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Diel vertical migration

diel vertical migration, diel vertical migration plankton
Diel vertical migration, also known as diurnal vertical migration, is a pattern of movement used by some organisms, such as copepods, living in the ocean and in lakes The migration occurs when organisms move up to the epipelagic zone at night and return to the mesopelagic zone of the oceans or to the hypolimnion zone of lakes during the day The word diel comes from the Latin dies day, and means a 24-hour period It is the greatest migration in the world in terms of biomass


  • 1 Discovery
  • 2 Types and stimuli of vertical migration
    • 21 Endogenous factors
    • 22 Exogenous factors
    • 23 Types of vertical migration
  • 3 Reasons for vertical migration
    • 31 Water transparency
  • 4 Importance for the biological pump
  • 5 See also
  • 6 References


During World War II the US Navy was taking sonar readings of the ocean when they discovered the deep scattering layer DSL The DSL was caused by large groupings of organisms that scattered the sonar to create a false or second bottom The false bottom was shallower during the night and deeper during the day; this was the first recording of diel vertical migration

Once scientists started to do more research on what was causing the DSL, it was discovered that a large range of organisms were vertically migrating Most types of plankton and some types of nekton have exhibited some type of vertical migration, although it is not always diel These migrations may have substantial effects on mesopredators and apex predators by modulating the concentration and accessibility of their prey eg, impacts on the foraging behavior of pinnipeds

Types and stimuli of vertical migration

There are two different factors that are known to play a role in vertical migration, endogenous and exogenous Endogenous factors originate from the organism itself; sex, age, biological rhythms, etc Exogenous factors are environmental factors acting on the organism such as light, gravity, oxygen, temperature, predator-prey interactions, etc

Endogenous factors

Endogenous rhythm 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 Thus suggestions that some type of internal response was causing the migration

Exogenous factors

Light Organisms want to find an optimum light intensity isolume Whether it is no light or a large amount of light, an organism will travel to where it is most comfortable Studies have shown that during a full moon organisms will not migrate up as far or during an eclipse they will start to migrate Temperature Sometimes thermoclines can act as a barrier that an organism will not cross Salinity In areas such as the Arctic melting ice causes a layer of freshwater which organisms cannot cross Predator kairomones A predator might release a chemical cue which could cause its prey to vertically migrate away

Types of vertical migration

Diel This is the most common form Organisms migrate daily, usually up to shallow waters at night and deep waters during the day Seasonal Organisms are found at different depths depending on what season it is Ontogenetic Organisms spend different stages of their life cycle at different depths

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 Light-dependent predation by fish is a common pressure that causes DVM behavior in zooplankton 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 Metabolic advantages By feeding in the warm surface waters at night and residing in the cooler deep waters during the day they can conserve energy 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 recent theory of DVM, termed the Transparency Regulator Hypothesis, argues that water transparency is the ultimate variable that determines the exogenous factor or combination of factors that causes DVM behavior in a given environment 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

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 800–1000 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 something 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 So while currently there is still much research being done on why organisms vertically migrate, it is clear that vertical migration plays a large role in the active transport of dissolved organic matter to depth

See also

  • Krill
  • Phytoplankton
  • Primary production


  1. ^ "Diel Vertical Migration DVM" Retrieved 5 April 2012 
  2. ^ Horning, M; Trillmich, F 1999 "Lunar cycles in diel prey migrations exert a stronger effect on the diving of juveniles than adult Galapagos fur seals" Proceedings of the Royal Society B 266: 1127–1132 doi:101098/rspb19990753 
  3. ^ Enright, JT; WM Hammer 1967 "Vertical Diurnal Migration and Endogenous Rhythmicity" Science 157 3791: 937–941 doi:101126/science1573791937 JSTOR 1722121 PMID 17792830 
  4. ^ Richards, Shane; Hugh Possingham; John Noye 1996 "Diel vertical migration: modeling light-mediated mechanisms" PDF Journal of Plankton Research 18 12: 2199–2222 doi:101093/plankt/18122199 
  5. ^ von Elert, Eric; Georg Pohnert 2000 "Diel Predator specificity of kairomones in diel vertical migration of Daphnia: a chemical approach" OIKOS 88 1: 119–128 doi:101034/j1600-07062000880114x ISSN 0030-1299 
  6. ^ Visser, Andre; Sigrun Jonasdottir 1999 "Lipids, buoyancy and the seasonal vertical migration of Calanus finmarchicus" Fisheries Oceanography 8: 100–106 doi:101046/j1365-2419199900001x 
  7. ^ Kobari, Toru; Tsutomu Ikeda 2001 "Octogenetic vertical migration and life cycle of Neocalanus plumchrus Crustacea:Copepoda in the Oyashio region, with notes on regional variations in body size" PDF Journal of Plankton Research 23 3: 287–302 doi:101093/plankt/233287 
  8. ^ Kerfoot, WC 1985 "Adaptive value of vertical migration: Comments on the predation hypothesis and some alternatives" Contributions in Marine Science 27: 91–113 
  9. ^ Dawidowicz, Piotr; Prędki, Piotr; Pietrzak, Barbara 2012-11-23 "Depth-selection behavior and longevity in Daphnia: an evolutionary test for the predation-avoidance hypothesis" Hydrobiologia 715 1: 87–91 doi:101007/s10750-012-1393-5 ISSN 0018-8158 
  10. ^ "Web of Science - Web of Science Core Collection Full Record" appswebofknowledgecom Retrieved 2015-11-14 
  11. ^ Tiberti, Rocco; Iacobuzio, Rocco 2012-12-09 "Does the fish presence influence the diurnal vertical distribution of zooplankton in high transparency lakes" Hydrobiologia 709 1: 27–39 doi:101007/s10750-012-1405-5 ISSN 0018-8158 
  12. ^ a b c Steinberg, Deborah; Sarah Goldthwait; Dennis Hansell 2002 "Zooplankton vertical migration and the active transport of dissolved organic and inorganic nitrogen in the Sargasso Sea" Deep-Sea Research Part I 49 8: 1445–1461 doi:101016/S0967-06370200037-7 ISSN 0967-0637 
  13. ^ Wiebe, PH; LP Madin; LR Haury; GR Harbison; LM Philbin 1979 "Diel Vertical Migration by Salpa aspera and its potential for large-scale particulate organic matter transport to the deep-sea" Marine Biology 53 3: 249–255 doi:101007/BF00952433 

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