Two hundred years of zooplankton vertical migration research

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dc.contributor.author Bandara, K.
dc.contributor.author Varpe, Ø.
dc.contributor.author Wijewardene, L.
dc.contributor.author Tverberg, V.
dc.contributor.author Eiane, K.
dc.date.accessioned 2022-11-09T04:39:01Z
dc.date.available 2022-11-09T04:39:01Z
dc.date.issued 2021-08
dc.identifier.citation Bandara, K., Varpe, Ø., Wijewardene, L., Tverberg, V., & Eiane, K. (2021). Two hundred years of zooplankton vertical migration research. Biological Reviews, 96(4), 1547-1589. en_US
dc.identifier.issn 1464-7931
dc.identifier.uri http://ir.lib.ruh.ac.lk/xmlui/handle/iruor/9151
dc.description.abstract Vertical migration is a geographically and taxonomically widespread behaviour among zooplankton that spans across diel and seasonal timescales. The shorter-term diel vertical migration (DVM) has a periodicity of up to 1 day and was first described by the French naturalist Georges Cuvier in 1817. In 1888, the German marine biologist Carl Chun described the longer-term seasonal vertical migration (SVM), which has a periodicity of ca. 1 year. The proximate control and adaptive significance ofDVM have been extensively studied and are well understood. DVM is generally a behaviour controlled by ambient irradiance, which allows herbivorous zooplankton to feed in food-rich shallower waters during the night when light-dependent (visual) predation risk is minimal and take refuge in deeper, darker waters during daytime. However, DVMs of herbivorous zooplankton are followed by their predators, producing complex predator–prey patterns that may be traced across multiple trophic levels. In contrast to DVM, SVM research is relatively young and its causes and consequences are less well understood. During periods of seasonal environmental deterioration, SVM allows zooplankton to evacuate shallower waters seasonally and take refuge in deeper waters often in a state of dormancy. Both DVM and SVM play a significant role in the vertical transport of organic carbon to deeper waters (biological carbon sequestration), and hence in the buffering of global climate change. Although many animal migrations are expected to change under future climate scenarios, little is known about the potential implications of global climate change on zooplankton vertical migrations and its impact on the biological carbon sequestration process. Further, the combined influence of DVM and SVM in determining zooplankton fitness and maintenance of their horizontal (geographic) distributions is not well understood. The contrasting spatial (deep versus shallow) and temporal (diel versus seasonal) scales over which these two migrations occur lead to challenges in studying them at higher spatial, temporal and biological resolution and coverage. Extending the largely population-based vertical migration knowledge base to individual-based studies will be an important way forward. While tracking individual zooplankton in their natural habitats remains a major challenge, conducting trophic-scale, high-resolution, year-round studies that utilise emerging field sampling and observation techniques, molecular genetic tools and computational hardware and software will be the best solution to improve our understanding of zooplankton vertical migrations. en_US
dc.language.iso en en_US
dc.publisher John Wiley & Sons Ltd, Cambridge Philosophical Society en_US
dc.subject Diel vertical migration en_US
dc.subject Seasonal vertical migration en_US
dc.subject Proximate cues en_US
dc.subject Adaptive significance en_US
dc.subject Vertical habitat choice en_US
dc.subject Zooplankton sampling methods en_US
dc.subject Climate change en_US
dc.subject Resting stages en_US
dc.title Two hundred years of zooplankton vertical migration research en_US
dc.type Article en_US


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