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Late Cambrian radiolarian faunas and biostratigraphy of the Cow Head Group, western Newfoundland

Published online by Cambridge University Press:  14 July 2015

Mun-Zu Won  and
William J. Iams
Mun-Zu Won
Affiliation:
Department of Marine Science, Pusan National University, Pusan, 609-735, South Korea,
William J. Iams
Affiliation:
Environmental Science/Studies, Sir Wilfred Grenfell College, Memorial University, University Drive, Corner Brook, Newfoundland, Canada A2H 6P9,
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Abstract

Well-preserved Late Cambrian radiolarian faunas were recovered from carbonate rocks of the Cow Head Group of the Great Northern Peninsula of the island of Newfoundland, Canada. Several different faunal assemblages were recognized from three strata at Green Point, one from a stratum at Martin Point, and three from strata at Broom Point South in Gros Morne National Park. The faunas contain nine genera, five of which are new, and 33 species, all but two of which are new. The five new genera are Curvechidnina, Grosmorneus, Pararcheoentactinia, Ramuspiculum, and Subechidnina. Most of the genera belong to the families Archeoentactinidae, Echidninidae, Palaeospiculumidae, and Protoentactiniidae; a few taxa have an uncertain taxonomic position. Echidnina, whose taxonomic identity was uncertain, is shown to be a radiolarian.

The diversity of each of these faunas is similar, but the difference in faunal compositions among the faunas examined is distinct. From this analysis, the Late Cambrian strata between Martin Point and Green Point can be more precisely correlated, and the previous correlation has been revised. With the recovery of the conodonts in this study, the provisionally placed boundary between the Franconian and Trempealeauan at Martin Point by earlier researchers is revised and positioned between unit 30 and unit 31.

The biostratigraphic range of the co-occurring conodonts indicates that the youngest fauna described in this paper belongs to the Eoconodontus notchpeakensis Zone of late Trempealeauan age and that the other faunas (from Martin Point and Green Point) are of Franconian age.

Type
Research Article
Information
Journal of Paleontology , Volume 76 , Issue 1 , January 2002 , pp. 1 - 33
Copyright
Copyright © The Paleontological Society

