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Katian (Ordovician) radiolarians from the Malongulli Formation, New South Wales, Australia, a reexamination

Published online by Cambridge University Press:  14 July 2015

Paula J. Noble  and
Barry D. Webby
Paula J. Noble
Affiliation:
1Department of Geological Sciences and Engineering, University of Nevada Reno, MS 172, Reno,
Barry D. Webby
Affiliation:
2Department of Earth and Planetary Sciences, Macquarie University, North Ryde, New South Wales, 2109, Australia,
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Abstract

Upper Ordovician radiolarians are described from limestone within the Malongulli Formation in the Cliefden Caves area using revised systematics. Eight genera and 12 species are described, including the following four new species: Protoceratoikiscum crossingi, Haplotaeniatum ovatum, Haplotaeniatum prolatum, and Borisella dunhilli, and two new combinations, Borisella subulata and Haplotaeniatum spongium. All samples are dominated by Kalimnasphaera maculosa, B. subulata, and Palaeoephippium octaramosum with lesser abundances of Haplotaeniaum spp. and Inanigutta complanata, and rare occurrences of Protoceratoikicsum spp. The rare species Etymalbaillella yennienii is reported for the first time outside of China. The Malongulli Formation is upper Eastonian through lower Bolindian (Katian global stage) based on graptolite and conodont biostratigraphy. From a stratigraphic standpoint, the limestone intervals sampled appear to represent two or possibly three stratigraphically separate intervals within the Malongulli Formation. Conodonts recovered from Coppermine Creek, Angullong/Belubula, and Gleesons Creek localities occur in the lower and middle parts of the formation and fall within one conodont zone, the O. velicuspis Zone. The stratigraphic position of the limestone at the Sugarloaf Creek locality is higher, possibly as high as lower Bolindian, based on proximity to the top of the formation where Bolindian graptolites have been recovered. Despite the different stratigraphic positions of the limestones, the radiolarians contained within are essentially the same fauna, barring some differences in relative abundance in Haplotaeniatum and Palaeoephippium. The Malongulli fauna is discussed with respect to other Upper Ordovician faunas, most notably those from siliceous facies in the eastern Lachlan Orogen and from the Hanson Creek Formation of Nevada, U.S. The radiolarian species occur across different depositional environments and from a range of geographically widespread localities, which bodes well for them being recognized as biostratigraphically important faunal markers with correlation potential within the Katian.

Type
Research Article
Information
Journal of Paleontology , Volume 83 , Issue 4 , July 2009 , pp. 548 - 561
Copyright
Copyright © The Paleontological Society 

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References

Afanasieva, M. S. 1986. Radiolarians of the family Pylentonemidae. Paleontologicheskiy Zhurnal, 3:22–35.Google Scholar
Afanasieva, M. S. 2000. New Radiolarians of the orders Aculearia and Sphaerellaria from the Devonian of the Timen-Pechora Province of Russia. Pylentonemidae. Paleontologicheskiy Zhurnal, 34:1–19.Google Scholar
Aitchison, J. C. 1998. A Lower Ordovician (Arenig) radiolarian fauna from the Ballantrae Complex, Scotland. Scottish Journal of Geology, 34:73–81.CrossRefGoogle Scholar
Bergström, S. M., Finney, S. C., Chen, X., Goldman, D., and Leslie, S. A. 2006. Three new Ordovician global stage names. Lethaia, 39:287–288.CrossRefGoogle Scholar
Buckman, S. and Aitchison, J. C., 2001. Middle Ordovician (Llandeilan) radiolarians from West Junggar, Xinjiang, China. Micropaleontology, 47:359–367.CrossRefGoogle Scholar
Cooper, R. A., Maletz, J., Taylor, L., and Zalasiewicz, J. A. 2004. Graptolites: Patterns of Diversity across Paleolatitudes, p. 281–293. In Webby, B. D., Paris, F., Droser, M. L. and Percival, I. G. (eds.), The Great Ordovician Biodiversification Event, Columbia University Press, New York.CrossRefGoogle Scholar
