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A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran

Published online by Cambridge University Press:  26 December 2018

Xiangdong Wang ,
Mohammad N. Gorgij  and
Le Yao
Xiangdong Wang*
Affiliation:
Center for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing 210023, China; and Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
Mohammad N. Gorgij
Affiliation:
Geology Department, Faculty of Sciences, University of Sistan and Baluchestan, Zahedan, Iran
Le Yao*
Affiliation:
Nanjing Institute of Geology and Palaeontology, and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China
*
*Corresponding author
*Corresponding author
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Abstract

Twelve rugose coral species belonging to seven genera are described and discussed based on 70 thin sections of 32 specimens collected from the Anarak section, northeast of Nain, Esfahan Province, Yazd Block, central Iran. These species include two new colonial rugose coral species, Antheria fedorowskii and Antheria robusta, and five previously named species of colonial rugose corals, Antheria lanceolata and Streptophyllidium scitulum, and solitary rugose corals, Arctophyllum jiangsiense, Caninophyllum cf. somtaiense, and Pseudotimania delicata. Five species are left in open nomenclature: Antheria sp., Arctophyllum sp., Caninophyllum sp., Nephelophyllum sp., and Yakovleviella sp. These Iranian corals are associated with the fusulinids Rauserites (several species) and Ultradaixina bosbytauensis, indicating a latest Carboniferous age (Gzhelian age). All the described genera and named species belong to the families Aulophyllidae, Bothrophyllidae, Cyathopsidae, and Kepingophyllidae, among which the family Kepingophyllidae has been previously documented only from China and Indochina. They are typical representatives of the Cathaysian rugose fauna, which was widely developed around the South China and Indochina blocks near the paleoequator and was absent from the Gondwanan and Cimmerian continents in high latitudes during the Late Pennsylvanian. Hence, the occurrence of the Cathaysian fauna from central Iran in the latest Carboniferous suggests that it may have had a close biogeographical connection with China and Indochina, which further implies its latitudinal position intermediate between the Gondwanan continent and South China and Indochina blocks during this time.

UUID: http://zoobank.org/5257d2bb-1346-4dee-8f3e-f4b1b33ba5a9

Type
Articles
Information
Journal of Paleontology , Volume 93 , Issue 3 , May 2019 , pp. 399 - 415
Copyright
Copyright © 2018, The Paleontological Society 

