Antarctic krill

Antarctic Krill

Scientific classification
Species:E. superba
Binomial name
Euphausia superba
Dana, 1850

The Antarctic krill (Euphausia superba 1) is a species of krill found in the Antarctic waters of the Southern Ocean. Antarctic krill (shrimp-like invertebrates) live in large schools, called swarms, sometimes reaching densities of 10,000–30,000 individual animals per cubic meterTemplate:Mn. They feed directly on minute phytoplankton, thereby using the primary production energy originally derived from the sun in order to sustain their pelagic life cycleTemplate:Mn. They grow to a length of 6 cm, weigh up to 2 grams, and can live for up to six years. They are the key species in the Antarctic ecosystem and are probably, in terms of biomass, the most successful animal species on the planet (~500 million tonnesTemplate:Mn).



All members of the krill order are shrimp-like animals of the crustacean superorder Eucarida. Their breastplate units, or thoracomers, are joined with the carapace. The short length of these thoracomers on each side of the carapace makes the gills of the Antartic krill visible to the human eye. The legs do not form a jaw structure, which differentiates this order from the crabs, lobsters and shrimp. (See also Euphausia superba at Wikispecies (

Life history

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The eggs are spawned close to the surface and start sinking. In the open ocean they sink for about 10 days: the nauplii hatch in ca. 3000 meter depth

The main spawning time of Antarctic krill is from January through March, both above the continental shelf and also in the upper region of deep sea oceanic areas. In the typical way of all euphausiaceans, the male attaches a sperm package to the genital opening of the female. For this purpose, the first pleopods of the male are constructed as tools. Females lay 6,000–10,000 eggs at one time. They are fertilised as they pass out of the genital opening by sperm liberated from spermatophores which have been attached by the malesTemplate:Mn.

According to the classical hypothesis of MarrTemplate:Mn, derived from the results of the expedition of the famous British research vessel "Discovery", egg development then proceeds as follows: Gastrulation sets in during the descent of the 0.6 mm eggs on the shelf at the bottom, in oceanic areas in depths around 2,000–3,000 m. From the time the egg hatches, the 1st nauplius (i.e., larval stage) starts migrating towards the surface with the aid of its three pairs of legs; the so-called developmental ascent.

The next two larval stages, termed 2nd nauplius and metanauplius, still do not eat but are nourished by the remaining yolk. After three weeks, the little krill has finished the ascent. Growing larger, additional larval stages follow (2nd and 3rd calyptopis, 1st to 6th furcilia). They are characterized by increasing development of the additional legs, the compound eyes and the setae (bristles). At 15 mm, the juvenile krill resembles the habitus of the adults. Krill reach maturity after two to three years. Like all crustaceans, krill must molt in order to grow. Approximately every 13 to 20 days krill shed their chitin skin and leave it behind as exuvia.


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The head of Antarctic krill. Observe the bioluminescent organ at the eyestalk and the nerves visible in the antennae, the gastric mill, the filtering net at the thoracopods and the rakes at the tips of the thoracopods.

The gut of E. superba can often be seen to be shining in green through the animal's transparent skin, an indication that this species feeds predominantly on phytoplankton—especially very small diatoms (20 micrometer), which it filters from the water with a feeding basket [1] ( The glass shells of the diatoms are cracked in the "gastric mill" and then digested in the hepatopancreas. They can also catch and eat copepods, amphipods and other small zooplankton. The gut forms a straight tube; its digestive efficiency is not very high and therefore a lot of carbon is still left in the feces (see below).

In aquaria, krill have been observed eating each other. When they are not fed in aquaria, they shrink in size after molting, which is exceptional for animals the size of krill. Likely this is an adaptation to the seasonality of their food supply, which is mostly limited in the dark winter months under the ice.

Filter feeding

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Krill feeding under high phytoplankton concentration. A slow motion movie (from 300 frames/sec; 490kB) is also available.

Main article: Filter feeder.

The Antarctic krill manages to directly utilize the minute phytoplankton cells, which no other higher animal of krill size can do. This is accomplished through filter feeding, using the krill's highly developed front legs, providing for a very efficient filtering apparatusTemplate:Mn: the six thoracopods form a very effective "feeding basket" used to collect phytoplankton from the open water. In the finest areas the openings are only 1 micrometer. SEM images of this amazing stucture can be studied here ( In the movie linked to the right, the krill is hovering at a 55° angle on the spot. In lower food concentrations, the feeding basket is pushed through the water for over half a meter in an opened position, like in the in situ image below, and then the algae are combed to the mouth opening with special setae on the inner side of the thoracopods.

