Trigonotarbida

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Trigonotarbida
Temporal range: Pridoli–Sakmarian Late Silurian to Early Permian
20201208 Trigonotarbida trigonotarbid.png
Palaeocharinus rhyniensis, Eophrynus prestvicii, johnsoni and celticus
Scientific classification e
Kingdom: Animalia
Phylum: Arthropoda
Subphylum: Chelicerata
Class: Arachnida
Order: Trigonotarbida
Petrunkevitch, 1949
Families
Synonyms
  • Anthracomarti Karsch, 1882
  • Meridogastra Thorell & Lindström, 1885
  • Eurymarti Matthew, 1895

The order Trigonotarbida is a group of extinct arachnids whose fossil record extends from the late Silurian to the early Permian (Pridoli to Sakmarian).[1][2][3] These animals are known from several localities in Europe and North America, as well as a single record from Argentina. Trigonotarbids can be envisaged as spider-like arachnids, but without silk-producing spinnerets. They ranged in size from a few millimetres to a few centimetres in body length and had segmented abdomens (opisthosoma), with the dorsal exoskeleton (tergites) across the backs of the animals' abdomens, which were characteristically divided into three or five separate plates.[1] Probably living as predators on other arthropods, some later trigonotarbid species were quite heavily armoured and protected themselves with spines and tubercles.[4] About seventy species are currently known, with most fossils originating from the Carboniferous coal measures. In July 2014 scientists used computer graphics to re-create a possible walking gait for the animal.[5][6] However, a subsequent biomechanical analysis proved the proposed coordination pattern as largely non-physiological.[7]

Historical background[]

Fossils of Eophrynus prestvicii

The first trigonotarbid was described in 1837 from the coal measures of Coalbrookdale in England by the famous English geologist Dean William Buckland.[8] He believed it to be a fossil beetle and named it Curculoides prestvicii. A much better preserved example was later discovered from Coseley near Dudley; also in the English West Midlands conurbation. Described in 1871 by Henry Woodward,[9] he correctly identified it as an arachnid and renamed it Eophrynus prestvicii—whereby the genus name comes from ἠώς (eos, meaning 'dawn'), and Phrynus, a genus of living whip spider (Amblypygi). Woodward subsequently described another trigonotarbid, Brachypyge carbonis, from the coal measures of Mons in Belgium;[10] although this fossil is known only from its abdomen and was initially mistaken for those of a crab.

A new arachnid order[]

Reconstruction of johnsoni, the eponymous species of Trigonotarbida.[11]

In 1882, the German zoologist Ferdinand Karsch described a number of fossil arachnids from the coal measures of Neurode in Silesia (now Poland), including one he named Anthracomartus voelkelianus in honour of Herr Völkel, the foreman of the mine where it was discovered.[12] This species was raised to a new, extinct, arachnid order which Karsch called Anthracomarti. The name is derived from ἄνθραξ (anthrax), the Greek word for coal. A number of other fossils which would eventually be placed in Trigonotarbida were discovered around this time. Hanns Bruno Geinitz described Kreischeria wiedei from the coal measures of Zwickau in Germany,[13] although he interpreted it as a fossil pseudoscorpion. Johann Kušta described Anthracomartus krejcii[14] from Rakovník in the Czech Republic, and published further descriptions in a number of subsequent papers.[15][16][17] In 1884, Samuel Hubbard Scudder described Anthracomartus trilobitus from Fayetteville, Arkansas—the first trigonotarbid from North America.[18]

Relationships[]

Trigonotarbita

Ricinulei

Tetrapulmonata

Araneae

Haptopoda

Amblypygi

Thelyphonida

Schizomida

Internal phylogeny of , showing position of Trigonotarbita and possible relationship with Ricinulei.[19][20] Extinct taxa indicaded by '†'.

Early studies tended to confuse trigonotarbids with other living or extinct groups of arachnids; particularly harvestmen (Opiliones). Petrunkevitch's division of the trigonotarbids into two, unrelated, orders was noted above. In detail, he divided the arachnids into suborders based on the width of the division between the two parts of the body (the prosoma and opisthosoma). Anthracomartida and another extinct order, Haptopoda, were grouped into a subclass Stethostomata defined by a broad division of the body and downward-hanging mouthparts. Trigonotarbida was placed in its own subclass Soluta and defined as having a division of the body which was variable in width. Petrunkevitch's scheme was largely followed in subsequent studies of fossil arachnids.

