View source for Eurypterid

{{Short description|Order of arthropods (fossil)}}
{{About|the order Eurypterida|the eurypterid family containing [[Eurypterus]] itself|Eurypteridae}}
{{Good article}}
{{Automatic taxobox
|fossil_range = [[Darriwilian]]-[[Late Permian]], {{Fossil range|467.3|251.9|earliest=491}}<small>Possible [[Jiangshanian]] record</small>
|image = Eurypterus remipes 001.jpg
|image_caption = Fossil specimen of ''[[Eurypterus remipes]]'' housed at the [[State Museum of Natural History Karlsruhe]] in [[Karlsruhe]], [[Germany]]
|taxon = Eurypterida
|authority = [[Hermann Burmeister|Burmeister]], 1843
|subdivision_ranks = Suborders
|subdivision = *†[[Eurypterina]] <small>Burmeister, 1843</small><br/>
*†[[Stylonurina]] <small>[[Carl Diener|Diener]], 1924</small>
{{collapsible list|bullets = true
 |title=<small>''Incertae sedis''</small>
|†''[[Dorfopterus]]''
|†''[[Marsupipterus]]''
}}
|synonyms = *Gigantostraca <small>[[Ernst Haeckel|Haeckel]], 1866</small>
*Cyrtoctenida <small>[[Leif Størmer|Størmer]] & Waterston, 1968</small>
}}

'''Eurypterids''', often informally called '''sea scorpions''', are a group of extinct marine [[arthropod]]s that form the [[Order (biology)|order]] '''Eurypterida'''. The earliest known eurypterids date to the [[Darriwilian]] stage of the [[Ordovician]] period, 467.3 [[Myr|million years ago]]. The group is likely to have appeared first either during the [[Early Ordovician]] or [[Late Cambrian]] period. With approximately 250 species, the Eurypterida is the most diverse [[Paleozoic]] [[Chelicerata|chelicerate]] order. Following their appearance during the Ordovician, eurypterids became major components of marine faunas during the [[Silurian]], from which the majority of eurypterid species have been described. The Silurian genus ''[[Eurypterus]]'' accounts for more than 90% of all known eurypterid specimens. Though the group continued to diversify during the subsequent [[Devonian]] period, the eurypterids were heavily affected by the [[Late Devonian extinction event]]. They declined in numbers and diversity until becoming extinct during the [[Permian–Triassic extinction event]] (or sometime shortly before) 251.9{{nbsp}}million years ago.

Although popularly called "sea scorpions", only the earliest eurypterids were [[Marine life|marine]]; many later forms lived in [[Brackish water|brackish]] or [[fresh water]], and they were not true [[scorpion]]s. Some studies suggest that a dual [[respiratory system]] was present, which would have allowed for short periods of time in terrestrial environments. The name ''Eurypterida'' comes from the [[Ancient Greek]] words {{wikt-lang|grc|εὐρύς}} (''{{grc-transl|εὐρύς}}''), meaning 'broad' or 'wide', and {{wikt-lang|grc|πτερόν}} (''{{grc-transl|πτερόν}}''), meaning 'wing', referring to the pair of wide swimming appendages present in many members of the group.

The eurypterid order includes the largest known arthropods ever to have lived. The largest, ''[[Jaekelopterus]]'', reached {{convert|2.5|m|ft|sp=us}} in length. Eurypterids were not uniformly large and most species were less than {{convert|20|cm|in|sp=us|0}} long; the smallest eurypterid, ''[[Alkenopterus]]'', was only {{convert|2.03|cm|in|sp=us}} long. Eurypterid fossils have been recovered from every continent. A majority of fossils are from fossil sites in [[North America]] and [[Europe]] because the group lived primarily in the waters around and within the ancient supercontinent of [[Euramerica]]. Only a handful of eurypterid groups spread beyond the confines of Euramerica and a few genera, such as ''[[Adelophthalmus]]'' and ''[[Pterygotus]]'', achieved a [[cosmopolitan distribution]] with fossils being found worldwide.

==Description==
[[File:Eurypterus_anatomy.png|left|thumb|Restoration of ''[[Eurypterus]]'' with body parts labelled|alt=]]
Like all other [[arthropod]]s, eurypterids possessed [[Segmentation (biology)|segmented]] bodies and jointed appendages (limbs) covered in a [[cuticle]] composed of [[protein]]s and [[chitin]]. As in other [[chelicerates]], the body was divided into two [[Tagmata (arthropod anatomy)|tagmata]] (sections); the frontal [[prosoma]] (head) and posterior [[opisthosoma]] (abdomen).{{sfn|Størmer|1955|p=23}} The prosoma was covered by a [[carapace]] (sometimes called the "prosomal shield") on which both [[compound eyes]] and the [[ocelli]] (simple eye-like sensory organs) were located.{{sfn|Braddy|Dunlop|1997|pp=437–439}}

The prosoma also bore six pairs of appendages which are usually referred to as appendage pairs I to VI. The first pair of appendages, the only pair placed before the mouth, is called the [[chelicerae]] ([[Homology (biology)|homologous]] to the fangs of spiders). They were equipped with small pincers used to manipulate food fragments and push them into the mouth.{{sfn|Braddy|Dunlop|1997|pp=437–439}} In one lineage, the [[Pterygotidae]], the chelicerae were large and long, with strong, well-developed teeth on specialised [[Chela (organ)|chelae]] (claws).{{sfn|Tetlie|Briggs|2009|p=1141}} The subsequent pairs of appendages, numbers II to VI, possessed gnathobases (or "tooth-plates") on the [[Arthropod coxa|coxae]] (limb segments) used for feeding. These appendages were generally walking legs that were cylindrical in shape and were covered in spines in some species. In most lineages, the limbs tended to get larger the farther back they were. In the [[Eurypterina]] [[suborder]], the larger of the two eurypterid suborders, the sixth pair of appendages was also modified into a swimming paddle to aid in traversing aquatic environments.{{sfn|Braddy|Dunlop|1997|pp=437–439}}

The opisthosoma comprised 12 segments and the [[telson]], the posteriormost division of the body, which in most species took the form of a blade-like shape.{{sfn|Braddy|Dunlop|1997|pp=437–439}} In some lineages, notably the [[Pterygotioidea]], the [[Hibbertopteridae]] and the [[Mycteroptidae]], the telson was flattened and may have been used as a rudder while swimming. Some genera within the superfamily [[Carcinosomatoidea]], notably ''[[Eusarcana]]'', had a telson similar to that of true [[scorpion]]s and may even have been capable of using it to inject [[venom]] like them.{{sfn|Plotnick|Baumiller|1988|p=22|pp=}}{{sfn|Clarke|Ruedemann|1912|p=244|pp=}} The coxae of the sixth pair of appendages were overlaid by a plate that is referred to as the metastoma, originally derived from a complete exoskeleton segment. The opisthosoma itself can be divided either into a "[[mesosoma]]" (comprising segments 1 to 6) and "[[metasoma]]" (comprising segments 7 to 12) or into a "preabdomen" (generally comprising segments 1 to 7) and "postabdomen" (generally comprising segments 8 to 12).{{sfn|Braddy|Dunlop|1997|pp=437–439}}

The underside of the opisthosoma was covered in structures evolved from modified opisthosomal appendages. Throughout the opisthosoma, these structures formed plate-like structures termed {{lang|de|Blattfüsse}} ({{lit|leaf-feet}} in German).<ref>{{cite web | url=https://core.ac.uk/reader/213406250 | title=Selectivity in the evolution of Palaeozoic arthropod groups, with focus on mass extinctions and radiations: A phylogenetic approach }}</ref> These created a branchial chamber (gill tract) between preceding {{lang|de|Blattfüsse|italics=unset}} and the [[ventral]] surface of the opisthosoma itself, which contained the respiratory organs. The second to sixth opisthosomal segments also contained oval or triangular organs that have been interpreted as organs that aid in respiration. These organs, termed {{lang|de|Kiemenplatten}} or "gill tracts", would potentially have aided eurypterids to breathe air above water, while {{lang|de|Blattfüssen|italics=unset}}, similar to organs in modern [[horseshoe crab]]s, would cover the parts that serve for [[underwater respiration]].{{sfn|Braddy|Dunlop|1997|pp=437–439}}

The appendages of opisthosomal segments 1 and 2 (the seventh and eighth segments overall) were fused into a structure termed the genital operculum, occupying most of the underside of the opisthosomal segment 2. Near the [[anterior]] margin of this structure, the genital appendage (also called the {{lang|de|Zipfel}} or the median abdominal appendage) protruded. This appendage, often preserved very prominently, has consistently been interpreted as part of the reproductive system and occurs in two recognized types, assumed to correspond to male and female.{{sfn|Braddy|Dunlop|1997|pp=437–439}}

==Biology==

===Size===
[[File:Mega-Eurypterids.svg|thumb|Size comparison of six of the largest eurypterids: ''[[Pterygotus|Pterygotus grandidentatus]]'', ''[[Pentecopterus|Pentecopterus decorahensis]]'', ''[[Acutiramus|Acutiramus macrophthalmus]]'', ''A. bohemicus'', ''[[Carcinosoma|Carcinosoma punctatum]]'', and ''[[Jaekelopterus|Jaekelopterus rhenaniae]]'']]
Eurypterids were highly variable in size, depending on factors such as lifestyle, living environment and [[Affinity (taxonomy)|taxonomic affinity]]. Sizes around {{convert|100|cm|ft|sp=us}} are common in most eurypterid groups.{{sfn|Tetlie|2007|pp=|p=557}} The smallest eurypterid, ''[[Alkenopterus|Alkenopterus burglahrensis]]'', measured just {{convert|2.03|cm|in|sp=us}} in length.{{sfn|Poschmann|Tetlie|pp=|p=189|2004}}

The largest eurypterid, and the largest known arthropod ever to have lived, is ''[[Jaekelopterus rhenaniae]]''. A chelicera from the [[Emsian]] [[Klerf Formation]] of Willwerath, [[Germany]] measured {{convert|36.4|cm|in|sp=us}} in length, but is missing a quarter of its length, suggesting that the full chelicera would have been {{convert|45.5|cm|in|sp=us}} long. If the proportions between body length and chelicerae match those of its closest relatives, where the ratio between claw size and body length is relatively consistent, the specimen of ''Jaekelopterus'' that possessed the chelicera in question would have measured between {{convert|233|and|259|cm|sp=us|ft}}, an average {{convert|2.5|m|ft|sp=us}}, in length. With the chelicerae extended, another meter (3.28&nbsp;ft) would be added to this length. This estimate exceeds the maximum body size of all other known giant arthropods by almost half a meter (1.64&nbsp;ft) even if the extended chelicerae are not included.{{sfn|Braddy|Poschmann|Tetlie|pp=|p=107|2008}} Two other eurypterids have also been estimated to have reached lengths of 2.5 metres; ''[[Erettopterus|Erettopterus grandis]]'' (closely related to ''Jaekelopterus'') and ''[[Hibbertopterus|Hibbertopterus wittebergensis]]'', but ''E. grandis'' is very fragmentary and the ''H. wittenbergensis'' size estimate is based on trackway evidence, not fossil remains.{{sfn|Lamsdell|Braddy|2009|pp=|p=|loc=[http://rsbl.royalsocietypublishing.org/content/suppl/2009/10/09/rsbl.2009.0700.DC1/rsbl20090700supp1.xls  Supplementary information]}}

The family of ''Jaekelopterus'', the Pterygotidae, is noted for several unusually large species. Both ''[[Acutiramus]]'', whose largest member ''A. bohemicus'' measured {{convert|2.1|m|ft|sp=us}}, and ''[[Pterygotus]],'' whose largest species ''P. grandidentatus'' measured {{convert|1.75|m|ft|sp=us}}, were gigantic.{{sfn|Braddy|Poschmann|Tetlie|pp=|p=107|2008}} Several different contributing factors to the large size of the pterygotids have been suggested, including courtship behaviour, predation and competition over environmental resources.{{sfn|Briggs|1985|pp=157–158}}

