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Aulopiformes
Aulopiformes
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Aulopiformes
Temporal range: 125–0 Ma Early Cretaceous to present[1]
Variegated lizardfish, Synodus variegatus
(Synodontoidei: Synodontidae)
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Actinopterygii
Clade: Eurypterygii
Superorder: Cyclosquamata
Order: Aulopiformes
D. E. Rosen, 1973
Type genus
Aulopus
Cloquet, 1816
Suborders
Synonyms

Macristiidae (see text)

Aulopiformes /ˈɔːləpɪfɔːrmz/[a] is a diverse order of marine ray-finned fish consisting of some 15 extant and several prehistoric families with about 45 genera and over 230 species. The common names grinners, lizardfishes and allies, or aulopiforms are sometimes used for this group. They are included in the superorder Cyclosquamata,[b] though modern taxonomists consider this superorder to be unwarranted.

Many extant aulopiforms are deep-sea fishes, with some species recognized as being hermaphroditic, a number of which are able to self-fertilise. Some are benthic, but most are pelagic swimmers (nektonic).[6][7] A clade of Aulopiformes, the suborder Enchodontoidei and its many constituent families, were dominant nektonic fish throughout much of the Late Cretaceous before the extinction of most of their members around the K–Pg event,[1][8] with the Dercetidae surviving for some time in the Cenozoic.[9][10]

Taxonomy

[edit]

Past authors have considered aulopiforms to be so distinct as to warrant separation in a monotypic superorder of the Teleostei, the Cyclosquamata. However, monotypic taxa are generally avoided by modern taxonomists if not necessary, and in this case a distinct superorder seems indeed unwarranted: together with the equally dubious superorder "Stenopterygii", the grinners appear to be closely related to some of the Protacanthopterygii, namely, the Salmoniformes (salmon, trout, and relatives), and should perhaps be part of that larger clade. As an alternative, the superorders are sometimes united as an unranked clade named Euteleostei, but in that case the Protacanthopterygii would need to be split further to account for the phylogenetic uncertainty. This would result in a highly cumbersome and taxonomically redundant group of two very small and no less than four monotypic superorders.[6][11]

Description

[edit]
A shortnose greeneye, Chlorophthalmus agassizi
(Chlorophthalmoidei: Chlorophthalmidae)

In general, aulopiform fish have a mixture of advanced and primitive characteristics relative to other teleost fish. Aulopiformes are grouped together (claded) because of common features in the structure of their gill arches; their second pharyngobranchial bone (part of the gill arch) is greatly elongated posterolaterally away from third pharyngobranchial, which lacks a cartilaginous condyle to articulate with the preceding bone, but is contacted by the elongated uncinate process of the second epibranchial. Aulopiforms have a gas bladder which is either vestigial or entirely absent, a hypaxialis muscle that is unusually extended forward at its upper end, attaching to the neurocranium below the spine (perhaps to snap the upper part of the skull down when catching prey), and the position of the maxillary bone. Other features include the position of the pelvic fins far back on the body, the fused medial processes of pelvic girdle, and the presence of an adipose fin (which is also typical for the Protacanthopterygii).[4][6][7]

The larvae of some Aulopiformes are extremely bizarre-looking, with elongated fins, and do not resemble the adult animals. They were not only described as distinct species, but also even separated as genera and finally in a family "Macristiidae" which was allied with various Protacanthopterygii (sensu lato), but the initial assessment – which found "Macristium" to resemble the deepwater lizardfishes (Bathysauridae) in some details – was in fact not far off the mark: "Macristium" species are now known to be the larvae of Bathysaurus, while the supposed other "macristiids" "Macristiella spp." are larvae of the deepsea tripodfish Bathytyphlops.[12]

Several extant aulopiform families have Cretaceous representatives, and phylogenetic evidence indicates that the extant families of the order diversified around the Early Cretaceous, making it rather ancient. These diversification events included the earliest adaptations for deep-sea living, which is common among many extant aulopiform taxa.[1] Below is a timeline indicating fossil evidence for the group:

