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Pyrosome
Pyrosome
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Pyrosomatidae
Temporal range: Neogene–Present
Pyrosoma atlanticum
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Subphylum: Tunicata
Class: Thaliacea
Order: Pyrosomatida
Jones, 1848[1]
Family: Pyrosomatidae
Lahille, 1888
Genera[3]

Pyrosomes are free-floating colonial tunicates in family Pyrosomatidae. Pyrosomes consist of colonies of small zooids. There are three genera, Pyrosoma, Pyrosomella and Pyrostremma, and eight species.[4][5] They usually live in the upper layers of the open ocean in warm seas, although some may be found at greater depths.[5] Pyrosomes exhibit bioluminescence,[6] and the name Pyrosoma derives from the Greek words pyro, meaning "fire", and soma, meaning "body".[7] Pyrosomes are hermaphroditic and reproduce via a two-part process.[8] They have the ability to create massive blooms that may affect pelagic food webs.[9]

Description

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Pyrosomes are commonly called "sea pickles", due to their tube-like gelatinous structure. Other nicknames include "sea worms", "sea squirts", "fire bodies", and "cockroaches of the sea".[10]

Each zooid opens both to the inside and outside of the "tube". The zooids draw in ocean water from the outside into their internal filtering mesh called the branchial basket, extracting the microscopic plant cells on which it feeds, and then expelling the filtered water to the inside of the colony's cylinder.[11][10]

Pyrosomes are planktonic, which means their movements are largely controlled by currents, tides, and waves in the oceans. On a smaller scale, however, each colony can move itself slowly by the process of jet propulsion, created by the coordinated beating of cilia in the branchial baskets of all the zooids, which also create feeding currents.[12]

Pyrosomes are brightly bioluminescent, flashing a pale blue-green light that can be seen for many tens of metres. Pyrosomes are closely related to salps, and are sometimes called "fire salps". Sailors on the ocean occasionally observe calm seas containing many pyrosomes, all luminescing on a dark night.[11][10]

Pyrosomes feed through filtration and they are among the most efficient filter feeders of any zooplankton species. These colonial tunicates also are known to provide a source of shelter, food, and settlement from other deep sea organisms. They are also known to play a role in the marine Carbon cycle, as dead colonies sink to the sea floor to be consumed as food by other animals.[13]

Anatomy and morphology

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Drawing of a pyrosome. Clearly shows the individual zooids that appear as small bumps on the surface of the tubular structure.

A single individual of a pyrosome colony is referred to as an ascidiozooid, or zooid. A pyrosome colony contains many zooids which form a gelatinous tube, the walls of which range from 0.2 - 2.0 cm.[14]

The zooids that make up a pyrosome are typically only a few mm long. Colonies of these zooids, which are bound together by a notochord and shared tissue, form a tube-like, hollow structure that is typically between 1 inch and 2 feet in length. However, giant pyrosomes can reach up to 60 feet in length, with a hollow opening up to 6 feet (2 meters) wide.[15] There have been some instances in which deep sea scientists have swam inside of a giant pyrosome's hollow body.[16]

Pyrosomes are transparent and gelatinous, with a slimy yet bumpy texture.[17] Zooids appear as small bumps on the colony, although the colony appears nearly smooth with perforated holes for each zooid on the inside.[18] Each zooid has a stomach that can be seen through the transparent body of the colony. These stomachs have been compared to "wire baskets".[16]

Bioluminescence

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Although many planktonic organisms are bioluminescent, pyrosome bioluminescence is unique due to the nature and origins of its brilliant light emissions. Pyrosomes often exhibit waves of light passing back and forth through the colony, as each individual zooid detects light and then emits light in response.[6] These waves of bioluminescence are most likely a response to photic stimulation as opposed to nerve impulses, though zooids have also been observed emitting light in response to mechanical stimulation.[19] Pyrosomes may use bioluminescence to signal danger or otherwise communicate with individuals of the same or nearby colonies.[19]

Each zooid contains a pair of light organs located near the outside of the tunic, or the protective outer layer, whose cells are full of organelles containing intracellular, bioluminescent bacteria.[19] While an exact taxonomic identification of this bacteria has not been made, the morphology of the double-membrane enclosed organelle and the bacteria itself is similar to that of other extracellular bioluminescent bacterial symbionts as well as other intracellular bacterial symbionts.[19][20] These bacteria live within the host cells, which assumably control bacterial light emissions, a phenomenon rarely seen in other bioluminescent marine organisms.[19] Uncertainties about the overall control mechanisms and evolutionary relationship between Pyrosoma and their specialized symbionts constitute a research gap and are continuing to be studied.[19][20]