Pantetrapulmonata[]

In the 1980s, Bill Shear and colleagues[21] carried out an important study on well preserved Mid Devonian trigonotarbids from Gilboa, New York. They questioned whether it was appropriate to define a group of animals on a variable character state and carried out the first cladistic analysis of fossil and living arachnids. They showed that trigonotarbids are closely related to a group of arachnids which have gone under various names (Caulogastra, Arachnidea, etc.), but for which the name Tetrapulmonata has become most widespread.[22] Members of the Tetrapulmonata include spiders (Araneae), whip spiders (Amblypygi), whip scorpions (Thelyphonida) and shorttailed whipscorpion (Schizomida) and, together with trigonotarbids, share characters like two pairs of book lungs and similar mouthparts with fangs operating rather like a pocket knife.[23] In a 2007 study of arachnid relationships, the Shear et al. hypothesis was largely supported and a group was proposed which comprises Trigonotarbida + Tetrapulmonata.[24] This has since been corroborated in more recent cladistic analyses.[25][26][27][28]

Trigonotarbids and ricinuleids[]

Reconstruction of Palaeocharinus, a genus known to have tiny pedipalpal claws.
The ricinuleid species Ricinoides atewa, showing divided tergites.

In 1892, Ferdinand Karsch suggested that the rare and rather bizarre-looking ricinuleids (Ricinulei) were the last living descendants of the trigonotarbids.[29] A similar hypothesis was reintroduced by Dunlop,[19] who pointed out distinct similarities and possible sister group relationship between these arachnid groups. Both have opisthosomal tergites divided into median and lateral plates and both have a complicated coupling mechanism between the prosoma and the opisthosoma which 'locks' the two halves of the body together. Although cladistic analysis has tended to recover ricinuleids in their traditional position closely related to mites and ticks, further discoveries have revealed that the tip of the pedipalp ends in a small claw in both trigonotarbids and ricinuleids.[20][30] If the hypothesis is true, ricinuleids, despite the lack of tetrapulmonate key characters (e.g. book lungs), may represent part of the pantetrapulmonate clade alongside trigonotarbids as well.[19][20][23]

Internal relationships[]

The first cladistic analysis of the trigonotarbids was published in 2014.[11] This recovered the families Anthracomartidae, , and Eophrynidae as monophyletic. In contrast , , , and were not. Two clades were consistently recovered with strong support—(Palaeocharinus (Archaeomartidae + Anthracomartidae)), and as sister group the 'eophrynid assemblage' ( ( ( (Kreischeria (Eophrynus + ))))).

Description[]

Dorsal (A) and ventral (B) morphology of a trigonotarbid.
External morphology of a trigonotarbid in sagittal section.

Trigonotarbids superficially resemble spiders, but can be easily recognised by having tergites on the dorsal side of the opisthosoma divided into median and lateral plates.[31] This character is shared with ricinuleids (Ricinulei) (see also Ricinulei#Relationships). As in other arachnids, the body is divided into a prosoma (or cephalothorax) and opisthosoma (or abdomen). Body length ranges from a couple of millimetres up to about 5 cm (2.0 in).[32]

Prosoma[]

The prosoma is covered by the carapace and always bears a pair of median eyes.[1] In the probably basal families , Anthracomartidae[33]—and perhaps also —there is an additional pair of lateral eye tubercles which, at least in palaeocharinids,[34] appear to have borne a series of individual lenses. In this sense palaeocharinids seem to be in the process of reducing a compound eye.[35] Anterior margin of the carapace protrude into a projection referred to as clypeus.[25]

