Cornulitida
Temporal range: Mid Ordovicianโ€“Late Carboniferous[1]
Cornulitid on a brachiopod valve (Upper Ordovician, SE Indiana)
Scientific classification Edit this classification
Kingdom:Animalia
Class:โ€ Tentaculita
Order:โ€ Cornulitida
Boucek, 1964
Genera

Cornulitida is an extinct order of encrusting animals from class Tentaculita, which were common around the globe in the Ordovician to Devonian oceans, and survived until the Carboniferous.[1][2][3] Organisms that may be the oldest cornulitids have been found in Cambrian sediments of Jordan.[4]

Cornulitids had shells, and were subject to predation by boring and other means from the Ordovician onwards. Many survived attacks by predators.[1] Several cornulitids were endobiotic symbionts in the stromatoporoids and tabulates.[5][6][7]

Their affinity is unknown; they have been placed in many phyla, and have been considered worms, corals, molluscs and more.[1] They appear to be closely related to other taxa of uncertain affinity, including the microconchids, trypanoporids and tentaculitids.[1]

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References

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  1. ^ a b c d e Vinn, O. (2009). "Attempted predation on Early Paleozoic cornulitids". Palaeogeography, Palaeoclimatology, Palaeoecology. 273 (1โ€“2): 87โ€“91. doi:10.1016/j.palaeo.2008.12.004. Retrieved 2014-06-11.
  2. ^ Vinn, O (2013). "Cornulitid tubeworms from the Ordovician of eastern Baltic". Carnets de Gรฉologie: 131โ€“138. doi:10.4267/2042/51214. Archived from the original on 2016-03-04. Retrieved 2024-01-31.
  3. ^ Vinn, O; Wilson, M.A. (2013). "Silurian cornulitids of Estonia (Baltica)". Carnets de Gรฉologie: 357โ€“368. doi:10.4267/2042/53034. Archived from the original on 2013-12-27.
  4. ^ Olaf Elicki (January 2011). "First skeletal microfauna from the Cambrian Series 3 of the Jordan Rift Valley (Middle East)". Memoirs of the Association of Australasian Palaeontologists. 42 (42): 153-173.
  5. ^ Vinn, O.; Mรตtus, M.-A. (2008). "The earliest endosymbiotic mineralized tubeworms from the Silurian of Podolia, Ukraine". Journal of Paleontology. 82 (2): 409โ€“414. doi:10.1666/07-056.1. S2CIDย 131651974. Archived from the original on 2016-03-04. Retrieved 2024-01-31.
  6. ^ Vinn, O.; Wilson, M.A. (2010). "Endosymbiotic Cornulites in the Sheinwoodian (Early Silurian) stromatoporoids of Saaremaa, Estonia". Neues Jahrbuch fรผr Geologie und Palรคontologie, Abhandlungen. 257: 13โ€“22. doi:10.1127/0077-7749/2010/0048. Archived from the original on 2023-11-06. Retrieved 2024-01-31.
  7. ^ Vinn, O.; Mรตtus, M.-A. (2012). "Diverse early endobiotic coral symbiont assemblage from the Katian (Late Ordovician) of Baltica". Palaeogeography, Palaeoclimatology, Palaeoecology. 321โ€“322: 137โ€“141. doi:10.1016/j.palaeo.2012.01.028. Archived from the original on 2023-12-17. Retrieved 2024-01-31.

๐Ÿ“š Artikel Terkait di Wikipedia

Cornulites

Cornulites is a genus of cornulitid tubeworms. Their shells have vesicular wall structure, and are both externally and internally annulated. They usually

Tabulata

corals with massive skeletons often contain endobiotic symbionts, such as cornulitids and Chaetosalpinx. Like rugose corals, they lived entirely during the

Ordovician

generally more mixed ecosystems, in which brachiopods, bryozoans, molluscs, cornulitids, tentaculitids and echinoderms all flourished, tabulate corals diversified

Brachiopod

Strophomenid brachiopod with attached cornulitid worm tube (Upper Ordovician, SE Indiana, USA). Brachiopod valves often serve as substrates for encrusting

Conchicolites

Conchicolites is a fossil genus of cornulitid tubeworms. Their shells lack vesicular wall structure and have a smooth lumen. They are externally covered

Trypanoporida

related to other taxa of uncertain affinity, including the microconchids, cornulitids, and tentaculitids. Spirally coiled trypanoporids (Devonian) were most

Septalites

Septalites is a genus of cornulitid tubeworms. Their shells lack vesicular wall structure and have a smooth lumen filled with numerous transverse septa

Coralloconchus

Coralloconchus is a genus of cornulitid tubeworms with small, slender, irregularly curved conical tubes with slowly increasing diameter. Tubes have thin