagic zone before returning to the benthic zone once more.

  8. Richard F. Heck - Wikipedia

    en.wikipedia.org/wiki/Richard_F._Heck

    Of the several reactions developed by Heck, the greatest societal impact has been from the palladium-catalyzed coupling of an alkyne with an aryl halide. This is the reaction that was used to couple fluorescent dyes to DNA bases, allowing the automation of DNA sequencing and the examination of the human genome ; the reaction also allows ...

  9. Bottom trawling - Wikipedia

    en.wikipedia.org/wiki/Bottom_trawling

    Midwater trawling catches pelagic fish such as anchovies and mackerel, whereas bottom trawling targets both bottom-living fish and semi-pelagic species such as cod, squid, shrimp, and rockfish. Trawling is done by a trawler , which can be a small open boat with only 30 hp (22 kW) or a large factory trawler with 10,000 hp (7,500 kW).

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