QuaternaryNeogenePaleogeneCretaceousHolocenePleistocenePlioceneMioceneOligoceneEocenePaleoceneLate CretaceousEarly CretaceousNotolepisScopelarchusScopelosaurusChlorophthalmusAulopusLabrophagusAulopopsisAcrognathusNematonotusQuaternaryNeogenePaleogeneCretaceousHolocenePleistocenePlioceneMioceneOligoceneEocenePaleoceneLate CretaceousEarly Cretaceous

Classification

[edit]
Lestrolepis japonica
(Alepisauroidei: Paralepididae)
Tripodfish; Bathypterois sp.
(Chlorophthalmoidei: Ipnopidae)
Enchodus petrosus, reconstruction
(Enchodontoidei: Enchodontidae)
Highfin lizardfish; Bathysaurus mollis
(Giganturoidei: Bathysauridae)

means extinct.

Footnotes

[edit]

References

[edit]

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Aulopiformes is an order of diverse, primarily marine ray-finned fishes, commonly known as lizardfishes and their allies, comprising approximately 16 families, 51 genera, and 280 species as of November 2025. These fishes are predominantly predatory and inhabit a broad spectrum of oceanic environments, from shallow coastal bottoms to abyssal depths, with many exhibiting specialized adaptations for pelagic or benthic lifestyles. The order is distinguished by unique osteological features in the gill arches, including an elongate uncinate process on the second epibranchial that bridges the second and third pharyngobranchials. Phylogenetically, Aulopiformes form a monophyletic group within the Neoteleostei, positioned as the to the Myctophiformes (lanternfishes), with a fossil record dating back to the . The order is divided into four main clades or suborders—Synodontoidei, Chlorophthalmoidei, Alepisauroidei, and Giganturoidei—reflecting evolutionary divergences in morphology and ecology, such as the absence of a in most taxa and the presence of epipleural bones extending anteriorly. Body sizes vary widely, from small lizardfishes around 10 cm to larger forms exceeding 1 m, with shapes ranging from slender and elongate to more robust in shallow-water species. Notable among Aulopiformes are deep-sea families like Giganturidae (telescopefishes) and Scopelarchidae, which possess tubular or highly modified eyes for low-light conditions, and some exhibit simultaneous hermaphroditism as a reproductive strategy suited to sparse populations. While most are confined to marine habitats worldwide, a few occur in brackish waters, and the group plays ecological roles as mid-level predators in food webs across all major basins. Ongoing taxonomic revisions, such as those in Eschmeyer's Catalog of Fishes, continue to refine counts and familial boundaries based on morphological and molecular .

Systematics and Taxonomy

Historical Perspectives

The taxonomic history of Aulopiformes began in the with the initial recognition of its constituent families as a distinct group of fishes, primarily through the work of ichthyologist Theodore N. Gill. In his 1893 , Gill established the suborder Myctophoidei to encompass families such as Myctophidae, Neoscopelidae, and Aulopidae, while also defining the suborder Synodonti for and Chlorophthalmidae, thereby grouping these taxa based on shared morphological traits like their elongate bodies and predatory adaptations, and placing them near the lanternfishes (Myctophiformes). This early framework highlighted the affinities among these deep-sea and benthic forms but did not yet formalize them as a unified order. By the mid-20th century, advancements in comparative anatomy led to the placement of Aulopiformes within the superorder Cyclosquamata, as proposed by Lev S. Berg in 1940. Berg's classification emphasized shared characteristics such as cycloid scales and the presence of an adipose fin, allying Aulopiformes with other cycloid-scaled teleosts like Myctophiformes and Salmoniformes to reflect their evolutionary convergence in open-water and deep-sea environments. This superordinal grouping persisted in subsequent schemes, providing a broader context for understanding aulopiform diversity amid the era's focus on scale morphology and fin structures as phylogenetic markers. A pivotal refinement occurred in 1966 with the seminal work of Greenwood et al., who, in their provisional of living teleostean fishes, elevated Aulopiformes to ordinal status within Cyclosquamata and introduced early subordinal divisions. They delineated the suborder Synodontoidei (including and Aulopidae) and Chlorophthalmoidei (encompassing Chlorophthalmidae and Bathysauridae), based on differences in jaw mechanics, eye structure, and body elongation, thereby establishing a more structured framework that integrated fossil and extant forms from the "Fishes of the World" tradition. Further evidence for the of Aulopiformes emerged from Rosen and Patterson's 1969 study on gill arch morphology, which identified unique synapomorphies in the upper pharyngeal elements, such as the modified second pharyngobranchial and uncinate process, distinguishing aulopiforms from neighboring groups like Myctophiformes. This anatomical analysis solidified Aulopiformes as a cohesive order by demonstrating shared derived traits in their suspensorium and branchial skeleton, influencing late-20th-century classifications up to the 1990s.

