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New Late Ordovician solitary rugose coral with perforate septa

Published online by Cambridge University Press:  14 July 2015

Robert J. Elias
Robert J. Elias*
Affiliation:
Department of Earth Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada
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Abstract

Neotryplasma floweri n. sp. is an epizoic solitary rugose coral characterized by two orders of perforate, monacanthine, carinate septa, a complex axial structure of septal lobes and lamellae, and a well developed broad dissepimentarium. It occurs in the Late Ordovician (late Edenian to earliest Maysvillian; late Caradoc) Upham Dolomite Member of the Second Value Dolomite, Montoya Group, at El Paso, Texas, U.S.A. Neotryplasma Kaljo, 1957, also includes two Late Ordovician species from the Estonian S.S.R. and one from the late Middle and Late Ordovician of the northern and middle Ural region, U.S.S.R. This genus is assigned to the Neotryplasmatidae n. fam., which is placed in the Suborder Monacanthina Neuman, 1984.

Neotryplasma appears to be closest to Sumsarophyllum Lavrusevich, 1971a, from the Late Ordovician of the Zeravshan-Gissar region, U.S.S.R. This is noteworthy because Erina (1978) and Erina and Kim (1980) suggested that the latter may be a scleractinian coral of the Order Fungiida Verrill, 1865. The rugosan mode of septal insertion has been confirmed in Neotryplasma. N. floweri seems to bear close resemblance to a poorly known Ordovician coral, Cyathophyllum (?) kjerulfi Kiaer, 1932, from Caradoc–Ashgill strata in the Trondheim region of Norway.

Type
Research Article
Information
Journal of Paleontology , Volume 60 , Issue 1 , January 1986 , pp. 14 - 25
Copyright
Copyright © The Journal of Paleontology 

