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Corallite increase in the Late Ordovician coral Agetolites, and its taxonomic implication

Published online by Cambridge University Press:  19 March 2019

Ning Sun ,
Robert J. Elias  and
Dong-Jin Lee
Ning Sun
Affiliation:
School of Earth Sciences and Resources, China University of Geosciences, Beijing, 100083, People's Republic of China
Robert J. Elias
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada
Dong-Jin Lee
Affiliation:
Department of Earth and Environmental Sciences, Andong National University, Andong, 36749, Republic of Korea
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Abstract

Agetolites is a problematic Late Ordovician genus possessing traits of both tabulate and rugose corals. The presence of numerous mural pores has often been considered to indicate a relation to tabulates, although an affinity to rugosans has also been proposed, based mainly on well-developed septa that alternate in length. To further consider the taxonomic position of Agetolites, growth characteristics of coralla representing three species from the Xiazhen Formation in South China are documented and assessed, focusing on modes of corallite increase. Three major modes of increase are recognized. By far the most common mode involves the development of an offset from a connective mural pore, without a clear relationship to a particular parent corallite. This mode of increase is usually associated with corner pores, but in one case occurs at a wall pore. The lateral mode of increase, which is relatively uncommon, is a typical feature in corallites along the boundary of intergrowths with stromatoporoids. The axial mode of increase is rare, occurring during rejuvenation of a damaged corallite or during regeneration following termination of a corallite. The mode of corallite increase that is characteristic of Agetolites, involving a connective mural pore and occurring without evidence of a particular parent, supports the interpretation that this genus is not a rugosan or a typical favositid tabulate. Mural pores are unknown in rugosans, and offsets arise from distinct parent corallites in favositids. The Ordovician genus Lichenaria, considered a representative of the most primitive stock of tabulate corals, shows the closest similarities with types of increase in Agetolites. Certain aspects of lateral and axial increase in Agetolites are comparable to features in a few more genera of Ordovician tabulates, further supporting a tabulate affinity. The phylogenetic relation of Agetolites to those and other tabulate genera, however, remains unresolved.

Type
Articles
Information
Journal of Paleontology , Volume 93 , Issue 5 , September 2019 , pp. 839 - 855
Copyright
Copyright © 2019, The Paleontological Society 

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References

Bae, B.-Y., Lee, D.-J., and Elias, R.J., 2006, Life-history strategies of a species of Catenipora (Tabulata; Upper Ordovician; southern Manitoba, Canada): Lethaia, v. 39, p. 141–156.10.1080/00241160600623723Google Scholar
Bae, B.-Y., Lee, D.-J., and Elias, R.J., 2008, Life-history strategies of Manipora amicarum Sinclair, 1955 (Tabulata; Upper Ordovician; southern Manitoba, Canada): Lethaia, v. 41, p. 367–381.10.1111/j.1502-3931.2008.00121.xGoogle Scholar
Bae, B.-Y., Elias, R.J., and Lee, D.-J., 2013, Growth characteristics in co-occurring Upper Ordovician species of the tabulate Catenipora from southern Manitoba, Canada: Lethaia, v. 46, p. 98–113.10.1111/j.1502-3931.2012.00326.xGoogle Scholar
Bassler, R.S., 1932, The stratigraphy of the Central Basin of Tennessee: Tennessee Division of Geology Bulletin, 38, 268 p.Google Scholar
Bassler, R.S., 1941, Lower Paleozoic tetracoral family Columnariidae: Geological Society of America Bulletin, v. 52, p. 1961.Google Scholar
Bassler, R.S., 1950, Faunal lists and descriptions of Paleozoic corals: Geological Society of America Memoir, 52, 315 p.Google Scholar