Reproduction

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Pyrosomes are hermaphroditic and have a two-part life cycle. In the first stage, a fertilized egg develops into a cyathozooid.[8] After this, the cyathazooid produces a tetrazooid, or four ascidizooids, via budding.[14] Colonies are able to self fertilize from one end of the tube to the other, as the closed end of the lobe is protandrous, meaning that male gametes are produced before female, while the open end is protogynous, with the female gametes maturing before the male.[21]

Food chain niche

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Pyrosomes are filter feeding tunicates that consume small particles like phytoplankton and detrital matter. That being said, their predator to prey mass ratio is very large at almost 50 million : 1.[5] Predator to prey mass ratio refers to the ratio between the mass of the predator organism vs. the mass of the prey organism. In this instance, the pyrosomes are generally 50 million times larger in mass than the prey they consume. Generally, pyrosomes graze a wide variety of microbes with most research surrounding larger eukaryotic phytoplankton but pyrosome feeding on smaller heterotrophic microbes is not well understood.[22]

Pyrosomes are essential members of the food chain on multiple fronts. Pyrosomes feed on large numbers of microbes, fall after death, vertically migrate while producing marine snow, and are prey for marine mammals, seabirds, turtles, or fish.[22] With these comes contribution to the marine carbon cycle. About 35% of the dry weight of Pyrosomes is carbon which is high for gelatinous organisms.[23] During their daily vertical migration of up to 900m or falls after death, Pyrosomes are prey to at least 62 pelagic organisms (like turtles and sea lions) and at least 33 benthic organisms (like sea urchins and crabs). Therefore, their role as contributors to the marine carbon cycle is likely very essential.[24]

Taxonomy

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Pyrosoma atlanticum by a tide pool in California

According to the World Register of Marine Species, the family is divided into two subfamilies and three genera, containing eight species.[3]

The three genera of pyrosomes, Pyrostremma, Pyrosomella, and Pyrosoma, have morphological similarities and differences. Most pyrosome colonies are finger-shaped, but there are two exceptions in the Pyrosoma genera; P. godeauxi and P. ovatum have a more globular appearance. Generally, pyrosomes have limp tests, or outer coverings. However, in some cases, Pyrosoma have tough, elastic tests. Each genera has test projections, those of Pyrostremma being triangular and spiny, Pyrosomella smooth, and Pyrosoma long and blunt.[21]

A colonial sphincter, or diaphragm, is present in Pyrosomella and Pyrosoma, but is absent in Pyrostremma. While Pyrostremma species have a slit-like arial sphincter, Pyrosoma and Pyrosomella have circular sphincters. The orientation of zooids differs between genera as well. In Pyrostremma, new zooids are added in a swirled pattern; Pyrosomella form zooids in parallel rows; Pyrosoma add zooids in a dense, random arrangement.[21] Pyrosomes can also develop into some of the longest animals in the ocean.[5] For example, the Pyrostremma spinosum, can fully extend up to 3 meters and grow up to 20 meters in length. [citation needed]

In regards to the three genera of pyrosomes, the cellular components of their tunic have been documented.[25] Multiple different cellular types have been found to be distributed in the tunic of Pyrosome atlanticum, Pyrosomella verticillata, and Pyrostremma spinosum. These cell types include Tunic amebocytes, which are found to be motile and shaped asymmetrically. They are also found to either contain granules or phagosomes within them. Another cell type is known as Spherical Tunic cells, in which contain spherical vesicle that often contain eosinophilic and acidic substances. Net cells form a net in which the cell's elongated filopodia connect with each other, forming a network. This network maintains a tension in order to reinforce the colony shape and support the cell's cloacal cavity. Multicellular cords also exist between the tunic cells and the zooids, and are known as test fibers. They are hypothesized to maintain and control muscle contractions of the zooids.

