Hostname: page-component-77c89778f8-cnmwb Total loading time: 0 Render date: 2024-07-19T05:44:34.021Z Has data issue: false hasContentIssue false
  • English
  • Français

Five Viséan conodont horizons in the north of England

Published online by Cambridge University Press:  01 May 2009

Ronald L. Austin
Ronald L. Austin
Affiliation:
Department Of Geology, The University, Southampton.
Get access Rights & Permissions [Opens in a new window]

Summary

Five faunal lists of conodonts recovered from isolated Viséan outcrops in the north of England are presented. The fauna of the Bowland Shale at Burnsall, Yorkshire, and that of the Orionastraea Bed at Bordley, Yorkshire, are representative of the Gnathodus mononodosus Assemblage Zone. The fauna of the Bollandoceras hodderense Bed (B1), and that of a limestone near the top of the Worston Shale Group (B2) at Little Mearley, Lancashire, represent the Mestognathus beckmanni-Gnathodus bilineatus Assemblage Zone. The presence of conodonts in the reef limestone of Swinden, Yorkshire, is also noted.

Type
Articles
Information
Geological Magazine , Volume 105 , Issue 4 , August 1968 , pp. 367 - 371
Copyright
Copyright © Cambridge University Press 1968

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

REFERENCES

Black, W. W. 1940. The Bowland shales from Thorlby to Burnsall, Yorkshire. Trans. Leeds Geol. Ass., 5, 308–321.Google Scholar
Black, W. W. 1957. A boulder Bed in the Bowland Shales near Burnsall, Yorkshire. Trans. Leeds Geol. Ass., 7, 24–33.Google Scholar
Black, W. W., 1958. The structure of the Burnsall-Cracoe district and its bearing on the origin of the Cracoe Knoll Reefs. Proc. Yorks. geol. Soc., 20, 257–291.Google Scholar
Bond, G. 1950a. The Lower Carboniferous reef limestones of Cracoe, Yorkshire. Q. Jl geol. Soc. Land., 105, 157–188.CrossRefGoogle Scholar
Bond, G. 1950b. The nomenclature of the Lower Carboniferous “reef” Limestones in the North of England. Geol. Mag., 87, 267–278.CrossRefGoogle Scholar
Earp, J. R., MaGraw, D., Poole, E. G., Land, D. H. & Whiteman, A. J. 1961. Geology of the country around Clitheroe and Nelson (one inch Geological sheet 68, new series). Mem. Geol. Surv., U.K.Google Scholar
Garwood, E. J. & Goodyear, E. 1924. The Lower Carboniferous succession in the Settle district and along the line of the Craven Faults. Q. Jl geol. Soc. Lond., 80, 184–273.CrossRefGoogle Scholar
Rhodes, F. H. T., Austin, R. L. & Druce, E. C. 1968. British Avonian (carboniferous) conodont faunas, and their value in local and intercontinental correlation. Bull. Br. Mus. Nat. Hist. (Geol.), Supplement No. 4.Google Scholar
Walker, C. T. 1963. Size fractionation applied to geochemical studies of boron in sedimentary rocks. J. sedim. Petrol., 33, 694–702.Google Scholar
Walker, C. T. 1967. Relation of Upper Viséan Sedimentology to the Bowland Shale overlap in Yorkshire, England. Sediment. Geol., 1, 117–136.CrossRefGoogle Scholar