Bian, L.Z., and Zhou, X.P., 1990, Calcareous algae from the Sanqushan Formation (Upper Ordovician) at the border area between Zhejiang Province and Jiangxi Province: Journal of Nanjing University (Earth Sciences), v. 3, p. 1–15. [in Chinese]Google Scholar
Chen, X., Rong, J.-Y., Qiu, J.-Y., Han, N.-R., Li, L.-Z., and Li, S.-J., 1987, Preliminary investigation of the Late Ordovician strata of Zhuzhai in Yushan of Jiangxi, their depositional features and environment: Journal of Stratigraphy, v. 11, p. 23–34. [in Chinese]Google Scholar
Chen, Z.-Y., Kim, M.-H., Choh, S.-J., Lee, D.-J., and Chen, X., 2016, Discovery of Anticostia uniformis from the Xiazhen Formation at Zhuzhai, South China and its stratigraphic implication: Palaeoworld, v. 25, p. 356–361.Google Scholar
Coates, A.G., and Oliver, W.A. Jr., 1973, Coloniality in zoantharian corals, in Boardman, R.S., Cheetham, A.H., and Oliver, W.A. Jr., eds., Animal Colonies; Development and Function Through Time: Stroudsburg, Dowden, Hutchinson & Ross, Inc., p. 3–27.Google Scholar
Elias, R.J., Lee, D.-J., and Woo, S.-K., 2008, Corallite increase and mural pores in Lichenaria (Tabulata, Ordovician): Journal of Paleontology, v. 82, p. 408–421.10.1666/06-114.1Google Scholar
Fedorowski, J., and Jull, R.K., 1976, Review of blastogeny in Palaeozoic corals and description of lateral increase in some Upper Ordovician rugose corals: Acta Palaeontologica Polonica, v. 21, p. 37–78.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.Google Scholar
Hall, J., 1847, Paleontology of New York, v. 1, in Natural History of New York, Pt. 6: Albany, Carroll and Cook, 338 p.Google Scholar
Hill, D., 1981, Tabulata, in Teichert, C., ed., Treatise on Invertebrate Paleontology, Part F: Coelenterata, Supplement 1, Rugosa and Tabulata, 2: Boulder and Lawrence, Geological Society of America and University of Kansas, p. F430–F669.Google Scholar
Jull, R.K., 1976, Septal development during hystero-ontogeny in the Ordovician tabulate coral Foerstephyllum: Journal of Paleontology, v. 50, p. 380–391.Google Scholar
Kim, A.I., 1962, Novye rannellandoveriyskie tabulyaty Zeravshanskogo Khrebta [New early Llandoverian tabulates of the Zeravshan Mountains], in Paleontologiya i stratigraphiya Uzbekistana i sopredelnykh rayonov: Tashkent, Akademiya Nauk Uzhekskoi SSR, v. 1, p. 117–121.Google Scholar
Kim, A.I., 1966, Tabulyatomorfnye korally paleozoya Zeravshano-Gissarskoy gornoy oblasti [Tabulatomorph corals of the Paleozoic of the Zeravshan-Gissar mountain region]: Tashkent, Ministry of Geology, Uzbekistan SSR, “Fan,” p. 1–71.Google Scholar
Kim, A.I., 1974, O filogenii i polozhenii v sisteme nekotorykh tabulyatomorfnykh korallov [On the phylogeny and systematic position of some tabulatomorph corals], in Sokolov, B.S., et al. , eds., Drevnie Cnidaria [Ancient Cnidaria.]: Novosibirsk, Nauka, Sibirskoe Otdelenie, v. 1, p. 118–122.Google Scholar
Kwon, S.-W., Park, J., Choh, S.-J., Lee, D.-C., and Lee, D.-J., 2012, Tetradiid-siliceous sponge patch reefs from the Xiazhen Formation (late Katian), southeast China: a new Late Ordovician reef association: Sedimentary Geology, v. 267–268, p. 15–24.Google Scholar
Lamarck, J.B.P.A. de M. de, 1816, Histoire naturelle des animaux sans vertèbres: Paris, the author, v. 2, 568 p.Google Scholar
Lee, D.-C., 2013, Late Ordovician trilobites from the Xiazhen Formation in Zhuzhai, Jiangxi Province, China: Acta Palaeontologica Polonica, v. 58, p. 855–882.Google Scholar
Lee, D.-C., Park, J., Woo, J.-S., Kwon, Y.-K., Lee, J.-G., Guan, L.M., Sun, N., Lee, S.-B., Liang, K., Liu, L., Rhee, C.-W., Choh, S.-J., Kim, B.-S., and Lee, D.-J., 2012, Revised stratigraphy of the Xiazhen Formation (Upper Ordovician) at Zhuzhai, South China, based on palaeontological and lithological data: Alcheringa, v. 36, p. 387–404.10.1080/03115518.2012.658724Google Scholar
Lee, D.-J., and Elias, R.J., 1991, Mode of growth and life-history strategies of a Late Ordovician halysitid coral: Journal of Paleontology, v. 65, p. 191–199.10.1017/S0022336000020424Google Scholar