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References

Alsharhan, A.S., and Nairn, A.E.M., 1995, Stratigraphy and sedimentology of the Permian in the Arabian Basin and adjacent areas: a critical review, in Scholle, P.A., Peryt, T.M., and Ulmer-Scholle, D.S., eds., The Permian of Northern Pangea, Volume 2, Sedimentary Basins and Economic Resources: Berlin, Springer-Verlag, p. 187–214.Google Scholar
Badpa, M., Poty, E., Ashouri, A., and Khaksar, K., 2016, Fasciculate Kleopatrinid corals from the Bashkirian (late Carboniferous) of Sardar Formation (Ozbak-Kuh Mountains, East-Central Iran): Revista Brasileira de Palaeontologia, v. 19, p. 151–166.Google Scholar
Chi, Y.S., 1931, Weiningian (Middle Carboniferous) corals of China: Palaeontologa Sinica, series B, v. 12, p. 1–70.Google Scholar
Chwieduk, E., 2014, Palaeogeographical and palaeoecological significance of the uppermost Carboniferous and Permian rugose corals of Spitsbergen: Poznañ, Adam Mickiewicz University Press, 270 p.Google Scholar
Dobrolyubova, T.A., 1937, Solitary corals of the Myachkovian and Podolskian horizons, Middle Carboniferous, Moscow Basin: Trudy Palaeontologicheskogo Instituta, Akademiya Nauk SSSR, v. 6, p. 5–92 [in Russian with English summary].Google Scholar
Dobrolyubova, T.A., and Kabakovitsch, N.V., 1948, Some Middle and upper Carboniferous representatives of the Rugosa from the Moscow Basin: Trudy Palaeontolgicheskogo Instituta, Akademiya Nauk SSSR, v. 14, p. 5–37 [in Russian].Google Scholar
Domeier, M., and Torsvik, T.H., 2014, Plate tectonics in the late Palaeozoic: Geoscience Frontiers, v. 5, p. 303–350.10.1016/j.gsf.2014.01.002Google Scholar
Douglas, L.A., 1936, A Permo-Carboniferous fauna from Southwest Persia (Iran): Memoirs of the Geological Survey of India, Palaeontologia Indica, New Series, 22, v. 6, p. 1–59.Google Scholar
Douglas, L.A., 1950, The Carboniferous and Permian faunas of south Iran and Iranian Baluchistan: Memoirs of the Geological Survey of India, Palaeontologia Indica, New Series 22, v. 7, p. 1–56.Google Scholar
Dybowski, W.N., 1873, Monographie der Zoantharia Sclerodermata Rugosa aus der Silurformation Estlands, Nordlivlands und der Insel Gotland: Archiv für Naturkunde Liv-, Ehst- und Kurlands, v. 1, p. 415–532.Google Scholar
Ehrenberg, C.G., 1834, Beitrage zur physiologischen Kenntniss der corallenthiere im allgemeinen, und besonders des Rothen Meeres, nebst einem Versuche zur physiologischen Systematik derselben: Adhandlungen der Königlichen Akademie der Wissenschaften zu Berlin, v. 1, p. 225–380.Google Scholar
Ezaki, Y., 1989, Morphological and phylogenetic characteristics of Late Permian rugose corals in Iran: Memoirs of the Association of Australasian Palaeontologists, v. 8, p. 275–281.Google Scholar
Ezaki, Y., 1991, Permian corals from Abadeh and Julfa, Iran, West Tethys: Journal of the Faculty of Science, Hokkaido University, v. 23, p. 53–146.Google Scholar
Fan, Y.N., 1978, Rugosa, in Chengdu Institute of Geology and Mineral Resources, ed., Palaeontological Atlas of Southwest China, Sichuan, Volume Part 2: Beijing, Geological Publishing House, p. 149–210 [in Chinese].Google Scholar
Fedorowski, J., 1975, On some upper Carboniferous Coelenterata from Bjornoya and Spitsbergen: Acta Geologica Polonica, v. 25, p. 27–78.Google Scholar
Fedorowski, J., 1997, Diachronism in the development and extinction of Permian Rugosa: Geologos, Uniwersytet im. Adama Mickiewicza, Instytut Geologii, v. 2, p. 59–164.Google Scholar
Flügel, H., 1963, Korallen aus der oberen Vise-Stufe (Kueizhouphyllum-Zone) Nord-Irans: Jahrbuch der Geologischen Bundesanstalt, Wien, v. 106, p. 365–404.Google Scholar
Flügel, H., 1964, The geology of the Upper Djadjerud and Lar Valleys (N-Iran). II. Permian corals from Ruteh Limestone: Revista Italiana di Palaeontologia e Stratigrafia, v. 70, p. 403–444.Google Scholar
Flügel, H., 1968, Korallen aus der oberen Nesen-Formation (Dzhulfa-Stufe, Perm) des Zentralen Elburz (Iran): Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, v. 130, p. 275–304.Google Scholar
Flügel, H., 1972, Die palaozoischen Korallenfaunen Ost-Irans. 2. Rugosa und Tabulate der Jarmal Formation (Darwasian?, Perm): Jahrbuch der Geologischen Bundesanstalt, v. 115, p. 49–102.Google Scholar
Flügel, H., 1990, Korallen aus dem Mittel-Perm Irans: Jahrbuch der Geologischen Bundesanstalt, Wien, v. 133, p. 523–536.Google Scholar
