Pricyclopyge

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Pricyclopyge
Temporal range: Ordovician
Pricyclopyge.jpg
P. binodosa
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Class: Trilobita
Order: Asaphida
Family: Cyclopygidae
Genus: Pricyclopyge
Richter & Richter, 1954
Type species
Aeglina prisca
Species
  • P. prisca(Barrande, 1872)
  • P. binodosa(Salter, 1859)
    • P. b. binodosa
    • P. b. eurycephala Fortey & Owens, 1987
    • P. b. synophthalma (Koucek, 1916)

Pricyclopyge is a genus of trilobites assigned to the family Cyclopygidae that occurs throughout the Ordovician. Pricyclopyge had an extratropical distribution, and there is evidence that it lived in darker parts of the water column (around 175m deep). Pricyclopyge has huge eyes, an inverted pear-shaped glabella, six thorax segments, with on the 3rd two small discs. [1] [2] Pricyclopyge is known from what are today China, the Czech Republic, France, and the United Kingdom. [3]

Contents

Description

Pygidium of P. longicephala Pricyclopyge longicephala pygidium CRF.jpg
Pygidium of P. longicephala

Like other cyclopygids, Pricyclopyge lacks genal spines. Pricyclopyge has six thorax segments of which the third from the front carries two very characteristic round discs that are presumed to have been bioluminescent organs, and if true, this suggests that Pricyclopyge swam upside down. It has a wide and stout axis, that tapers gradually backwards until it ends in a semicircle close to the border of the pygidium. The short side lobes (or pleurae) of the thorax segments gradually become wider further back so that the thorax is widest at its back, with the tips of the pleurae of the 6th segment sometimes enlarged, bent backwards and so bordering the pygidium. [1] The pygidium is more than twice as wide as long, the axis showing 3 or 4 clearly defined rings, while segmentation of the pleural area is barely visible. The pygidial border furrow is clear.

Eyes

Eye of P. binodosa, lenses missing, showing the arrangement of the ommatidia Pricyclopyge binodosa eye.jpg
Eye of P. binodosa, lenses missing, showing the arrangement of the ommatidia

Like all cyclopygids, Pricyclopyge has huge eyes, that largely encircle the inverted pear-shaped glabella. These eyes have a wide angle of view, both horizontal and vertical, reminiscent of the eyes of dragonflies. The individual lenses in the eyes are hexagonally arranged, with their centers approximately 0.25 mm apart. [4] Merger of both eyes, creating a visor, has appeared in several cyclopigid genera, but only in Pricyclopyge binodosa several stages in this development can be seen as a consecutive series of subspecies collected from successive zones in the late Arenig to the Llanvirn. [4] This development improves the sensitivity of the eye for objects that move relative to the eye, which might have been particularly useful under low-light conditions and when rapidly moving. The extant hyperiid amphipod Cystisoma also has such fused eyes. [5] Although the distance between the eyes varies within any one population of the earlier subspecies, the eyes only touch and merge in P. binodosa synophthalma. Monocular trilobites are always younger than closely related species with normal paired eyes, and is an example of a trend that occurred several times in parallel. [2] [4]

Ecology

It is presumed that Pricyclopyge swam upside down in dimly lit oceanic waters outside the tropic belt. It occurs together with other cyclopygids, blind or nearly blind deepwater benthic trilobites, and free-floating oceanic graptolites. [5] It probably hunted the zooplankton and may have migrated in the evening towards the surface and in the morning to greater depths, following prey and possibly avoiding some of its potential predators.

Related Research Articles

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<i>Olenoides</i> Genus of trilobites

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<i>Meteoraspis</i>

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

Lonchodomas is a genus of trilobites, that lived during the Ordovician. It was eyeless, like all raphiophorids, and had a long straight sword-like frontal spine, that gradually transforms into the relatively long glabella. Both the glabellar spine and the backward directed genal spines are subquadrate in section. Lonchodomas has five thorax segments and the pleural area of the pygidium has two narrow furrows. Lonchodomas occurred in what are today Argentina, Canada (Newfoundland), Estonia, Latvia, Norway, Sweden, the Russian Federation and the United States.

<span class="mw-page-title-main">Alokistocaridae</span>

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<i>Biceratops</i>

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<i>Conocoryphe</i>

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<i>Odontochile</i> Genus of trilobites

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

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<i>Cyclopyge</i> (trilobite) Extinct genus of trilobites

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

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<span class="mw-page-title-main">Cyclopygidae</span> Extinct family of trilobites

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<i>Pliomera</i>

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<i>Cedaria</i>

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<i>Kendallina</i> Genus of trilobites

Kendallina is a genus of parabolinoidid trilobite with an inverted egg-shaped outline, a wide headshield, small eyes, small deflected spines, 12 thorax segments and a small, short tailshield. It lived during the Late Cambrian in what are today Canada and the United States.

<i>Orygmaspis</i> Genus of trilobites

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<i>Placoparia</i> Genus of trilobites

Placoparia is a genus of trilobites of average size that lived during the late Lower to the early Upper Ordovician on the paleocontinents Gondwana, Avalonia and Laurentia, now the Czech Republic, France, Germany, Morocco, Portugal, Spain and Wales. Its headshield is semi-circular to rectangular with rounded frontal corners. It lacks eyes, but eye ridges are present. The fact that the facial sutures are opisthoparian is an exception in the otherwise proparian Cheirurina. The thorax has 11 or 12 segments, with the axis slightly wider than the ribs to its sides. The tips of the pleurae are free, which resembles an old-fashion central heating radiator. The axis in the small tailshield consists of four rings and a minute endpiece. The four pleurae end in spatulate spines that fit to corresponding indentations in the cephalon.

<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 497 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°.

<span class="mw-page-title-main">Telephinidae</span> Extinct family of trilobites

Telephinidae is a family of pelagic trilobites with large wide-angle eyes, occupying most of the free cheeks, downward directed facial spines and 9-10 thorax segments. The family is known during the entire Ordovician and occurred in deep water around the globe.

<i>Viaphacops</i>

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References

  1. 1 2 R.C. Moore, ed. (1959). Treatise on Invertebrate Paleontology. Part O – Arthropoda 1 – Arthropoda general features, Proarthropoda, Euarthropoda general features, Trilobitomorpha. Geological Society of America and University of Kansas Press.
  2. 1 2 Whittington, H. B. et al. (1997) Treatise on Invertebrate Paleontology. Part O, Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida.
  3. Paleobiology Database
  4. 1 2 3 Schoenemann, B.; Clarkson, E.N.K. (2011). "The Eyes of Bohemian Trilobites" (PDF). Geol. Výzk. Mor. Slez.: 45–50. Archived from the original (PDF) on 2016-03-04. Retrieved 2013-08-13.
  5. 1 2 McCormick, T.; Fortey, R.A. (1998). "Independent testing of a paleobiological hypothesis: the optical design of two Ordovician pelagic trilobites reveals their relative paleobathymetry". Paleobiology. 24 (2): 235–253. doi:10.1666/0094-8373(1998)024[0235:ITOAPH]2.3.CO;2. JSTOR   2401241. S2CID   132509541.