Lee, D.-J., and Elias, R.J., 2000, Paleobiologic and evolutionary significance of corallite increase and associated features in Saffordophyllum newcombae (Tabulata, Late Ordovician, southern Manitoba): Journal of Paleontology, v. 74, p. 404–425.Google Scholar
Lee, D.-J., and Elias, R.J., 2004, Paleobiologic features of Trabeculites maculatus (Tabulata, Late Ordovician, southern Manitoba): Journal of Paleontology, v. 78, p. 1056–1071.10.1017/S0022336000043870Google Scholar
Lee, D.-J., Jun, Y.-H., Bae, B.-Y., and Elias, R.J., 2007, Axial increase in some early tabulate corals, in Hubmann, B., and Piller, W.E., eds., Fossil Corals and Sponges; Proceedings of the 9th International Symposium on Fossil Cnidaria and Porifera, Graz 2003: Österreichische Akademie der Wissenschaften Schriftenreihe der Erdwissenschaftlichen Kommissionen, v. 17, p. 31–41.Google Scholar
Lee, M., Elias, R.J., Choh, S.-J., and Lee, D.-J., 2016, Insight from early coral-stromatoporoid intergrowth, Late Ordovician of China: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 463, p. 192–204.10.1016/j.palaeo.2016.10.010Google Scholar
Leleshus, V.L., 1963, O filogeneticheskoy svyazi mezhdu rodami Palaeofavosites i Agetolites [Phylogenetic relationship between the genera Palaeofavosites and Agetolites]: Akademiya Nauk SSSR, Paleontolicheskii Zhurnal, v. 1963, p. 144–148.Google Scholar
Li, Y., Kershaw, S., and Mu, X.N., 2004, Ordovician reef systems and settings in South China before the Late Ordovician mass extinction: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 205, p. 235–254.10.1016/j.palaeo.2003.12.010Google Scholar
Liang, K., Elias, R.J., Choh, S.-J., Lee, D.-C., and Lee, D.-J., 2016, Morphometrics and paleoecology of Catenipora (Tabulata) from the Xiazhen Formation (Upper Ordovician), Zhuzhai, South China: Journal of Paleontology, v. 90, p. 1027–1048.10.1017/jpa.2016.60Google Scholar
Lin, B.Y., 1960, Tabulata from the Upper Ordovician of the Yu-Shan region in the province of Jiangxi: Acta Palaeontologica Sinica, v. 8, p. 55–64. [in Chinese]Google Scholar
Lin, B.Y., and Chow, X.H., 1977, Late Ordovician tabulate and heliolitid corals from Zhejiang-Jiangxi provinces and its stratigraphic significance, v. 3, in Stratigraphy and Palaeontology Transactions. Beijing, Geological Publishing House, p. 108–208. [in Chinese]Google Scholar
Lin, B.Y., and Huang, H.P., 1986, Late Ordovician tabulate corals from Xinjing and Ningxia: Bulletin of the Chinese Academy of Geological Sciences, v. 12, p. 127–149. [in Chinese]Google Scholar
Lin, B.Y., Qiu, H.R., and Xu, C.C., 1984, New observations of Ordovician strata in Shetai district of Urad Front Bannor, Nei Mongol (Inner Mongolia): Geological Review, v. 30, p. 95–105. [in Chinese]Google Scholar
Lin, B.Y., Tchi, Y.Y., Jin, C.T., Li, Y.X., and Yan, Y.Y., 1988, Monograph of Palaeozoic Corals: Tabulatomorphic Corals: Beijing, Geological Publishing House, v. 1, 467 p. [in Chinese]Google Scholar
Lonsdale, W., 1845, Description of some characteristic Palaeozoic corals of Russia, in Murchison, R.I., Verneuil, E. de, and Keyserling, A. von, The Geology of Russia in Europe and the Ural Mountains: London, John Murray, v. 1, p. 591–634.Google Scholar
Mu, E.-Z., Li, J.-J., Ge, M.-Y., Chen, X., Lin, Y.-K., and Ni, Y.-N., 1993, Upper Ordovician graptolites of Central China region: Palaeontologia Sinica, New Series B, v. 189, p. 1–393. [in Chinese]Google Scholar
Nicholson, H.A., 1879, On the Structure and Affinities of the Tabulate Corals of the Palaeozoic Period: Edinburgh and London, William Blackwood and Sons, 342 p.Google Scholar
Nicholson, H.A., and Murie, J., 1878, The minute structure of the skeleton of Stromatopora and its allies: Journal of the Linnaean Society, London, Zoology, v. 14, p. 187–246.10.1111/j.1096-3642.1878.tb01833.xGoogle Scholar
