Hostname: page-component-586b7cd67f-vdxz6 Total loading time: 0 Render date: 2024-11-25T20:35:06.714Z Has data issue: false hasContentIssue false
  • English
  • Français

Magnetostratigraphy of lower Cambrian strata from the Siberian Platform: a palaeomagnetic pole and a preliminary polarity time-scale

Published online by Cambridge University Press:  01 May 2009

Joseph L. Kirschvink  and
A. Yu. Rozanov
Joseph L. Kirschvink
Affiliation:
Division of Geological and Planetary Sciences, The California Institute of Technology, Pasadena, Cal. 91125, U.S.A.
A. Yu. Rozanov
Affiliation:
Palaeontological Institute, Laboratory of Ancient Skeletal Organisms, U.S.S.R. Academy of Sciences, Profsoyuznaya 113, 117868, GSP-7, Moscow, B-321, U.S.S.R.
Get access Rights & Permissions [Opens in a new window]

Abstract

Four sedimentary sections seen in continuous exposures along the Lena River on the Siberian Platform in Yakutia contain a record of the geomagnetic field during the Tommotian and Atdabanian stages of Early Cambrian time. The direction of the stable remanent magnetization indicates that the Siberian platform was located on the equator, and the corresponding palaeomagnetic pole provides a well-dated extension of the Siberian apparent polar wander path. A belt of archaeocyathid bioherms which separates two major facies zones in the lower Cambrian was positioned on and aligned more or less parallel with the palaeoequator. The geographical position of this belt appears to have tracked the southward motion of the Siberian platform during post-Tommotian time. These palaeomagnetic results combined with the extensive biostratigraphy of the Siberian Platform provide a provisional geomagnetic polarity time scale for this part of Early Cambrian time. Comparison of these results with data of similar age from Central Australia suggests that strata of Tommotian and lower Atdabanian age are not present in the Amadeus Basin of Australia.

Type
Articles
Information
Geological Magazine , Volume 121 , Issue 3 , May 1984 , pp. 189 - 203
Copyright
Copyright © Cambridge University Press 1984

