Strabops Temporal range: Furongian, | |
---|---|
S. thacheri type specimen exhibited at the Peabody Museum of Natural History, Connecticut | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Arthropoda |
Order: | † Strabopida |
Family: | † Strabopidae |
Genus: | † Strabops Beecher, 1901 |
Type species | |
†Strabops thacheri Beecher, 1901 |
Strabops is a genus of strabopid, an extinct group of arthropods. Strabops is known from a single specimen from the Late Cambrian (Furongian age) of the Potosi Dolomite, Missouri, collected by a former professor, Arthur Thacher. It is classified in the family Strabopidae of the monotypic order Strabopida, a group closely related to the aglaspidids with uncertain affinities. The generic name is composed by the Ancient Greek words στραβός, meaning "squinting", and ὄψῐς, meaning "face" (and therefore, "squinting face").
The history of Strabops has been turbulent and confusing since its original description by Charles Emerson Beecher, who classified it as a eurypterid. Many authors do not agree with this and have classified Strabops and its allies as part of the Aglaspidida order, while others classify them in their own order. Although the latter is the taxonomic position currently accepted, other paleontologists prefer to simply omit the strabopids from their analyzes due to the poor preservation of their fossils. In addition, it has been suggested that the closely related Paleomerus represents a synonym of Strabops, which are uniquely differentiated by the size of the telson (the posteriormost division of the body) and the position of the eyes.
As the other strabopids, Strabops was a small-sized arthropod, measuring only 11 centimetres (4.3 inches) in length. [1] However, it was the largest of the strabopids, surpassing Paleomerus (9.3 cm, 3.7 in) [2] and Parapaleomerus (9.2 cm, 3.6 in). [3]
Like some other arthropod groups, the strabopids possessed segmented bodies and jointed appendages (limbs) covered in a cuticle composed of proteins and chitin. The arthropod body is divided into two tagmata (sections); the anterior prosoma (head) and posterior opisthosoma (abdomen). The appendages were attached to the prosoma, and although they are unknown in strabopids (except for one undescribed specimen of Parapaleomerus [4] ), it is most likely they owned several pairs of them. [5] Although the chemical composition of the strabopid exoskeleton is unknown, it was probably mineralized (with inorganic substances), [6] sturdy and calcareous (containing calcium). The head of the strabopids was very short, the back was rounded and lacked trilobation (being divided into three lobes), the abdomen was composed by 11 segments and was followed by a thick tail-like spine, the telson. [7] [4]
In the genus Strabops, the prosoma was short and broad, with a rounded outline. The eyes were located in the middle of the front of the prosoma. These were medium-sized, ovate and narrow, and pointed obliquely inwards (hence the name Strabops). Two spots between the eyes indicate the presence of the ocelli (light-sensitive simple eyes). In its abdomen, there were eleven segments, being the third the widest. The ends of the segments were rounded on the sides. In the posterior part of the segments, a row of tiny crenulations was visible. The first six segments were uniform in size, the three following ones were somewhat shorter and the last two were the longest. The telson was a broad, flat spine, and it rose slightly in the middle. [1] The appendages are unknown, although it has been suggested that they be less than seven pairs (what has been considered an overestimate). [8]
Strabops differed only from Paleomerus in the position of the eyes, which were closer together and farther from the margin than in Paleomerus, [6] and the size of the telson, being longer and narrower than in the latter. [8]
Strabops is known by one only well preserved specimen (YPM 9001, housed at the Peabody Museum of Natural History). [9] It was found by Arthur Thacher, a former professor at the Washington University in St. Louis, in the Potosi Dolomite of the St. Francois County, Missouri. The specimen was sent to Yale University, Connecticut. The American paleontologist Charles Emerson Beecher described it as the only Cambrian eurypterid, Strabops thacheri, the generic name derived from the Ancient Greek words στραβός (strabós, squinting) and ὄψῐς (ópsis, face) and refers to the inward turning eyes. He considered Strabops different enough from the other eurypterids to erect a new genus, although he did not assign it to any family. [1] In 1912, the American paleontologists John Mason Clarke and Rudolf Ruedemann assigned Strabops to the Eurypteridae family, as well as affirming the possession of a twelfth segment and changing the position of the eyes from anterolateral (in the middle of the front) to lateral. [10]
In his book Cambrian Merostomata of 1939, the American paleontologist and geologist Gilbert Oscar Raasch considered the descriptions of the joint authorship of 1912 erroneous and agreed with Beecher on all aspects of his description, except for some reservations about the ocelli. Despite its initial classification as a eurypterid, Raasch admitted that the description of Strabops concurred with the old thought of what an aglaspidid was. It is possible that Beecher was unaware of the similarity between it and Aglaspis because of the distorted illustration of the latter by the American zoologist and paleontologist Robert Parr Whitfield. Therefore, Raasch placed Strabops under the family Aglaspididae in the order Aglaspida. [11]
