Eurypterid

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Eurypterida
Temporal range: OrdovicianPermian
Haeckel Eurypterus tetragonophthalmus.jpg
Eurypterid from Ernst Haeckel's Kunstformen der Natur (1904)
Scientific classification
Kingdom: Animalia
Phylum: Arthropoda
Subphylum: Chelicerata
Class: Merostomata
Order: Eurypterida
Burmeister, 1843
Suborders

Stylonurina Diener, 1924
Eurypterina Burmeister, 1843

Eurypterids (sea scorpions) are an extinct group of arthropods that are related to arachnids and include the largest known arthropods to have ever lived. They are members of the extinct order Eurypterida (Chelicerata); which is the most diverse Paleozoic chelicerate order in terms of species.[1] The name Eurypterida comes from the Greek words eury- (meaning "broad" or "wide") and pteron (meaning "wing").[2] This name was chosen due to the pair of wide swimming appendages on the first fossil eurypterids discovered. The largest, such as Jaekelopterus, reached 2.5 metres (8 ft 2 in) in length, but most species were less than 20 centimetres (8 in). They were formidable predators that thrived in warm shallow water, in both seas and lakes,[3] from the mid Ordovician to late Permian (460 to 248 million years ago).

Although informally called "sea scorpions", only the earliest ones were marine (later ones lived in brackish or freshwater), and they were not true scorpions. According to theory, the move from the sea to fresh water had probably occurred by the Pennsylvanian subperiod. Eurypterids are believed to have undergone ecdysis, making their significance in ecosystems difficult to assess, because it can be difficult to tell a fossil moult from a true fossil carcass.[4] They went extinct during the Permian–Triassic extinction event 252.17 million years ago. Their fossils have a near global distribution.

About two dozen families of eurypterids are known. Perhaps the best-known genus of eurypterid is Eurypterus, of which around 16 fossil species are known. The genus Eurypterus was described in 1825 by James Ellsworth De Kay, a zoologist. He recognized the arthropod nature of the first-ever described eurypterid specimen, found by Dr. S. L. Mitchill. In 1984, that species, Eurypterus remipes was named the state fossil of New York.

Body structure[edit]

Eurypterus model, exhibited in Smithsonian National Museum of Natural History: Hall of Fossils

Eurypterids have been formally described as follows:[5]

"Small to very large merostomes with elongate lanceolate, rarely trilobed body; prosoma [head] of moderate size; opisthosoma [body] with 12 moveable segments and styliform to spatulate telson [tail], with division commonly into 7-segmented preabdomen and 5-segmented postabdomen; prosomal [head] appendages 6, comprising 3-jointed chelicerae, walking legs, the last pair commonly transformed into swimming legs. Mouth central, bordered posteriorly by endostoma and metastoma. Operculum with median genital appendage, abdominal appendages plate-shaped with nonlaminate gills. Ordovician-Permian."

The typical eurypterid had a large, flat, semicircular carapace, followed by a jointed section, and finally a tapering, flexible tail, most ending with a long spine at the end (Pterygotus, though, had a large flat tail, possibly with a smaller spine). Behind the head, eurypterids had twelve body segments, each of which was formed from a dorsal plate (tergite) and a ventral plate (sternite). The tail, known as the telson, is spiked in most eurypterids (just like in modern scorpions) and in some species it may have been used to inject venom, but so far there is no certain evidence that any eurypterids were venomous. Most eurypterids have paddles toward the end of the carapace and beyond, which were used to propel themselves through water. The suborder Stylonurina have walking legs instead of paddles. Some argue that the paddles were also used for digging. Underneath, in addition to the pair of swimming appendages, the creature had four pairs of jointed legs for walking, and two claws at the front, chelicerae, which were enlarged in pterygotids. The walking legs had odd hairs, similar to modern day crabs. Other features, common to ancient and modern arthropods of this type, include one pair of compound eyes and a pair of smaller eyes, called ocelli, located between the other larger pair of eyes.

Megarachne, a eurypterid closely related to Hibbertopterus from the Late Carboniferous

Many eurypterids had legs large and long enough to do more than allow them to crawl over the sea bottom; a number of species (particularly hibbertopterids) had large stout legs, and were probably capable of terrestrial locomotion (like land crabs today). Studies of what are believed to be their trackways indicate that eurypterids used in-phase, hexapodous (six-legged) and octopodous (eight-legged) gaits.[6] Some species may have been amphibious, emerging onto land for at least part of their life cycle; they may have been capable of breathing both in water and in air. A predatory arthropod known as Protichnites,[7] whose traces are found in Cambrian strata dating from 510 million years ago, is a possible stem group eurypterid, and is among the first evidence of animals on land.[8]

The largest sea-scorpion and the largest known arthropod ever to have lived is Jaekelopterus rhenaniae, supported by the finding of a 46 cm (18 in) long claw in 2007, indicating a body length of 2.5 m (8 ft 2 in).[9]

Relationships with other groups[edit]

The perception of the horseshoe crab as a modern sea scorpion is easy to understand given their physical similarities.

