krill$503375$ - перевод на испанский
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krill$503375$ - перевод на испанский

OIL DERIVED FROM EUPHAUSIA SUPERBA
Krill Oil

krill      
n. kril, conjunto de varias especies de crustáceos marinos de alto valor nutritivo
euphausiids         
  • fermented]] krill, used to make ''[[Bagoong alamang]]'', a type of [[shrimp paste]] from the [[Philippines]]
  • 50px
  • 50px]] Material 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 [[gill]]s of krill are externally visible
  • A krill swarm
  • Krill anatomy explained, using ''[[Euphausia superba]]'' as a model
  • Deep frozen plates of [[Antarctic krill]] for use as animal feed and raw material for cooking
  • nauplius]] of ''[[Euphausia pacifica]]'' hatching, emerging backwards from the egg
  • mm}}
  • Beating [[pleopod]]s of a swimming [[Antarctic krill]]
  • '''Processes in the biological pump'''}} Phytoplankton convert CO2, which has dissolved from the atmosphere into the surface oceans (90 Gt yr−1) into particulate organic carbon (POC) during primary production (~ 50 Gt C yr−1). Phytoplankton are then consumed by krill and small zooplankton grazers, which in turn are preyed upon by higher trophic levels. Any unconsumed phytoplankton form aggregates, and along with zooplankton faecal pellets, sink rapidly and are exported out of the mixed layer (< 12 Gt C yr−1 14). Krill, zooplankton and microbes intercept phytoplankton in the surface ocean and sinking detrital particles at depth, consuming and respiring this POC to CO2 (dissolved inorganic carbon, DIC), such that only a small proportion of surface-produced carbon sinks to the deep ocean (i.e., depths > 1000 m). As krill and smaller zooplankton feed, they also physically fragment particles into small, slower- or non-sinking pieces (via sloppy feeding, coprorhexy if fragmenting faeces), retarding POC export. This releases dissolved organic carbon (DOC) either directly from cells or indirectly via bacterial solubilisation (yellow circle around DOC). Bacteria can then remineralise the DOC to DIC (CO2, microbial gardening). Diel vertically migrating krill, smaller zooplankton and fish can actively transport carbon to depth by consuming POC in the surface layer at night, and metabolising it at their daytime, mesopelagic residence depths. Depending on species life history, active transport may occur on a seasonal basis as well. Numbers given are carbon fluxes (Gt C yr−1) in white boxes and carbon masses (Gt C) in dark boxes.<ref name=Cavan2019 />
  • '''Role of Antarctic krill in biogeochemical cycles'''}} Krill (as swarms and individuals) feed on phytoplankton at the surface (1) leaving only a proportion to sink as phytodetrital aggregates (2), which are broken up easily and may not sink below the permanent thermocline. Krill also release faecal pellets (3) whilst they feed, which can sink to the deep sea but can be consumed (coprophagy) and degraded as they descend (4) by krill, bacteria and zooplankton. In the marginal ice zone, faecal pellet flux can reach greater depths (5). Krill also release moults, which sink and contribute to the carbon flux (6). Nutrients are released by krill during sloppy feeding, excretion and egestion, such as iron and ammonium (7, see Fig. 2 for other nutrients released), and if they are released near the surface can stimulate phytoplankton production and further atmospheric CO2 drawdown. Some adult krill permanently reside deeper in the water column, consuming organic material at depth (8). Any carbon (as organic matter or as CO2) that sinks below the permanent thermocline is removed from subjection to seasonal mixing and will remain stored in the deep ocean for at least a year (9). The swimming motions of migrating adult krill that migrate can mix nutrient-rich water from the deep (10), further stimulating primary production. Other adult krill forage on the seafloor, releasing respired CO2 at depth and may be consumed by demersal predators (11). Larval krill, which in the Southern Ocean reside under the sea ice, undergo extensive diurnal vertical migration (12), potentially transferring CO2 below the permanent thermocline. Krill are consumed by many predators including baleen whales (13), leading to storage of some of the krill carbon as biomass for decades before the whale dies, sinks to the seafloor and is consumed by deep sea organisms.<ref name=Cavan2019 />
ORDER OF CRUSTACEANS
Euphausids; Euphausid; Euphausiids; Euphausiacea; Euphausiid; Euphausiidae; Euphausidae; Euphausiid shrimp; Euphausiid shrimps; Kril; Okiami; Euphasiacea
(n.) = euphausiacea, eufasiáceo
Ex: Oarfish feed primarily on zooplankton, selectively straining tiny euphausiids, shrimp, and other crustaceans from the water.
krill         
  • fermented]] krill, used to make ''[[Bagoong alamang]]'', a type of [[shrimp paste]] from the [[Philippines]]
  • 50px
  • 50px]] Material 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 [[gill]]s of krill are externally visible