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Alvarez, W., Arthur, M. A., Fischer, A. G., Lowrie, W., Napoleone, G., Silva, I. P. & Roggenthen, W. M. 1977. Upper Cretaceous–Paleogene magnetic stratigraphy at Gubbio, Italy. Geological Society of America Bulletin 88, 367–89.Google Scholar
Bingham, C. 1974. An antipodally symmetric distribution on the sphere. Annals of Statistics 2, 1201–25.CrossRefGoogle Scholar
Burek, P. J., Walter, M. R. & Wells, A. T. 1979. Magnetostratigraphic tests of lithostratigraphic correlations between lastest Proterozoic sequences in the Ngalia, Georgia and Amadeus Basins, central Australia. Bureau of Mineral Resources Journal 4 (1), 47–56.Google Scholar
Collinson, D. W. 1967. Chemical Demagnetization. In Methods in Paleomagnetism (ed. Collinson, D. W. et al. ), pp. 306–10. New York: Elsevier.Google Scholar
Collinson, D. W. 1983. Methods in Rock Magnetism and Paleomagnetism: Techniques and Instrumentation. New York; Chapman and Hall. 503pp.CrossRefGoogle Scholar
Cowie, J. W. 1978. I.U.G.S./I.G.C.P. Project 29 Precambrian–Cambrian boundary working group in Cambridge, 1978. Geological Magazine 115, 151–2.CrossRefGoogle Scholar
Debrenne, F. & Debrenne, M. 1978. Archaeocyathid faunas of the lowest fossiliferous levels of Tiout (Lower Cambrian, Southern Morocco). Geological Magazine 115, 101–9.CrossRefGoogle Scholar
Drozdova, N. A. Fonin, V. D., Grigorjeva, N. V., Ragozina, A. L., Rozanov, A. Yu., Sayutina, T. A., Voronova, L. G., Voronin, Yu. I. & Zhegallo, E. A. 1981. Precambrian Cambrian reference section in Mongolia. In Short papers for the Second International Symposium on the Cambrian system (ed. Taylor, M. E.), pp. 76–7. United States Geological Survey open file report 81–743.Google Scholar
Glaessner, M. F. & Walter, M. R. 1975. New Precambrian fossils from the Arumbera Sandstone, Northern Territory, Australia. Alcheringa 1, 59–69.Google Scholar
Epstein, A. G., Epstein, J. B. & Harris, L. D. 1977. Conodont color alteration – an index to organic metamorphism. Geological Society of America Special Paper 153, 108 pp.Google Scholar
Harland, W. B., Cox, A. V., Llewellyn, P. G., Pickton, C. A. G., Smith, A. G. & Walters, R. 1982. A Geologic Time Scale. Cambridge: Cambridge University Press. 131 pp.Google Scholar
Hedberg, H. D. 1976 International Stratigraphic Guide, a Guide to Stratigraphic Classification, Terminology and Procedure. New York: John Wiley and Sons. 200 pp.Google Scholar
Hedberg, H. A., Salvador, A. & Opdyke, N. D. 1979. Magnetostratigraphic polarity units – a supplementary chapter of the ISSC International Stratigraphic Guide. Geology 7, 578–83.Google Scholar
Keller, B. M. & Rozanov, A. Yu. (eds) (1979) Upper Precambrian and Cambrian stratigraphy of western part of the East-European Platform (in Russian). Moscow: Nauka.Google Scholar
Khramov, A. N. Petrova, G. N. & Pechersky, D. M. 1981. Paleomagnetism of the Soviet Union. In Geodynamics Series, vol. 2 (ed. McElhinny, M. W. et al. ), pp. 177–94. American Geophysical Union.Google Scholar
Kirschvink, J. L. 1978. The Precambrian–Cambrian Boundary Problem: magnetostratigraphy of the Amadeus Basin, central Australia. Geological Magazine 115, 139–50.CrossRefGoogle Scholar
Kirschvink, J. L. 1980. The least-squares line and plane and the analysis of paleomagnetic data. Geophysics Journal. Royal Astronomical Society 62, 699–718.CrossRefGoogle Scholar
Kirschvink, J. L. 1981. A quick, non-acidic chemical demagnetization technique for dissolving ferric minerals. EOS, Transactions of the American Geophysical Union 62, 849.Google Scholar
Landing, E., Nowland, G. S. & Fletcher, T. P. 1980. A microfauna associated with Early Cambrian trilobites of the Callavia zone, nothern Antigonish Highlands, Nova Scotia. Canadian Journal of Earth Science 17, 400–18.CrossRefGoogle Scholar
Lowenstam, H. A. 1950. Niagaran reefs on the Great Lakes area. Journal of Geology 48, 430–87.CrossRefGoogle Scholar
Luo, Huilin, Jiang, Zhiwen, Wu, Ziche, Song, Xueliang & Ouyang, Lin. 1982. The Sinian-Cambrian Boundary in Eastern Yunnan, China. Yunnan: People's Publishing Co. 300 pp.Google Scholar
McMenamin, M. A. S., Awramik, S. M. & Stewart, J. H. 1983. Precambrian–Cambrian transition problem in western North America. Part II. Early Cambrian skeletal fauna and associated fossils from Sonora, Mexico. Geology 11, 227–30.2.0.CO;2>CrossRefGoogle Scholar
Mehra, O. P. & Jackson, M. L. 1958. Iron oxide removal from soils and clays by dithionite-citrate system buffered with sodium bicarbonate. Clays and Clay Minerals 7, 317–27.Google Scholar
Missarzhevsky, V. V. & Mambetov, A. J. 1981. (Stratigraphy and fauna of Cambrian and Precambrian boundary beds of Maly Karatau.) Trudy Akademii Nauka SSSR 326 (in Russian).Google Scholar
Mount, J. F., Gevirtzman, D. A. & Signor, P. W. III. 1983. The Precambrian-Cambrian boundary of western North America, Part I. A Tommotian fauna in the southwestern Great Basin and its implications for the base of the Cambrian system. Geology 11, 224–6.2.0.CO;2>CrossRefGoogle Scholar
Onstott, T. C. 1980. Application of the Bingham distribution function in palaeomagnetic studies. Journal of Geophysical Research 85, 1500–10.CrossRefGoogle Scholar
Palmer, A. R. & Rozanov, A. Yu. 1976. Archaeocyatha from New Jersey: evidence for an intra-Cambrian unconformity in the North-Central Appalachians. Geology 4, 773–4.2.0.CO;2>CrossRefGoogle Scholar
Parrish, J. T., Ziegler, A. M., Scotese, C. R., Humphreville, R. G. & Kirschvink, J. L. 1983. Early Cambrian paleogeography, paleoceanography, and phosphorites. in Proterozoic and Cambrian Phosphorites (ed. Shergold, J. H. and Cook, P. J.). Cambridge University Press (in press).Google Scholar
Rozanov, A. Yu. 1966. The Cambrian Lower Boundary Problem. Moscow VINITI, pp. 92–111 (in Russia).Google Scholar
Rozanov, A. Yu. 1967. The Cambrian Lower Boundary Problem. Geological Magazine 104, 415–34.CrossRefGoogle Scholar
Rozanov, A. Yu. (ed.) 1982. The Pre-Cambrian–Cambrian boundary in the geosynclinal areas; the Joint Soviet-Mongolian Palaeontological expedition. Transactions Nauka Moscow 18, 150 pp. (in Russian).Google Scholar
Rozanov, A. Yu. & Debrenne, F. 1974. Age of archaeocyathid assemblages. American Journal of Science 274, 833–48.CrossRefGoogle Scholar
Rozanov, A. Yu., Missarzhevsky, V. V., Volkova, N. A., Voronova, L. C., Krylov, I. N., Keller, B. M., Korolyuk, I. K., Lendzion, K., Michniak, R., Pykhova, N. G. & Sidrov, A. D. 1969. The Tommotian Stage and the Cambrian Lower Boundary Problem (Raaben, M. E., ed., 1981 English translation), Amerind, New Delhi. 359 pp.Google Scholar
Rozanov, A. Yu. & Missarzhevsky, V. V. 1966. Biostratigraphy and fauna of Lower Cambrian horizons. Transactions of the Geological Institute of Moscow Nauka, 148, 126 (in Russian).Google Scholar
Rozanov, Yu. A. & Rozanov, A. Yu. 1973. [Carbonate rocks of the Precambrian–Cambrian boundary series in the middle reaches of the Aldan River, Siberia] (in Russian). Litologiya i Poleznye Iskopaemye 5, 106–11.Google Scholar
Subcommission on Magnetostratigraphic Nomenclature. 1973. Magnetic Polarity time scale. Geotimes 18, 21–2.Google Scholar