Jelly-falls are marine carbon cycling events whereby gelatinous zooplankton, primarily cnidarians, sink to the seafloor and enhance carbon and nitrogen fluxes via rapidly sinking particulate organic matter. These events provide nutrition to benthic megafauna and bacteria. Jelly-falls have been implicated as a major "gelatinous pathway" for the sequestration of labile biogenic carbon through the biological pump. The high abundance and wide geographic distribution of gelatinous zooplankton means that jelly-falls are a large component of the global biological pump. The contribution they provide to the export of labile organic carbon to the seafloor is comparable to that of other detrital pulses like phytoplankton blooms and marine snow aggregates. These events are common in protected areas with high levels of primary production and water quality suitable to support cnidarian species. These areas include estuaries and several studies have been conducted in fjords of Norway. In rare cases where scavengers are not present or the water is particularly still, thousands of jellyfish can accumulate in depressions on the seafloor to create "jelly-lakes".
Initiation
Jelly-falls are primarily made up of the decaying bodies of Cnidaria and Thaliacea (Pyrosomida, Doliolida, and Salpida). Several circumstances can trigger the death of gelatinous organisms which would cause them to sink. These include high levels of primary production that can clog the feeding apparatuses of the organisms, a sudden temperature change, when an old bloom runs out of food, when predators damage the bodies of the jellies, and parasitism. In general, however, jelly-falls are linked to jelly-blooms and primary production, with over 75% of the jelly falls in subpolar and temperate regions occurring after spring blooms, and over 25% of the jelly-falls in the tropics occurring after upwelling events. With global climates shifting towards creating warmer and more acidic oceans, conditions not favored by non-resilient species, jellies are likely to grow in population sizes. Eutrophic areas and dead zones can become jelly hot spots with substantial blooms. As the climate changes and ocean waters warm, jelly blooms become more prolific and the transport of jelly-carbon to the lower ocean increases. With a possible slowing of the classic biological pump, the transport of carbon and nutrients to the deep sea through jelly-falls may become more and more important to deep ocean.
Anthropogenic links Due to human activity there has been an increase in the frequency and intensity of jellyfish blooms. This in turn has been speculated to enhance the occurrence of jelly-falls. Overfishing small pelagic fishes and other zooplanktivores can reduce competition for planktonic resources and removes the key predators that feed on gelatinous zooplankton which allows jellyfish populations to increase. Coastal eutrophication from agricultural and urban runoff also creates hypoxic zones that are avoided by most fish and crustaceans species, but many cnidarians and thaliaceans can tolerate which further benefits jellyfish populations. Jelly derived carbon on the seafloor is expected to increase substantially due to these reasons along with the rise of sea surface temperatures primarily in coastal and shelf regions.
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