The chelicerae are of the "pocket-knife" type consisting of a basal segment and a sharp, curving fang.[1] The chelicerae are described as paleognathic: the fangs are held parallel to one another, like those of mesothele and mygalomorph spiders, but the chelicerae hang downwards like those of araneomorph spiders.[36] There is no evidence in well-preserved fossils for the opening of a venom gland, thus trigonotarbids were probably not venomous. The chelicerae may have been slightly retractable into the prosoma. Well-preserved palaeocharinids show evidence for a small, slit-like mouth with an upper lip (a labrum or rostrum) and a lower lip (or labium).[37] Inside the mouth there is some sort of filtering system formed from hairs or platelets which strongly suggests that trigonotarbids (like spiders and many other arachnids) could eat only preorally digested, liquified prey.[37]

The pedipalps have the typical arachnid structure with a coxa, trochanter, femur, patella, tibia and tarsus. They are pediform, i.e. they look like small legs and were not highly modified.[6] There is no evidence for a special sperm transfer device as in the modified palpal organ of male spiders. In at least the palaeocharinids and anthracomartids the tip of the pedipalp is modified into a small chela (claw) formed from the tarsal claw (or apotele) and a projection from the tarsus. As mentioned above, a very similar arrangement is seen at the end of the pedipalp in Ricinulei.[20][30]

The walking legs again follow the typical arachnid plan with a coxa, trochanter, femur, patella, tibia, metatarsus and tarsus.[1] The coxae surround a single sternum. In well preserved palaeocharinids there is a ring, or annulus, around the trochanter–femur joint which may be the remains of an earlier leg segment.[6] The legs are largely unmodified, although in Anthracosironidae the forelegs are quite large and spiny,[38] presumably to help catch prey. The legs end in three claws, two large ones and a smaller median claw.[6]

Opisthosoma[]

Fossil of roessleri, showing divided tergites.
Reconstruction of an anthracomartid trigonotarbid celticus, showing 5 rows of dorsal plates.

The opisthosoma is largely suboval in outline with a flatten dorsal surface.[6] It compose of 12 segments, with some of them had undergone degrees of fusion or reduction, hence the previous misinterpretation of around 8 to 11 segments.[23] Tergite of the first segment partially covered by the posterior margin of preceding carapace, forming a complicated coupling mechanism known as 'locking ridge'.[1][23] Tergites of segment 2 to 8 (segment 9 in some species) were all laterally divided into 3 (one median and two lateral) plates, with those of segment 2 and 3 fused to each other in most species.[23] However, the corresponding tergites of the family Anthracomartidae are further subdivided into 5 plates.[33] The last 3 segments are usually only visible from the ventral side,[1] with the 2 final segments constricted into a tiny ring-like section known as pygidium.[23]

Ventral side of opisthosomal segment 2 to 9 covered by series of lung-bearing opercula (2 and 3) and curved sternites (4 to 9).[1][23] The first segment apparently lacking any ventral plates. Just like other lung-bearing arachnids (scorpion and tetrapulmonate), the book lungs of trigonotarbids formed by layers of trabecula-bearing lamellae, which is a feature adapted to a terrestrial, air-breathing lifestyle.[39] A pair of ventral sacs located between the posterior operculum and following sternite had been observed in some species.[40][4][23]

Included taxa[]

As of 2020, 70 valid species had been included under Trigonotarbida as follows:[3]