Danelian, T. and Floyd, J. 2001. Progress in describing siliceous biodiversity from the Southern Uplands (Scotland). Transactions of the Royal Society of Edinburgh, Earth Science, 91:489–498.CrossRefGoogle Scholar
Deflandre, M. G. 1953. Radiolaires fossiles. In Grassé, P. P.Traité de Zoologie Anatomie Systématique, Biologie. Masson et Cie., Paris, 1(2):390–436.Google Scholar
Dunham, J. B. and Murphy, M.A. 1976. An occurrence of well-preserved Radiolaria from the Upper Ordovician (Caradocian), Eureka County, Nevada. Journal of Paleontology, 50:882–887.Google Scholar
Dumitrica, P., Caridroit, M., and De Wever, P. 2000. Archaeospicularia, ordre nouveau de radiolaires: une nouvelle étage pour la classification des radiolares du Paléozoique inférieur. Comptes rendus de l'Academie des Sciences, 330:563–569.Google Scholar
Ehrenberg, C. G. 1875. Fortsetzung der mikrogeologischen Studien als Gesammt übersicht der mikroskopischen Paläontologie gleichartig analysirter Gebirgsarten der Erde, mit specieller rücksicht auf den Polycystinen-Mergel von Barbados. Aus den Abhandlungen der Königlichen Akademie des Wissenschaften zu Berlin. Jahrgang 1875:1–226.Google Scholar
Ethington, R. L., Finney, S. C., Miller, J. F., Ross, R. J. Jr., and Valdes-Camin, C. 1995. Central Great Basin Transec, p. 1–50. In Cooper, J. D. (ed.), Ordovician of the Great Basin: Seventh International Symposium on the Ordovician System field-trip guidebook. Pacific Section, SEPM (Society for Sedimentary Geology) Book 78.Google Scholar
Fergusson, C. L. and Coney, P. J. 1992. Convergence and intraplate deformation in the Lachlan Fold Belt of southeastern Australia. Tectonophysics, 214:417–439.CrossRefGoogle Scholar
Fortey, R. A. and Holdsworth, K. B. 1971. The oldest known well-preserved Radiolaria. Bollettino della Societá Paleontologica Italiana, 10:35–41.Google Scholar
Glen, R. A., Meffre, S., and Scott, R. J. 2007. Benambran Orogeny in the Eastern Lachlan Orogen. Australian Journal of Earth Sciences, 54:385–415.CrossRefGoogle Scholar
Glen, R. A., Walshe, J. L., Barron, L. M., and Watkins, J. J. 1998. Ordovician convergent-margin volcanism and tectonism in the Lachlan sector of east Gondwana. Geology, 26:751–754.2.3.CO;2>CrossRefGoogle Scholar
Goldman, D., Leslie, S. A., Nõlvak, J., and Young, S. 2006. The Black Knob Ridge section, southeastern Oklahoma, USA: A Possible Global Sttratotype-section and Point (GSSSP) for the base of the Middle Stage of the Upper Ordovician Series. Ratified proposal. Website of the International Commission on Stratigraphy (http:/www.stratigraphy.org/BKR.pdf). 44 pp.Google Scholar
Goodbody, Q. H. 1986. Wenlock Palaeoscenidiidae and Entactininiidae (Radiolaria) from the Cape Phillips Formation of the Canadian Arctic Archipelago. Micropaleontology, 32:129–157.CrossRefGoogle Scholar
Goto, H. and Ishiga, H. 1991. Study of the Late Ordovician radiolarians from the Lachlan Fold Belt, Southeastern Australia. Geological Report, Shimane University, 10:57–62. (In Japanese)Google Scholar
Goto, H., Umeda, M., and Ishiga, H. 1992. Late Ordovician radiolarians from the Lachlan Fold Belt, Southeastern Australia. Memoirs of the Faculty of Science, Shimane University, 26:145–170. (In Japanese)Google Scholar
Holdsworth, B. K. 1969a. Namurian Radiolaria of the genus Ceratoikiscum from Stafford and Derbyshire, England. Micropaleontology, 15:221–229.CrossRefGoogle Scholar
Holdsworth, B. K. 1969b. The relationship between the genus Albaillella Deflandre and the ceratokiscid Radiolaria. Micropaleontology, 15:230–236.CrossRefGoogle Scholar
Iwata, K., Schmidt, B. L., Leitch, E. C., Allan, A. D. and Watanabe, T. 1995. Ordovician microfossils from the Ballast Formation (Girilambone Group) of New South Wales. Australian Journal of Earth Sciences, 42:371–376.CrossRefGoogle Scholar
Jones, M. K. and Noble, P. J. 2006. Sheinwoodian (late Early Silurian) Radiolaria from the Cape Phillips Formation, Nunavut, Canada. Micropaleontology, 32(4):289–315.CrossRefGoogle Scholar
Kozur, H. and Mostler, H. 1982. Entactinaria subordo nov., a new radiolarian suborder. Geologische-Paläontologische Mitteilungen Innsbruck, 11 (12):399–414.Google Scholar
