Discovery
The phenomenon was first documented by French naturalist Georges Cuvier in 1817. He noted that '' daphnia'', a type ofTypes of vertical migration
Diel
This is the most common form of vertical migration. Organisms migrate on a daily basis through different depths in the water column. Migration usually occurs between shallow surface waters of the epipelagic zone and deeper mesopelagic zone of the ocean or hypolimnion zone of lakes. There are three recognized types of diel vertical migration:Nocturnal vertical migration
In the most common form, nocturnal vertical migration, organisms ascend to the surface around dusk, remaining at the surface for the night, then migrating to depth again around dawn.Reverse migration
Reverse migration occurs with organisms ascending to the surface at sunrise and remaining high in the water column throughout the day until descending with the setting sun.Twilight diel vertical migration
Twilight diel vertical migration involves two separate migrations in a single 24-hour period, with the first ascent at dusk followed by a descent at midnight, often known as the "midnight sink". The second ascent to the surface and descent to the depths occurs at sunrise.Seasonal
Organisms are found at different depths depending on what season it is. Seasonal changes to the environment may influence changes to migration patterns. Normal diel vertical migration occurs in species ofOntogenetic
Organisms spend different stages of their life cycle at different depths. There are often pronounced differences in migration patterns of adult female copepods, like '' Eurytemora affinis,'' which stay at depth with only a small upward movement at night, compared to the rest of its life stages which migrate over 10 meters. In addition, there is a trend seen in other copepods, like ''Acartia spp''. that have an increasing amplitude of their DVM seen with their progressive life stages. This is possibly due to increasing body size of the copepods and the associated risk of visual predators, like fish, as being larger makes them more noticeable.Vertical migration stimuli
There are two different types of factors that are known to play a role in vertical migration, endogenous andEndogenous factors
Endogenous rhythm
Biological clocks are an ancient and adaptive sense of time innate to an organism that allows them to anticipate environmental changes and cycles so they are able to physiologically and behaviorally respond to the expected change. Evidence of circadian rhythms controlling DVM, metabolism, and even gene expression have been found in copepod species, ''Calanus finmarchicus''. These copepods were shown to continue to exhibit these daily rhythms of vertical migration in the laboratory setting even in constant darkness, after being captured from an actively migrating wild population. An experiment was done at the Scripps Institution of Oceanography which kept organisms in column tanks with light/dark cycles. A few days later the light was changed to a constant low light and the organisms still displayed diel vertical migration. This suggests that some type of internal response was causing the migration.Clock gene expression
Many organisms including the copepod ''C. finmarchicus'', has genetic material devoted to maintaining its biological clock. The expression of these genes varies temporally with the expression significantly increasing following dawn and dusk at times of greatest vertical migration seen in this species. These findings may indicate they work as a molecular stimulus for vertical migration.Body size
The relative body size of an organism has been found to effect DVM. Bull trout express daily and seasonal vertical migrations with smaller individuals always staying at a deeper layer than the larger individuals. This is most likely due to a predation risk, but is dependent on the individuals own size such that smaller animals may be more inclined to remain at depth.Exogenous factors
Light
"Light is the most common and critical cue for vertical migration". However, as of 2010, there had not been sufficient research to determine which aspect of the light field was responsible. As of 2020, research has suggested that both light intensity and spectral composition of light are important.Temperature
Organisms will migrate to a water depth with temperatures that best suit the organisms needs, for example some fish species migrate to warmer surface waters in order to aid digestion. Temperature changes can influence swimming behavior of some copepods. In the presence of a strong thermocline some zooplankton may be inclined to pass through it, and migrate to the surface waters, though this can be very variable even in a single species. The marine copepod, ''Calanus finmarchicus,'' will migrate through gradients with temperature differences of 6 °C over George's Ban''k;'' whereas, in the North Sea they are observed to remain below the gradient.Salinity