In 1971, the Swedish geologist and paleontologist Jan Bergström tentatively removed Strabopidae (at that time containing Strabops and Neostrabops ) and Paleomeridae (only containing Paleomerus) from the order Aglaspidida based on the fact that the head tagma was too short to accommodate the six pairs of appendages then assumed to be present in aglaspidids. Instead, he classified them in an uncertain order in the Merostomoidea class together with the emeraldellids. Ironically, Bergström speculated that the number of pairs of appendages present in the three genera could be fewer than seven, as well as including a possible antennal segment. [6] This is currently observed as an overestimate. [8] A study published by Derek Ernest Gilmor Briggs et al. in 1979 has shown that Aglaspis spinifer had between four and five pairs of appendages, but not six, weakening Bergström's argument. [12]
In 1997, Bergström and Hou Xian-guang, a Chinese paleontologist, completely removed Strabopidae (recognizing Paleomeridae as a junior synonym), as well as the family Lemoneitidae (containing Lemoneites ), from the order Aglaspidida to erect a new order, Strabopida, this time suggesting a number of no more than two pairs of appendages. However, this new clade (group) remained under the similarly-named Aglaspida subclass. [7] A year later, the British paleontologists Jason Andrew Dunlop and Paul Antony Selden eliminated Strabopida from the suborder Aglaspidida and classified them as the sister taxa of the latter based on the lack of aglaspidid apomorphies (distinctive characteristics), such as the lack of genal spines (a spine placed in the posterolateral part of the prosoma). [9] Other authors have reinforced this argument by the trapezoidal telson form of Paleomerus and Strabops in contrast to the long styliform telson of the aglaspidids. [8] However, some authors prefer to represent the taxonomic position of the strabopids as uncertain due to the poor preservation of their fossils. [13]
Strabops is classified in its own order, Strabopida, [14] in the clade Arachnomorpha, [8] along with Paleomerus, Parapaleomerus and potentially Khankaspis . [14] It was described originally as the only Cambrian eurypterid, [1] and later as an aglaspidid. [11] It would not be until 1997 when the order Strabopida was described, [7] but there is still doubt if the exclusion of them from Aglaspidida was really correct. The current status of the strabopids is of aglaspidid-like arthropods of uncertain affinities. [13]
Strabops shares with the other strabopids a series of characteristics that distinguish them all from the other arthropods. These are an abdomen divided into eleven segments followed by a thick spine, the telson. The head was short with sessile compound eyes. The back was rounded. Like Paleomerus, Strabops possessed prominent dorsal eyes, however, there is no evidence of this in the fossils of Parapaleomerus. [7] [14]
The great similarity that Strabops and Paleomerus share has cast doubt on many authors about whether both genera are really synonymous or not. The Norwegian paleontologist and geologist Leif Størmer described Paleomerus as an intermediate form between Xiphosura (commonly known as horseshoe crabs) and Eurypterida, only highlighting a unique feature different from Strabops, a twelfth segment. [2] Nevertheless, a fourth specimen found in Sweden has shown that this extra segment actually represented the telson of the animal, [8] making them virtually indistinguishable. [9] Although this should convert both genera into synonyms, over time, more differences have been highlighted, such as the position of the eyes (closer to each other and farther from the margin in Strabops than in Paleomerus) [6] and the size of the telson (longer and narrower in Strabops than in Paleomerus), which keeps them as separate but closely related genera. [8]
The cladogram below published by Jason A. Dunlop and Paul A. Selden (1998) is based on the major chelicerate groups (in bold, Aglaspida, Eurypterida and Xiphosurida, Scorpiones and other arachnid clades) and their outgroup taxa (used as a reference group). Strabops and Paleomerus are shown as the sister taxa of Aglaspida. [9]
Note that there are several outdated elements. For example, Lemoneites was remitted to the Glyptocystitida order of echinoderms in 2005. [14]
The type and only known specimen of Strabops has been found in Furongian (Upper Cambrian) deposits in eastern Missouri. [1] Strabops was at least an inhabitant of the sea, if not born in it. In addition, there are two specimens of the marine brachiopod Obolus lamborni and a poorly preserved trilobite head attached to the slab. [15]
Eurypterids, often informally called sea scorpions, are a group of extinct arthropods that form the order Eurypterida. The earliest known eurypterids date to the Darriwilian stage of the Ordovician period 467.3 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 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 251.9 million years ago.