Giant eurypterids were not limited to the family Pterygotidae. An isolated {{convert|12.7|cm|in|sp=us}} long fossil metastoma of the carcinosomatoid eurypterid ''[[Carcinosoma|Carcinosoma punctatum]]'' indicates the animal would have reached a length of {{convert|2.2|m|ft|sp=us}} in life, rivalling the pterygotids in size.{{sfn|Kjellesvig-Waering|1961|pp=|p=830}} Another giant was ''[[Pentecopterus|Pentecopterus decorahensis]]'', a primitive carcinosomatoid, which is estimated to have reached lengths of {{convert|1.7|m|ft|sp=us}}.{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=15|Witzke}}

Typical of large eurypterids is a lightweight build. Factors such as locomotion, energy costs in [[molting]] and respiration, as well as the actual physical properties of the [[exoskeleton]], limit the size that arthropods can reach. A lightweight construction significantly decreases the influence of these factors. Pterygotids were particularly lightweight, with most fossilized large body segments preserving as thin and unmineralized.{{sfn|Braddy|Poschmann|Tetlie|pp=|p=107|2008}} Lightweight adaptations are present in other giant paleozoic arthropods as well, such as the giant millipede ''[[Arthropleura]]'', and are possibly vital for the evolution of giant size in arthropods.{{sfn|Braddy|Poschmann|Tetlie|pp=|p=107|2008}}{{sfn|Kraus|Brauckmann|2003|pp=5–50|p=}}

In addition to the lightweight giant eurypterids, some deep-bodied forms in the family Hibbertopteridae were also very large. A carapace from the Carboniferous of Scotland referred to the species ''Hibbertoperus scouleri'' measures {{cvt|65|cm}} wide. As ''Hibbertopterus'' was very wide compared to its length, the animal in question could possibly have measured just short of {{convert|2|m|ft|sp=us}} in length. More robust than the pterygotids, this giant ''Hibbertopterus'' would possibly have rivalled the largest pterygotids in weight, if not surpassed them, and as such be among the heaviest arthropods.{{sfn|Tetlie|2008|p=19}}

===Locomotion===
{{Multiple images|align=right|direction=vertical|width=220|image1=Subaqueous flight.png|caption1=Illustration of subaqueous flight in ''[[Eurypterus]]'' in which the shape of the paddles and their motion through water is enough to generate [[Lift (force)|lift]]. This type of locomotion was limited to [[Eurypterina|eurypterine]] (with swimming paddles) eurypterids.|image2=Hibbertopterus scouleri.jpg|caption2=Illustration of ''[[Hibbertopterus]]'', a large [[Stylonurina|stylonurine]] (lacking swimming paddles) eurypterid}}

The two eurypterid suborders, Eurypterina and [[Stylonurina]], are distinguished primarily by the morphology of their final pair of appendages. In the Stylonurina, this appendage takes the form of a long and slender walking leg, while in the Eurypterina, the leg is modified and broadened into a swimming paddle.{{sfn|Tetlie|2007|pp=|p=559}} Other than the swimming paddle, the legs of many eurypterines were far too small to do much more than allow them to crawl across the [[sea floor]]. In contrast, a number of stylonurines had elongated and powerful legs that might have allowed them to walk on land (similar to modern [[crab]]s).{{sfn|Palaeos|p=}}

A [[fossil trackway]] was discovered in Carboniferous-aged fossil deposits of Scotland in 2005. It was attributed to the stylonurine eurypterid ''Hibbertopterus'' due to a matching size (the trackmaker was estimated to have been about {{convert|1.6|m|ft|sp=us}} long) and inferred leg anatomy. It is the largest terrestrial trackway—measuring {{convert|6|m|ft|sp=us}} long and averaging {{convert|95|cm|ft|sp=us}} in width—made by an arthropod found thus far. It is the first record of land locomotion by a eurypterid. The trackway provides evidence that some eurypterids could survive in terrestrial environments, at least for short periods of time, and reveals information about the stylonurine gait. In ''Hibbertopterus'', as in most eurypterids, the pairs of appendages are different in size (referred to as a heteropodous limb condition). These differently sized pairs would have moved in phase, and the short stride length indicates that ''Hibbertopterus'' crawled with an exceptionally slow speed, at least on land. The large telson was dragged along the ground and left a large central groove behind the animal. Slopes in the tracks at random intervals suggest that the motion was jerky.{{sfn|Whyte|2005|p=576}} The gait of smaller stylonurines, such as ''[[Parastylonurus]]'', was probably faster and more precise.{{sfn|Selden|1999|p=43|pp=}}

The functionality of the eurypterine swimming paddles varied from group to group. In the [[Eurypteroidea]], the paddles were similar in shape to oars. The condition of the joints in their appendages ensured their paddles could only be moved in near-horizontal planes, not upwards or downwards. Some other groups, such as the Pterygotioidea, would not have possessed this condition and were probably able to swim faster.{{sfn|Selden|1999|p=45}} Most eurypterines are generally agreed to have utilized a rowing type of propulsion similar to that of crabs and [[water beetle]]s. Larger individuals may have been capable of underwater flying (or [[Aquatic locomotion|subaqueous flight]]) in which the motion and shape of the paddles are enough to generate [[Lift (force)|lift]], similar to the swimming of [[sea turtle]]s and [[sea lion]]s. This type of movement has a relatively slower acceleration rate than the rowing type, especially since adults have proportionally smaller paddles than juveniles. However, since the larger sizes of adults mean a higher [[drag coefficient]], using this type of propulsion is more energy-efficient.{{sfn|Selden|1999|p=|pp=44–46}}
[[File:Palmichnium kosinskiorum (eurypterid tracks).jpg|thumb|The [[holotype]] of ''[[Palmichnium|Palmichnium kosinkiorum]]'', containing the largest eurypterid footprints known]]
Some eurypterines, such as ''[[Mixopterus]]'' (as inferred from attributed fossil trackways), were not necessarily good swimmers. It likely kept mostly to the bottom, using its swimming paddles for occasional bursts of movements vertically, with the fourth and fifth pairs of appendages positioned backwards to produce minor movement forwards. While walking, it probably used a gait like that of most modern insects. The weight of its long abdomen would have been balanced by two heavy and specialized frontal appendages, and the [[center of gravity]] might have been adjustable by raising and positioning the tail.{{sfn|Hanken|Størmer|p=|pp=262–267|1975}}

Preserved fossilized eurypterid trackways tend to be large and heteropodous and often have an associated telson drag mark along the mid-line (as with the Scottish ''Hibbertopterus'' track). Such trackways have been discovered on every continent except for South America. In some places where eurypterid fossil remains are otherwise rare, such as in [[South Africa]] and the rest of the former supercontinent [[Gondwana]], the discoveries of trackways both predate and outnumber eurypterid body fossils.{{sfn|Braddy|Almond|p=166|pp=|1999}} Eurypterid trackways have been referred to several ichnogenera, most notably ''[[Palmichnium]]'' (defined as a series of four tracks often with an associated drag mark in the mid-line),{{sfn|Braddy|Almond|p=|pp=168–170|1999}} wherein the holotype of the ichnospecies ''P. kosinkiorum'' preserves the largest eurypterid footprints known to date with the found tracks each being about {{convert|7.6|cm|in|sp=us}} in diameter.{{sfn|Brezinski|Kollar|p=39|pp=|2016}} Other eurypterid ichnogenera include ''[[Merostomichnites]]'' (though it is likely that many specimens actually represent trackways of crustaceans) and ''[[Arcuites]]'' (which preserves grooves made by the swimming appendages).{{sfn|Braddy|Almond|p=|pp=168–170|1999}}{{sfn|Hanken|Størmer|p=255|pp=|1975}}{{sfn|Vrazo|Ciurca|p=235|pp=|2017}}

===Respiration===
[[File:Oniscus asellus - male side 2 (aka).jpg|left|thumb|The supposed "gill tracts" of eurypterids have been compared to the air-breathing [[pseudotrachea]]e present in the [[Posterior (anatomy)|posterior]] legs of modern [[Isopoda|isopods]], such as ''[[Oniscus]]'' (pictured).]]
In eurypterids, the respiratory organs were located on the ventral body wall (the underside of the opisthosoma). {{lang|de|Blattfüsse|italics=unset}}, evolved from opisthosomal appendages, covered the underside and created a gill chamber where the "gill tracts" were located.{{sfn|Braddy|Dunlop|1997|pp=437–439}} Depending on the species, the eurypterid gill tract was either triangular or oval in shape and was possibly raised into a cushion-like state. The surface of this gill tract bore several [[spinule]]s (small spines), which resulted in an enlarged surface area. It was composed of spongy tissue due to many [[invagination]]s in the structure.{{sfn|Selden|1985|p=219|pp=}}

Though the {{lang|de|Kiemenplatte}} is referred to as a "gill tract", it may not necessarily have functioned as actual gills. In other animals, gills are used for oxygen uptake from water and are outgrowths of the body wall. Despite eurypterids clearly being primarily aquatic animals that almost certainly evolved underwater (some eurypterids, such as the pterygotids, would even have been physically unable to walk on land), it is unlikely the "gill tract" contained functional gills when comparing the organ to gills in other invertebrates and even fish. Previous interpretations often identified the eurypterid "gills" as homologous with those of other groups (hence the terminology), with gas exchange occurring within the spongy tract and a pattern of branchio-cardiac and dendritic veins (as in related groups) carrying oxygenated blood into the body. The primary analogy used in previous studies has been horseshoe crabs, though their gill structure and that of eurypterids are remarkably different. In horseshoe crabs, the gills are more complex and composed of many lamellae (plates) which give a larger surface area used for gas exchange. In addition, the gill tract of eurypterids is proportionally much too small to support them if it is analogous to the gills of other groups. To be functional gills, they would have to have been highly efficient and would have required a highly efficient circulatory system. It is considered unlikely, however, that these factors would be enough to explain the large discrepancy between gill tract size and body size.{{sfn|Selden|1985|p=|pp=220–221}}

It has been suggested instead that the "gill tract" was an organ for breathing air, perhaps actually being a [[lung]], [[Plastron (arthropod)|plastron]] or a [[pseudotrachea]].{{sfn|Selden|1985|p=221|pp=}} Plastrons are organs that some arthropods evolved secondarily to breathe air underwater. This is considered an unlikely explanation since eurypterids had evolved in water from the start and they  would not have organs evolved from air-breathing organs present. In addition, plastrons are generally exposed on outer parts of the body while the eurypterid gill tract is located behind the {{lang|de|Blattfüssen|italics=unset}}.{{sfn|Selden|1985|p=222|pp=}} Instead, among arthropod respiratory organs, the eurypterid gill tracts most closely resemble the pseudotracheae found in modern [[Isopoda|isopods]]. These organs, called pseudotracheae, because of some resemblance to the [[trachea]]e (windpipes) of air-breathing organisms, are lung-like and present within the [[pleopods]] (back legs) of isopods. The structure of the pseudotracheae has been compared to the spongy structure of the eurypterid gill tracts. It is possible the two organs functioned in the same way.{{sfn|Selden|1985|p=|pp=222–223}}

Some researchers have suggested that eurypterids may have been adapted to an amphibious lifestyle, using the full gill tract structure as gills and the invaginations within it as pseudotrachea. This mode of life may not have been physiologically possible, however, since water pressure would have forced water into the invaginations leading to [[asphyxiation]]. Furthermore, most eurypterids would have been aquatic their entire lives. No matter how much time was spent on land, organs for respiration in underwater environments must have been present. True gills, expected to have been located within the branchial chamber within the {{lang|de|Blattfüssen|italics=unset}}, remain unknown in eurypterids.{{sfn|Selden|1985|p=|pp=222–223}}