Changes in salinity may promote organism to seek out more suitable waters if they happen to bePressure
Pressure changes have been found to produce differential responses that result in vertical migration. Many zooplankton will react to increased pressure with positive phototaxis, a negative geotaxis, and/or a kinetic response that results in ascending in the water column. Likewise, when there is a decrease in pressure, the zoo plankton respond by passively sinking or active downward swimming to descend in the water column.Predator kairomones
A predator might release a chemical cue which could cause its prey to vertically migrate away. This may stimulate the prey to vertically migrate to avoid said predator. The introduction of a potential predator species, like a fish, to the habitat of diel vertical migrating zooplankton has been shown to influence the distribution patterns seen in their migration. For example, a study used ''Daphnia'' and a fish that was too small to prey of them (''Lebistus reticulatus''), found that with the introduction of the fish to the system the ''Daphnia'' remained below the thermocline, where the fish was not present. This demonstrates the effects of kairomones on ''Daphnia'' DVM''.''Tidal patterns
Some organisms have been found to move with the tidal cycle. A study looked at the abundance of a species of small shrimp, ''Acetes sibogae,'' and found that they tended to move further higher in the water column and in higher numbers during flood tides than during ebb tides experiences at the mouth of an estuary. It is possible that varying factors with the tides may be the true trigger for the migration rather than the movement of the water itself, like the salinity or minute pressure changes.Reasons for vertical migration
There are many hypotheses as to why organisms would vertically migrate, and several may be valid at any given time.Predator avoidance
The universality of DVM suggests that there is some powerful common factor behind it. The connection between available light and DVM has led researchers to theorize that organisms may stay in deeper, darker areas during the day to avoid being eaten by predators who depend on light to see and catch their prey. While the ocean's surface provides an abundance of food, it may be safest for many species to visit it at night. Light-dependent predation by fish is a common pressure that causes DVM behavior in zooplankton and krill. A given body of water may be viewed as a risk gradient whereby the surface layers are riskier to reside in during the day than deep water, and as such promotes varied longevity among zooplankton that settle at different daytime depths. Indeed, in many instances it is advantageous for zooplankton to migrate to deep waters during the day to avoid predation and come up to the surface at night to feed. For example, the northern krill ''Meganyctiphanes norvegica'' undergoes diel vertical migration to avoid planktivorous fish. Patterns among migrators seem to support the predator avoidance theory. Migrators will stay in groups as they migrate, a behavior that may protect individuals within the group from being eaten. Groups of smaller, harder to see animals begin their upward migration before larger, easier to see species, consistent with the idea that detectability by visual predators is a key issue. Small creatures may start to migrate upwards as much as 20 minutes before the sun sets, while large conspicuous fish may wait as long as 80 minutes after the sun goes down. Species that are better able to avoid predators also tend to migrate before those with poorer swimming capabilities. Squid are a primary prey for Risso's dolphins ('' Grampus griseus''), an air-breathing predator, but one that relies on acoustic rather than visual information to hunt. Squid delay their migration pattern by about 40 minutes when dolphins are about, lessening risk by feeding later and for a shorter time.Metabolic advantages
Another possibility is that predators can benefit from diel vertical migration as an energy conservation strategy. Studies indicate that male dogfish ('' Scyliorhinus canicula'') follow a "hunt warm - rest cool" strategy that enables them to lower their daily energy costs. They remain in warm water only long enough to obtain food, and then return to cooler areas where their metabolism can operate more slowly. Alternatively, organisms feeding on the bottom in cold water during the day may migrate to surface waters at night in order to digest their meal at warmer temperatures.Dispersal and transport
Organisms can use deep and shallow currents to find food patches or to maintain a geographical location.Avoid UV damage
The sunlight can penetrate into the water column. If an organism, especially something small like a microbe, is too close to the surface the UV can damage them. So they would want to avoid getting too close to the surface, especially during daylight.Water transparency