Eurypterus is an extinct genus of eurypterid, a group of organisms commonly called "sea scorpions". The genus lived during the Silurian period, from around 432 to 418 million years ago. Eurypterus is by far the most well-studied and well-known eurypterid. Eurypterus fossil specimens probably represent more than 95% of all known eurypterid specimens.
Hibbertopterus is a genus of eurypterid, a group of extinct aquatic arthropods. Fossils of Hibbertopterus have been discovered in deposits ranging from the Devonian period in Belgium, Scotland and the United States to the Carboniferous period in Scotland, Ireland, the Czech Republic and South Africa. The type species, H. scouleri, was first named as a species of the significantly different Eurypterus by Samuel Hibbert in 1836. The generic name Hibbertopterus, coined more than a century later, combines his name and the Greek word πτερόν (pteron) meaning "wing".
Aglaspidida is an extinct order of aquatic arthropods that were once regarded as primitive chelicerates. However, anatomical comparisons demonstrate that the aglaspidids cannot be accommodated within the chelicerates, and that they lie instead within the Artiopoda, thus placing them closer to the trilobites. Aglaspidida contains the subgroups Aglaspididae and Tremaglaspididae, which are distinguished by the presence of acute/spinose genal angles and a long spiniform tailspine in the Aglaspididae.
Slimonia is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Slimonia have been discovered in deposits of Silurian age in South America and Europe. Classified as part of the family Slimonidae alongside the related Salteropterus, the genus contains three valid species, S. acuminata from Lesmahagow, Scotland, S. boliviana from Cochabamba, Bolivia and S. dubia from the Pentland Hills of Scotland and one dubious species, S. stylops, from Herefordshire, England. The generic name is derived from and honors Robert Slimon, a fossil collector and surgeon from Lesmahagow.
Carcinosoma is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Carcinosoma are restricted to deposits of late Silurian age. Classified as part of the family Carcinosomatidae, which the genus lends its name to, Carcinosoma contains seven species from North America and Great Britain.
Alkenopterus is a genus of prehistoric eurypterid classified as part of the family Onychopterellidae. The genus contains two species, A. brevitelson and A. burglahrensis, both from the Devonian of Germany.
Parahughmilleria is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Parahughmilleria have been discovered in deposits of the Devonian and Silurian age in the United States, Canada, Russia, Germany, Luxembourg and Great Britain, and have been referred to several different species. The first fossils of Parahughmilleria, discovered in the Shawangunk Mountains in 1907, were initially assigned to Eurypterus. It would not be until 54 years later when Parahughmilleria would be described.
Helmetia is an extinct genus of arthropod from the middle Cambrian. Its fossils have been found in the Burgess Shale of Canada and the Jince Formation of the Czech Republic.
Unionopterus is a genus of eurypterid, an extinct group of aquatic arthropods commonly known as "sea scorpions". Fossils have been registered from the Early Carboniferous period. The genus contains only one species, U. anastasiae, recovered from deposits of Tournaisian to Viséan stages in Kazakhstan. Known from one single specimen which was described in a publication of Russian language with poor illustrations, Unionopterus' affinities are extremely poorly known.