===Ontogeny===
[[File:Strobilopterus proteus juveniles.jpg|thumb|[[Larva]]l (left) and juvenile (right) [[instar]]s of ''[[Strobilopterus]]'' (not to scale)]]
Like all arthropods, eurypterids matured and grew through static developmental stages referred to as [[instar]]s. These instars were punctuated by periods during which eurypterids went through [[ecdysis]] (molting of the cuticle) after which they underwent rapid and immediate growth. Some arthropods, such as insects and many crustaceans, undergo extreme changes over the course of maturing. Chelicerates, including eurypterids, are in general considered to be direct developers, undergoing no extreme changes after hatching (though extra body segments and extra limbs may be gained over the course of [[ontogeny]] in some lineages, such as [[xiphosura]]ns and [[sea spider]]s). Whether eurypterids were true direct developers (with hatchlings more or less being identical to adults) or hemianamorphic direct developers (with extra segments and limbs potentially being added during ontogeny) has been controversial in the past.{{sfn|Lamsdell|Selden|p=32|pp=|2013}}

Hemianamorphic direct development has been observed in many arthropod groups, such as [[trilobite]]s, [[megacheira]]ns, basal [[crustacean]]s and basal [[Myriapoda|myriapods]]. True direct development has on occasion been referred to as a trait unique to [[arachnid]]s. There have been few studies on eurypterid ontogeny as there is a general lack of specimens in the fossil record that can confidently be stated to represent juveniles.{{sfn|Lamsdell|Selden|p=32|pp=|2013}} It is possible that many eurypterid species thought to be distinct actually represent juvenile specimens of other species, with paleontologists rarely considering the influence of ontogeny when describing new species.{{sfn|Lamsdell|Selden|p=33|pp=|2013}}

Studies on a well-preserved fossil assemblage of eurypterids from the [[Pragian]]-aged [[Beartooth Butte Formation]] in [[Cottonwood Canyon (Wyoming)|Cottonwood Canyon]], [[Wyoming]], composed of multiple specimens of various developmental stages of eurypterids ''Jaekelopterus'' and ''[[Strobilopterus]]'', revealed that eurypterid ontogeny was more or less parallel and similar to that of extinct and extant xiphosurans, with the largest exception being that eurypterids hatched with a full set of appendages and opisthosomal segments. Eurypterids were thus not hemianamorphic direct developers, but true direct developers like modern arachnids.{{sfn|Lamsdell|Selden|p=44|pp=|2013}}

The most frequently observed change occurring through ontogeny (except for some genera, such as ''Eurypterus'', which appear to have been static) is the metastoma becoming proportionally less wide. This ontogenetic change has been observed in members of several superfamilies, such as the Eurypteroidea, the Pterygotioidea and the [[Moselopteroidea]].{{sfn|Lamsdell|Selden|p=34|pp=|2013}}

===Feeding===
[[File:Pterygotus abelov.jpg|thumb|''[[Pterygotus]]'' depicted hunting ''[[Birkenia]]'']]
No fossil gut contents from eurypterids are known, so direct evidence of their diet is lacking. The eurypterid biology is particularly suggestive of a carnivorous lifestyle. Not only were many large (in general, most predators tend to be larger than their prey), but they had [[stereoscopic vision]] (the ability to perceive depth).{{sfn|Selden|1999|p=46|pp=–}} The legs of many eurypterids were covered in thin spines, used both for locomotion and the gathering of food. In some groups, these spiny appendages became heavily specialized. In some eurypterids in the Carcinosomatoidea, forward-facing appendages were large and possessed enormously elongated spines (as in ''Mixopterus'' and ''[[Megalograptus]]''). In [[Primitive (phylogenetics)|derived]] members of the Pterygotioidea, the appendages were completely without spines, but had specialized claws instead.{{sfn|Selden|1999|p=47|pp=}} Other eurypterids, lacking these specialized appendages, likely fed in a manner similar to modern horseshoe crabs, by grabbing and shredding food with their appendages before pushing it into their mouth using their chelicerae.{{sfn|Hembree|Platt|Smith|pp=|p=77|2014}}

Fossils preserving [[digestive tracts]] have been reported from fossils of various eurypterids, among them ''Carcinosoma'', ''Acutiramus'' and ''[[Eurypterus]]''. Though a potential anal opening has been reported from the telson of a specimen of ''[[Buffalopterus]]'', it is more likely that the [[anus]] was opened through the thin cuticle between the last segment before the telson and the telson itself, as in modern horseshoe crabs.{{sfn|Selden|1999|p=46|pp=–}}

Eurypterid coprolites discovered in deposits of Ordovician age in Ohio containing fragments of a trilobite and eurypterid ''Megalograptus ohioensis'' in association with full specimens of the same eurypterid species have been suggested to represent evidence of [[cannibalism]]. Similar coprolites referred to the species ''[[Lanarkopterus|Lanarkopterus dolichoschelus]]'' from the Ordovician of Ohio contain fragments of [[jawless fish]] and fragments of smaller specimens of ''Lanarkopterus'' itself.{{sfn|Selden|1999|p=46|pp=–}}

Though [[apex predator]]y roles would have been limited to the very largest eurypterids, smaller eurypterids were likely formidable predators in their own right just like their larger relatives.{{sfn|Tetlie|2007|pp=|p=557}}

===Reproductive biology===
{{Multiple images|align=left|direction=vertical|width=220|image1=Pennsylvanian invertebrates of the Mazon Creek Area, Illinois Eurypterida figure 51.jpg|caption1=Type A genital appendage of ''[[Adelophthalmus|Adelophthalmus mansfieldi]]''|image2=A Revision of the Families and Genera of the Stylonuracea (Eurypterida) figure 97.jpg|caption2=Type B genital appendage of ''[[Kokomopterus|Kokomopterus longicaudatus]]''}}

As in many other entirely extinct groups, understanding and researching the reproduction and sexual dimorphism of eurypterids is difficult, as they are only known from fossilized shells and carapaces. In some cases, there might not be enough apparent differences to separate the sexes based on morphology alone.{{sfn|Palaeos|p=}} Sometimes two sexes of the same species have been interpreted as two different species, as was the case with two species of ''[[Drepanopterus]]'' (''D. bembycoides'' and ''D. lobatus'').{{sfn|Lamsdell|Braddy|Tetlie|pp=|p=1119|2009}}

The eurypterid prosoma is made up of the first six exoskeleton segments fused together into a larger structure. The seventh segment (thus the first opisthosomal segment) is referred to as the ''metastoma'' and the eighth segment (distinctly plate-like) is called the ''operculum'' and contains the genital aperature. The underside of this segment is occupied by the genital operculum, a structure originally evolved from ancestral seventh and eighth pair of appendages. In its center, as in modern horseshoe crabs, is a genital appendage. This appendage, an elongated rod with an internal duct, is found in two distinct morphs, generally referred to as "type A" and "type B".{{sfn|Palaeos|p=}} These genital appendages are often preserved prominently in fossils and have been the subject of various  interpretations of eurypterid reproduction and sexual dimorphism.{{sfn|Braddy|Dunlop|1997|pp=|p=436}}

Type A appendages are generally longer than those of type B. In some genera they are divided into different numbers of sections, such as in ''Eurypterus'' where the type A appendage is divided into three but the type B appendage into only two.{{sfn|Braddy|Dunlop|1997|pp=|p=438}} Such division of the genital appendage is common in eurypterids, but the number is not universal; for instance, the appendages of both types in the family Pterygotidae are undivided.{{sfn|Braddy|Poschmann|Tetlie|pp=|p=108|2008}} The type A appendage is also armed with two curved spines called {{lang|la|furca}} (lit. 'fork' in Latin). The presence of {{lang|la|furca|italics=unset}} in the type B appendage is also possible and the structure may represent the unfused tips of the appendages. Located between the [[Dorsal (anatomy)|dorsal]] and ventral surfaces of the {{lang|de|Blattfüsse|italics=unset}} associated with the type A appendages is a set of organs traditionally described as either "tubular organs" or "horn organs". These organs are most often interpreted as [[spermatheca]]e (organs for storing [[sperm]]), though this function is yet to be proven conclusively.{{sfn|Braddy|Dunlop|1997|pp=|p=439}} In arthropods, spermathecae are used to store the [[spermatophore]] received from males. This would imply that the type A appendage is the female morph and the type B appendage is the male.{{sfn|Palaeos|p=}} Further evidence for the type A appendages representing the female morph of genital appendages comes in their more complex construction (a general trend for female arthropod genitalia). It is possible that the greater length of the type A appendage means that it was used as an [[ovipositor]] (used to deposit eggs).{{sfn|Braddy|Dunlop|1997|pp=|p=449}} The different types of genital appendages are not necessarily the only feature that distinguishes between the sexes of eurypterids. Depending on the genus and species in question, other features such as size, the amount of ornamentation, and the proportional width of the body can be the result of sexual dimorphism.{{sfn|Braddy|Dunlop|1997|pp=437–439}} In general, eurypterids with type B appendages (males) appear to have been proportionally wider than eurypterids with type A appendages (females) of the same genera.{{sfn|Lamsdell|2014|p=|pp=175–177}}

[[File:Eurypterus sp. (YPM IP 543168).jpg|thumb|right|Type A genital appendage of ''Eurypterus'' sp.]]
The primary function of the long, assumed female, type A appendages was likely to take up spermatophore from the substrate into the [[reproductive tract]] rather than to serve as an ovipositor, as arthropod ovipositors are generally longer than eurypterid type A appendages. By rotating the sides of the operculum, it would have been possible to lower the appendage from the body. Due to the way different plates overlay at its location, the appendage would have been impossible to move without muscular contractions moving around the operculum. It would have been kept in place when not it use. The {{lang|la|furca|italics=unset}} on the type A appendages may have aided in breaking open the spermatophore to release the free sperm inside for uptake. The "horn organs," possibly spermathecae, are thought to have been connected directly to the appendage via tracts, but these supposed tracts remain unpreserved in available fossil material.{{sfn|Braddy|Dunlop|1997|pp=450–452|p=}}

Type B appendages, assumed male, would have produced, stored and perhaps shaped spermatophore in a heart-shaped structure on the dorsal surface of the appendage. A broad genital opening would have allowed large amounts of spermatophore to be released at once. The long {{lang|la|furca|italics=unset}} associated with type B appendages, perhaps capable of being lowered like the type A appendage, could have been used to detect whether a substrate was suitable for spermatophore deposition.{{sfn|Braddy|Dunlop|1997|pp=454–455|p=}}

==Evolutionary history==

===Origins===
[[File:Eurypterids Pentecopterus Vertical.jpg|thumb|A reconstruction of ''[[Pentecopterus]]'', the earliest known eurypterid. The family to which ''Pentecopterus'' belongs, the [[Megalograptidae]], was the first truly successful eurypterid group.]]
Until 1882 no eurypterids were known from before the Silurian. Contemporary discoveries since the 1880s have expanded the knowledge of early eurypterids from the [[Ordovician]] period.{{sfn|O'Connell|1916|pp=|p=11}} The earliest eurypterids known today, the [[Megalograptidae|megalograptid]] ''Pentecopterus'', date from the [[Darriwilian]] stage of the Middle Ordovician, 467.3 [[Myr|million years ago]].{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=1|Witzke}} There are also reports of even earlier fossil eurypterids in the [[Fezouata Formation|Fezouata Biota]] of Late [[Tremadocian]] (Early Ordovician) age in [[Morocco]], but these have yet to be thoroughly studied,{{sfn|Van Roy|Briggs|Gaines|pp=|p=6|2015}} and are likely to be [[Hurdiidae|peytoiid]] appendages.