Current Classification

Aulopiformes comprises approximately 16 extant families, around 50 genera, and over 300 species of primarily marine ray-finned fishes, with recent catalogs as of November 2025 listing about 300 valid species. The order is divided into several suborders, including the extant Alepisauroidei (encompassing families like Alepisauridae, known for lancetfishes), Giganturoidei (including Bathysauridae and Giganturidae), and Synodontoidei (such as and Chlorophthalmidae), alongside the extinct suborder Enchodontoidei. These suborders reflect morphological and ecological groupings, with Alepisauroidei representing the most species-rich radiation at around 173 species. The family-level taxonomy includes a mix of benthic, pelagic, and bathypelagic groups, with species counts varying widely. For instance, (lizardfishes) contains about 81 species across genera like Synodus and Saurida, primarily in shallow coastal waters. Paralepididae (barracudinas) is another diverse family with roughly 72 species in genera such as Paralepis and Lestidium. Smaller families like Aulopidae (flagfins) have around 16 species in four genera, including Aulopus. The following table summarizes key families with approximate extant species counts based on recent catalogs as of November 2025:
FamilyCommon NameApproximate Species CountRepresentative Genera
Lizardfishes81Synodus, Saurida
ParalepididaeBarracudinas72Paralepis, Stemonosudis
AlepisauridaeLancetfishes2Alepisaurus
ChlorophthalmidaeGreeneyes22Chlorophthalmus
EvermannellidaeSabertooth fishes8Evermannella, Coccorella
ScopelarchidaePearleyes18Scopelarchus, Benthalbella
AulopidaeFlagfins16Aulopus, Procerauropsis
GiganturidaeWhalefishes2Gigantura
BathysauridaeDeep-sea lizardfishes2Bathysaurus
Others (e.g., , Omosudidae)Various deep-sea forms<10 eachIpnops, Omosudis
Recent additions have incrementally increased diversity, including Synodus autumnus, a new lizardfish species described in 2025 from the , distinguished by unique scale and pigmentation patterns, contributing to ongoing updates in Eschmeyer's Catalog with 325 new fish species described globally in 2025. In Aulopidae, the genus was established with two new species from Australasian waters, contributing to refined understanding of regional . Taxonomic revisions continue to refine relationships, such as reassessments of distributional records within that clarify overlaps between species like S. autumnus and S. rubromarmoratus. Earlier morphological studies on aulopiform interrelationships have supported the stability of core family assignments, though ongoing molecular data may prompt further adjustments.

