zooplankton$93157$ - traducción al italiano
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zooplankton$93157$ - traducción al italiano

OCEAN'S BIOLOGICALLY DRIVEN SEQUESTRATION OF CARBON FROM THE ATMOSPHERE TO THE OCEAN INTERIOR AND SEAFLOOR
Carbonate pump; Zooplankton grazing; Biological carbon pump; Carbon pump; Bioluminescent shunt hypothesis; Ballast mineral; Ballast minerals; Zooplankton sloppy feeding; Zooplankton fecal pellet; Zooplankton fecal pellets
  • bibcode = 2013NatCC...3..195P}}</ref>}}
  • Bioluminescence shunt in the biological carbon pump in the ocean{{hsp}}<ref name=Tanet2020 />}}
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  • Solubility pump: Air-sea exchange of CO<sub>2</sub>}}
  • '''Components of the biological pump'''}}
  • 50px]] Modified text was copied from this source, which is available under a [https://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International License].</ref>
  •  The nitrogen fixing cyanobacteria ''[[Cyanothece]]'' sp. ATCC 51142
  • '''The fate of DOM in the ocean'''}}
  • 50px]] Modified text was copied from this source, which is available under a [https://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International License].</ref>
  • doi=10.2737/WO-GTR-95 }}</ref>
  • author1-link = Graeme Hays}}</ref>
  • 50px]] Modified text was copied from this source, which is available under a [https://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International License].</ref>
  • The microbial loop is a marine trophic pathway which incorporates [[dissolved organic carbon]] (DOC) into the food chain
  •  doi-access=free }}</ref> and the other from the NASA EXPORTS plan.<ref>[[Committee on Earth Observation Satellites]] (2014) "CEOS strategy for carbon observations from space". Response to the [[Group on Earth Observations]] (GEO) carbon strategy. Printed in Japan by JAXA and I&A Corporation.</ref></small>}}
  • '''Morphology of zooplankton fecal pellets{{hsp}}<ref name=Belcher2017 />'''<br />Collected from [[marine snow]] catchers (a–c) and [[sediment trap]]s (d–f).<br />Morphological classes: (a, d) round, (b, e) cylindrical, and (c, f) ovoid.<br /><small>Scale bar {{=}} 0.5 mm</small>}}
  • <small>EOVs {{=}} Essential Ocean Variables</small>}}
  • Oceanic Carbon Cycle — IPCC}}
  • The [[pelagic food web]], showing the central involvement of [[marine microorganism]]s in how the ocean imports carbon and then exports it back to the atmosphere and ocean floor}}
  • 20}} <small>Units are Tg C y<sup>−1</sup></small>
  • sedimentation]] (carbon export) and [[remineralization]] (release to the atmosphere).<ref name=Ionescu2015 />
  • 8}}<small>Carbon fluxes in white boxes are in Gt C yr<sup>−1</sup> and carbon masses in dark boxes are in Gt C</small>
  • 10.3354/ame028175}}.</ref></small>}}
  • '''Effect of temperature on the biological pump'''}} 
Effects of different water temperatures on organic carbon export and remineralization: more carbon is sequestered when temperature is colder compared to when is warmer.<ref name=Boscolo-Galazzo2018 />
  •  Global estimate of the vertically integrated anthropogenic [[dissolved inorganic carbon]] (DIC) in the ocean in recent times (1990s)
  •  The [[whale pump]] is the role played by whales and other marine mammals recycling nutrients in the ocean
  • ( see below ↓ )]]}}

zooplankton      
n. (Zool) zooplancton, gli organismi animali che compongono il plancton

Definición

zooplankton
['zu:?(?)?pla?(k)t(?)n, 'z???(?)-, 'zu:-]
¦ noun Biology plankton consisting of small animals.

Wikipedia

Biological pump

The biological pump (or ocean carbon biological pump or marine biological carbon pump) is the ocean's biologically driven sequestration of carbon from the atmosphere and land runoff to the ocean interior and seafloor sediments. In other words, it is a biologically mediated process which results in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. It is the part of the broader oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed into shells by certain organisms such as plankton and mollusks (carbonate pump).

Budget calculations of the biological carbon pump are based on the ratio between sedimentation (carbon export to the ocean floor) and remineralization (release of carbon to the atmosphere).

The biological pump is not so much the result of a single process, but rather the sum of a number of processes each of which can influence biological pumping. Overall, the pump transfers about 10.2 gigatonnes of carbon every year into the ocean's interior and a total of 1300 gigatonnes carbon over an average 127 years. This takes carbon out of contact with the atmosphere for several thousand years or longer. An ocean without a biological pump would result in atmospheric carbon dioxide levels about 400 ppm higher than the present day.