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Eurypterina is one of two of , an extinct group of commonly known as "sea scorpions". Eurypterine eurypterids are sometimes informally known as "swimming eurypterids". They are known from fossil deposits worldwide, though primarily in and .

Seventy-five percent of species are eurypterines; this represents 99% of specimens. The superfamily is the most species-rich clade, with 56 species, followed by the Adelophthalmoidea with 43 species; as , they comprise the most derived eurypterines. includes the , which are the only eurypterids known to have a cosmopolitan distribution.

Though more numerous both in specimens and taxa, the eurypterines have the shorter temporal range of the two eurypterid suborders. They first appeared around the same time as the in the Middle Ordovician. The suborder faced a slow extinction during the and , possibly tied to the emergence of jawed vertebrates. Every Eurypterine genus and lineage went extinct before the save for which would go extinct in the , millions of years before the Permian-Triassic extinction event that ended the stylonurines.


Description
The and Eurypterina are most easily distinguished by the morphology of the posteriormost prosomal appendage. In the Stylonurina, this appendage takes the form of a long and slender walking leg, lacking a modified spine (termed podomere 7a). In the Eurypterina, the leg is most usually modified and broadened into a swimming paddle and always includes a podomere 7a.

Swimming eurypterines represent the absolute majority of both known species and known specimens, though the morphology of the walking is almost as diverse in appearance, and the fossil record of the eurypterines may therefore simply be more complete than that of the stylonurines, possibly due to varying habitat preferences.


Paleobiogeography
The most basal eurypterines with swimming legs, the genus , are known from the east coast of close to the equator (a region that today is South Africa) from the Late Ordovician. It is not known whether or not the swimming forms originated here or not, but it is speculated that they migrated from , since most and basal swimming forms are predominantly known from Laurentia and Gondwana otherwise completely lacks basal swimming forms.

The were likely the first major successful group of eurypterids, evidenced by a radiation. All known members of the Megalograptoidea are from the Middle to Late of Laurentia, though potential records from the of are known in the form of the genus (though its classification as a megalograptoid is questionable).

are known from Laurentia and Baltica, with one known species from . and other eurypteroids appear to have been unable to spread beyond waters. The genus Eurypterus in particular dominated many eurypterid faunas of Laurentia. Despite its abundance, it appears to not have originated in Laurentia, the earliest records of the genus are from Baltica and Eurypterus was thus likely an in Laurentia, albeit one that managed to adapt well to the new habitats.

The majority of carcinosomatoid taxa are also known from Laurentia, Baltica and Avalonia. Isolated and fragmentary fossils from the of and the show that the of Annamia and Perunica were within the geographical range of the carcinosomatoids. Only a few basal carcinosomatoids (e.g. and ) have been found in deeper waters whilst the more derived forms, such as and have not. Basal carcinosomatoids () are likely responsible for the fossil remains in Vietnam and the Czech Republic and may have had a distribution similar to the cosmopolitan distribution of the , though were not as common nor as successful.

Adelophthalmoids were the longest lasting clade of eurypterines, becoming extinct in the , this is in part due to the survival of Adelophthalmus beyond the . The earliest records of the genus are from the of western , but following the amalgamation of during the and , the genus gained an almost cosmopolitan distribution. The basalmost species in the entire clade are from and most of the evolution within the basal members took place in . By the Devonian, representatives were found in both and long before the formation of Pangaea.

Although the only existed for a period of about 40 million years during a time when most continents were widely separated, the clade is the eurypterid clade with the most cosmopolitan distribution. Like other eurypterines, they are most common in Laurentia, Baltica and Avalonia, but are also found commonly in other . Fossil remains have been recovered from , , , , , , Iberia, , vast swaths of , and . The earliest pterygotioids are from the latest Llandovery of , Laurentia and and this mobility makes it difficult to pinpoint the geographical origin of the clade, though it is speculated to have been close to or in Laurentia like the Adelophthalmoidea.


Systematics and relationships
Eurypterina contains eight superfamilies - Onychopterelloidea, , , , Carcinosomatoidea, Waeringopteroidea, Adelophthalmoidea and . The relationships between them remain somewhat unclear, the is thought to be relatively primitive (between and the ) because they lack a of all more derived swimming forms; the modified distal margin of the sixth podomere of the swimming leg. This position is not necessarily true, since the sixth podomere in the swimming leg resembles the reduced podomere found in the , and they might instead belong between the Eurypteroidea and Carcinosomatoidea.

In contrast to the Megalograptoidea, the is a rather well-known clade that contains around 90% of all known eurypterid specimens. They were closely related, supported by numerous similarities, to the Carcinosomatoidea. The Carcinosomatoidea have a poorly resolved internal phylogeny, though can be easily recognised by -like appearance and heavily spinose appendages.

and Adelophthalmoidea are the two most derived clades as well as the most taxonomically diverse ones. Adelophthalmoidea contains 43 species, whereas Pterygotioidea contains 56. The superfamilies classified as part of Eurypterina contain the following families:'', a . At a length of 2.5 meters, it is one of the largest to have ever lived.]] Suborder Eurypterina Burmeister, 1843


Phylogeny
Eurypterines are characterised by the transformation of the posteriormost prosomal appendage into a swimming paddle, one of the main features used to distinguish them from the . The cladogram presented below, simplified from a study by Tetlie, showcases the phylogenetic relationships of the Eurypterina based on this adaptation, and the enlargement of the , which characterises the family , to be used for active prey capture.


See also

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