Flügel, H., 1991, Rugosa aus dem Karbon der Ozbak-Kuh-Gruppe Ost-Irans (Teil 1): Jahrbuch der Geologischen Bundesanstalt, v. 134, p. 657–688.Google Scholar
Flügel, H., 1994, Rugosa aus dem “Mittle”-Perm des Zentralen Elburz (Iran): Abhandlungen zur Geologischen Bundes-Anstalt, v. 50, p. 97–113.Google Scholar
Flügel, H., 1995, Biostratigraphie und Korallenfaunen des Jungpalaozoikums Ost-Irans: Geologische und Paläontologische Mitteilungen Innsbruck, v. 20, p. 35–49.Google Scholar
Fomichev, V.D., 1953, Korally Rugosa i stratigrafiya sredne- i verkhnekamennougolnykh i permskikh otlozheniy Donetskogo basseyna: Leningrad, Vsesoyuznyy Nauchno-Issledovatel'skiy Geologicheskiy Institut (VSEGEI), 622 p.Google Scholar
Fontaine, H., Suteethorn, V., and Vachard, D., 1995, The Carboniferous of northeast Thailand: a review with new data: Journal of Southeast Asian Earth Sciences, v. 12, p. l–17.Google Scholar
Graf, W., 1964, Permische Korallen aus dem Zagros-Gebirge, dem Elburz und aus Azerbeidjan, Iran: Senckenbergiana Lethaea, v. 45, p. 381–432.Google Scholar
Guo, Z.S., 1983, Middle and upper Carboniferous rugose corals from southern Daxinganling (MTS. Great Khingan): Acta Palaeontologica Sinica, v. 22, p. 220–230 [in Chinese with English abstract].Google Scholar
Harker, P. 1960. Corals, brachiopods, and molluscs of Grinnell Peninsula, in Harker, P., and Thorsteinsson, R., eds., Permian Rocks and Faunas of Grinnell Peninsula, Arctic Archipelago: Geological Survey of Canada Bulletin, v. 309, p. 39–79.Google Scholar
Hill, D., 1981, Coelenterata, Part F, Supplement 1, Rugosa and Tabulata, in Teichert, C., ed., Treatise on Invertebrate Palaeontology: Lawrence, Kansas, Geological Society of America and University of Kansas Press, p. 1–762.Google Scholar
Hudson, R.G.S., 1958, Permian corals from northern Iraq: Palaeontology, v. 1, p. 174–192.Google Scholar
Jia, H.Z., Xu, Y.S., Kuang, G.D., Zhang, B.F., Zuo, Z.B., and Wu, J.Z., 1977, Anthozoa, in Hubei Institute of Geological Science, Palaeontological Atlas of South-central China, Volume 2, Upper Palaeozoic: Beijing, Geological Publishing House, p. 109–270 [in Chinese].Google Scholar
Leven, E.Ja., and Gorgij, M.N., 2006, The first find of Gzhelian fusulinids in central Iran: Stratigraphy and Geological Correlation, v. 14, p. 22–32.Google Scholar
Leven, E.Ja., and Gorgij, M.N., 2011a, First record of Gzhelian and Asselian fusulinids from the Vazhnan Formation (Sanandaj-Sirjan Zone of Iran): Stratigraphy and Geological Correlation, v. 19, p. 16–31.Google Scholar
Leven, E.Ja., and Gorgij, M.N., 2011b, Fusulinids and stratigraphy of the Carboniferous and Permian in Iran: Stratigraphy and Geological Correlation, v. 19, p. 687–776.Google Scholar
Leven, E.Ja., and Mohaddam, H.V., 2004, Carboniferous-Permian stratigraphy and fusulinids of eastern Iran: The Permian in the Bag-E-Vang section (Shirgesht area): Rivista Italiana di Palaeontologia e Stratigrafia, v. 110, p. 441–465.Google Scholar
Leven, E.Ja., and Taheri, A., 2003, Carboniferous-Permian stratigraphy and fusulinids of East Iran: Gzhelian and Asselian deposits of the Ozbak-Kuh region: Rivista Italiana di Palaeontologia e Stratigrafia, v. 109, p. 399–415.Google Scholar
Leven, E.Ja., and Vaziri, H.M., 2004, Carboniferous-Permian stratigraphy and fusulinids of Eastern Iran: The Permian in the Bage Vang Section (Shirgesht Area): Rivista Italiana di Palaeontologia e Stratigrafia, v. 110, p. 441–465.Google Scholar
Leven, E.Ja., Davydov, V.I., and Gorgij, M.N., 2006, Pennsylvanian stratigraphy and fusulinids of Central and Eastern Iran: Palaeontologia Electronica, 9.1.1A, http://palaeo-electronica.org.Google Scholar
Lewis, H.P., 1929, On the Avonian coral Caninophyllum, gen. nov. and C. archiaci (Edwards and Haime): Annals and Magazine of Natural History, v. 10, p. 456–468.Google Scholar
Milne-Edwards, H., and Haime, J.A., 1850, A monograph of the British fossil corals: Palaeontographical Society Monographs, p. 1–71.Google Scholar
Milne-Edwards, H., and Haime, J.A., 1852, A monograph of the British fossil corals: Palaeontographical Society Monographs, p. 147–210.Google Scholar
Ogar, V.V., 2010, New data on the Carboniferous corals of the Donets Basin: Palaeoworld, v. 19, p. 284–293.Google Scholar
Partoazar, H., 1995, Permian deposits in Iran: Treatise on the geology of Iran: Geological Survey of Iran, Tehran, v. 22, p. 1–340 [in Persian with English summary].Google Scholar