Eurypterids have traditionally been regarded as close relatives of horseshoe crabs, together forming a group called Merostomata. Subsequent studies placed eurypterids closer to the arachnids in a group called Metastomata.[10] There has also been a prevailing idea that eurypterids are closely related to scorpions, which they resemble.[11] This hypothesis is reflected in the common name "sea scorpion". More recently it has been recognised that a little-known, extinct group called Chasmataspida also shares features with Eurypterida,[12] and the two groups were sometimes confused with one another. The most recent summary of the relationships between arachnids and their relatives recognised Eurypterida, Xiphosura and Arachnida as three major groups, but was not able to resolve the phylogenetic relationship of any shared details between them.[13]

List of families and genera[edit]

Mixopterus, a eurypterid of the Silurian
Eurypterus, the most commonly found eurypterid fossil and the first eurypterid genus to be described
Eurypterus fossil from the Bertie Waterlime (Upper Silurian) of New York.
A fossil of Jaekelopterus rhenaniae. At 2.5 m (8.2 ft) long, it is one of the two largest arthropods to have ever lived (the other being the land-living myriapod Arthropleura).

There are 246 valid species of eurypterids as of 2011. All of them are extinct. They are grouped into the following:[14]

Suborder Stylonurina Diener, 1924
Suborder Eurypterina Burmeister, 1843

The trace fossil trackways produced by eurypterids are placed in the ichnogenus Palmichnium.[15]

Phylogeny[edit]

Genera found in New York, illustrated by Charles R. Knight

The cladogram presented here is simplified from a study by Tetlie.[16] The most important phylogenetic breakdown is based on the two major innovations that characterise the evolution of the eurypterids. The most important was the transformation of the posteriormost prosomal appendage into a swimming paddle (as found in the clade Eurypterina). The second innovation was the enlargement of the chelicerae, (as found in the family Pterygotidae), allowing these appendages to be used for active prey capture.

75% of eurypterid species are eurypterines; this represents 99% of specimens.[1] The superfamily Pterygotioidea is the most species-rich clade, with 56 species, followed by the Adelophthalmoidea with 43 species; as sister taxa, they comprise the most derived eurypterids. Pterygotioidea includes the pterygotids, which are the only eurypterids to have a cosmopolitan distribution.[16] This clade is one of the best supported within the eurypterids.

It has been suggested that the development of dermal armour in certain groups of jawless vertebrates (such as the Heterostraci and the Osteostraci) is in response to predation pressure by increasingly sophisticated eurypterid predators[17] (specifically the pterygotids) although this has yet to be verified by detailed analysis.[18] An increase in fish diversity is tied to a decline in eurypterid diversity in the Lower Devonian,[19] although it is not thought that this represents competitive replacement; in fact, this is rare in the fossil record.[20]

Eurypterida


Stylonurina[Note 1]



Eurypterina

Megalograptoidea[Note 2]




Eurypteroidea




Mixopteroidea




Waeringopteroidea




Adelopthalmoidea


Pterygotioidea

Hughmilleria




Herefordopterus




Slimonia




Pterygotidae












  1. ^ The position of the stylonurids is highly uncertain, as noted by Tetlie.[16] [18]
  2. ^ The position of the megalograptids is uncertain.

See also[edit]

References[edit]

