Borchgrevinkium Temporal range: Lochkovian, | |
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Restoration of B. taimyrensis | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Arthropoda |
Subphylum: | Chelicerata |
Clade: | Euchelicerata |
Clade: | Prosomapoda (?) |
Genus: | † Borchgrevinkium Novojilov, 1959 |
Type species | |
†Borchgrevinkium taimyrensis Novojilov, 1959 |
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 (Lochkovian epoch) 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.
It had several unique characteristics that differentiated it from many other arthropods, such as its long parabolic (nearly U-shaped) prosoma (head), its elongated first and second segments and the presence of paired "ridges" in the surface of its third to tenth tergites (dorsal halves of the segments). Furthermore, the opisthosoma (the "trunk") of Borchgrevinkium was triangular, and its telson (the posteriormost division of its body), short and wedge-shaped. It was a small animal, approximately 3 centimetres (1.2 inches) long.
The only known specimen of the genus was collected in 1956 and described in 1959 by the Russian paleontologist Nestor Ivanovich Novojilov. He determined that it was a eurypterid and classified it in the family Mycteroptidae. However, its classification changed repeatedly over the years, being transferred from Eurypterida to Xiphosura and back to Eurypterida some time later. Borchgrevinkium is tentatively considered as a prosomapod, with more fossil material needed to ensure its current classification.
The size of the only known specimen of Borchgrevinkium, identified with the label PIN 1271/1, is estimated more or less at 3 centimetres (1.2 inches), making it a small arthropod. [1]
The prosoma was longer than wider (covering one third of the length of the animal), parabolic (nearly U-shaped) and with a length of 1.35 cm (0.53 in). The eyes are not preserved and therefore, their position or shape is unknown. The prosomal appendages (limbs) are only known by the tip of poorly preserved left pairs. They were short, undifferentiated and spiniferous. The opisthosoma (the "trunk") was triangular and 1.23 cm (0.48 in) long. It was composed of 12 segments, with the first one being exceptionally long and forming with the second segment an "extension" of the prosoma. The genital appendage (a ventral "rod" part of the reproductive system) of Borchgrevinkium was long, spanning from its first to its second segment. [1]
The third to tenth tergites (dorsal halves of the segments) had distal (outwards-pointing) lobes on their sides that delimitated the dorsal and ventral parts of the opisthosoma. Furthermore, these tergites had on their surfaces converging paired "folds" or "ridges" that progressively narrowed to the center of the tenth tergite. These ridges were almost parallel to the lateral lobes. On the eleventh tergite, the edges were slightly curved. The pretelson (the segment that preceded the telson) had a bifid (divided into two lobes) dorsal projection. The telson (the posteriormost division of the body) was cuneiform (wedge-like), short and narrow, and measured 0.45 cm (0.18 in). The ornamentation of the body was composed by short scales with broadly rounded edges. [1]
In 1956, the Russian paleontologist and geologist Vladimir Vasilyevich Menner discovered a series of fossils in Devonian deposits near the Imangda River at the southwest of the Taymyr Peninsula, near Norilsk, in the Krasnoyarsk Krai (Russia, then the Soviet Union). He sent them to the Russian paleontologist Nestor Ivanovich Novojilov, [2] who in 1959 described, among others, a specimen labelled as PIN 1271/1, which was nearly complete. It was deposited in the Paleontological Institute of the Russian Academy of Sciences, in Moscow, where it remains. Novojilov considered it unique enough to be erected as a new genus, Borchgrevinkium, named after the Anglo-Norwegian explorer Carsten Borchgrevink for his expeditions to Antarctica. He compared it with the then xiphosuran genus Weinbergina , assuming that Borchgrevinkium was also a xiphosuran. However, the Norwegian paleontologist Leif Størmer, who assisted him during his study, noticed that what Novojilov had considered to be an accidental fissure was actually part of the "macrosegment" (the first segment), finding as well the tip of the appendages after closer examination. The presence of this macrosegment convinced Novojilov that Borchgrevinkium represented a new eurypterid, and he classified it as such. [1]
In 1966, the American paleontologist Erik Norman Kjellesvig-Waering, during a study on the families and genera of the superfamily Stylonuracea (now known as Stylonuroidea), tentatively recorded an Upper Silurian occurrence of the genus Borchgrevinkium apart from the Lower Devonian one, believing that a new specimen had been found. [3] This specimen was later named as "Borchgrevinkium sp.". [4] In 2017, the British geologist and paleobiologist James C. Lamsdell and the Irish palaeontologist Derek Briggs found that this specimen was YPM IP 300790, collected in the Bertie Formation in the state of New York in 1967 by Samuel J. Ciurca, Jr., who identified it as a new undescribed species of Borchgrevinkium after contacting Størmer. Nevertheless, since this specimen was misidentified, it was redescribed as a new species of the chasmataspidid Diploaspis , D. praecursor, by Lamsdell and Briggs. [5]