''Pentecopterus'' was a relatively derived eurypterid, part of the megalograptid family within the carcinosomatoid superfamily. Its derived position suggests that most eurypterid clades, at least within the eurypterine suborder, had already been established at this point during the Middle Ordovician.{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=29|Witzke}} The earliest known stylonurine eurypterid, ''[[Brachyopterus]]'',{{sfn|Tetlie|2007|pp=|p=557}} is also Middle Ordovician in age. The presence of members of both suborders indicates that primitive stem-eurypterids would have preceded them, though these are so far unknown in the fossil record. The presence of several eurypterid clades during the Middle Ordovician suggests that eurypterids either originated during the Early Ordovician and experienced a rapid and explosive radiation and diversification soon after the first forms evolved, or that the group originated much earlier, perhaps during the [[Cambrian]] period.{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=29|Witzke}}

As such, the exact eurypterid time of origin remains unknown. Though fossils referred to as "primitive eurypterids" have occasionally been described from deposits of Cambrian or even [[Precambrian]] age,{{sfn|O'Connell|1916|pp=|p=12}} they are not recognized as eurypterids, and sometimes not even as related forms, today. Some animals previously seen as primitive eurypterids, such as the genus ''[[Strabops]]'' from the Cambrian of [[Missouri]],{{sfn|O'Connell|1916|pp=|p=13}} are now classified as [[Aglaspidida|aglaspidids]] or [[Strabopida|strabopids]]. The aglaspidids, once seen as primitive chelicerates, are now seen as a group more closely related to trilobites.{{sfn|Ortega-Hernández|Legg|Braddy|2012|p=15}}

The fossil record of Ordovician eurypterids is quite poor.  The majority of eurypterids once reportedly known from the Ordovician have since proven to be misidentifications or [[pseudofossil]]s. Today only 11 species can be confidently identified as representing Ordovician eurypterids. These taxa fall into two distinct ecological categories; large and active predators from the ancient continent of [[Laurentia]], and [[Demersal zone|demersal]] (living on the [[seafloor]]) and basal animals from the continents [[Avalonia]] and Gondwana.{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=1|Witzke}} The Laurentian predators, classified in the family Megalograptidae (comprising the genera ''[[Echinognathus]]'', ''Megalograptus'' and ''Pentecopterus''), are likely to represent the first truly successful eurypterid group, experiencing a small radiation during the Late Ordovician.{{sfn|Tetlie|2007|pp=|p=569}}

===Silurian===
[[File:Erettopterus osiliensis.jpg|left|thumb|Reconstruction of ''[[Erettopterus]]'', a member of the highly successful [[Silurian]] and [[Devonian]] eurypterid family [[Pterygotidae]]]]
Eurypterids were most diverse and abundant between the Middle Silurian and the Early Devonian, with an absolute peak in diversity during the [[Pridoli epoch]], 423 to 419.2 million years ago, of the very latest Silurian.{{sfn|Tetlie|2007|pp=|p=559}} This peak in diversity has been recognized since the early twentieth century; of the approximately 150 species of eurypterids known in 1916, more than half were from the Silurian and a third were from the Late Silurian alone.{{sfn|O'Connell|1916|pp=|p=11}}

Though stylonurine eurypterids generally remained rare and low in number, as had been the case during the preceding Ordovician, eurypterine eurypterids experienced a rapid rise in diversity and number.{{sfn|Tetlie|2007|pp=|p=567}} In most Silurian fossil beds, eurypterine eurypterids account for 90% of all eurypterids present.{{sfn|Tetlie|2007|pp=|p=570}} Though some were likely already present by the Late Ordovician (simply missing from the fossil record so far),{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=29|Witzke}} a vast majority of eurypterid groups are first recorded in [[Stratum|strata]] of Silurian age. These include both stylonurine groups such as the [[Stylonuroidea]], [[Kokomopteroidea]] and [[Mycteropoidea]] as well as eurypterine groups such as the Pterygotioidea, Eurypteroidea and [[Waeringopteridae|Waeringopteroidea]].{{sfn|Dunlop|Penney|pp=17–30|p=|Jekel|2018}}

The most successful eurypterid by far was the Middle to Late Silurian ''Eurypterus'', a [[Generalist and specialist species|generalist]], equally likely to have engaged in [[predation]] or [[scavenging]]. Thought to have hunted mainly small and soft-bodied invertebrates, such as [[worm]]s,{{sfn|Selden|1999|p=44|pp=}} species of the genus (of which the most common is the type species, ''E. remipes'') account for more than 90% (perhaps as many as 95%) of all known fossil eurypterid specimens.{{sfn|Tetlie|2007|pp=|p=570}} Despite their vast number, ''Eurypterus'' are only known from a relatively short temporal range, first appearing during the Late [[Llandovery epoch]] (around 432 million years ago) and being extinct by the end of the Pridoli epoch.{{sfn|Tetlie|2006|pp=|p=410}} ''Eurypterus'' was also restricted to the continent [[Euramerica]] (composed of the [[equator]]ial continents Avalonia, [[Baltica]] and Laurentia), which had been completely colonized by the genus during its merging and was unable to cross the vast expanses of ocean separating this continent from other parts of the world, such as the southern supercontinent Gondwana. As such, ''Eurypterus'' was limited geographically to the coastlines and shallow inland seas of Euramerica.{{sfn|Tetlie|2007|pp=|p=570}}{{sfn|Tetlie|Rábano|pp=|p=124|2007}}

During the Late Silurian the pterygotid eurypterids, large and specialized forms with several new adaptations, such as large and flattened telsons capable of being used as rudders, and large and specialized chelicerae with enlarged pincers for handling (and potentially in some cases killing) prey appeared.{{sfn|Tetlie|Briggs|2009|p=1141}}{{sfn|Plotnick|Baumiller|1988|p=22|pp=}} Though the largest members of the family appeared in the Devonian, large two meter (6.5+ ft) pterygotids such as ''Acutiramus'' were already present during the Late Silurian.{{sfn|Lamsdell|Braddy|2009|pp=|p=|loc=[http://rsbl.royalsocietypublishing.org/content/suppl/2009/10/09/rsbl.2009.0700.DC1/rsbl20090700supp1.xls  Supplementary information]}} Their ecology ranged from generalized predatory behavior to [[Ambush predator|ambush predation]] and some, such as ''Pterygotus'' itself, were active apex predators in Late Silurian marine ecosystems.{{sfn|McCoy|Lamsdell|Poschmann|Anderson|pp=|2015|p=3}} The pterygotids were also evidently capable of crossing oceans, becoming one of only two eurypterid groups to achieve a [[cosmopolitan distribution]].{{sfn|Tetlie|2007|pp=|p=571}}

===Devonian===
[[File:Adelophthalmus irinae.png|thumb|left|Reconstruction of ''[[Adelophthalmus]]'', the only [[Eurypterina|eurypterine]] (with swimming paddles) eurypterid to survive the [[Late Devonian extinction]] and persist into the subsequent [[Carboniferous]] and [[Permian]] periods.]]
Though the eurypterids continued to be abundant and diversify during the Early Devonian (for instance leading to the evolution of the pterygotid ''Jaekelopterus'', the largest of all arthropods), the group was one of many heavily affected by the [[Late Devonian extinction]]. The extinction event, only known to affect marine life (particularly trilobites, [[brachiopod]]s and [[reef]]-building organisms) effectively crippled the abundance and diversity previously seen within the eurypterids.{{sfn|Hallam|Wignall|1997|pp=|p=70}}

A major decline in diversity had already begun during the Early Devonian and eurypterids were rare in marine environments by the Late Devonian. During the [[Frasnian]] stage four families went extinct, and the later [[Famennian]] saw an additional five families going extinct.{{sfn|Hallam|Wignall|1997|pp=|p=70}} As marine groups were the most affected, the eurypterids were primarily impacted within the eurypterine suborder. Only one group of stylonurines (the family [[Parastylonuridae]]) went extinct in the Early Devonian. Only two families of eurypterines survived into the Late Devonian at all ([[Adelophthalmidae]] and Waeringopteridae). The eurypterines experienced their most major declines in the Early Devonian, during which over 50% of their diversity was lost in just 10 million years. Stylonurines, on the other hand, persisted through the period with more or less consistent diversity and abundance but were affected during the Late Devonian, when many of the older groups were replaced by new forms in the families Mycteroptidae and Hibbertopteridae.{{sfn|Lamsdell|Braddy|2009|pp=|p=265}}

It is possible that the catastrophic extinction patterns seen in the eurypterine suborder were related to the emergence of more derived fish. Eurypterine decline began at the point when jawless fish first became more developed and coincides with the emergence of [[Placodermi|placoderms]] (armored fish) in both North America and Europe.{{sfn|Lamsdell|Braddy|2009|pp=|p=266}}

Stylonurines of the surviving hibbertopterid and mycteroptid families completely avoided competition with fish by evolving towards a new and distinct ecological niche. These families experienced a radiation and diversification through the Late Devonian and Early Carboniferous, the last ever radiation within the eurypterids, which gave rise to several new forms capable of "sweep-feeding" (raking through the substrate in search of prey).{{sfn|Lamsdell|Braddy|2009|pp=|p=268}}

===Carboniferous and Permian===
[[File:CampylocephalusDB117.jpg|thumb|Reconstruction of the [[Hibbertopteridae|hibbertopterid]] ''[[Campylocephalus]]'', the last known surviving eurypterid. ''Campylocephalus'' went extinct during the [[Permian-Triassic extinction event]] or sometime shortly before.]]  Only three eurypterid families—Adelophthalmidae, Hibbertopteridae and Mycteroptidae—survived the extinction event in its entirety. It was assumed that these were all freshwater animals, which would have rendered the eurypterids extinct in marine environments,{{sfn|Hallam|Wignall|1997|pp=|p=70}} and with marine eurypterid predators gone, [[Sarcopterygii|sarcopterygians]], such as the [[Rhizodontida|rhizodonts]], were the new apex predators in marine environments.{{sfn|Lamsdell|Braddy|2009|pp=|p=266}} However, various recent findings raise doubts about this, and suggest that these eurypterids were euryhaline forms that lived in marginal marine environments, such as estuaries, deltas, lagoons, and coastal ponds. One argument is paleobiogeographical; pterygotoid distribution seems to require oceanic dispersal.{{sfn|Tetlie|2007}} A recent review of Adelophthalmoidea admitted that "There is much more of a marine influence in many of the sections yielding ''Adelophthalmus'' than has previously been acknowledged."<ref name="Tetlie & Poschmann 2008">{{cite journal |last1=Tetlie |first1=O. Erik |last2=Poschmann |first2=Markus |title=Phylogeny and palaeoecology of the Adelophthalmoidea (Arthropoda; Chelicerata; Eurypterida) |journal=Journal of Systematic Palaeontology |date=1 January 2008 |volume=6 |issue=2 |pages=237–249 |doi=10.1017/S1477201907002416 |bibcode=2008JSPal...6..237T |s2cid=59488956 |url=https://doi.org/10.1017/S1477201907002416 |language=en |issn=1477-2019|url-access=subscription }}</ref> Similarly, a study of the eurypterid ''Hibbertopterus'' from the Carboniferous of New Mexico concluded that the habitat of some eurypterids "may need to be re-evaluated".<ref name="Braddy et al. 2023">{{cite journal |last1=Braddy |first1=Simon J. |last2=Lerner |first2=Allan J |last3=Lucas |first3=Spencer G. |title=A new species of the eurypterid Hibbertopterus from the Carboniferous of New Mexico, and a review of the Hibbertopteridae |journal=Historical Biology |date=1 February 2023 |volume=35 |issue=2 |pages=257–263 |doi=10.1080/08912963.2022.2032690 |bibcode=2023HBio...35..257B |s2cid=246819305 |url=https://doi.org/10.1080/08912963.2022.2032690 |language=en |issn=0891-2963|url-access=subscription }}</ref> The sole surviving eurypterine family, Adelophthalmidae, was represented by only a single genus, ''[[Adelophthalmus]]''. The hibbertopterids, mycteroptids and ''Adelophthalmus'' survived into the Permian.{{sfn|Dunlop|Penney|pp=19 & 24|p=|Jekel|2018}}

