Delgadella

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Delgadella
Temporal range: Late Atdabanian to Botomian
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Delgadella.png
a drawing of Delgadella lenaicus, Lena River, Yakutia
Scientific classification
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Delgadella

Walcott, 1908
species
  • D. lusitanica(Delgado, 1904) (type species) = Lingulepis lusitanica
  • D. caudatus(Delgado, 1904) = Delgadodiscus caudatus, Microdiscus caudatus
  • D. lenaicus(Toll, 1899) = Microdiscus lenaicus
Synonyms

Alemtejoia, Delgadodiscus, Delgadoia, Pagetiellus, Pentagonalia

Contents

Delgadella is a diminutive trilobite that lived during the late Lower Cambrian (Atdabanian to Botomian, over 500 million years ago) and has been found in Russia (Siberian Platform, Altay Mountains), Mongolia, Spain, Italy (Sardinia), Portugal, Morocco and Canada (Newfoundland). It can be recognized by its strongly effaced headshield and tailshield, with narrow but distinct furrows and borders along its margins, and three thorax segments. [1]

Description

The headshield (or cephalon) is convex, and axial furrow that surrounds the central area (or glabella) almost obsolete, particularly on the external surface. The glabella has no transverse furrows. The border furrow is distinct and wide anteriorly, and the border distinct and narrow. The eye lobe (or palpebral lobe) is poorly defined. The free cheeks (or librigenae) are long. The thorax has three segments. The tailshield (or pygidium) has a long axis of 10 almost indiscernible rings. The furrow that defines the axis in the pygidium (or rhachis) is almost obsolete. The area outside the rhachis (or pleural zone) is usually smooth, and like on the cephalon, the border and border furrow are very narrow but distinct. [1]

Distribution

Related Research Articles

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<i>Phalagnostus</i>

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

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<i>Thoracocare</i>

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<i>Toragnostus</i>

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Ovatoryctocara is a genus of small corynexochid trilobites from the Cambrian, that lived in what now are Siberia, China, Greenland and Canada (Newfoundland). Ovatoryctocara can be recognised by the combination of the following characters: the central raised area of the cephalon is approximately cylindrical and has two rows of four triangular or round pits. The thorax only has 5 or 6 segments. The tailshield has an axis of 6 to 12 rings, the pleural furrows are well developed and the border is absent or narrow as a hair.

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<i>Cedaria</i>

Cedaria is a small, rather flat trilobite with an oval outline, a headshield and tailshield of approximately the same size, 7 articulating segments in the middle part of the body and spines at the back edges of the headshield that reach halflength of the body. Cedaria lived during the early part of the Upper Cambrian (Dresbachian), and is especially abundant in the Weeks Formation.

<i>Orygmaspis</i> Genus of trilobites

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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°.

References

  1. 1 2 Whittington, H. B.; et al., eds. (1997). Part O, Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida. Treatise on Invertebrate Paleontology.
  2. A.Y. Rozanov; V.V. Missarzhevsky; N.A. Volkova; L.G. Voronova; I.N. Krylov; B.M. Keller; I.K. Korolyuk; K. Lendzion; R. Mikhnyar; N.G. Pykhova; A.D. Sidorov (1969). "Tommotskiu jarus i problema nizhney granisty kembriya". Trudy Geoligske Institut Leningrad. 206: 1–379.cited inPaleobiological Database http://museumu03.museumwww.naturkundemuseum-berlin.de/cgi-bin/bridge.pl?action=basicCollectionSearch&collection_no=56855.{{cite web}}: Missing or empty |title= (help)[ permanent dead link ]
  3. I.V. Korovnikov (2007). "Trilobites of the Suborder Eodiscina from the Lower Cambrian of the Northeastern Siberian Platform (Khorbosuonka River Section)". Paleontological Journal. 41 (6): 614–620. doi:10.1134/s0031030107060044. S2CID   128398586.cited inPaleobiolobical Database http://museumu03.museumwww.naturkundemuseum-berlin.de/cgi-bin/bridge.pl?action=basicCollectionSearch&collection_no=96839.{{cite web}}: Missing or empty |title= (help)[ permanent dead link ]
  4. E.Y. Ivantsov; A. Y. Zhuravlev; A. V. Leguta; V. A. Krassilov; L. M. Melnikova; G. T. Ushatinskaya (2005). "Palaeoecology of the Early Cambrian Sinsk biota from the Siberian Platform". Palaeogeography, Palaeoclimatology, Palaeoecology. 220 (1–2): 69–88. doi:10.1016/j.palaeo.2004.01.022.cited inIvantsov, Andrey Yu.; Zhuravlev, Andrey Yu.; Leguta, Anton V.; Krassilov, Valentin A.; Melnikova, Lyudmila M.; Ushatinskaya, Galina T. (2005). "Palaeoecology of the Early Cambrian Sinsk biota from the Siberian Platform". Palaeogeography, Palaeoclimatology, Palaeoecology. 220 (1–2): 69–88. doi:10.1016/j.palaeo.2004.01.022.[ permanent dead link ]
  5. S. M. Rowland; V. A. Luchinina; I. V. Korovnikov; D. P. Sipin; A. I. Tarletskov; A. V. Fedoseev (1998). "Biostratigraphy of the Vendian-Cambrian Sukharikha River section, northwestern Siberian Platform". Canadian Journal of Earth Sciences. 35 (4): 339–352. Bibcode:1998CaJES..35..339R. doi:10.1139/cjes-35-4-339.cited inPaleobiological Database http://museumu03.museumwww.naturkundemuseum-berlin.de/cgi-bin/bridge.pl?action=basicCollectionSearch&collection_no=80843.{{cite web}}: Missing or empty |title= (help)[ permanent dead link ]
  6. Eladio Liñán (ed.). The Cambrian system in Iberia. Guadernos del Museo Minero. Instituto Geologico y Minero d’ Espagna. pp. 1–65.