Ice-algae raking

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Antarctic Krill feeding off ice-algae - the surface of the ice on the left side is colored green - click in the image for larger views - this picture has been taken by a ROV

Antarctic Krill can scrape off the green lawn of ice-algae from the underside of the pack ice [2] ( The image to the right, taken via a ROVTemplate:Mn, shows how most krill swim in an upside-down position directly under the ice. Only a single animal (in the middle) can be seen hovering in the free water. Krill have developed special rows of rake-like setae at the tips of the thoracopods, and graze the ice in a zig-zag fashion, akin to a lawnmower. One krill can clear an area of a square foot in about 10 minutes. It is relatively new knowledge that the film of ice algae is very well developed over vast areas, often containing much more carbon than the whole water column below. Krill find an extensive energy source here, especially in the spring.

The biological pump and carbon sequestration

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In situ image taken with an ecoSCOPE - a green spit ball is visible in the lower right of the image and a green fecal string in the lower middle (for higher resolution and history click into the image)

The krill is a highly untidy feeder, and it often spits out aggregates of phytoplankton (spit balls) containing thousands of cells sticking together. It also produces fecal strings that still contain significant amounts of carbon and the glass shells of the diatoms. Both are heavy and sink very fast into the abyss. This process is called the biological pump. As the waters around Antarctica are very deep (2,000 – 4,000 m), they act as a Carbon dioxide sink: this process exports large quantities of carbon (fixed Carbon dioxide, CO2) from the biosphere and sequesters it for about 1,000 years.

If the phytoplankton is consumed by other components of the pelagic ecosystem, most of the carbon remains in the upper strata. There is speculation that this process is one of the largest biofeedback mechanisms of the planet, maybe the most sizable of all, driven by a gigantic biomass. Still more research is needed to quantify the Southern Ocean ecosystem.

Biological peculiarities


Missing image
Watercolor of bioluminescent krill

Krill are often referred to as light-shrimp because they can emit light, produced by bioluminiscent organs. These organs are located on various parts of the individual krill's body: one pair of organs at the eyestalk (c.f. the image of the head above), another pair on the hips of the 2nd and 7th thoracopods, and singular organs on the four pleonsternites. These light organs emit a yellow-green light periodically, for up to 2 to 3 seconds. They are considered so highly developed that they can be compared with a torchlight: a concave reflector in the back of the organ and a lens in the front guide the light produced, and the whole organ can be rotated by muscles. The function of these lights is not yet fully understood; some hypotheses have suggested they serve to compensate the krill's shadow so that they are not visible to predators from below; other speculations maintain that they play a significant role in mating or schooling at night.

The krill's bioluminescent organs contain several fluorescent substances. The major component has a maximum fluorescence at an excitation of 355 nm and emission of 510 nmTemplate:Mn.

Escape reaction

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Lobstering krill

Krill use an escape reaction to evade predators, swimming backwards very quickly by flipping their telson. This swimming pattern is also known as lobstering. Krill can reach speeds of over 60 cm per secondTemplate:Mn. The trigger time to optical stimulus is, despite the low temperatures, only 55 milliseconds.

The compound eye

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Electron microscope image of the compound eye - the eyes are deep black in the living animal

Although the uses for and reasons behind the development of their massive black compound eyes remain a mystery, there is no doubt that antarctic krill have one of the most fantastic structures for vision seen in nature.

As mentioned above, krill can shrink in size from one molt to the next, which is generally thought to be a survival strategy to adapt to scarce food supplies (a smaller body needs less energy, i.e., food). However, the animal's eyes do not shrink when this happens. The ratio between eye size and body length has thus been found to be a reliable indicator of starvationTemplate:Mn.

Geographical distribution

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Krill distribution on a NASA SeaWIFS image - the main concentrations are in the Scotia Sea at the Antarctic Peninsula

Antarctic Krill are found thronging the surface waters of the Southern Ocean; they have a circumpolar distribution, with the highest concentrations located in the Atlantic sector.