Geographic Distribution

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Pyrosomes are globally distributed organisms, with recorded sightings in every ocean, with the exception of the Arctic Ocean, and are typically latitudinally confined within 50°N and 50°S.[21][26] However, some pyrosome species have been shown to expand their geographic range in response to increasing ocean temperatures, which has unknown implications for the already existing ecosystems.[26] Additionally, there is some evidence pointing towards geographic distribution changes of pyrosome colonies in relation to changes in the season.[9]

In relation to vertical distribution and diel vertical migration, pyrosomes have been shown to travel between 20 meters to greater than 700 meters in the water column.[5] Although most pyrosome sightings occur relatively near the surface at night, there is still wide intraspecies variation in migration distance, ranging from travel distances of 20 meters to more than 500 meters per day.[5][9]

Blooms

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Pyrosomes have the ability to create enormous blooms, which are rapid and substantial increases in population. Some scientists hypothesize that the presence of a food fall can contribute to these blooms.[27] Since pyrosomes are food-limited organisms, they may take advantage of these circumstances to increase reproduction.[27]

Past evidence suggests that sustained, multi-year blooms are not environmentally favorable, but blooms may become increasingly prevalent as warming water temperatures globally can provide favorable conditions for recurring pyrosome blooms.[28] In 2017, pyrosomes were observed to have spread in unprecedented numbers along the Pacific coast of North America as far north as Alaska. The causes remain unknown, but one hypothesis is that this bloom may have resulted in part from unusually warm water along the coast over several preceding years. Also, weak upwelling off the coast of northern California creates an ideal environment for blooms.[9] Scientists were concerned that should there be a massive die-off of the pyrosomes, it could create a huge dead zone as the decomposition of their bodies could consume much of the oxygen dissolved in the surrounding seawater.[29][30][31]

Scientists have observed that large blooms can hurt pelagic food webs, for an increased population leads to increased grazing pressure, ultimately affecting the transfer of energy in these environments.[9] Through this excessive phytoplankton grazing, the amount of food available for other organisms to feed on decreases. However, pyrosomes contain a lot of energy and have been reported being consumed by pelagic fish and cetaceans; there have also been jelly-falls containing pyrosomes, suggesting that these organisms can provide carbon for benthic organisms to consume.[9]

References

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Bibliography

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Pyrosomes are gelatinous, free-floating colonial belonging to the order Pyrosomida in the class and phylum Chordata, forming hollow, tube-shaped colonies composed of thousands of genetically identical zooids embedded in a shared . These pelagic organisms are that drift passively with ocean currents, primarily consuming particles ranging from 3 to 150 μm in size. Named after words pyro () and soma (body) due to their ability to emit a faint blue bioluminescent glow, pyrosomes are distributed globally in tropical to temperate waters between approximately 50°N and 50°S latitudes. Pyrosomes exhibit a complex life cycle characterized by hermaphroditism and via . Colonies vary greatly in size depending on the ; for instance, typically measures 6–600 mm in length, while Pyrostremma spinosum can exceed 20 m. They inhabit depths from the surface to at least 750 m, with some records suggesting occurrences as deep as 5,000 m, and prefer water temperatures between 12°C and 29°C. Their gelatinous structure, rich in carbon, contributes significantly to vertical carbon flux in the , with blooms exporting 10–1,000 mg C m⁻² d⁻¹ to deeper waters. Ecologically, pyrosomes play a pivotal role in marine food webs as both grazers and prey; during blooms, they can remove 53–95% of available , potentially reshaping microbial communities and nutrient cycling. They serve as food for at least 62 species of and three species of sea turtles, though their low nutritional value limits their appeal to some predators. Massive blooms, which can clog nets and coastal intakes, have been documented worldwide, with recent range expansions into temperate regions like the Northeast Pacific attributed to warming ocean conditions. Their , triggered mechanically or by light, produces coordinated waves of light across the colony, aiding in startling predators or attracting prey in the open ocean.

Overview and Classification

Description

Pyrosomes are pelagic, free-floating colonial belonging to the class and order Pyrosomatida, forming hollow, gelatinous tube-shaped colonies that can reach lengths of up to 20 meters. These organisms consist of numerous genetically identical zooids embedded in a shared , creating a cohesive structure that drifts in open ocean waters. The name "pyrosome" derives from the Greek words pyros (fire) and sōma (body), reflecting their striking bioluminescent glow, which produces a faint blue light when disturbed. As filter-feeding zooplankton, pyrosomes consume microscopic plankton by pumping water through their colony, playing a key role in marine ecosystems via bioluminescence for predator deterrence and nutrient cycling through the deposition of organic matter to the seafloor. Their colonial architecture also enables coordinated jet propulsion for slow, directed movement. Pyrosomes were first scientifically described in the early , with the Pyrosoma established by French naturalist François Péron in 1804 based on specimens from southern oceans. Subsequent observations by 19th-century zoologists expanded knowledge of their morphology and distribution, highlighting their enigmatic presence in pelagic environments.