plesion taxa
  • Dunlop, 1999
    • (Dunlop, 1996) – Late Silurian, England
Hirst, 1923
  • Shear, Selden & Rolfe, 1987
    • Shear, Selden & Rolfe, 1987 – Mid Devonian, United States
  • Shear, Selden & Rolfe, 1987
    • Shear, Selden & Rolfe, 1987 – Mid Devonian, United States
    • Shear, Selden & Rolfe, 1987 – Mid Devonian, United States
    • Shear, Selden & Rolfe, 1987 – Mid Devonian, United States
    • Shear, Selden & Rolfe, 1987 – Mid Devonian, United States
  • Shear, 2000
    • Shear, 2000 – Late Devonian, United States
  • Shear, Selden & Rolfe, 1987
    • Shear, Selden & Rolfe, 1987 – Mid Devonian, United States
  • Palaeocharinus Hirst, 1923
    • Palaeocharinus calmani Hirst, 1923 – Early Devonian, Scotland
    • Hirst, 1923 – Early Devonian, Scotland
    • Hirst, 1923 – Early Devonian, Scotland
    • Hirst, 1923 – Early Devonian, Scotland
    • Hirst, 1923 – Early Devonian, Scotland
    • Fayers, Dunlop & Trewin, 2005 – Early Devonian, Scotland
  • Poschmann & Dunlop, 2011
Haase, 1890
  • Størmer, 1970
    • Størmer, 1970 - Devonian, Alken an der Mosel
Anthracomartidae Haase, 1890
  • synonyms
    • = Promygalidae Frič, 1904
    • = Brachypygidae Pocock, 1911
    • = Coryphomartidae Petrunkevitch, 1945
    • = Pleomartidae Petrunkevitch, 1945
  • Karsch, 1882
    • synonyms
      • = Brachylycosa Frič, 1904
      • = Cleptomartus Petrunkevitch, 1949
      • = Coryphomartus Petrunkevitch, 1945
      • = Cryptomartus Petrunkevitch, 1945
      • = Oomartus Petrunkevitch, 1953
      • = Perneria Frič, 1904
      • = Pleomartus Petrunkevitch, 1945
      • = Promygale Frič, 1901
    • (Frič, 1901) – Late Carboniferous, Czech Republic
    • (Frič, 1901) – Late Carboniferous, Czech Republic
      • synonyms
        • = Promygale rotunda Frič, 1901
        • = Perneria salticoides Frič, 1904
    • Frič, 1901 – Late Carboniferous, Czech Republic
    • Pocock, 1911 – Late Carboniferous, England
      • synonyms
        • = Cleptomartus hangardi Guthörl, 1965
        • = Cryptomartus meyeri Guthörl, 1964
        • = Cleptomartus planus Petrunkevitch, 1949
        • = Cryptomartus rebskei Brauckmann, 1984
    • Frič, 1904 – Late Carboniferous, Poland
    • (Opluštil, 1986) – Late Carboniferous, Czech Republic
    • Petrunkevitch, 1953 – Late Carboniferous, Czech Republic
    • Kušta, 1884 – Late Carboniferous, Czech Republic
      • synonym
        • = Anthracomartus socius Kušta, 1888
    • (Petrunkevitch, 1953) – Late Carboniferous, Czech Republic
    • Ammon, 1901 – Late Carboniferous, Germany
    • Pocock, 1911 – Late Carboniferous, England
      • synonyms
        • = Anthracomartus denuiti Pruvost, 1922
        • = Cleptomartus plautus Petrunkevitch, 1949
    • (Opluštil, 1985) – Late Carboniferous, Czech Republic
    • Petrunkevitch, 1913 – Late Carboniferous, Canada
    • Scudder, 1884 – Late Carboniferous, United States
    • Karsch, 1882 – Late Carboniferous, Poland
  • Woodward, 1878
    • Woodward, 1878 – Late Carboniferous, Belgium
  • Pocock, 1911
    • (Pocock, 1902) – Late Carboniferous, Europe
      • synonym
        • = Maiocercus orbicularis Gill, 1911
Pocock, 1903
  • Pocock, 1903
    • Pocock, 1903 – Late Carboniferous, Europe
      • synonym
        • = Anthracosiro elongatus Waterlot, 1934
    • Pocock, 1903 – Late Carboniferous, Europe
      • synonyms
        • = Anthracosiro corsini Pruvost, 1926
        • = Anthracosiro latipes Gill, 1909
  • Dunlop & Selden, 2004
    • Dunlop & Selden, 2004 – Early Devonian, Wales
  • Frič, 1904
    • (Roemer, 1878) - Carboniferous, Silesia
Petrunkevitch, 1949
  • Pocock, 1911
    • Petrunkevitch, 1955 – Late Carboniferous, France
    • Pocock, 1911 – Late Carboniferous, England
    • Schultka, 1991 – Early Devonian, Germany
Dunlop, 1995
  • Petrunkevitch, 1949