Phylogenetic Position

Aulopiformes occupy a basal position within the Euteleostei, specifically as the to Ctenosquamata (encompassing Myctophiformes and ) in the Eurypterygii, based on a combined morphological and molecular phylogeny that analyzed 258 morphological characters and eight molecular loci across 78 euteleost taxa. This placement positions Aulopiformes as a foundational lineage in the radiation of advanced teleosts, with Ateleopodiformes serving as the to the entire Eurypterygii. Although earlier morphological studies suggested potential affinities to Protacanthopterygii or due to shared primitive euteleost features, the total evidence analysis rejects direct sister-group relationships, instead emphasizing Aulopiformes' distinctiveness within Eurypterygii. Molecular phylogenies reinforce Aulopiformes as a within Neoteleostei, nested in the infracohort Eurypterygia and section Cyclosquamata, derived from genomic-scale analyses of nearly 2,000 fish species using nuclear and mitochondrial markers. Subsequent updates, including phylogenomic studies with ultraconserved elements, uphold this basal neoteleost position, confirming high nodal support (100%) for Aulopiformes' monophyly and its placement adjacent to myctophiforms and acanthomorphs. These molecular frameworks align closely with morphological evidence, resolving Aulopiformes as a key early-diverging lineage in the euteleost tree, predating the diversification of percomorphs. Defining synapomorphies of Aulopiformes include modifications to the gill arches, such as an enlarged uncinate process on the second epibranchial that bridges the second and third pharyngobranchials, and the absence of a cartilaginous condyle on the third pharyngobranchial for epibranchial articulation, reflecting elongated and restructured arch morphology. The order is further characterized by the complete reduction or absence of the gas bladder, a derived loss that distinguishes it from outgroups like stomiiforms, and unique caudal fin support involving anterior extensions of epipleural ribs to at least the second vertebra, enhancing structural reinforcement. Uncertainties persist regarding the monophyly of certain aulopiform families, notably Chlorophthalmidae, which appears paraphyletic in total evidence phylogenies due to nested positions of genera like Parasudis outside core chlorophthalmids, and non-monophyletic in molecular trees based on sequence divergences. Ongoing cladistic analyses, incorporating expanded morphological datasets and phylogenomic markers, continue to refine these relationships, with debates centering on homoplasy in gill arch and maxillary characters that challenge family boundaries.

Morphology and Anatomy

Adult Characteristics

Adult Aulopiformes exhibit a diverse array of body forms adapted to marine environments, ranging from small to large sizes. Many species possess elongated, tubular bodies that are subcylindrical anteriorly and moderately compressed posteriorly, such as in lizardfishes (), which can reach up to 60 cm in length. Scales are typically or spinoid, often and absent from the top of the head, with examples including the moderately large, non- scales in Synodus autumnus. Body sizes vary widely, from around 32 cm maximum length in Bathysauropsis (Bathysauropsidae) to over 2 m in Alepisaurus (Alepisauridae), reflecting adaptations to different depths and habitats. The order is distinguished by unique osteological features in the gill arches, including an elongate uncinate process on the second epibranchial that bridges the second and third pharyngobranchials. The fins and skeletal structure of adult Aulopiformes are characterized by the absence of fin spines and a posterior positioning of the , often inserted over or behind the pelvic fins, which are abdominal or thoracic in placement. For instance, in Aulopidae, the has 14-22 rays, the anal fin 8-14 rays, and the pelvic fins 9 rays, with a total vertebral count of 36-53. The gas is vestigial or entirely absent in many deep-sea forms, an adaptation that supports without reliance on gas regulation in high-pressure environments. Sensory adaptations in adult Aulopiformes are pronounced, particularly in deep-sea species, with large, often tubular eyes positioned laterally or dorsally to enhance light detection in low-illumination conditions; for example, Chlorophthalmus (Chlorophthalmidae) has round eyes with a teardrop and a brilliant green tapetum. Bioluminescent organs occur in some families, such as internal luminescent structures in Chlorophthalmus and Scopelarchidae, aiding in or prey attraction. Lath-like gill rakers are present in families like Aulopidae and Chlorophthalmidae, aiding in the capture of small prey during carnivorous feeding. Hermaphroditism is common in several Aulopiformes families, with synchronous (simultaneous) hermaphroditism reported in Chlorophthalmidae, , Scopelarchidae, and Notosudidae, where individuals possess both ovarian and testicular tissues in functional gonads. In contrast, Aulopidae exhibit with separate sexes. This reproductive strategy is linked to deep-sea lifestyles, potentially enhancing mating opportunities in sparse populations.