Taxonomy

Pyrosomes are classified within the phylum Chordata, subphylum Tunicata, class Thaliacea, order Pyrosomatida, and family Pyrosomatidae. This placement positions them as pelagic colonial tunicates closely related to other thaliaceans, such as salps and doliolids. The family Pyrosomatidae includes three genera: Pyrosoma, Pyrosomella, and Pyrostremma, with a total of eight accepted species worldwide. The genus Pyrosoma is the most prominent, encompassing species such as Pyrosoma atlanticum Péron, 1804, and Pyrostremma spinosum Herdman, 1888, which are distributed across temperate and tropical oceans. Other genera include Pyrosomella verticillata (Neumann, 1909) and Pyrostremma agassizi Ritter & Byxbee, 1905. As derived , pyrosomes exhibit salp-like traits, including colonial organization and , and represent a lineage that diverged from solitary ascidian ancestors within the . Molecular phylogenies confirm as monophyletic, with pyrosomes branching basally among thaliacean orders. Their record is extremely limited due to the soft-bodied nature of , with no direct pyrosome s known and the earliest traces appearing in the early . Recent molecular phylogenetic studies, including analyses of mitochondrial and nuclear genes, have refined thaliacean relationships and supported the division of Pyrosomatidae into subfamilies like Pyrosomatinae and Pyrostremmatinae, aiding in the resolution of cryptic diversity through approaches such as . These revisions underscore the family's bioluminescent traits as a shared apomorphy.

Morphology and Physiology

Anatomy and Morphology

Pyrosomes are colonial that form gelatinous, cylindrical tubes composed of thousands of genetically identical zooids embedded within a shared outer , or test, constructed primarily from tunicin, a cellulose-like unique to . This communal structure allows the colony to function as a single, cohesive unit, with zooids arranged in species-specific patterns: densely packed and seemingly random in Pyrosoma, parallel rows in Pyrosomella, and whorl-like configurations in Pyrostremma. The provides structural support while remaining flexible due to its high , typically exceeding 95% in composition. Each individual within the is bilaterally symmetric and exhibits a barrel-shaped body, featuring an incurrent at the anterior end for drawing in water and an excurrent at the posterior end for expelling filtered water and waste. Inside, a prominent branchial basket, lined with numerous gill slits (), serves as the primary filter-feeding apparatus, where a net secreted by cells traps , , and other particulates from the incoming water current generated by ciliary action. Zooids also possess longitudinal and circular muscles that enable contractions to propel water through the siphons, contributing to both feeding and the colony's overall movement via synchronized activity. Colony sizes vary widely across species and environmental conditions, ranging from a few centimeters in smaller forms like Pyrosoma atlanticum (typically 6–600 mm in length) to over 18 meters in giants such as Pyrostremma spinosum. Shapes are predominantly elongated tubes, though some genera exhibit slight variations, such as tapered or cone-like forms, while maintaining the hollow, open-ended cylindrical morphology that facilitates water flow through the entire colony. Morphological adaptations enhance survival in the open ocean; the colony's high transparency, resulting from the watery gelatinous matrix and minimal pigmentation, provides effective against predators by blending with surrounding water. Additionally, the relatively rigid maintains the colony's structural integrity, aiding through its low , which helps keep the colony neutrally buoyant in the . These features support synchronized muscular contractions that enable jet-like propulsion for locomotion.

Bioluminescence

Pyrosomes generate through an oxidative reaction involving the substrate coelenterazine as and a specialized known as PyroLuc as , occurring within photocytes—light-producing cells clustered in circular light organs underlying the incurrent of each . This biochemical process yields blue-green with peak emission wavelengths of 475–493 nm, optimized for transmission in oceanic waters. The reaction is catalyzed in the presence of oxygen, producing without generating significant heat, and is encoded by a chordate-specific that has evolved convergently from dehalogenase ancestors across multiple phyla. Triggers for include mechanical disturbance, chemical signals, electrical stimuli, and photic exposure, which initiate a coordinated display where individual zooids sequentially activate, creating rippling waves of that propagate along the at speeds of 2.1–4.1 mm/s. This synchronized flashing contrasts with the brief pulses typical of many planktonic organisms, instead producing sustained illumination that can persist for minutes. The transparency of the pyrosome's further facilitates even of this throughout the structure. Evolutionary advantages of pyrosome encompass predator deterrence through a "burglar " mechanism, where the conspicuous glow attracts secondary predators to interrupt attacks on the colony, as well as potential to blend with light for in dimly lit depths. Additionally, the light facilitates intraspecific communication among zooids, enabling coordinated responses unique to this colonial organism. Intensity varies by species, with displaying particularly brilliant and sustained emissions visible up to 100 m in clear water. Recent post-2020 studies have advanced understanding of the genetic basis of these photoproteins, including evidence of intracellular bacterial symbionts like Photobacterium contributing to the light organs, though the primary mechanism remains tied to host-encoded enzymes.