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References

Aitchison, J. C. 1993. Devonian (Frasnian) radiolarians from the Gogo Formation, Canning Basin, Western Australia. Palaeontographica, Abteilung. A., 228(4–6):105–135 Google Scholar
Aitchison, J. C. 1998. A Lower Ordovician (Arenig) radiolarian fauna from the Ballantrae Complex, Scotland. Scottish Journal of Geology, 34(1):73–81 Google Scholar
Aitchison, J. C., Flood, P. G., and Malpas, J. 1998. Lowermost Ordovician (basal Tremadoc) radiolarians from the Little Port Complex, western Newfoundland. Geological Magazine, 135(3):413–419 Google Scholar
An, T.-X., Zhang, F., Xiang, W., Zhang, Y., Xu, X., Zhang, H., Jiang, D., Yang, C., Lin, L., Cui, Z., and Yang, X. 1983. The conodonts of north China and the adjacent regions. Science Publishing Company, Beijing, 223. (In Chinese)Google Scholar
Barnes, C. R. 1988. The proposed Cambrian-Ordovician global boundary stratotype and point (GSSP) in western Newfoundland, Canada. Geological Magazine, 125(4):381–414 Google Scholar
Bengtson, S. 1986. Siliceous microfossils from the Upper Cambrian of Queensland. Alcheringa, 10(3–4):195–216 Google Scholar
Deflandre, G. 1972. Nothotripodiscinus nov. gen., Radiolaire (?) aberrant à squelette creux, d'une vase du Pacifique tropical, type d'une famille nouvelle, Nothotripodiscinidae, de position systématique incertaine. C. R. Acad. sci., Paris, Volume 275, Ser. D, 229–232.Google Scholar
Dong, X., Knoll, A. H., and Lipps, J. H. 1997. Late Cambrian Radiolarians from Hunan, China. Journal of Paleontology, 71(5):753–758 Google Scholar
Druce, E. C., and Jones, P. J. 1971. Cambro-Orodovician conodonts from the Burke River structural belt, Queensland. Australia Bureau of Mineral Resources Bulletin, 110, 167 p.Google Scholar
Dumitrica, P. 1989. Internal skeletal structures of the superfamily Pyloniacea (Radiolaria), a basis of a new systematics. Revista Espannola de Micropaleontologia, Volume 21, no. 2, 207–264.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(5):882–887 Google Scholar
Fortey, R. A., and Holdsworth, B. K. 1972. The oldest known well-preserved Radiolaria. Bollettino della Societa Paleontologia Italiana, 10(1):35–41 Google Scholar
Fortey, R. A., Landing, E., and Skevington, D. 1982. The Cambrian-Ordovician boundary sections in the Cow Head Group, western Newfoundland, p. 95–129. In Bassett, M. G. and Dean, W. T. (eds.), The Cambrian-Ordovician Boundary Sections, Fossil Distribution, and Correlations. National Museum of Wales Geological Series.Google Scholar
Goto, H., and Ishiga, H. 1991. Study of Late Ordovician radiolarians from the Lachlan Fold Belt, southeastern Australia. Geological Reports of Shimane University, 10:57–62.Google Scholar
Goto, H., Umeda, M., and Ishiga, H. 1992. Middle Ordovician radiolarians from the Lachlan fold belt, southeastern Australia. Memoirs of the Faculty of Science, Shimane University, 26:131–140.Google Scholar
Haeckel, E. 1860. Uber neue, lebende Radiolarien des Mittelmeeres. Kgl. Preuss. Akad. Wiss. Berlin, Monatsber., Jahre 1860, 794–817.Google Scholar
Haeckel, E. 1862. Die Radiolarien (Rhizopoda Radiolaria), Eine Monographie. Reimer, Berlin. 572 p., 35 pls.CrossRefGoogle Scholar
Holdsworth, B. K. 1977. Paleozoic Radiolaria: Stratigraphic distribution in Atlantic borderlands, p. 167–184. In Swain, F. M., (ed.). Stratigraphic Micropaleontology of Atlantic Basin and Borderlands. Developments in Paleontology and Stratigraphy, 6, Elsevier.CrossRefGoogle Scholar
James, N. J., and Stevens, R. K. 1986. Stratigraphy and correlation of the Cambro-Ordovician Cow Head Group, western Newfoundland. Bulletin of Geological Survey of Canada, 336, 143 p.Google Scholar
Kindle, C. H. 1981. Cambrian faunas in the limestone conglomerates of western Newfoundland, p. 106–110. In Taylor, M. E. (ed.), Short Papers for the Second International Symposium on the Cambrian System. U.S. Geological Survey, Open-File Report 81–743.Google Scholar
Kindle, C. H. 1982. The C. H. Kindle Collection: Middle Cambrian to Lower Ordovician trilobites from the Cow Head Group, western Newfoundland, p. 1–17. In Current Research, pt. C, Geological Society of Canada Paper 82–1C.CrossRefGoogle Scholar
Kindle, C. H., and Whittington, H. B. 1958. Stratigraphy of the Cow Head region, western Newfoundland. Bulletin of Geological Survey of Canada, 69:315–342.CrossRefGoogle Scholar
Kozur, H. W., Mostler, H., and Repetski, J. E. 1996. Well-preserved Tremadocian primitive Radiolaria from the Windfall Formation of the Antelope Range, Eureka County, Nevada, U.S.A. Geologisch-Palaeontologisch Mitteilungen Innsbruck, 21:245–271.Google Scholar