    • (Petrunkevitch, 1913) – Late Carboniferous, United States
    • (Petrunkevitch, 1913) – Late Carboniferous, United States
Petrunkevitch, 1945
  • synonym
    • = Trigonomartidae Petrunkevitch, 1949
  • Størmer, 1970
    • Størmer, 1970 - Devonian, Alken an der Mosel
  • Pocock, 1911
    • synonyms
      • = Trigonomartus Petrunkevitch, 1913
      • = Phrynomartus Petrunkevitch, 1945a
    • Pocock, 1911 – Early/Late Carboniferous, Europe
      • synonyms
        • = Aphantomartus pococki Pruvost, 1912
        • = Trigonomartus dorlodoti Pruvost, 1930
        • = Eophrynus waechteri Guthörl, 1938
        • = ?Trigonomartus pruvosti van der Heide, 1951
        • = ?Brachylycosa manebachensis Müller, 1957
    • (Scharf, 1924) – Permian, Germany
    • (Scudder, 1884) – Late Carboniferous, Europe, North America
      • synonyms
        • = ?Kreischeria villeti Pruvost, 1912
        • = Cleptomartus plötzensis Simon, 1971
Haase, 1890
  • Petrunkevitch, 1953
    • (Pruvost, 1919) – Late Carboniferous, France
  • Pinto & Hünicken, 1980
    • Pinto & Hünicken, 1980 – Late Carboniferous, Argentina
  • Frič, 1904
    • (Thevenin, 1902) – Late Carboniferous, France
  • Kreischeria Geinitz, 1882
    • Kreischeria wiedei Geinitz, 1882 – Late Carboniferous, Germany
  • Petrunkevitch, 1953
    • (Gill, 1924) – Late Carboniferous, England
      • synonym
        • = Eophrynus varius Petrunkevitch, 1949
Eophrynidae Karsch, 1882
  • synonym
    • = Hemiphrynidae Frič, 1904
  • Eophrynus Woodward, 1871
    • Eophrynus prestvicii (Buckland, 1837) – Late Carboniferous, England
    • Brauckmann, Koch & Kemper, 1985 – Late Carboniferous, Germany
  • Harvey & Selden, 1995
    • synonym
      • Hemiphrynus Frič, 1901
    • (Frič, 1901) – Late Carboniferous, Czech Republic
    • (Frič, 1901) – Late Carboniferous, Czech Republic
  • Frič, 1904
    • Frič, 1904 – Late Carboniferous, Czech Republic
  • Petrunkevitch, 1953
    • (Kušta, 1883) – Late Carboniferous, Czech Republic
      • synonym
        • = Anthracomartus affinis Kušta, 1885
  • Petrunkevitch, 1945a
    • (Pocock, 1911) – Late Carboniferous, UK, United States
      • synonym
        • = Eophrynus warei Dix & Pringle, 1930
        • = Pleophrynus ensifer Petrunkevitch, 1945a
        • = Eophrynus jugatus Ambrose & Romano, 1972
  • Petrunkevitch, 1953
    • (Ewing, 1930) – Early Carboniferous, United States
  • Jux, 1982
    • Jux, 1982
  • Frič, 1904
    • synonyms
      • = Cyclotrogulus Frič, 1904
      • = Pseudoeophrynus Příbyl, 1958
    • (Stur, 1877) – Late Carboniferous, Czech Republic
      • synonyms
        • = Cyclotrogulus sturii Frič, 1904 [non Hasse, 1890]
        • = Pseudoeophrynus ostraviensis Příbyl, 1958
Family uncertain
  • Poschmann, Dunlop, Bértoux & Galtier, 2016
    • Poschmann, Dunlop, Bértoux & Galtier, 2016 - Carboniferous, Graissessac, France
  • Poschmann & Dunlop, 2010
    • (Dunlop & Brauckmann, 2006) - Carboniferous, Hagen-Vorhalle
      • synonyms
        • = Archaeomartus roessleri Dunlop & Brauckmann, 2006
  • Dunlop & Rößler, 2013
    • Dunlop & Rößler, 2013 Permian, Chemnitz
  • Hradská & Dunlop, 2013
    • Hradská & Dunlop, 2013 - Carboniferous, Týnec
incertae sedis
  • Andrée, 1913
    • Andrée, 1913 – Late Carboniferous, Germany
  • Petrunkevitch, 1913
    • Petrunkevitch, 1913 - Carboniferous, West Virginia
  • Eophrynusscharfi Scharf, 1924 – Early Permian, Germany
  • Pocock, 1911
    • (Scudder, 1893) - Carboniferous, Rhode Island
nomina dubia
  • Anthracomartus buchi (Goldenberg, 1873) – Late Carboniferous, Germany
  • Anthracomartus hageni (Goldenberg, 1873) – Late Carboniferous, Germany
  • Elaverimartus pococki Petrunkevitch, 1953 – Late Carboniferous, Scotland
  • Eurymartus latus Matthew, 1895 – Late Carboniferous, Canada
  • ?Eurymartus spinulosus Matthew, 1895 – Late Carboniferous, Canada