Locomotion

Pyrosomes achieve locomotion primarily through , a process driven by the coordinated contractions of muscles within individual that line the colony's tubular structure. Each zooid draws in through its oral , filters it for particles, and expels the water into the colony's central cavity; this expelled water then exits collectively through the posterior excurrent opening, generating continuous thrust directed backward. This mechanism distinguishes pyrosomes as the only known animals employing truly continuous , rather than pulsatile bursts, enabling steady forward movement suited to their pelagic lifestyle. Coordination among zooids occurs via their embedding in a shared gelatinous , which facilitates synchronous pumping actions that propagate as wave-like along the colony's length. This allows for fine-tuned directional control and orientation, with zooids arranged in whorl-like or linear patterns depending on the , enhancing overall maneuverability without a centralized . Swimming speeds typically range from 3 to 7 cm/s, often augmented by passive drift due to the provided by the low-density gelatinous , which traps water and minimizes sinking. Behavioral observations from field studies in the , including acoustic profiling and net tows in regions like the and Eastern Atlantic, reveal that pyrosomes undertake pronounced diel vertical migrations tied to light cycles. Colonies typically ascend to the upper 75 m of the at night for feeding and descend to 100–500 m during the day, covering vertical distances up to 760 m; these movements are likely regulated by phototaxis and support their role in carbon transport. The jet propulsion system integrates with filter-feeding, as the same water currents used for movement capture microbial prey across the .

Reproduction and Development

Reproduction

Pyrosomes exhibit a complex reproductive strategy involving both asexual and sexual phases, enabling rapid formation and propagation. are composed of hermaphroditic blastozooids, which reproduce sexually through within the , where eggs in the atrial cavity are fertilized by from other zooids, often enabling self-fertilization due to protandry at the older (closed) end and protogyny at the younger (open) end. The resulting develops into a short-lived oozooid, also known as a cyathozooid, within a brood pouch of the parent blastozooid. This oozooid then initiates through budding, producing an initial quartet of blastozooids that form the foundational tetrazooid stage of a new ; the oozooid subsequently degenerates. Colony expansion occurs primarily via ongoing , as blastozooids continue to bud new zooids from a basal , allowing for and the development of elongated, tubular structures that can reach several meters in length. This two-part life cycle—sexual production of the founder oozooid followed by asexual proliferation of blastozooids—lacks the strict alternation of solitary and colonial generations seen in other thaliaceans like salps, but supports the formation of dense blooms under favorable conditions. Reproductive success in pyrosomes is strongly influenced by environmental factors, particularly and availability, as documented in laboratory experiments and field observations from the and . Optimal reproduction and growth occur in waters with temperatures below 18°C and high , indicated by elevated chlorophyll-a concentrations, which provide the necessary nutritional resources for production and . Warmer temperatures associated with marine heatwaves have been linked to range expansions and increased bloom frequencies, though extreme heat may limit development; conversely, abundant supplies enhance and rates, driving population surges in productive regions.

Development

Pyrosome development commences with sexual fertilization, where eggs within the atrial cavity of a blastozooid are fertilized by sperm from another in the . The fertilized undergoes ovoviviparous development inside the blastozooid, directly forming the oozooid (cyathozooid) without a free-swimming larval stage, unlike many other . This oozooid serves as the founder for colony formation through subsequent stolon-based asexual budding. Colony growth proceeds in phases marked by exponential addition of zooids at the posterior end, with the rate influenced by , abundance, and conditions; mature colonies, capable of , can be achieved in several weeks to months under favorable oceanic environments.