''Adelophthalmus'' became the most common of all late Paleozoic eurypterids, existing in greater number and diversity than surviving stylonurines, and diversified in the absence of other eurypterines.{{sfn|Tetlie|Van Roy|pp=|p=79|2006}} Out of the 33 species referred to ''Adelophthalmus'', 23 (69%) are from the Carboniferous alone.{{sfn|Dunlop|Penney|pp=|p=24|Jekel|2018}}{{sfn|Lamsdell|McCoy|Perron-Feller|Hopkins|2020|p=1}} The genus reached its peak diversity in the Late Carboniferous. Though ''Adelophthalmus'' had already been relatively widespread and represented around all major landmasses in the Late Devonian, the amalgamation of [[Pangaea]] into a global supercontinent over the course of the last two periods of the Paleozoic allowed ''Adelophthalmus'' to gain an almost worldwide distribution.{{sfn|Tetlie|2007|pp=|p=570}}

During the Late Carboniferous and [[Cisuralian|Early Permian]] ''Adelophthalmus'' was widespread, living primarily in brackish and freshwater environments adjacent to coastal plains. These environments were maintained by favorable climate conditions. They did not persist as climate changes owing to Pangaea's formation altered depositional and vegetational patterns across the world. With their habitat gone, ''Adelophthalmus'' dwindled in number and had already gone extinct by the [[Leonardian]] stage of the Early Permian.{{sfn|Kues|Kietzke|pp=|p=727|1981}}

Mycteroptids and hibbertopterids continued to survive for some time, with one genus of each group known from Permian strata: ''[[Hastimima]]'' and ''[[Campylocephalus]]'' respectively.{{sfn|Dunlop|Penney|pp=|p=19|Jekel|2018}} ''Hastimima'' went extinct during the Early Permian,{{sfn|White|1927|pp=|p=575}} as ''Adelophthalmus'' had, while ''Campylocephalus'' persisted longer. A massive incomplete carapace from Permian deposits in Russia represents the sole fossil remains of the species ''C. permianus'', which might have reached {{convert|1.4|m|ft|sp=us}} in length, while originally considered to be Late Permian in age{{sfn|Lamsdell|Braddy|2009|loc=[http://rsbl.royalsocietypublishing.org/content/suppl/2009/10/09/rsbl.2009.0700.DC1/rsbl20090700supp1.xls  Supplementary information]}} other sources suggest a [[Kungurian]]-[[Roadian]] age (~283-267 million years ago) for the specimen.{{sfn|Poschmann|Rozefelds|2021}} A fragment of eurypterid cuticle, given the species name ''[[Woodwardopterus|Woodwardopterus freemanorum]]'' is known from the terminal Permian of Australia, which represents the youngest known eurypterid.{{sfn|Poschmann|Rozefelds|2021}} No eurypterids are known from fossil beds higher than the Permian. This indicates that the last eurypterids died either in the catastrophic extinction event at its end or at some point shortly before it. This extinction event, the [[Permian&ndash;Triassic extinction event]], is the most devastating [[extinction event|mass extinction]] recorded, and rendered many other successful Paleozoic groups, such as the trilobites, extinct.{{sfn|Bergstrom|Dugatkin|2012|pp=|p=515}}

==History of study==
{{See also|Timeline of eurypterid research}}
[[File:The_Eurypterida_of_New_York_figure_1.jpg|alt=|left|thumb|Figure of ''[[Eurypterus remipes]]'' by [[James Ellsworth De Kay|James E. De Kay]] (1825).]]
The first known eurypterid specimen was discovered in the Silurian-aged rocks of [[New York (state)|New York]], to this day one of the richest eurypterid fossil locations. [[Samuel L. Mitchill]] described the specimen, discovered near [[Westmoreland, New York|Westmoreland]] in [[Oneida County, New York|Oneida county]] in 1818. He erroneously identified the fossil as an example of the fish ''[[Silurus]]'', likely due to the strange, [[catfish]]-like appearance of the carapace. Seven years later, in 1825, [[James Ellsworth De Kay|James E. DeKay]] examined the fossil and recognized it as clearly belonging to an arthropod. He thought the fossil, which he named ''Eurypterus remipes'', represented a crustacean of the order [[Branchiopoda]], and suggested it might represent a missing link between the trilobites and more derived branchiopods.{{sfn|Clarke|Ruedemann|1912|p=13|pp=}} The name ''Eurypterus'' derives from Greek {{transliteration|grc|eurús}} ({{wikt-lang|grc|εὐρύς}} 'broad, wide') and {{transliteration|grc|pteron}} ({{wikt-lang|grc|πτερόν}} 'wing').{{sfn|Nudds|Selden|2008|p=|pp=78–82}}

In 1843, [[Hermann Burmeister]] published his view on trilobite taxonomy and how the group related to other organisms, living and extinct, in the work ''Die Organisation der [[Trilobite]]n aus ihren lebenden Verwandten entwickelt''. He considered the trilobites to be crustaceans, as previous authors had, and classified them together with what he assumed to be their closest relatives, ''Eurypterus'' and the genus ''[[Cytherina]]'', within a clade he named "Palaeadae". Within Palaeadae, Burmeister erected three families; the "Trilobitae" (composed of all trilobites), the "Cytherinidae" (composed only of ''Cytherina'', an animal today seen as an [[ostracod]]) and the [[Eurypteridae]] (composed of ''Eurypterus'', then including three species).{{sfn|Burmeister|1843|p=|pp=62–64}}

The fourth eurypterid genus to be described (following ''Hibbertopterus'' in 1836 and ''Campylocephalus'' in 1838, not identified as eurypterids until later), out of those still seen as [[Valid name (zoology)|taxonomically valid]] in modern times, was ''Pterygotus'' ({{lit|winged one}}), described by [[Louis Agassiz]] in 1839.{{sfn|Dunlop|Penney|pp=|p=27|Jekel|2018}} ''Pterygotus'' was considerably larger in size than ''Eurypterus'' and when the first fossils were discovered by quarrymen in [[Scotland]] they were referred to as "[[Seraph]]ims" by the workers. Agassiz first thought the fossils represented remains of fish, only recognizing their nature as arthropod remains five years later in 1844.{{sfn|Kjellesvig-Waering|1964|pp=|p=331}}

In 1849, [[Frederick McCoy|Frederick M'Coy]] classified ''Pterygotus'' together with ''Eurypterus'' and ''[[Belinurus]]'' (a genus today seen as a xiphosuran) within Burmeister's Eurypteridae. M'Coy considered the Eurypteridae to be a group of crustaceans within the order [[Entomostraca]], closely related to horseshoe crabs.{{sfn|M'Coy|1849|pp=|p=393}} A fourth genus, ''[[Slimonia]]'', based on fossil remains previously assigned to a new species of ''Pterygotus'', was referred to the Eurypteridae in 1856 by [[David Page (geologist)|David Page]].{{sfn|Henderson|1866|pp=|p=18}}
[[File:The Eurypterida of New York diagram np 1.jpg|thumb|[[Evolutionary tree]] of eurypterids as imagined by [[John Mason Clarke]] and [[Rudolf Ruedemann]] in 1912.]]
Jan Nieszkowski's ''De Euryptero Remipede'' (1858) featured an extensive description of ''Eurypterus fischeri'' (now seen as synonymous with another species of ''Eurypterus'', ''E. tetragonophthalmus''), which, along with the monograph ''On the Genus Pterygotus'' by [[Thomas Henry Huxley]] and [[John William Salter]], and an exhaustive description of the various eurypterids of New York in Volume 3 of the ''Palaeontology of New York'' (1859) by [[James Hall (paleontologist)|James Hall]], contributed massively to the understanding of eurypterid diversity and biology. These publications were the first to fully describe the whole anatomy of eurypterids, recognizing the full number of prosomal appendages and the number of preabdominal and postabdominal segments. Both Nieszkowski and Hall recognized that the eurypterids were closely related to modern chelicerates, such as horseshoe crabs.{{sfn|Clarke|Ruedemann|1912|p=14|pp=}}

In 1865, [[Henry Woodward (geologist)|Henry Woodward]] described the genus ''[[Stylonurus]]'' (named and figured, but not thoroughly described, by David Page in 1856) and raised the rank of the Eurypteridae to that of order, effectively creating the Eurypterida as the taxonomic unit it is seen as today.{{sfn|Woodward|1865|p=|pp=484–486}} In the work ''Anatomy and Relations of the Eurypterida'' (1893), [[Malcolm Laurie]] added considerably to the knowledge and discussion of eurypterid anatomy and relations. He focused on how the eurypterids related to each other and to trilobites, crustaceans, scorpions, other arachnids and horseshoe crabs. The description of ''Eurypterus fischeri'' by Gerhard Holm in 1896 was so elaborate that the species became one of the most completely known of all extinct animals, so much so that the knowledge of ''E. fischeri'' was comparable with the knowledge of its modern relatives (such as the [[Atlantic horseshoe crab]]). The description also helped solidify the close relationship between the eurypterids and other chelicerates by showcasing numerous [[Homology (biology)|homologies]] between the two groups.{{sfn|Clarke|Ruedemann|1912|p=19|pp=}}

In 1912, [[John Mason Clarke]] and [[Rudolf Ruedemann]] published ''The Eurypterida of New York'' in which all eurypterid species thus far recovered from fossil deposits there were discussed. Clarke and Ruedemann created one of the first phylogenetic trees of eurypterids, dividing the order into two families; Eurypteridae (distinguished by smooth eyes and including ''Eurypterus'', ''[[Anthraconectes]]'', ''Stylonurus'', ''[[Eusarcus (eurypterid)|Eusarcus]]'', ''[[Dolichopterus]]'', ''[[Onychopterella|Onychopterus]]'' and ''Drepanopterus'') and Pterygotidae (distinguished by faceted eyes and including ''Pterygotus'', ''Erettopterus'', ''Slimonia'' and ''[[Hughmilleria]]''). Both families were considered to be descended from a common ancestor, ''Strabops''.{{sfn|Clarke|Ruedemann|1912|p=|pp=124–125}} In line with earlier authors, Clarke and Ruedemann also supported a close relationship between the eurypterids and the horseshoe crabs (united under the [[Class (biology)|class]] Merostomata) but also discussed alternative hypotheses such as a closer relation to arachnids.{{sfn|Clarke|Ruedemann|1912|p=135 & 137|pp=}}

==Classification==
{{Multiple images|align=right|direction=vertical|width=220|image1=Limulus polyphemus (aq.).jpg|caption1=|image2=Heterophrynus 02.jpg|caption2=|footer=Eurypterids have historically been seen as closely related to [[xiphosura]]ns such as the [[Atlantic horseshoe crab]] (top), united in the class Merostomata. Recent studies are in favor of a closer relationship to [[arachnids]] such as ''[[Heterophrynus]]'' (bottom), united under the clade [[Sclerophorata]].}}

Historically, a close relationship between eurypterids and xiphosurans (such as the modern Atlantic horseshoe crab) has been assumed by most researchers. Several homologies encourage this view, such as correlating segments of the appendages and the prosoma. Additionally, the presence of plate-like appendages bearing the "gill tracts" on appendages of the opisthosoma (the {{lang|de|Blattfüssen|italics=unset}}) was cited early as an important homology. In the last few decades of the nineteenth century, further homologies were established, such as the similar structures of the compound eyes of ''Pterygotus'' and horseshoe crabs (seen as especially decisive as the eye of the horseshoe crab was seen as possessing an almost unique structure) and similarities in the ontogeny within both groups.{{sfn|Clarke|Ruedemann|1912|p=135|pp=}} These ontogenetical similarities were seen as most apparent when studying the [[nepionic stage]]s (the developmental stage immediately following the embryonic stage) in both groups, during which both xiphosurans and eurypterids have a proportionally larger carapace than adults, are generally broader, possess a distinct ridge down the middle, have a lesser number of segments which lack differentiation and have an underdeveloped telson.{{sfn|Clarke|Ruedemann|1912|p=136|pp=}}