The history of Borchgrevinkium soon became turbulent, being classified as a xiphosuran in 1989, [6] and back to Eurypterida years later. [7] Borchgrevinkium was tentatively moved by Lamsdell in 2013 to the clade (taxonomic group) Prosomapoda. [8]
Novojilov, during his description of Borchgrevinkium, noted a certain resemblance to Weinbergina, especially for the paired "ridges" that both have on their tergites. Based on the aforementioned macrosegment, Novojilov classified the genus as a mycteroptid eurypterid and compared it to the species Mycterops matthieui and Woodwardopterus scabrosus (members of the family), without finding many similarities but still classifying Borchgrevinkium in the eurypterid group. [1] Nowadays, however, his descriptions are considered inexhaustive and based only on the best preserved material. [2] Nevertheless, the genus continued being considered by other authors as a eurypterid. In 1966, Kjellesvig-Waering classified Borchgrevinkium with Woodwardopterus in the family Woodwardopteridae. He based this conclusion on the similarity of the ornamentation, the shape of the prosoma and the exceptional size of the first two segments of both. [3]
In 1972, Størmer questioned the affiliation of the genus in this clade and suggested that it might represent a chasmataspidid within the order Xiphosura. [9] Following this recommendation, Victor P. Tollerton, Jr. reclassified it in 1989 inside this order during his revision of Eurypterida. [6] In 2004, the Norwegian paleontologist Odd Erik Tetlie did not support this change and transferred Borchgrevinkium as eurypterid, again in the family Woodwardopteridae with Woodwardopterus and Mycterops, but now in a different suborder, Woodwardopterina, suggesting that these arthropods actually could not represent eurypterids. The woodwardopterines were presumably united by the great elongation of the first two segments. [7] This point of view was not approved by other researchers, and eventually Woodwardopterina was synonymized with Stylonurina and Woodwardopteridae with Mycteroptidae. [10] In addition, Lamsdell considered the genus as needing a redescription. [7]
Nowadays, Borchgrevinkium is a highly uncertain and problematic genus. Its eurypterid nature was soon denied again in 2013, when Lamsdell placed it in the clade Prosomapoda. It encompasses all chelicerates with prosomal uniramous appendages (appendages composed of a single series of segments attached end-to-end) in the adult stage (excluding the sixth and last pair of appendages). However, the appendages of Borchgrevinkium are poorly known. Lamsdell made a note in it and in Anderella , determining that in order to consolidate the classification of both genera in Prosomapoda, new fossil material is needed. [8]
A phylogenetic analysis (the results presented in a cladogram below) conducted by Lamsdell in 2013 on the relationships within Xiphosura and the relations to other closely related groups concluded that Xiphosura, as presently understood, was paraphyletic (that is, it was a group sharing a last common ancestor but not including all descendants of this ancestor) and thus not a valid phylogenetic group. Prosomapoda was erected to include several chelicerates formerly classified mostly as xiphosurans, as well as the xiphosurans themselves and Planaterga. Borchgrevinkium was not included due to its scarce known material. [8]
The only known specimen of Borchgrevinkium has been recovered in Early Devonian (Lochkovian) deposits of the Taymyr Peninsula in Siberia, Russia. It was found alongside specimens of the chasmataspidids Dvulikiaspis menneri , Heteroaspis stoermeri and Skrytyaspis andersoni , as well as indeterminate eurypterids like Acutiramus . The lithology (physical characteristics of the rocks) of the place has been described as dark gray marls with gypsiferous and dolomitic; rich in dolomite occurrences. The fossils were collected 60 metres (200 feet) below the Early Devonian–Middle Devonian boundary. [1] [2]
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.
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".
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.
Chasmataspidids, sometime referred to as chasmataspids, are a group of extinct chelicerate arthropods that form the order Chasmataspidida. Chasmataspidids are probably related to horseshoe crabs (Xiphosura) and/or sea scorpions (Eurypterida), with more recent studies suggest that they form a clade (Dekatriata) with Eurypterida and Arachnida. Chasmataspidids are known sporadically in the fossil record through to the mid-Devonian, with possible evidence suggesting that they were also present during the late Cambrian. Chasmataspidids are most easily recognised by having an opisthosoma divided into a wide forepart (preabdomen) and a narrow hind part (postabdomen) each comprising 4 and 9 segments respectively. There is some debate about whether they form a natural group.
Nanahughmilleria is a genus of eurypterid, an extinct group of aquatic arthropods. Fossils of Nanahughmilleria have been discovered in deposits of Devonian and Silurian age in the United States, Norway, Russia, England and Scotland, and have been referred to several different species.