Li, H. 1995. New genera and species of Middle Ordovician Nassellaria and Albaillellaria from Baijingsi, Qilian Mountains, China. Scientia Geologica Sinica, 4:331–346. (In Chinese)Google Scholar
MacDonald, E. W. 1998. Llandovery Secuicollactinae aand Rotasphaeridae (Radiolaria) from the Cape Phillips Formation, Cornwallis Island, Arctic Canada. Journal of Paleontology, 72:585–604.CrossRefGoogle Scholar
MacDonald, E. W. 2004. Palaeoscenidiidae (Radiolaria) from the Lower Silurian of the Cape Phillips Formation, Cornwallis Island, Nunavut, Canada. Journal of Paleontology, 78:257–274.2.0.CO;2>CrossRefGoogle Scholar
Maletz, J. and Bruton, D. L. 2007. Lower Ordovician (Chewtonian to Castlemainian) radiolarians of Spitsbergen. Journal of Systematic Palaeontology, 5:245–288.CrossRefGoogle Scholar
Moors, H. T. 1970. Ordovician graptolites from the Cliefden Caves area, Mandurama, N.S.W., with a re-appraisal of their stratigraphic significance. Proceedings of the Royal Society of Victoria, 83:253–287.Google Scholar
Nazarov, B. B. 1975. Lower and Middle Paleozoic radiolarians of Kazakhstan (research methods, systematics, stratigraphic importance) Akademia Nauk SSSR. Trudy Geologicheskii Institut (Moscow), 275:1–203. (In Russian)Google Scholar
Nazarov, B. B. 1988. Paleozoic Radiolaria. Practical Manual of Microfauna of the U.S.S.R., Vol. 2. Nedra, Leningrad. 1–232. (In Russian)Google Scholar
Nazarov, B. B. and Ormiston, A. R. 1984. Tentative system of Paleozoic Radiolaria, p. 64–87. In Petrushevskaya, M. and Stepanjants, S. D. (eds.), Morphology, ecology and evolution of Radiolaria. Zoological Institute, Academia Nauk SSSR, Leningrad. (In Russian)Google Scholar
Nazarov, B. B. and Ormiston, A. R. 1993. New biostratigraphically important Paleozoic Radiolaria of Eurasia and North America, p. 22–60. In Blueford, J. R. and Murchet, B. (eds.), Radiolaria of Giant and Subgiant Fields in Asia. Nazarov Memorial Volume. Micropaleontology Special Publication 6.Google Scholar
Nazarov, B. B. and Popov, L. E. 1980. Stratigraphy and fauna of Ordovician siliceous-carbonate deposits of Kazakhstan. Trudy Geologicheskii Institut Akademiia Nauk SSSR, 331:1–190. (In Russian)Google Scholar
Noble, P. J. 1994. Silurian radiolarian zonation for the Caballos Novaculite, Marathon uplift, West Texas, Bulletins of American Paleontology, 106(345):155. Paleontological Research Institution, Ithaca, New York.Google Scholar
Noble, P. J. 2000. Revised stratigraphy and structural relationships in the Roberts Mountains allochthon of Nevada (USA) based on radiolarian cherts, p. 439–449. In Cluer, J. K., Price, J. G., Struhsacker, E. M., Hardyman, R. F. and Morris, C. L. (eds.), Geology and Ore Deposits 2000: The Great Basin and Beyond: Symposium Proceedings. Geological Society of Nevada, Reno. May 15–18, 2000.Google Scholar
Noble, P. J., and Aitchison, J. C. 2000. Early Paleozoic radiolarian zonation. Geology, 28:367–370.2.0.CO;2>CrossRefGoogle Scholar
Noble, P. J. and Maletz, J. 2000. Radiolaria from the Telychian (Llandovery, Early Silurian) of Dalarna, Sweden. Micropaleontology, 46:265–275.CrossRefGoogle Scholar
Percival, I. G. 1976. The geology of the Licking Hole Creek area, near Walli, central-western New South Wales. Journal and Proceedings of the Royal Society of New South Wales, 109:7–23.CrossRefGoogle Scholar
Percival, I. G. 1978. Inarticulate brachiopods from the Late Ordovician of New South Wales, and their paleoecological significance. Alcheringa, 2:117–141.CrossRefGoogle Scholar
Percival, I. G. 1979. Ordovician plectambonitacean brachiopods from New South Wales. Alcheringa, 3:91–116.CrossRefGoogle Scholar
Percival, I. G. and Webby, B. D. 1996. Island benthic assemblages: With examples from the Late Ordovician of Eastern Australia. Historical Biology, 11:171–185.CrossRefGoogle Scholar
Renz, G. W. 1990. Late Ordovician (Caradocian) radiolarians from Nevada. Micropaleontology, 36:367–377.CrossRefGoogle Scholar
Riedel, W. R. 1967. Some new families of Radiolaria. Proceedings of the Geological Society of London, 1640:148–149.Google Scholar