Due to these similarities, the xiphosurans and eurypterids have often been united under a single class or [[Subclass (biology)|subclass]] called Merostomata (erected to house both groups by Henry Woodward in 1866). Though xiphosurans (like the eurypterids) were historically seen as crustaceans due to their respiratory system and their aquatic lifestyle, this hypothesis was discredited after numerous similarities were discovered between the horseshoe crabs and the arachnids.{{sfn|Clarke|Ruedemann|1912|p=136|pp=}} Some authors, such as [[John Sterling Kingsley]] in 1894, classified the Merostomata as a sister group to the Arachnida under the class "Acerata" within a subphylum "Branchiata". Others, such as [[Ray Lankester]] in 1909, went further and classified the Merostomata as a subclass within the Arachnida, raised to the rank of class.{{sfn|Clarke|Ruedemann|1912|p=137|pp=}}

In 1866, [[Ernst Haeckel]] classified the Merostomata (containing virtually only the Eurypterida) and Xiphosura within a group he named Gigantostraca within the crustaceans. Though Haeckel did not designate any taxonomic rank for this clade, it was interpreted as equivalent to the rank of subclass, such as the Malacostraca and Entomostraca, by later researchers such as John Sterling Kinsgsley.{{sfn|Kingsley|1894|p=119|pp=}} In subsequent research, Gigantostraca has been treated as synonymous with Merostomata (rarely) and Eurypterida itself (more commonly).{{sfn|Lankester|1886|p=366|pp=}}{{sfn|Dunlop|Penney|pp=|p=17|Jekel|2018}}
A phylogenetic analysis (the results presented in a cladogram below) conducted by James Lamsdell in 2013 on the relationships within the Xiphosura and the relations to other closely related groups (including the eurypterids, which were represented in the analysis by genera ''Eurypterus'', ''Parastylonurus'', ''[[Rhenopterus]]'' and ''[[Stoermeropterus]]'') concluded that the Xiphosura, as presently understood, was [[paraphyletic]] (a group sharing a [[Last Common Ancestor|last common ancestor]] but not including all descendants of this ancestor) and thus not a valid phylogenetic group.{{sfn|Lamsdell|2012|p=19|pp=}} Eurypterids were recovered as closely related to arachnids instead of xiphosurans, forming the group [[Sclerophorata]] within the clade [[Dekatriata]] (composed of sclerophorates and [[Chasmataspidida|chasmataspidids]]). Lamsdell noted that it is possible that Dekatriata is synonymous with Sclerophorata as the reproductive system, the primary defining feature of sclerophorates, has not been thoroughly studied in chasmataspidids. Dekatriata is, in turn, part of the [[Prosomapoda]], a group including the [[Xiphosurida]] (the only monophyletic xiphosuran group) and other stem-genera.{{sfn|Lamsdell|2012|p=|pp=20–21}}

{{clade
  |style=font-size:80%; line-height:80%
  |label1=[[Arthropoda]]
  |sublabel1=
  |1={{clade
      |label1=
      |1=†''[[Fuxianhuia]]''
      |2={{clade
          |label1=†[[Antennulata]]
          |1={{clade
              |label1=
              |1=†''[[Emeraldella]]''
              |2=†[[Trilobitomorpha]]
              |3=†''[[Sidneyia]]''
              }} 
          |2={{clade
              |label1= †[[Megacheira]] 
              |1={{clade
                  |label1=
                  |1=†''[[Yohoia]]''
                  |2={{clade
                      |1=†''[[Alalcomenaeus]]''
                      |2=†''[[Leanchoilia]]''
                      }}
                  }}
              |label2= [[Chelicerata]] 
              |2={{clade
                  |label1= [[Pycnogonida]]  
                  |1={{clade
                      |label1=
                      |1=†''[[Palaeoisopus]]''
                      |2={{clade
                          |1=''[[Pycnogonum]]''
                          |2=†''[[Haliestes]]''
                          }}
                      }}
                  |label2= [[Euchelicerata]] 
                  |2={{clade
                      |1=†''[[Offacolus]]''
                      |label2= [[Prosomapoda]]  
                      |2={{clade
                          |label1=
                          |1=†''[[Weinbergina]]''
                          |2={{clade
                              |label1=
                              |1={{clade
                                  |1=†''[[Venustulus]]''
                                  |2=†''[[Camanchia]]''
                                  }}
                              |2={{clade
                                  |label1=
                                  |1=†''[[Legrandella]]''
                                  |2={{clade
                                      |label1= [[Xiphosura]]  
                                      |1={{clade
                                          |label1=
                                          |1=†''[[Kasibelinurus]]''
                                          |2={{clade
                                              |1=†''[[Willwerathia]]''
                                              |label2= [[Xiphosurida]]  
                                              |2={{clade
                                                  |label1=
                                                  |1=†''[[Lunataspis]]''
                                                  |2={{clade
                                                      |1=†[[Belinurina]]
                                                      |2=[[Limulina]]
                                                      }}
                                                  }}
                                              }}
                                          }}
                                      |label2= [[Planaterga]] 
                                      |2={{clade
                                          |label1=
                                          |1={{clade
                                              |1=†''[[Pseudoniscus]]''
                                              |2=†''[[Cyamocephalus]]''
                                              }}
                                          |2=†''[[Pasternakevia]]''
                                          |3={{clade
                                              |1=†''[[Bunodes]]''
                                              |2=†''[[Limuloides]]''
                                              }}
                                          |4=†''[[Bembicosoma]]''
                                          |label5= [[Dekatriata]] 
                                          |5={{clade
                                              |1=†[[Chasmataspidida]]
                                              |label2= [[Sclerophorata]] 
                                              |2={{clade
                                                  |1=[[Arachnida]]
                                                  |2=†'''Eurypterida'''
                                                  }}
                                              }}
                                          }}
                                      }}
                                  }}
                              }}
                          }}
                      }}
                  }}
              }}
          }}
      }}
  }}

===Internal relationships===
{{Multiple images|align=right|direction=vertical|width=220|image1=Bassipterus virginicus swimming leg.png|caption1=|image2=Parastylonurus ornatus sixth appendage.png|caption2=|footer=The most important taxonomic character in eurypterids is the morphology of the sixth pair of appendages. In most eurypterids of the suborder [[Eurypterina]], such as ''[[Bassipterus]]'' (top), this leg is modified into a swimming paddle. In eurypterids of the suborder [[Stylonurina]], such as ''[[Parastylonurus]]'' (bottom), it is not.}}The internal classification of eurypterids within the Eurypterida is based mainly on eleven established characters. These have been used throughout the history of eurypterid research to establish clades and genera. These characters include: the shape of the prosoma, the shape of the metastoma, the shape and position of the eyes, the types of prosomal appendages, the types of swimming leg paddles, the structure of the doublure (the fringe of the dorsal exoskeleton), the structure of the opisthosoma, the structure of the genital appendages, the shape of the telson and the type of ornamentation present. It is worth noting that not all of these characters are of equal taxonomic importance.{{sfn|Tollerton|1989|p=642|pp=}} They are not applicable to all eurypterids either; stylonurine eurypterids lack swimming leg paddles entirely.{{sfn|Tetlie|2007|pp=|p=559}} Some characters, including the prosoma and metastoma shapes and the position and shapes of the eyes, are seen as important only for the distinction between different genera.{{sfn|Tollerton|1989|p=|pp=642–644}} Most superfamilies and families are defined based on the morphology of the appendages.{{sfn|Tollerton|1989|p=649|pp=}}

The most important character used in eurypterid taxonomy is the type of prosomal appendages as this character is used to define entire suborders. General leg anatomy can also be used to define superfamilies and families. Historically, the chelicerae were considered the most important appendages from a taxonomical standpoint since they only occurred in two general types: a eurypterid type with small and toothless pincers and a pterygotid type with large pincers and teeth. This distinction has historically been used to divide the Eurypterida into the two suborders Eurypterina (small chelicerae) and "Pterygotina" (large and powerful chelicerae).{{sfn|Tollerton|1989|p=646|pp=}} This classification scheme is not without problems. In Victor Tollerton's 1989 taxonomic revision of the Eurypterida, with suborders Eurypterina and Pterygotina recognized, several clades of eurypterids today recognized as stylonurines (including hibbertopterids and mycteroptids) were reclassified as non-eurypterids in the new separate order "Cyrtoctenida" on the grounds of perceived inconsistencies in the prosomal appendages.{{sfn|Tollerton|1989|p=650|pp=}}

Modern research favors a classification into suborders Eurypterina and Stylonurina instead, supported by phylogenetic analyses.{{sfn|Lamsdell|Briggs|Liu|pp=|5=2015|p=25|Witzke}}{{sfn|Lamsdell|Selden|2013|p=34|pp=}} In particular, pterygotid eurypterids share a number of homologies with derived eurypterine eurypterids such as the adelophthalmids, and are thus best classified as derived members of the same suborder.{{sfn|Tetlie|Cuggy|2007|pp=|p=350}} In the Stylonurina, the sixth pair of appendages is represented by long and slender walking legs and lack a modified spine (referred to as the podomere 7a). In most eurypterids in the Eurypterina, the sixth pair of appendages is broadened into swimming paddles and always has a podomere 7a. 75% of eurypterid species are eurypterines and they represent 99% of all fossil eurypterid specimens.{{sfn|Tetlie|2007|pp=|p=559}} Of all eurypterid clades, the Pterygotioidea is the most species-rich, with over 50 species. The second most species-rich clade is the Adelophthalmoidea, with over 40 species.{{sfn|Tetlie|2007|pp=|p=570}}

A complete analysis of the taxonomy and phylogenetics of eurypterids was published in 2025 by Lamsdell based on all his research on the group, recognizing similar relationships to previous studies but also adding one new superfamily, ten new families, six new genera, and one new species. Every described species was evaluated, though not all were included in the analysis, with ''[[Dorfopterus]]'' and ''[[Marsupipterus]]'' removed from Eurypterida as indeterminate arthropods. The resultint interreelationships of Eurypterida can be seen below, showing orders, superfamilies, and families.{{sfn|Lamsdell|2025}}

{{clade|style=font-size:85%; line-height:85%;
|label1='''Eurypterida'''
|1={{clade
 |label1=[[Stylonurina]]
 |1={{clade
  |1={{clade
  |label1=[[Rhenopteroidea]]
  |1={{clade
   |1=[[Brachyopteridae]]
   |2={{clade
    |1=[[Brachyopterellidae]]
    |2=[[Rhenopteridae]] }} }} }}
  |2={{clade
   |1={{clade
   |label1=[[Stylonuroidea]]
   |1={{clade
    |1=[[Parastylonuridae]]
    |2={{clade
     |1=[[Stylonurellidae]]
     |2=[[Stylonuridae]] }} }} }}
   |2={{clade
    |label1=[[Kokomopteroidea]]
    |1={{clade
     |1=[[Hardieopteridae]]
     |2=[[Kokomopteridae]] }}
    |label2=[[Mycteropoidea]]
    |2={{clade
     |1=[[Drepanopteridae]]
     |2={{clade
      |1=[[Hibbertopteridae]]
      |2=[[Mycteropidae]] }} }} }} }} }}
 |label2=[[Eurypterina]]
 |2={{clade
  |1={{clade
  |label1=[[Moselopteroidea]]
  |1=[[Moselopteridae]] }}
  |2={{clade
   |1={{clade
   |label1=[[Alkenopteroidea]]
   |1=[[Alkenopteridae]] }}
   |2={{clade
    |1={{clade
    |label1=[[Onychopterelloidea]]
    |1=[[Onychopterellidae]] }}
    |2={{clade
     |1={{clade
     |label1=[[Dolichopteroidea]]
     |1={{clade
      |1=[[Dolichopteridae]]
      |2={{clade
       |1=[[Erieopteridae]]
       |2=[[Strobilopteridae]] }} }} }}
     |2={{clade
      |label1=[[Eurypteroidea]]
      |1=[[Eurypteridae]]
      |label2=[[Diploperculata]]
      |2={{clade
       |1={{clade
       |label1=[[Carcinosomatoidea]]
       |1={{clade
        |1=[[Megalograptidae]]
        |2={{clade
         |1=[[Carcinosomatidae]]
         |2={{clade
          |1=[[Mixopteridae]]
          |2=[[Lanarkopteridae]] }} }} }} }}
       |2={{clade
        |1={{clade
        |label1=[[Waeringopteroidea]]
        |1=[[Waeringopteridae]] }}
        |2={{clade
         |label1=[[Pterygotoidea]]
         |1={{clade
          |1=[[Hunanopteridae]]
          |2={{clade
           |1=[[Hughmilleriidae]]
           |2={{clade
            |1=[[Herefordopteridae]]
            |2={{clade
             |1=[[Slimoniidae]]
             |2={{clade
              |1=[[Ciurcopteridae]]
              |2=[[Pterygotidae]] }} }} }} }} }}
         |label2=[[Adelophthalmoidea]]
         |2={{clade
          |1=[[Nanahughmilleriidae]]
          |2={{clade
           |1=[[Parahughmilleriidae]]
           |2={{clade
            |1=[[Pittsfordipteridae]]
            |2=[[Adelophthalmidae]] }} }} }} }} }} }} }} }} }} }} }} }} }}