Onychopterella is a genus of predatory eurypterid, an extinct group of aquatic arthropods. Fossils of Onychopterella have been discovered in deposits from the Late Ordovician to the Late Silurian. The genus contains three species: O. kokomoensis, the type species, from the Early Pridoli epoch of Indiana; O. pumilus, from the Early Llandovery epoch of Illinois, both from the United States; and O. augusti, from the Late Hirnantian to Early Rhuddanian stages of South Africa.
Willwerathia is a genus of Devonian arthropod. It is sometimes classified as synziphosurine, a paraphyletic group of horseshoe crab-like fossil chelicerate arthropods, while some studies compare its morphology to an artiopod. Willwerathia known only by one species, Willwerathia laticeps, discovered in deposits of the Devonian period from the Klerf Formation, in the Rhenish Slate Mountains of Germany.
Tylopterella is a genus of eurypterid, a group of extinct aquatic arthropods. Only one fossil of the single and type species, T. boylei, has been discovered in deposits of the Late Silurian period in Elora, Canada. The name of the genus is composed by the Ancient Greek words τύλη, meaning "knot", and πτερόν, meaning "wing". The species name boylei honors David Boyle, who discovered the specimen of Tylopterella.
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.
Legrandella is a genus of synziphosurine, a paraphyletic group of fossil chelicerate arthropods. Legrandella was regarded as part of the clade Prosomapoda. Fossils of the single and type species, L. lombardii, have been discovered in deposits of the Devonian period in Cochabamba, Bolivia.
Pasternakevia is a genus of synziphosurine, a paraphyletic group of fossil chelicerate arthropods. Pasternakevia was regarded as part of the clade Planaterga. Fossils of the single and type species, P. podolica, have been discovered in deposits of the Silurian period in Podolia, Ukraine.
Weinbergina is a genus of synziphosurine, a paraphyletic group of fossil chelicerate arthropods. Fossils of the single and type species, W. opitzi, have been discovered in deposits of the Devonian period in the Hunsrück Slate, Germany.
Synziphosurina is a paraphyletic group of chelicerate arthropods previously thought to be basal horseshoe crabs (Xiphosura). It was later identified as a grade composed of various basal euchelicerates, eventually excluded from the monophyletic Xiphosura sensu stricto and only regarded as horseshoe crabs under a broader sense. Synziphosurines survived at least since early Ordovician to early Carboniferous in ages, with most species are known from the in-between Silurian strata.
Pterygotidae is a family of eurypterids, an extinct group of aquatic arthropods. They were members of the superfamily Pterygotioidea. Pterygotids were the largest known arthropods to have ever lived with some members of the family, such as Jaekelopterus and Acutiramus, exceeding 2 metres (6.6 ft) in length. Their fossilized remains have been recovered in deposits ranging in age from 428 to 372 million years old.
Pterygotioidea is a superfamily of eurypterids, an extinct group of aquatic arthropods. Pterygotioids were the most derived members of the infraorder Diploperculata and the sister group of the adelophthalmoid eurypterids. The group includes the basal and small hughmilleriids, the larger and specialized slimonids and the famous pterygotids which were equipped with robust and powerful cheliceral claws.
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.
The metastoma is a ventral single plate located in the opisthosoma of non-arachnid dekatriatan chelicerates such as eurypterids, chasmataspidids and the genus Houia. The metastoma located between the base of 6th prosomal appendage pair and may had functioned as part of the animal's feeding structures. It most likely represented a fused appendage pair originated from somite 7, thus homologous to the chilaria of horseshoe crab and 4th walking leg pair of sea spider. In eurypterids, the plate was typically cordate (heart-shaped) in shape, though differed in shape in some genera, such as Megalograptus.
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.
Camanchia is a genus of synziphosurine, a paraphyletic group of fossil chelicerate arthropods. Camanchia was regarded as part of the clade Prosomapoda. Fossils of the single and type species, C. grovensis, have been discovered in deposits of the Silurian period in Iowa, in the United States. Alongside Venustulus, Camanchia is one of the only Silurian synziphosurine with fossil showing evidence of appendages.
Anderella is a genus of synziphosurine, a paraphyletic group of fossil chelicerate arthropods. Anderella was regarded as part of the clade Prosomapoda. Fossils of the single and type species, A. parva, have been discovered in deposits of the Carboniferous period in Montana, in the United States. Anderella is the first and so far the only Carboniferous synziphosurine being described, making it the youngest member of synziphosurines. Anderella is also one of the few synziphosurine genera with fossil showing evidence of appendages, but the details are obscure due to their poor preservation.