References[]

  1. ^ Jump up to: a b c d e f g h Garwood, Russell J.; Dunlop, Jason A. (2010). "Fossils Explained: Trigonotarbids". Geology Today. 26 (1): 34–37. doi:10.1111/j.1365-2451.2010.00742.x. Retrieved June 12, 2015.
  2. ^ Dunlop, J. A.; Rößler, R. (2013-08-01). "The youngest trigonotarbid Permotarbus schuberti n. gen., n. sp. from the Permian Petrified Forest of Chemnitz in Germany". Fossil Record. 16 (2): 229–243. doi:10.5194/fr-16-229-2013. ISSN 2193-0074.
  3. ^ Jump up to: a b Dunlop, J. A., Penney, D. & Jekel, D. 2020. A summary list of fossil spiders and their relatives. In World Spider Catalog. Natural History Museum Bern, online at http://wsc.nmbe.ch, version 20.5
  4. ^ Jump up to: a b Dunlop, Jason; Garwood, Russell (2014). "Tomographic reconstruction of the exceptionally preserved trigonotarbid arachnid Eophrynus prestvicii". Acta Palaeontologica Polonica. doi:10.4202/app.2012.0032.
  5. ^ Jonathan Amos (9 July 2014). "Ancient arachnid 'walks again'". BBC News. Retrieved 9 July 2014.
  6. ^ Jump up to: a b c d e Garwood, Russell J.; Dunlop, Jason A. (July 2014). "The walking dead: Blender as a tool for paleontologists with a case study on extinct arachnids". Journal of Paleontology. 88 (4): 735–746. doi:10.1666/13-088. ISSN 0022-3360. S2CID 131202472. Retrieved July 21, 2015.
  7. ^ Weihmann, Tom; Goetzke, Hanns Hagen; Günther, Michael (November 2015). "Requirements and limits of anatomy-based predictions of locomotion in terrestrial arthropods with emphasis on arachnids". Journal of Paleontology. 89 (6): 980–990. doi:10.1017/jpa.2016.33. S2CID 86908527.
  8. ^ William Buckland (1837). Treatise IV. Geology and mineralogy with reference to natural theology. The Bridgewater treatises on the power, wisdom and goodness of God as manifested in the creation. (2nd ed.). London: William Pickering.
  9. ^ H. Woodward (1871). "On the discovery of a new and very perfect Arachnide from the ironstone of the Dudley Coal-field". Geological Magazine. 8 (9): 1–4. Bibcode:1871GeoM....8..385W. doi:10.1017/s0016756800192817.
  10. ^ H. Woodward (1878). "Discovery of the remains of a fossil crab (Decapoda–Bracyura) in the Coal Measures of the Environs of Mons, Belgium". Geological Magazine. new series. 2 (5): 433–436. doi:10.1017/S0016756800152616.
  11. ^ Jump up to: a b Jones, Fiona; Dunlop, Jason A.; Friedman, Matthew; Garwood, Russell J. (2014). "Trigonotarbus johnsoni Pocock, 1911, revealed by X-ray computed tomography, with a cladistic analysis of the extinct trigonotarbid arachnids". Zoological Journal of the Linnean Society. 172 (1): 49–70. doi:10.1111/zoj.12167.
  12. ^ F. Karsch (1882). "Ueber ein neues Spinnenthier aus der Schlesischen Steinkohle und die Arachnoiden überhaupt". Zeitschrift der Deutschen Geologischen Gesellschaft (in German). 34: 556–561.
  13. ^ H. B. Geinitz (1882). "Kreischeria wiedei, ein Pseudoskorpion aus der Steinkohlenformation von Zwickau". Zeitschrift der Deutschen Geologischen Gesellschaft (in German). 34: 238–242.
