Delgadella
| Delgadella Temporal range: Late Atdabanian to Botomian | |
|---|---|
 | |
| a drawing of Delgadella lenaicus, Lena River, Yakutia | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| Class: | Trilobita |
| Order: | Agnostida |
| Suborder: | Eodiscina |
| Superfamily: | Eodiscoidea |
| Family: | Hebediscidae |
| Genus: | Delgadella Walcott, 1908 |
| species | |
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| Synonyms | |
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Alemtejoia, Delgadodiscus, Delgadoia, Pagetiellus, Pentagonalia | |
Delgadella is a diminutive trilobite that lived during the late Lower Cambrian (Atdabanian to Botomian) 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 transvers 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
- Delgadella occurs in the Lower Cambrian of the Russian Federation (Atdabanian, Judomia trilobite-zone, Tyuser Formation, Chekurovka village, Biskeebit River mouth near Lena River 71.0° N, 127.5° E, [2] Erkeket Formation, Mattaiya Creek, 71.5° N, 124.6° E,[3] Bergeroniellus gurarii trilobite-zone, Sinsk Formation, Algal Lens Yakutia, 61.1° N, 126.6°;[4] Botomian, Lapworthella bella small shelly-zone, Krasnoporog Formation, Sukharikha River, Krasnoyarskiy Kray, 67.2° N, 87.0° E).[5] and Spain (Atdabanian, upper part of the La Hoya member, Alconera Formation)[6]
References
- ↑ 1.0 1.1 Whittington, H. B. et al., ed. (1997). Part O, Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida. Treatise on Invertebrate Paleontology.
- ↑ 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 in Paleobiological Database http://museumu03.museumwww.naturkundemuseum-berlin.de/cgi-bin/bridge.pl?action=basicCollectionSearch&collection_no=56855
|url=missing title (help). - ↑ 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. Unknown parameter
|cited in=ignored (help) - ↑ 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: 69–88. doi:10.1016/j.palaeo.2004.01.022. Unknown parameter
|cited in=ignored (help); - ↑ 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. Unknown parameter
|cited in=ignored (help); - ↑ Eladio Liñán (Ed.). The Cambrian system in Iberia. Guadernos del Museo Minero (3). Instituto Geologico y Minero d’ Espagna. pp. 1–65.