Rigby, J. K. and Webby, B. D. 1988. Late Ordovician sponges from the Malongulli Formation of central New South Wales, Australia. Palaeontographica Americana, 56:1–147, 1–44 pls.Google Scholar
Scheibner, E. 1973. Geology of the Taralga 1:100,000 Sheet 8829. Geological Survey of New South Wales, Sydney. vi + 1–79 pp., 6 pls., plus geological map.Google Scholar
Smith, R. E. 1966. The Geology of Mandurama-Panuara. Journal and Proceedings of the Royal Society of New South Wales, 98:239–262CrossRefGoogle Scholar
Stait, B., Webby, B. D., and Percival, I. G. 1985. Late Ordovician nautiloids from central New South Wales, Australia. Alcheringa, 9:143–157.CrossRefGoogle Scholar
Trotter, J. A. and Webby, B. D. 1995. Upper Ordovician conodonts from the Malongulli Formation, Cliefden Caves area, central New South Wales. AGSO Journal of Australian Geology and Geophysics, 15:475–499.Google Scholar
Vandenberg, A. H. M. and Cooper, R. A. 1992. The Ordovician graptolite sequence of Australasia. Alcheringa, 16:33–85.CrossRefGoogle Scholar
Wakamatsu, H., Sugiyama, K. and Furutani, H. 1990. Silurian and Devonian radiolarians from the Kurosegawa Tectonic Zone, southwest Japan. Journal of Earth Science, Nagoya University, 37:157–192.Google Scholar
Wang, Y. J. 1993. Middle Ordovician radiolarians from the Pingliang Formation of Gansu Province, China, p. 98–114. In Blueford, J. R., and Murchey, B. L. (eds.), Radiolaria of giant and subgiant fields in Asia. Nazarov Memorial Volume. Micropaleontology, Special Publication 6. Micropaleontology Press, American Museum of Natural History, New York.Google Scholar
Wang, X. F., Chen, X., Chen, X. H., and Zhu, C. Y. 1996. Stratigraphical Lexicon of China. The Ordovician System. Geological Publishing House, Beijing, i–xi, 1–192.Google Scholar
Webby, B. D. 1973. Remopleurides and other Upper Ordovician trilobites from New South Wales. Palaeontology, 16:445–475.Google Scholar
Webby, B. D. 1974. Upper Ordovician trilobites from central New South Wales. Palaeontology, 17:203–252.Google Scholar
Webby, B. D. 1988. The Ordovician genus Favistina Flower and a related colonial coral from New South Wales, Australia. New Mexico Bureau of Mines and Mineral Resources, Memoir, 44:139–152.Google Scholar
Webby, B. D. and Blom, W.M. 1986. The first well-preserved radiolarians from the Ordovician of Australia. Journal of Paleontology, 60:145–167.CrossRefGoogle Scholar
Webby, B. D. and Packham, G. H. 1982. Stratigraphy and regional setting of the Cliefden Caves Limestone Group (Late Ordovician), central-western New South Wales. Journal of the Geological Society of Australia, 29:297–317.CrossRefGoogle Scholar
Webby, B. D. and Trotter, J. A. 1993. Ordovician sponge spicules from New South Wales. Journal of Paleontology, 67:28–41.CrossRefGoogle Scholar
Webby, B. D., Moors, H. T., and McLean, R. A. 1970. Malongullia and Encrinuraspis, new Ordovician trilobites from New South Wales, Australia. Journal of Paleontology, 44:881–887.Google Scholar
Webby, B. D., Zhen, Y.-Y., and Percival, I. G. 1997. Ordovician coral- and sponge-bearing associations: Distribution and significance in volcanic island shelf to slope habitats, Eastern Australia. Boletin de la Real Sociedad Española de Historia Natural (Sección Geológia), 92:163–175.Google Scholar
Webby, B. D., Cooper, R. A., Bergström, S. M., and Paris, F. 2004. Stratigraphic Framework and Time Slices, p. 41–47. In Webby, B. D., Paris, F., Droser, M. L., and Percival, I. G. (eds.), The Great Ordovician Biodiversification Event. Columbia University Press, New York.CrossRefGoogle Scholar
Won, M.-Z. 1997. Review of the family Entactiniidae (Radiolaria) and taxonomy and morphology of Entactiniidae in the Late Devonian (Frasnian) Gogo Formation, Australia. Micropaleontology, 43:333–369.CrossRefGoogle Scholar
Won, M.-Z., Blodgett, R. B., and Nestor, V. 2002. Llandoverian (Early Silurian) radiolarians from the Road River Formation of East-central Alaska and the new family Haplotaeniatumidae. Journal of Paleontology, 76:941–964.2.0.CO;2>CrossRefGoogle Scholar