Ptychoparia

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Ptychoparia
Temporal range: Middle Cambrian
Trilobites - Ptychoparia striata.JPG
Ptychoparia striata from Czech Republic, at the National Museum (Prague)
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Ptychoparia

Hawle and Corda, 1847
Type species
Conocephalus striatus [1]
Species
  • P. striata(Emmrich, 1839) [2] = Conocephalus striatus, Trilobites sulzeri var. γ, P. gracilis, P. lobifera, Lobocephalus cylindricus
  • P. dubinkaKordule, 2006
  • P. tuberosaFeniak, 1952
  • P. clusia Walcott, 1917
  • P. homfrayi(Hicks [Salter ms.]), 1872

Ptychoparia is a genus of ptychopariid trilobites, and is the type genus of the family Ptychopariidae, and the order Ptychopariida.

Contents

Fossils of the various species are found in Middle Cambrian-aged marine strata of Eurasia and North America, about 513 ± 0.3 to 499 ± 1.7 million years ago.

Distribution

Fossils have been found in Middle Cambrian marine strata of the Czech Republic, India, Mexico, Norway, South Korea, the United Kingdom, United States (Montana, New York, Virginia, and possibly Pennsylvania).

Reassigned species

Several species of trilobite that were originally assigned to Ptychoparia have now been moved to other genera. [1]

Description

Like all Ptychopariidae, the dorsal exoskeleton in Ptychoparia has an inverse egg-shaped outline. The central raised axis, that is defined by a furrow, is moderately convex and narrow, at its widest about ⅛ of the maximum width of the headshield (or cephalon). The part of the axis in the cephalon, called glabella, tapers forward, is rounded-truncate at its front, is inserted by for pairs of furrows that do not contact across the midline, and one at the back that defines the occipital ring. The fourth pair of lateral furrows curve strongly inward until parallel with the midline. A border is defined by a furrow running parallel to the margin of the cephalon, and this border furrow is deep at the front. The areas outside the axis are almost flat. Between the front of the glabella and the border, is a somewhat convex area of the cheek that is comparable in length (along the midline) to the occipital ring. In well preserved specimens the cheeks in front of the eye are adorned with very fine ridges (or striae) that probably represent parts of the digestive system (see Kordule, 2006, p. 283, figure 2.a/f). The eye ridges are threadlike, evenly curved, extending from the anterior corners of the glabella to halfway the genal angles, while the visual surface makes an abrupt angle, is shaped like a bracket parallel to the midline and ±⅛ of the length of the cephalon. Like in most trilobites, the division between the outer free cheek (or librigena) and the inner fixed cheek (or fixigena) is a line (or suture) where the exoskeleton splits to assist in moulting. It always follows the inside of the visual surface of the eye. In Ptychoparia, the part of this suture behind the eye cuts to the posterior margin just to the inside of the genal spine (or the suture is gonatoparian), and the part in front of the eye diverges from the midline. There is a spine in the back corners of the cephalon (or genal spine) that reaches approximately to the third thorax segment, and is confluent with the outer margin of the cephalon. The articulate midsection of the body (or thorax) has 13 (P. striata) or 14 (P. dubinka) segments. Tail shield (or pygidium) is slightly over half as wide as the cephalon (a state called micropygous). The pygidial axis (or rachis) has 5 or 6 rings and a termination and 4 or 5 ribs in the outlying pleural regions. The pygidium in Ptychoparia lacks a border. [2]

Related Research Articles

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<i>Paradoxides</i> Extinct genus of trilobites

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<i>Triarthrus</i>

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<i>Asaphus</i> Extinct genus of trilobites

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<i>Dikelocephalus</i>

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<i>Acimetopus</i>

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<i>Dicerodiscus</i>

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<i>Yunnanocephalus</i> Extinct genus of trilobites

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<i>Meteoraspis</i>

Meteoraspis is an extinct genus of ptychopariid trilobites of the family Tricrepicephalidae. The various species lived from 501 to 490 million years ago during the Dresbachian faunal stage of the late Cambrian Period. Fossils of Meteoraspis are characteristic of Late Cambrian strata in North America, though they are found in Late Cambrian strata elsewhere in the world, such as M. nevensis from Victoria Land, Antarctica.

<i>Eoredlichia</i> Extinct genus of trilobites

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Holmiidae

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Alokistocaridae

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<i>Conocoryphe</i>

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<i>Cedaria</i>

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<i>Tricrepicephalus</i>

Tricrepicephalus is an extinct genus of ptychopariid trilobites of the family Tricrepicephalidae with species of average size. Its species lived from 501 to 490 million years ago during the Dresbachian faunal stage of the late Cambrian Period. Fossils of Tricrepicephalus are widespread in Late Cambrian deposits in North America, but is also known from one location in South-America. Tricrepicephalus has an inverted egg-shaped exoskeleton, with three characteristic pits in the fold that parallels the margin of the headshield just in front of the central raised area. The articulating middle part of the body has 12 segments and the tailshield carries two long, tubular, curved pygidial spines that are reminiscent of earwig's pincers that rise backwards from the plain of the body at approximately 30°.

Anabaraspis is a genus of redlichiid trilobite. A. splendens occurs in the uppermost Lower Cambrian and lowest Middle Cambrian of Russia. In Anabaraspis there is a long area in front of the glabella which is not differentiated in a border and a preglabellar field. This is a unique character in the family Paradoxididae. The frontal lobe of the central raised area of the headshield is slightly pointed, rather than rounded or truncate, a character shared with Plutonides, though, in Plutonides it hangs over the short anterior border.

<i>Viaphacops</i>

Viaphacops is a genus of trilobites in the order Phacopida, family Phacopidae, that lived during the Middle Devonian, and is known from North and South America, Asia.

References

  1. 1 2 Moore, R.C. (1959). Arthropoda I - Arthropoda General Features, Proarthropoda, Euarthropoda General Features, Trilobitomorpha. Treatise on Invertebrate Paleontology. Part O. Boulder, Colorado/Lawrence, Kansas: Geological Society of America/University of Kansas Press. pp. O190, O207, O212, O233, O237, O238, O252, O282, O304, O305, O306, O309, O313, O519, O522, O525. ISBN   0-8137-3015-5.
  2. 1 2 3 Kordule, V. (2006). "Ptychopariid trilobites in the Middle Cambrian of Central Bohemia (taxonomy, biostratigraphy, synecology)" (PDF). Bulletin of Geosciences. 81 (4): 277–304. doi: 10.3140/bull.geosci.2006.04.277 .
  3. Palmer, Allison R. (1954). "An Appraisal of The Great Basin Trilobites described before 1900". Geological Survey Professional Paper. 264-D.
  4. 1 2 3 Bridge, J.; Girthy, G.H. (1937). "A Redescription of Ferdinand Roemer's Palaeozoic types from Texas". United States Geological Survey Professional Papers (186–M).
  5. 1 2 3 4 5 Palmer, A.R. (1954). "An Appraisal of the Great Basin Middle Cambrian Trilobites described before 1900". Geological Survey Professional Paper. 264-D: 57.