Larval and Developmental Features

The larvae of certain Aulopiformes, particularly in the family Bathysauridae, display highly specialized, leptocephalus-like forms characterized by leaf-shaped, laterally compressed bodies and exceptionally high myomere counts exceeding 100, features that initially led to their classification as a distinct family, Macristiidae. These elongated, transparent larvae differ markedly from the adults, reflecting adaptations for a prolonged pelagic phase in deep-sea environments. Early developmental stages feature small, transparent preflexion larvae with prominent yolk sacs for initial , often accompanied by peritoneal pigment patches that increase in number as growth proceeds. marks a dramatic transformation, with rapid body elongation, posterior migration of the , and development of and paired fins occurring between approximately 20 and 50 mm standard length, though some species like Bathysaurus exhibit extended larval durations up to 127 mm. Family-specific larval traits enhance predatory efficiency and dispersal; for instance, larvae possess disproportionately large mouths suited for ambush predation on small planktonic prey, mirroring adult behaviors but in a more buoyant form. In contrast, Alepisauridae larvae exhibit pronounced elongation of the posterior body and tail, facilitating enhanced swimming in open oceanic waters. Historical misclassifications arose from the enigmatic morphology of these larvae; in the , studies by Okiyama linked specimens of Bathysaurus and the related Bathytyphlops to Aulopiformes through comparative analysis of head spines, fin development, and myomere patterns, resolving their placement within the order.

Ecology and Biology

Habitat and Distribution

Aulopiformes exhibit a broad geographic distribution across to temperate oceans worldwide, occupying four of the five major pelagic realms and 27 of the 30 benthic or coastal realms. Their highest occurs in the region, where numerous genera and families, including and Aulopidae, are concentrated, reflecting the area's rich marine . For instance, species of the genus Synodus (lizardfishes) are recorded from shallow coastal waters to depths of up to 1000 m across and Atlantic regions. Members of the order inhabit diverse types, primarily benthic, nektonic, and deep-sea environments. Benthic species, such as lizardfishes in the family , typically rest on sandy or muddy sediments in coastal and shelf areas, often burying partially in the substrate. Nektonic forms, like lancetfishes (Alepisaurus spp.), occupy midwater pelagic zones, while deep-sea representatives, including Bathysaurus ferox, are adapted to the ocean floor at depths reaching 600–3500 m. Aulopiformes are primarily marine, with rare occurrences in brackish waters but absent from freshwater systems, and no records of or riverine adaptations. Certain taxa, such as greeneyes in the genus Chlorophthalmus, are characteristic of continental slopes, inhabiting or clay bottoms on the upper slope at depths of 200–800 m in temperate to tropical waters. Recent distributional data from 2025 highlight expanded records for Synodus autumnus, a newly described lizardfish species now confirmed across the eastern to the western Pacific, including localities from and to and .

Reproduction and Development

Aulopiformes display diverse reproductive modes, with simultaneous hermaphroditism prevalent in several lineages, particularly within the suborder Alepisauroidei, where it represents the oldest known occurrence of this strategy among vertebrates, evolving once in the stem lineage during the . This condition allows individuals to function as both concurrently, often with , as seen in like Chlorophthalmus agassizi of the family Chlorophthalmidae. In contrast, gonochoristic reproduction with separate sexes characterizes families such as , exemplified by Synodus , where males engage in lek-like and both sexes are promiscuous during spawning. Spawning strategies vary by habitat and ecology; deep-water and mesopelagic forms typically release pelagic eggs that float freely in the water column, while benthic species often produce demersal eggs or spawn in midwater close to the substrate. For instance, Trachinocephalus myops deposits small, spherical pelagic eggs (0.95–1.25 mm diameter) lacking oil globules. In temperate regions, spawning is often seasonal, peaking in spring for species like C. agassizi, though some exhibit prolonged periods extending into autumn. The life cycle of Aulopiformes involves a planktonic larval phase following hatching, with no provided; larvae drift passively in the before undergoing and settlement. exceeds 10 years in many taxa, such as C. agassizi, accompanied by slow growth rates especially in deep-sea , which contribute to delayed maturity and low reproductive output. typically occurs after a larval duration of several weeks to months, marked by body elongation, pigment development, and shifts in the position of the and fins, transitioning to juvenile forms at sizes ranging from 25–40 mm depending on the .