Haikoucaris is a genus of megacheiran arthropod that contains the single species Haikoucaris ercaiensis. It was discovered in the Cambrian Chengjiang biota of China.
Parapaleomerus is a genus of strabopid of small size found in Chengjiang biota, China. It contains one species, P. sinensis. Unlike the other members of Strabopida, Parapaleomerus lacks dorsal eyes and only possesses ten trunk tergites. The telson has been described as trapezoidal. All the trunk tergites are straight and increasingly curve backwards abaxially from T4–10. Specimens of Parapaleomerus sinesis are typically dorsoventrally compressed. The exoskeleton of P. sinensis has a semi-elliptical head shield that lacks any indication of the presence of dorsal eyes. The largest specimen described is recorded as 9.2 cm long, with a maximum width of 9 cm.
Cucumericrus ("cucumber-leg") is an extinct genus of stem-arthropod. The type and only species is Cucumericrus decoratus, with fossils discovered from the Maotianshan Shales of Yunnan, China.
Slimonidae is a family of eurypterids, an extinct group of aquatic arthropods. Slimonids were members of the superfamily Pterygotioidea and the family most closely related to the derived pterygotid eurypterids, which are famous for their cheliceral claws and great size. Many characteristics of the Slimonidae, such as their flattened and expanded telsons, support a close relationship between the two groups.
Herefordopterus is a genus of eurypterid, an extinct group of aquatic arthropods. Herefordopterus is classified as part of the family Hughmilleriidae, a basal family in the highly derived Pterygotioidea superfamily of eurypterids. Fossils of the single and type species, H. banksii, have been discovered in deposits of Silurian age in Herefordshire and Shropshire, England. The genus is named after Herefordshire, where most of the Herefordopterus fossils have been found. The specific epithet honors Richard Banks, who found several well-preserved specimens, including the first Herefordopterus fossils.
Borchgrevinkium is an extinct genus of chelicerate arthropod. A fossil of the single and type species, B. taimyrensis, has been discovered in deposits of the Early Devonian period in the Krasnoyarsk Krai, Siberia, Russia. The name of the genus honors Carsten Borchgrevink, an Anglo-Norwegian explorer who participated in many expeditions to Antarctica. Borchgrevinkium represents a poorly known genus whose affinities are uncertain.
Strabopidae is the only family of the order Strabopida, an extinct group of arthropods known from the Cambrian period.
Paleomerus is a genus of strabopid, a group of extinct arthropods. It has been found in deposits from the Cambrian period. It is classified in the family Strabopidae of the monotypic order Strabopida. It contains two species, P. hamiltoni from Sweden and P. makowskii from Poland. The generic name is composed by the Ancient Greek words παλαιός (palaiós), meaning "ancient", and μέρος (méros), meaning "part".
Dvulikiaspis is a genus of chasmataspidid, a group of extinct aquatic arthropods. Fossils of the single and type species, D. menneri, have been discovered in deposits of the Early Devonian period in the Krasnoyarsk Krai, Siberia, Russia. The name of the genus is composed by the Russian word двуликий (dvulikij), meaning "two-faced", and the Ancient Greek word ἀσπίς (aspis), meaning "shield". The species name honors the discoverer of the holotype of Dvulikiaspis, Vladimir Vasilyevich Menner.
Luolishania is an extinct genus of lobopodian panarthropod and known from the Lower Cambrian Chiungchussu Formation of the Chengjiang County, Yunnan Province, China. A monotypic genus, it contains one species Luolishania longicruris. It was discovered and described by Hou Xian-Guang and Chen Jun-Yuan in 1989. It is one of the superarmoured Cambrian lobopodians suspected to be either an intermediate form in the origin of velvet worms (Onychophora) or basal to at least Tardigrada and Arthropoda. It is the basis of the family name Luolishaniidae, which also include other related lobopods such as Acinocricus, Collinsium, Facivermis, and Ovatiovermis. Along with Microdictyon, it is the first lobopodian fossil discovered from China.