Landing, E. 1983. Highgate gorge: Upper Cambrian and Lower Ordovician continental slope deposition and biostratigraphy, northwestern Vermont. Journal of Paleontology, 57:1149–1187.Google Scholar
Li, H.-S. 1995. New genera and species of Middle Ordovician Nassellaria and Albaillellaria from Bai-jingsi, Quilian Mountains, China. Scientia Geologica Sinica, 4(3):331–46Google Scholar
Meyen, F. J. F. 1834. Über das Leuchten des Meeres, und Beschreibung einiger Polypen und anderer niederer Thiere. In Beiträge zur Zoologie, gesammelt auf einer Reise um die Erde. Kaiserl. Leopold.-Carol. Akad. Naturforsch., Verh., Volume 16(vol, 8), suppl. 1, abh. 5: P. 125–216.Google Scholar
Miller, J. F. 1969. Conodont fauna of the Notch Peak Limestone (Cambro-Ordovician), House Range, Utah: Journal of Paleontology, 43:33–60.Google Scholar
Miller, J. F. 1980. Taxonomic revisions of some Upper Cambrian and Lower Ordovician conodonts with comments on their evolution. University of Kansas Paleontological Contributions, Paper 99, 43 p.Google Scholar
Müller, K. J. 1959. Kambrische Conodonten. Zeitschrift der deutschen geologischen Gesellschaft, 111:439–485.CrossRefGoogle Scholar
Müller, K. J., and Hinz, I. 1991. Upper Cambrian conodonts from Sweden. Fossils and Strata, 28:1–153.Google Scholar
Nazarov, B. B. 1975. Radiolaria of the Lower-Middle Paleozoic of Kazakstan. Trudy Akademiia NAUK SSSR, Geologic Institute, 275, 203 p. (In Russian)Google Scholar
Nazarov, B. B. 1977. A new radiolarian family from the Ordovician of Kazakhstan. Paleontologicheskiy Zhurnal, 11(2):165–171 Google Scholar
Nazarov, B. B., and Ormiston, A. R. 1984. Tentative system of Paleozoic Radiolaria, p. 64–87. In Petrushevskaya, M. G. and Stepanjants, S. D. (eds.), Morphology, Ecology and Evolution of Radiolaria. (Eurorad IV Symposium volume, October 1984). Zool. Inst., Leningrad, Nauka. (In Russian with English summary)Google Scholar
Nazarov, B. B., and Ormiston, A. 1986. Trends in the Development of Paleozoic Radiolaria. Marine Micropaleontology, 11:3–32.CrossRefGoogle Scholar
Nazarov, B. B., and Ormiston, A. 1993. New biostratigraphically important Paleozoic Radiolaria of Eurasia and North America, p. 22–60. In Blueford, J. R. and Murchey, B. (eds.), Radiolaria of Giant and Subgiant Fields in Asia. Micropaleontology, Special Publication Number 6.Google Scholar
Nazarov, B. B., and Popov, L. E. 1976. Radiolarians, inarticulate brachiopods and organisms of uncertain systematic position from the Middle Ordovician of eastern Kazakhstan. Paleontologicheskiy Zhurnal, 4:33–42.Google Scholar
Nazarov, B. B., and Popov, L. E. 1980. Stratigrafiya i fauna Kremnisto—Karbonatnykh tolshch ordovika kazakhstana; radiolarii i bezzamkovye brakhiopody [Stratigraphy and fauna of the siliceous-carbonate sequence of the Ordovician of Kazakhstan (Radiolarians and inarticulate brachiopods). Trudy Geologicheskiy Institut Akademiy a Nauk SSSR, 331, 190 p. (In Russian)Google Scholar
Noble, P. J. 1994. Silurian radiolarian zonation for the Caballos Novaculite, Marathon Uplift, West Texas. Bulletin of American Paleontology, 106(345), 55 p.Google Scholar
Nogami, Y. 1967. Kambrishce Conodonten von China, Teil I, Conodonten aus den oberkambrishen Kushan-Schichten: Kyoto Univ., Coll. Sci., Nen. Ser. B, 33:211–219.Google Scholar
Renz, G. W. 1990a. Late Ordovician (Caradocian) radiolarians from Nevada. Micropaleontology, 36(4):367–377 CrossRefGoogle Scholar
Renz, G. W. 1990b. Ordovician Radiolaria from Nevada and Newfoundland: a comparison at the family level. Marine Micropaleontology, 15(3–4):393–452 CrossRefGoogle Scholar
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.Google Scholar
Van Wamel, W. A. 1974. Conodont biostratigraphy of the Upper Cambrian and Lower Ordovician of northwestern Öland, south-eastern Sweden. Utrecht Micropaleontological Bulletin, 10, 126 p.Google Scholar
Wang, Y. 1993. Middle Ordovician radiolarians from the Pingliang Formation of Gansu Province, China, p. 98–114. In Blueford, J. R. and Murchey, B. (eds.), Radiolaria of Giant and Subgiant Fields in Asia. Micropaleontology, Special Publication Number 6.Google Scholar
Webby, B. D., and Blom, W. 1986. The first well-preserved radiolarians from the Ordovician of Australia. Journal of Paleontology, 60(1):145–157.CrossRefGoogle Scholar
Won, M.-Z. 1997. The proposed new radiolarian subfamily Retentactiniinae (Entactiniidae) from the Late Devonian (Frasnian) Gogo Formation, Australia. Micropaleontolgy, 43(4):371–418 Google Scholar
Won, M.-Z., and Below, R. 1999. Cambrian radiolarians from the Georgina Basin, Queensland, Australia. Micropaleontology, 45(4):325–363 Google Scholar