==See also==
{{Portal|Arthropods|Palaeontology}}
* [[List of eurypterid genera]]
* [[Nepidae]]—an unrelated family of insects, commonly known as "water scorpions".
* [[Cottidae]]—family of fishes in which some members contain "sea scorpion" in their common name.
* [[History of life]]

== References ==

===Citations===
{{Reflist|20em}}

===Bibliography===
{{Refbegin|40em}}
*{{Cite book|title=Evolution|last1=Bergstrom|first1=Carl T.|publisher=Norton|year=2012|isbn=978-0393913415|url=https://books.google.com/books?id=SeaEZwEACAAJ|last2=Dugatkin|first2=Lee Alan}}
*{{Cite journal|last1=Braddy|first1=Simon J.|last2=Dunlop|first2=Jason A.|date=1997|title=The functional morphology of mating in the Silurian eurypterid, ''Baltoeurypterus tetragonophthalmus'' (Fischer, 1839) |journal=Zoological Journal of the Linnean Society|volume=120|issue=4|pages=435–461|doi=10.1111/j.1096-3642.1997.tb01282.x|issn=0024-4082|doi-access=free}}
*{{Cite journal|last1=Braddy|first1=Simon J.|last2=Almond|first2=John E.|date=1999|title=Eurypterid trackways from the Table Mountain Group (Ordovician) of South Africa|journal=Journal of African Earth Sciences |volume=29 |issue=1|pages=165–177|doi=10.1016/S0899-5362(99)00087-1|bibcode=1999JAfES..29..165B}}
*{{Cite journal|last1=Braddy|first1=Simon J.|last2=Poschmann|first2=Markus|last3=Tetlie|first3=O. Erik |date=2008|title=Giant claw reveals the largest ever arthropod|journal=Biology Letters|volume=4|issue=1 |pages=106–109 |doi=10.1098/rsbl.2007.0491|pmc=2412931|pmid=18029297}}
*{{Cite journal|last1=Brezinski|first1=David K.|last2=Kollar|first2=Albert D.|date=2016|title=Reevaluation of the Age and Provenance of the Giant ''Palmichnium kosinskiorum'' Eurypterid Trackway, from Elk County, Pennsylvania|journal=Annals of Carnegie Museum|volume=84|issue=1|pages=39–45|doi=10.2992/007.084.0105|s2cid=90662577}}
*{{Cite journal|last=Briggs|first=Derek E. G.|date=1985|title=Gigantism in Palaeozoic arthropods|url=https://www.palass.org/publications/special-papers-palaeontology/archive?number=33|journal=Special Papers in Palaeontology|volume=33|pages=157–158}}
*{{Cite book|title=Die Organisation der Trilobiten aus ihren lebenden Verwandten entwickelt|last=Burmeister|first=Hermann|publisher=Georg Reimer|year=1843|url=https://www.biodiversitylibrary.org/item/37331}}
*{{Cite book|title=The Eurypterida of New York|last1=Clarke|first1=John Mason|last2=Ruedemann|first2=Rudolf|publisher=University of California Libraries|year=1912|isbn=978-1125460221|url=https://en.wikisource.org/wiki/The_Eurypterida_of_New_York/Volume_1/Eurypteridae}}
*{{Cite book|title=World Spider Catalog|last1=Dunlop|first1=Jason A.|publisher=Natural History Museum Bern|year=2018|last2=Penney|first2=David|last3=Jekel|first3=Denise|chapter=A summary list of fossil spiders and their relatives|chapter-url=http://www.wsc.nmbe.ch/resources/fossils/Fossils18.5.pdf}}
*{{Cite book|title=Mass Extinctions and Their Aftermath|last1=Hallam|first1=Anthony|last2=Wignall|first2=Paul B.|publisher=Oxford University Press|year=1997|isbn=978-0198549161|url=https://books.google.com/books?id=06yrErJt_NsC&q=eurypterid}}
*{{Cite journal|last1=Hanken|first1=Nils-Martin|last2=Størmer|first2=Leif|date=1975|title=The trail of a large Silurian eurypterid|url=https://foreninger.uio.no/ngf/FOS/pdfs/F%26S_04_p255.pdf|journal=Fossils and Strata|volume=4|pages=255–270|doi=10.18261/8200049639-1975-16|isbn=82-00-04963-9}}
*{{Cite book|title=Experimental Approaches to Understanding Fossil Organisms: Lessons from the Living|last1=Hembree|first1=Daniel I.|last2=Platt|first2=Brian F.|first3=Jon J.|last3=Smith|year=2014|publisher=Springer Science & Business|isbn=978-9401787208|url=https://books.google.com/books?id=zwfFBAAAQBAJ&q=eurypterid+feeding}}
*{{Cite journal|last=Henderson|first=John|date=1866|title=IV. Notice of ''Slimonia Acuminata'', from the Silurian of the Pentland Hills|journal=Transactions of the Edinburgh Geological Society|volume=1|issue=1|pages=15–18|doi=10.1144/transed.1.1.15|s2cid=131539776|url=https://zenodo.org/record/1872903}}
*{{Cite journal|last=Kingsley|first=John Sterling|date=1894|title=The Classification of the Arthropoda|journal=The American Naturalist|volume=28|pages=118–135|issue=326|jstor=2452113|doi=10.1086/275878|bibcode=1894ANat...28..118K |s2cid=83826460}}
*{{Cite journal|last=Kjellesvig-Waering|first=Erik N.|date=1961|title=The Silurian Eurypterida of the Welsh Borderland|journal=Journal of Paleontology|volume=35|issue=4|pages=789–835|jstor=1301214}}
*{{Cite journal|last=Kjellesvig-Waering|first=Erik N.|date=1964|title=A Synopsis of the Family Pterygotidae Clarke and Ruedemann, 1912 (Eurypterida)|journal=Journal of Paleontology|volume=38|issue=2|pages=331–361 |jstor=1301554}}
*{{Cite journal|last1=Kraus|first1=Otto|last2=Brauckmann|first2=Carsten|date=2003|title=Fossil giants and surviving dwarfs. Arthropleurida and Pselaphognatha (Atelocerata, Diplopoda): characters, phylogenetic relationships and construction|url=https://eurekamag.com/research/022/674/022674152.php|journal=Verhandlungen des Naturwissenschaftlichen Vereins in Hamburg|volume=40|pages=5–50}}
*{{Cite journal|last1=Kues|first1=Barry S.|date=1981|title=A Large Assemblage of a New Eurypterid from the Red Tanks Member, Madera Formation (Late Pennsylvanian-Early Permian) of New Mexico|journal=Journal of Paleontology |volume=55|pages=709–729|last2=Kietzke|first2=Kenneth K.|issue=4|jstor=1304420}}
*{{Cite journal|last=Lamsdell|first=James C.|date=2025|title=Codex Eurypterida: A Revised Taxonomy Based on Concordant Parsimony and Bayesian Phylogenetic Analyses|journal=Bulletin of the American Museum of Natural History|volume=2025|issue=473|pages=1–196|doi=10.1206/0003-0090.473.1.1}}
*{{Cite journal|last1=Lamsdell|first1=James C.|last2=Braddy|first2=Simon J.|date=2009|title=Cope's Rule and Romer's theory: patterns of diversity and gigantism in eurypterids and Palaeozoic vertebrates|journal=Biology Letters |volume=6|issue=2|pages=265–269|doi=10.1098/rsbl.2009.0700|pmc=2865068|pmid=19828493}}
*{{Cite journal|last1=Lamsdell|first1=James C.|last2=Braddy|first2=Simon J.|date=2009|title=Redescription of ''Drepanopterus abonensis'' (Chelicerata: Eurypterida: Stylonurina) from the late Devonian of Portishead, UK |journal=Palaeontology|volume=52|issue=5|pages=1113–1139|doi=10.1111/j.1475-4983.2009.00902.x|first3=O. Erik|last3=Tetlie|bibcode=2009Palgy..52.1113L |s2cid=129243775 |issn=1475-4983}}
*{{Cite journal|last1=Lamsdell|first1=James C.|last2=Braddy|first2=Simon J.|date=2010|title=The systematics and phylogeny of the Stylonurina (Arthropoda: Chelicerata: Eurypterida)|journal=Journal of Systematic Palaeontology |volume=8|issue=1|pages=49–61|doi=10.1080/14772011003603564|first3=O. Erik|last3=Tetlie|s2cid=85398946|issn=1478-0941|doi-access=free|bibcode=2010JSPal...8...49L }}
*{{Cite journal|title=Air Breathing in an Exceptionally Preserved 340-Million-Year-Old Sea Scorpion|first1=James C.|last1=Lamsdell|first2=Victoria E.|last2=McCoy|first3=Opal A.|last3=Perron-Feller|first4=Melanie J. |last4=Hopkins|journal=[[Current Biology]]|volume=30|pages=4316–4321|year=2020|issue=21|doi=10.1016/j.cub.2020.08.034|pmid=32916114|s2cid=221590821|doi-access=free|bibcode=2020CBio...30E4316L }}
*{{Cite journal|last=Lamsdell|first=James C.|date=2012|title=Revised systematics of Palaeozoic 'horseshoe crabs' and the myth of monophyletic Xiphosura|journal=Zoological Journal of the Linnean Society|volume=167|pages=1–27 |doi=10.1111/j.1096-3642.2012.00874.x|doi-access=free}}
*{{Cite journal|last1=Lamsdell|first1=James C.|last2=Selden|first2=Paul|date=2013|title=Babes in the wood – a unique window into sea scorpion ontogeny|journal=[[BMC Evolutionary Biology]]|volume=13|issue=98 |doi=10.1186/1471-2148-13-98|page=98|pmid=23663507|pmc=3679797 |doi-access=free |bibcode=2013BMCEE..13...98L }}
*{{Cite book|title=Selectivity in the evolution of Palaeozoic arthropod groups, with focus on mass extinctions and radiations: a phylogenetic approach|last=Lamsdell|first=James C.|publisher=University of Kansas|year=2014|url=https://kuscholarworks.ku.edu/handle/1808/14519}}
*{{Cite journal|last1=Lamsdell|first1=James C.|last2=Briggs|first2=Derek E. G.|last3=Liu|last4=Witzke |first3=Huaibao|first4=Brian J.|last5=McKay|first5=Robert M.|date=2015|title=The oldest described eurypterid: a giant Middle Ordovician (Darriwilian) megalograptid from the Winneshiek Lagerstätte of Iowa|journal=[[BMC Evolutionary Biology]]|volume=15|issue=169|pages=169 |doi=10.1186/s12862-015-0443-9 |pmc=4556007|pmid=26324341 |doi-access=free |bibcode=2015BMCEE..15..169L }}
*{{Cite journal|last=Lankester|first=E. Ray|date=1886|title=Professor Claus and the classification of the Arthropoda|journal=Annals and Magazine of Natural History|volume=17|issue=100|pages=364–372|doi=10.1080/00222938609460154|url=https://www.biodiversitylibrary.org/partpdf/52287}}
*{{Cite journal|last=M'Coy|first=Frederick|date=1849|title=XLI.—On the classification of some British fossil Crustacea, with notices of new forms in the University Collection at Cambridge|journal=Annals and Magazine of Natural History|volume=4|issue=24|pages=392–414|doi=10.1080/03745486009494858|url=https://zenodo.org/record/1752854}}