The northern boundary of the Southern Ocean with its Atlantic, Pacific Ocean and Indian Ocean sectors is defined more or less by the Antarctic convergence, a circumpolar front where the cold Antarctic surface water submerges below the warmer subantarctic waters. This front runs roughly at 55° South; from there to the continent, the Southern Ocean covers 32 million square kilometers. This is 65 times the size of the North Sea. In the winter season, more than three quarters of this area become covered by ice, whereas 24 million square kilometers become ice free in summer. The water temperatures range between - 1.3 and 3° C.

The waters of the Southern Ocean form a system of currents. Whenever there is a West Wind Drift, the surface strata travels around Antarctica in an easterly direction. Near the continent, the East Wind Drift runs counterclockwise. At the front between both, large eddies develop, for example, in the Weddell Sea. The krill schools drift with these water masses, to establish one single stock all around Antarctica, with gene exchange over the whole area. Currently, there is little knowledge of the precise migration patterns since individual krill cannot be tagged yet to track their movements.

Position in the Antarctic ecosystem

The Antarctic krill is the keystone species of the Antarctica ecosystem, and provides an important food source for whales, seals, Leopard Seals, fur seals, Crabeater Seals, squid, icefish, penguins, albatrosses and many other species of birds. Crabeater seals have even developed special teeth as an adaptation to catch this abundant food source: its most unusual multilobed teeth enable this species to sieve krill from the water. Its dentition looks like a perfect strainer, but how it operates in detail is still unknown. Crabeaters are the most abundant seal in the world; their diet consists to 98% of E. superba. These seals consume over 63 million tonnes of krill each yearTemplate:Mn. Leopard seals have developed similar teeth (45% krill in diet). All seals consume 63–130 million tonnes, all whales 34–43 million tonnes, the birds 15–20 million tonnes, the squids 30–100 million tonnes, and the fish 10–20 million tonnes, adding up to 152–313 million tonnes of krill consumption each yearTemplate:Mn.

The size step between krill and its prey is unusually large: generally it takes three or four steps from the 20 micrometer-tiny phytoplankton cells to a krill-sized organism (via small copepods, large copepods, mysids to 5 cm fish)Template:Mn. The next size step in the food chain to the whales is also enormous, a phenomenon only found in the Antarctic ecosystem. E. superba lives only in the Southern Ocean. In the North Atlantic, Meganyctiphanes norvegica and in the Pacific, Euphausia pacifica are the dominant species.

Biomass and Production

The Antarctic krill's biomass is estimated to be between 125 to 725 million tonnesTemplate:Mn, making E. superba the most successful animal species on the planet. It should be noted that of all animals visible to the naked eye some biologists speculate that ants provide the largest biomass (but this speculation adds up hundreds of different species) whilst others speculate that it could be the copepods, but this too would be the sum of many hundreds of species that exist over the planet. To get an impression of the biomass of E. superba against that of other species: The total non-krill yield from all world fisheries, finfish, shellfish, cephalopods and plankton is about 100 million tonnes per year whilst estimates of the Antarctic krill production are between 13 million to several billion tonnes per year. The reason Antarctic krill are able to build up such a high biomass and production is that the waters around the icy Antarctic continent harbor one of the the largest plankton assemblages in the world, possibly the largest. It is filled with phytoplankton, as the water rises from the depths to the light flooded surface, it brings nutrients from all of the world's oceans back into the photic zone. Thus primary production range between 1 and 2 g carbon per square meter, this, however, is not an outstanding production. Close to the ice it can reach 30–50 g carbon per square meter, but the area of good production is just enormous, and in the Austral summer there are many hours of daylight.

Decline with shrinking pack ice

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after data compiled by Loeb et al. 1997Template:Mn - temperature and pack ice area - the scale for the ice is inverted to demonstrate the correlation - the horizontal line is the freezing point - the oblique line the average of the temperature - in 1995 the temperature reached the freezing point

There are concerns that the Antarctic krill's overall biomass has been declining rapidly over the last few decades. Some scientists have speculated this value being as high as 80%. This could be caused by the reduction of the pack ice zone due to the consequence of global warmingTemplate:Mn. The graph on the right depicts the rising temperatures of the Southern Ocean and the loss of pack ice (on an inverted scale) over the last years 40 years. Antarctic krill, especially in the early stages of development, seem to need the pack ice structures in order to have a fair chance of survival. The pack ice provides natural cave-like features which the krill uses to evade their predators. In the years of low pack ice conditions the krill is substituted by SalpsTemplate:Mn.