  • A krill swarm
  • Krill anatomy explained, using ''[[Euphausia superba]]'' as a model
  • Deep frozen plates of [[Antarctic krill]] for use as animal feed and raw material for cooking
  • nauplius]] of ''[[Euphausia pacifica]]'' hatching, emerging backwards from the egg
  • mm}}
  • Beating [[pleopod]]s of a swimming [[Antarctic krill]]
  • '''Processes in the biological pump'''}} Phytoplankton convert CO2, which has dissolved from the atmosphere into the surface oceans (90 Gt yr−1) into particulate organic carbon (POC) during primary production (~ 50 Gt C yr−1). Phytoplankton are then consumed by krill and small zooplankton grazers, which in turn are preyed upon by higher trophic levels. Any unconsumed phytoplankton form aggregates, and along with zooplankton faecal pellets, sink rapidly and are exported out of the mixed layer (< 12 Gt C yr−1 14). Krill, zooplankton and microbes intercept phytoplankton in the surface ocean and sinking detrital particles at depth, consuming and respiring this POC to CO2 (dissolved inorganic carbon, DIC), such that only a small proportion of surface-produced carbon sinks to the deep ocean (i.e., depths > 1000 m). As krill and smaller zooplankton feed, they also physically fragment particles into small, slower- or non-sinking pieces (via sloppy feeding, coprorhexy if fragmenting faeces), retarding POC export. This releases dissolved organic carbon (DOC) either directly from cells or indirectly via bacterial solubilisation (yellow circle around DOC). Bacteria can then remineralise the DOC to DIC (CO2, microbial gardening). Diel vertically migrating krill, smaller zooplankton and fish can actively transport carbon to depth by consuming POC in the surface layer at night, and metabolising it at their daytime, mesopelagic residence depths. Depending on species life history, active transport may occur on a seasonal basis as well. Numbers given are carbon fluxes (Gt C yr−1) in white boxes and carbon masses (Gt C) in dark boxes.<ref name=Cavan2019 />
  • '''Role of Antarctic krill in biogeochemical cycles'''}} Krill (as swarms and individuals) feed on phytoplankton at the surface (1) leaving only a proportion to sink as phytodetrital aggregates (2), which are broken up easily and may not sink below the permanent thermocline. Krill also release faecal pellets (3) whilst they feed, which can sink to the deep sea but can be consumed (coprophagy) and degraded as they descend (4) by krill, bacteria and zooplankton. In the marginal ice zone, faecal pellet flux can reach greater depths (5). Krill also release moults, which sink and contribute to the carbon flux (6). Nutrients are released by krill during sloppy feeding, excretion and egestion, such as iron and ammonium (7, see Fig. 2 for other nutrients released), and if they are released near the surface can stimulate phytoplankton production and further atmospheric CO2 drawdown. Some adult krill permanently reside deeper in the water column, consuming organic material at depth (8). Any carbon (as organic matter or as CO2) that sinks below the permanent thermocline is removed from subjection to seasonal mixing and will remain stored in the deep ocean for at least a year (9). The swimming motions of migrating adult krill that migrate can mix nutrient-rich water from the deep (10), further stimulating primary production. Other adult krill forage on the seafloor, releasing respired CO2 at depth and may be consumed by demersal predators (11). Larval krill, which in the Southern Ocean reside under the sea ice, undergo extensive diurnal vertical migration (12), potentially transferring CO2 below the permanent thermocline. Krill are consumed by many predators including baleen whales (13), leading to storage of some of the krill carbon as biomass for decades before the whale dies, sinks to the seafloor and is consumed by deep sea organisms.<ref name=Cavan2019 />
ORDER OF CRUSTACEANS
Euphausids; Euphausid; Euphausiids; Euphausiacea; Euphausiid; Euphausiidae; Euphausidae; Euphausiid shrimp; Euphausiid shrimps; Kril; Okiami; Euphasiacea
(n.) = eufasiáceo, euphausiacea, camarón
Ex: Krill is a general term used to describe about 85 species of open-ocean crustaceans known as euphausiids.

Определение

krill
¦ plural noun small shrimp-like planktonic crustaceans which are the principal food of baleen whales. [Meganyctiphanes norvegica and other species, order Euphausiacea.]
Origin
early 20th cent.: from Norw. kril 'small fish fry'.
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Википедия

Krill oil

Krill oil is an extract prepared from a species of Antarctic krill, Euphausia superba. Processed krill oil is commonly sold as a dietary supplement. Two components of krill oil are omega-3 fatty acids similar to those in fish oil, and phospholipid-derived fatty acids (PLFA), mainly phosphatidylcholine (alternatively referred to as marine lecithin).

https://en.wikipedia.org/wiki/Krill oil
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