*{{Cite journal|last1=McCoy|first1=Victoria E.|last2=Lamsdell|first2=James C.|last3=Poschmann |last4=Anderson|first3=Markus|first4=Ross P.|last5=Briggs|first5=Derek E. G.|date=2015|title=All the better to see you with: eyes and claws reveal the evolution of divergent ecological roles in giant pterygotid eurypterids|journal=Biology Letters|volume=11|issue=8|pages=20150564|doi=10.1098/rsbl.2015.0564|pmc=4571687|pmid=26289442}}
*{{Cite book|title=Fossil Ecosystems of North America: A Guide to the Sites and their Extraordinary Biotas|last1=Nudds|first1=John R.|publisher=Manson Publishing|year=2008|isbn=978-1-84076-088-0|url=https://books.google.com/books?id=_z-ca7JAVJIC&pg=PA78|last2=Selden|first2=Paul}}
*{{Cite journal|last=O'Connell|first=Marjorie|date=1916|title=The Habitat of the Eurypterida|url=https://en.wikisource.org/wiki/The_Habitat_of_the_Eurypterida|journal=The Bulletin of the Buffalo Society of Natural Sciences|volume=11|issue=3|pages=1–278}}
*{{Cite journal|last1=Ortega-Hernández|first1=Javier|last2=Legg|first2=David A.|date=2012|title=The phylogeny of aglaspidid arthropods and the internal relationships within Artiopoda|journal=[[Cladistics (journal)|Cladistics]]|volume=29|pages=15–45|doi=10.1111/j.1096-0031.2012.00413.x|issn=1502-3931|first3=Simon J.|last3=Braddy|issue=1|pmid=34814371|s2cid=85744103}}
*{{Cite journal|last1=Plotnick|first1=Roy E.|last2=Baumiller|first2=Tomasz K.|date=1988|title=The pterygotid telson as a biological rudder|journal=Lethaia|volume=21|issue=1|pages=13–27 |doi=10.1111/j.1502-3931.1988.tb01746.x |bibcode=1988Letha..21...13P |issn=1502-3931}}
*{{Cite journal|last1=Poschmann|first1=Markus|last2=Rozefelds|first2=Andrew|date=2021-11-30|title=The last eurypterid – a southern high-latitude record of sweep-feeding sea scorpion from Australia constrains the timing of their extinction|journal=Historical Biology|volume=34 |issue=10 |pages=2020–2030|doi=10.1080/08912963.2021.1998033|s2cid=252467508|issn=0891-2963}}
*{{Cite journal|last1=Poschmann|first1=Markus|last2=Tetlie|first2=O. Erik|date=2004|title=On the Emsian (Early Devonian) arthropods of the Rhenish Slate Mountains: 4. The eurypterids ''Alkenopterus'' and ''Vinetopterus'' n. gen. (Arthropoda: Chelicerata)|journal=Senckenbergiana Lethaea|volume=84|issue=1–2|pages=173–193|doi=10.1007/BF03043470|s2cid=127313845}}
*{{Cite journal|last=Selden|first=Paul|date=1985|title=Eurypterid respiration|url=http://www.paulselden.net/uploads/7/5/3/2/7532217/euryresp.pdf|journal=Philosophical Transactions of the Royal Society B: Biological Sciences|volume=309|issue=1138|pages=219–226|doi=10.1098/rstb.1985.0081|bibcode=1985RSPTB.309..219S}}
*{{Cite journal|last=Selden|first=Paul|date=1999|title=Autecology of Silurian Eurypterids|url=http://homepage.mac.com/paulselden/Sites/Website/Autecology.pdf|journal=Special Papers in Palaeontology|volume=32|pages=39–54|url-status=dead|issn=0038-6804|archive-url=https://web.archive.org/web/20110803072653/http://homepage.mac.com/paulselden/Sites/Website/Autecology.pdf|archive-date=August 3, 2011}}
*{{Cite book|title=Treatise on Invertebrate Paleontology, Part P Arthropoda 2, Chelicerata|last=Størmer|first=Leif|publisher=University of Kansas Press|year=1955|chapter=Merostomata|asin=B0043KRIVC|title-link=Treatise on Invertebrate Paleontology}}
*{{Cite journal|last=Tetlie|first=O. Erik|date=2006|title=Two new Silurian species of ''Eurypterus'' (Chelicerata: Eurypterida) from Norway and Canada and the phylogeny of the genus|url=http://www.museunacional.ufrj.br/mndi/Aracnologia/Eurypterida/Tetlie%202006%20Silurian%20Eurypterus.pdf|journal=Journal of Systematic Palaeontology|volume=4|issue=4|pages=397–412|doi=10.1017/S1477201906001921|bibcode=2006JSPal...4..397T|s2cid=83519549|issn=1478-0941|access-date=2018-10-09|archive-date=2020-06-06|archive-url=https://web.archive.org/web/20200606161847/http://www.museunacional.ufrj.br/mndi/Aracnologia/Eurypterida/Tetlie%202006%20Silurian%20Eurypterus.pdf|url-status=dead}}
*{{Cite journal|last1=Tetlie|first1=O. Erik|last2=Van Roy|first2=Peter|date=2006|title=A reappraisal of ''Eurypterus dumonti'' Stainier, 1917 and its position within the Adelophthalmidae Tollerton, 1989|url=http://www.vliz.be/imisdocs/publications/255340.pdf|journal=Bulletin de l'Institut Royal des Sciences Naturelles de Belgique|volume=76|pages=79–90}}
*{{Cite journal|last=Tetlie|first=O. Erik|date=2007|title=Distribution and dispersal history of Eurypterida (Chelicerata)|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|volume=252|issue=3–4|pages=557–574 |doi=10.1016/j.palaeo.2007.05.011|bibcode=2007PPP...252..557T |issn=0031-0182}}
*{{Cite journal|last1=Tetlie|first1=O. Erik|last2=Cuggy|first2=Michael B.|date=2007|title=Phylogeny of the basal swimming eurypterids (Chelicerata; Eurypterida; Eurypterina)|journal=Journal of Systematic Palaeontology |volume=5|issue=3|pages=345–356 |doi=10.1017/S1477201907002131|bibcode=2007JSPal...5..345T |s2cid=88413267}}
*{{Cite journal|last1=Tetlie|first1=O. Erik|last2=Rábano|first2=Isabel|date=2007|title=Specimens of ''Eurypterus'' (Chelicerata, Eurypterida) in the collections of Museo Geominero (Geological Survey of Spain), Madrid|url=http://www.igme.es/internet/Boletin/2007/118_1_2007/ART.%209.pdf|journal=Boletín Geológico y Minero|volume=118|issue=1|pages=117–126|issn=0366-0176|archive-url=https://web.archive.org/web/20110722131826/http://www.igme.es/internet/Boletin/2007/118_1_2007/ART.%209.pdf|archive-date=July 22, 2011|url-status=dead}}
*{{Cite journal|last=Tetlie|first=O. Erik|date=2008|title=''Hallipterus excelsior'', a Stylonurid (Chelicerata: Eurypterida) from the Late Devonian Catskill Delta Complex, and Its Phylogenetic Position in the Hardieopteridae|journal=Bulletin of the Peabody Museum of Natural History|volume=49|issue=1|pages=19–30|doi=10.3374/0079-032X(2008)49[19:HEASCE]2.0.CO;2|s2cid=85862868 }}
*{{Cite journal|last1=Tetlie|first1=O. Erik|last2=Briggs|first2=Derek E. G.|date=2009|title=The origin of pterygotid eurypterids (Chelicerata: Eurypterida)|journal=Palaeontology|volume=52|issue=5|pages=1141–1148 |doi=10.1111/j.1475-4983.2009.00907.x|bibcode=2009Palgy..52.1141T |issn=0024-4082|doi-access=|s2cid=84268058 }}
*{{Cite journal|last=Tollerton|first=Victor P.|date=1989|title=Morphology, Taxonomy, and Classification of the Order Eurypterida Burmeister, 1843|journal=Journal of Paleontology|volume=63|issue=5|pages=642–657 |jstor=1305624|doi=10.1017/S0022336000041275|bibcode=1989JPal...63..642T |s2cid=46953627 }}
*{{Cite journal|last1=Van Roy|first1=Peter|last2=Briggs|first2=Derek E. G.|last3=Gaines|first3=Robert R.|date=2015|title=The Fezouata fossils of Morocco; an extraordinary record of marine life in the Early Ordovician|url=http://jgs.lyellcollection.org/content/early/2015/06/29/jgs2015-017|journal=Journal of the Geological Society|volume=172|issue=5|pages=541–549|doi=10.1144/jgs2015-017|issn=0016-7649|bibcode=2015JGSoc.172..541V|s2cid=129319753|hdl=1854/LU-8714212|hdl-access=free}}
*{{Cite journal|last1=Vrazo|first1=Matthew B.|last2=Ciurca|first2=Samuel J. Jr.|date=2017|title=New trace fossil evidence for eurypterid swimming behaviour|journal=Palaeontology|volume=61|issue=2 |pages=235–252 |doi=10.1111/pala.12336|s2cid=133765946|doi-access=free}}
*{{Cite journal|last=White|first=David|date=1927|title=Flora of the Hermit Shale, Grand Canyon, Arizona |journal=Proceedings of the National Academy of Sciences of the United States of America|volume=13 |issue=8|pages=574–575 |doi=10.1073/pnas.13.8.574|pmid=16587225|pmc=1085121|doi-access=free}}
*{{Cite journal|last=Whyte|first=Martin A.|date=2005|title=A gigantic fossil arthropod trackway|journal=[[Nature (journal)|Nature]]|volume=438|issue=7068|pages=576 |doi=10.1038/438576a|pmid=16319874 |bibcode=2005Natur.438..576W|s2cid=4422644|doi-access=free}}
*{{Cite journal|last=Woodward|first=Henry|date=1865|title=On some New Species of Crustacea belonging to the Order Eurypterida|journal=Quarterly Journal of the Geological Society|volume=21|issue=1–2|pages=484–486 |doi=10.1144/GSL.JGS.1865.021.01-02.52|s2cid=129427356}}
{{Refend}}

====Websites====
* {{cite web|url=http://www.palaeos.com/Invertebrates/Arthropods/Chelicerata/Eurypterida/Eurypterida.html|title=Palaeos - Eurypterida|first=M. Alan|last=Kazlev|date=2002|website=www.palaeos.com|language=en|archive-url=https://web.archive.org/web/20070813065212/http://www.palaeos.com/Invertebrates/Arthropods/Chelicerata/Eurypterida/Eurypterida.html|archive-date=13 August 2007|ref=CITEREFPalaeos}}

==External links==
{{Commons category|Eurypterida}}
{{Wikisource portal|Eurypterids}}
{{Wikispecies|Eurypterida}}
{{Wiktionary|eurypterid}}
* [https://web.archive.org/web/20111009021215/http://www.eurypterids.co.uk/ Eurypterids.co.uk] – An online resource of eurypterid data and research
* [https://web.archive.org/web/20170222113755/http://www.eurypterid.net/index.html eurypterid.net]

{{Eurypterida}}
{{Taxonbar|from=Q19436}}
{{Authority control}}


[[Category:Prehistoric_chelicerates]]
[[Category:Eurypterida]]
[[Category:Chelicerate orders]]
[[Category:Darriwilian first appearances]]
[[Category:Lopingian extinctions]]
[[Category:Apex predators]]