Poty, E., 1981, Recherches sur les tétracoralliaires et les hétérocoralliaires du viséen de la belgique: Mededelingen Rijks Geologische Dienst, v. 35-1, p. 1–161.Google Scholar
Spasskiy, N.Y., and Kachanov, E.I., 1974, Novye primitivnye rannekamennougolnye korally Altaya i Urala: Leningrad Gornyi Institut, Zapiski, v. 59, p. 48–64.Google Scholar
Toula, F., 1875, Eine Kohlenkalk-Fauna von den Barents-Inseln (Nowaja Semlja N.W.): Sitzungsberichte der Akademieder Wissenschaften in Wien, Mathematisch-Naturwissenschaftliche Klasse, v. 71, p. 527–608.Google Scholar
Vachard, D., 1996, The Carboniferous of Iran, in Wagner, R.H., Winkler, P.C.F., and Granados, L.F., eds., The Carboniferous of the World (III). IUGS Publication, v. 33, p. 491–521.Google Scholar
Verrill, A.E., 1865, Classification of polyps (Extract condensed from a synopsis of the North Pacific Exploring Expedition, under captains Ringgold and Rodgers, U.S.N.): Essex Institute Proceeding, v. 4, p. 145–149.Google Scholar
Wang, H.C., 1950, A revision of the Zoantharia Rugosa in the light of their minute skeletal structures: Philosophical Transactions of the Royal Society of London, Series B, Biological Sciences, v. 611, p. 175–264.Google Scholar
Wang, H.D., 1986, Corals, in Xiao, W.M., Wang, H.D., Zhang, L.X., and Dong, W.L., eds., Early Permian Strata and Fauna of South Guizhou: Guiyang, Guizhou People's Press, p. 199–272 [in Chinese with English summary].Google Scholar
Wang, X.D., and Sugiyama, T., 2002, Permian coral faunas of eastern Cimmerian Continent and palaeogeographical implications: Journal of Asian Earth Science, v. 20, p. 589–597.Google Scholar
Wang, X.D., Ueno, K., Mizuno, Y., and Sugiyama, T., 2001, Late Palaeozoic faunal, climatic, and geographic changes in the Baoshan block as a Gondwana-derived continental fragment in southwest China: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 170, p. 197–223.Google Scholar
Wang, X.D., Yao, L., and Lin, W., 2018, Permian rugose corals in the world, in Lucas, S.G., and Shen, S.Z., eds., The Permian Timescale: Geological Society, London, Special Publications, v. 450, p. 165–184.Google Scholar
Wu, W.S., and Kong, L., 1983, Rugose corals from the Carboniferous-Permian boundary beds in Yunnan, Guangxi and Guizhou provinces: Palaeontologia Cathayana, v. 1, p. 367–410.Google Scholar
Wu, W.S., and Zhao, J.M., 1974, Carboniferous corals, in Nanjing Institute of Geology and Palaeontology, Academia Sinica., ed., Handbook of the Stratigraphy and Palaeontology of Southwest China: Beijing, Science Press, p. 265–272 [in Chinese].Google Scholar
Wu, W.S., and Zhao, J.M., 1989, Carboniferous and Early Permian Rugosa from western Guizhou and eastern Yunnan, SW China: Acta Palaeontologica Sinica, B, v. 24, p. 1–230 [in Chinese with English summary].Google Scholar
Wu, W.S., and Zhou, K.J., 1982, Upper Carboniferous rugose corals from Kalpin, Xinjiang: Bulletin of the Nanjing Institute of Geology and Palaeontology, Academia Sinica, v. 4, p. 213–239 [in Chinese with English abstract].Google Scholar
Yu, J.Z., Lin, Y.T., Shi, Y., Huang, X.Z., and Yu, X.G., 1981, The Carboniferous and Permian corals: Changchun, Jilin People's Publishing House, 355 p. [in Chinese with English summary].Google Scholar
Zhang, X.H., 2002, The late Carboniferous and early Permian rugose corals from Ziyun County and Qinlong County, South Guizhou: Acta Palaeontologica Sinica, v. 41, p. 283–294 [in Chinese with English abstract].Google Scholar
Zhao, J.M., 1988, Corals, in Geological Institute of Guizhou Petroleum Prospecting Section and Nanjing Institute of Geology and Palaeontology, Academia Sinica, eds., Permian Fauna from South Guizhou: Guiyang, Guizhou People's Press, p. 124–161 [in Chinese].Google Scholar
Zhao, J.M., and Zhou, G.D., 1995, Records of the Kepingophyllum coral fauna from Mt. Qimantage of Qinghai: Acta Palaeontologica Sinica, v. 34, p. 575–601 [in Chinese with English summary].Google Scholar
Zheng, C.Z., 1986, Rugose corals from upper Carboniferous Maping Formation in West Guizhou and North Guangxi: Acta Palaeontologica Sinica, v. 25, p. 531–543 [in Chinese with English summary].Google Scholar
Zhu, Z.G., and Zhao, J.M., 1992, Late late Carboniferous and earliest Permian rugose corals from Jiangxi: Acta Palaeontologica Sinica, v. 31, p. 657–677 [in Chinese with English abstract].Google Scholar