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Annual world catch of E. superba, compiled from FAO dataTemplate:Mn.

Main article: Krill fishery.

The fishery of the Antarctic krill is on the order of 100,000 tonnes per year. The major catching nations are Japan and Poland. The products are used largely in Japan as a delicacy and worldwide as animal food and fish bait. Krill fisheries are difficult to operate in two important respects. First, a krill net needs to have very fine meshes, as it has a very high drag, producing a bow wave that deflects the krill to the sides. Second, fine meshes tend to clog very fast. Additionally, a fine net is also, by definition, a very delicate net, and the first krill nets designed exploded while fishing through the krill schools.

Yet another problem is bringing the krill catch on board. When the full net is hauled out of the water, the organisms compress each other, resulting in great loss of the krill's liquids. Experiments have been carried out to pump krill, while still in water, through a large tube on board. Special krill nets also are currently under development. The processing of the krill must be very rapid since the catch deteriorates within several hours. Processing aims are splitting the muscular hind part from the front part and separating the chitin armor, in order to produce frosted products and concentrate powders. Its high protein and vitamin content makes krill quite suitable for both direct human consumption and the animal-feed industryTemplate:Mn.

Future visions and ocean engineering

Despite the scarce knowledge available about the whole Antarctic ecosystem, large scale experiments involving krill are already being performed to increase carbon sequestration: in vast areas of the Southern Ocean there are plenty of nutrients, but still, the phytoplankton does not grow much. These areas are termed HNLC (high nutrient, low carbon). The phenomenon is called the Antarctic Paradox, and occurs because iron is missing [3] ( Relatively small injections of iron from research vessels trigger very large blooms, covering many miles. The hope is that such large scale exercises will draw down carbon dioxide as compensation for the burning of fossil fuels [4] ( Krill is the key player in collecting the minute plankton cells so as to sink faster, in the form of spit balls and fecal strings. The vision is that in the future a fleet of tankers would circle the Southern Seas, injecting iron, so this relatively unknown animal might help keep cars and air conditioners running.


Note 1: This species is often misspelled Euphasia superba [5] ( or Eupausia superba [6] (


Further reading

  • Template:Mnb2 Hempel, I.; Hempel, G.: Field observations on the developmental ascent of larval Euphausia superba (Crustacea). Polar Biol 6; pp. 121 – 126; 1986.
  • Template:Mnb2 Hempel, G.: Antarctic marine food webs. In Siegfried, W. R.; Condy, P. R.; Laws, R. M. (eds): Antarctic nutrient cycles and food webs. Springer-Verlag, Berlin, pp. 266 – 270; 1985.
  • Template:Mnb2 Hempel, G.: The krill-dominated pelagic system of the Southern Ocean. Envir. Inter. 13, pp. 33 – 36; 1987.
  • Template:Mnb2 Hempel, G.: Life in the Antarctic sea ice zone. Polar Record 27(162); pp. 249 – 253; 1991
  • Template:Mnb2 Hempel, G.; Sherman, K.: Large marine ecosystems of the world: trends in exploitation, protection, and research. Elsevier, Amsterdam: Large marine ecosystems 12, 423 pp; 2003
  • Template:Mnb2 Mauchline, J.; Fisher, L.R.: The biology of euphausiids. Adv. Mar. Biol. 7; 1969.
  • Template:Mnb2 Nicol, S.; Foster, J.: Recent trends in the fishery for Antarctic krill (, Aquat. Living Resour. 16, pp. 42 – 45; 2003.
  • Template:Mnb2 Quetin, L. B., Ross, R. M. and Clarke, A.: Krill energetics: seasonal and environmental aspects of the physiology of Euphausia superba. In El-Sayed, S. Z. (ed.): Southern Ocean Ecology: the BIOMASS perspective, pp. 165 – 184. Cambridge University Press, 1994.
  • Template:Mnb2 Sahrhage, D.: Antarctic Krill Fisheries: Potential Resources and Ecological Concerns. In Caddy, J. F. (ed.): Marine Invertebrate Fisheries; their assessment and management; pp. 13 – 33. Wiley, 1989.

External links

de:krill es:krill fr:Krill ja:オキアミ nl:Krill no:krill pl:Kryl antarktyczny sv:Krill


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