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  2. Phytoplankton - Wikipedia

    en.wikipedia.org/wiki/Phytoplankton

    Phytoplankton (/ ˌ f aɪ t oʊ ˈ p l æ ŋ k t ə n /) are the autotrophic (self-feeding) components of the plankton community and a key part of ocean and freshwater ecosystems.The name comes from the Greek words φυτόν (phyton), meaning 'plant', and πλαγκτός (planktos), meaning 'wanderer' or 'drifter'.

  3. Ocean fertilization - Wikipedia

    en.wikipedia.org/wiki/Ocean_fertilization

    Adding urea to the ocean can cause phytoplankton blooms that serve as a food source for zooplankton and in turn feed for fish. This may increase fish catches. [54] However, if cyanobacteria and dinoflagellates dominate phytoplankton assemblages that are considered poor quality food for fish then the increase in fish quantity may not be large. [55]

  4. Freshwater phytoplankton - Wikipedia

    en.wikipedia.org/wiki/Freshwater_phytoplankton

    Chlorophyll α is the core photosynthetic pigment that all phytoplankton possess. Concentrations of this pigment, which can be measured remotely, is used as a proxy for phytoplankton biomass in a given location general, the more chlorophyll a, the more phytoplankton biomass, although the CHL a to C ratio May vary between species, and even within the species.

  5. Marine food web - Wikipedia

    en.wikipedia.org/wiki/Marine_food_web

    If phytoplankton dies before it is eaten, it descends through the euphotic zone as part of the marine snow and settles into the depths of sea. In this way, phytoplankton sequester about 2 billion tons of carbon dioxide into the ocean each year, causing the ocean to become a sink of carbon dioxide holding about 90% of all sequestered carbon. [16]

  6. Heterotrophic picoplankton - Wikipedia

    en.wikipedia.org/wiki/Heterotrophic_picoplankton

    Heterotrophic picoplankton play a critical role in nutrient and carbon recycling in ecological food webs [4] by transforming and mineralizing organic matter. [7] Aquatic dissolved organic matter is one of the largest organic pools on Earth and a major part of the carbon cycle. [8]

  7. High-nutrient, low-chlorophyll regions - Wikipedia

    en.wikipedia.org/wiki/High-nutrient,_low...

    Iron availability is not the only regulator of phytoplankton productivity and biomass. [39] [40] In the Southern Ocean, prevailing low temperatures are believed to have a negative impact on phytoplankton growth rates. [40] Phytoplankton growth rate is very intense and short lived in open areas surrounded by sea ice and permanent sea-ice zones.

  8. Planktivore - Wikipedia

    en.wikipedia.org/wiki/Planktivore

    A planktivore is an aquatic organism that feeds on planktonic food, including zooplankton and phytoplankton. [1] [2] Planktivorous organisms encompass a range of some of the planet's smallest to largest multicellular animals in both the present day and in the past billion years; basking sharks and copepods are just two examples of giant and microscopic organisms that feed upon plankton.

  9. Tetraselmis - Wikipedia

    en.wikipedia.org/wiki/Tetraselmis

    Tetraselmis is a genus of phytoplankton. Tetraselmis is a green algal genus within the order Chlorodendrales, and they are characterized by their intensely-colored green chloroplast, their flagellated cell bodies, the presence of a pyrenoid within the chloroplast, and a scale-produced thecal-wall.