Aquatic Invertebrates Codexery

Salp

Barrel-shaped planktonic tunicates with efficient jet propulsion.

Salp

Salps are barrel-shaped, gelatinous creatures that drift through the ocean as plankton. They belong to the family Salpidae and move by squeezing their bodies to jet water through themselves, a method of propulsion that ranks among the most efficient in the animal kingdom. To eat, they filter phytoplankton from the water using internal feeding nets. These animals are found in equatorial, temperate, and cold seas, often near the surface either alone or linked together in long, stringy colonies. The Southern Ocean around Antarctica holds the densest populations, where salps sometimes gather in enormous swarms—often in deep water—and can outnumber krill. Since 1910, krill numbers in that region have dropped while salp numbers have risen. They have also been appearing more frequently along the coast of Washington state. Salps have a two-part life cycle that alternates between generations. Both stages live together in the sea and look quite different, though both are mostly transparent, tubular, and gelatinous, typically 1 to 10 centimeters long. The solitary phase, called an oozooid, is a single barrel-shaped individual that reproduces asexually by budding off a chain of tens to hundreds of tiny salps. These chains form the aggregate phase, where the individuals—called blastozooids—stay attached as they swim and feed, each growing larger. The blastozooids are sequential hermaphrodites: they mature first as females and are fertilized by sperm from older chains. Each then grows a single embryo oozooid attached to its body wall. When released, these young oozooids feed and grow into the solitary phase, completing the cycle. This alternation allows for rapid generation times, and when phytoplankton is plentiful, it leads to short-lived blooms. The blooms end when the salps have filtered out most of the food. During such blooms, mushroom corals and those in the genus *Heteropsammia* sometimes feed on the salps. In 1920, a massive incursion of *Salpa fusiformis* into the North Sea caused the Scottish herring fishery to fail. Salps succeed partly because they respond so quickly to phytoplankton blooms. When food is abundant, they clone themselves rapidly, grazing and growing faster than probably any other multicellular animal, stripping the water of phytoplankton. If the bloom is too dense, however, salps can clog and sink to the bottom. During these events, beaches may become slimy with mats of salp bodies, and other plankton species can see their numbers fluctuate due to competition. The sinking fecal pellets and dead bodies of salps carry carbon to the seafloor, and because salps are so abundant, they significantly affect the ocean’s biological pump. Large shifts in their numbers or distribution could alter the ocean’s carbon cycle and potentially influence climate change. Salps are closely related to other pelagic tunicates—doliolids and pyrosomes—as well as to bottom-dwelling tunicates. Though they look like jellyfish due to their simple, planktonic form, they are actually chordates: animals with a dorsal nerve cord, related to vertebrates. Small fish sometimes swim inside salps for protection. The World Register of Marine Species lists the following classification for the order Salpida:

Order Salpida Family Salpidae Subfamily Cyclosalpinae Genus *Cyclosalpa*: *C. affinis*, *C. bakeri*, *C. foxtoni*, *C. ihlei*, *C. pinnata*, *C. polae*, *C. quadriluminis*, *C. sewelli*, *C. strongylenteron* Genus *Helicosalpa*: *H. komaii*, *H. virgula*, *H. younti*

Subfamily Salpinae Genus *Brooksia*: *B. berneri*, *B. rostrata* Genus *Ihlea*: *I. magalhanica*, *I. punctata*, *I. racovitzai* Genus *Metcalfina*: *M. hexagona* Genus *Pegea*: *P. bicaudata*, *P. confederata* Genus *Ritteriella*: *R. amboinensis*, *R. picteti*, *R. retracta* Genus *Salpa*: *S. aspera*, *S. fusiformis*, *S. gerlachei*, *S. maxima*, *S. thompsoni*, *S. tuberculata*, *S. younti* Genus *Soestia* (also accepted as *Iasis*): *S. cylindrica*, *S. zonaria* Genus *Thalia*: *T. cicar*, *T. democratica*, *T. longicauda*, *T. orientalis*, *T. rhinoceros*, *T. rhomboides*, *T.

field
Marine biology, planktonic tunicates
known_for
Efficient jet propulsion, rapid reproduction during phytoplankton blooms, role in ocean carbon cycle
distribution
Equatorial, temperate, and cold seas; most abundant in the Southern Ocean
size
Typically between 1 and 10 cm (0.4 and 3.9 in) long

Quick Facts

Taxon
Salpidae
Subdivision
See text

Facts from the source article.

Lore & Background

Salps are barrel-shaped, gelatinous tunicates that move by contracting their bodies to pump water through them, a method considered one of the most efficient forms of jet propulsion in the animal kingdom. They feed by straining phytoplankton through internal feeding filters. These animals are common in equatorial, temperate, and cold seas, appearing at the surface either singly or in long, stringy colonies. The highest concentrations are found in the Southern Ocean near Antarctica, where they sometimes form enormous swarms in deep water, occasionally outnumbering krill. Since 1910, salp populations in the Southern Ocean have increased while krill have declined, and they have also been seen in growing numbers off the coast of Washington, United States. Salps are closely related to other pelagic tunicates like Doliolida and Pyrosoma, as well as to bottom-dwelling tunicates. Despite resembling jellyfish, they are chordates with dorsal nerve cords, linking them to vertebrates. Small fish sometimes swim inside salps for protection. A notable historical event occurred in 1920 when a large incursion of *Salpa fusiformis* into the North Sea caused the failure of the Scottish herring fishery.