  1. ^ a b Dunlop, J. A.; D. Penney; O. E. Tetlie; L. I. Anderson (2008). "How many species of fossil arachnids are there?". Journal of Arachnology 36 (2): 267–272. doi:10.1636/CH07-89.1. ISSN 0161-8202. 
  2. ^ Webster's New Universal Unabridged Dictionary. 2nd ed. 1979.
  3. ^ Joseph T. Hannibal, Spencer G. Lucas, Allan J. Lerner & Dan S. Chaney (2005). An eurypterid (Adelophthalmus sp.) from a plant-rich lacustrine facies of Upper Pennsylvanian strata in El Cobre Canyon, New Mexico (PDF). In S. G. Lucas, K. E. Zeigler & J. A. Spielmann. "The Permian of Central New Mexico". New Mexico Museum of Natural History and Science Bulletin 31: 34–38. 
  4. ^ Brandt, Danita; McCoy, Victoria (2009). "Scorpion taphonomy: criteria for distinguishing fossil scorpion molts and carcasses". Journal of Arachnology 37 (3): 312. doi:10.1636/sh09-07.1. 
  5. ^ L. Størmer (1955). "Merostomata". Treatise on Invertebrate Paleontology, Part P Arthropoda 2, Chelicerata. p. 23. 
  6. ^ Whyte, Martin A. (2005). "Palaeoecology: A gigantic fossil arthropod trackway". Nature 438 (7068): 576–576. doi:10.1038/438576a. PMID 16319874. 
  7. ^ Richard Owen (1852). "Description of the impressions and footprints of the Protichnites from the Potsdam Sandstone of Canada". Quarterly Journal of the Geological Society of London 8: 214–225. doi:10.1144/GSL.JGS.1852.008.01-02.26. 
  8. ^ Lancaster D. Burling (1917). "Protichnites and Climactichnites. A critical study of some Cambrian trails". American Journal of Science 44 (263): 387–398. doi:10.2475/ajs.s4-44.263.387. 
  9. ^ Simon J. Braddy, Markus Poschmann & O. Erik Tetlie (2008). "Giant claw reveals the largest ever arthropod". Biology Letters 4 (1): 106–109. doi:10.1098/rsbl.2007.0491. PMC 2412931. PMID 18029297. 
  10. ^ P. Weygoldt & H. F. Paulus (1979). "Untersuchungen zur Morphologie, Taxonomie und Phylogenie der Chelicerata". Zeitschrift für zoologische Systematik und Evolutionsforschung 17 (2): 85–116, 177–200. doi:10.1111/j.1439-0469.1979.tb00694.x. 
  11. ^ J. Versluys & R. Demoll (1920). "Die Verwandtschaft der Merostomata mit den Arachnida und den anderen Abteilungen der Arthropoda". Koninklijke Akademie van Wetenschappen Amsterdam 23: 739–765. 
  12. ^ O. Erik Tetlie & Simon J. Braddy (2004). "The first Silurian chasmataspid, Loganamaraspis dunlopi gen. et sp. nov. (Chelicerata: Chasmataspidida) from Lesmahagow, Scotland, and its implications for eurypterid phylogeny". Transactions of the Royal Society of Edinburgh: Earth Sciences 94 (3): 227–234. doi:10.1017/S0263593300000638. 
  13. ^ Jeffrey W. Shultz (2007). "A phylogenetic analysis of the arachnid orders based on morphological characters". Zoological Journal of the Linnean Society 150 (2): 221–265. doi:10.1111/j.1096-3642.2007.00284.x. CiteSeerX: 10.1.1.119.850. 
  14. ^ Jason A. Dunlop, David Penney, & Denise Jekel; with additional contributions from Lyall I. Anderson, Simon J. Braddy, James C. Lamsdell, Paul A. Selden, & O. Erik Tetlie (2011). "A summary list of fossil spiders and their relatives". In Norman I. Platnick. The world spider catalog, version 11.5. American Museum of Natural History. Retrieved May 21, 2011. 
  15. ^ Adolf Seilacher (2007). "Arthropod trackways". Trace Fossil Analysis. Springer. pp. 18–31. ISBN 978-3-540-47225-4. 
  16. ^ a b c O. Erik Tetlie (2007). "Distribution and dispersal history of Eurypterida (Chelicerata)" (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology 252 (3–4): 557–574. doi:10.1016/j.palaeo.2007.05.011. 
  17. ^ Romer, A. S. (1933). "Eurypterid influence on vertebrate history". Science 78 (2015): 114–117. doi:10.1126/science.78.2015.114. PMID 17749819. 
  18. ^ a b O. Erik Tetlie & Derek E. G. Briggs (2009). "The origin of pterygotid eurypterids (Chelicerata: Eurypterida)". Palaeontology 52 (5): 1141–1148. doi:10.1111/j.1475-4983.2009.00907.x. 
  19. ^ Briggs, D. E. G.; R. A. Fortey; E. N. K. Clarkson (1988). "Extinction and the fossil record of Arthropods". In G.P. Larwood. Extinction and survival in the fossil record. Oxford [Oxfordshire]: Published for the Systematics Association by Clarendon Press. pp. 171–209. ISBN 0198577087. 
  20. ^ Ridley, Mark (2004). Evolution. Wiley-Blackwell. ISBN 978-1-4051-0345-9. 

Further reading[edit]

External links[edit]