[C] Open Seas

Cards (12)

  • The epipelagic zone is associated with the euphotic zone, high in photosynthetic activity
  • Plankton - movements change their position, but the current moves their location
    Nekton - ability to swim against strong currents
    Seston - any particle suspended in the sea
  • Living seston - plankton
    Nonliving seston - tripton
    • Plankton and tripton occur concurrently as seston
    • Implications - plastics are eaten when plankton are eaten
  • Phytoplankton - primary producers
    Zooplankton - heterotrophic, eukaryotic
    Bacterioplankton - archaeans and bacteria
    Viriplankton - free viruses, most abundant
  • In higher latitudes, plankton diversity goes down, but biomass goes up
  • Plankton classifications in terms of motility
    • Akinetic
    • Viruses, diatoms, foraminiferans
    • Kinetic
    • Most plankton
    • Move by flagella or jet propulsion
  • Planktons in terms of size (Traditional)
    • Macroplankton
    • Visible to the naked eye, exceed 1mm
    • Microplankton
    • Could be caught with standard plankton net
    • Nanoplankton
    • Centrifuge plankton
    • Pass through plankton nets
  • Planktons in terms of size (Modern) - FPNMMM
    • Femtoplankton
    • Less than 0.0002 mm
    • Picoplankton
    • Less than 0.002 mm
    • Nanoplankton
    • Less than 0.02 mm
    • Microplankton
    • Less than 0.2 mm
    • Mesoplankton
    • Less than 20 mm
    • Macroplankton and Megaplankton
    • 200 - 2000 mm
    • Sargassum weed, larval fishes, jellyfish
  • Plankton in terms of spatial distribution
    • Neritic
    • Low latitudes, shallow waters
    • Meroplankton
    • Nauplius and cyprid larvae of barnacles
    • Oceanic
    • Less diverse in diatoms
    • More salps, larvaceans, sea butterflies
    • Neuston
    • Close to the water surface
    • Pleuston
    • Neuston that extend above the surface
  • Translucent, cobwebby aggregates of marine microbes
    Marine snow
  • Mixed group of zooplankton and fishes that gives a false image of a surface hanging in midwater
    Deep scattering layer
  • Vertical migration
    • Singular upward migration at sunset, single downward migration at sunrise
    • Reasons:
    • Energy conservation
    • Avoidance of predators
    • Exploitation of different currents