A theory known as the “transparency-regulator hypothesis" predicts that "the relative roles of UV and visual predation pressure will vary systematically across a gradient of lake transparency." In less transparent waters, where fish are present and more food is available, fish tend to be the main driver of DVM. In more transparent bodies of water, where fish are less numerous and food quality improves in deeper waters, UV light can travel farther, thus functioning as the main driver of DVM in such cases.Unusual events
Due to the particular types of stimuli and cues used to initiate vertical migration, anomalies can change the pattern drastically. For example, the occurrence of midnight sun in the Arctic induces changes to planktonic life that would normally perform DVM with a 24-hour night and day cycle. In the summers of the Arctic the Earth's north pole is directed toward the sun creating longer days and at the high latitude continuous day light for more than 24-hours. Species of foraminifera found in the ocean have been observed to cease their DVM pattern, and rather remain at the surface in favor of feeding on the phytoplankton. For example ''Neogloboquadrina pachyderma'', and for those species that contain symbionts, like ''Turborotalita quinqueloba'', remain in sunlight to aid photosynthesis. Changes in sea-ice and surface chlorophyll concentration are found to be stronger determinants of the vertical habitat of Arctic ''N. pachyderma''. There is also evidence of changes to vertical migration patterns during solar eclipse events. In the moments that the sun is obscured during normal day light hours, there is a sudden dramatic decrease in light intensity. The decreased light intensity, replicates the typical lighting experienced at night time that stimulate the planktonic organisms to migrate. During an eclipse, some copepod species distribution is concentrated near the surface, for example ''Calanus finmarchicus'' displays a classic diurnal migration pattern but on a much shorter time scale during an eclipse.Importance for the biological pump
The biological pump is the conversion of CO2 and inorganic nutrients by plant photosynthesis into particulate organic matter in the euphotic zone and transference to the deeper ocean. This is a major process in the ocean and without vertical migration it wouldn't be nearly as efficient. The deep ocean gets most of its nutrients from the higher water column when they sink down in the form of marine snow. This is made up of dead or dying animals and microbes, fecal matter, sand and other inorganic material. Organisms migrate up to feed at night so when they migrate back to depth during the day they defecate large sinking fecal pellets. Whilst some larger fecal pellets can sink quite fast, the speed that organisms move back to depth is still faster. At night organisms are in the top 100 metres of the water column, but during the day they move down to between 800 and 1000 meters. If organisms were to defecate at the surface it would take the fecal pellets days to reach the depth that they reach in a matter of hours. Therefore, by releasing fecal pellets at depth they have almost 1000 metres less to travel to get to the deep ocean. This is known as active transport. The organisms are playing a more active role in moving organic matter down to depths. Because a large majority of the deep sea, especially marine microbes, depends on nutrients falling down, the quicker they can reach the ocean floor the better. Zooplankton and salps play a large role in the active transport of fecal pellets. 15–50% of zooplankton biomass is estimated to migrate, accounting for the transport of 5–45% of particulate organic nitrogen to depth. Salps are large gelatinous plankton that can vertically migrate 800 meters and eat large amounts of food at the surface. They have a very long gut retention time, so fecal pellets usually are released at maximum depth. Salps are also known for having some of the largest fecal pellets. Because of this they have a very fast sinking rate, small detritus particles are known to aggregate on them. This makes them sink that much faster. As previously mentioned, the lipid pump represents a substantial flux of POC to the deep ocean in the form of lipids produced by large overwintering copepods. Through overwintering, these lipids are transported to the deep in autumn and are metabolized at depths below the thermocline through winter before the copepods rise to the surface in the spring. The metabolism of these lipids reduces this POC at depth while producing CO2 as a waste product, ultimately serving as a potentially significant contributor to oceanicSee also
* Krill * Phytoplankton *References
{{collective animal behaviour Aquatic ecology Biological oceanography Marine biology Planktology Animal migration