  14. ^ Johann Kušta (1883). "Anthracomartus krejcii, eine neue Arachnide aus dem Böhmischen Karbon". Sitzungsberichte der Königlich Böhmischen Gesellschaft der Wissenschaften, Mathematisch-Naturwissenschaftliche Klasse (in German). 1883: 7.
  15. ^ Johann Kušta (1884). "Neue Arachniden aus der Steinkohlenformation von Rakonitz". Sitzungsberichte der Königlich Böhmischen Gesellschaft der Wissenschaften, Mathematisch-Naturwissenschaftliche Klasse (in German). 1884: 398–401.
  16. ^ Johann Kušta (1885). "Neue fossile Arthropoden aus dem Noeggarathienschiefer von Rakonitz". Sitzungsberichte der Königlich Böhmischen Gesellschaft der Wissenschaften, Mathematisch-Naturwissenschaftliche Klasse (in German). 1885: 1–7.
  17. ^ Johann Kušta (1888). "O nových arachnidech z karbonu Rakovnického. (Neue Arachniden aus der Steinkohlenformation bei Rakonitz)". Sitzungsberichte der Königlich Böhmischen Gesellschaft der Wissenschaften, Mathematisch-Naturwissenschaftliche Klasse (in Czech). 1888: 194–208.
  18. ^ Samuel H. Scudder (1884). "A contribution to our knowledge of Paleozoic Arachnida". Proceedings of the American Academy of Arts and Sciences. 20: 13–22. doi:10.2307/25138764. hdl:2027/hvd.32044107176828. JSTOR 25138764.
  19. ^ Jump up to: a b c Jason A. Dunlop (1996). "Evidence for a sister group relationship between Ricinulei and Trigonotarbida" (PDF). Bulletin of the British Arachnological Society. 10 (6): 193–204.
  20. ^ Jump up to: a b c d Jason A. Dunlop, Carsten Kamenz and Giovanni Talarico (2009). "A fossil trigonotarbid arachnid with a ricinuleid-like pedipalpal claw". Zoomorphology. 128 (4): 305–313. doi:10.1007/s00435-009-0090-z. S2CID 6769463.
  21. ^ William A. Shear, Paul A. Selden, W. D. I. Rolfe, Patricia M. Bonamo & James D. Grierson (1987). "New terrestrial arachnids from the Devonian of Gilboa, New York". American Museum Novitates. 2901: 1–74. hdl:2246/5166.CS1 maint: multiple names: authors list (link)
  22. ^ Jeffrey W. Shultz (1990). "Evolutionary morphology and phylogeny of Arachnida". Cladistics. 6 (1): 1–38. doi:10.1111/j.1096-0031.1990.tb00523.x. S2CID 85410687.
  23. ^ Jump up to: a b c d e f g h Dunlop, Jason A.; Lamsdell, James C. (2017). "Segmentation and tagmosis in Chelicerata". Arthropod Structure & Development. 46 (3): 395. ISSN 1467-8039.
  24. ^ 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.
  25. ^ Jump up to: a b Garwood, Russell J.; Dunlop, Jason A. (2014). "Three-dimensional reconstruction and the phylogeny of extinct chelicerate orders". PeerJ. 2: e641. doi:10.7717/peerj.641. PMC 4232842. PMID 25405073.
  26. ^ Garwood, Russell J.; Dunlop, Jason A.; Selden, Paul A.; Spencer, Alan R. T.; Atwood, Robert C.; Vo, Nghia T.; Drakopoulos, Michael (2016). "Almost a spider: a 305-million-year-old fossil arachnid and spider origins". Proceedings of the Royal Society B: Biological Sciences. 283 (1827): 20160125. doi:10.1098/rspb.2016.0125. ISSN 0962-8452.
  27. ^ Wang, Bo; Dunlop, Jason A.; Selden, Paul A.; Garwood, Russell J.; Shear, William A.; Müller, Patrick; Lei, Xiaojie (2018). "Cretaceous arachnid Chimerarachne yingi gen. et sp. nov. illuminates spider origins". Nature Ecology & Evolution. 2 (4): 614–622. doi:10.1038/s41559-017-0449-3. ISSN 2397-334X.