Distribution and Ecology

Geographic Distribution

Pyrosomes inhabit tropical and subtropical waters across all major ocean basins, from the Atlantic and Pacific to the , typically occurring from the surface down to depths of 100–500 m during the day and the upper 75 m at night, though records extend to over 700 m and up to nearly 5000 m in some databases during daytime migrations. Highest densities are associated with warm oceanic currents, such as those in the region of the western North Atlantic, where favorable conditions support their pelagic lifestyle. Their latitudinal distribution is generally confined between approximately 40°N and 40°S, with occurrences becoming rare poleward of these limits due to cooler temperatures, though vagrant individuals have been documented in temperate zones up to 50°N and 50°S. This zonation is influenced by environmental factors, including surface temperatures of 15–30°C and salinities of 30–35 ppt, which align with the oligotrophic conditions of open ocean gyres and convergent zones. Species-level distributions show regional preferences; for instance, , the most cosmopolitan species, predominates in the Atlantic Ocean but extends to the , while Pyrostremma spinosum is more characteristic of the Indo-Pacific tropical waters. These patterns reflect adaptations to specific hydrographic regimes, with P. atlanticum tolerating a broader range of 10–22°C compared to the warmer preferences of Indo-Pacific congeners. In the , platforms and integrated satellite-database analyses have revealed evidence of range expansions, particularly northward in the northeast Pacific, linked to climate-driven ocean warming and marine heatwaves that have shifted thermal boundaries. For example, unprecedented abundances of P. atlanticum have been recorded off the U.S. West Coast since 2015, extending into waters previously considered marginal for the . These observations, corroborated by oceanographic models, suggest ongoing poleward shifts in response to rising sea temperatures.

Blooms

Pyrosome blooms refer to dense aggregations of colonies, often exceeding 100 individuals per cubic meter in extreme cases, which can form extensive visible surface slicks stretching kilometers in length. These events arise from rapid population increases, where colonies cluster in high densities, sometimes reaching over 3,800 individuals per cubic meter during peak outbreaks. Such aggregations are transient but can dominate local pelagic communities, altering dynamics through their collective filter-feeding activity. These blooms are triggered by favorable oceanographic conditions, including nutrient-rich , marine heatwaves, and El Niño events that enhance primary productivity while reducing predation pressure from and other predators. The exponential growth is facilitated by through , allowing a single colony to rapidly produce chains of new individuals under optimal temperatures above 12°C and abundant . Notable pyrosome blooms occurred in the from 2017 to 2019, following the 2014–2016 , with peak densities clogging fishing nets and disrupting commercial fisheries by damaging gear and reducing catch efficiency. In the region, outbreaks were documented in 2024 near Timor-Leste, where seasonal drove dense aggregations, detected through environmental DNA (eDNA) sampling that confirmed high pyrosome presence amid ecosystems. Monitoring pyrosome blooms involves a combination of via to detect surface slicks, diver and surveys for direct of colony densities, and predictive modeling that integrates circulation data with projections to forecast bloom risks under warming scenarios. These methods enable early detection, with models indicating that intensified heatwaves could increase bloom frequency by up to 100% in eastern boundary currents by mid-century.

Ecological Role

Pyrosomes function as primary consumers in marine ecosystems, primarily through filter-feeding on , , and at a low . Each can process substantial volumes of , with clearance rates reaching up to 5.5 liters per hour for a typical 55 mm , enabling efficient grazing that clears from the . This feeding activity contributes to carbon export to the by packaging consumed material into dense fecal pellets that sink rapidly, facilitating the and transferring organic carbon below the euphotic zone. As prey, pyrosomes occupy an intermediate position in pelagic food webs, serving as a food source for higher trophic levels including various species, sea turtles, seabirds, and marine mammals such as sea lions. Their bioluminescence, while primarily a defensive or communicative trait, can inadvertently attract predators in low-light conditions, enhancing their visibility to visual hunters. Through these interactions, pyrosomes transfer energy upward, though their gelatinous composition provides lower nutritional value compared to zooplankton, potentially limiting transfer efficiency to top predators. Pyrosomes provide key ecosystem services, including vertical nutrient transport via diel migrations and the production of fast-sinking fecal pellets that redistribute , carbon, and biogenic silica to deeper waters. Their also indirectly supports oxygen production by controlling densities, preventing excessive blooms that could deplete oxygen, while their silica-containing fecal pellets contribute to remineralization cycles in the ocean's interior. During blooms, pyrosomes can significantly perturb local food webs by dominating biomass, comprising up to 90% in affected regions like the Current during the 2010s marine heatwaves, thereby reducing availability of more nutritious prey for and altering . Studies from the 2020s highlight how such events redirect carbon pathways and diminish overall zooplankton diversity, with pyrosomes contributing 10-50% of total in bloom hotspots and influencing higher trophic dynamics for years post-event.

References

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