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References

Bruton, D. L. and Bockelie, J. F. 1982. The Løkken-Hølonda-Støren areas, p. 77–91. In Bruton, D. L. and Williams, S. H. (eds.), Field Excursion Guide, IV International Symposium on the Ordovician System. Paleontological Contributions from the University of Oslo, 279.Google Scholar
Elias, R. J. 1981. Solitary rugose corals of the Selkirk Member, Red River Formation (late Middle or Upper Ordovician), southern Manitoba. Geological Survey of Canada Bulletin 344, 53 p.Google Scholar
Elias, R. J. 1985. Solitary rugose corals of the Upper Ordovician Montoya Group, southern New Mexico and westernmost Texas. Paleontological Society Memoir 16 (Journal of Paleontology, 59(5), supp.), 58 p.Google Scholar
Erina, M. V. 1978. Rugozy, p. 64–74. In Sokolov, B. S. and Yolkin, E. A. (eds.), Pogranichnye sloi ordovika i silura Altae-Sayanskoy oblasti i Tyan-Shanya. Akademiya Nauk SSSR, Sibirskoe Otdelenie, Institut Geologii i Geofiziki, Trudy, 397.Google Scholar
Erina, M. V. and Kim, A. I. 1980. On some Ordovician Scleractinia-like corals from the South Tien-Shan. Acta Palaeontologica Polonica, 25(3–4):375–379.Google Scholar
Flower, R. H. 1961. Part I: Montoya and related colonial corals. New Mexico State Bureau of Mines and Mineral Resources Memoir 7, p. 1–97, 121–141, 150–229.Google Scholar
Hayes, P. T. 1975. Cambrian and Ordovician rocks of southern Arizona and New Mexico and westernmost Texas. U.S. Geological Survey Professional Paper 873, 98 p.Google Scholar
Hill, D. 1951. The Ordovician corals. Royal Society of Queensland Proceedings, 62(1):1–27.CrossRefGoogle Scholar
Hill, D. 1981. Part F, Coelenterata: Supplement 1, Rugosa and Tabulata, vol. 1, p. 1–378, vol. 2, p. 379–762. In Teichert, C. (ed.), Treatise on Invertebrate Paleontology. Geological Society of America and University of Kansas, Lawrence.Google Scholar
Kaljo, D. L. 1957. Codonophyllacea ordovika i llandoveri Pribaltiki. Eesti NSV Teaduste Akadeemia Juures, Loodusuurijate Seltsi Aastaraamat, 50:153–168.Google Scholar
Kaljo, D. L. and Reiman, V. M. 1958. Dva novykh vida roda Calostylis iz nizhnego silura Estonii. Eesti NSV Teaduste Akadeemia, Geoloogia Instituudi, Uurimused, 2:27–31.Google Scholar
Kiaer, J. 1932. The coral fauna of the Kalstad Limestone in Meldalen, p. 103–113. In Kiaer, J., The Hovin Group in the Trondheim Area. Norske Videnskaps-Akademi i Oslo, Skrifter, 1, Matematisk-Naturvidenskapelig Klasse, 1932, 4.Google Scholar
Kjerulf, T. 1871. Om Trondhjems stifts geologi. Nyt Magazin for Naturvidenskaberne, 18(4):1–78.Google Scholar
Lavrusevich, A. I. 1971a. Novye pozdneordovikskie rugozy Zeravshano-Gissarskoy gornoy oblasti. Paleontologicheskii Zhurnal, 1971(4):3–7.Google Scholar
Lavrusevich, A. I. 1971b. New Late Ordovician Rugosa of the Zeravshan-Gissar Mountain region. Paleontological Journal, 1971(4):421–425 (translation of Lavrusevich, 1971a).Google Scholar
Lavrusevich, A. I. 1975. Razvitie rugoz yuzhnogo Tyan-Shanya v ordovike, silure i devone, p. 124–130. In Sokolov, B. S. (ed.), Drevnie Cnidaria, vol. 2. Nauka, Sibirskoe Otdelenie.Google Scholar
Baoyu, Lin. 1965. Ordovikskie korally prov. Guychzhou i Sychuan i ikh stratigraficheskoe znachenie. Acta Palaeontologica Sinica, 13(1):64–93 (in Chinese and Russian).Google Scholar
Lindström, G. 1868. Om tvenne nya öfversiluriska koraller från Gotland. Öfversigt af Konglig Vetenskapsakademiens, Förhandlingar, 25(8):419–428.Google Scholar
Neuman, B. 1968. Two new species of Upper Ordovician rugose corals from Sweden. Geologiska Föreningens i Stockholm, Förhandlingar, 90:229–240.Google Scholar
Neuman, B. 1984. Origin and early evolution of rugose corals, p. 119–126. In Oliver, W. A. Jr., et al. (eds.), Recent Advances in the Paleobiology and Geology of the Cnidaria, Proceedings of the Fourth International Symposium on Fossil Cnidaria (and Archaeocyathids and Stomatoporoids) held in Washington, D.C., U.S.A., August, 1983. Palaeontographica Americana, 54.Google Scholar
Prantl, F. 1957. O rodu Helminthidium Lindström z českého siluru (Rugosa). Ústředního Ústavu Geologickeho, Sborník, 23:475–496.Google Scholar
Shurygina, M. V. 1973. Rugozy, p. 142–147. In Varganov, V. G., Antsygin, N. Ya., Nasedkina, V. A., Militsina, V. S. and Shurygina, M. V., Stratigrafiya i fauna ordovika srednego Urala. Ministerstvo Geologii SSSR, Uralskoe Territoryalnoe Geologicheskoe Upravlenie.Google Scholar
Soshkina, E. D. 1955. Korally, p. 118–128. In Ivanova, E. A., Soshkina, E. D., Astrova, G. G. and Ivanova, V. A., Fauna ordovika i gotlandiya nizhnego techniya r. Podkamennoy Tunguski, ee ekologiya i stratigraficheskoe znachenie, p. 93–196. In Sarycheva, T. G. (ed.), Materialy po faune i flore paleozoya Sibiri. Akademiya Nauk SSSR, Paleontologicheskii Institut, Trudy, 56.Google Scholar
Sweet, W. C. 1979. Late Ordovician conodonts and biostratigraphy of the western Midcontinent Province, p. 45–85. In Sandberg, C. A. and Clark, D. L. (eds.), Conodont Biostratigraphy of the Great Basin and Rocky Mountains. Brigham Young University Geology Studies, 26(3).Google Scholar
Verrill, A. E. 1865. Classification of polyps (Extract condensed from a synopsis of the polypi of the North Pacific Exploring Expedition, under Captains Ringgold and Rodgers, U.S.N.). Essex Institute Proceedings, 4:145–149.Google Scholar
Weyer, D. 1973. Über den Ursprung der Calostylidae Zittel 1879 (Anthozoa Rugosa, Ordoviz-Silur). Freiberger Forschungsheft, C282:23–87.Google Scholar
Weyer, D. 1982. Das Rugosa-Genus Neotryplasma Kaljo (1957) aus dem Ordoviz der europäischen UdSSR. Freiberger Forschungsheft, C366:89–95.Google Scholar
Zhavoronkova, R. A. 1972. Opisanie korallov, p. 17–55. In Tyazheva, A. P. and Zhavoronkova, R. A., Korally i brakhiopody pogranichnykh otlozheniy silura i nizhnego devona zapadnogo sklona yuzhnogo Urala. Akademiya Nauk SSSR, Bashkir Filial, Institut Geologii.Google Scholar
Zittel, K. A. von. 1879. Handbuch der Palaeontologie, I: Band 1, Abtheilung, Protozoa, Coelenterata, Echinodermata und Molluscoidea. Oldenbourg, R., 765 p. (1876–1880).Google Scholar