Oliver, W.A. Jr., and Coates, A.G., 1987, Phylum Cnidaria, in Boardman, R.S., Cheetham, A.H., and Rowell, A.J., eds., Fossil Invertebrates: Palo Alto, Blackwell Scientific Publications, p. 140–193.Google Scholar
Pandolfi, J.M., 1989, Phylogenetic analysis of the early tabulate corals: Palaeontology, v. 32, p. 745–764.Google Scholar
Park, J., Lee, J.-H., Hong, J., Choh, S.-J., Lee, D.-C., and Lee, D.-J., 2017, Crouching shells, hidden sponges: unusual Late Ordovician cavities containing sponges: Sedimentary Geology, v. 347, p. 1–9.Google Scholar
Plusquellec, Y., 1989, Increase in Turnacipora (Tabulata), from the Tournaisian of Transcaucasia, in Jell, P.A., and Pickett, J.W., eds., Fossil Cnidaria 5: Association of Australasian Palaeontologists Memoir 8, p. 99–107.Google Scholar
Schouppé, A. von, and Oekentorp, K., 1974, Morphogenese und Bau der Tabulata unter besonderer Berücksichtigung der Favositida: Palaeontographica Abteilung A, v. 145, p. 79–194.Google Scholar
Scrutton, C.T., 1997, The Palaeozoic corals, Ι: origins and relationships: Proceedings of the Yorkshire Geological Society, v. 51, p. 177–208.Google Scholar
Scrutton, C.T., 1998, The Palaeozoic corals, II: structure, variation and palaeoecology: Proceedings of the Yorkshire Geological Society, v. 52, p. 1–57.Google Scholar
Sinclair, G.W., 1955, Some Ordovician halysitoid corals: Royal Society of Canada Transactions, Series 3, v. 49, p. 95–103.Google Scholar
Sokolov, B.S., 1955, Tabulyaty paleozoya evropeyskoy chasti SSSR,Vvedenie: Obshchie voprosy sistematiki i istorii razvitiya tabulyat [Paleozoic Tabulata of the European parts of the USSR: introduction to the general study of the systematics and development of the tabulates]: Vsesoiuznyi Neftyanoy Nauchno-Issledovatelskii Geologo-Razvedochny Institut (VNIGRI), Trudy, n.s., v. 85, 527 p.Google Scholar
Stel, J.H., 1979, Lateral increase in Paleofavosites asper (D'Orbigny, 1850) and other tabulates: Journal of Paleontology, v. 53, p. 501–505.Google Scholar
Sun, N., Lee, D.-J., and Wang, X.-L., 2014, Septal patterns in Agetolites from the Xiazhen Formation (Upper Ordovician) at Zhuzhai, Yushan County, Jiangxi Province, South China: Science China: Earth Sciences, v. 57, p. 247–257.Google Scholar
Sun, N., Elias, R.J., Choh, S.-J., Lee, D.-C., Wang, X.-L., and Lee, D.-J., 2016, Morphometrics and palaeoecology of the coral Agetolites from the Xiazhen Formation (Upper Ordovician), Zhuzhai, South China: Alcheringa, v. 40, p. 251–274.Google Scholar
Twenhofel, W.H., 1914, The Anticosti Island fauna: Geological Survey of Canada Museum Bulletin, Geological Series, 19, 38 p.Google Scholar
Wedekind, R., 1937, Einführung in die Grundlagen der historischen Geologie, II; Band; Mikrobiostratigraphie, Die Korallen- und Foraminiferenzeit: Stuttgart, Ferdinand Enke, 136 p.Google Scholar
Winchell, N.H., and Schuchert, C., 1895, Sponges, graptolites and corals from the Lower Silurian of Minnesota, in Lesquereux, L., Woodward, A., Thomas, B.W., Schuchert, C., Ulrich, E.O., and Winchell, N.H., The Geology of Minnesota; Vol. III. Pt. I of the Final Report; Paleontology: Minneapolis, Minnesota Geological and Natural History Survey, p. 55–95.Google Scholar
Xu, S.C., Elias, R.J., and Lee, D.-J., 1999, The systematic position of Agetolites: Tabulata or Rugosa?, in Abstracts, 8th International Symposium on Fossil Cnidaria and Porifera: Sendai, Japan, p. 33.Google Scholar
Yu, C.M., and Zhang, Z.C., 1963, Subclass Tabulata, in Yu, C.M., Wu, W.S., Zhao, J.M., and Zhang, Z.C., eds., Fossil Corals in China: Beijing, Science Press, p. 214–292. [in Chinese]Google Scholar
Zhang, M., Xia, F.-S., Taylor, P.D., Liang, K., and Ma, J.-Y., 2018, Upper Ordovician bryozoans from the Xiazhen Formation of Yushan, northeastern Jiangxi, East China: Palaeoworld, v. 27, p. 343–359.Google Scholar
Zhang, Y.-D., Chen, X., Yu, G.-H., Goldman, D., and Liu, X., 2007, Ordovician and Silurian Rocks of Northwest Zhejiang and Northeast Jiangxi Provinces, SE China: Hefei, University of Science and Technology of China Press, 189 p.Google Scholar