Feeding and Behavior

Aulopiformes exhibit a predominantly carnivorous diet, consisting primarily of smaller fishes, crustaceans, cephalopods, and occasionally other . Benthic representatives, such as those in the family (lizardfishes), typically ambush prey like crustaceans and small fish from concealed positions on the seafloor, darting forward rapidly to seize them. In contrast, pelagic members, including the Alepisauridae (lancetfishes), actively pursue more mobile prey such as and mesopelagic fishes through opportunistic foraging in open water columns. Dietary composition often reflects seasonal prey availability and regional abundance, with shifts toward more diverse items during periods of high resource overlap. Feeding mechanisms in Aulopiformes are adapted for efficient prey capture, featuring expansive mouths and prominent sharp teeth that secure struggling victims. These structures enable a gape sufficient to engulf prey larger than the fish's head in some cases, supporting both suction-assisted and biting strategies across habitats. In deeper-water species, such as barracudinas (Paralepididae), extended storage allows for infrequent but substantial feeding bouts on energy-rich mesopelagic prey. Behavioral patterns vary by habitat and life stage, with many species displaying nocturnal activity to exploit diel migrations of prey in shallower zones. Juveniles often aggregate in loose schools for protection and enhanced efficiency, transitioning to solitary habits as adults to minimize and predation risk. Agonistic interactions are infrequent, as most adults maintain territorial or cryptic postures rather than overt displays. Within deep-sea ecosystems, Aulopiformes serve as key intermediate or mesopredators, bridging primary consumers like with apex predators such as tunas and billfishes, thereby facilitating energy transfer across trophic levels. In benthic communities, species like Synodus can function as apex predators where large piscivores are scarce. Their opportunistic habits contribute to the resilience of food webs in dynamic oceanic environments.

Evolutionary History

Fossil Record

The fossil record of Aulopiformes extends from the to the , with the earliest known occurrences dating to the stage (approximately 127–125 million years ago), represented by marine deposits containing early enchodontoid forms such as . , a prominent within the extinct Enchodontidae, persisted through the into the ( stage, approximately 66–64 million years ago), with widespread distribution across , , , and . The order encompasses approximately 30 recognized fossil across several extinct families, including the dominant Enchodontidae and the elongate-jawed Dercetidae, which together highlight the group's early diversification in marine environments. Enchodontids, in particular, achieved body lengths up to 1 meter or more, as evidenced by articulated specimens from Tethyan deposits. Key fossil sites include the Santana Formation in , a renowned yielding articulated aulopiform skeletons from marine concretions, and the Early El Chango quarry in , , where exceptional preservation reveals complete skulls, lateral lines, and even stomach contents in enchodontids. In the Eocene, the Monte Bolca locality in provides transitional forms, such as the paralepidid Holosteus esocinus, preserved in shallow marine limestones that capture detailed and impressions. Fossils from extant families, such as Omosudis (Alepisauridae) from the middle Yokoo Formation in , demonstrate the persistence of aulopiform lineages into the . These sites demonstrate the order's adaptation to marine habitats, with fossils often showing physoclistous or absent swim bladders inferred from skeletal features like reduced abdominal cavities, indicative of early deep-sea specializations.

Origins and Diversification

The order Aulopiformes originated during the , approximately 140 million years ago, from basal euteleost ancestors that inhabited marine inshore environments with separate sexes and laterally directed eyes. This emergence aligned with the expansion of marine niches in the , allowing the group to persist through the end-Cretaceous mass extinction and contribute to post-extinction recovery in teleost assemblages. Major diversification events began with a radiation in the , marked by deep-sea colonization near the Jurassic-Cretaceous boundary around 145 million years ago, as part of a broader pulse involving multiple lineages. Subsequent bursts occurred during the , with high speciation rates from the Early to Middle epochs, driven by shifts in bathymetric ranges and environmental changes that favored both shallow and deep habitats. Most extant families arose between the Late Cretaceous and Eocene, reflecting adaptive expansions into pelagic and bathypelagic zones. Key adaptive drivers included the single evolution of simultaneous hermaphroditism in the stem species of the deep-sea suborder Alepisauroidei during the (around 128 million years ago), which supported reproduction in sparse populations of aphotic environments. also arose repeatedly across deep-sea aulopiform lineages, enhancing predation efficiency and species-specific signaling in lightless depths, as seen in families like Scopelarchidae where orbital light organs promote . Phylogenetic studies indicate contrasting evolutionary trajectories, with morphological stasis prevalent in some deep-sea clades due to stable selective pressures, while shallow-water lineages like exhibit ongoing tied to transitions and body-shape innovations.

References

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