  28. ^ Garwood, Russell J.; Dunlop, Jason A.; Knecht, Brian J.; Hegna, Thomas A. (2017). "The phylogeny of fossil whip spiders". BMC Evolutionary Biology. 17 (1). doi:10.1186/s12862-017-0931-1. ISSN 1471-2148. PMC 5399839.
  29. ^ Ferdinand Karsch (1892). "Ueber Cryptostemma Guèr. als einziger recenter Ausläufer der fossilen Arachnoideen-Ordnung Meridogastra Thor". Berliner Entomologische Zeitschrift (in German). 37 (1): 25–32. doi:10.1002/mmnd.18920370108.
  30. ^ Jump up to: a b Russell Garwood, Jason A. Dunlop & Mark D. Sutton (2009). "High-fidelity X-ray micro-tomography reconstruction of siderite-hosted Carboniferous arachnids". Biology Letters. 5 (6): 841–844. doi:10.1098/rsbl.2009.0464. PMC 2828000. PMID 19656861.
  31. ^ Stephen R. Fayers, Jason A. Dunlop & Nigel H. Trewin (2005). "A new early Devonian trigonotarbid arachnid from the Windyfield chert, Rhynie, Scotland". Journal of Systematic Palaeontology. 2 (4): 269–284. doi:10.1017/S147720190400149X. S2CID 140706387.
  32. ^ Ronny Rößler & Jason A. Dunlop (1997). "Redescription of the largest trigonotarbid arachnid – Kreischeria wiedei Geinitz 1882 from the Upper Carboniferous of Zwickau, Germany". Paläontologische Zeitschrift. 71 (3–4): 237–245. doi:10.1007/BF02988493. S2CID 129447249.
  33. ^ Jump up to: a b Garwood, Russell J.; Dunlop, Jason A. "Morphology and systematics of anthracomartidae (Arachnida: Trigonotarbida)". Palaeontology. 54 (1): 145–161. ISSN 0031-0239.
  34. ^ Stanley Hirst & S. Maulik (1926). "On some arthropod remains from the Rhynie Chert (Old Red Sandstone)". Geological Magazine. 63 (2): 69–71. Bibcode:1926GeoM...63...69H. doi:10.1017/S0016756800083692.
  35. ^ Miether, Sebastian T.; Dunlop, Jason A. (2016). "Lateral eye evolution in the arachnids". Arachnology. 17 (2): 103–119. doi:10.13156/arac.2006.17.2.103. ISSN 2050-9928.
  36. ^ Dunlop, J.A. (1997). "Palaeozoic arachnids and their significance for arachnid phylogeny" (PDF). Proceedings of the 16th European Colloquium of Arachnology. Siedlce: Wydawnictwo Wyzszej Skoly Rolniczo-Pedagogicznej. pp. 65–82. Retrieved 2016-03-19.
  37. ^ Jump up to: a b Jason A. Dunlop (1994). "Comparative anatomy of filtration mechanisms in tetrapulmonate arachnids (Trigonotarbida, Araneae, Amblypygi, Uropygi and Schizomida)". Bulletin of the British Arachnological Society. 9: 267–273.
  38. ^ R. I. Pocock (1903). "A new Carboniferous arachnid". Geological Magazine. Decade 4. 10 (6): 247–251. Bibcode:1903GeoM...10..247P. doi:10.1017/S001675680011252X.
  39. ^ Kamenz, Carsten; Dunlop, Jason A; Scholtz, Gerhard; Kerp, Hans; Hass, Hagen (2008-04-23). "Microanatomy of Early Devonian book lungs". Biology Letters. 4 (2): 212–215. doi:10.1098/rsbl.2007.0597. ISSN 1744-9561. PMC 2429929. PMID 18198139.
  40. ^ Fayers, Stephen R.; Dunlop, Jason A.; Trewin, Nigel H. (2005). "A new early devonian trigonotarbid arachnid from the Windyfield Chert, Rhynie, Scotland" (PDF). Journal of Systematic Palaeontology. 2 (4): 269–284. doi:10.1017/S147720190400149X. ISSN 1477-2019.
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