Reader's Guide

Salps are significant for their rapid response to phytoplankton blooms. When food is plentiful, they can bud off clones at a rate probably faster than any other multicellular animal, quickly stripping phytoplankton from the sea. Their blooms can cause beaches to become slimy with mats of salp bodies and lead to fluctuations in other planktonic species due to competition. Sinking fecal pellets and bodies of salps carry carbon to the seafloor, making them abundant enough to affect the ocean's biological pump. Large changes in their abundance or distribution may alter the ocean's carbon cycle and potentially play a role in climate change.

Did You Know?

Life as a Planktonic Drifter

Salps occupy a distinctive niche within the water column as metazoan zooplankton, a category often described as drifters. Unlike nektons—those powerful swimmers whose active propulsion lets them overcome the pull of currents—salps possess only limited motility. This means they remain suspended in the water column, largely at the mercy of surrounding water movements, drifting along with currents rather than swimming against them. They sit between the truly passive zooplankton, such as most aquatic larvae which have no motility at all, and the actively swimming nektons, representing an intermediate mode of aquatic locomotion. Their ecological positioning is purely environmental: they are grouped with other planktonic organisms not by shared ancestry but by the habitat they inhabit, making them part of a polyphyletic assemblage. Any morphological or behavioral resemblances they share with fellow drifters, such as jellyfish or larvaceans, are products of convergent evolution rather than close kinship. This drift-based existence shapes every aspect of their biology, from feeding strategies to reproductive dispersal.

Respiration and Aquatic Physiology

As a fully aquatic organism, a salp spends its entire existence immersed in a body of water, whether that is a saltwater ocean, a brackish estuary, or a freshwater system. Like the vast majority of animals that never leave the water, it relies on aquatic respiration to extract dissolved oxygen from its surroundings. This can occur through specialized gill structures, across the surface of the skin, or via the mucosal linings of the digestive tract. This stands in sharp contrast to secondarily aquatic creatures—marine mammals and reptiles that evolved from land ancestors and must surface to take a breath of air using lungs, effectively holding their breath during submersion. A salp has no such option. Remove it from the water for any extended period and it faces rapid death through dehydration or hypoxia, as its respiratory surfaces collapse or it suffocates under its own body weight. Its physiology is therefore entirely dependent on the chemical and physical properties of the water it inhabits, tying its survival to the health of its aquatic environment.

Reproduction and Life Cycle

Like nearly all aquatic animals, salps carry out their reproductive processes within the water itself, whether they release eggs into the current in an oviparous strategy or give birth to live young through viviparous reproduction. Their life cycle is tightly bound to the aquatic medium, and many species in the broader planktonic community pass through fully aquatic stages—typically as eggs and larvae—before any later developmental changes. Some aquatic organisms, such as certain amphibians and flying insects, eventually metamorphose into terrestrial or semi-aquatic adults, but planktonic drifters like salps remain suspended in the water column throughout their existence. Many aquatic species also undertake migrations between different water bodies at various points in their life cycle, a pattern that helps disperse populations and maintain genetic diversity. Because their reproductive success depends on water quality, temperature, and current patterns, any disruption to these environmental factors can directly impact their ability to reproduce and sustain populations across generations.

Ecological Role and Conservation Pressures

Salps, alongside aquatic plants, algae, and microbial communities, form essential links in the food webs of marine, brackish, and freshwater ecosystems. As members of the planktonic community, they serve as a vital trophic link, transferring energy between primary producers and larger predators. Their ecological importance extends beyond simple predation dynamics; they contribute to nutrient cycling and the overall productivity of the water bodies they inhabit. However, the very environments that sustain them are under mounting pressure. Aquatic animals face threats from overfishing and destructive harvesting practices, water pollution, ocean acidification, climate change, and competition from invasive species. Habitat destruction and fragmentation of aquatic ecosystems compound these risks. Conservationists pay particular attention to aquatic biodiversity because of the inherent fragility of these environments. The loss of species like salps would ripple through entire food webs, undermining the food, energy, and economic resources that aquatic ecosystems provide to the broader world.

Frequently Asked Questions

What is a salp?

A salp is a small, barrel-shaped marine tunicate that drifts through the open ocean as part of the plankton community. They typically measure between 1 and 10 centimeters in length and belong to the family Salpidae.

How do salps propel themselves?

Salps swim by rhythmically squeezing their gelatinous bodies, which forces water out in a jet-like burst. This contraction-based locomotion makes them one of the most energy-efficient jet-propulsion systems found in any animal.

What do salps feed on?

They filter-feed on phytoplankton by drawing water through their bodies and trapping microscopic algae with internal feeding structures. During phytoplankton blooms, salp populations can expand very rapidly.

Where can you find salps?

They occur in equatorial, temperate, and polar waters worldwide, but are particularly abundant in the Southern Ocean around Antarctica. There they sometimes aggregate into massive, string-like colonies or enormous swarms.

Why are salps ecologically important?

Salps play a significant role in the ocean carbon cycle by converting surface phytoplankton into dense fecal pellets that sink to deeper waters. Their rapid reproduction and large biomass make them a key link in transferring carbon from the sunlit surface to the deep sea.

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